Formation of green rust and elemental sulfur in an analogue for oxygenated ferro-euxinic transition zones of Precambrian oceans-Reference-Cited by-同舟云学术

Formation of green rust and elemental sulfur in an analogue for oxygenated ferro-euxinic transition zones of Precambrian oceans

Author:

Koeksoy E.¹,Sundman A.¹,Byrne J.M.¹,Lohmayer R.²,Planer-Friedrich B.²,Halevy I.³,Konhauser K.O.⁴,Kappler A.¹⁵

Affiliation:

1. Geomicrobiology, University of Tuebingen, 72076 Tuebingen, Germany

2. Environmental Geochemistry, Bayreuth Center for Ecology and Environmental Research (BayCEER), University of Bayreuth, 95440 Bayreuth, Germany

3. Department of Earth and Planetary Sciences, Weizmann Institute of Science, Rehovot 76100, Israel

4. Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta T6G 2E3, Canada

5. Center for Geomicrobiology, Aarhus University, 8000 Aarhus, Denmark

Publisher

Geological Society of America

Subject

Geology

Link

Reference40 articles.

2. Iron formations: Their origins and implications for ancient seawater chemistry;Bekker,2014

3. Iron isotopes in an Archean ocean analogue;Busigny;Geochimica et Cosmochimica Acta,2014

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