Bralower, T. J. et al. (1997): High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism; is there a causal link?

Leg/Site/Hole:
ODP 165
ODP 165 1001
ODP 165 999
Identifier:
1997-072417
georefid

10.1130/0091-7613(1997)025<0963:HRROTL>2.3.CO;2
doi

Creator:
Bralower, T. J.
University of North Carolina, Department of Geology, Chapel Hill, NC, United States
author

Thomas, D. J.
University of California at Santa Cruz, Santa Cruz, CA, United States
author

Zachos, J. C.
University of North Carolina, Chapel Hill, NC, United States
author

Hirschmann, M. M.
Bremen University, Bremen, Federal Republic of Germany
author

Roehl, U.
University of Rhode Island, Narragansett, RI, United States
author

Sigurdsson, H.
Wesleyan University, Middletown, CT, United States
author

Thomas, E.
author

Whitney, D. L.
author

Identification:
High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism; is there a causal link?
1997
Geology (Boulder)
Geological Society of America (GSA), Boulder, CO, United States
25
11
963-966
Two recently drilled Caribbean sites contain expanded sedimentary records of the late Paleocene thermal maximum, a dramatic global warming event that occurred at ca. 55 Ma. The records document significant environmental changes, including deep-water oxygen deficiency and a mass extinction of deep-sea fauna, intertwined with evidence for a major episode of explosive volcanism. We postulate that this volcanism initiated a reordering of ocean circulation that resulted in rapid global warming and dramatic changes in the Earth's environment.
English
Serial
Coverage:Geographic coordinates:
North:22.0000
West:-78.4422East: -60.0000
South:9.0000

Stratigraphy; Atlantic Ocean; Caribbean Sea; Cenozoic; clastic rocks; claystone; global change; global warming; high-resolution methods; Leg 165; North Atlantic; Ocean Drilling Program; ODP Site 1001; ODP Site 999; paleo-oceanography; Paleocene; paleocirculation; paleoclimatology; Paleogene; paleotemperature; sedimentary rocks; Tertiary; upper Paleocene; volcaniclastics; volcanism;

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