The iron speciation paleoredox proxy:
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...
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| Main Author: | |
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| Format: | Electronic eBook |
| Language: | English |
| Published: |
Cambridge
Cambridge University Press
2021
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| Series: | Cambridge elements
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| Subjects: | |
| Online Access: | BSB01 FHN01 Volltext |
| Summary: | 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 |
| Item Description: | Title from publisher's bibliographic system (viewed on 22 Feb 2021) |
| Physical Description: | 1 Online-Ressource (24 Seiten) |
| ISBN: | 9781108847148 |
| DOI: | 10.1017/9781108847148 |
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| isbn | 9781108847148 |
| language | English |
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| spelling | Poulton, Simon ca. 20./21. Jh. (DE-588)1231497858 aut The iron speciation paleoredox proxy Simon W. Poulton Cambridge Cambridge University Press 2021 1 Online-Ressource (24 Seiten) txt rdacontent c rdamedia cr rdacarrier Cambridge elements Title from publisher's bibliographic system (viewed on 22 Feb 2021) 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 Biogeochemical cycles Iron / Environmental aspects Erscheint auch als Druck-Ausgabe 978-1-108-81068-5 https://doi.org/10.1017/9781108847148 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Poulton, Simon ca. 20./21. Jh The iron speciation paleoredox proxy Biogeochemical cycles Iron / Environmental aspects |
| title | The iron speciation paleoredox proxy |
| title_auth | The iron speciation paleoredox proxy |
| title_exact_search | The iron speciation paleoredox proxy |
| title_exact_search_txtP | The iron speciation paleoredox proxy |
| title_full | The iron speciation paleoredox proxy Simon W. Poulton |
| title_fullStr | The iron speciation paleoredox proxy Simon W. Poulton |
| title_full_unstemmed | The iron speciation paleoredox proxy Simon W. Poulton |
| title_short | The iron speciation paleoredox proxy |
| title_sort | the iron speciation paleoredox proxy |
| topic | Biogeochemical cycles Iron / Environmental aspects |
| topic_facet | Biogeochemical cycles Iron / Environmental aspects |
| url | https://doi.org/10.1017/9781108847148 |
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