Marine ecosystem role in setting up preindustrial and future climate.
basic_science · Level V
Where this comes from
- Record sourced from PubMed, PMID 40044713.
- Also identified by DOI 10.1038/s41467-025-57371-y and PMC identifier 11883021.
- Licence recorded as CC BY.
- The licence permits redistribution, so the abstract is shown in full and the full text is available from the publisher.
Abstract
The ocean ecosystem is a vital component of the global carbon cycle, storing enough carbon to keep atmospheric CO<sub>2</sub> considerably lower than it would otherwise be. However, this conception is based on simple models, neglecting the coupled land-ocean feedback. Using an interactive Earth system model, we show that the role ocean biology plays in controlling atmospheric CO<sub>2</sub> is more complex than previously thought. Atmospheric CO<sub>2</sub> in a new equilibrium state after the biological pump is shut down increases by more than 50% (163 ppm), lower than expected as approximately half the carbon lost from the ocean is adsorbed by the land. The abiotic ocean is less capable of taking up anthropogenic carbon due to the warmer climate, an absent biological surface pCO<sub>2</sub> deficit and a higher Revelle factor. Prioritizing research on and preserving marine ecosystem functioning would be crucial to mitigate climate change and the risks associated with it.