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Substantial iron sequestration during green-clay authigenesis in modern deep-sea sediments
Baldermann, A.; Warr, L.N.; Letofsky-Papst, I.; Mavromatis, V. (2015). Substantial iron sequestration during green-clay authigenesis in modern deep-sea sediments. Nature Geoscience 8(11): 885–889. http://dx.doi.org/10.1038/ngeo2542
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908
Peer reviewed article  
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Auteurs  Top 
  • Baldermann, A.
  • Warr, L.N.
  • Letofsky-Papst, I.
  • Mavromatis, V.
Abstract
    Pyrite formation has been considered a key iron sink in organic-rich marine sediments. Analyses of sediments from the Ivory Coast–Ghana Marginal Ridge demonstrate that iron can be buried at greater rates during green-clay formation.
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