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OverviewIn 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. Full Product DetailsAuthor: Simon W. Poulton (University of Leeds)Publisher: Cambridge University Press Imprint: Cambridge University Press Dimensions: Width: 23.00cm , Height: 0.20cm , Length: 15.00cm Weight: 0.680kg ISBN: 9781108810685ISBN 10: 1108810683 Pages: 75 Publication Date: 04 March 2021 Audience: Professional and scholarly , Professional & Vocational Format: Paperback Publisher's Status: Active Availability: Manufactured on demand  We will order this item for you from a manufactured on demand supplier. Table of Contents1. Introduction; 2. Systematics of the Fe Speciation Paleoredox Proxy; 3. Methodology; 4. Case Studies; 5. Outlook; 6. Key Papers.ReviewsAuthor InformationProfessor 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. Tab Content 6Author Website:Countries AvailableAll regions |
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