Long-term sedimentary recycling of rare sulphur isotope anomalies
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作者:
Reinhard, Christopher T.
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CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USACALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
Reinhard, Christopher T.
[1
,2
]
Planavsky, Noah J.
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CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USACALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
Planavsky, Noah J.
[1
,2
]
Lyons, Timothy W.
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Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USACALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
Lyons, Timothy W.
[2
]
机构:
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91126 USA
[2] Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA
The accumulation of substantial quantities of O-2 in the atmosphere has come to control the chemistry and ecological structure of Earth's surface. Non-mass-dependent (NMD) sulphur isotope anomalies in the rock record(1) are the central tool used to reconstruct the redox history of the early atmosphere. The generation and initial delivery of these anomalies to marine sediments requires low partial pressures of atmospheric O-2 (p(O2); refs 2, 3), and the disappearance of NMD anomalies from the rock record 2.32 billion years ago(1,4) is thought to have signalled a departure from persistently low atmospheric oxygen levels (less than about 10(-5) times the present atmospheric level) during approximately the first two billion years of Earth's history. Here we present a model study designed to describe the long-term surface recycling of crustal NMD anomalies, and show that the record of this geochemical signal is likely to display a 'crustalmemory effect' following increases in atmospheric p(O2) above this threshold. Once NMD anomalies have been buried in the upper crust they are extremely resistant to removal, and can be erased only through successive cycles of weathering, dilution and burial on an oxygenated Earth surface. This recycling results in the residual incorporation ofNMDanomalies into the sedimentary record long after synchronous atmospheric generation of the isotopic signal has ceased, with dynamic and measurable signals probably surviving for as long as 10-100 million years subsequent to an increase in atmospheric p(O2) to more than 10(-5) times the present atmospheric level. Our results can reconcile geochemical evidence for oxygen production and transient accumulation with the maintenance of NMD anomalies on the early Earth(5-8), and suggest that future work should investigate the notion that temporally continuous generation of new NMD sulphur isotope anomalies in the atmosphere was likely to have ceased long before their ultimate disappearance from the rock record.
机构:
Stockholm Univ, Balt Sea Ctr, S-10691 Stockholm, Sweden
Stockholm Univ, Dept Environm Sci & Analyt Chem, S-10691 Stockholm, Sweden
Univ Helsinki, Tvarminne Zool Stn, JA Palmenin Tie 260, Hango 10900, FinlandStockholm Univ, Balt Sea Ctr, Balt Nest Inst, S-10691 Stockholm, Sweden
Humborg, Christoph
Slomp, Caroline P.
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Univ Utrecht, Dept Earth Sci, Geochem, POB 80-021, NL-3508 TA Utrecht, NetherlandsStockholm Univ, Balt Sea Ctr, Balt Nest Inst, S-10691 Stockholm, Sweden
Slomp, Caroline P.
Gustafsson, Bo G.
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Stockholm Univ, Balt Sea Ctr, Balt Nest Inst, S-10691 Stockholm, Sweden
Univ Helsinki, Tvarminne Zool Stn, JA Palmenin Tie 260, Hango 10900, FinlandStockholm Univ, Balt Sea Ctr, Balt Nest Inst, S-10691 Stockholm, Sweden
机构:
Univ Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Capo, Eric
Debroas, Didier
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Univ Blaise Pascal, Univ Clermont Auvergne, Lab Microorganismes Genome & Environm, BP 10448, F-63000 Clermont Ferrand, France
CNRS, UMR 6023, LMGE, Campus Univ Cezeaux, F-63171 Aubiere, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Debroas, Didier
Arnaud, Fabien
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Univ Savoie Mt Blanc, CNRS, UMR 5204, EDYTEM, 5 Blvd Mer Caspienne, F-73376 Le Bourget Du Lac, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Arnaud, Fabien
Guillemot, Typhaine
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Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR 6249, CNRS, 16 Route Gray, F-25000 Besancon, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Guillemot, Typhaine
Bichet, Vincent
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Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR 6249, CNRS, 16 Route Gray, F-25000 Besancon, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Bichet, Vincent
Millet, Laurent
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Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR 6249, CNRS, 16 Route Gray, F-25000 Besancon, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Millet, Laurent
Gauthier, Emilie
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Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR 6249, CNRS, 16 Route Gray, F-25000 Besancon, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Gauthier, Emilie
Massa, Charly
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Univ Bourgogne Franche Comte, Lab Chronoenvironm, UMR 6249, CNRS, 16 Route Gray, F-25000 Besancon, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Massa, Charly
Develle, Anne-Lise
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Univ Savoie Mt Blanc, CNRS, UMR 5204, EDYTEM, 5 Blvd Mer Caspienne, F-73376 Le Bourget Du Lac, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France
Develle, Anne-Lise
Pignol, Cecile
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Univ Savoie Mt Blanc, CNRS, UMR 5204, EDYTEM, 5 Blvd Mer Caspienne, F-73376 Le Bourget Du Lac, FranceUniv Savoie Mt Blanc, CARRTEL, INRA, F-74200 Thonon Les Bains, France