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In one form or another, iron speciation has had a long history as a paleoredox proxy. This Element covers the theory behind the proxy, methods involved in applying the technique, and potential complications in interpreting Fe speciation data.

Produktbeschreibung
In one form or another, iron speciation has had a long history as a paleoredox proxy. This Element covers the theory behind the proxy, methods involved in applying the technique, and potential complications in interpreting Fe speciation data.
Autorenporträt
Professor Simon Poulton is Chair of Biogeochemistry and Earth History at the University of Leeds. Originally trained as a geologist, his research focuses on geochemical and biogeochemical processes in modern sediments and waters, with a view to applying this understanding to ancient environments.