Constraints on Early Paleozoic Deep‐Ocean Oxygen Concentrations From the Iron Geochemistry of the Bay of Islands Ophiolite

Author:

Stolper Daniel A.1ORCID,Pu Xiaofei2ORCID,Lloyd Max K.13ORCID,Christensen Nikolas I.4ORCID,Bucholz Claire E.5,Lange Rebecca A.2ORCID

Affiliation:

1. Department of Earth and Planetary Science University of California Berkeley CA USA

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

3. Department of Geosciences The Pennsylvania State University University Park PA USA

4. Department of Earth, Ocean and Atmospheric Sciences University of British Columbia Vancouver BC Canada

5. Divison of Geological and Planetary Sciences California Institute of Technology Pasadena CA USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference88 articles.

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

2. Reconstruction of secular variation in seawater sulfate concentrations

3. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: A synthesis of results from site 504 (DSDP legs 69, 70, and 83, and ODP legs 111, 137, 140, and 148);Alt J. C.;Proceedings of the Ocean Drilling Program, Scientific Results,1996

4. K–Ar ages of amphiboles from the Bay of Islands ophiolite and the Little Port Complex, western Newfoundland, and their geological implications

5. Iron and sulfide oxidation within the basaltic ocean crust: implications for chemolithoautotrophic microbial biomass production

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