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Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming

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Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming (English)

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2

James C. Zachos

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Gerald R. Dickens

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3

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Gerald R. Dickens

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Richard E. Zeebe

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1

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Richard E. Zeebe

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language of work or name

English

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publication date

13 July 2009

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published in

Nature Geoscience

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volume

2

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issue

8

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page(s)

576-580

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cites work

An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Atmosphere. An ancient carbon mystery

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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A transient rise in tropical sea surface temperature during the Paleocene-Eocene thermal maximum

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Deep-sea temperature and circulation changes at the Paleocene-Eocene Thermal Maximum

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene Thermal Maximum: Inferences from TEX86 and isotope data

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7 January 2021

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Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Rapid acidification of the ocean during the Paleocene-Eocene thermal maximum

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An alternative age model for the Paleocene–Eocene thermal maximum using extraterrestrial 3He

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Warming the fuel for the fire: Evidence for the thermal dissociation of methane hydrate during the Paleocene-Eocene thermal maximum

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7 January 2021

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Abrupt reversal in ocean overturning during the Palaeocene/Eocene warm period

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7 January 2021

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On the duration of the Paleocene-Eocene thermal maximum (PETM)

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7 January 2021

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

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7 January 2021

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Oceans. Carbon emissions and acidification

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A humid climate state during the Palaeocene/Eocene thermal maximum

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Sedimentary response to Paleocene-Eocene Thermal Maximum carbon release: A model-data comparison

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Possible methane-induced polar warming in the early Eocene

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New chronology for the late Paleocene thermal maximum and its environmental implications

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https://api.crossref.org/works/10.1038%2FNGEO578

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7 January 2021

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Identifiers

DOI

10.1038/NGEO578

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ResearchGate publication ID

242713253

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(Q56017466)

Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming

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