High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: Is there a causal link?: Reply

Geology

Volumn 26, Issue 7, 1998, Pages 671-

  Bralower, Timothy J ^a   Thomas, Deborah J ^a   Thomas, Ellen ^b   Zachos, James C ^c  

^a UNIVERSITY OF NORTH CAROLINA   (United States)

^b WESLEYAN UNIVERSITY   (United States)

^c UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

GEOLOGICAL RECORD; HYPSITHERMAL; PALEOCENE; SPATIAL RESOLUTION; TEMPERATURE ANOMALY; VOLCANISM;

ATLANTIC OCEAN; CARIBBEAN SEA;

EID: 0000537141     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/0091-7613(1997)025<0963:HRROTL>2.3.CO;2     Document Type: Letter

References (9)

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2. Dickens, G. R., O'Neil, J. R., Rea, D. K., and Owen, R. M., 1995, Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene: Paleoceanography, v. 10, p. 965-971.
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7. Robert, C., and Kennett, J. P., 1994, Antarctic subtropical humid episode at the Paleocene-Eocene boundary: Clay mineral evidence: Geology, v. 22, p. 211-214.
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9. Thomas, E., Zachos, J. C., and Bralower, T. J., in press, Deep-sea environments on a warm earth: Latest Paleocene to early Eocene, in Huber, B. T., MacLeod, K.G., and Wing, S. L., eds., Warm climates in Earth history: Cambridge, Cambridge University Press(26[7]).