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A new model for atmospheric oxygen over Phanerozoic time
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- Carbon dioxide emissions by rock organic carbon oxidation and the net geochemical carbon budget of the Mackenzie River Basin
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- Supercontinents and the case for Pannotia
- Nature of the sedimentary rock record and its implications for Earth system evolution
- An evaluation of sedimentary molybdenum and iron as proxies for pore fluid paleoredox conditions
- Analysis of gases in fossil amber
- Model based Paleozoic atmospheric oxygen estimates: a revisit to GEOCARBSULF
- Mountain glaciation drives rapid oxidation of rock-bound organic carbon
- Glacial weathering, sulfide oxidation, and global carbon cycle feedbacks
- A model for the decrease in amplitude of carbon isotope excursions across the Phanerozoic
- Tectonic controls on the long-term carbon isotope mass balance
- Metabolic evolution and the self-organization of ecosystems
- A modeling case for high atmospheric oxygen concentrations during the Mesozoic and Cenozoic
- Seawater residence times of some elements of geochemical interest and the salinity of the oceans
- Earliest land plants created modern levels of atmospheric oxygen
- Sufficient oxygen for animal respiration 1,400 million years ago
- Flourishing ocean drives the end-Permian marine mass extinction
- Cretaceous Oceans and Ocean Modeling
- The 'Anthropocene as a ratified unit in the ICS International Chronostratigraphic Chart: fundamental issues that must be addressed by the Task Group
- Dynamic model constraints on oxygen-17 depletion in atmospheric O2 after a snowball Earth
- Sulfur isotopes in coal constrain the evolution of the Phanerozoic sulfur cycle
- Section 6. Deep Time: Modelling of Atmospheric CO2 and the Marine CO2-Carbonic Acid-Carbonate System
- Section 4. Deep Time: Observational Evidence from the Sedimentary Rock Record
- Section 7. Synthesis of Ocean-Atmosphere-Carbonate Sediment Evolution During the Phanerozoic
- From black mud to earth system science: A scientific autobiography
- Mercury (Hg) mineral evolution: A mineralogical record of supercontinent assembly, changing ocean geochemistry, and the emerging terrestrial biosphere
- Section 9. The History of the Iron Biogeochemical Cycle
- Stratigraphic Control on Source-Rock Distribution: First and Second Order Scale
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- SECULAR VARIATIONS IN THE PHANEROZOIC REEF ECOSYSTEM
- ROLE OF TECTONICS IN PHOSPHORUS DISTRIBUTION AND CYCLING
- SILURIAN AND DEVONIAN REEFS: 80 MILLION YEARS OF GLOBAL GREENHOUSE BETWEEN TWO ICE AGES
- VARIATIONS IN THE GLOBAL PHOSPHORUS CYCLE
- THE GLOBAL DIAGENETIC FLUX OF PHOSPHORUS FROM MARINE SEDIMENTS TO THE OCEANS: REDOX SENSITIVITY AND THE CONTROL OF ATMOSPHERIC OXYGEN LEVELS
- The Triassic isotope record
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- Methane and the CH4 related greenhouse effect over the past 400 million years
- Patterns in the Evolution of Nares Size and Secondary Palate Length in Anomodont Therapsids (Synapsida): Implications for Hypoxia as a Cause of End-Permian Tetrapod Extinctions
- Confirmation of Romer's Gap as a low oxygen interval constraining the timing of initial arthropod and vertebrate terrestrialization
- Reply
- Comment: Mesozoic Atmospheric Oxygen: (Comment on "MAGic: A phanerozoic model for the geochemical cycling of major rock-forming components" by Rolf S. Arvidson, Fred T. Mackenzie and Michael Guidry, American Journal of Science, v. 306, p. 135-190.)
- MAGic: A Phanerozoic Model for the Geochemical Cycling of Major Rock-Forming Components
- The Rise of Oxygen over the Past 205 Million Years and the Evolution of Large Placental Mammals
- Massive release of hydrogen sulfide to the surface ocean and atmosphere during intervals of oceanic anoxia
- Seawater Sulfur Isotope Fluctuations in the Cretaceous
- A model for calcium, magnesium and sulfate in seawater over Phanerozoic time
- COPSE: A new model of biogeochemical cycling over Phanerozoic time
- Burning of forest materials under late Paleozoic high atmospheric oxygen levels
- Permian-Triassic boundary interval as a model for forcing marine ecosystem collapse by long-term atmospheric oxygen drop
- A NEW SOFT-BODIED FAUNA: THE PIOCHE FORMATION OF NEVADA
- Cretaceous and Cenozoic evolution of seawater composition, atmospheric O2 and CO2: A model perspective
- Biomineralization and Global Biogeochemical Cycles
- Examination of hypotheses for the Permo-Triassic boundary extinction by carbon cycle modeling
- Fire-prone plant communities and palaeoclimate of a Late Cretaceous fluvial to estuarine environment, Pecinov quarry, Czech Republic
- Biogenic Methane, Hydrogen Escape, and the Irreversible Oxidation of Early Earth
- Hovering Performance of Hummingbirds in Hyperoxic Gas Mixtures
- 14C-Dead Living Biomass: Evidence for Microbial Assimilation of Ancient Organic Carbon During Shale Weathering
- Terrestrial record of methane hydrate dissociation in the Early Cretaceous
- On the Origins of Photosynthesis
- Isotopic Evolution of the Biogeochemical Carbon Cycle During the Precambrian
- Impact of a Permo-Carboniferous high O2 event on the terrestrial carbon cycle
- Isotope Fractionation and Atmospheric Oxygen: Implications for Phanerozoic O2 Evolution
- Global terrestrial productivity in the Mesozoic era
- Atmospheric oxygen over Phanerozoic time
- PALEOCLIMATE:The Sulfur Cycle and Atmospheric Oxygen
- Sulfur Isotopic Composition of Cenozoic Seawater Sulfate
- Biogeochemical Controls and Feedbacks on Ocean Primary Production
- The legacy of Charles Lyell: advances in our knowledge of coal and coal-bearing strata
- Middle to Late Paleozoic Atmospheric CO2 Levels from Soil Carbonate and Organic Matter
- Redox Stabilization of the Atmosphere and Oceans by Phosphorus-Limited Marine Productivity
- Paleozoic Atmospheric CO2: Importance of Solar Radiation and Plant Evolution
- Carbon/sulphur/iron relationships in upwelling sediments
- Examination of hypotheses for the Permo-Triassic boundary extinction by carbon cycle modeling
- Impact of a Permo-Carboniferous high O2 event on the terrestrial carbon cycle
- 14C-Dead Living Biomass: Evidence for Microbial Assimilation of Ancient Organic Carbon During Shale Weathering