Theriosynoecum wyomingense (Branson, 1935), a possible guide ostracode to the salt water mash member of the Morrison formation /

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Bibliographic Details
Author / Creator:Sohn, I. G. (Israel Gregory), 1911-2000.
Imprint:[Washington, D.C.] : United States Department of the Interior, Geological Survey
Washington : United States Government Printing Office
Description:1 online resource (iii, 10 pages) : map.
Language:English
Series:Contributions to general geology
Geological Survey bulletin ; 1161-A
Contributions to general geology.
Geological Survey bulletin ; 1161-A.
Subject:
Format: E-Resource Map U.S. Federal Government Document Book
URL for this record:http://pi.lib.uchicago.edu/1001/cat/bib/10919093
Hidden Bibliographic Details
Other authors / contributors:Peck, Raymond E.
Notes:This volume was published as separate chapters A-I in Contributions to General Geology 1962.
"The ostracode species Theriosynoecum wyomingense (Branson, 1935) appears to be restricted to the Salt Wash Member of the Morrison Formation in the Colorado Plateau area and to equivalents of the Salt Wash Member in lithologically undifferentiated sedimentary rocks in Wyoming, South Dakota, and Montana. Associated charophytes tend to support this hypothesis."
Includes bibliographical references (pages A9-A10).
Other form:Print version: Sohn, I.G. (Israel Gregory), 1911-2000. Theriosynoecum wyomingense (Branson, 1935), a possible guide ostracode to the salt water mash member of the Morrison formation
GPO item no.:0620 (online)
Govt.docs classification:I 19.3:1161-A

MARC

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245 1 0 |a Theriosynoecum wyomingense (Branson, 1935), a possible guide ostracode to the salt water mash member of the Morrison formation /  |c by I.G. Sohn and R.E. Peck. 
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490 1 |a Contributions to general geology 
490 1 |a Geological Survey bulletin ;  |v 1161-A 
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504 |a Includes bibliographical references (pages A9-A10). 
500 |a "The ostracode species Theriosynoecum wyomingense (Branson, 1935) appears to be restricted to the Salt Wash Member of the Morrison Formation in the Colorado Plateau area and to equivalents of the Salt Wash Member in lithologically undifferentiated sedimentary rocks in Wyoming, South Dakota, and Montana. Associated charophytes tend to support this hypothesis." 
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