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Leg 199 summary

By J. Backman, W.H. Busch, H.K. Coxall, K. Faul, P.A. Gaillot, S.A. Hovan, T.R. Janecek, P. Knoop, S. Kruse, L. Lanci, C.H. Lear, M. Lyle, T.C. Moore, C.A. Nigrini, H. Nishi, R. Nomura, R.D. Norris, H. Pälike, J.M. Parés, L. Quintin, I. Raffi, B.R. Rea, D.K. Rea, T.H. Steiger, A.K. Tripati, M.D. Vanden Berg, B.S. Wade and P.A. Wilson


Ocean Drilling Program (ODP) Leg 199, "The Paleogene Equatorial Transect" (Sites 1215-1222), was designed to study the evolution of the equatorial Pacific current and wind system as Earth went from maximum Cenozoic warmth to initial Antarctic glaciations. The drilling program was primarily devoted to a transect along the 56- to 57-Ma crust, old enough to capture the Paleocene/Eocene boundary in the basal, more carbonate-rich sediments. The Leg 199 transect extends from a paleolatitude of ~4°N- ~4°S to encompass a relatively thick lower Eocene sediment section perhaps 8° north of the paleoequator. One site (1218) was also drilled on ~40-Ma crust to collect a near-equatorial sediment sequence from the middle Eocene to the Oligocene in order to investigate the transition in global climate from the Eocene "greenhouse" to Oligocene "icehouse." <br/>The Pacific plate has drifted northward through Cenozoic time transporting biogenic sediments deposited under the high-productivity equatorial belt into a zone of extremely slow sediment (red clay) accumulation. Thus, the central tropical North Pacific Ocean is an ideal region in which to sample shallowly buried Paleogene sequences of equatorially deposited biogenic sediments. The thin Neogene cover of red clay in the area means that the entire Paleogene sediment section is potentially drillable by ODP advanced piston coring and extended core barrel methods

Topics: QE
Publisher: Texas A & M University Ocean Drilling Program (CDROM)
Year: 2002
OAI identifier: oai:eprints.soton.ac.uk:41902
Provided by: e-Prints Soton

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