Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4

Here we use high-precision carbon isotope data (δ(13)C-CO(2)) to show atmospheric CO(2) during Marine Isotope Stage 4 (MIS 4, ~70.5-59 ka) was controlled by a succession of millennial-scale processes. Enriched δ(13)C-CO(2) during peak glaciation suggests increased ocean carbon storage. Variations in...

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Detalles Bibliográficos
Autores principales: Menking, James A., Shackleton, Sarah A., Bauska, Thomas K., Buffen, Aron M., Brook, Edward J., Barker, Stephen, Severinghaus, Jeffrey P., Dyonisius, Michael N., Petrenko, Vasilii V.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9481522/
https://www.ncbi.nlm.nih.gov/pubmed/36114188
http://dx.doi.org/10.1038/s41467-022-33166-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9481522/
https://www.ncbi.nlm.nih.gov/pubmed/36114188
http://dx.doi.org/10.1038/s41467-022-33166-3

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