A sedimentary record of the evolution of the global marine phosphorus cycle-Reference-Cited by-同舟云学术

A sedimentary record of the evolution of the global marine phosphorus cycle

Published:2022-12-05 Issue:2 Volume:21 Page:168-174
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Planavsky Noah J.¹,Asael Dan¹^ORCID,Rooney Alan D.¹^ORCID,Robbins Leslie J.¹,Gill Benjamin C.²,Dehler Carol M.³,Cole Devon B.⁴^ORCID,Porter Susannah M.⁵^ORCID,Love Gordon D.⁶^ORCID,Konhauser Kurt O.⁷,Reinhard Christopher T.⁴^ORCID

Affiliation:

1. The Department of Earth & Planetary Sciences Yale University New Haven Connecticut USA

2. Department of Geosciences Virginia Institute of Technology Blacksburg Virginia USA

3. Department of Geology Utah State University Logan Utah USA

4. School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta Georgia USA

5. Department of Earth Sciences University of California Santa Barbara California USA

6. Department of Earth Sciences University of California Riverside California USA

7. Department of Earth and Atmospheric Sciences University of Alberta Edmonton Alberta Canada

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12536

Reference46 articles.

1. Stepwise Earth oxygenation is an inherent property of global biogeochemical cycling

2. Oxygen overshoot and recovery during the early Paleoproterozoic

3. Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides

4. The transition from a cyanobacterial to algal world and the emergence of animals

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