Poulton, SW orcid.org/0000-0001-7621-189X (2021) The Iron Speciation Paleoredox Proxy. Elements in Geochemical Tracers in Earth System Science . Cambridge University Press ISBN 9781108847148
Abstract
In one form or another, iron speciation has had a long history as a paleoredox proxy. The technique has been refined considerably over the years, and the most recent scheme is unique in its potential to distinguish three major oceanic redox states - oxygenated, ferruginous and euxinic. This Element covers the theory behind the proxy, methods involved in applying the technique, and potential complications in interpreting Fe speciation data. A series of case studies are also provided, which highlight how more advanced consideration of the data, often in concert with other techniques, can provide unprecedented insight into the redox state of ancient oceans.
Metadata
Item Type: | Book |
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Authors/Creators: |
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Keywords: | Fe speciation; paleoredox; ferruginous; euxinic; anoxia |
Dates: |
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Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Earth Surface Science Institute (ESSI) (Leeds) |
Funding Information: | Funder Grant number Royal Society WM150108 |
Depositing User: | Symplectic Publications |
Date Deposited: | 28 Oct 2020 15:55 |
Last Modified: | 04 Dec 2023 16:54 |
Published Version: | https://doi.org/10.1017/9781108847148 |
Status: | Published |
Publisher: | Cambridge University Press |
Series Name: | Elements in Geochemical Tracers in Earth System Science |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:167303 |