Cold-water corals in the Subpolar North Atlantic Ocean exposed to aragonite undersaturation if the 2 °C global warming target is not met

The net uptake of carbon dioxide (CO2) from the atmosphere is changing the ocean’s chemical state. Such changes, commonly known as ocean acidification, include a reduction in pH and the carbonate ion concentration ([CO3 2− ]), which in turn lowers oceanic saturation states for calcium carbonate (CaC...

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Bibliographic Details
Main Author: García-Ibáñez, Maribel I. (author)
Other Authors: Bates, Nicholas R. (author), Bakker, Dorothee C.E. (author), Fontela, Marcos (author), Velo, Antón (author)
Format: article
Language:eng
Published: 2021
Subjects:
Ocean acidification
Aragonite saturation state
Atlantic Meridional Overturning Circulation
Eastern-Subpolar North Atlantic Ocean
Online Access:http://hdl.handle.net/10400.1/16785
Country:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/16785

Internet

http://hdl.handle.net/10400.1/16785

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