An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago

Weiqiang Li, Andrew D. Czaja, Martin Van Kranendonk, Brian L. Beard, Eric E. Roden, Clark M. Johnson

Research output: Contribution to journalArticle

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Abstract

The oxidation state of the atmosphere and oceans on the early Earth remains controversial. Although it is accepted by many workers that the Archean atmosphere and ocean were anoxic, hematite in the 3.46 billion-year-old (Ga) Marble Bar Chert (MBC) from Pilbara Craton, NW Australia has figured prominently in arguments that the Paleoarchean atmosphere and ocean was fully oxygenated. In this study, we report the Fe isotope compositions and U concentrations of the MBC, and show that the samples have extreme heavy Fe isotope enrichment, where δ56Fe values range between +1.5‰ and +2.6‰, the highest δ56Fe values for bulk samples yet reported. The high δ56Fe values of the MBC require very low levels of oxidation and, in addition, point to a Paleoarchean ocean that had high aqueous Fe(II) contents. A dispersion/reaction model indicates that O2 contents in the photic zone of the ocean were less than 10-3μM, which suggests that the ocean was essentially anoxic. An independent test of anoxic conditions is provided by U-Th-Pb isotope systematics, which show that U contents in the Paleoarchean ocean were likely below 0.02ppb, two orders-of-magnitude lower than the modern ocean. Collectively, the Fe and U data indicate a reduced, Fe(II)-rich, U-poor environment in the Archean oceans at 3.46 billion years ago. Given the evidence for photosynthetic communities provided by broadly coeval stromatolites, these results suggests that an important photosynthetic pathway in the Paleoarchean oceans may have been anoxygenic photosynthetic Fe(II) oxidation.

Original languageEnglish
Pages (from-to)65-79
Number of pages15
JournalGeochimica et Cosmochimica Acta
Volume120
DOIs
Publication statusPublished - Nov 1 2013
Externally publishedYes

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Calcium Carbonate
Isotopes
Oxidation
ocean
chert
marble
Earth (planet)
isotope
oxidation
atmosphere
Archean
Chemical analysis
early Earth
photic zone
anoxic conditions
hematite
craton

ASJC Scopus subject areas

  • Geochemistry and Petrology

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An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago. / Li, Weiqiang; Czaja, Andrew D.; Van Kranendonk, Martin; Beard, Brian L.; Roden, Eric E.; Johnson, Clark M.

In: Geochimica et Cosmochimica Acta, Vol. 120, 01.11.2013, p. 65-79.

Research output: Contribution to journalArticle

Li, Weiqiang ; Czaja, Andrew D. ; Van Kranendonk, Martin ; Beard, Brian L. ; Roden, Eric E. ; Johnson, Clark M. / An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago. In: Geochimica et Cosmochimica Acta. 2013 ; Vol. 120. pp. 65-79.
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