Atmosphere‐Ocean CO 2 Exchange Across the Last Deglaciation From the Boron Isotope Proxy-Reference-Cited by-同舟云学术

Atmosphere‐Ocean CO 2 Exchange Across the Last Deglaciation From the Boron Isotope Proxy

Published:2019-10 Issue:10 Volume:34 Page:1650-1670
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Shao Jun¹^ORCID,Stott Lowell D.¹^ORCID,Gray William R.²³^ORCID,Greenop Rosanna²^ORCID,Pecher Ingo⁴^ORCID,Neil Helen L.⁵,Coffin Richard B.⁶,Davy Bryan⁷^ORCID,Rae James W.B.²^ORCID

Affiliation:

1. Department of Earth Science University of Southern California Los Angeles CA USA

2. School of Earth and Environmental Sciences University of St Andrews St Andrews UK

3. Laboratoire des Sciences du Climat et de l'Environnement (LSCE/IPSL) Gif‐sur‐Yvette France

4. School of Environment University of Auckland Auckland New Zealand

5. Department of Marine Geology The National Institute of Water and Atmospheric Research Auckland New Zealand

6. Department of Physical and Environmental Sciences Texas A&M University Corpus Christi TX USA

7. Department of Marine Geosciences GNS Science Lower Hutt New Zealand

Funder

Natural Environment Research Council

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018PA003498

Reference85 articles.

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

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

3. A study of cleaning procedures used for foraminiferal Mg/Ca paleothermometry

4. Interhemispheric Atlantic seesaw response during the last deglaciation

5. Breakup of last glacial deep stratification in the South Pacific

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