Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedback.
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Eutrophication, microbial-sulfate reduction and mass extinctionsFlourishing ocean drives the end-Permian marine mass extinctionGigantism in unique biogenic magnetite at the Paleocene-Eocene Thermal Maximum.Methane Hydrates in Quaternary Climate Change: The Clathrate Gun HypothesisMarine ecosystem responses to Cenozoic global change.Abrupt reversal in ocean overturning during the Palaeocene/Eocene warm period.Earth system feedback statistically extracted from the Indian Ocean deep-sea sediments recording Eocene hyperthermals.A new family of gymnodont fish (Tetraodontiformes) from the earliest Eocene of the Peri-Tethys (Kabardino-Balkaria, northern Caucasus, Russia)Quantifying export production in the Southern Ocean: Implications for the BaxsproxyAtmospheric composition, radiative forcing, and climate change as a consequence of a massive methane release from gas hydratesCarbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pumpEvidence of surface water oligotrophy during the Paleocene-Eocene thermal maximum: Nannofossil assemblage data from Ocean Drilling Program Site 690, Maud Rise, Weddell SeaCould changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?New palynology-based astronomical and revised 40Ar/39Ar ages for the Eocene maar lake of Messel (Germany)The immediate environmental effects of tephra emissionOn the duration of the Paleocene-Eocene thermal maximum (PETM)Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene-Eocene Thermal MaximumWarm plankton soup and red herrings: calcareous nannoplankton cellular communities and the Palaeocene-Eocene Thermal MaximumVolcanic ash supply to the surface ocean—remote sensing of biological responses and their wider biogeochemical significanceA factorial analysis of the marine carbon cycle and ocean circulation controls on atmospheric CO2An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal MaximumHigh-resolution record of export production in the eastern equatorial Pacific across the Eocene-Oligocene transition and relationships to global climatic recordsNorth American continental margin records of the Paleocene-Eocene thermal maximum: Implications for global carbon and hydrological cyclingAn impulse response function for the “long tail” of excess atmospheric CO2in an Earth system modelRecovering the true size of an Eocene hyperthermal from the marine sedimentary recordA comparison between excess barium and barite as indicators of carbon exportExport productivity and carbonate accumulation in the Pacific Basin at the transition from a greenhouse to icehouse climate (late Eocene to early Oligocene)Paleoredox changes across the Paleocene-Eocene thermal maximum, Walvis Ridge (ODP Sites 1262, 1263, and 1266): Evidence from Mn and U enrichment factorsRapid carbon sequestration at the termination of the Palaeocene–Eocene Thermal MaximumVolcanic Ash versus Mineral Dust: Atmospheric Processing and Environmental and Climate ImpactsOn the Role of Climate Forcing by Volcanic Sulphate and Volcanic Ash
P2860
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P2860
Termination of global warmth at the Palaeocene/Eocene boundary through productivity feedback.
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2000 nî lūn-bûn
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2000 թուականի Սեպտեմբերին հրատարակուած գիտական յօդուած
@hyw
2000 թվականի սեպտեմբերին հրատարակված գիտական հոդված
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2000年の論文
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2000年論文
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2000年論文
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2000年論文
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2000年論文
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2000年論文
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2000年论文
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name
Termination of global warmth a ...... through productivity feedback.
@ast
Termination of global warmth a ...... through productivity feedback.
@en
type
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Termination of global warmth a ...... through productivity feedback.
@ast
Termination of global warmth a ...... through productivity feedback.
@en
prefLabel
Termination of global warmth a ...... through productivity feedback.
@ast
Termination of global warmth a ...... through productivity feedback.
@en
P2093
P356
P1433
P1476
Termination of global warmth a ...... through productivity feedback.
@en
P2093
P2888
P304
P356
10.1038/35025035
P407
P577
2000-09-01T00:00:00Z
P5875
P6179
1020626378