scholarly article | Q13442814 |
P819 | ADS bibcode | 2011PNAS..108.3876S |
P356 | DOI | 10.1073/PNAS.1011836108 |
P8608 | Fatcat ID | release_elhbp6bfirea5kxblsabbk4n3i |
P932 | PMC publication ID | 3053972 |
P698 | PubMed publication ID | 21368152 |
P5875 | ResearchGate publication ID | 50267140 |
P50 | author | Lee Kump | Q3228900 |
Bruce Runnegar | Q991790 | ||
Benjamin C. Gill | Q43083855 | ||
Timothy W. Lyons | Q109798074 | ||
Matthew R. Saltzman | Q114844235 | ||
P2093 | author name string | Seth A Young | |
P2860 | cites work | Devonian rise in atmospheric oxygen correlated to the radiations of terrestrial plants and large predatory fish | Q24624525 |
Dynamics of the Neoproterozoic carbon cycle | Q24680184 | ||
Late-Neoproterozoic deep-ocean oxygenation and the rise of animal life | Q28278079 | ||
Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry | Q28288401 | ||
Proterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge? | Q29395660 | ||
The evolution of modern eukaryotic phytoplankton | Q29617943 | ||
Calibrating the Ordovician Radiation of marine life: implications for Phanerozoic diversity trends | Q31007363 | ||
The Shifting Balance of Diversity Among Major Marine Animal Groups | Q33683201 | ||
Isotope fractionation and atmospheric oxygen: implications for phanerozoic O(2) evolution | Q33891914 | ||
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 ocean | Q44442073 | ||
Association of orogenic activity with the Ordovician radiation of marine life | Q46370456 | ||
Biogeochemical evidence for dinoflagellate ancestors in the early cambrian | Q47751503 | ||
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The abundance of 13C in marine organic matter and isotopic fractionation in the global biogeochemical cycle of carbon during the past 800 Ma | Q55967232 | ||
Plankton ecology and the Proterozoic-Phanerozoic transition | Q55970397 | ||
Biogeochemical controls on photic-zone euxinia during the end-Permian mass extinction | Q56059850 | ||
The Ordovician Biodiversification: revolution in the oceanic trophic chain | Q56460449 | ||
Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation | Q56621108 | ||
The Great Ordovician Biodiversification Event (GOBE): The palaeoecological dimension | Q56768202 | ||
Controls on marine animal biomass through geological time | Q57399754 | ||
Macroevolutionary interplay between planktic larvae and benthic predators | Q58006323 | ||
BRYOCARB: A process-based model of thallose liverwort carbon isotope fractionation in response to CO2, O2, light and temperature | Q58071076 | ||
Carbon isotope evidence implying high O2/CO2 ratios in the Permo-Carboniferous atmosphere | Q58071126 | ||
Phosphorus, nitrogen, and the redox evolution of the Paleozoic oceans | Q58457903 | ||
The SPICE carbon isotope excursion in Siberia: a combined study of the upper Middle Cambrian–lowermost Ordovician Kulyumbe River section, northwestern Siberian Platform | Q59267352 | ||
P433 | issue | 10 | |
P407 | language of work or name | English | Q1860 |
P304 | page(s) | 3876-3881 | |
P577 | publication date | 2011-02-22 | |
P1433 | published in | Proceedings of the National Academy of Sciences of the United States of America | Q1146531 |
P1476 | title | Pulse of atmospheric oxygen during the late Cambrian | |
P478 | volume | 108 |