ERC Starting Grant · 2024
Deep-sea carbonates under pressure: mechanisms of dissolution and climate feedbacks
As humanity grapples with the escalating crisis of climate change, understanding and mitigating the sources of carbon dioxide (CO2) emissions is imperative. A lesser-known yet significant aspect of this crisis lies in the vast expanses of marine sediments which encompass two-thirds of the Earth’s surface. A key component of these sediments is calcium carbonate (CaCO3), a family of minerals that makes up the shells and skeletons of marine organisms. CO2 emissions lead to ocean acidification, triggering CaCO3 dissolution, which in turn neutralizes CO2, acting as a crucial CO2 sink over millennial timescales. However, the mechanisms and rate of this dissolution remain unknown due to the…
From the public funding record at EU CORDIS. Describes the funded project, not the reviews below.
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