A long-term record of early to mid-Paleozoic marine redox change

Author:

Sperling Erik A.1ORCID,Melchin Michael J.2,Fraser Tiffani3ORCID,Stockey Richard G.1ORCID,Farrell Una C.14ORCID,Bhajan Liam1ORCID,Brunoir Tessa N.1,Cole Devon B.5ORCID,Gill Benjamin C.6ORCID,Lenz Alfred7,Loydell David K.8ORCID,Malinowski Joseph9ORCID,Miller Austin J.1,Plaza-Torres Stephanie10,Bock Beatrice11ORCID,Rooney Alan D.12ORCID,Tecklenburg Sabrina A.1ORCID,Vogel Jacqueline M.1,Planavsky Noah J.12ORCID,Strauss Justin V.9ORCID

Affiliation:

1. Department of Geological Sciences, Stanford University, Stanford, CA, USA.

2. Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada.

3. Yukon Geological Survey, Whitehorse, Yukon, Canada.

4. Department of Geology, Trinity College Dublin, Dublin 2, Ireland.

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

6. Department of Geosciences, Virginia Polytechnic University and State University, Blacksburg, VA, USA.

7. Department of Earth Sciences, Western University Canada, London, ON, Canada.

8. School of the Environment, Geography and Geosciences, University of Portsmouth, Portsmouth, UK.

9. Department of Earth Sciences, Dartmouth College, Hanover, NH, USA.

10. Department of Geology, University of Puerto Rico, Mayagüez, Puerto Rico.

11. Department of Earth and Environmental Sciences, Vanderbilt University, Nashville, TN, USA.

12. Department of Earth and Planetary Sciences, Yale University, New Haven, CT, USA.

Abstract

Early Paleozoic bottom waters were mainly ferruginous, like the Neoproterozoic, with a shift to increased euxinia in the Devonian.

Funder

National Science Foundation

Alfred P. Sloan Foundation

Agouron Institute

Natural Sciences and Engineering Research Council of Canada

Stanford Program on Deep-water Depositional Systems

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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