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