Southern Ocean Oxygenation Changes Inferred From Redox‐Sensitive Trace Metals Across Marine Isotope Stage 11-Reference-Cited by-同舟云学术

Southern Ocean Oxygenation Changes Inferred From Redox‐Sensitive Trace Metals Across Marine Isotope Stage 11

Published:2021-08 Issue:8 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Rohde E. E.¹,Hayes C. T.¹^ORCID,Redmond N.¹^ORCID,Glasscock S. K.¹

Affiliation:

1. School of Ocean Science and Engineering University of Southern Mississippi Stennis Space Center MS USA

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009921

Reference58 articles.

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2. Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO 2

3. GEOTRACES intercalibration of230Th,232Th,231Pa, and prospects for10Be

4. Late-Quaternary changes in productivity of the Southern Ocean

5. Deep‐Sea Oxygen Depletion and Ocean Carbon Sequestration During the Last Ice Age

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1. Anomalous 234U/238U isotopic composition in Southern Ocean sediments;Geochimica et Cosmochimica Acta;2023-12

2. Diverse glacial ventilation in deep Pacific: An integrated record from Mariana Trench and Magellan Seamounts over last 1.2 Myr;Global and Planetary Change;2023-11

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