Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
about
A whiff of oxygen before the great oxidation event?The role of biology in planetary evolution: cyanobacterial primary production in low-oxygen Proterozoic oceansArsenic stress after the Proterozoic glaciationsBenthic perspective on Earth's oldest evidence for oxygenic photosynthesisHypothesized link between Neoproterozoic greening of the land surface and the establishment of an oxygen-rich atmosphereBioavailability of metal ions and evolutionary adaptationPalaeoproterozoic ice houses and the evolution of oxygen-mediating enzymes: the case for a late origin of photosystem IIAtmospheric oxygenation caused by a change in volcanic degassing pressure.Explaining the structure of the Archean mass-independent sulfur isotope record.The rise of oxygen in Earth's early ocean and atmosphere.Evolutionary ecology during the rise of dioxygen in the Earth's atmosphere.Rapid oxygenation of Earth's atmosphere 2.33 billion years agoAtmospheric oxygen regulation at low Proterozoic levels by incomplete oxidative weathering of sedimentary organic carbon.The evolutionary consequences of oxygenic photosynthesis: a body size perspective.A Zn isotope perspective on the rise of continents.Long-term sedimentary recycling of rare sulphur isotope anomalies.Crown group Oxyphotobacteria postdate the rise of oxygen.Advent of Continents: A New Hypothesis.Redox variations in Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth's oxygenation.Atmospheric oxygenation and volcanism.Oxygen in the evolution of complex life and the price we pay.Zinc starvation response in a cyanobacterium revealed.Statistical geochemistry reveals disruption in secular lithospheric evolution about 2.5 Gyr ago.Earth science: Sea change for the rise of oxygen.A late Archean sulfidic sea stimulated by early oxidative weathering of the continents.A record of deep-ocean dissolved O2 from the oxidation state of iron in submarine basalts.Osmium evidence for synchronicity between a rise in atmospheric oxygen and Palaeoproterozoic deglaciation.Dating phototropic microbial lineages with reticulate gene histories.A non-zircon Hf isotope record in Archean black shales from the Pilbara craton confirms changing crustal dynamics ca. 3 Ga ago.Exoplanet Biosignatures: Understanding Oxygen as a Biosignature in the Context of Its Environment.Earth’s early O2 cycle suppressed by primitive continentsPlate-tectonic evolution of the Earth: bottom-up and top-down mantle circulationExperimental Constraints on Sulphur Behaviour in Subduction Zones: Implications for TTG and Adakite Production and the Global Sulphur Cycle since the ArcheanGaillard et al. replyAtmospheric hydrogen peroxide and Eoarchean iron formationsMicrobiological processes in banded iron formation deposition
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P2860
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
description
2007 nî lūn-bûn
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2007年の論文
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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
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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
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2007年學術文章
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2007年學術文章
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name
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@en
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@nl
type
label
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@en
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@nl
prefLabel
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@en
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@nl
P356
P1433
P1476
Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
@en
P2093
Lee R Kump
Mark E Barley
P2888
P304
P356
10.1038/NATURE06058
P407
P577
2007-08-01T00:00:00Z
P6179
1052127551