Ice Age‐Holocene Similarity of Foraminifera‐Bound Nitrogen Isotope Ratios in the Eastern Equatorial Pacific-Reference-Cited by-同舟云学术

Ice Age‐Holocene Similarity of Foraminifera‐Bound Nitrogen Isotope Ratios in the Eastern Equatorial Pacific

Published:2021-05 Issue:5 Volume:36 Page:
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanogr Paleoclimatol

Author:

Studer Anja S.¹²^ORCID,Mekik Figen³^ORCID,Ren Haojia⁴,Hain Mathis P.⁵^ORCID,Oleynik Sergey⁶^ORCID,Martínez‐García Alfredo²,Haug Gerald H.²⁷,Sigman Daniel M.⁶^ORCID

Affiliation:

1. Department of Environmental Sciences University of Basel Basel Switzerland

2. Max Planck Institute for Chemistry Climate Geochemistry Department Mainz Germany

3. Department of Geology Grand Valley State University Allendale MI USA

4. Department of Geosciences National Taiwan University Taipei Taiwan

5. University of California Earth and Planetary Sciences Department Santa Cruz CA USA

6. Department of Geosciences Princeton University Princeton NJ USA

7. ETH Zurich Geological Institute Zurich Switzerland

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020PA004063

Reference120 articles.

1. Southern Ocean upwelling, Earth’s obliquity, and glacial-interglacial atmospheric CO 2 change

2. Nitrogen isotopic evidence for micronutrient control of fractional NO3 − utilization in the equatorial Pacific

3. Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization

5. The effect of millennial-scale changes in Arabian Sea denitrification on atmospheric CO2

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