Less Remineralized Carbon in the Intermediate‐Depth South Atlantic During Heinrich Stadial 1-Reference-Cited by-同舟云学术

Less Remineralized Carbon in the Intermediate‐Depth South Atlantic During Heinrich Stadial 1

Published:2019-07 Issue:7 Volume:34 Page:1218-1233
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Lacerra Matthew¹²^ORCID,Lund David C.¹^ORCID,Gebbie Geoffrey³^ORCID,Oppo Delia W.⁴^ORCID,Yu Jimin⁵^ORCID,Schmittner Andreas⁶^ORCID,Umling Natalie E.⁴⁷^ORCID

Affiliation:

1. Department of Marine Sciences University of Connecticut Groton CT USA

2. Now at Department of Geosciences Princeton University Princeton NJ USA

3. Department of Physical Oceanography Woods Hole Oceanographic Institution Woods Hole MA USA

4. Department of Geology and Geophysics Woods Hole Oceanographic Institution Woods Hole MA USA

5. Research School of Earth Sciences Australian National University Acton ACT Australia

6. College of Earth, Ocean, and Atmospheric Sciences Oregon State University Corvallis OR USA

7. Department of Earth and Planetary Sciences American Museum of Natural History New York NY USA

Funder

Division of Ocean Sciences

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018PA003537

Reference69 articles.

1. Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination

2. Redfield ratios of remineralization determined by nutrient data analysis

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

4. Interhemispheric Atlantic seesaw response during the last deglaciation

5. Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation

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