|2007 GSA Denver Annual Meeting (28–31 October 2007)|
|Paper No. 144-27|
|Presentation Time: 8:00 AM-12:00 PM|
ENVIRONMENTAL CONDITIONS OF THE TECOPA BASIN DURING THE MIDDLE PLEISTOCENE BASED ON FOSSILIZED DIATOM ASSEMBLAGES BELOW THE BISHOP TUFF
SCHUMAKER, Dave, Department of Geosciences, San Francisco State University, 1600 Holloway Ave, San Francisco, CA 94132, email@example.com|
Sedimentary deposits found within the Tecopa Basin of southeastern California, located in the Basin and Range physiographic province, are thought to have formed in a lake that persisted throughout the Pleistocene. Sparse evidence from fossilized ostracodes found within basin sediments suggest that the Tecopa Basin may have been primarily a spring-fed hydrologic system. Diatom samples from within the basin were collected near the town of Shoshone, California and analyzed to better determine the paleohydrologic enviornment of the Tecopa Basin. The diatoms found within these samples are similar to modern diatoms found at Mono Lake and other hypersaline and alkaline lakes throughout the Basin and Range province and are dominated by the genera Denticula, Fragillaria, and Navicula. Diatom specimens from modern spring systems found within the basin were collected for comparison to Tecopa Basin diatoms. Diatoms were rare and only poorly preserved in the modern spring samples but included Anomoeoneis and Stauroneis. Further research in the area may prove useful to determine the paleontological conditions and depositional environments of the Tecopa Basin deposits.
2007 GSA Denver Annual Meeting (28–31 October 2007)
General Information for this Meeting
|Session No. 144--Booth# 110|
Paleontology (Posters) II: Environments, Ecosystems, and Interactions
Colorado Convention Center: Exhibit Hall E/F
8:00 AM-12:00 PM, Tuesday, 30 October 2007
Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 401
© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.