14 Sediments, Soils, and Stratigraphy (Posters)
Tuesday, 22 March 2016
8:00 AM - 5:30 PM
Riverview B
STRATIGRAPHY AND DEPOSITIONAL ENVIRONMENT OF SAUROPOD DINOSAUR TRACK SITES, LOWER CRETACEOUS GLEN ROSE FORMATION, COW HOUSE CREEK CENTRAL TEXAS
Paper number: 14-6
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
Abstract
A total of 14.5 meters of section have been measured, varying in lithology from limestone to marl and calcareous shale. All three members of the Glen Rose Formation are present in the outcrop (the lower Glen Rose, the Thorp Springs, and the upper Glen Rose members). The track-bearing layer occurs in the lower Glen Rose member. The depositional environment varies from supratidal to intertidal and subtidal zones. The tracklayer appears to have been deposited in the supratidal zone. The most likely trackmaker was Sauroposeidon.
Geological Society of America Abstracts with Programs. Vol. 48, No. 1
doi: 10.1130/abs/2016SC-273227
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