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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