Ostracodes in Owens Lake core OL-92: Alteration of saline and freshwater forms through time

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Edited by: George I. Smith and James L. Bischoff

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Abstract

Ostracode species’ geographic distributions are limited by parameters such as water temperature, salinity, and dissolved-ion composition. Because these parameters are, in part, determined by climate, ostracode biogeographic distributions serve as proxies for past climates. Therefore, the ostracodes in Core OL-92 from Owens Lake, southeast California, reveal climatic oscillations during the past 800,000 yr. The climatic history of the Owens Lake area, as indicated by the fossil ostracode record, reflects a number of high-latitude glacial and interglacial episodes in which glacial-period terminations fall at approximately 120 ka (Termination II), 225 ka (Termination III), 340 ka (Termination IV), and 438 ka (Termination V). A plot of saline versus freshwater ostracodes over time agrees quite well with a number of other geochemical and biological climatic indicators from the Owens Lake core.

Suggested Citation

Carter, C., 1997, Ostracodes in Owens Lake core OL-92: Alteration of saline and freshwater forms through time, chap. of An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California, v. 317, p. 113-119, https://doi.org/10.1130/0-8137-2317-5.113.

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Publication type Book chapter
Publication Subtype Book Chapter
Title Ostracodes in Owens Lake core OL-92: Alteration of saline and freshwater forms through time
DOI 10.1130/0-8137-2317-5.113
Volume 317
Year Published 1997
Language English
Publisher Geological Society of America
Description 7 p.
Larger Work Type Book
Larger Work Subtype Monograph
Larger Work Title An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California
First page 113
Last page 119
Country United States
State California
Other Geospatial Owens Lake
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