Diagenetic cycling of trace elements in the bottom sediments of the Swan River Estuary,Western Australia |
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| Institution: | 1. Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, F-75005 Paris, France;2. Laboratoire Biogéosciences, UMR 6282, CNRS, Université Bourgogne Franche-Comté, 21000 Dijon, France;3. School of Earth and Environmental Sciences, University of St. Andrews, KY16 9AL, Scotland, UK;4. Max-Planck-Institute for Biogeochemistry, Hans-Knoell-Str. 10, 07745 Jena, Germany;5. MARUM, Center for Marine Environmental Sciences, University of Bremen, Germany;6. Dept. Earth & Space Sciences and Astrobiology Program, University of Washington, Seattle 98195, United States;7. Metis, Université Pierre et Marie Curie, UMR 7619 CNRS, F-75005 Paris, France;1. College of History, Geography and Tourism, Shangrao Normal University, Shangrao 334000, China;2. Agro-Environmental Protection Institute, Ministry of Agriculture, Tianjin 300191, China;3. Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China |
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| Abstract: | Teflon strips were used in-situ in the bottom sediments at two sites in the Swan River Estuary to collect diagenetic Fe–Mn oxyhydroxides and monitor monthly changes in their morphology and trace element geochemistry. This study demonstrates that substantial concentrations of trace elements accumulate at the redox front during the formation of diagenetic Fe–Mn oxyhydroxides. It is likely that the Fe–Mn oxyhydroxides initially nucleate and grow on the Teflon strips via bacterial activity. Trace element geochemistry of the diagenetic Fe–Mn oxyhydroxides is influenced by changes in the supply of trace elements from either the bottom sediments and/or water column or changes in the physico-chemical status of bottom and porewaters. If sufficient diagenetic Fe–Mn oxyhydroxides are preserved in the upper layer(s) of the bottom sediment it is possible that diagenetic (secondary) trace element enrichment profiles may be produced which modify the historical input of natural or anthropogenic trace element sources. Alternatively, partial or complete dissolution of the diagenetic Fe–Mn oxyhydroxides in response to temporal changes in the redox status of the bottom sediment may lead to a substantial underestimate of trace element fluxes in historical bottom sediment profiles. This study highlights that considerable care must be taken when interpreting short- to long-term geochemical profiles in bottom sediments due to the possible occurrence of rapid, seasonally mediated diagenetic processes. |
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