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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Autores principales: M. Dumont, L. Pichevin, W. Geibert, X. Crosta, E. Michel, S. Moreton, K. Dobby, R. Ganeshram
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/5577b384c09448919ec90d1c309ed494
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