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1
|
Iron isotope constraints on the Archean and Paleoproterozoic ocean redox state.
|
Science
|
2005
|
2.86
|
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2
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The evolution of the marine phosphate reservoir.
|
Nature
|
2010
|
1.69
|
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3
|
Widespread iron-rich conditions in the mid-Proterozoic ocean.
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Nature
|
2011
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1.55
|
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4
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Proterozoic ocean redox and biogeochemical stasis.
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Proc Natl Acad Sci U S A
|
2013
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1.54
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5
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Geological constraints on the origin of oxygenic photosynthesis.
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Photosynth Res
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2010
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1.43
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6
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Organic-walled microfossils in 3.2-billion-year-old shallow-marine siliciclastic deposits.
|
Nature
|
2010
|
1.43
|
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7
|
Large colonial organisms with coordinated growth in oxygenated environments 2.1 Gyr ago.
|
Nature
|
2010
|
1.35
|
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8
|
Aerobic bacterial pyrite oxidation and acid rock drainage during the Great Oxidation Event.
|
Nature
|
2011
|
1.29
|
|
9
|
Sulfur record of rising and falling marine oxygen and sulfate levels during the Lomagundi event.
|
Proc Natl Acad Sci U S A
|
2012
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1.10
|
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10
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Deposition of 1.88-billion-year-old iron formations as a consequence of rapid crustal growth.
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Nature
|
2012
|
0.93
|
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11
|
Biological carbon precursor to diagenetic siderite with spherical structures in iron formations.
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Nat Commun
|
2013
|
0.77
|