Redox conditions, solute sources and biogeochemical cycling in the Orosirian ocean: Geochemical and isotopic evidence from stromatolitic carbonates of ∼1.9 Ga Tadpatri Formation, Cuddapah Basin, India
The Orosirian Period of the middle Paleoproterozoic Era was marked by a decline in atmospheric oxygen and a reducing ocean after a brief oxidized interval of the preceding Great Oxidation Event. Here, we present CO, Nd-Sr isotopic and trace element geochemistry of ∼1.9 Ga stromatolitic Tadpatri Car...
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| Hauptverfasser: | , |
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| Format: | Artigo |
| Sprache: | Inglês |
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Elsevier
2025-08-01
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| Schriftenreihe: | Geosystems and Geoenvironment |
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| Online-Zugang: | http://www.sciencedirect.com/science/article/pii/S2772883825000366 |
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