25 Paleontology and Paleobotany
Friday, 6 April 2001
8:20 AM - 11:40 AM
IMPLICATIONS OF K/T BOUNDARY DEPOSITS FROM DE SOTO CANYON, GULF OF MEXICO
Paper number: 25-8
Program: Technical Sessions
Time: 10:40 AM – 11:00 AM
Authors
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Timothy J. BralowerUniv of North Carolina at Chapel Hill, Chapel Hill, NC
Abstract
Cores E67-128 and E68-151A contained unconformities from Upper Campanian to Middle Paleocene age. This is possibly due to truncation of Upper Cretaceous beds, as seen in seismic studies from sections across the De Soto Canyon area, and sediment bypass associated with seismic shaking and tsunamis that resulted from the KTB impact. Destabilization of the margin and a eustatic sea level low during the early Paleocene may account for the hiatus as seen in core and seismic studies from the De Soto Canyon area. The results of this investigation agree with the hypothesis that the initial formation of the De Soto Canyon was linked to the KTB impact.