Schmidt, Gavin A. and Shindell, Drew T. (2003): Atmospheric composition, radiative forcing, and climate change as a consequence of a massive methane release from gas hydrates

Leg/Site/Hole:
ODP 113
ODP 143
ODP 171B
ODP 171B 1051
ODP 113 690
ODP 143 865
Identifier:
2003-051840
georefid

10.1029/2002PA000757
doi

Creator:
Schmidt, Gavin A.
NASA, Goddard Institute for Space Studies, New York, NY, United States
author

Shindell, Drew T.
author

Identification:
Atmospheric composition, radiative forcing, and climate change as a consequence of a massive methane release from gas hydrates
2003
Paleoceanography
American Geophysical Union, Washington, DC, United States
18
1
4.1-4.9
The massive perturbation to global climate and the carbon cycle during the Paleocene/Eocene Thermal Maximum (PETM) may have been forced by a catastrophic release of methane gas (CH (sub 4) ) from hydrate deposits on the continental slope. We investigate whether reported PETM paleotemperature and paleo-CO (sub 2) proxies are consistent with this hypothesis by considering the impact of large increases in CH (sub 4) emissions to the atmosphere. Significant effects on atmospheric chemistry and CH (sub 4) lifetime are seen for a range of plausible emission rates. (modified journ. abstr.)
English
Coverage:Geographic coordinates:
North:30.0311
West:-179.3321East: 1.1218
South:-65.0938

Stratigraphy; aliphatic hydrocarbons; alkanes; Atlantic Ocean; atmosphere; Cenozoic; climate change; cores; Eocene; Foraminifera; gas hydrates; general circulation models; hydrocarbons; Invertebrata; Leg 113; Leg 143; Leg 171B; lower Eocene; methane; microfossils; numerical models; Ocean Drilling Program; ODP Site 1051; ODP Site 690; ODP Site 865; organic compounds; Pacific Ocean; paleo-oceanography; Paleocene; paleoclimatology; paleoenvironment; Paleogene; paleotemperature; Protista; Southern Ocean; Tertiary; upper Paleocene;

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