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Diagenetic and Hydrothermal Processes Produce Heavy Molybdenum Isotope Signatures in Pelagic Sediments of the North and South Pacific

Abstract Molybdenum isotopes (δ98Mo) have been used for more than two decades to investigate past‐ocean redox conditions due to the distinct behavior of this element in oxic and anoxic environments. The oxic sink is generally accepted to have a near‐constant δ98Mo value of −0.7‰, a value derived pri...

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Autori principali: P. L. Fraga‐Ferreira, C. Siebert, M. Frank, F. Scholz
Natura: Artigo
Lingua:Inglês
Pubblicazione: Wiley 2026-02-01
Serie:Geochemistry, Geophysics, Geosystems
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Accesso online:https://doi.org/10.1029/2025GC012749
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