Crown-of-thorns outbreaks are not a new phenomenon. Four major outbreaks have swept the Great Barrier Reef since the 1960s, and rising densities detected near Lizard Island suggest a fifth is now underway. What drives these population explosions has long divided researchers, with three broad hypotheses on the table: bottom-up boosts in larval food supply, top-down release from predation on juveniles and adults, and natural population fluctuations. None of these mechanisms is mutually exclusive, but the new study, led by Frances Patel of the Australian Institute of Marine Science together with colleagues at the University of Otago, homes in on the first of them with unusual precision—asking not just whether food matters, but when and for how long.

The researchers conducted five experiments in total, using separate larval cohorts spawned from broodstock collected from mid-shelf reefs near Townsville between 2022 and 2025. All rearing was performed at the National Sea Simulator in Townsville in an automated flow-through feeding system that held food concentrations at tightly controlled levels, a marked improvement over daily manual feeding setups used in most previous crown-of-thorns larval studies. Larvae were fed mixtures of the algae Dunaliella sp. and Tisochrysis lutea at either satiating high food levels—0.6 to 1.7 micrograms of chlorophyll a per litre, corresponding to 2,205 to 3,405 algal cells per millilitre—or limiting low food levels of 0.12 to 0.44 micrograms chlorophyll a per litre. Crucially, these concentrations mirror real conditions: the high food levels match those measured on mid-shelf reefs after nutrient pulses from upwelling or river runoff, while the low levels resemble typical surface waters on the Great Barrier Reef outside flood events.

The first set of experiments tested a long-standing but unverified idea: that crown-of-thorns larvae might harbor photosynthetic microbial symbionts capable of supplementing their nutrition through light-driven metabolite transfer. Such associations have been documented in coral larvae and in larvae of the tropical sea star Mithrodia clavigera, and a microbial study had suggested that crown-of-thorns larvae contain bacteria potentially capable of photosynthesis. If true, light could act as a nutritional lifeline for larvae drifting through the food-poor waters that characterize much of the reef. The result was emphatically negative. Larvae raised under a 12-hour light and 12-hour dark cycle performed no better—or worse—than larvae raised in complete darkness, at both food levels. Food concentration alone drove development: 57 to 62 percent of high-food larvae had reached the brachiolaria stage by day seven, compared with just 5 to 9 percent under low food, and by day fifteen roughly 80 percent of high-food larvae had progressed to mid or late brachiolaria versus about 1 percent of low-food larvae. Settlement success under high food reached 46 to 50 percent, with no influence of light, while no larvae settled at all under low food conditions.

The second set of experiments manipulated the timing of food availability. Larvae were switched between high and low food regimes five days after the onset of feeding, at seven days post-fertilisation. Larvae given high food early and then switched to low food still developed far better than larvae given low food early and then switched to high food. By day eleven, 88 percent of larvae kept on constant high food had reached mid to late brachiolaria stages, compared with 67 percent of the high-to-low group, 26 percent of the low-to-high group, and only 1 percent of larvae on constant low food. This asymmetry reveals a striking developmental plasticity with a clear message: food encountered early in larval life matters far more than food delivered later. Larvae that started well partially recovered when conditions improved, but they never caught up with siblings that had a strong start.

The third experiment delivered the study’s most consequential result by quantifying exactly how many days of high food are needed. Larvae exposed to one to three days of high food showed modest benefits, with 17 to 37 percent reaching advanced stages. But at four days of high food—a threshold response—more than 70 percent of larvae reached mid to late brachiolaria, essentially matching larvae raised on high food for the entire nine-day experiment. Settlement, however, required a slightly longer window: fewer than 1 percent of larvae exposed to only one or two days of high food settled, around 6 percent settled after three to four days, and 34 to 69 percent settled after five to nine days of high food exposure. In other words, a bloom lasting roughly four to five days at the start of the larval phase is sufficient to push most larvae onto a fast developmental track and to lift settlement rates to levels comparable with permanent abundance.

The physiological logic behind this sensitivity lies in the energetics of early development. Crown-of-thorns larvae at about two days old develop a functional gut and begin feeding, but maternal resources in the egg are depleted by the late bipinnaria stage. Marine invertebrate larvae carry lipids as their dominant energy reserve, yet accumulating carbohydrates during the bipinnaria stages may fuel the protein-rich brachiolaria phase and metamorphosis that follow. Previous work on related sea stars has shown that well-fed larvae establish higher carbohydrate concentrations during early development, and that later starvation does not necessarily compromise settlement if early nutrition was adequate. The authors suggest two possible outcomes from the pulse-feeding experiments: larvae that received high food in their first five days accumulated sufficient energy reserves to fuel complete development regardless of later nutrition, while larvae that started on low food accrued inadequate reserves that later abundance could not repay.

These results mesh tightly with what is known about phytoplankton dynamics on the Great Barrier Reef during the seastar’s spawning season. Intense rainfall events push nutrients into coastal waters through river runoff, while intrusions of nutrient-rich upwelled water fertilize deeper layers where larvae have recently been found at depths of up to 30 metres. Phytoplankton can double in abundance one to two times per day, allowing blooms to develop rapidly and persist for days to weeks. One recorded bloom lasting five days reached the reef corridor between Cairns and Lizard Island—the so-called outbreak initiation zone. That duration sits squarely within the four-to-five-day window the new experiments identify as sufficient to dramatically boost larval development, suggesting that even a single episodic bloom coinciding with spawning could amplify the number of larvae surviving to settlement.

The study also carries implications for how reef managers think about water quality. Nutrient enrichment from catchment runoff has long been suspected of feeding crown-of-thorns outbreaks, but the mechanistic link has been difficult to demonstrate because larvae are notoriously hard to sample in the wild. By showing that the critical nutritional window is narrow, early, and quantitatively defined, the research makes the bottom-up hypothesis testable against environmental monitoring data: blooms of sufficient concentration and duration overlapping the spawning season become a concrete, observable trigger to look for. Shorter larval development times may also increase larval retention near source reefs, a process previously proposed to contribute to primary outbreak initiation.

Important caveats remain. Laboratory settlement rates cannot be translated directly into recruitment success, because newly settled juveniles face heavy predation and other mortality in the field, and nutritional carryover effects into the juvenile stage may not be visible at settlement. The light experiments were also conducted under aquarium conditions that may lack the diverse natural microbial communities needed to establish photosynthetic symbionts, so the authors caution that the symbiont question warrants further study with larvae from natural environments. Still, the core conclusion stands: light does not rescue food-limited larvae, but a brief, well-timed pulse of phytoplankton abundance can transform larval fortunes. In the seasonal rhythm of the Great Barrier Reef, where floods and upwelling punctuate an otherwise nutrient-poor sea, those transient windows of plenty may be precisely what turns an ordinary spawning season into the beginning of an outbreak.

Subject of Research: Effects of light and short-term phytoplankton food pulses on larval development and settlement of the coral-eating crown-of-thorns seastar (Acanthaster cf. solaris)

Article Title: Does light and short-term high food availability enhance larval success in the coral eating crown-of-thorns seastar (Acanthaster cf. solaris)?

Article References: Patel, F., McDowell, E., Bastin, L., Gomez Cabrera, M., Lamare, M., & Uthicke, S. (2026). Does light and short-term high food availability enhance larval success in the coral eating crown-of-thorns seastar (Acanthaster cf. solaris)?. Coral Reefs. https://doi.org/10.1007/s00338-026-02962-4

Image Credits: AI Generated

DOI: 10.1007/s00338-026-02962-4

Keywords: crown-of-thorns seastar, Acanthaster cf. solaris, Great Barrier Reef, phytoplankton blooms, larval development, larval settlement, nutrient enrichment, upwelling, river runoff, coral reef decline, population outbreaks, developmental plasticity

The researchers set out to answer a deceptively simple question. Where does the nitrogen that is increasingly loading the waters of the northern Gulf of Mexico actually come from? Elevated nutrient levels have been linked to coral bleaching and disease, but tracing those nutrients to their source is notoriously difficult in open ocean environments. The team’s solution was to turn the corals themselves into witnesses, reading the chemical records locked inside their skeletons decade by decade, stretching all the way back to the middle of the eighteenth century.

Stony corals such as the star corals sampled in this study grow slowly but continuously, laying down their calcareous skeletons in layered bands much like the annual rings of a tree. Because the corals of the Flower Garden Banks can live for centuries, their skeletons preserve a continuous environmental archive. The researchers analyzed core samples collected during an expedition by the U.S. National Oceanic and Atmospheric Administration, extracting nitrogen isotope data spanning the years 1753 to 2023. The key lies in the ratio of the heavy isotope nitrogen-15 to the lighter nitrogen-14, a chemical fingerprint that carries information about where the nutrients consumed by the coral originally came from and, by extension, about the history of the water in which the coral grew.

The isotope record tells a striking story of human transformation. From 1753 to roughly 1850, the nitrogen isotope values in the coral skeletons looked exactly like what would be expected in a largely natural environment, with little to no detectable input of river-borne nitrogen. After about 1850, however, the signal begins to shift, recording a growing contribution of nitrogen from human activities. The timing is not random. It coincides with European settlement and agricultural expansion across the Mississippi River region, including the increasing use of organic fertilizers. One particularly vivid marker is a rise in guano-derived nitrogen beginning in 1856, the very year the U.S. Congress authorized guano mining on Pacific and Caribbean islands, opening the door to a new era of fertilizer chemistry.

The precision with which historical events appear in the coral record surprised even the researchers. In the areas where they detected significant changes in the nitrogen signal, they examined what was happening around the Mississippi River basin during those periods, and the correspondence proved remarkable. The signal intensified again after the removal of the so-called Second Great Raft in the mid-1870s, a massive, naturally formed log jam in the Red River, a tributary of the Mississippi. Clearing the raft reduced inland flooding, but it also increased the flow velocity of the Mississippi and its Atchafalaya branch, accelerating the delivery of nutrients to coastal waters. Then, beginning in 1882, the construction of levees along the river to contain floodwaters meant that river water, along with its sediments and dissolved nutrients, flushed ever more directly into the Gulf.

The most dramatic transformation arrived with the Green Revolution of the 1960s, when synthetic fertilizers became widely available and agricultural production across the American heartland intensified. The concentration of anthropogenic nitrogen recorded in the coral skeletons rose sharply and has continued climbing ever since. By the end of the twentieth century, nitrogen washing in from the Mississippi basin accounted for 30 to 50 percent of the total reaching the Flower Garden Banks. In the last decade, that share exceeded 60 percent, and in 2023 it reached a staggering 80 percent. The researchers conclude that the Mississippi River is now the primary source of nutrients in the northern Gulf of Mexico, delivering fertilizer-derived nitrogen to reef ecosystems located 448 kilometers, or 278 miles, from the river’s mouth. The scale of this connection is extraordinary when one considers that the Mississippi basin today drains roughly 41 percent of the land area of the continental United States, stretching from Idaho in the west, through Canada in the north, to New York in the east.

What makes these findings urgent is the way the nitrogen record aligns with the recent deterioration of the reefs. The study found that the highest nitrogen inputs occurred in 2016 and between 2022 and 2023. These were precisely the years in which the Flower Garden Banks suffered exceptional marine heat waves, experienced their first major coral bleaching events, and saw increased outbreaks of coral disease. For reefs that had shrugged off decades of environmental pressure, the combination proved devastating. According to the research team, the pairing of unprecedented nutrient loads with extreme heat is the decisive factor behind the recent decline in reef health at the sanctuary.

The underlying science explains why the two stressors are so damaging in combination. Excess nitrogen fuels the growth of algae and microbial communities on and around coral colonies, shifting the delicate balance of the reef ecosystem and making corals more vulnerable to pathogens. When marine heat waves push water temperatures past coral tolerance thresholds, the symbiotic algae that corals depend on for energy are expelled, causing bleaching. A nutrient-enriched, microbially active environment can turn a bleaching event into a mortality event, and it can accelerate the spread of disease through already stressed colonies. In other words, nitrogen pollution does not merely coexist with warming; it amplifies its consequences, undermining the resilience that had allowed the Flower Garden Banks to persist while reefs elsewhere collapsed.

The implications reach far beyond a single sanctuary. Because the Mississippi basin encompasses so much of the continent, nutrient management decisions made hundreds or even thousands of kilometers inland reverberate through Gulf waters. Fertilizer applied to corn and soybean fields in the Midwest, or to lawns and pastures across the basin, ultimately contributes to the nitrogen reaching the reefs. The researchers warn that disease outbreaks and bleaching events should be expected to increase as long as nitrogen pollution from the Mississippi watershed remains at its current high levels while ocean temperatures continue to rise. Reducing nutrient runoff, they suggest, is not just a water quality issue but a direct intervention for reef survival.

Beyond its warning, the study demonstrates the power of corals as environmental archives. By reading the chemical records preserved in their skeletons, scientists can reconstruct ocean conditions stretching back before industrialization, establishing natural baselines that resource managers can use to guide conservation decisions in the Gulf. As Kristine DeLong, professor at Louisiana State University and second author of the study, notes, the corals of the Flower Garden Banks are valuable archives of past ocean and environmental conditions, and there is much still to learn from them about the state of the oceans before human influence. Jonathan Jung, the study’s first author and a postdoctoral researcher at the Max Planck Institute for Chemistry in Mainz, emphasizes how precisely historical events are documented in the core samples. For a reef system that once seemed immune to the pressures reshaping coral ecosystems worldwide, the message written in its own skeleton is now unmistakable: without action on nutrient pollution, even the strongest reefs cannot withstand the heat that is coming.

The isotope approach used in the study offers a level of source attribution that conventional water sampling cannot match. Grab samples of seawater capture nutrient concentrations only at a single moment, and nitrogen from different origins mixes and transforms rapidly in the water column, erasing clues about where it came from. Coral skeletons, by contrast, integrate the isotopic signal over the entire lifespan of the colony, allowing researchers to distinguish river-derived nitrogen from other sources such as atmospheric deposition or nitrogen fixation by marine organisms across nearly three centuries of continuous record.

The findings also connect to a broader body of concern about nutrient enrichment in the Gulf of Mexico. Nitrogen carried by the Mississippi has long been implicated in the seasonal development of large low-oxygen zones along the Louisiana and Texas continental shelf, where algal blooms fueled by river nutrients sink and decompose, stripping oxygen from bottom waters. The new evidence that the same continental runoff reaches offshore reef ecosystems adds a previously underappreciated dimension to this well-documented coastal problem, extending its consequences to habitats once thought to lie beyond the river’s influence.

For the managers of the Flower Garden Banks National Marine Sanctuary, the study provides something rare: a quantified, time-resolved link between inland agricultural activity and offshore reef condition. Because the sanctuary sits far from the river’s plume, its waters were long assumed to be buffered from continental runoff. The isotope record demonstrates that mixing processes transport nitrogen-rich water across the intervening distance, meaning that upstream conservation measures, improved fertilizer efficiency, and nutrient reduction efforts within the vast basin could yield tangible benefits for reef health even at this remote location.

Subject of Research: Nitrogen isotope analysis of coral skeletons tracing Mississippi River fertilizer pollution and its impact on reef health in the Gulf of Mexico

Article Title: Fertilizers and Extreme heat are damaging coral reefs in the Gulf of Mexico

Article References: Fertilizers and Extreme heat are damaging coral reefs in the Gulf of Mexico. (n.d.). Original publication

Image Credits: AI Generated

DOI: Not provided

Keywords: coral reefs, Flower Garden Banks, Mississippi River, nitrogen isotopes, fertilizer runoff, coral bleaching, marine heat waves, Gulf of Mexico, Science Advances, paleoceanography, coral disease, nutrient pollution