Spend enough time walking along a salt marsh and you’ll eventually stop noticing the marsh rabbits.
Not because they’ve disappeared.
Because they’ve become part of the landscape.
They feed quietly along the marsh edge, slipping into the grasses when startled before appearing again somewhere you didn’t expect. Some evenings you may count half a dozen. Other days you wonder if there were ever any there at all.
Unlike the brighter cottontails many people are used to seeing, marsh rabbits are darker, with coarse brown to reddish-brown fur, a grayish underside, and a rusty cinnamon patch along the back of the neck. Even the tail gives them away. Instead of flashing bright white, it appears darker and more bluish, one reason marsh rabbits have sometimes been called “bluetails” (Chapman & Trani, 2007; Chapman & Willner, 1981).
Like so much of the marsh, they’re easy to overlook.
A marsh rabbit may look like a familiar backyard visitor, but its role reaches far beyond the grass beneath it. | Image credit: skylarkymalarkey, iNaturalist
For more than a century, naturalists have described marsh rabbits (Sylvilagus palustris) by documenting where they lived, what they looked like, and what they ate (Rhoads & Young, 1897). Those observations gave us our first understanding of the species. Today, ecology invites us to ask a different question.
What happens because marsh rabbits are here?
The answer reaches far beyond the rabbit itself.
We often measure an animal’s importance by how exciting it is to watch.
The marsh doesn’t.
The marsh measures importance by how many lives are connected to one another (Soulé et al., 2003).
Following One Rabbit
If you’ve ever taken a science class, you’ve probably learned the First Law of Conservation of Energy: energy cannot be created or destroyed. It only changes form.
For many of us, that idea remained in a textbook or written across a classroom whiteboard. It became something to memorize rather than something we expected to witness.
Yet every walk beside a salt marsh quietly brings that principle to life.
Standing beside a marsh, it’s easy to underestimate what you’re seeing. From a distance, much of it appears to be little more than grass. Yet every growing season those grasses capture enormous amounts of energy from the sun, making salt marshes among the most productive ecosystems on Earth (Frizzell, 1988).
That productivity, however, cannot remain in the plants.
It has to move.
Imagine following a single marsh rabbit through its life.
Following one marsh rabbit means following the grasses, cover, and hidden pathways that connect it to the larger marsh. | Image credit: jorgenols, iNaturalist
At only about 2.5 to 3.5 pounds, its small body holds energy gathered first by the marsh plants around it (Chapman & Trani, 2007; Chapman & Willner, 1981).The grasses it consumes become muscle, bone, blood, fur, and new life. That rabbit may one day feed a hawk, an owl, a fox, a bobcat, or a snake. Throughout its life it supports parasites. After its death it feeds scavengers, fungi, bacteria, and countless decomposers before eventually returning nutrients to the marsh where another season of growth begins.
Nothing has appeared from nowhere.
Nothing has truly disappeared.
The energy has simply changed form.
Every day, marsh rabbits transform marsh vegetation into something that can support an entirely different community of organisms (Chapman & Trani, 2007; Chapman & Willner, 1981).
The rabbit isn’t the end of the story.
In many ways, it’s where the story begins.
More Than a Meal
Spend a few minutes watching a marsh rabbit and it may not seem particularly busy.
It grazes along the marsh edge, pauses to listen, slips into dense cover, then returns to feeding when the danger seems to have passed. At first glance, it looks like a small animal moving through its day.
But even before a marsh rabbit becomes food for something else, it is already shaping the marsh around it.
Every bite influences which plants are grazed and which continue growing (Conner & Cherry, 2017). As it moves between the marsh edge, nearby cover, and slightly higher ground, the rabbit is also moving through the boundary between habitats most of us see as separate. The same dense vegetation that protects the rabbit also provides shelter for insects, reptiles, amphibians, birds, and countless other small lives moving through the marsh (Canepuccia et al., 2023; Larsen & Gray et al., 2021; Wigley & Lancia, 1998).
A marsh rabbit browses at the edge, where each ordinary bite helps move energy through the landscape. | Image credit: cadecampbell, iNaturalist
This is why the rabbit matters before the hawk ever appears.
Its value is not limited to becoming prey. Its ordinary life helps move energy, shape vegetation, and connect habitats long before that energy travels farther up the food web (Chapman & Trani, 2007; Chapman & Willner, 1981; Conner & Cherry, 2017).
Perhaps that is the quiet work of a marsh rabbit.
Not simply feeding something else.
But helping hold together the conditions that allow so much else to live there.
Why There Are So Many
Sometimes marsh rabbits seem to be everywhere — in yards, along road edges, near parking lots, and wherever the Spartina meets slightly higher ground.
A young marsh rabbit beside an adult shows the visible side of abundance, but reproduction is only part of the story. | Image credit: Wolfgang, iNaturalist
The easy explanation is that rabbits reproduce quickly. They can produce several litters in a year, often three to seven, with roughly 15 to 20 young produced annually under favorable conditions (Holler & Conaway, 1979).
That is true, but it is not the whole story.
Nature rarely invests heavily in something that does not matter. In a marsh, abundance is not waste. It is part of the system.
Marsh rabbits live under constant pressure. Every choice — where to feed, when to move, when to freeze, and when to disappear into the grasses — is shaped by predators, tides, weather, and the daily balance between finding food and becoming food (Hill et al., 2019; Holler & Conaway, 1979).
Predators influence far more than the animals they catch. Their presence can change where prey feed, how long they remain exposed, and how energy moves through the landscape (Suraci et al., 2019). When predator communities shift, those changes can ripple through the food web in ways that affect many other species (Bransford et al., 2024; Jiménez et al., 2019) .
Seen this way, abundant marsh rabbits are not simply evidence of successful reproduction.
They are evidence of how much work this one ordinary species performs.
The Rabbit You Didn’t See
Perhaps this also explains something you’ve probably noticed yourself.
One moment several marsh rabbits are feeding along the marsh edge.
You look away for only a moment.
When you look back, they’re gone.
They haven’t left the marsh.
Unlike many rabbits people are used to seeing, marsh rabbits are strong swimmers. Water is not simply something they avoid; it is part of the landscape they know how to use. In a place shaped by tides, wet ground, and narrow edges of cover, the ability to move through water helps explain how they can vanish so completely without ever leaving the marsh (Chapman & Trani, 2007; Chapman & Willner, 1981).
The same dense vegetation that feeds them also protects them. Slight changes in elevation, the rhythm of the tides, the angle of the evening sun, and generations of natural selection have shaped an animal that survives by knowing exactly when to be seen — and when not to be (Chapman & Willner, 1981; Holler & Conaway, 1979).
The rabbit disappeared from sight.
Its place in the marsh never did.
Looking at the Marsh Differently
The next time you notice a marsh rabbit quietly feeding along the marsh edge, pause before it disappears.
What once looked like an ordinary rabbit is now something entirely different.
Not because the rabbit has changed.
But because you can now see the countless connections passing through it (Soulé et al., 2003).
And once you see those connections, the marsh becomes harder to overlook.
A marsh rabbit slips back into the edge, leaving only a glimpse of the connections still moving through the marsh. | Image credit: maxnel, iNaturalist
References
Bransford, T. D., Harris, S. A., & Forys, E. A. (2024). Seasonal variation in mammalian Mesopredator spatiotemporal overlap on a barrier island complex. Animals, 14(16), 2431. https://doi.org/10.3390/ani14162431
Canepuccia, A. D., Fanjul, M. S., & Iribarne, O. O. (2023). Global distribution and richness of terrestrial mammals in tidal marshes. Diversity and Distributions, 29(5), 598-612. https://doi.org/10.1111/ddi.13683
Chapman, B. R., & Trani, M. K. (2007). Marsh Rabbit (Sylvilagus palustris). In The Land Manager’s Guide to Mammals of the South (pp. 247-251). Durham, NC: The Nature Conservancy; Atlanta, GA: U.S. Forest Service.
Conner, L. M., & Cherry, M. J. (2017). Considering Herbivory and Predation in Forest Management. In Ecological Restoration and Management of Longleaf Pine Forests (1st ed., p. 12). CRC Press.
Frizzell, E. K. (1988). Mammals and Wetlands. In The Ecology and Management of Wetlands: Volume 1: Ecology of Wetlands (1st ed., pp. 213-226). Croom Helm Ltd.; Timber Press.
Hill, J. E., DeVault, T. L., & Belant, J. L. (2019). Cause‐specific mortality of the world’s terrestrial vertebrates. Global Ecology and Biogeography, 28(5), 680-689. https://doi.org/10.1111/geb.12881
Holler, N. R., & Conaway, C. H. (1979). Reproduction of the marsh rabbit (Sylvilagus palustris) in South Florida. Journal of Mammalogy, 60(4), 769-777. https://doi.org/10.2307/1380192
Jiménez, J., Nuñez-Arjona, J. C., Mougeot, F., Ferreras, P., González, L. M., García-Domínguez, F., Muñoz-Igualada, J., Palacios, M. J., Pla, S., Rueda, C., Villaespesa, F., Nájera, F., Palomares, F., & López-Bao, J. V. (2019). Restoring APEX predators can reduce mesopredator abundances. Biological Conservation, 238, 108234. https://doi.org/10.1016/j.biocon.2019.108234
Larsen-Gray, A. L., Loeb, S. C., & Kalcounis-Rueppell, M. C. (2021). Rodent population and community responses to experimental, large scale, long-term coarse Woody debris manipulations. Forest Ecology and Management, 496, 119427. https://doi.org/10.1016/j.foreco.2021.119427
Macarthur, R., & Levins, R. (1967). The limiting similarity, convergence, and divergence of coexisting species. The American Naturalist, 101(921), 377-385. https://doi.org/10.1086/282505
Rhoads, S. N., & Young, R. T. (1897). Notes on a Collection of Small Mammals from Northeastern North Carolina. Proceedings of the Academy of Natural Sciences of Philadelphia, 49, 303-312. https://www.jstor.org/stable/4062279?seq=1
Soulé, M. E., Estes, J. A., Berger, J., & Del Rio, C. M. (2003). Ecological effectiveness: Conservation goals for interactive species. Conservation Biology, 17(5), 1238-1250. https://doi.org/10.1046/j.1523-1739.2003.01599.x
Suraci, J. P., Clinchy, M., Zanette, L. Y., & Wilmers, C. C. (2019). Fear of humans as APEX predators has landscape‐scale impacts from mountain lions to mice. Ecology Letters, 22(10), 1578-1586. https://doi.org/10.1111/ele.13344
Wigley, T. B., & Lancia, R. A. (1998). Wildlife Communities. In Southern Forested Wetlands (1st ed., p. 32). Routledge.
A reader recently asked me about five birds he had seen over the sounds of Surf City last weekend. He was convinced they were five different kinds of “sea hawks.”
At first glance, it was an understandable conclusion.
Each bird was large. Each spent time soaring overhead or hesitating up high over the water. Each occupied the same stretch of coastal North Carolina sky.
Yet every photograph and description reflected the same species: an osprey.
Distance has a way of simplifying wildlife. Colors disappear. Markings fade. Details are lost. What remains is a silhouette against the sky.
Most of us learn to recognize birds by their appearance. Raptors are often easier to understand by their behavior.
What is the bird doing?
Is it hovering over the water?
Circling without flapping?
Perched motionless on a fence post?
Drifting above a marsh?
Crossing silently through the trees after sunset?
The answer often reveals more than the feathers.
The skies above Onslow County are shared by a community of predators. Some hunt fish. Some hunt rodents. Some hunt insects. Some hunt other birds. Some hunt only at night. Others serve as nature’s cleanup crew.
At a distance they may look similar.
Spend enough time watching them, however, and the differences become impossible to miss.
Following the Fish
Osprey: The Fisherman
If there is a signature bird of the coast, it may be the osprey (Pandion haliaetus).
You notice one long before you identify it. The bird appears above a creek, river, or stretch of open water, turns into the wind, and suddenly seems to stop moving. For a few seconds it hangs there, suspended above the surface before plunging feet-first toward the water below.
That moment of hesitation is not hesitation at all.
The bird is making a final decision.
Water distorts light. Fish change direction. Wind roughens the surface. What appears obvious from a dock or kayak becomes much more complicated from above. The osprey’s brief hover allows it to judge distance, depth, and movement before committing to the dive (Poole, 1989; Bierregaard et al., 2020).
The splash usually draws everyone’s attention.
The fish often draws the next question.
Watch an osprey leave the water carrying a mullet or menhaden and it is difficult not to wonder how the bird manages to hold onto it. Fish are essentially living bars of soap wrapped in muscle, built to slip through water and escape predators. Osprey solve that problem with feet lined by tiny backward-facing spicules and a reversible outer toe that help secure slippery prey (Poole, 1989; Bierregaard et al., 2020).
Then, almost as soon as the bird becomes airborne, something else happens.
The fish turns.
Within seconds the osprey has repositioned its catch so the fish faces forward. What looks like a small adjustment saves energy over the course of the flight. A fish carried sideways catches air. A fish carried headfirst moves through it. Often the bird gives its catch a vigorous shake as it climbs away from the water, shedding excess water before continuing on its way. Together, these adjustments reduce drag and make transporting a heavy, slippery meal through the air more efficient (Allen et al., 2018; Poole, 1989; Bierregaard et al., 2020).
Around nesting season, however, it is often the noise rather than the fishing that gets people’s attention.
Osprey rarely seem quiet.
Calls echo from nesting platforms, channel markers, dead trees, and utility poles throughout the breeding season. Adults announce arrivals. Mates communicate with one another. Young birds call constantly whenever food appears nearby. What sounds chaotic from a distance is often a family carrying on a conversation (Bierregaard et al., 2020).
By late summer, that family becomes easier to see.
Several birds may gather near a nest, perched along the same stretch of water where they have spent months raising young. Then, without warning, they take to the air together. The younger birds follow the adults across creeks, marshes, and open water, practicing turns, landings, and the flight skills that will eventually carry them south. What appears at first to be a loose gathering of osprey is often a family still learning from one another long after the young birds have left the nest (Poole, 1989; Bierregaard et al., 2020).
To boaters, it is a channel marker in the New River in Jacksonville, NC. To an osprey, it is home. Many coastal nests are rebuilt and expanded year after year, becoming landmarks visible across the water. | Image credit: A. Mitchell
The nests themselves remain long after the birds have departed.
Many osprey return to the same sites year after year, adding sticks, repairing damage, and expanding structures that can eventually become enormous. What begins as a modest nest slowly grows into a landmark visible from hundreds of yards away (Poole, 1989; Bierregaard et al., 2020).
For many coastal residents, those nests become part of the landscape.
And when spring returns, so do the birds that built them.
Bald Eagle: The Opportunist
If you spend enough time around the water, eventually you’ll see it happen.
An osprey leaves the surface carrying a fish. For a few moments, everything appears normal. Then a second bird enters the scene.
Larger.
Heavier.
Built on an entirely different scale.
The bald eagle (Haliaeetus leucocephalus) begins to follow.
What started as a successful fishing trip suddenly becomes a chase.
From below, the interaction can look almost personal. The osprey twists and climbs. The eagle closes the distance. Sometimes the osprey escapes. Sometimes it drops the fish. The eagle wheels downward after the falling meal while the osprey continues on empty-taloned.
Why go through all that trouble?
Because catching a fish requires energy.
An osprey may spend considerable time searching the water, hovering above the surface, adjusting for currents, and committing to a dive before finally securing a meal. An eagle watching from a nearby perch can recognize that success immediately. From the eagle’s perspective, the fish has already been found. The difficult part of the hunt is over (Buehler, 2020).
This often leads people to wonder whether bald eagles are better fishermen than osprey.
The answer depends on how you define fishing.
If the goal is catching fish, the osprey remains the specialist. Nearly every aspect of its anatomy is designed around that task. Its feet grip slippery prey with remarkable efficiency, and its entire hunting strategy revolves around locating fish beneath the water’s surface.
A bald eagle approaches the world differently.
Rather than specializing in a single food source, eagles take advantage of opportunities wherever they find them. Fish remain important, particularly along the New River, Stump Sound, the Intracoastal Waterway, and the countless creeks that thread through coastal marshes. Yet waterfowl, mammals, reptiles, and carrion can also become part of the menu (Buehler, 2020).
A closer look at their feet reveals those differences. Osprey feet are designed to hold fish. Eagle talons are designed to seize and restrain a wider variety of prey. One bird is built around precision. The other is built around versatility (Buehler, 2020).
That versatility helps explain why bald eagles have become increasingly common sights along the Onslow County coast. Open water, abundant prey, expansive marshes, and large trees provide everything they need. Whether soaring above an estuary, perched along a creek, or watching from a pine overlooking the water, eagles occupy a position near the top of the coastal food web (Buehler, 2020).
And every so often, that position allows them to let someone else do the fishing.
The Hunters of Marsh and Forest
Red-shouldered Hawk: The Watcher on the Fence
Not every raptor announces itself from the sky.
Some introduce themselves by showing up in the yard.
You glance out the window and notice a hawk perched on the fence. Hours later it seems to be in exactly the same place. The next morning it is back again.
Eventually curiosity takes over.
What is it watching?
Perched above a yard in Jacksonville, NC, a red-shouldered hawk waits for movement. From elevated vantage points, these woodland hunters watch patiently for opportunities hidden within the landscape below. | Image credit: A. Mitchell
Many people assume the hawk is focused on the house, the dog, or the family moving through the yard.
In reality, the bird is usually paying attention to everything else.
A well-maintained yard often provides excellent hunting habitat. Frogs move through flower beds. Lizards bask along retaining walls. Small snakes hunt beneath shrubs. Mice travel fence lines and wood piles. The red-shouldered hawk watches for movement, waiting for the landscape to reveal itself (Dykstra et al., 2020).
That patient approach reflects the habitats these birds prefer.
Unlike the open-country red-tailed hawk, red-shouldered hawks (Buteo lineatus) are closely tied to places where woods and water meet. Creek corridors, swamp edges, ponds, marshes, and bottomland forests provide the cover and diversity of prey they rely upon (Dykstra et al., 2020).
A red-shouldered hawk feeds on captured prey in a parking lot. While often associated with swamps and wooded wetlands, these adaptable hunters frequently take advantage of opportunities in suburban landscapes. | Image credit: A. Mitchell
Along the coast, those habitats frequently overlap with where people live.
The fence post is simply the best seat in the house.
From there, the hawk can watch an entire ecosystem unfold beneath it.
Red-tailed Hawk: Master of the Open Sky
A red-tailed hawk (Buteo jamaicensis) – and my personal favorite bird – often attracts attention by doing remarkably little.
You notice one circling high above a field.
Several minutes later it is still there.
The wings barely move.
At first, most people wonder how the bird can remain in the air for so long without flapping. The answer lies in the atmosphere itself. As the ground warms, pockets of heated air rise into the sky. Red-tailed hawks locate these invisible thermals and circle within them, gaining altitude while expending very little energy (Kerlinger, 1989; Preston & Beane, 2024).
But staying aloft is only part of the story.
The real question is why the bird wants to be up there in the first place.
The answer becomes clearer when compared to the red-shouldered hawk.
A red-shouldered hawk often hunts by focusing on a particular place. A pond edge. A marsh creek. A backyard. It watches patiently from a perch, waiting for the landscape to reveal movement (Dykstra et al., 2020).
A red-tailed hawk takes the opposite approach.
Rather than concentrating on one corner of the landscape, it climbs high enough to see how all of those pieces connect. Fields blend into hedgerows. Roadsides meet forest edges. Open ground transitions into cover. From above, what appear to be separate places from the ground become a single hunting landscape.
That broader view is the red-tail’s specialty.
What appears to us as an empty field is filled with clues. A rabbit pauses along a fence line. A squirrel breaks from cover. A mouse rustles through the grass. The bird is not searching for a specific animal. It is searching for movement, patterns, and opportunities spread across hundreds of acres (Preston & Beane, 2024).
The thermal keeps the hawk aloft long enough to gather that information. Height becomes an advantage. Distance becomes information.
The bird is not circling because it has nowhere else to be.
It is circling because the sky offers the best view.
And from that vantage point, one movement in the wrong place at the wrong time is often all it takes.
Cooper’s Hawk: The Pursuit Hunter
If you maintain a bird feeder long enough, sooner or later the yard will go silent.
One moment cardinals, doves, and finches are moving between the feeder and nearby trees.
The next, everything disappears.
Then a gray blur streaks through the yard.
The first time you see it happen, it feels almost impossible that a bird that large could move that quickly through such a cluttered space.
Unlike the red-tailed hawk searching from hundreds of feet above the landscape or the red-shouldered hawk watching patiently from a perch, the Cooper’s hawk (Astur cooperii) hunts in motion. It is built for pursuit (Rosenfield et al., 2025).
Its long tail acts like a rudder while relatively short wings allow it to twist, turn, and accelerate through spaces that would seem impossible for most raptors. Branches, fences, shrubs, and backyard obstacles that slow other birds become part of the chase (Rosenfield et al., 2025).
That agility allows the hawk to exploit something many predators cannot.
Confusion.
A flock of birds startled into flight rarely moves in a straight line. Individuals scatter in different directions, darting through vegetation and searching for cover. The Cooper’s hawk follows.
What appears chaotic to us is a hunting opportunity to the hawk.
Yet not every backyard attracts a Cooper’s hawk.
If you’ve ever noticed that these birds seem more common in some neighborhoods than others, the surrounding landscape is often the reason. Cooper’s hawks favor places where trees, forest edges, wooded corridors, and open spaces meet. Those transitions provide both cover and opportunity, allowing the bird to move quickly between concealment and pursuit (Rosenfield et al., 2025).
A bird feeder placed within that landscape can become part of the story, not because the feeder attracts the hawk, but because it concentrates movement. Birds travel between the feeder and nearby cover. The hawk is already watching the area. The feeder simply makes activity easier to find.
Which is why the sudden silence is often the first clue.
Long before most people see the hawk, the birds have already noticed it.
For a few moments, the yard belongs to the fastest hunter in the neighborhood.
The Hunters of the Air
Mississippi Kite: Catching the Wind
At first glance, a Mississippi kite (Ictinia mississippiensis) looks like it should behave like any other hawk.
It drifts overhead with long, pointed wings, barely moving as it rides the summer air. Then it suddenly changes direction, banking sharply, twisting through the sky, and accelerating after something too small for most people to see.
The first time you notice it, the behavior feels strange.
What is that hawk chasing? Is it chasing dragonflies?
The bird banks again, then again, each turn seeming impossibly precise. Whatever it is pursuing appears far too small to interest a raptor. Yet the longer you watch, the clearer the answer becomes.
While many hawks spend their time searching the ground for prey, Mississippi kites have turned the air itself into a hunting ground. Dragonflies, cicadas, beetles, and other flying insects become meals captured directly on the wing. What appears to be effortless wandering is often an active hunt unfolding overhead (Parker, 2020).
That hunting style explains why they seem so different from other raptors.
The red-shouldered hawk watches a particular place. The red-tailed hawk surveys an entire landscape. The Cooper’s hawk chases prey through trees and backyards. The Mississippi kite is hunting somewhere entirely different.
Its long wings and graceful flight allow it to maneuver with remarkable precision, changing direction quickly as insects dart, climb, and shift with the wind (Parker, 2020).
The same warm air currents that help other raptors gain altitude also gather flying insects into concentrated pockets, creating opportunities for a predator adapted to exploit them (Parker, 2020).
The result is a bird that often feels more like a swallow than a hawk.
An osprey may be hunting fish below. A red-tailed hawk may be watching a field nearby. A Cooper’s hawk may be moving along a forest edge. Above them all, a Mississippi kite may be feeding on insects carried by the same air currents that support the rest of the ecosystem.
The bird is not ignoring the landscape beneath it.
It has simply found opportunity in a place most predators never think to look.
For the Mississippi kite, the sky is not a pathway.
It is habitat.
The Cleanup Crew
Turkey Vulture: Death Becomes Renewal
A turkey vulture (Cathartes aura) lands on your roof and suddenly everyone becomes concerned.
To us, it looks like a warning. To the vulture, it is simply another perch from which to read the landscape. | Image credit: A. Mitchell
Some people take it as a bad omen. Others wonder if something nearby has died. Before long, the bird becomes the center of attention despite doing little more than sitting still.
The turkey vulture, meanwhile, is completely unaware of the stories being told about it.
Most of the time, something far less dramatic is happening.
A rooftop provides warmth on a cool morning, a place to dry rain-soaked feathers, or a convenient perch where rising air currents can be reached without much effort. The bird is not predicting death. It is simply taking advantage of the landscape (Kirk & Mossman, 2020).
Yet the association exists for a reason.
Unlike the hawks and eagles we have encountered so far, turkey vultures are searching for something very different. They are not looking for prey. They are looking for what remains after life has already moved on.
A dead fish along the shoreline.
A raccoon hidden in roadside vegetation.
A deer beyond the edge of a forest.
But how do they find it?
Part of the answer can be seen on the bird’s face. If you are fortunate enough to observe a turkey vulture through binoculars or at close range, you may notice something unusual about its nostrils, or nares. Unlike our own noses, the openings pass completely through the beak. In the right light, you can literally see from one side of the nostril to the other (Kirk & Mossman, 2020).
A close comparison of a turkey vulture (top) and black vulture (bottom) reveals one clue to how they read the landscape differently. Turkey vultures use an exceptional sense of smell to locate carrion, while black vultures depend more on vision and the behavior of other vultures. Arrows highlight differences in the nostril openings of the two species. | Image credit: T. Lisney
That adaptation supports one of the most powerful senses of smell in the bird world. While many raptors rely primarily on vision, turkey vultures are able to detect the scent of carrion from remarkable distances, allowing them to locate food sources hidden beneath vegetation and, in some cases, even beneath the soil itself (Grigg et al., 2017; Kirk & Mossman, 2020).
Finding carrion, however, is only part of the challenge.
Consuming it presents an entirely different set of problems.
The turkey vulture’s bald head, which many people find unsettling, is actually an important adaptation. Unlike a feathered head that could trap blood, bacteria, and other organic material, the bare skin can be cleaned much more easily after feeding. What gives the bird its ominous appearance also helps protect it from the very things it eats (Roggenbuck et al., 2018).
The same is true inside the bird.
Turkey vultures possess an extraordinarily acidic digestive system capable of destroying many of the bacteria and pathogens that would make other animals sick. Organisms responsible for diseases such as anthrax, botulism, cholera, and salmonella are often neutralized during digestion, allowing the vulture to safely consume material that would be dangerous for most scavengers (DeVault et al., 2016; Kirk & Mossman, 2020).
Even their hygiene is unusual.
Turkey vultures practice a behavior known as urohidrosis, in which they defecate on their own legs. While it may seem unpleasant from a human perspective, the highly acidic waste helps kill bacteria picked up while walking on carcasses and also provides a cooling effect during hot weather (Arad et al., 1989; Kirk & Mossman, 2020).
Taken together, these adaptations solve a difficult ecological problem. Dead animals can become reservoirs for bacteria, disease, and decay. Turkey vultures have evolved to exploit that resource while avoiding many of the risks associated with it.
Black vultures, which are often seen alongside them, approach the problem differently. Their nostrils are narrower and not open from side to side. Rather than relying so heavily on smell, they depend more on vision and often watch the movements of turkey vultures to help locate food (Buckley et al., 2020).
That relationship creates an interesting partnership. Turkey vultures are often the first to detect a carcass hidden beneath vegetation, while black vultures are quick to notice where the turkey vultures are gathering. One species excels at finding the scent. The other excels at finding the finder (Buckley et al., 2020; Kirk & Mossman, 2020.
Together, the two species accomplish something few other animals can.
They return nutrients to the landscape.
What appears to be an ending becomes the beginning of something else. Energy stored within a fish, a raccoon, or a deer does not simply disappear. Vultures help move those nutrients back into the ecosystem where they become available to countless other organisms (DeVault et al., 2016) .
The bird on your roof is not waiting for something bad to happen.
More often than not, it is part of the reason the landscape remains healthy after it does.
Black Vulture: Following the Leader
A single turkey vulture on a rooftop often attracts attention.
Ten vultures attract concern.
What appears to be a crowd is often an information network. Black vultures frequently roost together, sharing a landscape where opportunities can appear and disappear without warning. | Image credit: jspruill, iNaturalist
Unlike turkey vultures, which are frequently seen soaring alone or in small numbers, black vultures (Coragyps atratus) often seem to arrive as a group, called a committee. One bird becomes five. Five become ten. Before long, an entire rooftop, parking lot, or dead tree appears covered in vultures (Buckley et al., 2020).
The first question is usually the same.
Why are there so many?
Part of the answer lies in how black vultures find food.
While turkey vultures rely heavily on their extraordinary sense of smell, black vultures depend much more on vision and on one another. They watch the landscape, but they also watch other vultures. A turkey vulture dropping toward a hidden carcass can reveal an opportunity that a black vulture might never have discovered on its own (Buckley et al., 2020).
That difference creates an unusual relationship between the two species.
Turkey vultures are often the first to locate carrion concealed beneath vegetation or hidden from view. Black vultures are often the first to notice that the turkey vultures have found something worth investigating (Buckley et al., 2020).
One species excels at finding the scent.
The other excels at finding the finder.
Their social nature extends beyond feeding. Black vultures frequently roost together, travel together, and gather in numbers that can seem surprising to people unfamiliar with them. What appears to be a crowd is often a network of birds sharing information about a landscape filled with unpredictable opportunities (Buckley et al., 2020).
That strategy has served them well.
A dead fish washed onto a shoreline, a raccoon along a roadside, or a deer hidden beyond the edge of a forest represents a resource that appears without warning and disappears quickly. By paying attention to one another, black vultures can exploit those opportunities efficiently.
To most people, the meal is something to avoid. To a black vulture, it is an opportunity. By consuming carrion that would otherwise decay on the landscape, vultures help return nutrients to the ecosystem while reducing the spread of disease. | Image credit: A. Mitchell
Like the turkey vulture, the black vulture plays an important role in returning nutrients to the ecosystem.
It simply approaches the problem differently.
Where the turkey vulture trusts its nose, the black vulture trusts its neighbors.
The Night Shift
As daylight fades, a different group of predators takes over.
The thermals weaken. The soaring hawks settle. Shadows lengthen across marshes and forests.
Then the owls emerge.
Eastern Screech-Owl: Master of Camouflage
Many people have an eastern screech-owl (Megascops asio) living in their neighborhood and never realize it.
Not because the owl is rare.
Because it is exceptionally good at remaining unnoticed.
You might spend years walking past the same tree without ever seeing this small bird tucked inside a cavity or pressed against the bark. Then one evening, just after sunset, a soft trill or whinny drifts through the yard and suddenly you realize there has been an owl nearby the entire time (Gehlbach, 2009; Ritchison et al., 2020).
The discovery often raises an interesting question.
If eastern screech-owls feed on many of the same insects, rodents, reptiles, and amphibians as some daytime raptors, why don’t we see them more often? (Gehlbach, 2009; Ritchison et al., 2020)
Part of the answer is timing.
While hawks spend the day watching fields, marshes, forests, and backyards, the eastern screech-owl waits for darkness. As daylight fades and the daytime hunters settle into roosts, the owl begins its own shift (Ritchison et al., 2020).
But timing alone does not explain its success.
The owl’s real advantage is concealment.
Its mottled gray and brown feathers blend remarkably well with tree bark, allowing it to disappear into the landscape even when it is in plain sight. During the day, many spend hours motionless inside tree cavities or against trunks where they become nearly impossible to detect (Gehlbach, 2009; Ritchison et al., 2020).
That camouflage allows the owl to remain close to people while largely escaping notice.
Neighborhoods, wooded lots, parks, forest edges, and suburban backyards can all provide suitable habitat. The insects drawn to porch lights, the rodents moving along fence lines, and the small reptiles hiding among shrubs create hunting opportunities throughout the night (Gehlbach, 2009; Ritchison et al., 2020).
By the time most people realize an eastern screech-owl is nearby, it has often been there all along.
Its success does not come from being the largest predator in the landscape.
It comes from being the one you never knew was watching.
Barn Owl: Sound Becomes Sight
A pale shape crosses a field at dusk.
For a moment it hardly seems real. The bird appears almost white against the fading light, gliding silently above the grass before disappearing into the darkness beyond.
The first question is often simple.
What did I just see?
For centuries, encounters like that have inspired stories of ghosts, spirits, and things that move through the night unseen. The barn owl’s piercing scream has only reinforced that reputation. Unlike the familiar hoots people associate with owls, barn owls produce calls that can sound startlingly human, often described as shrieks, screams, or cries drifting through the darkness. Heard for the first time from a forest edge or old barn, it is easy to understand how the bird became woven into folklore (Marti et al., 2024).
Yet the call serves a practical purpose.
In darkness, sound becomes one of the most effective ways for Americanbarn owls (Tyto alba pratincola) to communicate with mates, defend territories, and maintain contact with one another. What sounds eerie to us is simply part of life for an owl that spends most of its time hunting when the rest of the landscape is asleep (Marti et al., 2024).
The hunt itself is equally remarkable.
Barn owls are among the most specialized rodent hunters in North America. Their heart-shaped facial disks act like satellite dishes, funneling sound toward asymmetrical ears capable of pinpointing prey with astonishing precision. A mouse rustling through grass can reveal its location long before the owl ever sees it (Payne, 1971; Marti et al., 2024).
That adaptation helps explain another common experience.
Step quietly into an old barn, abandoned building, or large outbuilding and you may discover one or more barn owls perched overhead. They often watch intruders with an intense stare, swaying and bobbing from side to side as they study the unfamiliar visitor below (Marti et al., 2024).
At first glance, the behavior appears nervous or even strange.
In reality, the owl is gathering information. The subtle movements help it judge distance, depth, and position before deciding whether to remain still or slip silently into the darkness.
Fields, agricultural landscapes, marsh edges, and open grasslands provide ideal hunting habitat (Marti et al., 2024). Every mouse captured represents energy transferred from one part of the ecosystem to another, helping regulate populations that might otherwise grow unchecked.
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The pale bird crossing the field is not a ghost.
It is one of the most effective hunters the night shift has to offer.
For the barn owl, sound does not simply reveal the landscape.
It becomes a way of seeing it.
Barred Owl: The Voice of the Swamp
“Who cooks for you? Who cooks for you-all?”
Once you hear it, you rarely forget it.
The call drifts through wooded neighborhoods, swamp edges, and forested wetlands after sunset, often carrying much farther than people expect. Many coastal residents know the sound long before they ever see the bird responsible for making it (Bierregaard et al., 2025).
The question naturally follows.
Who is calling from the darkness?
More often than not, it is a barred owl.
Unlike the barn owl crossing open fields or the eastern screech-owl disappearing into a backyard tree, barred owls (Strix varia) are closely tied to forests and wetlands. Swamps, creek corridors, bottomland hardwoods, and wooded neighborhoods provide the cover, water, and diversity of prey they need (Bierregaard et al., 2025).
The call itself serves several purposes. Barred owls use it to communicate with mates, establish territories, and maintain contact across dense forests where visibility is limited. What sounds like a conversation to us is often exactly that (Bierregaard et al., 2025).
Those forests and wetlands provide hunting opportunities throughout the year. Frogs call from wetland edges. Crayfish move through shallow water. Rodents travel beneath fallen leaves. Snakes, insects, and small birds all become potential prey. Rather than specializing in a single food source, barred owls have learned to take advantage of whatever the swamp provides (Bierregaard et al., 2025).
The swamp, however, does not make hunting easy.
Prey hides beneath vegetation, beneath water, and beneath layers of leaf litter. Fallen logs, tangled branches, and dense understory create countless places to disappear.
Barred owls overcome many of those challenges through silence.
The leading edges of their feathers are specially adapted to break up airflow, reducing the sound of flight to nearly nothing. A mouse rustling beneath leaves, a frog moving along a wetland edge, or a crayfish crossing shallow water may never hear the owl approaching (Bachmann & Wagner, 2016).
For prey, the danger often arrives without warning.
By the time a barred owl commits to an attack, silence has already done much of the work.
That ability helps explain why barred owls are among the most successful predators in the region.
It also reveals something many people do not realize.
Hunting is not simply a switch that turns on when a young owl leaves the nest.
Juvenile barred owls must learn. They practice. They miss opportunities. They refine the skills needed to locate, pursue, and capture prey in a complex environment. In wildlife rehabilitation settings, young barred owls that fail to develop those hunting skills cannot be successfully returned to the wild (Watson et al., 2023).
Instinct provides the foundation.
Experience builds the hunter.
Perhaps that is why barred owls have become such a familiar voice in the coastal night. Their success comes not from mastering a single prey species or hunting strategy, but from learning to adapt to whatever the swamp provides.
For the barred owl, the swamp is more than habitat.
It is a hunting ground, a classroom, and a home.
Great Horned Owl: Ruler of the Night
The night can be surprisingly noisy.
A barred owl calls from the swamp.
Tree frogs answer from the wetlands.
Crickets fill the spaces in between.
Then, sometimes, the woods erupt with alarm calls.
Crows mob during the day. Smaller birds call from hidden roosts after sunset. Even other predators seem suddenly aware that something has changed.
What happened?
Often, a great horned owl (Bubo virginianus) has arrived.
While many predators spend their lives worrying about what might hunt them, the great horned owl occupies a different position in the food web. Rabbits, squirrels, rodents, reptiles, birds, and even other predators can become prey. Where great horned owls occur, few animals completely ignore them (Artuso et al., 2020).
That includes other owls.
Barred owls, screech-owls, and other nocturnal hunters may alter their behavior when a great horned owl is nearby (Artuso et al., 2020). The question is not simply what the owl is hunting.
The question is whether anything wants to become its next opportunity.
Part of that success comes from versatility. Great horned owls hunt forests, wetlands, agricultural fields, suburban neighborhoods, and coastal habitats with equal confidence. Rather than specializing in a single prey species, they take advantage of whatever opportunities the landscape provides (Artuso et al., 2020).
Yet versatility alone does not explain why other animals react when one arrives.
Power does.
A great horned owl’s grip rivals that of a bald eagle. The force generated by its talons can exceed 270 newtons, allowing it to seize and control prey with remarkable efficiency (Ward et al., 2002). Those feet are capable of exerting tremendous force once they close around a target (Ward et al., 2002; Lingham-Soliar, 2014).
Combined with a wingspan approaching five feet, the result is a predator that commands attention even before it leaves the ground (Artuso et al., 2020).
Yet perhaps the most remarkable thing about a great horned owl is how quietly all of that power moves through the landscape.
Like other owls, the leading edges of their feathers break up airflow, reducing the sound of flight to nearly nothing. A bird carrying a wingspan wider than many people are tall can pass overhead with little more than a faint rush of air (Bachmann & Wagner, 2016).
Sometimes not even that.
The first indication that a great horned owl is nearby is often the reaction of everything else around it.
That silence becomes even more effective when paired with another adaptation.
Many people believe owls can rotate their heads completely around.
They cannot.
A great horned owl can rotate its head roughly 270 degrees, allowing it to scan much of the landscape without moving its body (Ward et al., 2002). Unlike our eyes, an owl’s eyes are largely fixed within the skull. To change its view, it must move its head (Ward et al., 2002; Lingham-Soliar, 2014).
For an ambush predator, that matters.
Every movement risks revealing its position. The ability to gather information while remaining nearly motionless allows the owl to watch far more than most animals realize.
And that may be the real reason so many creatures react when one arrives.
The great horned owl combines strength, silence, patience, and awareness in a way few predators can. By the time a rabbit, squirrel, snake, or even another owl realizes it is being watched, the great horned owl has often been watching for quite some time.
Perhaps that is why other animals seem to know when one is nearby.
The great horned owl is not simply another hunter in the night.
It is often the hunter watching the hunters.
Reading the Sky
At first glance, they all appear similar.
Large birds.
Broad wings.
Silhouettes against the sky.
Yet an osprey hovering above the water, a red-shouldered hawk watching from a fence post, a Mississippi kite chasing dragonflies, a vulture riding a thermal, and a barred owl moving through the darkness are not performing the same job.
They are reading the landscape in different ways.
The osprey watches the water.
The red-tailed hawk watches entire fields.
The Cooper’s hawk watches movement between trees.
The Mississippi kite watches the air itself.
Even the vultures, often dismissed as scavengers, are searching for clues that most of us never notice.
The next time a large bird catches your attention, resist the urge to identify it immediately.
Instead, watch what it does.
Does it hover?
Circle?
Perch?
Glide?
Disappear into the trees?
The answer often tells you as much as the feathers.
Because the sky is not filled with birds doing the same thing.
It is filled with specialists solving different problems.
And once you begin to notice those differences, the sky becomes a little easier to read.
At a distance, every raptor can seem like little more than a shape against the clouds. Spend enough time watching, however, and the sky becomes easier to read. | Image credit: A. Mitchell
References
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Artuso, C., Houston, C. S., Smith, D. G., & Rohner, C. (2020). Great Horned Owl (Bubo virginianus). In Birds of the World (1.0th ed.). Cornell Lab of Ornithology.
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Bierregaard, R. O., Poole, A. F., Martell, M. S., Pyle, P., & Patten, M. A. (2020). Osprey (Pandion haliaetus). In Birds of the World (1.0th ed.). Cornell Lab of Ornithology.
Buckley, N. J., Kluever, B. M., Driver, R., & Rush, S. A. (2020). Black Vulture (Coragyps atratus). In Birds of the World (2.0th ed.). Cornell Lab of Ornithology.
Buehler, D. A. (2022). Bald Eagle (Haliaeetus leucocephalus). In Birds of the World (2.0th ed.). Cornell Lab of Ornithology.
DeVault, T. L., Beasley, J. C., Olson, Z. H., Moleón, M., Carrete, M., Margalida, A., & Sánchez-Zapata, J. A. (2016). Ecosystem Services Provided by Avian Scavengers. In Why Birds Matter: Avian Ecological Function and Ecosystem Services (pp. 235-270). University of Chicago Press.
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Gehlbach, F. R. (2009). The eastern screech owl: Life history, ecology, and behavior in the suburbs and countryside. Texas A&M University Press.
Grigg, N. P., Krilow, J. M., Gutierrez-Ibanez, C., Wylie, D. R., Graves, G. R., & Iwaniuk, A. N. (2017). Anatomical evidence for scent guided foraging in the Turkey vulture. Scientific Reports, 7(1). https://doi.org/10.1038/s41598-017-17794-0
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Most changes in the ocean happen long before we notice them.
The water still looks blue. Waves continue to break across the sandbars. Beachgoers spread their towels beneath the same summer sun, children chase ghost crabs along the tide line, and anglers cast into the surf hoping for a bite.
Yet beneath the surface, a warming ocean is altering the conditions that shape life along the coast.
The changes begin with microscopic organisms drifting through the water column and ripple outward through fish, shellfish, jellyfish, and eventually the people who swim, fish, and play in these waters. Scientists have documented rising ocean temperatures worldwide, with the ocean absorbing the vast majority of the excess heat generated by a warming climate (IPCC, 2023; NASA, 2025).
For beachgoers along the Onslow County coast, these changes often appear as small observations. Water that feels warmer than it once did. Green swirls visible in drone photographs. Jellyfish gathering along the shoreline. Questions about bacteria, shellfish closures, and changing fish patterns.
At first glance, these may seem unrelated.
In reality, they are all connected.
A Longer Summer Beneath the Surface
The ocean does not warm as quickly as the air above it, but it holds heat much longer.
As coastal waters warm earlier in spring and remain warm later into autumn, marine organisms experience something similar to a longer growing season on land. Processes that once occurred over a few summer months may now persist for much longer periods – lasting later into the year or shifting the timing of organisms that are responding to environmental conditions (IPCC, 2023; Menzel et al., 2006).
For marine life, temperature influences nearly everything. Growth rates, feeding behavior, reproduction, migration, and metabolism are all affected by the warmth of the surrounding water (Pörtner & Knust, 2007).
For many species, warmer water means increased biological activity. But every response carries consequences that ripple through the food web.
The first organisms to respond are often the smallest.
When Tiny Things Respond First
Most beachgoers never think about what is suspended in the water around them.
Unlike a forest, marsh, or coral reef, much of the ocean’s life is not immediately visible. Looking across the surf, the water may appear empty except for an occasional fish, jellyfish, or diving bird.
Yet the water column itself is home to countless drifting organisms. Some are microscopic plants. Others are microscopic animals. Together, they form a community known as plankton.
Among the most important are phytoplankton—tiny plant-like organisms that drift with currents and tides. Though nearly invisible to the naked eye, they capture sunlight, form the foundation of marine food webs, and produce much of the oxygen found in Earth’s atmosphere (Falkowski et al., 1998).
Feeding on them are zooplankton, a diverse group of drifting animals that includes tiny crustaceans, larval fish, and the early life stages of many marine organisms. Nearly everything in the ocean depends on this microscopic world in some way.
As temperatures rise and sunlight remains abundant, phytoplankton growth can increase. In many cases, this increased productivity benefits marine ecosystems by providing more food for zooplankton, shellfish, and small fish.
Sometimes, however, the changes become visible.
Drone photographs, fishing reports, and satellite imagery occasionally reveal ribbons and swirls of green water along the coastline. Many people assume these colors indicate pollution, but the explanation is often more complex.
In some cases, the green color reflects increased concentrations of phytoplankton. In others, it may result from suspended sediment, river discharge, or other naturally occurring materials in the water (Behrenfeld et al., 2006).
Green water does not automatically mean unhealthy water.
More often, it is a visible reminder that biological activity is taking place beneath the surface—activity that most beachgoers never see.
In fact, many periods of greener water reflect productive conditions that support marine food webs. Increased phytoplankton can provide more food for zooplankton, shellfish, and small fish, creating benefits that ripple through the ecosystem. The presence of abundant microscopic life is often a sign that the ocean is actively supporting the organisms that depend upon it.
Not all blooms are beneficial, however.
Occasionally, beachgoers hear news reports about harmful algal blooms and wonder whether the water they are seeing is part of one.
Under certain conditions, a small number of phytoplankton species can reproduce so rapidly that they begin affecting the ecosystem around them. These events are known as harmful algal blooms.
Along U.S. coastlines, some of the better-known examples include Karenia brevis, which causes many Gulf Coast red tides; Alexandrium species, which can produce toxins associated with paralytic shellfish poisoning; and Pseudo-nitzschia, which produces domoic acid and has been linked to shellfish closures and wildlife impacts in several regions (Anderson et al., 2012; Trainer et al., 2012).
Unlike the seasonal increases in phytoplankton that help support marine food webs, harmful blooms can stress marine life and create concerns for people. Some produce toxins that accumulate in shellfish, leading to temporary harvesting closures. Others contribute to oxygen declines as large concentrations of algae die and decompose (Anderson et al., 2002).
For beachgoers, the challenge is that harmful blooms do not always look the way people expect. A bloom may appear as a patch of unusually dense water, a streak of discoloration, or sometimes little different from surrounding water. Color alone rarely tells the whole story.
In some cases, blooms may discolor the water, turning it red, rust-colored, brown, orange, or an unusually dense green. Some may also produce odors that people describe as sulfur-like, fishy, or similar to decaying vegetation (Gilbert et al., 2005; Gobler, 2020).
Not all green water is the same. Satellite imagery can reveal differences in phytoplankton concentrations across coastal waters. Many blooms support productive marine ecosystems, while others may become dense enough to affect water quality and ecosystem health. | Image credit: EPA cyanWeb, https://qed.epa.gov/cyanweb/
Fortunately, most periods of pale green, emerald green, or slightly tea-colored water along the Carolina coast are not harmful algal blooms. More often, they reflect normal concentrations of phytoplankton, suspended sediment, river discharge, or other natural processes.
The challenge is that the water does not always reveal which is which at first glance. What appears to be a simple color change may be telling a much more complicated story beneath the surface.
The Oxygen Paradox
Warm water creates a biological contradiction.
As temperatures rise, marine organisms require more oxygen to stay active and carry out basic life processes. At the same time, warmer water naturally holds less dissolved oxygen—the tiny oxygen molecules mixed into the water that fish, crabs, and many other marine animals breathe. Unlike oxygen in the air around us, this oxygen must remain suspended within the water itself, and warmer water cannot hold as much of it as cooler water (Keeling et al., 2010).
In other words, as the demand for oxygen increases, the supply decreases. Scientists refer to this growing challenge as ocean deoxygenation, a phenomenon driven in part by warming oceans and documented in coastal waters around the world (Breitburg et al., 2018; Diaz & Rosenberg, 2008).
The effects are often invisible to beachgoers. Unlike a jellyfish bloom or a patch of green water, low oxygen leaves few obvious clues for someone standing on the shoreline.
Fish may become sluggish, gather near inlets or channels, or disappear from places where they are normally common long before any obvious signs appear at the surface. Crabs, shrimp, and other marine organisms must work harder to find places with enough oxygen to survive. Some may move into shallower water, concentrate in tidal channels, or bury themselves in sediment where conditions remain tolerable. Some areas become less favorable, while others provide temporary pockets of suitable habitat.
The ocean begins to rearrange itself.
Following the Fish
Stand on the beach long enough and patterns begin to emerge.
A stretch of water that looked empty an hour ago suddenly flickers with baitfish. Birds gather over a patch of surf. A school of fish appears just beyond a sandbar, then vanishes as quickly as it arrived.
Most of these movements happen without drawing much attention. To someone walking the shoreline, the ocean can seem unchanged from one day to the next.
Beneath the surface, however, marine life is constantly adjusting.
Fish are not fixed to one place. They move through the water searching for conditions that suit them, often responding to changes that people cannot see. A slight difference in temperature, a pocket of water with more oxygen, or a concentration of prey can be enough to shift where fish gather (Pörtner & Knust, 2007).
Along the beaches of Onslow County, these adjustments may be playing out right in front of us.
Anglers sometimes notice schools of mullet, menhaden, silversides, or other baitfish stacked along a sandbar. Predatory fish such as bluefish, Spanish mackerel, red drum, or even small sharks may linger near an inlet. Feeding activity may suddenly erupt close to shore, with baitfish leaping from the water as predators chase them, birds diving repeatedly into the surf, and flashes of silver visible just beyond the breakers. Tides, currents, and seasonal migrations all help shape these patterns, but fish are also responding to the changing conditions around them.
Even the breaking surf can matter.
Where waves tumble across shallow bars, the water is constantly being mixed and stirred. Oxygen from the atmosphere is worked back into the water, creating conditions with higher oxygen levels than nearby areas where the water is calmer and moves less. What looks like nothing more than a line of breaking waves can become a place where marine life gathers.
Most beachgoers never notice these subtle shifts.
They simply see fish where fish happen to be.
Yet changing ocean conditions are becoming an increasingly important part of the story. Fish may feed in a different stretch of surf than usual, baitfish may gather in unexpected places, or seasonal arrivals may occur a little earlier or later than expected. Most of the time, the reasons remain hidden beneath the surface, but the movements themselves reveal that marine life is responding to a changing ocean (Pinsky et al., 2013).
The ocean is not standing still.
And neither are the fish.
The Species That Thrive
Not every organism responds to warming water in the same way.
Some struggle.
Others thrive.
For many beachgoers, one of the most noticeable signs of seasonal change arrives as translucent shapes drifting through the surf. As plankton populations increase and warm conditions persist, the same environmental changes influencing fish and other marine life can also create favorable conditions for jellyfish.
Jellyfish are a familiar part of coastal life in Onslow County, but their numbers can vary dramatically from season to season. During late spring, summer, and early fall, when air and water temperatures commonly reach about 68–86°F (20–30°C), conditions often become more favorable for larger jellyfish populations than during the colder months.
Most people first notice them while wading in the shallows, scanning the water from a pier, or walking the beach after a storm. A shoreline that seemed empty a few weeks earlier may suddenly hold dozens of stranded jellyfish along the tide line. Depending on the season, visitors might encounter moon jellies pulsing just beneath the surface, cannonball jellies washing ashore in clusters, or the unmistakable blue floats of Portuguese man o’ war carried in by winds and currents.
A shoreline covered with cannonball jellies can appear almost overnight. In reality, the conditions supporting these blooms often develop over weeks or months as water temperatures, food availability, and ocean currents change. | Image credit: Cape Hatteras National Seashore
These appearances can feel sudden, but they rarely are.
A shoreline that seems free of jellyfish one week may be dotted with them the next. To someone standing on the beach, it can feel as though they arrived overnight.
Much of a jellyfish’s life unfolds out of sight. Many drift offshore, while others pass through life stages that most people never notice. As waters warm and food becomes more abundant, conditions can support larger populations. Sometimes the result is a bloom—a period when unusually large numbers gather in coastal waters and become difficult to ignore.
In reality, the conditions that support them may have been developing for weeks or even months. While warmer water does not automatically mean more jellyfish everywhere (Condon et al., 2012), seasonal warming can contribute to periods when jellyfish become unusually abundant in nearshore waters. Currents, food availability, and other environmental factors also influence when and where these blooms occur (Purcell, 2005; Richardson et al., 2009).
For observers on the shore, jellyfish are often among the first visible reminders that changes in ocean conditions do not stay hidden beneath the surface for long.
Not every organism has the ability to drift or swim away.
The Organisms That Cannot Leave
Fish can relocate.
Jellyfish can drift with currents.
Shellfish remain where they are.
For many beachgoers, oysters, clams, and mussels are simply part of the coastal landscape—something encountered at low tide, served at a seafood restaurant, or harvested during shellfish season.
Yet these animals spend their lives doing something remarkable.
Oysters, clams, mussels, and other shellfish continuously draw water through their bodies, removing microscopic food particles as they feed. This is why they are known as filter feeders. A single adult oyster can filter up to 50 gallons (190 L) of water per day, depending on temperature, salinity, and other environmental factors (Jansen, 2023; zu Ermgassen et al., 2012).
An oyster reef does not simply sit on the bottom. Day and night, every oyster is quietly filtering the estuary around it.
Because they process so much water, shellfish become closely connected to the conditions around them. Changes in temperature, oxygen levels, harmful algal blooms, and water quality can all affect their health and survival (Shumway, 1990).
For this reason, shellfish often serve as some of the earliest indicators that environmental conditions have changed.
When shellfish harvesting areas are temporarily closed, many people assume pollution is the only explanation. In reality, closures may occur for a variety of reasons, including elevated levels of bacteria such as fecal coliforms, Escherichia coli (E. coli), or Enterococcus, harmful algal blooms, or other conditions that could affect human health (Food & Drug Administration (FDA), 2023).
In many cases, these closures are evidence that monitoring programs are working exactly as intended.
The shellfish are not causing the problem.
They are revealing it.
By filtering the surrounding water day after day, they provide a glimpse into conditions that might otherwise go unnoticed.
Sometimes, what they reveal is a bacterium that has received increasing attention in recent years.
The Bacteria That Was Already Here
Few marine organisms have generated more public concern in recent summers than Vibrio bacteria.
News headlines often make it sound like a new arrival.
It is not.
Like the phytoplankton, zooplankton, and countless other organisms drifting through coastal waters, Vibrio vulnificushas always been part of the hidden community beneath the surface.
Most beachgoers never notice it. They cannot see it. They do not think about it while wading through the surf or collecting shells along the shoreline.
Yet these bacteria have long occupied an important ecological role.
Vibrio species occur naturally in coastal and estuarine waters around the world. They help break down organic matter and recycle nutrients, returning materials to the food web where they can be used again by other organisms. If they were somehow eradicated, scientists would expect dead plants, algae, fish, and other organic material to break down more slowly. Over time, beach wrack could linger longer along shorelines, decaying material could accumulate in marshes and tidal flats, and nutrients normally returned to the water and sediment would become less available to the organisms that depend on them. These changes might not be obvious at first, but they could gradually alter the health and productivity of coastal ecosystems (Oliver, 2005).
The organic material accumulating along a wrack line supports a hidden community of decomposers. Among them are naturally occurring bacteria that help recycle nutrients and keep coastal ecosystems functioning. Image credit: S. Hilldebrand, U. S. Fish and Wildlife Service
What often changes first is not the presence of these organisms, but their abundance.
Just as warmer conditions can influence phytoplankton growth, they can also affect microbial communities.
Most of the time, these changes remain invisible.
The water may look the same. The beach may feel the same. Nothing about a morning walk along the shoreline suggests that microscopic populations are shifting beneath the surface.
Yet they are.
When water temperatures rise well above the normal seasonal range for a region and remain elevated for extended periods, conditions can become more favorable for certain Vibrio species. Their populations may increase, raising the likelihood of human exposure (Baker-Austin et al., 2012; Baker-Austin et al., 2018).
For most healthy beachgoers, swimming in coastal waters remains a normal part of enjoying the beach.
However, individuals with open wounds, compromised immune systems, or underlying health conditions may face greater risks and should pay closer attention to local advisories and public health guidance.
The story is not really about a dangerous bacterium suddenly appearing where it did not belong.
It is another example of a broader pattern that runs throughout coastal ecosystems.
As environmental conditions change, the organisms already living there respond. Some become more abundant. Others become less common. Together, their responses reveal something easy to miss while standing at the water’s edge: the shoreline is alive with countless forms of life that most of us never see.
Even the smallest inhabitants are connected to the larger changes unfolding around them.
Reading the Signs
Most beachgoers will never measure dissolved oxygen or monitor water temperatures.
What they will notice are the signs: water that stays warm later into autumn, green swirls visible from a fishing pier or drone photograph, jellyfish gathering along a tide line, fish appearing in unexpected places, temporary shellfish closures, or questions about bacteria that have long existed in coastal waters.
None of these observations tells the whole story on its own.
Taken together, however, they reveal an ecosystem responding to warmer conditions one species, one season, and one degree at a time.
Looking Beneath the Surface
Most changes in the ocean begin out of sight.
Long before beachgoers notice a jellyfish drifting through the surf or a patch of green water offshore, microscopic organisms are already responding to changing conditions. Fish adjust their movements. Oxygen levels shift. Shellfish filter whatever the water brings.
By the time we notice the signs, the ecosystem has often been responding for weeks or months.
The water may feel the same as it always has beneath our feet. Yet each summer offers new clues about the changes taking place below the surface—if we know where to look.
The ocean often appears unchanged from one day to the next. Beneath the surface, however, countless organisms are responding to shifting temperatures, oxygen levels, food availability, and water quality. The more we learn to observe, the more the shoreline reveals. | Image credit: A. Mitchell
References
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Anderson, D. M., Glibert, P. M., & Burkholder, J. M. (2002). Harmful algal blooms and eutrophication: Nutrient sources, composition, and consequences. Estuaries, 25(4), 704-726. https://doi.org/10.1007/bf02804901
Baker-Austin, C., Oliver, J. D., Alam, M., Ali, A., Waldor, M. K., Qadri, F., & Martinez-Urtaza, J. (2018). Vibrio spp. infections. Nature Reviews Disease Primers, 4(1), 1-9. https://www.nature.com/articles/s41572-018-0005-8
Baker-Austin, C., Trinanes, J. A., Taylor, N. G., Hartnell, R., Siitonen, A., & Martinez-Urtaza, J. (2012). Emerging vibrio risk at high latitudes in response to ocean warming. Nature Climate Change, 3(1), 73-77. https://doi.org/10.1038/nclimate1628
Behrenfeld, M. J., O’Malley, R. T., Siegel, D. A., McClain, C. R., Sarmiento, J. L., Feldman, G. C., Milligan, A. J., Falkowski, P. G., Letelier, R. M., & Boss, E. S. (2006). Climate-driven trends in contemporary ocean productivity. Nature, 444(7120), 752-755. https://doi.org/10.1038/nature05317
Breitberg, D., Levin, L. A., Oschlies, A., Grégoire, M., Chavez, F. P., Conley, D. J., Garçon, V., Gilbert, D., Gutiérrez, D., & Zhang, J. (2018). Declining oxygen in the global ocean and coastal waters. Science, 359(6371). https://doi.org/10.1126/science.aam7240
Condon, R. H., Graham, W. M., Duarte, C. M., Pitt, K. A., Lucas, C. H., Haddock, S. H., Sutherland, K. R., Robinson, K. L., Dawson, M. N., Decker, M. B., Mills, C. E., Purcell, J. E., Malej, A., Mianzan, H., Uye, S., Gelcich, S., & Madin, L. P. (2012). Questioning the rise of gelatinous zooplankton in the world’s oceans. BioScience, 62(2), 160-169. https://doi.org/10.1525/bio.2012.62.2.9
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Most beachgoers look across the shoreline and see a boundary.
The ocean ends. The land begins.
But the strip of sand where waves wash ashore and slide back toward the sea is not really either one. It is a threshold—a place that becomes ocean and land again with every passing wave.
At first glance, this narrow band of wet sand appears empty. There are no marsh grasses, no oyster reefs, and no obvious schools of fish. Yet beneath the surface, the sand is alive with animals digging, filtering, feeding, hunting, and breathing.
This is the swash zone: the constantly shifting seam between ocean and land.
It is one of the most overlooked ecosystems on the North Carolina coast.
The swash zone is the narrow strip of shoreline where waves wash ashore and then retreat back toward the sea. Though it may appear to be little more than wet sand, it supports a diverse community of animals adapted to life between ocean and land. | Image credit: J. Morales
The Beach That Never Stops Moving
Unlike a marsh, oyster reef, or seagrass meadow, the swash zone never stays still.
Each wave pushes seawater into the sand and then pulls it back out again. Water moves through the spaces between sand grains, carrying oxygen, microscopic algae, bacteria, and organic matter. The sand itself acts almost like a living filter, supporting communities of organisms adapted to conditions that change minute by minute (Brown & McLachlan, 2018; McLachlan & Defeo, 2018).
To survive here, animals must tolerate burial, shifting sediments, crashing waves, changing salinity, and predators arriving from both land and sea.
Few species can endure such instability.
Those that do are specialists (Defeo et al., 2009).
The Living Wave Riders: Mole Crabs and Coquina Clams
If you’ve ever noticed the wet sand suddenly shimmer or seem to move as a wave retreats, you’ve likely witnessed two of the swash zone’s most abundant residents.
Atlantic Mole Crabs (Emerita talpoida)
An Atlantic mole crab, in Surf City, NC, briefly exposed at the surface of the swash zone. Within seconds, these specialized crustaceans can bury themselves beneath the sand, where they spend most of their lives filtering food from the surf. | Image credit: johnnybirder, iNaturalist
Known locally as sand fleas, Atlantic mole crabs spend nearly their entire lives buried beneath the surface of the swash zone.
They are not true crabs. Instead, they belong to a group of highly specialized crustaceans adapted for life where waves break on the shore. Their bodies are smooth, streamlined, and shaped almost like a small bean. Using powerful rear legs, they can bury themselves in saturated sand in seconds (Abude et al., 2024).
When waves wash overhead, they extend feathery antennae into the water and filter microscopic plankton and organic particles from the surf (Abude et al., 2024).
Rather than remaining stationary, mole crabs occupy the constantly shifting swash zone, where food and oxygen are delivered by breaking waves. Their abundance makes them one of the most important food sources for shorebirds, fish, and ghost crabs (Abude et al., 2024).
Coquina Clams (Donax variabilis)
Sharing the same habitat is one of the most recognizable shells on Atlantic beaches.
Coquina clams are the tiny, brightly colored shells scattered across the tide line in shades of pink, yellow, purple, blue, orange, and white.
Most people only notice the shells.
The living animal beneath them is remarkably adapted to life in moving sand.
Coquinas live just beneath the surface of the swash zone where they filter microscopic algae and suspended particles from the water. As waves advance and retreat, they repeatedly rebury themselves, using a muscular foot to dig into the sand with astonishing speed (Ellers, 1995).
Like mole crabs, coquinas are adapted to the dynamic conditions of the swash zone. Their abundance provides food for fish, crabs, and shorebirds, making them a critical link between microscopic plankton and larger coastal predators (Wilson, 1999).
Standing at the water’s edge, it is easy to think the beach is motionless.
In reality, thousands of coquinas and mole crabs may be moving beneath your feet with every wave.
The Night Shift: Atlantic Ghost Crabs (Ocypode quadrata)
Higher on the beach, above the reach of most waves, another resident waits.
Atlantic ghost crabs spend daylight hours hidden inside deep burrows excavated into the sand. Their pale coloration blends almost perfectly with the beach, making them difficult to see unless they move.
Atlantic ghost crabs spend daylight hours hidden in burrows above the tide line. Their pale coloration provides excellent camouflage against the sand, making them surprisingly difficult to spot until they move. | Image credit: A. Mitchell
While the swash zone below is dominated by animals filtering food from the surf, ghost crabs are hunters and scavengers.
After sunset, they emerge to patrol the shoreline, feeding on mole crabs, coquina clams, stranded marine organisms, insects, carrion, and whatever other opportunities the beach provides (Wolcott, 1978).
Many beachgoers never see them at all. Instead, they notice the evidence they leave behind. Round burrow openings dot the upper beach. Fresh tracks crisscross the sand overnight and disappear with the next tide. Occasionally, a pale shape darts sideways through the beam of a flashlight before vanishing into darkness.
Those burrows tell a story of their own. Beaches with abundant ghost crab burrows often support richer communities of animals living both above and below the sand, which is why scientists sometimes use ghost crabs as one way of assessing beach condition and disturbance (Schlacher et al., 2016).
The next time you notice a round hole in the upper beach with a pile of freshly excavated sand nearby, you are likely looking at the entrance to a ghost crab burrow—and evidence that the beach is still very much alive after dark.
Between the Grains
The largest residents of the swash zone are only part of the story.
Beneath the surface lies an even larger community that most beachgoers never see. Between individual grains of sand are tiny water-filled spaces that form a hidden habitat known as the interstitial zone. To us, a handful of wet sand looks solid. To these organisms, it is an underwater landscape of tunnels, chambers, and passageways (Higgins & Thiel, 1988).
The beach is layered with hidden communities. From amphipods and ghost crabs higher on the shore to coquina clams and mole crabs at the water’s edge, different species occupy distinct zones shaped by waves, moisture, food availability, and shifting sand. | Image credit: Michel et al., 2016
Amphipods: The Cleanup Crew
The line of seaweed, shells, and debris left behind by the tide may look messy, but it is often one of the busiest places on the beach.
Hidden among the wrack, in the upper intertidal zone, are amphipods, small crustaceans often called Atlantic beach hoppers (Americorchestia longicornis). If you sift through a pile of damp seaweed or drift algae, you may catch a glimpse of them springing away before disappearing back into cover.
Much of what washes ashore eventually becomes food for something else. Amphipods feed on decaying seaweed, dead animals, and other organic material stranded by the tide. In doing so, they help break down material that would otherwise accumulate along the shoreline. They also become food themselves, supporting shorebirds, fish, and other invertebrates that forage along the beach (Dugan et al., 2003).
Polychaete Worms: Engineers Beneath the Sand
Most beachgoers never see the worms living beneath the tide line, but their work is happening constantly beneath the surface.
As polychaete worms burrow through the sand, they create tiny pathways that allow water and oxygen to penetrate deeper into the sediment. In many ways, they perform the same role that earthworms do in a garden, except their garden is the beach itself.
Some species spend their lives feeding on organic material trapped between the sand grains, such as Lugworms (Arenicolidae). Others hunt small crustaceans and worms moving through the sediment such as Bloodworms (Glyceridae) and Paddle Worms / Shimmy Worms (Nephtyidae). As they burrow, feed, and move through the beach, they continually mix the sand and help create conditions that allow countless other organisms to survive there (McLachlan & Defeo, 2018).
Ribbon Worms: Hidden Predators
Not every animal beneath the sand is feeding on algae, bacteria, or decaying material.
Ribbon worms (Nemertea) are predators, though few people ever realize they are there. Hidden beneath the surface, they hunt some of the same tiny animals that share the spaces between the sand grains, including small worms, crustaceans, and other invertebrates moving through the sediment (Thiel & Kruse, 2001).
Many possess a remarkable feeding structure called a proboscis that can be rapidly extended to capture prey (Thiel & Kruse, 2001).
Most beachgoers will never see a ribbon worm, yet they are part of the same hidden food web as the amphipods, copepods, and nematodes surrounding them. Even beneath a seemingly empty stretch of sand, animals are feeding, avoiding predators, and competing for resources every hour of the day.
Nematodes: Life at Microscopic Scale
If you could shrink yourself down and explore a handful of wet sand, the landscape would look very different.
What appears solid to us is actually filled with tiny spaces between the grains. Moving through those water-filled passages are microscopic animals called nematodes (phylum Nematoda).
These tiny roundworms feed on bacteria, algae, fungi, and organic matter coating the sand. Though nearly invisible, they are among the most abundant animals on many beaches and play an important role in breaking down organic material and recycling nutrients throughout the sediment (Coull, 1999; Schratzberger & Ingels, 2018).
Harpacticoid Copepods: Tiny Links in the Food Web
Sharing those same microscopic spaces are harpacticoid copepods (Paraleptastacus wilsoni), tiny crustaceans that spend their lives moving between individual sand grains.
They graze on algae and microbial films coating the sediment, feeding on resources too small for larger animals to use directly. In turn, they become prey for larger invertebrates and juvenile fishes.
Most beachgoers will never see a harpacticoid copepod. Yet every handful of wet sand may contain a community of animals like these, quietly connecting the microscopic world to the larger food web of the beach (Schratzberger & Ingels, 2018).
Individually, these animals are easy to overlook.
Collectively, they form much of the living foundation of the tide line. The coquinas, mole crabs, ghost crabs, fishes, and shorebirds visible along the shoreline all depend, directly or indirectly, on countless small interactions taking place beneath the sand.
Following the Birds
One of the easiest ways to observe this hidden ecosystem is not by looking down.
It is by looking up.Anyone who spends time on the beach has likely watched sanderlings (Calidris alba) racing along the edge of the surf. They dart forward as a wave retreats, stop suddenly to probe the sand, and then sprint away from the next incoming wave. A little farther up the beach, ruddy turnstones (Arenaria interpres) pick through wrack lines left behind by the tide. Along the surf edge, Eastern willets (Tringa semipalmata semipalmata) walk deliberately through the shallows, searching for movement beneath the water.
To many beachgoers, they are simply birds feeding along the shoreline.
What they are actually doing is reading the beach.
Each probe into the sand is a search for prey hidden beneath the surface. Mole crabs, small worms, amphipods, coquinas, and other invertebrates living within the tide line provide food for these birds (Dugan et al., 2003; Hubbard & Dugan, 2003).
The birds go where the food is.
When shorebirds gather along a stretch of beach, they are often revealing an ecosystem that would otherwise remain invisible. Their presence tells us that the sand beneath them is alive with prey, even if we cannot see it ourselves.
In many ways, shorebirds act as interpreters of the tide line. By watching where they feed, pause, and congregate, we gain a glimpse into the hidden community supporting them below.
Reading the Beach
From a distance, the tide line can seem almost empty. A narrow strip of wet sand separates the ocean from the rest of the beach. Waves arrive, waves leave, and little appears to change.
Spend a few minutes watching, however, and a different picture begins to emerge.
Shorebirds gather where the surf is most active. Tiny shells appear and disappear with the retreating waves. Fresh ghost crab burrows punctuate the upper beach. Even the wrack line left behind by the tide becomes a gathering place for scavengers and foraging birds.
What first appears to be a simple boundary between land and sea begins to look more like a busy shoreline neighborhood.
At first glance, the tide line can appear almost empty. Look a little longer, however, and the clues begin to emerge—feeding shorebirds, scattered shells, and the constant movement of the surf all hint at the hidden community living beneath the sand. | Image credit: A. Mitchell
The animals living here are responding to the same thing: the constant movement of the tide. Food arrives with the surf, becomes available for a brief moment, and is quickly claimed by whatever creature is best adapted to find it. Some filter it from the water. Some collect it from the sand. Others hunt the animals already feeding there.
Because these organisms live so closely tied to the conditions of the beach, changes in their numbers can provide clues about the habitat itself (Defeo et al., 2009). A shoreline where birds are feeding, ghost crab burrows remain active, and life continues to reveal itself at the edge of the surf is often a sign that this narrow strip of beach is supporting the community that depends upon it.
When those communities decline, the change may not be immediately obvious. Yet over time the beach can begin to feel quieter. Fewer birds stop to feed. Fewer burrows appear in the sand. The signs become harder to find. Those changes can ripple outward through the food web, affecting species both on the beach and beyond it (Peterson et al., 2006).
The Threshold
The next time you stand at the edge of the surf, watch where the waves pause before sliding back toward the sea.
It is easy to see this narrow strip of shoreline as a boundary. Ocean on one side. Land on the other.
But the tide line is not really a dividing line at all.
It is a place where both worlds meet.
With every passing wave, food, oxygen, and life arrive from the ocean. Beneath the sand, animals capture it, consume it, recycle it, and pass it on. Shorebirds search for it. Ghost crabs emerge after dark to hunt it. Countless organisms spend their entire lives within a space that is neither fully ocean nor fully land.
Most people walk across this strip of beach without ever noticing it.
Yet it is one of the busiest places along the coast.
The next time you see shells appearing and disappearing in the surf, a flock of sanderlings racing the tide, or ghost crab burrows scattered across the upper beach, remember that these are not separate observations. They are pieces of the same story.
What appears to be an empty stretch of wet sand is actually a living threshold—a place where ocean and land remain connected through countless interactions happening beneath every step.
And once you see it, it becomes difficult to look at the shoreline the same way again.
The tide line in Surf City, NC may appear to be little more than wet sand. Yet beneath every retreating wave lies a hidden community connecting ocean and land through countless interactions, most of them unseen. | Image credit: A. Mitchell
References
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Hubbard, D. M., & Dugan, J. E. (2003). Shorebird use of an exposed sandy beach in Southern California. Estuarine, Coastal and Shelf Science, 58, 41-54. https://doi.org/10.1016/s0272-7714(03)00048-9
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Most people standing on the beach watch the Atlantic as though the ocean ends where detail disappears.
Nearshore water is easy to read. Pelicans diving offshore reveal where baitfish have gathered near the surface. The first sea turtle crawls of the season begin appearing along the upper beach. Sandbars reveal themselves through shifting wave patterns and changes in water color. Even when the water is murky, the coastline still feels structured because the movement happening near shore leaves visible clues.
Farther offshore, those visible clues become harder to read.
Beyond the breakers, past the shrimp boats and distant military vessels that sometimes mark the horizon, the Atlantic off Onslow County drops across the continental shelf into deeper pelagic water. From shore, that open water can appear empty simply because most of its structure is hidden beneath distance, depth, and moving currents. But the offshore ocean is highly organized. Temperature layers separate water masses. Squid and fish rise toward the surface at night and descend again before daylight. Currents gather plankton and compress bait schools into dense patches of life that may stretch for miles before dissolving again.
And moving through those shifting layers are sharks most beachgoers never see.
Species like the bigeye thresher shark, scalloped hammerhead, Carolina hammerhead, smooth hammerhead, great hammerhead, and tiger shark all occupy different parts of the same Atlantic system connected to North Carolina’s coast. They are not interchangeable predators simply sharing the same water. Each species is specialized for a different way of hunting, sensing, and moving through the pelagic environment.
Even though most people never see these sharks directly, their influence does not remain offshore.
They work their way back toward the coast through changes in prey behavior, bait distribution, migration timing, and the balance of the food web itself.
The Shark Built for Dim Water
The bigeye thresher shark (Alopias superciliosus) does not resemble most sharks people imagine from coastal documentaries or fishing piers. Its eyes are unusually large, and nearly half of its body length is tail.
A bigeye thresher shark (Alopias superciliosus) moves through dim offshore Atlantic water beyond the Carolina coast. Its enlarged eyes help it hunt in low light, while its elongated tail can be used to stun schooling prey before feeding. | Image credit: NC Sea Grant
Both features are tied directly to life in deeper offshore water.
Bigeye threshers spend much of their time moving vertically through the water column, often descending into dim water during daylight hours and returning closer to the surface at night as squid and mesopelagic fish migrate upward under darkness (Weng & Block, 2004). Offshore pelagic systems are layered environments. Light fades rapidly with depth, and many prey species spend daylight hours far below the surface where visibility is limited.
The shark’s large eyes help gather more available light in those darker layers.
For someone standing on the beach at sunset, the horizon still appears bright. Offshore, hundreds of feet below the surface, the bigeye thresher is already hunting in water where daylight barely penetrates.
Its tail is equally specialized. Schooling fish survive by moving together in synchronized motion, creating confusion for predators trying to isolate individual prey. The elongated upper lobe of the thresher’s tail evolved as a way to disrupt that coordination. Researchers have documented threshers using powerful overhead tail strikes to stun schooling fish before circling back to feed (Oliver et al., 2013).
That hunting strategy matters ecologically because the species targeted by threshers are often highly connected to broader Atlantic food webs. Squid, mackerel, and schooling pelagic fish move energy between offshore and coastal systems. Large predators help regulate those populations and alter how tightly schools gather, where they move, and how heavily they feed on smaller forage species beneath them in the food web (Heithaus et al., 2008).
Without predators thinning and disrupting those mid-level prey schools, feeding pressure shifts downward. Larger populations of squid and predatory fish consume more small forage species, including baitfish that later support seabirds, larger fish, and predators closer to shore. The result is not an empty ocean, but a gradual reorganization of how energy moves through the coastal ecosystem.
What beachgoers may eventually notice are changes in feeding activity: fewer concentrated bird flocks offshore, shifting bait movements, or less predictable surface eruptions beyond the breakers.
The Sharks That Hunt Electricity
Hammerheads occupy a different sensory world than most coastal predators.
The broad hammer-shaped head shared by species like the scalloped hammerhead, great hammerhead, smooth hammerhead, and Carolina hammerhead is called a cephalofoil. Spread across that wide structure are sensory pores known as ampullae of Lorenzini, specialized organs capable of detecting weak electrical fields produced by other animals (Kajiura, 2001).
Every muscle contraction and heartbeat generated by prey produces tiny electrical signals in the water.
A stingray buried beneath sand may be invisible to a human observer, but to a hammerhead it is still broadcasting electrical information.
The widened head helps the shark compare those signals across a broader sensory field, improving directional accuracy while hunting. Scientists have compared shark electroreception to detecting the output of a small household battery from extraordinary distances under ideal conditions, though in the ocean the system functions at close range to help sharks pinpoint hidden prey.
While beachgoers scan the water looking for dorsal fins, hammerheads are effectively scanning the seafloor for living electrical currents.
That sensory adaptation helps explain why multiple hammerhead species can occupy overlapping Atlantic waters without performing identical ecological roles.
The Offshore Traveler
The scalloped hammerhead (Sphyrna lewini) is one of the more oceanic hammerhead species associated with continental shelf edges, offshore structures, and migratory routes through deeper Atlantic water (Klimley, 1993).
A scalloped hammerhead shark (Sphyrna lewini) moves through offshore Atlantic water beyond the Carolina coast. The broad cephalofoil spreading from its head contains electroreceptors capable of detecting faint electrical signals produced by prey hidden beneath sand and low-visibility water. | Image credit: A. Murch
Scalloped hammerheads often move in schools, particularly when younger, and feed heavily on fish, squid, and smaller sharks. Their body shape and behavior are well suited for highly mobile pelagic hunting where prey concentrations shift constantly with temperature and current boundaries.
They are not simply “using deeper water.” They are adapted to a system where the structure itself is always moving.
Warm and cool water masses sliding against one another can compress bait into narrow feeding corridors. Squid rise toward the surface after dark. Pelagic fish move vertically and horizontally depending on light levels and prey availability. The scalloped hammerhead’s movement patterns mirror that instability.
Because they occupy such mobile offshore environments, scalloped hammerheads help regulate prey populations across broad sections of the continental shelf rather than within a single localized habitat.
The Hidden Hammerhead
For decades, scientists believed many hammerheads moving through the western Atlantic belonged to the same species.
But the Carolina hammerhead (Sphyrna gilberti) had likely been there the entire time unnoticed.
Researchers eventually discovered that some sharks identified as scalloped hammerheads were genetically distinct and consistently possessed fewer vertebrae, revealing that two separate species had been moving through the same waters unnoticed (Quattro et al., 2013).
Radiographs of the Carolina hammerhead (Sphyrna gilberti) (left) helped reveal that a second hammerhead species had been moving through western Atlantic waters largely unnoticed. Although visually similar to the scalloped hammerhead (right), skeletal differences and genetic analysis confirmed the Carolina hammerhead as a distinct species in 2013. | Image credit: J. Quattro et al., 2013 (left); S. Raredon, Smithsonian Institution, National Museum of Natural History (right)
The discovery revealed that even sharks moving through the same Atlantic waters were more specialized than they first appeared.
From the beach, the offshore Atlantic often appears open and uniform because distance hides most of its detail. But even scientists were still uncovering hidden structures within those waters. Sharks that looked nearly identical from the surface were occupying the same coastline as separate species with potentially different ecological roles.
The Carolina hammerhead still overlaps geographically with other hammerheads along the southeastern United States, and researchers are continuing to study how those species divide habitat, prey, and movement through the Atlantic.
For beachgoers, the discovery is a reminder that the Atlantic beyond the breakers is more ecologically layered than it first appears, with multiple shark species occupying waters that can look uniform from shore.
The Ray Hunter
The great hammerhead (Sphyrna mokarran) occupies a different ecological role than its smaller relatives.
A great hammerhead shark (Sphyrna mokarran) moves through offshore water. The species is highly specialized for hunting rays, using its broad cephalofoil to improve maneuverability and detect prey hidden along the seafloor. | Image credit: Oregon State University
Great hammerheads are more solitary and strongly associated with rays, including stingrays and cownose rays. Their cephalofoil is not simply a sensory structure. It also improves maneuverability and may help pin rays against the seafloor during feeding attempts (Strong et al., 1990).
That specialization matters because rays themselves strongly influence coastal ecosystems.
Rays such as cownose rays and Atlantic stingrays disturb sediment, expose buried organisms, and alter benthic communities while feeding across shallow coastal bottoms. Great hammerheads help regulate those ray populations and influence where rays spend time feeding.
Great hammerheads influence more than the number of rays moving through coastal habitats. The presence of large predators changes prey behavior as well. Rays may avoid lingering in exposed feeding areas when hammerheads are nearby, redistributing feeding pressure across habitats.
For beachgoers, those ecological effects may eventually appear through changes in ray abundance, feeding activity, or shifting patterns of disturbed sediment along shallow coastal waters.
The Cooler-Water Hunter
The smooth hammerhead (Sphyrna zygaena) can look, at first glance, like another variation of the same hammerhead design.
But its head gives away part of its story.
Unlike the scalloped hammerhead, the smooth hammerhead lacks the central notch along the front edge of the cephalofoil. That difference may seem small to a casual observer, but it reflects a separate species adapted to a somewhat different part of the Atlantic system. Smooth hammerheads are often associated with cooler temperate waters and feed heavily on schooling fish and cephalopods moving through offshore shelf waters (Compagno, 2001).
A smooth hammerhead shark (Sphyrna zygaena) moves through open offshore water. Unlike the scalloped hammerhead, the smooth hammerhead lacks the central notch along the front edge of the cephalofoil and is more commonly associated with cooler temperate waters and schooling prey along the continental shelf. | Image credit: S. Judd
That specialization matters because schooling fish and squid help move energy through the open Atlantic.
These prey species do not stay fixed in one place. They shift with temperature, currents, light, and season, gathering in patches that may appear briefly before dispersing again. Smooth hammerheads are part of the predator community that follows and regulates that movement through cooler portions of the continental shelf.
The relationship is not simply a shark chasing fish through open water. By feeding within those moving schools, smooth hammerheads help shape how prey gathers, how long those schools remain concentrated, and how much pressure they place on smaller forage species below them in the food web.
For beachgoers, those ecological effects may eventually appear through seasonal changes in bait movement, bird activity, or the mix of predators feeding along the shelf as offshore waters warm and cool through the year.
The Shark That Connects Habitats
Few sharks move between offshore and coastal systems as fluidly as the tiger shark.
Tiger sharks (Galeocerdo cuvier) are often reduced in public imagination to sensational headlines or descriptions as “garbage eaters,” largely because of their opportunistic feeding behavior and willingness to consume a wide range of prey.
But ecological flexibility is precisely what makes them important.
A tiger shark (Galeocerdo cuvier) moves through tropical offshore water. Tiger sharks travel between offshore habitats, shoals, and coastal systems following seasonal prey movements, linking distant parts of the Atlantic food web through their wide-ranging movements and opportunistic feeding behavior. | Image credit: Fishes of Sarasota County, FL
Tiger sharks move between offshore waters, shoals, nearshore habitats, and sometimes estuarine environments following seasonal prey movements and temperature shifts (Heithaus, 2001). Sea turtles, rays, fish, carrion, and other prey species all become part of that broader movement pattern.
Their presence changes how other animals use the same habitats.
Sea turtles may avoid grazing too heavily in exposed areas when tiger sharks are nearby. Rays redistribute feeding activity. Schools of fish alter where they gather. The presence of a large predator changes how long prey species remain in one place and how intensely they feed before moving on. Areas that might otherwise experience constant grazing or disturbance begin receiving periods of recovery as animals move more cautiously through the habitat (Heithaus et al., 2008).
That movement connects habitats that people often think of as separate parts of the ocean.
A tiger shark feeding offshore may later move closer to shoals, estuaries, or coastal waters as prey shifts with season and temperature. The same predator influencing sea turtle grazing patterns offshore may eventually pass along the edges of bait schools closer to shore weeks later.
For beachgoers, those connections may appear through changing patterns of sea turtle activity, shifting schools of fish near the breakers, or the seasonal movement of predators along the Carolina coast.
The Sharks People Talk About Most
Not all sharks connected to Onslow County remain far offshore.
Species like the great white shark and bull shark tend to dominate public attention because they are more familiar through media coverage and coastal sightings. Tagged great whites moving along the Atlantic coast frequently make headlines, while sharks seen near inlets or murky water are often assumed to be bull sharks whether identification is confirmed or not.
But those assumptions can flatten the complexity of the coastal ecosystem.
Bull sharks (Carcharhinus leucas)are well known for their ability to tolerate freshwater, but they are not the only sharks capable of handling changing salinity. Along the Carolina coast, species such as bonnetheads and juvenile hammerheads also use estuarine environments where tides, rainfall, and river flow constantly shift the balance between salt and fresh water. Coastal systems are not divided into simple categories of “ocean” and “freshwater.” They are gradients, and many sharks are adapted to move through those changing conditions.
A bull shark (Carcharhinus leucas) moves through offshore water accompanied by remoras. Although bull sharks are known for their ability to tolerate lower salinity and move into estuaries and rivers, they are also highly mobile coastal and offshore predators that regularly travel through marine waters along the Atlantic coast. | Image credit: B. Skinstad
Great whites (Carcharodon carcharias), meanwhile, are often discussed as solitary coastal hunters, but along the western Atlantic they are also highly migratory predators tied to seasonal prey movements, temperature ranges, and offshore habitats (Block et al., 2011).
A great white shark (Carcharodon carcharias) moves through open offshore water. Great whites are highly migratory predators capable of traveling vast distances between offshore habitats and productive coastal feeding grounds, linking distant regions of the Atlantic and Pacific through seasonal movement. | Image credit: E. Levy
Both species are part of the broader Atlantic system connected to North Carolina’s coast, but the sharks occupying pelagic waters beyond the visible horizon often receive far less attention despite shaping offshore food webs just as strongly.
Why Recovery Takes So Long
Many fish species along the Carolina coast mature quickly and reproduce in enormous numbers. Menhaden, mullet, and other forage fish may begin reproducing within only a few years while releasing hundreds of thousands—or even millions—of eggs.
Large sharks follow a very different strategy.
Species like great hammerheads, tiger sharks, and threshers often require more than a decade to reach reproductive maturity, and they produce far fewer offspring than most bony fish (Cortés, 2000). Some large female sharks may spend well over a decade surviving storms, fishing pressure, predators, disease, and changing ocean conditions before producing pups for the first time.
That slower reproductive strategy evolved partly because large sharks occupy upper levels of the food web where adults face relatively few natural predators. Evolution favored longer lifespans, slower growth, and fewer offspring with higher survival chances.
But the same strategy creates vulnerability.
A fish population capable of reproducing within two or three years can rebound relatively quickly after declines. A shark population that requires fifteen years or more to produce breeding adults cannot.
The offshore Atlantic built these predators slowly.
And when populations decline, recovery happens slowly as well.
Why More Sightings Do Not Always Mean More Sharks
For many people along the Carolina coast, sharks can feel more visible now than they did decades ago.
Drone footage from the North Carolina coast reveals how modern technology now captures shark movement near beaches that would have gone largely unseen from shore only a few decades ago. Increased visibility does not necessarily mean sharks are suddenly overwhelming coastal waters, but it does change how people perceive the Atlantic around them. | Image credit: L. Abed
Anglers report more sharks taking hooked fish before they can be reeled in, a behavior known as depredation. Drone footage captures feeding activity that would have gone unseen from shore years ago. Social media spreads sightings quickly, sometimes creating the impression that sharks are suddenly overwhelming coastal waters.
Some shark populations have shown signs of recovery following decades of decline and changing fishing regulations. Long-time fishers noticing more shark encounters in certain areas may not be imagining it. In some cases, there likely are more sharks present than there were during periods of heavier population decline in the late twentieth century.
But recovery is not the same as overabundance.
Forty years ago, far fewer people were fishing offshore, kayaking through estuaries, filming the surf with drones, or posting shark encounters online in real time. Coastal waters are now observed more continuously than at any point in history, while recreational fishing activity itself creates more opportunities for sharks and people to interact.
Even with signs of recovery, many large shark species along the Atlantic coast still exist at a fraction of the population levels seen before major declines in the late twentieth century (Baum et al., 2003; Worm et al., 2013).
A true overabundance of large predators would likely look very different along the Carolina coast. Bait schools would become harder to find, feeding activity along the surface would begin thinning out, and predators would increasingly compete over limited prey. Instead, much of what people are witnessing today is the overlap between recovering shark populations, concentrated recreational fishing activity, and a coastline watched more closely than ever before (Heithaus et al., 2008).
For beachgoers, that change can make sharks feel suddenly more common, even as many offshore ecosystems are still rebuilding from declines that unfolded over generations.
What Changes Along the Coast When They Decline
By the time most people arrive at the beach in summer, the offshore system is already in motion.
Pelicans are not simply following random schools of fish. The bait moving through the breakers may have spent weeks feeding along temperature boundaries farther offshore. Rays passing through the shallows are connected to predators that hunt them beyond the visible edge of the continental shelf. Squid rising toward the surface at night become part of a food web that stretches from deep Atlantic water back toward the surf zone.
Most of those connections remain invisible from shore.
A person standing on the beach cannot see a bigeye thresher moving through dim offshore water hundreds of feet below the surface, or a hammerhead sweeping across the bottom searching for the electrical signals of buried prey. They cannot see tiger sharks shifting between offshore and coastal habitats as water temperatures change through the season.
But those predators still influence what eventually reaches the coastline.
The schools of fish birds gather over, the movement of rays through shallow water, the distribution of predators and prey along the continental shelf, and even the timing of seasonal feeding activity are tied to an offshore ecosystem organized partly by sharks most people never encounter directly.
From the beach, the Atlantic often appears flat and open beyond the horizon.
In reality, it is layered with movement, specialization, and predators adapted to parts of the ocean most people never realize are there.
What the Horizon Conceals
From the beach, the Atlantic often appears flat and empty beyond the breakers. Most people will never see a bigeye thresher rising from dim offshore water or a hammerhead sweeping across the continental shelf searching for prey hidden beneath the sand. The larger structure of the pelagic Atlantic remains mostly invisible from shore.
But the absence of visibility is not the same as absence of life.
Far beyond the swimming beaches and nearshore bars, sharks continue moving through layered offshore habitats shaped by depth, temperature, migration, and prey. Some travel between offshore waters and shoals. Others patrol deeper pelagic systems where sunlight fades and the surface reveals little of what exists below.
Those movements eventually connect back to the coast itself.
The same Atlantic that carries sea turtle hatchlings past the breakers, pushes baitfish toward the shoreline, and gathers pelicans over feeding fish also extends outward into a far larger offshore ecosystem organized by predators most people never see directly.
The horizon does not separate the beach from another ocean.
It only marks the point where the visible Atlantic gives way to the hidden one.
Even from the shoreline, the Atlantic extends into a far larger offshore ecosystem shaped by predators, migration, depth, and movement beyond what can easily be seen from shore. The horizon does not mark the end of the ocean’s structure, only the limit of what we can observe from the beach. | Image credit: A. Mitchell
References
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Block, B. A., Jonsen, I. D., Jorgensen, S. J., Winship, A. J., Shaffer, S. A., Bograd, S. J., Hazen, E. L., Foley, D. G., Breed, G. A., Harrison, A., Ganong, J. E., Swithenbank, A., Castleton, M., Dewar, H., Mate, B. R., Shillinger, G. L., Schaefer, K. M., Benson, S. R., Weise, M. J., … Costa, D. P. (2011). Tracking APEX marine predator movements in a dynamic ocean. Nature, 475(7354), 86-90. https://doi.org/10.1038/nature10082
Compagno, L. J. (2001). Sharks of the world: An annotated and illustrated catalogue of shark species known to date (2nd ed.). Food and Agriculture Organization of the United Nations.
Heithaus, M. R. (2001). The biology of tiger sharks, Galeocerdo Cuvier, in Shark Bay, Western Australia: Sex ratio, size distribution, diet, and seasonal changes in catch rates. Environmental Biology of Fishes, 61(1), 25-36. https://doi.org/10.1023/a:1011021210685
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Kajiura, S. M. (2001). Head morphology and Electrosensory pore distribution of Carcharhinid and Sphyrnid sharks. Environmental Biology of Fishes, 61(2), 125-133. https://doi.org/10.1023/a:1011028312787
Klimley, A. P. (1993). The Behavior and Ecology of the Scalloped Hammerhead Shark. Stanford University Press.
Oliver, S. P., Turner, J. R., Gann, K., Silvosa, M., & D’Urban Jackson, T. (2013). Thresher sharks use tail-slaps as a hunting strategy. PLoS ONE, 8(7), e67380. https://doi.org/10.1371/journal.pone.0067380
Quattro, J. M., Driggers, W. B., Grady, J. M., Ulrich, G. F., & Roberts, M. A. (2013). Sphyrna gilberti, a new hammerhead shark (Carcharhiniformes, Sphyrnidae) from the western Atlantic Ocean. Zootaxa, 3702(2), 159. https://doi.org/10.11646/zootaxa.3702.2.5
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Strong, W. R., Snelson, F. F., & Gruber, S. H. (1990). Hammerhead shark predation on Stingrays: An observation of prey handling by Sphyrna mokarran. Copeia, 1990(3), 836. https://doi.org/10.2307/1446449
Worm, B., Davis, B., Kettemer, L., Ward-Paige, C. A., Chapman, D., Heithaus, M. R., Kessel, S. T., & Gruber, S. H. (2013). Global catches, exploitation rates, and rebuilding options for sharks.
Sometimes the estuary changes before people notice why.
The water may look normal from shore, but drifting just beneath the surface are long ribbons of translucent gelatin — soft strands that gather along marsh edges, collect in eddies, or drift through the current like mucus suspended in the tide. In Surf City this week, people described them as “whale snot.”
Gelatinous material collected from Murrells Inlet, South Carolina at the low tide edge. Such suspended material may include colonial tunicates, salps, mucus-rich plankton aggregates, and other organic matter associated with productive estuarine conditions. | Image credit: J. Mattevi
They are more likely colonial tunicates or salps, gelatinous filter-feeders that can appear suddenly when conditions in the water favor rapid plankton growth (Bone, 1998; Madin & Deibel, 1998).
What matters is not only the organisms themselves, but what their appearance says about the estuary around them.
The drifting forms
These blooms often form when the water column becomes temporarily stable and productive (Madin, 1982). Warmer temperatures, calmer conditions, reduced wave turbulence, and elevated plankton concentrations create an environment where filter-feeding gelatinous organisms can reproduce rapidly. Water moving through the inlets may also transport offshore plankton communities into the estuary, concentrating them in tidal creeks and slower-moving surface water (Bone, 1998; Madin, 1982).
In these calmer stretches, the water column begins separating into layers. Suspended plankton remains concentrated near the surface while weaker turbulence allows fragile gelatinous colonies to persist long enough for blooms to form. What would normally disperse through wave action instead remains suspended within the estuary itself (Madin, 1982).
To most people, they look like debris.
Ecologically, they are processing the estuary in real time.
Salps and colonial tunicates continuously pump water through their bodies, removing suspended phytoplankton, bacteria, and organic particles from the water column. During bloom periods, enormous volumes of water can be filtered each day (Madin, 1982; Sutherland et al., 2010). In effect, the estuary briefly develops a drifting layer of living filtration suspended between the surface and the bottom.
Each colony filters continuously. Thousands moving through a tidal creek or marsh edge at once can collectively filter enormous volumes of suspended material over short periods of time, temporarily altering the clarity and composition of the surrounding water (Riisgård & Larsen, 2010).
That shift affects everything around them.
When these blooms are abundant, water clarity can temporarily improve as suspended particles are removed. Organic material becomes concentrated into mucus-rich waste pellets and decaying gelatinous tissue that sink toward the bottom, transferring energy from the surface into benthic food webs below (Madin & Deibel, 1998). Microbes, worms, crustaceans, and scavengers begin responding almost immediately (Madin, 1982; Madin & Deibel, 1998).
Instead of remaining suspended near the surface, nutrients and organic matter begin settling downward through the water column. What had been dispersed through open water becomes concentrated along the bottom, where deposit-feeding worms, small crustaceans, microbes, and scavengers begin incorporating that material into the estuary below (Madin, 1982).
The bloom itself becomes food.
The drifting masses also create temporary structure within otherwise open water. Small fish gather along their edges. Tiny invertebrates gather within folds and strands of gelatinous tissue. Predators begin responding not only to the bloom itself, but to the concentration of life forming around it (Bone, 1998; Madin & Deibel, 1998).
Small fish and invertebrates feed around the edges of these drifting masses. Juvenile fishes may remain near these drifting masses as food becomes concentrated around them. Sea turtles, some fishes, and other gelatinous predators may increase feeding activity where blooms become dense enough to concentrate prey (Bone, 1998).
But like many ecological events, balance matters.
If too few filter-feeders are present during periods of elevated nutrients, water grows murkier and oxygen conditions become less stable, particularly during heat and nighttime respiration. But filtration at the opposite extreme can also reshape the food web. Too many gelatinous filter-feeders, however, may strip large amounts of plankton from the water column, altering food availability for larval fishes and other plankton-dependent organisms higher in the food web (Petersen & Riisgård, 1992).
Most blooms are temporary.
Currents disperse them. Heat and bacteria break them apart. Waves fragment the colonies into nearly invisible strands that disappear back into the system as quickly as they arrived. Even in collapse, the bloom continues feeding the estuary. Decaying tissue is broken apart by bacteria, consumed by scavengers, and recycled back into the same nutrient pathways that allowed the bloom to form in the first place (Madin, 1982).
But for a short period, the estuary reveals something normally hidden: the water between the marsh and the bottom is not empty space. It is an active habitat, filled with organisms that filter, recycle, transport, and redistribute energy through the coastal ecosystem (Bone, 1998; Madin, 1982).
The attached forms
Not all tunicates remain suspended in the water column. Some attach themselves directly to the surfaces that hold still long enough for life to accumulate—dock pilings, oyster shell, ropes, marsh grass roots, floats, and the shaded undersides of piers where current continues moving but turbulence drops away.
Along the estuaries of Onslow County, these attached forms become part of what looks, at first glance, like simple buildup.
The surfaces beneath docks rarely stay bare for long (Wahl, 1989; Lindeyer & Gittenberger, 2011). Marine scientists often describe these layered growths as fouling communities, but along the estuary they appear simply as the layer of life that forms on anything left in the water long enough. First comes a film too thin to notice, then algae, then colonies of organisms layered over one another until wood, shell, and rope begin carrying part of the estuary itself.
Sea squirts and other attached filter-feeders beneath a dock in Surf City, North Carolina. | Image credit: A. Mitchell
Tunicates are part of that layer.
Along this coast, attached tunicates can include solitary species like the pleated sea squirt (Styela plicata) and the sea grape (Molgula manhattensis), as well as colonial species such as Clavelina oblonga and sea pork (Aplidium stellatum) (Van Name, 1945; Lambert, 2007).
Some grow individually, attached like soft sacs with openings at the top. Others spread as colonial sheets or clustered lobes, sharing a common outer covering while continuously filtering water moving past them. Around pilings and floating docks, entire communities can form this way—sponges beside hydroids, bryozoans layered against tunicates, all responding to current, salinity, temperature, and suspended food moving through the tide (Wahl, 1989).
To most people, these surfaces register as slime.
Ecologically, they are filtration, habitat, and nutrient transfer occurring simultaneously (Wahl, 1989).
Sea squirts
The organisms most people recognize first are usually sea squirts. They appear as rubbery sacs attached beneath docks or clustered along ropes, and shell. Press one accidentally and water jets outward through small siphons near the top of the body, giving rise to the common name.
A sea squirt partially coated in algae and sediment beneath shallow estuarine water in Surf City, North Carolina. The two siphon openings are part of the continuous filtration process occurring beneath docks and marsh edges. | Image credit: A. Mitchell
Species such as the pleated sea squirt (Styela plicata) often develop thick, wrinkled outer coverings ranging from tan and off-white to purple, while the sea grape (Molgula manhattensis) forms smaller rounded bodies attached within the layered communities growing beneath docks and along estuarine structure — what marine scientists often call fouling communities (Van Name, 1945).
What looks like a reaction is actually the visible end of a process already underway.
Sea squirts continuously pull water inward through one siphon, filter out phytoplankton, bacteria, and suspended particles from the water, then expel the filtered water back into the estuary through another opening. The animal does not begin filtering when disturbed. It has been filtering the entire time (Riisgård & Larsen, 2010).
In productive estuarine water, thousands of these organisms may be pumping simultaneously (Riisgård & Larsen, 2010).
That filtration matters.
As suspended particles are removed, nutrients become concentrated into waste and biomass that can be transferred downward into bottom communities. Water clarity may improve locally (Riisgård & Larsen, 2010). Microbial activity shifts around them. Small invertebrates begin using the folds and surfaces their bodies create.
Their presence also signals something about the surrounding water.
Sea squirts tend to cluster where flow remains steady enough to deliver oxygen and suspended food continuously, but not so violent that colonies are torn free. Around tidal creeks, dock edges, and quieter stretches of the Intracoastal Waterway, their abundance often reflects a system carrying enough suspended productivity to sustain constant filtration (Barros, 2009).
Sea pork
Some tunicates take a different form entirely.
One of these is sea pork, commonly associated with colonial tunicates such as Aplidium stellatum, which spread outward as shared gelatinous colonies rather than isolated individuals (Van Name, 1945).
Sea pork, a colonial tunicate, washed ashore along Surf City, North Carolina. Though it appears as a single gelatinous mass, it is made up of thousands of tiny filter-feeding animals embedded within a shared outer layer. | Image credit: D. Miles
Sea pork spreads across submerged surfaces in thick, rubbery colonies that look less like individual animals and more like flesh-colored mats attached beneath floats and pilings. Depending on the species and age of the colony, the surface may appear muted pink, tan, orange, or almost translucent beneath the waterline.
Most people don’t realize they are looking at colonies made up of thousands of tiny individual filter-feeding bodies embedded together within a shared outer layer.
The colony functions collectively (Van Name, 1945).
Water moves continuously through countless small openings across the surface, carrying suspended plankton and organic particles into the colony while waste and filtered water move back outward into the surrounding estuary (Riisgård & Larsen, 2010).
That structure changes the surface around it.
Sea pork colonies trap sediment and create small protected surfaces where microorganisms and invertebrates begin to accumulate between folds and protected edges. Tiny crustaceans move across them. Worms and microbial films develop within the folds and protected spaces between colonies. What appears smooth from above becomes, at smaller scales, complex terrain (Wahl, 1989).
Like other filter-feeding communities along this coast, sea pork helps transfer suspended energy from the water column into the attached world beneath docks and marsh edges.
And once that layered habitat forms, other organisms begin responding to it—including the nudibranchs moving slowly across its surface.
Nudibranchs
At low tide along the edges of the sound—where pilings hold a thin skin of life and oyster shells stack into uneven ridges—the water sometimes carries color that doesn’t belong to the sand or the grass. It moves slowly, almost deliberately, across surfaces that most people step over without noticing. What looks like a fragment of drifting algae or a soft piece of shell resolves, if you stop long enough, into something alive.
These are nudibranchs.
They are not fish, not worms, not plants. They are marine gastropods—relatives of snails—but without shells (Valdés et al., 2006). Along the coast of Onslow County, they appear in the quiet places: beneath docks in the Intracoastal Waterway, along the edges of Topsail Island marsh creeks, and on the submerged surfaces where current slows just enough for growth to take hold.
Along shallow estuarine structure in this region—beneath docks, across pilings, and within the layered growth attached to ropes and shell—nudibranchs may include species such as the striped nudibranch (Cratena pilata), the Brazilian aeolid sea slug (Spurilla braziliana), the fringeback dondice (Dondice occidentalis), Thecacera pennigera, Berghia rissodominguezi, and the brackish-water species Tenellia adspersa (Marcus, 1972; Valdés et al., 2006).
Most people never see them. But they are there, working through the same system that shapes everything else along this coast.
A nudibranch collected near Morehead City, North Carolina, viewed under magnification. The cerata along its back increase surface area for respiration and, in some species, store defensive stinging cells obtained from prey. | Image credit: marineinvertgirl, iNaturalist
Built for sensing, not speed
A nudibranch’s body is built for sensing and feeding, not speed. The two structures at the front—rhinophores—sample the water chemically, reading it the way a shoreline bird reads the wind. Along their backs, many species carry cerata, small extensions that look ornamental but function as both respiration and defense.
In aeolid nudibranchs like Spurilla braziliana, Cratena pilata, and Berghia rissodominguezi, these cerata become important sites for both respiration and defensive storage of stinging cells obtained from prey (Goodheart et al., 2018).
The Brazilian aeolid sea slug (Spurilla braziliana) moving across submerged structure near Morehead City, North Carolina. The cerata lining its back function in respiration and can store defensive stinging cells obtained from prey such as anemones and hydroids. | Image credit: wonglab, iNaturalist
They move slowly because they can afford to. Their food doesn’t run.
Sponges, hydroids, bryozoans—these are the surfaces most people would describe as “growth” on docks or shells. To a nudibranch, those surfaces are structure, habitat, and food all at once (Valdés et al., 2006).
The work they do (even when no one’s watching)
Along this coastline, growth is constant. Give any hard surface—an old piling, a piece of shell, a boat hull—enough time in the water and it becomes layered. First a film, then algae, then invertebrates. The system builds upward and outward, creating what scientists call structural complexity, but what you actually see is texture: roughness where there used to be smoothness (Wahl, 1989).
Along shallow estuarine bottoms, algae, shell, and attached growth begin forming the layered habitat that supports juvenile fish, crabs, filter-feeders, and the organisms moving through the estuary food web. | Image credit: A. Mitchell
Nudibranchs move through that texture selectively.
Many species feed on a single type of prey. One may specialize in a particular sponge. Another tracks hydroids, those delicate branching animals that resemble tiny underwater ferns. Species such as Dondice occidentalis, Cratena pilata, and Tenellia adspersa are commonly associated with hydroids and other organisms growing across submerged pilings, docks, ropes and shell in shallow coastal environments (Marcus, 1972; Valdés et al., 2006). This selectivity matters more than their size suggests. They are not removing everything. They are removing specific pieces of the system.
That kind of feeding does not flatten the landscape—it shapes it.
Where one organism begins to dominate, nudibranchs can limit its spread. Where surfaces would otherwise become uniform, their grazing introduces variation. Over time, this helps maintain the uneven habitat small fish, shrimp, and juvenile invertebrates depend on (Wahl, 1989).
Growth that begins as algae quickly becomes habitat. Along shallow estuarine edges, layered vegetation and attached organisms create shelter for crabs, juvenile fish, shrimp, and other small life moving through the system. | Image credit: A. Mitchell
It’s easy to miss because nothing dramatic happens. There’s no visible clearing, no sudden absence. But the balance of what grows, and where, shifts quietly in response to their presence.
Borrowed defenses, redistributed energy
Some nudibranchs do something that seems improbable until you see it up close: they take the defenses of what they eat and keep them.
Hydroids and certain cnidarians carry stinging cells—nematocysts—that function as protection. When a nudibranch feeds on them, those cells pass through the digestive system intact and are stored within the cerata along its back. The nudibranch doesn’t just consume its prey; it incorporates part of its defense (Goodheart et al., 2018).
This changes how energy moves through the system.
Instead of defenses being lost when prey is consumed, they are transferred upward. The nudibranch becomes both grazer and deterrent, a small organism that is less likely to be eaten because of what it has already eaten.
You can see the result in their coloration. Many are bright, almost out of place against the muted tones of sand and shell. That color is not decoration—it’s a signal (Avila, 1995). Along this coast, where predation pressure is constant, visibility can function as warning rather than risk.
Where they sit in the trophic cascade
They are not apex predators. They don’t regulate fish populations or move through the system in ways that draw attention. But they occupy a position that connects the base of the food web to everything above it.
They feed on organisms that build habitat.
Those organisms—sponges, hydroids, bryozoans—form the living surface that supports small invertebrates and juvenile fish. Those smaller organisms, in turn, become prey for larger fish, which then connect to the predators people are more familiar with along this coast—species like blacktip shark (Carcharhinus limbatus) and Atlantic sharpnose shark (Rhizopriodion terranovae) that move along the breakers and through the sounds.
Remove the visible predators, and people notice quickly.
Remove something like a nudibranch, and what changes is slower, but it moves in the same direction. Surfaces become dominated by fewer species. Habitat becomes more uniform. The small organisms that rely on variation lose space. That change works its way upward, not as a single event, but as a shift in the system’s capacity to support diversity.
Even small organisms attached to pilings and submerged structure become part of much larger coastal food webs. Scientific food-web models show nudibranchs, hydroids, bryozoans, worms, shrimp, and fishes linked together through the transfer of energy across the ecosystem.
Generalized food web showing how organisms associated with sponge and attached invertebrate communities connect upward through coastal ecosystems. Nudibranchs, hydroids, bryozoans, worms, shrimp, and fishes all participate in the transfer of energy through these layered habitats. Adapted from Archer et al. (2020).
Why they stay hidden
There’s a reason most beachgoers never encounter them.
They live where water movement slows just enough to allow growth to accumulate, but not so still that oxygen drops away. Around docks, inside creeks, along the quieter edges of the New River estuary, they remain attached to the surfaces that feed them.
Out in the open surf, where sand shifts constantly and hard structure is buried and exposed with each change in wind and tide, there’s less for them to hold onto and less for them to eat. The breakers are a moving environment (Wahl, 1989). Nudibranchs belong to the places that hold still just long enough for complexity to form.
What changes if they’re gone
Nothing you would notice in a single afternoon at the beach.
But over time, the surfaces beneath the waterline would begin to simplify. One or two fast-growing organisms would spread further, covering space that would otherwise remain shared. The small sheltered spaces used by larval fish, juvenile shrimp, and small crabs would begin to thin out.
That loss doesn’t stay at the bottom.
It moves upward, changing how much life the system can support, and how evenly that life is distributed. By the time it reaches the fish people see from the shore, the cause is no longer visible. But it started here, in the slow movement of something small across a surface most people never look at twice.
Nudibranchs don’t reshape the coastline in ways that draw attention. They don’t mark their presence with absence or disturbance. Instead, they work within what’s already there—adjusting, redistributing, and maintaining the uneven structure that makes this coast function.
If you happen to see one, it won’t be moving fast. It won’t need to.
What they’re feeding on (and why it looks familiar)
Along the docks and pilings of Onslow County, the surfaces most people notice first aren’t fish at all. They’re the things attached to everything.
The branching, plant-like fuzz that brushes your hand when you reach into the water—those are hydroids. The firm, uneven coatings that look like they’re part of the structure itself are often sponges or bryozoans.
It’s easy to group all of it together as buildup. Something slimy, something in the way.
But that “squirt” people laugh about isn’t random. A tunicate pulls water in, filters out plankton and suspended particles, and then expels that water back out. What looks like a reaction is just the visible end of constant filtration. They are processing the water column—removing particles, cycling nutrients, and clarifying the water in small, continuous ways (Riisgård & Larsen, 2010).
Hydroids are doing something different. They are predators at a scale most people don’t consider, capturing microscopic prey drifting past. Sponges filter continuously as well, pulling bacteria and organic matter from the water and converting it into biomass that other organisms can use.
A sea anemone beneath shallow estuarine water in Surf City, North Carolina. Organisms like these become part of the layered communities that nudibranchs, tunicates, hydroids, and other invertebrates move through beneath the surface. | Image credit: A. Mitchell
This is the surface layer of the ecosystem. And it doesn’t stay unchecked.
The ones moving across the surface
Species like the Brazilian aeolid sea slug (Spurilla braziliana) often feed directly on anemones associated with these same submerged communities, while smaller species such as Tenellia adspersa are frequently associated with hydroids in brackish and estuarine waters (Valdés et al., 2006).
The nudibranchs moving across these surfaces are not all the same, and what they eat tells you what role they’re playing.
Some of the small, leaf-like sea slugs in this region—species in the genus Elysia—feed on algae and can even retain the chloroplasts from what they consume, briefly using sunlight as part of their energy system. They blur the line between grazing and something closer to plant-like function (Valdés et al., 2006).
Others, like Cratena pilata and Dondice occidentalis, track hydroids specifically. Where hydroids begin to spread across a piling, these nudibranchs follow, feeding in a way that limits how dense those colonies can become (Marcus, 1972).
Species such as Thecacera pennigera are often associated with the layered communities growing beneath docks and harbor structure, while Berghia rissodominguezi and Spurilla braziliana move through shallow cnidarian-rich habitat where anemones and hydroids provide both food and defensive material (Valdés et al., 2006).
Heavier-bodied nudibranchs—often in groups like Doris—tend to feed on sponges. Not all sponges, and not everywhere, but selectively enough that no single form easily dominates a surface for long.
Even their eggs reflect this connection. The ribbon-like spirals sometimes seen attached to docks are laid directly where food is available. The next generation doesn’t disperse randomly—it begins where the system is already functioning.
Beneath the surface layer
Most of the time, these organisms go unnoticed.
People see the drifting ribbons and call them whale snot. They scrape tunicates from pilings without thinking about what those colonies were filtering from the water. They brush past hydroids and sponges growing beneath docks without realizing those surfaces are part of the estuary’s food web just as much as the fish moving above them.
But the water between the marsh and the bottom is never empty.
It carries suspended plankton, drifting larvae, dissolved nutrients, bacteria, predators, scavengers, and colonies of organisms filtering continuously through the tide. Along the quieter edges of Onslow County—beneath floats, around oyster shells, beside marsh grass roots, and inside the slower water of creeks and sounds—entire communities form within that suspended layer (Wahl, 1989; Lindeyer & Gittenberger, 2011).
Some drift. Some attach. Some graze slowly across the surface consuming the organisms beneath them.
Together, they reshape the estuary constantly.
The gelatinous ribbons appearing this week are not separate from the rest of the system. They are one visible moment in a larger cycle of filtration, growth, decay, grazing, and redistribution that normally happens out of sight (Bone, 1998; Madin, 1982). For a short time, the estuary simply becomes easier to see.
What appears empty from above often contains layered communities of algae, filter-feeders, invertebrates, and microorganisms quietly redistributing energy through the estuary. Surf City, North Carolina. | Image credit: A. Mitchell
References
Avila, C. (1995). Natural products of opisthobranch molluscs: A biological review. In Oceanography and marine biology: An annual review (33rd ed., pp. 487-559). UCL Press.
Barros, R. (2009). Human-mediated global dispersion of Styela plicata (Tunicata, Ascidiacea). Aquatic Invasions, 4(1), 45-57. https://doi.org/10.3391/ai.2009.4.1.4
Bone, Q. (1998). The biology of pelagic tunicates. Oxford University Press on Demand.
Encarnação, J., Seyer, T., Teodósio, M. A., & Leitão, F. (2020). First record of the nudibranch Tenellia adspersa (Nordmann, 1845) in Portugal, associated with the invasive hydrozoan Cordylophora caspia (Pallas, 1771). Diversity, 12(6), 214. https://doi.org/10.3390/d12060214
Goodheart, J. A., Bleidißel, S., Schillo, D., Strong, E. E., Ayres, D. L., Preisfeld, A., Collins, A. G., Cummings, M. P., & Wägele, H. (2018). Comparative morphology and evolution of the cnidosac in Cladobranchia (Gastropoda: Heterobranchia: Nudibranchia). Frontiers in Zoology, 15(1). https://doi.org/10.1186/s12983-018-0289-2
Korshunova, T., Lundin, K., Malmberg, K., Picton, B., & Martynov, A. (2018). First true brackish-water nudibranch mollusc provides new insights for phylogeny and biogeography and reveals paedomorphosis-driven evolution. PLOS ONE, 13(3), e0192177. https://doi.org/10.1371/journal.pone.0192177
Lambert, G. (2007). Invasive sea squirts: A growing global problem. Journal of Experimental Marine Biology and Ecology, 342(1), 3-4. https://doi.org/10.1016/j.jembe.2006.10.009
Lindeyer, F., & Gittenberger, A. (2011). Ascidians in the succession of marine fouling communities. Aquatic Invasions, 6(4), 421-434. https://doi.org/10.3391/ai.2011.6.4.07
Madin, L. P. (1982). Production, composition and sedimentation of salp fecal pellets in oceanic waters. Marine Biology, 67(1), 39-45. https://doi.org/10.1007/bf00397092
Petersen, J., & Riisgard, H. (1992). Filtration capacity of the ascidian Ciona intestinalis and its grazing impact in a shallow fjord. Marine Ecology Progress Series, 88, 9-17. https://doi.org/10.3354/meps088009
Riisgård, H., & Larsen, P. (2010). Particle capture mechanisms in suspension-feeding invertebrates. Marine Ecology Progress Series, 418, 255-293. https://doi.org/10.3354/meps08755
Sutherland, K. R., Madin, L. P., & Stocker, R. (2010). Filtration of submicrometer particles by pelagic tunicates. Proceedings of the National Academy of Sciences, 107(34), 15129-15134. https://doi.org/10.1073/pnas.1003599107
Valdés, Á., Behrens, D. W., & DuPont, A. (2006). Caribbean Sea slugs: A Field guide to the opisthobranch mollusks from the tropical Nortwestern Atlantic. Sea Challengers Natural History Books.
Van Name, W. G. (1945). The North and South American Ascidians. Bulletin of American Museum of Natural History, 84, 1-476. http://hdl.handle.net/2246/1186
Wahl, M. (1989). Marine epibiosis. I. Fouling and antifouling: Some basic aspects. Marine Ecology Progress Series, 58, 175-189. https://doi.org/10.3354/meps058175
On a late spring morning along Surf City, the first movement is often above the water, not within it. Brown pelicans travel low and steady just beyond the breakers, their wingtips nearly touching the surface as they follow a line that seems invisible from shore. Farther out, a group of terns holds in place against the wind, hovering, adjusting, then dropping sharply into the water before rising again. Closer to the sound side of Topsail Island, an osprey circles once, then folds into a dive toward a channel edge that looks, at first glance, no different than the water around it.
Nothing about these movements is random. They are responses to structure that exists beneath the surface—structure shaped by tide, wind, and the movement of other organisms. What appears as scattered bird activity is, in practice, a map of where the water is concentrating life.
For someone standing at the edge of it, that movement is one of the most accessible ways to read what cannot be seen directly.
What Birds Are Following Beneath the Surface
The birds that move along this stretch of coast are not searching broadly; they are tracking concentration. Along barrier island systems like those in Onslow County, physical processes—tidal exchange through inlets, wind-driven surface currents, and subtle differences in bottom shape—create zones where small fish, shrimp, and other prey accumulate (Peterson & Peterson, 1979; Piersma, 1997).
When the tide moves through places like New River Inlet, water does not flow evenly across the landscape. It accelerates through constrictions, slows along marsh edges, and bends around sandbars and channels. These shifts in speed and direction compress organisms into tighter spaces, particularly along boundaries where moving water meets something that resists it—an edge, a drop-off, or a change in depth (Wright et al., 1985).
Small schooling fish respond to that compression by tightening their formation. In doing so, they become more visible and more vulnerable. Larger fish—bluefish, Spanish mackerel, and juvenile coastal sharks—often move in from below, using that same concentration to feed. The pressure from below pushes prey upward, sometimes all the way to the surface.
Coastal birds feeding where prey has been concentrated near the surface along the breakers. | Image credit: A. Mitchell
What appears overhead depends on which part of that concentration each species is built to exploit.
Terns hovering and diving are often responding to prey that has been driven upward by predatory fish (Safina & Burger, 1985). Brown pelicans, which rely on plunge-diving, tend to follow more stable schools of fish that remain near the surface for longer periods (Shields, 2014). Ospreys, in contrast, depend on clear water and individual fish they can visually isolate, which is why their activity often aligns with calmer conditions and defined channel edges (Poole et al., 2002).
Each species is not simply feeding in the same place; each is reading a different layer of the same system.
When Surface Activity Signals Pressure Below
From the shoreline, bird activity can appear as isolated events—one dive, then another, then a sudden shift down the beach. Watched over time, a pattern emerges. A cluster of terns may concentrate in one location for several minutes, then disperse abruptly, reforming farther along the shoreline. Pelicans may align along a narrow band just beyond the breakers, following it as it drifts.
These shifts often reflect changes in how prey is being compressed and released beneath the surface. When predatory fish move through a bait school, the school tightens, rises, and becomes briefly accessible from above. When that pressure dissipates, the school spreads out again, and the birds move on.
This movement of energy—from smaller organisms to larger predators, and upward through the water column—is one visible expression of a trophic cascade. The term itself is often used to describe longer chains of ecological influence, but along the coast it can be observed in compressed moments, where the effects of predation become visible within seconds (Heithaus et al., 2008).
Birds do not initiate this process. They respond to it. Their presence marks where the system has already intensified.
Indicator Species at the Water’s Edge
From the beach, the difference is subtle. The water does not change color dramatically, and the waves continue to break as they did before. The level of activity shifts within that band—first visible in the air, then inferred below– marking places where the system has tightened, energy is moving through multiple layers at once, and the distance between surface and depth has, for a time, narrowed (Heithaus et al., 2008; Estes et al., 2011).
For someone entering the water, these differences in bird behavior can offer practical information, not in a predictive or absolute sense, but as indicators of what is happening just below the surface.
Brown pelicans traveling low in a consistent line often indicate schools of fish moving parallel to shore. Terns repeatedly diving in a tight area suggest smaller prey being pushed upward, frequently by larger fish feeding below. Ospreys focusing on a specific channel edge reflect clearer water and individual prey availability, rather than broad schooling events. Along the shoreline, shorebirds probing the sand at low tide are responding to invertebrates exposed by receding water, signaling a different layer of the system entirely—one tied to sediment and tidal timing rather than active predation (Colwell, 2010; Piersma, 1997).
None of these signals point directly to a specific species beneath the surface. What they indicate is concentration, and concentration is what draws larger predators closer to shore.
Along the coast of North Carolina, nearshore and juvenile shark presence is often associated with areas of high prey density, particularly where schooling fish aggregate (Heupel & Hueter, 2002). These conditions are not constant, and they shift with tide, temperature, and time of day. Birds make those shifts visible in real time.
At times, that activity stretches into lines that run the length of the breakers.
For someone stepping into the water, that narrowing matters. Not as a warning in the abstract, but as a recognition that the conditions supporting visible feeding above often extend below, linking organisms that are rarely seen together into the same moving structure.
Where the System Tightens
The patterns become easier to see near places where the water is forced to narrow, turn, or accelerate. The most consistent bird activity along this coast tends to occur where water movement is constrained and redirected. Inlets, marsh edges, sandbars, and the transitions between the Intracoastal Waterway and adjacent sounds create these zones (Wright et al., 1985).
At New River and its inlet, tidal flow compresses water into narrow channels before releasing it into broader areas, creating gradients in speed and depth. Along these gradients, prey accumulates, predators follow, and birds gather above.
These are not fixed points. As tide rises and falls, and as wind reshapes surface conditions, the locations of these compression zones shift. The birds move with them, tracing patterns that are constantly changing but not random.
For someone watching from shore, these movements can be read as lines, clusters, and absences—places where activity intensifies, and places where it suddenly drops away.
Standing Within It
Entering the water along this coast means stepping into a system already in motion. The surface may appear uniform, but the activity above it often reveals where that motion is focused.
Birds diving repeatedly in a confined area, or tracking a narrow band just beyond the breakers, indicate where prey is concentrated. Those same conditions are what draw larger predators into closer proximity to shore, not as an anomaly, but as part of the same process.
Watching the birds does not eliminate risk, and it does not provide certainty about what is beneath the surface. What it offers is context—a way to recognize when the water is more active, more compressed, and more connected across its layers.
What appears as feeding from above is part of a larger structure moving through the water. The birds do not create it, and they do not remain once it passes. They mark it, briefly, making visible what is otherwise difficult to see.
Bird movement along the shoreline often draws attention toward activity that remains unseen beneath the surface. | Image credit: A. Mitchell
References
Castro, J. I. (1993). The shark nursery of bulls Bay, South Carolina, with a review of the shark nurseries of the southeastern coast of the United States. Environmental Biology of Fishes, 38(1-3), 37-48. https://doi.org/10.1007/bf00842902
Colwell, M. A. (2010). Shorebird ecology, conservation, and management. University of California Press.
Estes, J. A., Terborgh, J., Brashares, J. S., Power, M. E., Berger, J., Bond, W. J., Carpenter, S. R., Essington, T. E., Holt, R. D., C. Jackson, J. B., Marquis, R. J., Oksanen, L., Oksanen, T., Paine, R. T., Pikitch, E. K., Ripple, W. J., Sandin, S. A., Scheffer, M., Schoener, T. W., & Wardle, D. A. (2011). Trophic downgrading of planet Earth. Science, 33(6040), 301-306. https://doi.org/10.1126/science.1205106
Heithaus, M. R., Frid, A., Wirsing, A. J., & Worm, B. (2008). Predicting ecological consequences of marine top predator declines. Trends in Ecology & Evolution, 23(4), 202-210. https://doi.org/10.1016/j.tree.2008.01.003
Heupel, M. R., & Hueter, R. E. (2002). Importance of prey density in relation to the movement patterns of juvenile blacktip sharks ( Carcharhinus limbatus ) within a coastal nursery area. Marine and Freshwater Research, 53(2), 543-550. https://doi.org/10.1071/mf01132
Piersma, T. (1997). Do global patterns of habitat use and migration strategies Co-evolve with relative investments in Immunocompetence due to spatial variation in parasite pressure? Oikos, 80(3), 623-631. https://doi.org/10.2307/3546640
Poole, A. F., Bierregaard, R. O., & Martell, M. S. (2002). Osprey (Pandion haliaetus). In The Birds of North America (1st ed.). Cornell Lab of Ornithology.
Safina, C., & Burger, J. (1985). Common tern foraging: Seasonal trends in prey fish densities and competition with bluefish. Ecology, 66(5), 1457-1463. https://doi.org/10.2307/1938008
Shields, M. (2014). Brown Pelican (Pelecanus occidentalis). In Birds of North America (1st ed.). Cornell Lab of Ornithology.
Wright, L., Short, A., & Green, M. (1985). Short-term changes in the morphodynamic states of beaches and surf zones: An empirical predictive model. Marine Geology, 62(3-4), 339-364. https://doi.org/10.1016/0025-3227(85)90123-9
There are places along the edges of the water in Onslow County where the ground stops behaving like ground.
You find them along the sound side, at the margins of tidal creeks, and in the quieter edges of channels that drain toward New River Inlet. Places like the shallows near Soundside Park or the creek edges around Kenneth D. Batts Family Park look ordinary when the tide is in—flat water, sometimes with a darker tone beneath the surface, but otherwise unremarkable.
As the tide pulls away, that surface is left behind, exposed in a way that suggests continuity, as though it will hold underfoot the same way sand does along the open beach.
It holds just long enough to believe that.
Then it gives way.
A step sinks past the ankle before there is time to adjust, and the next carries deeper, the sediment tightening around your leg—not suddenly, but with a steady resistance that makes each movement slower than expected, until pulling free requires more effort than the surface first suggested and the footing you thought you had no longer offers anything solid to push against.
Sometimes the mud keeps what you brought with you.
It holds—until it doesn’t. | Image credit: Florida Tech
Each step releases a faint, unmistakable sulfur smell from below, brief but distinct, rising as the sediment shifts and settling again as it closes around the space you’ve displaced.
Nothing about it suggests stability, and yet nothing about it is still.
Where It Forms: Water That Slows Down
If you step back—onto firmer ground, where your footing holds—the pattern begins to show itself.
These places gather along edges where water loses momentum. Along the sound side, there are no breaking waves to constantly overturn the bottom. Water moves in, spreads thin across the flats, and then drains back through the same narrow paths, slowing as it goes.
When that movement slows, what the water was carrying no longer stays suspended.
Fine silts and clays begin to settle. Fragments of marsh grass drift down. Microscopic shells and organic particles—too small to notice while they are moving—collect layer by layer until the bottom changes character (Folk, 1980; Riggs et al., 2008).
Much of that material begins only a few feet away.
Where the water slows, what it carries begins to settle. | Image credit: A. Mitchell
Along the edges of these creeks, smooth cordgrass—Spartina alterniflora—holds the shoreline in place. When it dies back, it doesn’t disappear. It breaks apart, and with each tide, that material moves outward. What looks like loss becomes movement—organic matter carried away from the marsh and into these quieter edges (Odum, 1980).
Where the water lingers, that material accumulates.
And over time, accumulation becomes something you can step into.
The Surface: What Almost Holds
From above, it can look continuous.
In certain light—especially when the sun is low—there is a faint sheen across the surface, something smoother and more uniform than water alone would create. It can appear firm enough to cross, at least for a step or two.
That thin layer is not just sediment.
It settles just enough to look stable—until the weight shifts. | Image credit: A. Mitchell
Microscopic organisms—diatoms and cyanobacteria—spread across the surface, forming a film that binds particles together. They produce substances that hold grains in place, creating a surface that can briefly support weight before it gives way beneath it (Rimmer et al., 2025).
It is just enough structure to mislead you.
Just enough to suggest that what lies beneath it will behave the same way.
Why It Gives Way: Structure Without Support
Once that surface breaks, the difference becomes immediate.
The particles here are small enough to trap water between them, and once that water is there, it does not drain the way it does through sand. The sediment remains saturated, and when pressure is applied, the water has nowhere to go.
Instead of holding its shape, the ground shifts.
There is a way to describe how well a surface resists that kind of movement—shear strength. Sand has enough of it to support your weight.
This does not (Folk, 1980).
There’s form here, but no support—only water and loosened sediment. | Image credit: A. Mitchell
And beneath the surface, the structure is already interrupted. Burrows open and collapse. Small voids form and disappear. Gas collects in pockets that shift when disturbed. What looks continuous from above is already moving below.
So when your foot sinks, it is not breaking through something solid.
It is entering something that was never still to begin with.
Below the Surface: Where the Air Runs Out
The smell arrives as soon as the surface opens.
It rises quickly, sharp and distinct, and then fades again as the mud closes.
Just beneath the surface, oxygen is used up rapidly by microorganisms breaking down the organic material that has accumulated there. Below that thin layer, the sediment becomes anoxic—oxygen is no longer present (Fenchel & Riedl, 1970; Jørgensen & Nelson, 2004).
But the process doesn’t stop.
Bacteria continue to break material down, using sulfate from seawater instead of oxygen. That shift produces hydrogen sulfide gas, which remains trapped until the sediment is disturbed (Kasten & Jørgensen, 2000).
Each step releases it.
The smell is not separate from the system. It is evidence that the breakdown is still happening—just without air.
And because it is happening without oxygen, it happens more slowly.
What Stays Behind
If that same plant material were left exposed to air, it would break down quickly. Most of what it contains would return to the atmosphere as carbon dioxide.
Here, much of it does not.
The organic material that settles into this mud—marsh grass, algae, microscopic debris—is buried into a system where oxygen disappears almost immediately. Without that oxygen, decomposition slows, and a portion of that carbon remains stored in the sediment instead of returning to the air (Chmura et al., 2003).
It does not stop changing.
It is broken down, reworked, and shifted. But it is not fully released.
Layer after layer builds beneath the surface—material that was once living, now held within the mud you step into.
What smells like decay is also storage.
The Surface Is Breathing
Even without oxygen below, the surface is not sealed.
If you stand still long enough, you begin to see small openings, slight movements, places where the mud seems to shift or pulse.
Water moves in and out with the tide. Burrows connect the surface to what lies below. Worms, shrimp, and crabs pull oxygenated water downward as they move through the sediment (Aller, 1982; McCave, 1976).
And the plants at the edge are part of it too.
Marsh grasses do not just sit in the mud. They move oxygen from the air above down into their roots. Some of that oxygen leaks into the surrounding sediment, creating small zones where oxygen briefly exists before it is used up again.
It is uneven. Temporary. Constantly shifting.
At the surface, gases move both ways.
Oxygen enters. Carbon dioxide leaves. Small amounts of other gases—products of what is happening below—escape when the sediment is disturbed or when pressure changes with the tide.
The boundary is thin.
But it is active.
Movement You Don’t See
If you stop looking for stable ground and begin watching the surface itself, other patterns start to emerge.
What looks still is already in use. | Image credit: A. Mitchell
Small openings appear—round, spaced in ways that suggest something below rather than something left behind. Around them, slight mounds form and disappear as the mud dries and softens again.
These are not marks left on the surface. They are the surface expression of what is moving through it.
Polychaete worms pass through the sediment, ingesting it and depositing what remains behind them (Rhoads, 1974). Burrowing shrimp and amphipods maintain tunnels that allow water—and with it, oxygen—to move deeper into the mud than it otherwise could (Aller, 1982).
Crabs hold the edges.
Fiddler crabs open and close their burrows with the tide. Blue crabs move through when water returns, feeding within the same soft substrate that gives way underfoot. Mud crabs remain within it, emerging only when conditions allow.
Bivalves stay buried beneath it all, filtering water when submerged, holding position when exposed.
Sometimes you don’t see them until you feel them.
A sharp edge beneath your foot where the mud shifted just moments before.
The surface does not tell you everything that is there.
When the Water Returns
Then the water comes back.
It fills the same space that resisted your footing, covering the surface without changing what lies beneath it. The ground that gave way becomes part of a shallow, moving system again.
Fish arrive with the water.
Killifish move into these margins first, tolerating the low oxygen conditions that remain in the sediment. Flounder settle directly onto the bottom, their bodies flattening, their coloration shifting until they disappear against it.
Juvenile blue crabs move through these same areas, using them as nursery habitat—protected, shallow, and full of food (Bilkovic et al., 2020).
They are not just using the space. They are feeding on what the mud is processing.
Detritus, microbes, and organic material move through the system below the surface, supporting what arrives above it.
Other species follow.
Stingrays glide over the surface, feeding on what is buried below. Croaker move through slightly deeper channels. Along exposed flats near The Point at Topsail Beach, shorebirds track the retreating tide—probing, picking, following the movement of water as it exposes and covers the same ground again.
As the water returns, the surface changes—and life moves with it. | Image credit: A. Mitchell
What looked still becomes active.
Not because it changed.
But because the conditions around it did.
What Comes From the Marsh
At the edge where your footing gave way, the connection is already there.
The marsh does not end where the grass stops. It extends outward through what it releases.
This isn’t separate from the marsh—it’s what the marsh leaves behind. | Image credit: A. Mitchell
The grasses along the shoreline slow the water, trapping sediment and holding the edge in place. During storms, they absorb energy that would otherwise move inland, reducing erosion and limiting how much material is carried away (Barbier, 2012).
But they also export material.
As grasses break down, they move with the tide—out of the marsh, into the creeks, and into these quieter margins where the water slows again.
What settles here is not separate from the marsh.
It is what the marsh becomes once it begins to move—and what it leaves behind when it does.
What Changes, and What Doesn’t
The ground beneath you is not fixed.
Periods of calm allow fine sediments to build, thickening the layer and increasing the amount of organic material held within it. Warmer temperatures increase microbial activity, accelerating what is happening below the surface.
A storm can undo that quickly.
Sediment lifts back into the water, moves elsewhere, and settles in new places. Edges shift. Channels deepen or fill. What held you in place one week may not exist in the same way the next (Pilkey et al., 2014).
Other changes move more slowly.
Development alters how water flows. Marsh edges are reduced or hardened. Invasive plants like Vitex rotundifolia change how sediment is captured and released.
The system continues.
But the way it moves through the landscape can change.
Standing at the Edge of It
Standing at the edge of one of these places, it is easy to focus on the moment your footing failed—the way the ground gave way when it seemed like it shouldn’t.
But nothing about it failed.
What felt unstable is a working layer—one that gathers what the marsh releases, slows its return to the air, supports what can move within it, and disappears beneath the water as the tide returns.
The same ground that held you in place becomes part of something continuous again, connected to marsh, creek, sound, and ocean.
It does not hold because it is not meant to.
It holds because it is already in motion.
Nothing here failed—it’s doing exactly what it’s meant to do. | Image credit: A. Mitchell
References
Able, K., Manderson, J., & Studholme, A. (1999). Habitat quality for shallow water fishes in an urban estuary:the effects of man-made structures on growth. Marine Ecology Progress Series, 187, 227-235. https://doi.org/10.3354/meps187227
Aller, R. C. (1982). The effects of Macrobenthos on chemical properties of marine sediment and overlying water. Topics in Geobiology, 53-102. https://doi.org/10.1007/978-1-4757-1317-6_2
Barbier, E. B. (2012). Progress and challenges in valuing coastal and marine ecosystem services. Review of Environmental Economics and Policy, 6(1), 1-19. https://doi.org/10.1093/reep/rer017
Bilkovic, D., Isdell, R., Stanhope, D., Angstadt, K., Havens, K., & Chambers, R. (2021). Nursery habitat use by juvenile blue crabs in created and natural marshes. Ecological Engineering, 170(106333). https://doi.org/10.1016/j.ecoleng.2021.106333
Chmura, G. L., Anisfeld, S. C., Cahoon, D. R., & Lynch, J. C. (2003). Global carbon sequestration in tidal, saline wetland soils. Global Biogeochemical Cycles, 17(4). https://doi.org/10.1029/2002gb001917
Fenchel, T. M., & Riedl, R. J. (1970). The sulfide system: A new biotic community underneath the oxidized layer of marine sand bottoms. Marine Biology, 7(3), 255-268. https://doi.org/10.1007/bf00367496
Folk, R. L. (1980). Petrology of sedimentary rocks (2nd ed.). Hemphill Publishing Company.
Jørgensen, B. B., & Nelson, D. C. (2004). Sulfide oxidation in marine sediments: Geochemistry meets microbiology. Sulfur Biogeochemistry – Past and Present. https://doi.org/10.1130/0-8137-2379-5.63
Kasten, S., & Jørgensen, B. B. (2000). Sulfate Reduction in Marine Sediments. In Marine Geochemistry (pp. 263-264). Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-04242-7_8
McCave, I. N. (1976). Organism-Sediment Relationships. In The Benthic Boundary Layer (pp. 273-295). Plenum Press.
Odum, E. P. (1980). The status of three ecosystem-level hypotheses regarding salt marsh estuaries: Tidal subsidy, outwelling, and detritus-based food chains. Estuarine Perspectives, 485-495. https://doi.org/10.1016/b978-0-12-404060-1.50045-9
Pilkey, O. H., Rice, T. M., & Neal, W. J. (2014). How to read a North Carolina beach: Bubble holes, Barking sands, and rippled Runnels. UNC Press Books.
Riggs, S. R., Ames, D. V., & Dawkins, K. R. (2008). Coastal processes and conflicts: North Carolina’s Outer Banks: A curriculum for middle and high school students (NCU-E-08-002). NOAA Oceanic and Atmospheric Research; Sea Grant. https://repository.library.noaa.gov/view/noaa/46454/noaa_46454_DS1.pdf
Rimmer, J., Blight, A., Chocholek, M., & Paterson, D. (2025). Response of natural estuarine Microphytobenthic Biofilms to multiple anthropogenic stressors. Environmental Pollution, 387(127285). https://doi.org/10.1016/j.envpol.2025.127285
In the last few weeks, the water along the edges of Onslow County has felt different.
Not because the water itself has changed—but because something beneath it has become harder to ignore.
Schools of cownose ray (Rhinoptera bonasus) move just below the surface nearshore, their wingbeats lifting faint clouds from the bottom as they pass. In the soundside shallows, where the water thins over sand and mud, Atlantic stingray (Hypanus sabinus) settle into the substrate, half-buried and nearly invisible until a step comes too close and the outline breaks.
People are seeing them more often now—but they’re also reacting to them.
A pause mid-step in shallow water. A quick shift backward when something moves. Fishermen lifting a line and stopping for a second longer than usual—not what they expected to find.
There is awe in it.
And sometimes hesitation.
Because the same thing that makes them easy to notice now also makes them easy to miss.
The question follows quickly:
Are there more of them this year?
Maybe.
But that question lingers longer than the answer.
Cownose rays migrating in Swansboro, NC. | Image credit: Pogie’s Academy
What Brings Them Here
As spring settles in along the North Carolina coast, the system begins to reorganize.
Water temperatures rise, and with that rise comes a shift in metabolism. Rays—like many coastal species—become more active as conditions move into a narrower range that supports feeding and movement (Smith & Merriner, 1987; Schwartz & Dahlberg, 1978).
For cownose rays, this seasonal transition includes a northward migration along the Atlantic coast, bringing large groups into nearshore and estuarine waters (Smith & Merriner, 1987).
Large groups of cownose rays like these move north along our coast each season, arriving together in shallow water. | Image credit: Vidyacharan A. Alchi
But movement alone does not explain what people are seeing.
What matters is where that movement meets the structure of the environment.
The water does not always look the same—some days it is flat and clear enough to see straight to the bottom, and other days the slightest movement turns it cloudy, changing what can be seen and what remains hidden (Peterson et al., 2001).
And beneath all of it is food.
Cownose rays move through the shallows, sweeping across the bottom and disrupting what lies beneath them, crushing clams, oysters, and other shelled invertebrates with broad, flattened tooth plates (Collins et al., 2007; Fisher, 2010).
Atlantic stingrays hold low against the bottom, burying into the sand as they feed and working within the sediment itself—not moving across it—uncovering and drawing in small invertebrates hidden below (Snelson et al., 1988; Schwartz & Dahlberg, 1978).
Atlantic stingrays hold close to the bottom, often blending in until something shifts and gives them away. | Image credit: Andy Murch
Where prey is accessible, rays follow.
Where prey is concentrated in shallow, warming water, rays do not just pass through—they stay, turn, feed, and linger.
And in doing so, they cross into the same narrow band of space where people enter the water (Bangley et al., 2018).
They are not simply “here more.”
They are here in ways—and in places—that make them visible.
What Happens When They Feed
When a ray feeds, the bottom does not remain the same.
A cownose ray moving across a flat is not just searching—it is actively restructuring the surface beneath it. As it passes, the bottom is turned over behind it, patches of sand and mud disturbed where clams and other buried life have just been uncovered and crushed (Peterson et al., 2001; Smith & Merriner, 1985).
Feeding pits left behind by rays. Easy to mistake for crab holes at first—until you start to recognize the pattern and what’s actually shaping the bottom. | Image credit: Giaroli et al., 2024
Atlantic stingrays leave a different kind of trace. Where they settle, the surface shifts more subtly—small depressions, softened patches, places where the sediment has been worked rather than overturned, as buried invertebrates are uncovered and drawn in (Snelson et al., 1988; Schwartz & Dahlberg, 1978).
This is bioturbation—the bottom being reworked by the animals moving through it and within it (Thrush & Dayton, 2002).
As they feed, the bottom lifts into the water—fine particles rising and hanging there, turning clear water slightly cloudy (Thrush & Dayton, 2002).
Oysters and clams quietly filter the water as they feed, and when their numbers shift—even in small areas—the water and everything moving through it begins to change with them (Newell, 2004; zu Ermgassen et al., 2013).
In places where rays have been feeding, those filtering communities can be reduced or redistributed (Peterson et al., 2001).
Not removed entirely—but changed.
And that change does not stay in one place.
It moves outward, carried in the way the water looks, the way it settles, and what it can hold.
Layers of the Food Web
Rays do not sit at the top of the system, and they are not at the bottom of it.
As mesopredators, they feed on what is buried in the sediment, but they are also available to what moves through the water above. That position—between—links parts of the system that do not often meet directly (Myers et al., 2007; Heithaus et al., 2008).
What they do in that space matters.
As cownose rays move through andAtlantic stingrays work within the bottom, they are not just feeding—they are shaping what persists there. Clams, oysters, and other invertebrates do not simply accumulate unchecked. Their numbers are reduced, redistributed, and in some places kept from becoming dominant (Peterson et al., 2001).
Movement like this doesn’t stay in one place for long.
That pressure shapes the bottom itself.
Bivalves filter the water. Invertebrates stabilize sediment. When their abundance shifts, the system responds—sometimes toward clearer water, sometimes toward more suspended material, depending on what remains and where (Newell, 2004; zu Ermgassen et al., 2013).
Rays do not create those conditions alone—but they influence which direction the system moves.
At the same time, they carry that energy upward.
Juvenile sharks moving through these shallow waters encounter not just prey, but a system already in motion—areas where the bottom has been disturbed, where feeding has recently occurred, where something has been uncovered or displaced (Bangley et al., 2018).
And in some cases, the rays themselves become part of that exchange.
This is what it means to sit in the middle.
Not just connecting layers—but regulating how energy and movement pass between them.
If that middle shifts, the balance does not disappear.
It changes direction.
Why It Feels Sudden
There is a moment, standing in shallow water, when the bottom stops feeling like something you can trust.
What looked like sand shifts. What felt still is no longer still.
Sometimes you notice it in time—a shape lifting away, a shadow moving just beneath the surface. A plume of fine sediment rising to the surface under a paddleboard with a trail following it.
The moment when the bottom stops looking empty. | Image credit: iStock
Sometimes you don’t.
A step comes down where something is already settled. Hidden in the sand. Working within it.
The reaction is immediate. Surprise first. Then pain. Then the realization of what was there all along.
But what you are stepping into is not a single event.
It is a convergence.
Water temperatures have risen, bringing rays into the shallows as they feed and move through these systems (Smith & Merriner, 1987; Schwartz & Dahlberg, 1978).
Tides narrow the space, concentrating movement into a thinner band of water.
The bottom has already been worked—turned by cownose rays moving through, disturbed by Atlantic stingrays holding within it.
And at the same time, people have returned to the water.
For a brief window, all of it overlaps.
Not more. But more visible.
It feels sudden because you are standing at the point where all of these things meet.
And for a moment, the system lets you see it.
References
Bangley, C. W., Paramore, L., Dedman, S., & Rulifson, R. A. (2018). Delineation and mapping of coastal shark habitat within a shallow lagoonal Estuary. PLOS ONE, 13(4), e0195221. https://doi.org/10.1371/journal.pone.0195221
Giaroli, M. L., Byrne, I., Gilby, B. L., Taylor, M., Chargulaf, C. A., & Tibbetts, I. R. (2024). The distribution and significance of stingray feeding pits in Quandamooka (Moreton Bay), Australia. Marine and Freshwater Research, 75(18). https://doi.org/10.1071/mf23247
Heithaus, M. R., Frid, A., Wirsing, A. J., & Worm, B. (2008). Predicting ecological consequences of marine top predator declines. Trends in Ecology & Evolution, 23(4), 202-210. https://doi.org/10.1016/j.tree.2008.01.003
Kolmann, M. A., Huber, D. R., Motta, P. J., & Grubbs, R. D. (2015). Feeding biomechanics of the cownose ray, Rhinoptera bonasus, over ontogeny. Journal of Anatomy, 227(3), 341-351. https://onlinelibrary.wiley.com/doi/full/10.1111/joa.12342
Myers, R. A., Baum, J. K., Shepherd, T. D., Powers, S. P., & Peterson, C. H. (2007). Cascading effects of the loss of APEX predatory sharks from a coastal ocean. Science, 315(5820), 1846-1850. https://doi.org/10.1126/science.1138657
Newell, R. I. (2004). Ecosystem influences of natural and cultivated populations of suspension-feeding bivalve molluscs: A review. 23(1), 51–61. Journal of Shellfish Research, 23(1), 51-61. https://go.gale.com/ps/i.do?id=GALE%7CA118543914
Peterson, C. H., Fodrie, J. F., Summerson, H. C., & Powers, S. P. (2001). Site-specific and density-dependent extinction of prey by schooling rays: generation of a population sink in top-quality habitat for bay scallops. Oecologia, 129, 349-356. https://link.springer.com/article/10.1007/s004420100742
Schwartz, F. J., & Dahlberg, M. D. (1978). Biology and ecology of the Atlantic Stingray, Dasyatis Sabina (Pisces: Dasyatidae) in North Carolina and Georgia. Northeast Gulf Science, 2(1). https://doi.org/10.18785/negs.0201.01
Smith, J. W., & Merriner, J. V. (1985). Food habits and feeding behavior of the Cownose ray, Rhinoptera bonasus, in lower Chesapeake Bay. Estuaries, 8(3), 305. https://doi.org/10.2307/1351491
Smith, J. W., & Merriner, J. V. (1987). Age and growth, movements and distribution of the Cownose ray, Rhinoptera bonasus, in Chesapeake Bay. Estuaries, 10(2), 153. https://doi.org/10.2307/1352180
Snelson, F. F., Williams-Hooper, S. E., & Schmid, T. H. (1988). Reproduction and ecology of the Atlantic Stingray, Dasyatis Sabina, in Florida coastal lagoons. Copeia, 1988(3), 729. https://doi.org/10.2307/1445395
Thrush, S. F., & Dayton, P. K. (2002). Disturbance to marine benthic habitats by trawling and dredging: Implications for marine biodiversity. Annual Review of Ecology and Systematics, 33(1), 449-473. https://doi.org/10.1146/annurev.ecolsys.33.010802.150515
Zu Ermgassen, P. S., Spalding, M. D., Blake, B., Coen, L. D., Dumbauld, B., Geiger, S., Grabowski, J. H., Grizzle, R., Luckenbach, M., McGraw, K., Rodney, W., Ruesink, J. L., Powers, S. P., & Brumbaugh, R. (2012). Historical ecology with real numbers: Past and present extent and biomass of an imperilled estuarine habitat. Proceedings of the Royal Society B: Biological Sciences, 279(1742), 3393-3400. https://doi.org/10.1098/rspb.2012.0313
There are mornings along the edges of the water in Onslow County when the surface looks still enough to trust.
The marsh grass has not yet reached its summer height. What stands there leaves more water exposed between the stems, and without sustained wind, the surface holds its shape. You can see farther into it now than you will in a few weeks, before suspended sediment and constant movement return it to opacity. The water carries less of the season, and because of that, more of what moves beneath it becomes visible—if you are willing to wait long enough to see the difference between movement and reflection.
This is when people begin to notice them again.
Not all at once. Not everywhere. Just a change that does not follow wind or tide. A line that holds where the rest of the surface releases. Something that holds its position in a system that is always adjusting.
An alligator does not arrive in that moment.
It becomes visible.
Alligator emerging from the mud. | Photo credit: Gilbert Grant, iNaturalist
Seasonal Absence Is Not Absence
Through winter, they remain within these same creeks, marsh edges, and quieter channels. What changes is not location, but how they occupy it. As temperatures fall, activity narrows. Movement slows, and the need for it slows with it. Energy is conserved, not spent. And the surface carries fewer signs of what lies beneath it. Individuals hold in deeper water or along softer margins where mud retains heat longer than the surrounding water column, remaining within conditions that allow them to persist without constant movement (Nifong et al., 2014; Rosenblatt & Heithaus, 2011).
The same stretch of water that in spring will hold a visible form can pass through winter without interruption, its stillness mistaken for absence.
But the system does not empty.
It compresses.
The System Wakes in Layers
By early spring, that compression begins to release—not all at once, but in layers that build on each other before they are recognized. Shallow water warms first, taking in solar heat more quickly than deeper channels. Along these edges, fish begin to hold longer. Movements that in winter passed through quickly begin to extend into areas that had remained quiet. Invertebrates return to the sediment surface, and the water column begins to carry more suspended life, even before it becomes visible as turbidity.
Birds respond to this before most other changes are noticed. Their movements tighten. Landings become more frequent, departures more abrupt. What they are tracking is not random. It is the redistribution of energy into places where it can be accessed.
The alligator moves within that shift.
Not as a trigger. Not as something layered on top. But as part of a system reorganizing itself across temperature, light, and movement at the same time.
Great blue heron and alligator are part of an interconnected system. | Photo credit: Audubon North Carolina
Reading What It Is Responding To
When one becomes visible along the edge of a creek or marsh, it is easy to reduce that moment to temperature alone. Warmer water allows for more activity.
But what draws it into that position is more specific than warmth.
It is the arrangement of prey.
Along the margins where water meets land, movement compresses. Fish traveling with the tide encounter shallow gradients that limit how long they can remain. Small mammals moving between marsh and upland must cross exposed edges. Birds landing to feed do so in places where depth and access align for only short intervals.
These are not isolated events. They are recurring patterns shaped by tidal cycles, substrate, and seasonal change.
The alligator positions itself within those patterns.
Its diet reflects that flexibility, spanning invertebrates, fish, birds, reptiles, and mammals depending on size and availability (Nifong, 2016). But the diet alone does not explain its placement. What matters is where energy becomes concentrated, even briefly.
That concentration is not constant. It forms and dissolves with tide, with light, with movement.
And the predator tracks that.
And what appears as a single movement—a fish turning, a bird lifting, something crossing the edge of the marsh—is part of a larger structure that holds only briefly before dissolving again.
The alligator does not respond to the individual movement.
It responds to the pattern that produces it.
Where Freshwater Meets Salt
These are not just places where water mixes.
They are places where movement is forced—and where that movement becomes available to something waiting at the top of it.
There are places along this coastline where those changes concentrate.
At the mouths of creeks, along the edges of the Intracoastal Waterway, and near the shifting bars of New River Inlet, the water does not settle into a single condition. Freshwater moves outward with tide and rainfall, meeting saltwater pressing back in with tidal exchange. The result is not a fixed boundary, but a gradient that shifts continuously—sometimes visible as a faint line, sometimes only detectable in how the surface moves differently from one side to the other.
This is where alligators are most often encountered—because this is where the system compresses into something they can use.
They are not marine animals. They do not possess the specialized salt glands that allow for extended life in high salinity environments. Over time, saltwater carries a physiological cost, requiring a return to freshwater to restore balance (Rosenblatt & Heithaus, 2011; Fujisaki et al., 2014).
But that limitation does not exclude them.
It defines how they move through them.
In these mixing zones, salinity is not constant. It rises and falls with tide, with rainfall, with wind direction. A location that carries higher salinity at one stage may shift toward fresher conditions hours later. What appears to be a boundary is, in practice, a moving field.
Within that field, movement compresses.
Fish traveling with the tide are funneled into narrower pathways. Shallow gradients limit how long they can remain in deeper water. Schools tighten. Individuals encounter edges that restrict escape. The system concentrates energy into space.
The predator does not need to range widely in these conditions.
It needs to hold where movement is forced.
And so it does.
An alligator near the tall grass near Marine Corps Air Station New River | Photo credit: Martin Egnash
At the Edge of the Open Water
There are moments when that pattern extends beyond the mixing zones, into places that appear, at first, outside of where an alligator belongs.
Along the shoreline, in the breaking waves where the ocean meets sand, one will sometimes appear—rising and falling with the swell, holding position just beyond where the water turns over onto the beach. It looks misplaced, as though it has moved beyond the system that defines it.
It has not.
The surf zone is one of the most compressed environments along the coast. Waves reduce depth, disrupt orientation, and concentrate movement into a narrow band where escape is limited. Fish pushed into breaking water lose some ability to maintain direction. Schools fragment. Individuals become briefly exposed in ways that do not occur in deeper, more stable water.
For a predator capable of stillness followed by short bursts of movement, that compression creates opportunity.
But the cost is higher.
Salinity is elevated. The water is in constant motion. There is no stable refuge within immediate reach. Time in this environment cannot be extended indefinitely.
And so it does not.
Movements into higher salinity water tend to be brief—extensions outward, followed by a return to freshwater or lower salinity conditions where balance can be restored (Nifong et al., 2014).
What appears as an anomaly is part of a larger pattern.
The predator crosses the boundary not to remain, but to use it, moving where the system briefly offers more than it costs.
The same forces that shape the marsh edge—compression, constraint, and brief exposure—are recreated here, just for a moment, in a different place.
An alligator rests at the ocean’s edge in North Topsail. | Photo credit: Fox8 Digital Desk
What Its Presence Changes
Most of what that presence changes cannot be seen when it is observed.
Long before any direct interaction occurs, it is already altering how other organisms use space.
Fish moving along the edge do not simply pass through. They adjust their depth, their speed, the amount of time they remain exposed. Birds land with shorter intervals between contact and departure. Mammals approaching the water shift their paths or their timing. These changes are not dramatic in isolation. But they are continuous.
Over time, they accumulate into structure—the kind that determines who feeds, where they feed, and how long they remain.
The influence of a predator at this level extends beyond what it consumes. It shapes behavior across multiple species, redistributing where and how energy moves through the system. The possibility of predation—present even when not observed—alters interactions in ways that regulate access to habitat and resources (Heithaus et al., 2008; Ripple et al., 2014; Estes et al., 2011).
What holds the system in place is not removal alone.
It is pressure.
What is being shaped is not just movement, but access—and access is what determines how energy moves through the system.
More Than Predation
The influence of the alligator does not end with what it hunts, but extends beyond those interactions.
As it moves through shallow systems, it disturbs sediment, creating depressions and pathways that alter how water is retained and how nutrients are redistributed. These small changes in physical structure create conditions that other species use—temporary refuges, feeding areas, and zones where organic material accumulates (Eversole et al., 2018; Subalusky et al., 2009).
In wetland systems, these disturbances have been linked to broader effects, including nutrient cycling and carbon storage, where the presence of large predators contributes to the retention of organic material within the system rather than its export (Murray et al., 2025; Atwood et al., 2015).
These processes do not occur in isolation.
They intersect with the same patterns of movement, feeding, and behavior that define the system at larger scales.
Seeing the Surface, Reading the System
When one becomes visible along the surface, it is easy to treat the moment as singular.
A sighting. An encounter. Something separate from everything around it.
But that form at the surface is supported by layers extending beyond what can be seen.
It reflects water temperatures crossing into ranges that support sustained activity. It reflects prey moving into positions where access becomes possible. It reflects a system where behavior is still shaped by the presence of something at the top.
The alligator is not an interruption to that system.
It is an expression of it.
What Becomes Visible
Seeing one does not indicate that something has entered the water.
It indicates that enough beneath the surface is functioning to hold it.
Not in a static sense. Not as balance in the way it is often described. But as a set of interactions that remain connected—movement, response, pressure—each shaping the others even when they are not directly observed.
What becomes visible at the surface is only a fraction of that structure.
But it is enough to know that the rest is still in place.
An alligator in Onslow County sits at the edge of the saltmarsh. |Photo credit: Gilbert Grant, iNaturalist
When That Pressure Is Reduced
If that pressure is reduced, the system does not leave an obvious gap.
It shifts.
Movements that were once constrained begin to extend. Species that passed quickly through exposed areas begin to remain longer. Edges that functioned as transition zones become used differently—not because the physical environment has changed, but because the conditions that shaped behavior within it have relaxed.
Mid-level predators expand their activity under these conditions, increasing their access to prey and space when not constrained from above (Nifong et al., 2013).
The change is subtle.
It appears in how long something stays. In how often it returns. In where it lingers. In how quietly the structure of behavior begins to loosen.
The food web and trophic cascade of the American alligator in the Florida Everglades.
A System Written Into Temperature
There is another layer to this that does not show itself at the surface.
The structure of that presence is set years earlier, in a place that can be overlooked when standing at the water’s edge. Along the margins of marsh and wetland, slightly above the reach of regular water movement, nests are built from vegetation and sediment, forming mounds that hold heat as they decompose.
Within those mounds, temperature determines something that will not be visible for much later.
Sex is not fixed at fertilization. It emerges during incubation, shaped by the thermal conditions held within the nest. A difference of only a few degrees is enough to shift the outcome, producing more males or more females depending on where within that range the nest remains (Lang & Andrews, 1994; Janzen, 1994).
Under variable conditions—differences in shading, rainfall, timing, and placement—those outcomes are distributed across the landscape. Some nests produce more females, others more males. That variability holds the population in a form that can sustain itself over time.
When conditions become more consistent, that variation narrows.
Warmer nights hold heat longer within the nest. Seasonal transitions extend. The range of outcomes compresses. What was once distributed begins to align.
And that alignment carries forward into the structure of the population—into how individuals occupy space, into how pressure is applied across the system, into what will eventually be visible at the surface.
Alligator eggs hatch after 65 days of incubation in the fall. The babies will chirp to alert their mom, who then digs out the nest while the babies use their egg tooth to hatch from their eggs. Their mom will then safely carry them to the water.
Where the Next Generation Is Set
The placement of those nests depends on something even more constrained.
A narrow band of land that remains above water just long enough to hold them.
That band is not fixed.
It shifts with tide, with rainfall, with the gradual reworking of shoreline that occurs across seasons and years. With rising sea levels, water reaches farther into areas that once remained above it. Flooding becomes more frequent, not always through singular events, but through repeated intrusions that saturate and destabilize what had previously held (Joanen & McNease, 1989; Sweet et al., 2022).
Human alteration compresses this space further.
Hardened shorelines, dredging, and development reduce the gradual transition between land and water. Where there was once a slope capable of holding multiple elevations, there becomes a defined edge. That edge does not provide the same range of conditions required for successful nesting.
The number of suitable sites decreases.
More importantly, the variability between them narrows.
And with that, the system loses one of the mechanisms that allowed it to absorb change.
Alligator on her nest that can hold up to 60 eggs. | Photo credit: National Park Service (NPS)
What Its Presence Means
When an alligator becomes visible along the surface, it reflects conditions that have aligned across multiple layers.
Temperature has reached a range that supports activity. Prey has moved into positions where access becomes possible. Behavioral pressure remains in place across the system. Reproduction has held across enough years, in enough suitable places, to sustain what is now present.
What is seen at the surface is not separate from them.
It is supported by them.
Seeing one does not signal that something has entered the water.
It signals that enough of what lies beneath it—movement, pressure, response, and continuity—remains intact.
And that—even when most of it is not visible—the system is still holding together.
And that is what becomes visible—just long enough to be seen, before the system closes back over it again.
The system does not end at the water’s edge.
Epilogue: Chicken Nugget
We came across him along the New River, near the courthouse in Jacksonville.
We were there to clear what had been left behind—fishing line caught along the walkways, hooks, and the overflow from a trash can that had spilled out onto the edge. Fast food containers, grocery store chicken trays, scattered along the bank. The signs were clear enough. People had been there for a while—crabbing, fishing, eating, leaving what remained.
He was directly below us.
Small enough to miss at first. Still enough to blend into the water until you stopped looking for movement and started noticing what held its position.
A juvenile alligator, watching.
He stayed there while we worked, then slipped beneath the surface and crossed the small bay. On the opposite side, someone tossed a piece of food into the water. He surfaced almost immediately, took it, and remained.
Waiting.
I came back later and stayed longer.
The pattern repeated. He would disappear until footsteps approached, then return to the same place along the edge. Holding position. Watching. Waiting for something to fall.
No fishermen or crabbers passed through while I was there, but the behavior was consistent with what happens when food becomes predictable. Bait, catch, scraps—anything that can be taken without the cost of searching or pursuing.
Energy, without effort.
It is easy to see something like that and respond to what it looks like in that moment. A small animal. Still. Attentive. Something that feels close enough to interact with.
But what is being shaped there is not just a single interaction.
It is behavior.
A shift away from the conditions that formed it—toward something more efficient, more immediate, and less stable over time. The system that once required movement, patience, and response begins to narrow into expectation.
And expectation changes how an animal uses space.
What happens when that animal is no longer small is not a separate question.
It is the continuation of the same pattern.
Alligators do not forget where food has been easy to obtain. They return to it. They hold in those places. They begin to associate presence—human presence—with opportunity.
What begins as something that feels harmless becomes something that alters how the system functions around it.
Not just for the animal, but for everything that responds to it.
There are instincts at work here that were shaped long before any walkway, any dock, any place where food might be dropped from above. Those instincts are not just about survival in isolation. They are part of how pressure is applied, how movement is shaped, how the system holds.
When those instincts are replaced with something easier, the effect does not remain contained.
It carries outward.
He stayed there while I watched. Returning to the same place. Holding the same position. Waiting for something to fall.
There is a kind of kindness in wanting to give something to an animal like that.
But there is another kind in leaving it as it is.
Not interrupting the conditions that shape it. Not narrowing what it has learned to expect. Not replacing a system built on movement and response with one built on waiting.
Let it remember the water as it is.
And you, only as something that passed through it.
We affectionately named this juvenile alligator in the New River in Jacksonville, NC “Chicken Nugget” for all of the chicken nugget boxes left behind on the walkway from an overflowing trash can. | Photo credit: A. Mitchell
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