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Iron and manganese diagenesis in deep sea volcanogenic sediments and the origins of pore water colloids

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Volcanogenic sediments are typically rich in Fe- and Mn-bearing minerals that undergo substantial alteration during early marine diagenesis, however their impact on the global biogeochemical cycling of Fe and Mn has not been widely addressed. This study compares the near surface (0-20 cm below sea floor [cmbsf]) aqueous (
Original languageEnglish
Pages (from-to)5032-5048
Number of pages17
JournalGeochimica et Cosmochimica Acta
Issue number17
Publication statusPublished - 1 Sep 2011

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