Published in Nature Climate Change, the research analysed ESA's Climate Change Initiative records of sea surface temperature, ocean colour and sea ice extent, combined with pigment data from over 14,000 in-situ samples collected between 1997 and 2023. Machine learning models linked satellite and sample data to map phytoplankton group changes.
Results show a marked decline in diatoms across the Antarctic continental shelf until 2016, when sea ice retreat triggered both a diatom rebound and rapid cryptophyte growth. Haptophytes increased before 2017, while West Antarctica continued to see diatom declines after that year.
Diatoms, making up 46% of phytoplankton in the region, are more efficient than smaller nanoplankton such as haptophytes and cryptophytes at locking away carbon, as their silica shells sink with absorbed carbon. They are also the preferred food of krill, which sustain higher predators.
Satellites like Copernicus Sentinel-3 cannot directly detect phytoplankton types but measure subtle changes in ocean colour. These reflect chlorophyll and accessory pigments, which can be linked to species composition using in-situ pigment profiles.
ESA's new Phyto-CCI project will create global phytoplankton type records from space, improving monitoring of marine ecosystem health and the ocean's climate role. Lead author Alexander Hayward warned that fewer diatoms could weaken the biological carbon pump, reducing carbon transfer to the deep ocean.
Research Report:Antarctic phytoplankton communities restructure under shifting sea-ice regimes
As the world churns - a history of ecosystem engineering in the oceans
New Haven CT (SPX) Aug 15, 2025 -
The murky world at the bottom of the oceans is now a little clearer, thanks to a new study that tracks the evolution of marine sediment layers across hundreds of millions of years.
It is a story of world-building on a grand, yet granular, scale, accomplished by a succession of marine animals that burrowed and tunneled their way through heat and cold, species expansions and mass die-offs. Scientists call the process bioturbation - the excavation and mixing of sediments and soils by burrowing animals, particularly for shelter and sustenance.
"Bioturbation is one of the most important forms of ecosystem engineering today, both in the oceans and on land," said Lidya Tarhan, assistant professor of Earth and planetary sciences in Yale's Faculty of Arts and Sciences, and lead author of the study published in the journal Science Advances.
"In the oceans, bioturbation plays a critical role in shaping the habitability and ecology of the seafloor, as well as in regulating nutrient cycling in overlying ocean waters," Tarhan said. "However, how bioturbation has varied through Earth's past, and the evolutionary timing of when bioturbators became the enormously impactful 'engineers' they are today, has long been poorly understood."
In addition to their own data - which includes observations from geologic field work in the U.S., Canada, Spain, and Australia and sediment drill cores collected from the modern oceans - Tarhan and her collaborators surveyed more than 1,000 previous scientific studies. They looked specifically for information about how intensively seafloor sediments were churned, as well as six types of fossilized burrows that have typically been among the deepest burrows in the seafloor. Ultimately, they amassed a database covering 540 million years of Earth's history - nearly the full evolutionary history of animal life.
The team gleaned several new insights from their research.
First, they found that the two main types of bioturbation - burrowing and sediment mixing by the animals - developed separately. Deep burrowing began early in the evolution of animals; sediment mixing took hundreds of millions of years to develop.
"Burrowing animals such as worms, and later, clams and crustaceans were abundant and widespread, at least in the shallow oceans," said Tarhan, who is also an assistant curator at the Yale Peabody Museum. "It took longer for them to venture to the deep oceans. But sediment mixing lagged behind. We hypothesize that ocean oxygen stress, particularly in intervals of warm, 'greenhouse' climates, may have been a major driver."
Ocean oxygen levels were likely very low when seafloor animal communities were first establishing themselves, she said. Under warmer water temperatures, animals' metabolic rates increase and so does their need for oxygen. That likely meant that sediment mixing, which requires a great expenditure of energy, took a backseat to less-intensive burrowing.
The researchers also were able to begin documenting how bioturbation has been affected by major environmental changes and mass extinction events throughout history. For example, during the End-Permian mass extinction 252 million years ago, when potentially more than 90% of animal species were wiped out, bioturbation ceased for a time. Then small, horizontal burrows slowly began to reappear.
Further research will explore what role this greatly reduced bioturbation had on the reestablishment of nutrients in the ocean and the eventual regrowth of ecosystems.
"Without a clear picture of how bioturbators responded to environmental stressors and how quickly they were able to rebound following extinctions, our understanding of the mechanics of the ecological cascades that drive extinction and dictate recovery is decidedly murky," Tarhan said. "This certainly compounds the challenges we face in attempting to predict the ecological impacts of our current extinction crisis."
Research Report:Tracking bioturbation through time: The evolution of the marine sedimentary mixed and transition layers
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