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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 CO, Nd-Sr isotopic and trace element geochemistry of ∼1.9 Ga stromatolitic Tadpatri Car...

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Principais autores: M. Ashok, Nurul Absar
פורמט: Artigo
שפה:Inglês
יצא לאור: Elsevier 2025-08-01
סדרה:Geosystems and Geoenvironment
נושאים:
Orosirian
Stromatolite geochemistry
Carbon cycle
Paleoredox
Solute sources
Dolomitization
גישה מקוונת:http://www.sciencedirect.com/science/article/pii/S2772883825000366
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