Stable W and Mo isotopic evidence for increasing redox-potentials from the Paleoarchean towards the Paleoproterozoic deep ocean

Volume: 309, Pages: 366 - 387
Published: Sep 1, 2021
Abstract
• Stable W isotope variations of Archean shales. • Stable W isotopes trace redox of anoxic ferruginous, but not euxinic sediments. • Eh evolution of the Archean Ocean. The scavenging of dissolved trace metals such as chromium (Cr), molybdenum (Mo) and tungsten (W) and their authigenic enrichment in sedimentary archives mainly occur by particle shuttling that cause resolvable isotope fractionation. Because their scavenging is also dependent on...
Paper Details
Title
Stable W and Mo isotopic evidence for increasing redox-potentials from the Paleoarchean towards the Paleoproterozoic deep ocean
Published Date
Sep 1, 2021
Volume
309
Pages
366 - 387
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