Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event - Wikidata - wikimedia - TriplyDB

Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

http://www.wikidata.org/entity/Q43530841

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Mechanical instability of monocrystalline and polycrystalline methane hydrates.Fungal decomposition of terrestrial organic matter accelerated Early Jurassic climate warming Jurassic climate mode governed by ocean gateway Effect of a Jurassic oceanic anoxic event on belemnite ecology and evolution Man and the last great wilderness: human impact on the deep sea.Thermodynamic stability of hydrogen clathrates Proliferation of Oberhauserellidae during the recovery following the Late Triassic extinction: paleoecological implications Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis Timescales of methane seepage on the Norwegian margin following collapse of the Scandinavian Ice Sheet Guest-free monolayer clathrate and its coexistence with two-dimensional high-density ice.Astronomical pacing of methane release in the Early Jurassic period.A humid climate state during the Palaeocene/Eocene thermal maximum.Changes in carbon dioxide during an oceanic anoxic event linked to intrusion into Gondwana coals.Palaeoceanography: methane release in the Early Jurassic period.Relation of Phanerozoic stable isotope excursions to climate, bacterial metabolism, and major extinctions.Bacteria and Archaea physically associated with Gulf of Mexico gas hydrates.Global dispersion and local diversification of the methane seep microbiome.'Fish' (Actinopterygii and Elasmobranchii) diversification patterns through deep time.Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event.Marine ecosystem resilience during extreme deoxygenation: the Early Jurassic oceanic anoxic event.Warm tropical ocean surface and global anoxia during the mid-Cretaceous period.Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates.Theoretical insights into nucleation of CO2 and CH4 hydrates for CO2 capture and storage.A hydrothermal origin for isotopically anomalous cap dolostone cements from south China.Carbon isotope ratio analysis of organic moieties from fossil mummified wood: establishing optimum conditions for off-line pyrolysis extraction using gas chromatography/mass spectrometry.Freshwater lake to salt-water sea causing widespread hydrate dissociation in the Black Sea.New insights on the systematics, palaeoecology and palaeobiology of a plesiosaurian with soft tissue preservation from the Toarcian of Holzmaden, Germany.Lepidopteris callipteroides, an earliest Triassic seed fern of the Sydney Basin, southeastern Australia Parasequence development in the Ediacaran Shuram Formation (Nafun Group, Oman): high-resolution stratigraphic test for primary origin of negative carbon isotopic ratios Geochemistry of oceanic anoxic events Thallium isotopes reveal protracted anoxia during the Toarcian (Early Jurassic) associated with volcanism, carbon burial, and mass extinction Modeling evidences for global warming, Arctic seawater freshening, and sluggish oceanic circulation during the Early Toarcian anoxic event Prokaryotic cells of the deep sub-seafloor biosphere identified as living bacteria Drowning of a carbonate platform as a precursor stage of the Early Toarcian global anoxic event (Southern Provence sub-Basin, South-east France)Evidence for major environmental perturbation prior to and during the Toarcian (Early Jurassic) oceanic anoxic event from the Lusitanian Basin, Portugal Microbes, mud and methane: cause and consequence of recurrent Early Jurassic anoxia following the end-Triassic mass extinction Carbon cycle dynamics following the end-Triassic mass extinction: Constraints from pairedδ13Ccarbandδ13Corgrecords Carbon cycle perturbation and stabilization in the wake of the Triassic-Jurassic boundary mass-extinction event The interaction of climate change and methane hydrates New multiproxy record of the Jenkyns Event (also known as the Toarcian Oceanic Anoxic Event) from the Mecsek Mountains (Hungary): Differences, duration and drivers

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P2860

Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

http://www.wikidata.org/entity/Q43530841

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2000 nî lūn-bûn

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2000年の論文

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2000年学术文章

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

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Massive dissociation of gas hydrate during a Jurassic oceanic anoxic event

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Bjerrum CJ

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Farrimond P

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Green OR

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Grocke DR

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P2860

Comparative Earth history and Late Permian mass extinction.

Carbon cycling and chronology of climate warming during the Palaeocene/Eocene transition

Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene

Stratigraphy, paleoceanography, and evolution of Cretaceous Pacific guyots; relics from a greenhouse Earth

The early Toarcian (Early Jurassic) and the Cenomanian–Turonian (Late Cretaceous) mass extinctions: similarities and contrasts

Role of the Bering Strait in controlling North Atlantic ocean circulation and climate

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10.1038/35019044

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6794

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406

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Hugh C. Jenkyns

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2000-07-01T00:00:00Z

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12384316

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