Metastable Iron (Mono)sulfides in the Shallow-Sea Hydrothermal Sediments of Milos, Greece-Reference-Cited by-同舟云学术

Metastable Iron (Mono)sulfides in the Shallow-Sea Hydrothermal Sediments of Milos, Greece

Published:2022-03-17 Issue:4 Volume:6 Page:920-931
ISSN:2472-3452
Container-title:ACS Earth and Space Chemistry
language:en
Short-container-title:ACS Earth Space Chem.

Author:

Kotopoulou Electra¹^ORCID,Godelitsas Athanasios¹,Göttlicher Jörg²,Steininger Ralph²,Price Roy³,Fike David A.⁴,Amend Jan P.⁵,Gilhooly William P.⁶,Druschell Gregory⁶,Nomikou Paraskevi¹,Gamaletsos Platon N.⁷,Lozios Stylianos¹

Affiliation:

1. Department of Geology and Geoenvironment, National and Kapodistrian University of Athens, Zografou Campus, GR-15784 Athens, Greece

2. ANKA Synchrotron Radiation Facility, Karlsruhe Institute of Technology, 76344 Karlsruhe, Germany

3. School of Marine and Atmospheric Sciences, SUNY Stony Brook, Stony Brook, New York 11790, United States

4. Department of Earth and Planetary Sciences, Washington University in St. Louis, St. Louis, Missouri 63105, United States

5. Department of Earth Sciences, University of Southern California, Los Angeles, California 90089, United States

6. Department of Earth Sciences, Indiana University−Purdue University Indianapolis, Indianapolis, Indiana 46202, United States

7. School of Mineral Resources Engineering, Technical University of Crete, GR-73100 Chania, Greece

Funder

National Science Foundation

Greek State Scholarships Foundation (IKY) - Deutscher Akademischer Austauschdienst (DAAD)

Publisher

American Chemical Society (ACS)

Subject

Space and Planetary Science,Atmospheric Science,Geochemistry and Petrology

Link

https://pubs.acs.org/doi/pdf/10.1021/acsearthspacechem.1c00305

Reference94 articles.

1. Chemistry of Iron Sulfides

2. Rethinking the Ancient Sulfur Cycle

3. The Biogeochemical Sulfur Cycle of Marine Sediments

4. Pyrite formation from FeS and H2S is mediated through microbial redox activity

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