Pulse of atmospheric oxygen during the late Cambrian

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Pulse of atmospheric oxygen during the late Cambrian is …
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scholarly articleQ13442814

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P819ADS bibcode2011PNAS..108.3876S
P356DOI10.1073/PNAS.1011836108
P8608Fatcat IDrelease_elhbp6bfirea5kxblsabbk4n3i
P932PMC publication ID3053972
P698PubMed publication ID21368152
P5875ResearchGate publication ID50267140

P50authorLee KumpQ3228900
Bruce RunnegarQ991790
Benjamin C. GillQ43083855
Timothy W. LyonsQ109798074
Matthew R. SaltzmanQ114844235
P2093author name stringSeth A Young
P2860cites workDevonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fishQ24624525
Dynamics of the Neoproterozoic carbon cycleQ24680184
Late-Neoproterozoic deep-ocean oxygenation and the rise of animal lifeQ28278079
Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometryQ28288401
Proterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge?Q29395660
The evolution of modern eukaryotic phytoplanktonQ29617943
Calibrating the Ordovician Radiation of marine life: implications for Phanerozoic diversity trendsQ31007363
The Shifting Balance of Diversity Among Major Marine Animal GroupsQ33683201
Isotope fractionation and atmospheric oxygen: implications for phanerozoic O(2) evolutionQ33891914
The Ordovician Radiation: A Follow-up to the Cambrian Explosion?Q43566509
Origin of planktotrophy--evidence from early molluscs.Q43919607
Geochemical evidence for widespread euxinia in the later Cambrian oceanQ44442073
Association of orogenic activity with the Ordovician radiation of marine lifeQ46370456
Biogeochemical evidence for dinoflagellate ancestors in the early cambrianQ47751503
Biodiversity: past, present, and futureQ47785429
Evolution. Oxygen and evolution.Q52679370
Origination, extinction, and mass depletions of marine diversityQ53954452
Ordovician and Silurian sea–water chemistry, sea level, and climate: A synopsisQ54031687
The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 MaQ55967232
Plankton ecology and the Proterozoic-Phanerozoic transitionQ55970397
Biogeochemical controls on photic-zone euxinia during the end-Permian mass extinctionQ56059850
The Ordovician Biodiversification: revolution in the oceanic trophic chainQ56460449
Effect of Phytoplankton Cell Geometry on Carbon Isotopic FractionationQ56621108
The Great Ordovician Biodiversification Event (GOBE): The palaeoecological dimensionQ56768202
Controls on marine animal biomass through geological timeQ57399754
Macroevolutionary interplay between planktic larvae and benthic predatorsQ58006323
BRYOCARB: A process-based model of thallose liverwort carbon isotope fractionation in response to CO2, O2, light and temperatureQ58071076
Carbon isotope evidence implying high O2/CO2 ratios in the Permo-Carboniferous atmosphereQ58071126
Phosphorus, nitrogen, and the redox evolution of the Paleozoic oceansQ58457903
The SPICE carbon isotope excursion in Siberia: a combined study of the upper Middle Cambrian–lowermost Ordovician Kulyumbe River section, northwestern Siberian PlatformQ59267352
P433issue10
P407language of work or nameEnglishQ1860
P304page(s)3876-3881
P577publication date2011-02-22
P1433published inProceedings of the National Academy of Sciences of the United States of AmericaQ1146531
P1476titlePulse of atmospheric oxygen during the late Cambrian
P478volume108