Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy
Vertebrate fossils have been discovered at several locations in the Bighorn Basin (Wyoming). The Virginia Museum of Natural History's (VMNH) digsite is located in the eastern part of the Bighorn Basin, in the Coyote Basin. Many scientists have worked within these basins trying to describe the s...
Main Author: | |
---|---|
Other Authors: | |
Format: | Others |
Published: |
Virginia Tech
2014
|
Subjects: | |
Online Access: | http://hdl.handle.net/10919/35709 http://scholar.lib.vt.edu/theses/available/etd-11152001-170826/ |
id |
ndltd-VTETD-oai-vtechworks.lib.vt.edu-10919-35709 |
---|---|
record_format |
oai_dc |
spelling |
ndltd-VTETD-oai-vtechworks.lib.vt.edu-10919-357092020-09-29T05:45:23Z Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy Wilborn, Brooke K. Geological Sciences Bambach, Richard K. Kowalewski, Michal Fraser, Nicholas C. Ostrom Cloverly Bighorn Basin vertebrate paleontology Morrison stratigraphy Vertebrate fossils have been discovered at several locations in the Bighorn Basin (Wyoming). The Virginia Museum of Natural History's (VMNH) digsite is located in the eastern part of the Bighorn Basin, in the Coyote Basin. Many scientists have worked within these basins trying to describe the stratigraphy. One question specifically asked is where the boundary between the Morrison Fm. (Jurassic) and the Cloverly Fm. (Cretaceous) lies. This new study attempted to show if the current method (Kvale, 1986) of determining the boundary is appropriate. The stratigraphy of the area was examined using Kvale, 1986, Ostrom, 1970, and Moberly, 1960's work in order to see which model was more robust. The fossils in the VMNH digsite were used to supplement the stratigraphic data in determining the age of specific beds. All of Ostrom's units were identified throughout the study area. There is some doubt as to whether the units would be acceptable outside of the Coyote Basin because of laterally discontinuity. Nevertheless, his description of units is satisfactory for the study area, and is more appropriate than other methods. The geologic age of the dinosaurs uncovered in the VMNH quarry is in agreement with the age determined stratigraphically. The VMNH site is below Ostrom's Unit II, which would place it in the Late Jurassic. The determination of the Jurassic/Cretaceous stratigraphic boundary has not been resolved. However, since the Pryor Conglomerate member of the Cloverly Fm. can be identified throughout this area, it is proposed as the Morrison Fm./Cloverly Fm. boundary. Master of Science 2014-03-14T20:47:58Z 2014-03-14T20:47:58Z 2001-08-10 2001-11-15 2004-12-14 2001-12-14 Thesis etd-11152001-170826 http://hdl.handle.net/10919/35709 http://scholar.lib.vt.edu/theses/available/etd-11152001-170826/ etdthesis.pdf figure_1.pdf figure_2.pdf figure_3.pdf figure_4.pdf figure_5.pdf figure_6.pdf figure_7.pdf figure_8.pdf figure_9.pdf figure_10.pdf figure_11.pdf figure_12.pdf figure_13.pdf figure_14.pdf figure_15.pdf figure_16.pdf figure_17.pdf figure_18.pdf figure_19.pdf figure_20.pdf figure_21.pdf figure_22.pdf figure_23.pdf figure_24.pdf figure_25.pdf figure_26.pdf In Copyright http://rightsstatements.org/vocab/InC/1.0/ application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf application/pdf Virginia Tech |
collection |
NDLTD |
format |
Others
|
sources |
NDLTD |
topic |
Ostrom Cloverly Bighorn Basin vertebrate paleontology Morrison stratigraphy |
spellingShingle |
Ostrom Cloverly Bighorn Basin vertebrate paleontology Morrison stratigraphy Wilborn, Brooke K. Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
description |
Vertebrate fossils have been discovered at several locations in the Bighorn Basin (Wyoming). The Virginia Museum of Natural History's (VMNH) digsite is located in the eastern part of the Bighorn Basin, in the Coyote Basin. Many scientists have worked within these basins trying to describe the stratigraphy. One question specifically asked is where the boundary between the Morrison Fm. (Jurassic) and the Cloverly Fm. (Cretaceous) lies. This new study attempted to show if the current method (Kvale, 1986) of determining the boundary is appropriate. The stratigraphy of the area was examined using Kvale, 1986, Ostrom, 1970, and Moberly, 1960's work in order to see which model was more robust. The fossils in the VMNH digsite were used to supplement the stratigraphic data in determining the age of specific beds.
All of Ostrom's units were identified throughout the study area. There is some doubt as to whether the units would be acceptable outside of the Coyote Basin because of laterally discontinuity. Nevertheless, his description of units is satisfactory for the study area, and is more appropriate than other methods. The geologic age of the dinosaurs uncovered in the VMNH quarry is in agreement with the age determined stratigraphically. The VMNH site is below Ostrom's Unit II, which would place it in the Late Jurassic. The determination of the Jurassic/Cretaceous stratigraphic boundary has not been resolved. However, since the Pryor Conglomerate member of the Cloverly Fm. can be identified throughout this area, it is proposed as the Morrison Fm./Cloverly Fm. boundary. === Master of Science |
author2 |
Geological Sciences |
author_facet |
Geological Sciences Wilborn, Brooke K. |
author |
Wilborn, Brooke K. |
author_sort |
Wilborn, Brooke K. |
title |
Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
title_short |
Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
title_full |
Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
title_fullStr |
Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
title_full_unstemmed |
Two New Dinosaur Bonebeds From the Late Jurassic Morrison Formation, Bighorn Basin, Wy: an Analysis of the Paleontology and Stratigraphy |
title_sort |
two new dinosaur bonebeds from the late jurassic morrison formation, bighorn basin, wy: an analysis of the paleontology and stratigraphy |
publisher |
Virginia Tech |
publishDate |
2014 |
url |
http://hdl.handle.net/10919/35709 http://scholar.lib.vt.edu/theses/available/etd-11152001-170826/ |
work_keys_str_mv |
AT wilbornbrookek twonewdinosaurbonebedsfromthelatejurassicmorrisonformationbighornbasinwyananalysisofthepaleontologyandstratigraphy |
_version_ |
1719346033848221696 |