The Southern Ocean is a major carbon sink, but knowledge of its variability is limited, especially in the coastal Antarctic. Now, results based on 25 years of observations in the West Antarctic Peninsula show that the carbon sink is increasing rapidly, driven by summertime biological production linked to sea ice dynamics.
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Decline in plankton diversity and carbon flux with reduced sea ice extent along the Western Antarctic Peninsula
Nature Communications Open Access 16 August 2021
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Change history
16 September 2019
In the version of this News & Views originally published, the ORCID (0000-0002-1165-1074) for author Nicholas Metzl was missing; it has now been added.
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Metzl, N. A canary in the Southern Ocean. Nat. Clim. Chang. 9, 651–652 (2019). https://doi.org/10.1038/s41558-019-0562-1
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DOI: https://doi.org/10.1038/s41558-019-0562-1
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Decline in plankton diversity and carbon flux with reduced sea ice extent along the Western Antarctic Peninsula
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