Edinburgh Research Explorer

Abiotic Pyrite Formation Produces a Large Fe Isotope Fractionation

Research output: Contribution to journalArticle

Related Edinburgh Organisations

Open Access permissions

Open

Documents

  • Download as Adobe PDF

    Rights statement: This is the author's version as submitted for publication following peer-review. The final version was published by the American Association for the Advancement of Science (2012).

    Accepted author manuscript, 968 KB, PDF-document

Original languageEnglish
Pages (from-to)1548-1551
Number of pages4
JournalScience
Volume332
Issue number6037
DOIs
Publication statusPublished - 24 Jun 2011

Abstract

The iron isotope composition of sedimentary pyrite has been proposed as a potential proxy to trace microbial metabolism and the redox evolution of the oceans. We demonstrate that Fe isotope fractionation accompanies abiotic pyrite formation in the absence of Fe(II) redox change. Combined fractionation factors between Fe(II)(aq), mackinawite, and pyrite permit the generation of pyrite with Fe isotope signatures that nearly encapsulate the full range of sedimentary delta Fe-56(pyrite) recorded in Archean to modern sediments. We propose that Archean negative Fe isotope excursions reflect partial Fe(II)(aq) utilization during abiotic pyrite formation rather than microbial dissimilatory Fe(III) reduction. Late Proterozoic to modern sediments may reflect greater Fe(II)(aq) utilization and variations in source composition.

Download statistics

No data available

ID: 2319871