Abstract
Many independent lines of evidence document a large increase in the Earth's surface oxidation state 2,400 to 2,200 million years ago1,2,3,4, and a second biospheric oxygenation 800 to 580 million years ago, just before large animals appear in the fossil record5,6. Such a two-staged oxidation implies a unique ocean chemistry for much of the Proterozoic eon, which would have been neither completely anoxic and iron-rich as hypothesized for Archaean seas, nor fully oxic as supposed for most of the Phanerozoic eon7. The redox chemistry of Proterozoic oceans has important implications for evolution8, but empirical constraints on competing environmental models are scarce. Here we present an analysis of the iron chemistry of shales deposited in the marine Roper Basin, Australia, between about 1,500 and 1,400 million years ago, which record deep-water anoxia beneath oxidized surface water. The sulphur isotopic compositions of pyrites in the shales show strong variations along a palaeodepth gradient, indicating low sulphate concentrations in mid-Proterozoic oceans. Our data help to integrate a growing body of evidence favouring a long-lived intermediate state of the oceans, generated by the early Proterozoic oxygen revolution and terminated by the environmental transformation late in the Proterozoic eon.
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References
Holland, H. D. in Early Life on Earth (ed. Bengtson, S.) 237–244 (Columbia Univ. Press, New York, 1994)
Farquhar, J., Bao, H. & Thiemans, M. H. Atmospheric influence of the Earth's earliest sulphur cycle. Science 289, 756–758 (2000)
Canfield, D. E., Habicht, K. S. & Thamdrup, B. The Archean sulfur cycle and the early history of atmospheric oxygen. Science 288, 658–661 (2000)
Des Marais, D. J., Strauss, H., Summons, R. E. & Hayes, J. M. Carbon isotopic evidence for the stepwise oxidation of the Precambrian environment. Nature 359, 605–609 (1992)
Derry, L. A., Kaufman, A. J. & Jacobsen, S. B. Sedimentary cycling and environmental change in the late Proterozoic: evidence from stable and radiogenic isotopes. Geochim. Cosmochim. Acta 56, 1317–1329 (1992)
Canfield, D. E. & Teske, A. Late Proterozoic rise in atmospheric oxygen concentrations inferred from phylogenetic and stable-isotope studies. Nature 382, 127–132 (1996)
Canfield, D. E. A new model for Proterozoic ocean chemistry. Nature 396, 450–453 (1998)
Anbar, A. D. & Knoll, A. H. Proterozoic ocean chemistry and evolution: A bioinorganic bridge? Science 297, 1137–1142 (2002)
Abbott, S. T. & Sweet, I. P. Tectonic control on third-order sequences in a siliciclastic ramp-style basin: an example from the Roper Superbasin (Mesoproterozoic), northern Australia. Aust. J. Earth Sci. 47, 637–657 (2000)
Raiswell, R. & Canfield, D. E. Sources of iron for pyrite formation in marine sediments. Am. J. Sci. 298, 219–245 (1998)
Raiswell, R., Newton, R. & Wignall, P. B. An indicator of water-column anoxia: resolution of biofacies variations in the Kimmeridge clay (upper Jurassic, U.K.). J. Sedim. Res. 71, 286–294 (2001)
Shen, Y., Canfield, D. E. & Knoll, A. H. Middle Proterozoic ocean chemistry: Evidence from the McArthur Basin, northern Australia. Am. J. Sci. 302, 81–109 (2002)
Wijsman, J. W. M., Middelburg, J. J., Herman, P. M. J., Böttcher, M. E. & Heip, C. H. R. Sulfur and iron speciation in surface sediments along the northwestern margin of the Black Sea. Mar. Chem. 74, 261–278 (2001)
Jackson, M. J. & Raiswell, R. Sedimentology and carbon-sulphur geochemistry of the Velkerri Formation, a mid-Proterozoic potential oil source in northern Australia. Precambr. Res. 54, 81–108 (1991)
Hayes, J. M., Lambert, I. B. & Strauss, H. in The Proterozoic Biosphere: A Multidisciplinary Study (eds Schopf, J. W. & Klein, C.) 129–134 (Cambridge Univ. Press, Cambridge, 1992)
Canfield, D. E. & Raiswell, R. The evolution of the sulfur cycle. Am. J. Sci. 299, 697–723 (1999)
Muir, M. D., Donnelly, T. H., Wilkins, R. W. T. & Armstrong, K. J. Stable isotope, petrological, and fluid inclusion studies of minor mineral deposits from the McArthur Basin: implications for the genesis of some sediment-hosted base metal mineralization from the Northern Territory. Aust. J. Earth Sci. 32, 239–260 (1985)
Zaback, D. A., Pratt, L. M. & Hayes, J. M. Transport and reduction of sulfate and immobilization of sulfide in marine black shales. Geology 21, 141–144 (1993)
Donnelly, T. H. & Crick, I. H. Depositional environment of the middle Proterozoic Velkerri Formation in northern Australia: geochemical evidence. Precambr. Res. 42, 165–172 (1988)
Lyons, T. W. Sulfur isotopic trends and pathways of iron sulphide formation in upper Holocene sediments of the anoxic Black Sea. Geochim. Cosmochim. Acta 61, 3367–3382 (1997)
Gautier, D. Cretaceous shales from the western interior of North America: sulfur/carbon ratios and sulfur isotope composition. Geology 14, 225–228 (1986)
Logan, G. A., Hayes, J. M., Hieshima, G. B. & Summons, R. E. Terminal Proterozoic reorganization of biogeochemical cycles. Nature 376, 53–56 (1995)
Lyons, T. W., Luepke, J. J., Schreiber, M. E. & Zeig, G. A. Sulfur geochemical constraints on Mesoproterozoic restricted marine deposition: lower Belt Supergroup, northwestern United States. Geochim. Cosmochim. Acta 64, 427–437 (2000)
Strauss, H. & Schieber, J. A sulfur isotope study of pyrite genesis: The Mid-Proterozoic Newland Formation, Belt Supergroup, Montana. Geochim Cosmochim Acta 54, 197–204 (1990)
Kah, L. C., Lyons, T. W. & Chesley, J. T. Geochemistry of a 1.2 Ga carbonate-evaporite succession, northern Baffin and Bylot Islands: implications for Mesoproterozoic marine evolution. Precambr. Res. 111, 203–234 (2001)
Hurtgen, M. T., Arthur, M. A., Suits, N. S. & Kaufman, A. J. The sulfur isotopic composition of Neoproterozoic seawater sulfate: implications for a snowball Earth? Earth Planet. Sci. Lett. 203, 413–429 (2002)
Pavlov, A. A., Hurtgen, M. T., Kasting, J. F. & Arthur, M. A. Methane-rich Proterozoic atmosphere? Geology 31, 87–90 (2003)
Baker, P. A. & Kastner, M. Constraints on the formation of sedimentary dolomite. Science 213, 214–216 (1981)
Knoll, A. H. & Carroll, S. B. Early animal evolution: emerging views from comparative biology and geology. Science 284, 2129–2137 (1999)
Ross, G. M., Bloch, J. D. & Krouse, H. R. Neoproterozoic strata of the southern Canadian Cordillera and the isotopic evolution of seawater sulfate. Precambr. Res. 73, 71–99 (1995)
Acknowledgements
We thank A. Bauer and J. Brocks for help in sample collection, J. Fong and L. Liu for help with geochemical analysis, J. Payne for help with statistics, and D. Canfield, J. Hayes, M. Hurtgen, T. Lyons and G. Ross for comments and suggestions. This study was supported by an NRC Research Associateship (Y.S.), the NASA Exobiology programme, the Astrobiology Institute, Macquarie University, and the Australian Research Council.
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Shen, Y., Knoll, A. & Walter, M. Evidence for low sulphate and anoxia in a mid-Proterozoic marine basin. Nature 423, 632–635 (2003). https://doi.org/10.1038/nature01651
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DOI: https://doi.org/10.1038/nature01651
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