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Climate Change Could Cause Devastating Mass Exodus of Tropical Plankton

A microscope image of a shelled plankton. According to research from The University of Texas at Austin, plankton populations like this flourished in the tropics during past global cooling and may vanish as the climate warms. Credit: Tracy Aze

The tropical oceans harbor the most varied plankton communities on our planet, which serve as the foundation of marine food webs. However, it may come as a surprise that the modern diversity of plankton in the tropics has only emerged recently, within the past 8 million years, due to global cooling. This was recently discovered in a recent study led by researchers at The University of Texas at Austin.

The discovery has sparked concerns about the potential impact of rapid ocean warming on plankton distribution, as they may be compelled to migrate away from the tropics, resulting in adverse consequences for marine ecosystems. This could have detrimental effects on key fish speciesA species is a group of living organisms that share a set of common characteristics and are able to breed and produce fertile offspring. The concept of a species is important in biology as it is used to classify and organize the diversity of life. There are different ways to define a species, but the most widely accepted one is the biological species concept, which defines a species as a group of organisms that can interbreed and produce viable offspring in nature. This definition is widely used in evolutionary biology and ecology to identify and classify living organisms.” data-gt-translate-attributes=”[{“attribute”:”data-cmtooltip”, “format”:”html”}]”>species like tuna and billfish, as well as on coastal communities that rely on them. The study was recently published in the journal Nature.

Using microfossils to track the history of a group of zooplankton called Foraminifera, the researchers found that the last time Earth was this warm – just before global cooling began 8 million years ago – tropical plankton populations lived in waters more than 2,000 miles from where they are today. The natural cooling of the past 8 million years that allowed the plankton to flourish in the tropics has been reversed by climate change during the past century.

The scientific drilling ship Joides Resolution near the Greek island of Santorini in 2023. Aboard was mission scientist Adam Woodhouse, a postdoctoral fellow at the University of Texas Institute for Geophysics. His studies of microfossils gathered on previous missions have revealed how the climate affects global plankton populations. Credit: Thomas Ronge

“Earth’s current biosphere evolved for ice ages,” said lead author Adam Woodhouse, a postdoctoral fellow at the University of Texas Institute for Geophysics. “By suddenly switching to an Earth of 8 million years ago, we’re not just killing off a few species, we’re changing the entire chemistry of the atmosphere and oceans, and nothing is ready for that.”

To conduct the study, researchers analyzed a database of 500,000 microfossils — the largest of its kind — gathered during 55 years of scientific ocean drilling. Each fossilized shell tells where and when the plankton lived, how deep its habitat was, and the conditions of the ocean around it.

The scientists grouped the information and analyzed it alongside a geologic record of past climate change. They found that as global cooling began 8 million years ago, plankton species were pushed toward the equator. By the modern age, the most diverse plankton populations had moved to the tropics, while the poles of today became too harsh for all but a handful of specialized species.

With global temperatures and atmospheric carbon dioxide now approaching what they were 8 million years ago, the findings suggest that plankton species could evacuate the equator and head poleward, researchers said. Other studies of modern plankton have already documented signs of this happening. Researchers fear that the loss of diversity in plankton populations could trigger a cascade of extinctions like those seen in rainforests after logging and fires.

“The important thing now is to determine how the effect of climate change on those species will cascade across food webs,” said Harvard University network scientist Anshuman Swain, who co-led the research.

When analyzing the data, the researchers used a technique better known for investigating social structures like Twitter to reveal connections between plankton evolution, habitats, and climate change over deep time. First developed to explore social interactions and friendships in sociology, network analysis is increasingly being used in ecology and environmental science and could help inform action to mitigate the worst effects of climate change, Swain said.

The time for action, however, could be running out, said Tracy Aze, an associate professor of marine micropaleontology at the University of Leeds who helped develop the plankton database but was not involved in the current study. According to Aze, today’s unprecedented warming means that the world is now operating on unpredictable time scales.

“The fact that we’ve already begun seeing an appreciable difference in the diversity of many marine groups like fish and the plankton means we might be closer to certain temperature tipping points than we thought,” she said.

Reference: “Late Cenozoic cooling restructured global marine plankton communities” by Adam Woodhouse, Anshuman Swain, William F. Fagan, Andrew J. Fraass and Christopher M. Lowery, 15 February 2023, Nature.
DOI: 10.1038/s41586-023-05694-5

The plankton database, Triton, was developed and published at the University of Leeds and the University of OxfordThe University of Oxford is a collegiate research university in Oxford, England that is made up of 39 constituent colleges, and a range of academic departments, which are organized into four divisions. It was established circa 1096, making it the oldest university in the English-speaking world and the world's second-oldest university in continuous operation after the University of Bologna.” data-gt-translate-attributes=”[{“attribute”:”data-cmtooltip”, “format”:”html”}]”>University of Oxford in 2021. The current research was funded by the University of Maryland and University of Texas Institute for Geophysics, a research unit of the Jackson School of Geosciences.

Source: SciTechDaily