Isotopically "heavy" pyrite in marine sediments due to high sedimentation rates and non-steady-state deposition

Isotopically "heavy" pyrite in marine sediments due to high sedimentation rates and non-steady-state deposition

Sedimentary pyrite formation links the global biogeochemical cycles of carbon, sulfur, and iron, which, in turn, modulate the redox state of the planet's surficial environment over geological time scales. Accordingly, the sulfur isotopic composition (δ34S) of pyrite has been widely employed as...

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Main Authors: Liu, Jiarui (Author), Antler, Gilad (Author), Pellerin, André (Author), Izon, Gareth (Author), Dohrmann, Ingrid (Author), Findlay, Alyssa J. (Author), Røy, Hans (Author), Ono, Shuhei (Author), Turchyn, Alexandra V. (Author), Kasten, Sabine (Author), Jørgensen, Bo Barker (Author)
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences (Contributor)
Format: Article
Language:English
Published: Geological Society of America, 2021-09-30T15:45:50Z.
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