Interglacial dust, ocean fertilisation and Neoproterozoic earth oxygenation

Abstract Feedback processes that drove Earth's second major increase in ocean–atmosphere oxygen levels during the Neoproterozoic are poorly constrained. Variability in seawater redox over geological timescales is commonly linked to changes in the biogeochemical cycling of P and thus the rate of...

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Bibliographic Details
Main Authors: Leandro G. DaSilva, Peir K. Pufahl, Noel P. James
Format: Article
Language:English
Published: Wiley 2025-04-01
Series:The Depositional Record
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Online Access:https://doi.org/10.1002/dep2.323
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