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PALEOCEANOGRAPHY, VOL. 16, NO. 6, PAGES 549–562, 2001

Uncorking the Bottle: What Triggered the Paleocene/Eocene Thermal Maximum Methane Release?

Miriam E. Katz

Department of Geological Sciences, Rutgers University, Piscataway, New Jersey, USA.


Benjamin S. Cramer

Department of Geological Sciences, Rutgers University, Piscataway, New Jersey, USA.


Gregory S. Mountain

Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA.


Samuel Katz

Department of Earth and Environment Science, Rensselaer Polytechnic Institute, Troy, New York, USA.


Kenneth G. Miller

Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA.


Abstract

The Paleocene/Eocene thermal maximum (PETM) was a time of rapid global warming in both marine and continental realms that has been attributed to a massive methane (CH4) release from marine gas hydrate reservoirs. Previously proposed mechanisms for this methane release rely on a change in deepwater source region(s) to increase water temperatures rapidly enough to trigger the massive thermal dissociation of gas hydrate reservoirs beneath the seafloor. To establish constraints on thermal dissociation, we model heat flow through the sediment column and show the effect of the temperature change on the gas hydrate stability zone through time. In addition, we provide seismic evidence tied to borehole data for methane release along portions of the U.S. continental slope; the release sites are proximal to a buried Mesozoic reef front. Our model results, release site locations, published isotopic records, and ocean circulation models neither confirm nor refute thermal dissociation as the trigger for the PETM methane release. In the absence of definitive evidence to confirm thermal dissociation, we investigate an alternative hypothesis in which continental slope failure resulted in a catastrophic methane release. Seismic and isotopic evidence indicates that Antarctic source deepwater circulation and seafloor erosion caused slope retreat along the western margins of the North Atlantic in the late Paleocene. Continued erosion or seismic activity along the oversteepened continental margin may have allowed methane to escape from gas reservoirs trapped between the frozen hydrate-bearing sediments and the underlying buried Mesozoic reef front, precipitating the Paleocene/Eocene boundary methane release. An important implication of this scenario is that the methane release caused (rather than resulted from) the transient temperature increase of the PETM. Neither thermal dissociation nor mechanical disruption of sediments can be identified unequivocally as the triggering mechanism for methane release with existing data. Further documentation with high-resolution benthic foraminiferal isotopic records and with seismic profiles tied to borehole data is needed to clarify whether erosion, thermal dissociation, or a combination of these two was the triggering mechanism for the PETM methane release.

Received 7 December 2000; accepted 31 August 2001.

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Citation: Katz, M. E., B. S. Cramer, G. S. Mountain, S. Katz, and K. G. Miller (2001), Uncorking the Bottle: What Triggered the Paleocene/Eocene Thermal Maximum Methane Release?, Paleoceanography, 16(6), 549–562.