The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
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Two Antarctic penguin genomes reveal insights into their evolutionary history and molecular changes related to the Antarctic environment.The radish genome and comprehensive gene expression profile of tuberous root formation and developmentKeeping it simple: the value of an irreducibly simple climate modelThermodynamic stability of hydrogen clathratesMethane Hydrates in Quaternary Climate Change: The Clathrate Gun HypothesisWidespread methane seepage along the continental margin off Svalbard - from Bjørnøya to Kongsfjorden.Estimating the potential for twenty-first century sudden climate change.Bacteria and Archaea physically associated with Gulf of Mexico gas hydrates.Microbial communities from methane hydrate-bearing deep marine sediments in a forearc basin.A persistent oxygen anomaly reveals the fate of spilled methane in the deep Gulf of Mexico.Impact ejecta at the Paleocene-Eocene boundary.Apoptosis and the selective survival of host animals following thermal bleaching in zooxanthellate corals.A Palaeogene perspective on climate sensitivity and methane hydrate instability.Methane oxidation by anaerobic archaea for conversion to liquid fuels.Gas hydrates: past and future geohazard?Aerobic and anaerobic methanotrophs in the Black Sea water column.Global change: hydrocarbon-driven warming.Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates.Tertiary giant lacewings (Neuroptera: Polystoechotidae): Revision and description of new taxa from western north America and DenmarkAtmospheric composition, radiative forcing, and climate change as a consequence of a massive methane release from gas hydratesTwo massive, rapid releases of carbon during the onset of the Palaeocene–Eocene thermal maximumSudden spreading of corrosive bottom water during the Palaeocene–Eocene Thermal MaximumEvidence of surface water oligotrophy during the Paleocene-Eocene thermal maximum: Nannofossil assemblage data from Ocean Drilling Program Site 690, Maud Rise, Weddell SeaUncorking the bottle: What triggered the Paleocene/Eocene thermal maximum methane release?Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?The first representative of Tipulomorpha (Diptera) from Early Eocene Cambay amber (India)The extraterrestrial impact evidence at the Palaeocene-Eocene boundary and sequence of environmental change on the continental shelfOn the duration of magnetochrons C24r and C25n and the timing of early Eocene global warming events: Implications from the Ocean Drilling Program Leg 208 Walvis Ridge depth transectAssessing the Past and Future Stability of Global Gas Hydrate ReservoirsInterpreting transient carbonate compensation depth changes by marine sediment core modelingDepth dependency of the Paleocene-Eocene carbon isotope excursion: Paired benthic and terrestrial biomarker records (Ocean Drilling Program Leg 208, Walvis Ridge)Episodes of intensified biological productivity in the subtropical Atlantic Ocean during the termination of the Middle Eocene Climatic Optimum (MECO)Methane Hydrate Instability: A View from the PalaeogeneGas hydrates on the brink
P2860
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P2860
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
description
1999 nî lūn-bûn
@nan
1999 թուականի Նոյեմբերին հրատարակուած գիտական յօդուած
@hyw
1999 թվականի նոյեմբերին հրատարակված գիտական հոդված
@hy
1999年の論文
@ja
1999年論文
@yue
1999年論文
@zh-hant
1999年論文
@zh-hk
1999年論文
@zh-mo
1999年論文
@zh-tw
1999年论文
@wuu
name
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@ast
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@en
type
label
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@ast
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@en
prefLabel
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@ast
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@en
P2093
P1433
P1476
The Source and Fate of Massive Carbon Input During the Latest Paleocene Thermal Maximum.
@en
P2093
P304
P356
10.1126/SCIENCE.286.5444.1531
P407
P577
1999-11-01T00:00:00Z