ERC Advanced Grant · 2020
Seeking Constraints on Open Ocean Biocalcification
Coccolithophores and foraminifera, single-celled mineralising plankton, convert atmospheric CO2 into limestone. Together, they produce over 2 billion tonnes of calcite/year. Anthropogenic change creates myriad threats to the future of marine calcifiers, the foundation of the ocean ecosystem and global carbon cycle. Much work has focussed on the impact of acidification and declining carbonate saturation state on calcifier mineralisation. But the modern ocean is four times supersaturated with respect to calcite. Hence SCOOBi asks: What limits modern marine calcification rates? How will they respond to future change? All modern marine carbonate producers are solar-powered and rely directly on…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.