Abstract
of paper presented at the 2001 annual meeting of the Geological Society of
America:
A
remarkable vertebrate assemblage from the Lance Formation, Niobrara County,
Wyoming. SPENCER, L., EHRC, 4736 Carberry Ck. Rd.,
Jacksonville, OR 97530, lspencer@bco.com; TURNER, L. E., Dept. of Mathematics and Physical
Sciences, CHADWICK, A. V., Dept of
Geology, Southwestern Adventist University, Keene, TX 76059.
During
the process of an on-going taphonomic study of the Lance vertebrates, a small
quarry was opened up on a sandstone ridge abutting a calcareous cemented cobbly
sandstone bone bed one meter in thickness.
The deposit concerned here occurs in a poorly cemented well-sorted
immature white sandstone that appears to be a lag deposit on the trailing edge
of the larger mass of the bone bed itself.
Transport of the entire unit appears to have been to the south, based
upon imbrication of the flat pebble clasts contained in the unit. The bone bed contains bones in all size
categories, ranging from small bone chips and ossified tendons to whole femurs.
The lag deposit contains a variety of bones, but all of them tend to be smaller
than those of the main bone bed, and the entire thickness of the lag deposit is
less than 20 cm. The profile of the lag
tails and disappears in the white sandstone over a distance of two meters
proximal to the bone bed. The materials
described below were recovered from 20 cm depth in an area of a little more
than one square meter in this lag.
The lag
deposit contained a variety of bones of Edmontosaurus, fragments of turtle
bones and fish scales, and numerous teeth.
While the majority of the teeth were those of Edmontosaurus, and
a dentary of a juvenile Edmontosaurus was recovered, teeth of at least
six other species of dinosaur were
recovered, including Triceratops horridus, Tyrannosaurus rex, Nannotyrannus
sp., and Troodon formosus. Associated with the dinosaur teeth were
teeth from crocodiles, fish, multituberculates and other forms still under
study. The accumulation of such a
variety of species in such a small area is consistent with the lag developing
downstream from a high energy debris accumulation
2001
L. Spencer, L. Turner and A.V. Chadwick, A remarkable vertebrate assemblage
from the Lance Formation, Niobrara County, Wyoming. Geological Society of
America. Abstracts with Program 33:A499.