A paleosol record of the evolution of Cr redox cycling and evidence for an increase in atmospheric oxygen during the Neoproterozoic-Reference-Cited by-同舟云学术

A paleosol record of the evolution of Cr redox cycling and evidence for an increase in atmospheric oxygen during the Neoproterozoic

Published:2019-08-22 Issue:6 Volume:17 Page:579-593
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Colwyn David Auerbach¹^ORCID,Sheldon Nathan D.²^ORCID,Maynard J. Barry³,Gaines Robert⁴,Hofmann Axel⁵,Wang Xiangli¹⁶⁷,Gueguen Bleuenn¹⁸,Asael Dan¹,Reinhard Christopher T.⁹,Planavsky Noah J.¹

Affiliation:

1. Department of Geology and Geophysics Yale University New Haven CT USA

2. Department of Earth and Environmental Sciences University of Michigan Ann Arbor MI USA

3. Department of Geology University of Cincinnati Cincinnati OH USA

4. Geology Department Pomona College Claremont CA USA

5. Department of Geology University of Johannesburg Johannesburg South Africa

6. Department of Marine Sciences University of South Alabama Mobile AL USA

7. Dauphin Island Sea Lab Dauphin Island AL USA

8. Institut Universitaire Européen de la Mer CNRS UMS 3113, Université de Brest Plouzané France

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

Funder

National Science Foundation

NASA Astrobiology Institute

Division of Earth Sciences

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.12360

Reference106 articles.

1. Modern rather than Mesoarchaean oxidative weathering responsible for the heavy stable Cr isotopic signatures of the 2.95 Ga old Ijzermijn iron formation (South Africa)

2. A Whiff of Oxygen Before the Great Oxidation Event?

3. Weathering profiles, mass-balance analysis, and rates of solute loss: Linkages between weathering and erosion in a small, steep catchment

4. Kinetic stable Cr isotopic fractionation between aqueous Cr(III)-Cl-H2O complexes at 25 °C: Implications for Cr(III) mobility and isotopic variations in modern and ancient natural systems

5. Chromium geochemistry of the ca. 1.85 Ga Flin Flon paleosol

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