In situ trace metal analysis of Neoarchaean - Ordovician shallow-marine microbial-carbonate-hosted pyrites

Pre‐Cambrian atmospheric and oceanic redox evolutions are expressed in the inventory of redox‐sensitive trace metals in marine sedimentary rocks. Most of the currently available information was derived from deep‐water sedimentary rocks (black shale/banded iron formation). Many of the studied trace m...

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Veröffentlicht in:Geobiology 2015-07, Vol.13 (4), p.316-339
Hauptverfasser: Gallagher, M., Turner, E. C., Kamber, B. S.
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Sprache:eng
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