Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
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The Anthropocene is functionally and stratigraphically distinct from the HoloceneThe geological record of ocean acidificationTemperature and atmospheric CO2 concentration estimates through the PETM using triple oxygen isotope analysis of mammalian bioapatiteConsequences of elevated temperature and pCO2 on insect folivory at the ecosystem level: perspectives from the fossil recordEvidence for a rapid release of carbon at the Paleocene-Eocene thermal maximumCenozoic mean greenhouse gases and temperature changes with reference to the Anthropocene.Evolution of the earliest horses driven by climate change in the Paleocene-Eocene Thermal Maximum.Impact ejecta at the Paleocene-Eocene boundary.Maximum rates of climate change are systematically underestimated in the geological recordEarth's oxygen cycle and the evolution of animal lifeExtreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum.Very large release of mostly volcanic carbon during the Palaeocene-Eocene Thermal Maximum.A probabilistic assessment of the rapidity of PETM onset.Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene.Constraining shifts in North Atlantic plate motions during the Palaeocene by U-Pb dating of Svalbard tephra layers.Palaeoclimate: Volcanism caused ancient global warming.Geochemistry: Bubbles from the deep.Two massive, rapid releases of carbon during the onset of the Palaeocene–Eocene thermal maximumSudden spreading of corrosive bottom water during the Palaeocene–Eocene Thermal MaximumDeep time evidence for climate sensitivity increase with warmingThe Anthropocene: a comparison with the Ordovician–Silurian boundaryA middle Eocene carbon cycle conundrumAssessing offsets between theδ13C of sedimentary components and the global exogenic carbon pool across early Paleogene carbon cycle perturbationsConstraints on hyperthermalsAn 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 recordReply to 'Constraints on hyperthermals'Integrated stratigraphy of the Paleocene-Eocene thermal maximum in the New Jersey Coastal Plain: Toward understanding the effects of global warming in a shelf environmentChemostratigraphic implications of spatial variation in the Paleocene-Eocene Thermal Maximum carbon isotope excursion, SE Bighorn Basin, WyomingImplementation of methane cycling for deep-time global warming simulations with the DCESS Earth system model (version 1.2)The Paleocene-Eocene Thermal Maximum: How much carbon is enough?
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Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
description
im Juni 2011 veröffentlichter wissenschaftlicher Artikel
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в червні 2011
@uk
name
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
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Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
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type
label
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
@en
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
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prefLabel
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
@en
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
@nl
P2093
P2860
P356
P1433
P1476
Slow release of fossil carbon during the Palaeocene–Eocene Thermal Maximum
@en
P2093
Aaron F. Diefendorf
Adam J. Charles
Andy J. Ridgwell
Christopher K. Junium
Ian C. Harding
Lee R. Kump
Nathan M. Urban
P2860
P2888
P304
P356
10.1038/NGEO1179
P407
P577
2011-06-05T00:00:00Z