2014
DOI: 10.1016/j.marpolbul.2014.09.055
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Organic matter and pyritization relationship in recent sediments from a tropical and eutrophic bay

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Cited by 16 publications
(1 citation statement)
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“…0.2-7 wt% Fe; Anbuselvan et al, 2018;Koukina et al, 2017) under tropical climate, this correlation suggests that TOC might be a limiting factor for Fe(III) microbial reduction (and in turn, pyritization) in the studied Fe-rich lagoon sediments of New Caledonia. This limiting character of the TOC available to fuel microbial reduction of Fe(III) associated with goethite and/or clay minerals has already been proposed to explain the low formation of pyrite in subsurface redox transition zone or sediments (Benzine et al, 2013;Sabadini-Santos et al, 2014;Wu et al, 2017).…”
Section: Influence Of the Redox Conditions On Fe And Ni Speciation Inmentioning
confidence: 73%
“…0.2-7 wt% Fe; Anbuselvan et al, 2018;Koukina et al, 2017) under tropical climate, this correlation suggests that TOC might be a limiting factor for Fe(III) microbial reduction (and in turn, pyritization) in the studied Fe-rich lagoon sediments of New Caledonia. This limiting character of the TOC available to fuel microbial reduction of Fe(III) associated with goethite and/or clay minerals has already been proposed to explain the low formation of pyrite in subsurface redox transition zone or sediments (Benzine et al, 2013;Sabadini-Santos et al, 2014;Wu et al, 2017).…”
Section: Influence Of the Redox Conditions On Fe And Ni Speciation Inmentioning
confidence: 73%