Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?
- 10 May 2002
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 17 (2)
- https://doi.org/10.1029/2001pa000678
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- Uncorking the bottle: What triggered the Paleocene/Eocene thermal maximum methane release?Paleoceanography and Paleoclimatology, 2001
- Numerical evidence against reversed thermohaline circulation in the warm Paleocene/Eocene oceanJournal of Geophysical Research: Oceans, 2001
- An osmium isotope excursion associated with the Late Paleocene thermal maximum: Evidence of intensified chemical weatheringPaleoceanography and Paleoclimatology, 2001
- Stratigraphic and climatic implications of clay mineral changes around the Paleocene/Eocene boundary of the northeastern US marginPublished by Elsevier ,2000
- High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: Is there a causal link?Geology, 1997
- Latest Paleocene benthic foraminiferal extinction and environmental changes at Tawanui, New ZealandPaleoceanography and Paleoclimatology, 1996
- Dynamic support by the Icelandic plume and vertical tectonics of the northeast Atlantic continental marginsJournal of Geophysical Research, 1995
- Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the PaleocenePaleoceanography and Paleoclimatology, 1995
- Abrupt Climate Change and Transient Climates during the Paleogene: A Marine PerspectiveThe Journal of Geology, 1993
- Multiple Equilibria of the Global Thermohaline CirculationJournal of Physical Oceanography, 1991