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Selenium Isotope Paleobiogeochemistry

Selenium Isotope Paleobiogeochemistry

290 kr

290 kr

På lager

On., 26 mars - ti., 1 april


Sikker betaling

14 dagers åpent kjøp


Selges og leveres av

Adlibris


Produktbeskrivelse

The attraction of selenium isotopes as a paleoenvironmental tracer lies in the high redox potential of selenium oxyanions (SeIV and SeVI), the dominant species in the modern ocean. The largest isotopic fractionations occur during oxyanion reduction, which makes selenium isotopes a sensitive proxy for the redox evolution of our planet. As a case study we review existing data from the Neoarchean and Paleoproterozoic, which show that significant isotopic fractionations are absent until 2.5 Ga, and prolonged isotopic deviations only appear around 2.3 Ga. Selenium isotopes have thus begun to reveal complex spatiotemporal redox patterns not reflected in other proxies.

Artikkel nr.

cfca6346-9185-541b-8874-0b0b8ea53649

Selenium Isotope Paleobiogeochemistry

290 kr

290 kr

På lager

On., 26 mars - ti., 1 april


Sikker betaling

14 dagers åpent kjøp


Selges og leveres av

Adlibris