Abiotic Pyrite Formation Produces a Large Fe Isotope Fractionation-Reference-Cited by-同舟云学术

Abiotic Pyrite Formation Produces a Large Fe Isotope Fractionation

Published:2011-06-24 Issue:6037 Volume:332 Page:1548-1551
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Guilbaud Romain¹²,Butler Ian B.¹²,Ellam Rob M.²³

Affiliation:

1. School of Geosciences, University of Edinburgh, Grant Institute, Edinburgh EH9 3JW, UK.

2. Scottish Universities Environmental Research Centre, Rankine Avenue, East Kilbride G75 0QF, UK.

3. ECOSSE (Edinburgh Collaborative of Subsurface Science and Engineering), a Joint Research Institute of the Edinburgh Research Partnership in Engineering and Mathematics, Edinburgh EH9 3JW, UK.

Abstract

Iron isotope signatures may not differentiate abiotic and biological processes in sediments.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference40 articles.

1. Controls on iron-isotope fractionation in organic-rich sediments (Kimmeridge Clay, Upper Jurassic, Southern England)

2. Iron Isotope Constraints on the Archean and Paleoproterozoic Ocean Redox State

3. The effect of early diagenesis on the Fe isotope compositions of porewaters and authigenic minerals in continental margin sediments

4. Equilibrium iron isotope fractionation factors of minerals: Reevaluation from the data of nuclear inelastic resonant X-ray scattering and Mössbauer spectroscopy

5. Fe isotope fractionation on FeS formation in ambient aqueous solution

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