Atlantic deep water provenance decoupled from atmospheric CO(2) concentration during the lukewarm interglacials

Ice core records show that atmospheric CO(2) concentrations and Antarctic temperature were lower during the ‘lukewarm interglacials’ from 800 to 430 ka than the subsequent five interglacials. These different interglacial ‘strengths’ have been hypothesised to be controlled by Antarctic overturning ci...

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Detalles Bibliográficos
Autores principales: Howe, Jacob N. W., Piotrowski, Alexander M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5722826/
https://www.ncbi.nlm.nih.gov/pubmed/29222483
http://dx.doi.org/10.1038/s41467-017-01939-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5722826/
https://www.ncbi.nlm.nih.gov/pubmed/29222483
http://dx.doi.org/10.1038/s41467-017-01939-w

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