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Expanded oxygen minimum zones during the late Paleocene-early Eocene: hints from multi-proxy comparison and ocean modelling

Abstract:

Anthropogenic warming could well drive depletion of oceanic oxygen in the future. Important insight into the relationship between de-oxygenation and warming can be gleaned from the geological record, but evidence is limited because few ocean oxygenation records are available for past greenhouse climate conditions. We use I/Ca in benthic foraminifera to reconstruct late Paleocene through early Eocene bottom and pore-water redox conditions in the South Atlantic and Southern Indian Oceans, and c...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher's version

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Publisher copy:
10.1002/2016PA003020

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Publisher:
American Geophysical Union Publisher's website
Journal:
Paleoceanography Journal website
Volume:
31
Issue:
12
Pages:
1532–1546
Publication date:
2016-01-01
Acceptance date:
2016-11-02
DOI:
EISSN:
1944-9186
ISSN:
0883-8305
Pubs id:
pubs:657466
URN:
uri:8cb03e8f-2196-4014-ba70-afdf93f2654b
UUID:
uuid:8cb03e8f-2196-4014-ba70-afdf93f2654b
Local pid:
pubs:657466
Paper number:
12

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