Can We Better Constrain the Timing of GNAIW/UNADW Variability in the Western Equatorial Atlantic and Its Relationship to Climate Change During the Last Deglaciation?-Reference-Cited by-同舟云学术

Can We Better Constrain the Timing of GNAIW/UNADW Variability in the Western Equatorial Atlantic and Its Relationship to Climate Change During the Last Deglaciation?

Published:2021-08 Issue:8 Volume:36 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanogr Paleoclimatol

Author:

Guilderson Thomas P.¹²^ORCID,Allen Katherine³^ORCID,Landers Jordan P.⁴^ORCID,Ettwein Virginia J.²⁵,Cook Mea S.⁶

Affiliation:

1. Department of Ocean Sciences University of California‐Santa Cruz Santa Cruz CA USA

2. Center for Accelerator Mass Spectrometry Lawrence Livermore National Laboratory Livermore CA USA

3. School of Earth and Climate Sciences University of Maine Orono ME USA

4. Greenwings Biomedical Irvine CA USA

5. Department of Earth Sciences University of Oxford Oxford UK

6. Department of Geosciences Williams College Williamstown MA USA

Funder

Lamont-Doherty Earth Observatory, Columbia University

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020PA004187

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4. Correction of accelerator mass spectrometry14C ages measured in planktonic foraminifera: Paleoceanographic implications

5. The North Atlantic atmosphere-sea surface 14C gradient during the Younger Dryas climatic event

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