Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
about
Assessing "dangerous climate change": required reduction of carbon emissions to protect young people, future generations and natureExamination of hypotheses for the Permo-Triassic boundary extinction by carbon cycle modeling.Potential effects of gas hydrate on human welfareIsotopes, ice ages, and terminal Proterozoic earth historyAtmospheric carbon dioxide concentrations over the past 60 million yearsSubtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximumThe geological record of ocean acidificationRelease of methane from a volcanic basin as a mechanism for initial Eocene global warmingTemperature and atmospheric CO2 concentration estimates through the PETM using triple oxygen isotope analysis of mammalian bioapatiteCoccolithophore calcification response to past ocean acidification and climate change.Evidence for a rapid release of carbon at the Paleocene-Eocene thermal maximumClimate sensitivity, sea level and atmospheric carbon dioxideTime-dependent climate sensitivity and the legacy of anthropogenic greenhouse gas emissionsCenozoic climate change and diversification on the continental shelf and slope: evolution of gastropod diversity in the family Solariellidae (Trochoidea)Transient dwarfism of soil fauna during the Paleocene-Eocene Thermal MaximumMethane Hydrates in Quaternary Climate Change: The Clathrate Gun HypothesisTimescales of methane seepage on the Norwegian margin following collapse of the Scandinavian Ice SheetAstronomical pacing of methane release in the Early Jurassic period.Critical issues in trace gas biogeochemistry and global change.Thermogenic methane release as a cause for the long duration of the PETM.Are there pre-Quaternary geological analogues for a future greenhouse warming?A persistent oxygen anomaly reveals the fate of spilled methane in the deep Gulf of Mexico.Past extreme warming events linked to massive carbon release from thawing permafrost.Astronomical pacing of late Palaeocene to early Eocene global warming events.Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary.The global methane cycle: isotopes and mixing ratios, sources and sinks.The Bacteriohopanepolyol Inventory of Novel Aerobic Methane Oxidising Bacteria Reveals New Biomarker Signatures of Aerobic Methanotrophy in Marine Systems.The effect of temperature on organic carbon degradation in marine sedimentsA Palaeogene perspective on climate sensitivity and methane hydrate instability.Very large release of mostly volcanic carbon during the Palaeocene-Eocene Thermal Maximum.Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene.Gas hydrates: past and future geohazard?Reducing uncertainty about carbon dioxide as a climate driver.Earth system feedback statistically extracted from the Indian Ocean deep-sea sediments recording Eocene hyperthermals.Thresholds of catastrophe in the Earth system.Onset of carbon isotope excursion at the Paleocene-Eocene thermal maximum took millennia, not 13 years.Massive dissociation of gas hydrate during a Jurassic oceanic anoxic eventGeochemistry: Bubbles from the deep.Global change: hydrocarbon-driven warming.Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates.
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Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
description
article
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im Dezember 1995 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
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наукова стаття, опублікована в грудні 1995
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ലേഖനം
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name
Dissociation of oceanic methan ...... on at the end of the Paleocene
@en
Dissociation of oceanic methan ...... on at the end of the Paleocene
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type
label
Dissociation of oceanic methan ...... on at the end of the Paleocene
@en
Dissociation of oceanic methan ...... on at the end of the Paleocene
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prefLabel
Dissociation of oceanic methan ...... on at the end of the Paleocene
@en
Dissociation of oceanic methan ...... on at the end of the Paleocene
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P2093
P2860
P356
P1433
P1476
Dissociation of oceanic methan ...... on at the end of the Paleocene
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P2093
David K. Rea
Gerald R. Dickens
James R. O'Neil
Robert M. Owen
P2860
P304
P356
10.1029/95PA02087
P577
1995-12-01T00:00:00Z