Episodic release of CO2 from the high-latitude North Atlantic Ocean during the last 135 kyr

Glacial-interglacial variations in atmospheric pCO2 remain unexplained. Here, the authors show that the Norwegian Sea, an modern area of intense CO2 uptake, acted as a CO2 source during the terminations of Heinrich stadials 1, 4 and 11, sometimes characterized by rapid increases in atmospheric pCO2.

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Autores principales: Mohamed M. Ezat, Tine L. Rasmussen, Bärbel Hönisch, Jeroen Groeneveld, Peter deMenocal
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/69d80a91cd8743aeb2f953dfcde65140
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