The nature of deep overturning and reconfigurations of the silicon cycle across the last deglaciation

Global atmospheric CO2 varies between glacial–interglacial cycles. Here, the authors study these changes using Si records and how the Si flux and ocean circulation changes controlled the global Si distribution across the last deglaciation, based on high-resolution Si-isotope records from the Indian...

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Bibliographic Details
Published in:Nature Communications
Main Authors: M. Dumont, L. Pichevin, W. Geibert, X. Crosta, E. Michel, S. Moreton, K. Dobby, R. Ganeshram
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2020
Subjects:
Science
Q
Southern Ocean
Indian
Online Access:https://doi.org/10.1038/s41467-020-15101-6
https://doaj.org/article/5577b384c09448919ec90d1c309ed494
Description
Summary:Global atmospheric CO2 varies between glacial–interglacial cycles. Here, the authors study these changes using Si records and how the Si flux and ocean circulation changes controlled the global Si distribution across the last deglaciation, based on high-resolution Si-isotope records from the Indian Sector Southern Ocean.

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