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Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary

Author

Listed:
  • Appy Sluijs

    (Palaeoecology, Institute of Environmental Biology, Utrecht University, Laboratory of Palaeobotany and Palynology,)

  • Henk Brinkhuis

    (Palaeoecology, Institute of Environmental Biology, Utrecht University, Laboratory of Palaeobotany and Palynology,)

  • Stefan Schouten

    (Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, 1790 AB, Den Burg, Texel, The Netherlands)

  • Steven M. Bohaty

    (University of California Santa Cruz, Santa Cruz, California 95060, USA)

  • Cédric M. John

    (University of California Santa Cruz, Santa Cruz, California 95060, USA
    Present addresses: Integrated Ocean Drilling Program, Texas A&M University, 1000 Discovery Drive, College Station, Texas 77845, USA (C.M.J.); GNS Science, PO Box 30-368, Lower Hutt, New Zealand (E.M.C.).)

  • James C. Zachos

    (University of California Santa Cruz, Santa Cruz, California 95060, USA)

  • Gert-Jan Reichart

    (Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands)

  • Jaap S. Sinninghe Damsté

    (Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands
    Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, 1790 AB, Den Burg, Texel, The Netherlands)

  • Erica M. Crouch

    (Palaeoecology, Institute of Environmental Biology, Utrecht University, Laboratory of Palaeobotany and Palynology,
    Present addresses: Integrated Ocean Drilling Program, Texas A&M University, 1000 Discovery Drive, College Station, Texas 77845, USA (C.M.J.); GNS Science, PO Box 30-368, Lower Hutt, New Zealand (E.M.C.).)

  • Gerald R. Dickens

    (Rice University, 6100 Main Street, Houston, Texas 77005, USA)

Abstract

Early warming signs The Palaeocene/Eocene thermal maximum — a period of intense global warming about 55 million years ago — was associated with a massive release of isotopically distinctive greenhouse gases into the ocean-atmosphere system. It remains unclear, however, whether this input caused or resulted from the global warming and environmental change that characterize the event. Sluijs et al. use high-resolution records of environmental change across the Palaeocene/Eocene boundary from two sediment sections in New Jersey to shed light on this question. They find that the onset of environmental change and surface-ocean warming preceded the input of greenhouse gases by several thousand years at this location. This sequence of events is consistent with the proposal that deep-ocean warming caused the dissociation of submarine gas hydrates, releasing massive amounts of the greenhouse gas methane. But the cause of the early warming remains uncertain.

Suggested Citation

  • Appy Sluijs & Henk Brinkhuis & Stefan Schouten & Steven M. Bohaty & Cédric M. John & James C. Zachos & Gert-Jan Reichart & Jaap S. Sinninghe Damsté & Erica M. Crouch & Gerald R. Dickens, 2007. "Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary," Nature, Nature, vol. 450(7173), pages 1218-1221, December.
  • Handle: RePEc:nat:nature:v:450:y:2007:i:7173:d:10.1038_nature06400
    DOI: 10.1038/nature06400
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    Cited by:

    1. Mingsong Li & Timothy J. Bralower & Lee R. Kump & Jean M. Self-Trail & James C. Zachos & William D. Rush & Marci M. Robinson, 2022. "Astrochronology of the Paleocene-Eocene Thermal Maximum on the Atlantic Coastal Plain," Nature Communications, Nature, vol. 13(1), pages 1-13, December.

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