North Atlantic Deep Water Production during the Last Glacial Maximum

Changes in deep ocean ventilation are commonly invoked as the primary cause of lower glacial atmospheric CO(2). The water mass structure of the glacial deep Atlantic Ocean and the mechanism by which it may have sequestered carbon remain elusive. Here we present neodymium isotope measurements from co...

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Detalles Bibliográficos
Autores principales: Howe, Jacob N. W., Piotrowski, Alexander M., Noble, Taryn L., Mulitza, Stefan, Chiessi, Cristiano M., Bayon, Germain
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4895795/
https://www.ncbi.nlm.nih.gov/pubmed/27256826
http://dx.doi.org/10.1038/ncomms11765

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4895795/
https://www.ncbi.nlm.nih.gov/pubmed/27256826
http://dx.doi.org/10.1038/ncomms11765

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