Bottom-water deoxygenation at the Peruvian margin during the last deglaciation recorded by benthic foraminifera
<p>Deciphering the dynamics of dissolved oxygen in the mid-depth ocean during the last deglaciation is essential to understand the influence of climate change on modern oxygen minimum zones (OMZs). Many paleo-proxy records from the eastern Pacific Ocean indicate an extension of oxygen-depleted...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-06-01
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| Series: | Biogeosciences |
| Online Access: | https://www.biogeosciences.net/17/3165/2020/bg-17-3165-2020.pdf |