Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
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When did oxygenic photosynthesis evolve?The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean EarthThe paleobiological record of photosynthesisMethane, oxygen, photosynthesis, rubisco and the regulation of the air through timeAtmospheric Prebiotic Chemistry and Organic HazesAtmospheric oxygenation caused by a change in volcanic degassing pressure.Geological sulfur isotopes indicate elevated OCS in the Archean atmosphere, solving faint young sun paradox.The S3- ion is stable in geological fluids at elevated temperatures and pressures.17O excess transfer during the NO2 + O3 → NO3 + O2 reaction.Explaining the structure of the Archean mass-independent sulfur isotope record.Using biogenic sulfur gases as remotely detectable biosignatures on anoxic planetsAtmospheric oxygenation three billion years ago.Atmospheric record in the Hadean Eon from multiple sulfur isotope measurements in Nuvvuagittuq Greenstone Belt (Nunavik, Quebec).Evolutionary ecology during the rise of dioxygen in the Earth's atmosphere.Pathways for Neoarchean pyrite formation constrained by mass-independent sulfur isotopes.Production, preservation, and biological processing of mass-independent sulfur isotope fractionation in the Archean surface environment.The evolution of Photosystem II: insights into the past and future.The recurrent assembly of C4 photosynthesis, an evolutionary tale.Anomalous fractionations of sulfur isotopes during thermochemical sulfate reduction.Extreme 15N-enrichments in 2.72-Gyr-old sediments: evidence for a turning point in the nitrogen cycle.Carbon and sulfur isotopic signatures of ancient life and environment at the microbial scale: Neoarchean shales and carbonates.Decoding Redox Evolution Before Oxygenic Photosynthesis Based on the Sulfur-Mass Independent Fractionation (S-MIF) Record.First-principles C band absorption spectra of SO2 and its isotopologues.Five-S-isotope evidence of two distinct mass-independent sulfur isotope effects and implications for the modern and Archean atmospheresA bistable organic-rich atmosphere on the Neoarchaean EarthExperimental Constraints on Sulphur Behaviour in Subduction Zones: Implications for TTG and Adakite Production and the Global Sulphur Cycle since the ArcheanPlate tectonics caused the demise of banded iron formationsManganese enrichment in the Gowganda Formation of the Huronian Supergroup: A highly oxidizing shallow-marine environment after the last Huronian glaciation
P2860
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P2860
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
description
2007 nî lūn-bûn
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2007年の論文
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2007年学术文章
@wuu
2007年学术文章
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2007年学术文章
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2007年学术文章
@zh-my
2007年学术文章
@zh-sg
2007年學術文章
@yue
2007年學術文章
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2007年學術文章
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name
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@en
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@nl
type
label
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@en
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@nl
prefLabel
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@en
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry.
@nl
P2093
P356
P1433
P1476
Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry
@en
P2093
Alan J Kaufman
Andrew Masterson
Harald Strauss
James Farquhar
Marc Peters
Uwe Wiechert
P2888
P304
P356
10.1038/NATURE06202
P407
P577
2007-10-01T00:00:00Z
P5875
P6179
1047813729
P698
P819
2007Natur.449..706F