Abiotic pyrite formation produces a large Fe isotope fractionation

Science

Volumn 332, Issue 6037, 2011, Pages 1548-1551

  Guilbaud, Romain ^a,b   Butler, Ian B ^a,b   Ellam, Rob M ^b,c  

^a UNIVERSITY OF EDINBURGH   (United Kingdom)

^b SCOTTISH UNIVERSITIES ENVIRONMENTAL RESEARCH CENTRE   (United Kingdom)

^c Edinburgh Research Partnership in Engineering and Mathematics   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

FERRIC ION; FERROUS ION; PYRITE;

IRON; ISOTOPIC FRACTIONATION; METABOLISM; PROTEROZOIC; PYRITE; REDOX CONDITIONS;

ARCHEAN; ARTICLE; FRACTIONATION; MICROBIAL METABOLISM; NONHUMAN; OXIDATION REDUCTION REACTION; PRIORITY JOURNAL; PROTEROZOIC; SEA; SEDIMENT;

BACTERIA; FERRIC COMPOUNDS; FERROUS COMPOUNDS; GEOLOGIC SEDIMENTS; IRON; IRON ISOTOPES; OXIDATION-REDUCTION; SULFIDES;

EID: 79959513214     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1202924     Document Type: Article

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