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

W. Homoky; D. Hembury; L. Hepburn; R. Mills; P. Statham; Gary Fones

doi:10.1016/j.gca.2011.06.019

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

W. Homoky
, D. Hembury
, L. Hepburn
, R. Mills
, P. Statham
, Gary Fones

Research output: Contribution to journal › Article › peer-review

Abstract

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 language	English
Pages (from-to)	5032-5048
Number of pages	17
Journal	Geochimica et Cosmochimica Acta
Volume	75
Issue number	17
DOIs	https://doi.org/10.1016/j.gca.2011.06.019
Publication status	Published - 1 Sept 2011

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abstract = "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 (",

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AU - Homoky, W.

AU - Hembury, D.

AU - Hepburn, L.

AU - Mills, R.

AU - Statham, P.

AU - Fones, Gary

PY - 2011/9/1

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N2 - 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 (

AB - 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 (

U2 - 10.1016/j.gca.2011.06.019

DO - 10.1016/j.gca.2011.06.019

M3 - Article

SN - 0016-7037

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JO - Geochimica et Cosmochimica Acta

JF - Geochimica et Cosmochimica Acta

IS - 17

ER -

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

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