Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling-Reference-Cited by-同舟云学术

Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling

Published:2021-07 Issue:7 Volume:35 Page:
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem Cycles

Author:

Farmer J. R.¹²^ORCID,Hertzberg J. E.³^ORCID,Cardinal D.⁴^ORCID,Fietz S.⁵,Hendry K.⁶^ORCID,Jaccard S. L.⁷⁸^ORCID,Paytan A.⁹^ORCID,Rafter P. A.¹⁰^ORCID,Ren H.¹¹,Somes C. J.¹²^ORCID,Sutton J. N.¹³^ORCID,

Affiliation:

1. Department of Geosciences Princeton University Princeton NJ USA

2. Max‐Planck Institute for Chemistry Mainz Germany

3. International Ocean Discovery Program Texas A&M University College Station TX USA

4. LOCEAN (UMR7159) Sorbonne Université IRD CNRS MNHN Paris France

5. Department of Earth Sciences Stellenbosch University Stellenbosch South Africa

6. School of Earth Sciences University of Bristol Bristol UK

7. Institute of Geological Sciences and Oeschger Center for Climate Change Research, University of Bern Bern Switzerland

8. Institute of Earth Sciences University of Lausanne Lausanne Switzerland

9. Institute of Marine Sciences University of California, Santa Cruz Santa Cruz CA USA

10. Department of Earth System Science University of California Irvine CA USA

11. Department of Geosciences National Taiwan University Taipei Taiwan

12. GEOMAR Helmholtz Centre for Ocean Research Kiel Kiel Germany

13. University of Brest CNRS IRD Ifremer Institut Universitaire Européen de la Mer LEMAR Plouzané France

Funder

National Science Foundation

Past Global Changes

Akademie der Naturwissenschaften

Max-Planck-Gesellschaft

Princeton University

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GB006775

Reference209 articles.

1. CARBON ISOTOPE FRACTIONATION IN FORMATION OF AMINO ACIDS BY PHOTOSYNTHETIC ORGANISMS

2. Siple Dome ice reveals two modes of millennial CO2 change during the last ice age

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

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

5. GEOTRACES: Accelerating Research on the Marine Biogeochemical Cycles of Trace Elements and Their Isotopes

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