At depths between several tens and hundreds of metres, large parts of the tropical oceans are poorly supplied with dissolved oxygen, and are therefore hostile to most marine life. Scientists suspect that these zones are sensitive to climate change, but previous studies have arrived at conflicting conclusions regarding exactly how and why a more CO2-rich world affects oceanic oxygen content.
A team led by Andreas Oschlies of the Leibniz Institute of Marine Sciences in
"Carbon dioxide fertilizes biological production," says Oschlies. "It's really like junk food for plants. When the carbon-fattened excess biomass sinks it gets decomposed by bacteria which first consume the oxygen, and then the nutrients."
…"Nobody really has ever modelled the feedback of rising CO2 on oceanic oxygen concentrations in such a credible way," says Gian-Kaspar Plattner, a carbon-cycle modeller at the Swiss Federal Institute of Technology Zürich (ETH). "A 50% volume increase of oxygen-poor zones is much more than I would have expected. But further studies, with different climate parameters, are needed to add robustness to these results and reduce uncertainty."
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