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dc.creatorBoger, P. D.en_US
dc.creatorGlaze, Frances F.en_US
dc.creatorSummerson, C. H.en_US
dc.creatorFaure, Gunteren_US
dc.date.accessioned2006-07-06T20:41:49Z
dc.date.available2006-07-06T20:41:49Z
dc.date.issued1973-01en_US
dc.identifier.citationThe Ohio Journal of Science. v73, n1 (January, 1973), 28-33en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/21952
dc.descriptionAuthor Institution: Department of Geology and Mineralogy, The Ohio State Universityen_US
dc.description.abstractNine analyses of the isotopic composition of strontium in the carbonate shells of marine fossils from the Kendrick Shale (Lower Pennsylvanian) of Kentucky indicate an average 87Sr/86Sr ratio of 0.7086^O.OOOSS at the 95 percent confidence limit. This value is in satisfactory agreement with previous measurements by Peterman et al. (1970) and confirms that strontium in the oceans during Early Pennsylvanian time was anomalously enriched in radiogenic 87Sr, compared to that in earlier and later periods. The isotopic composition of strontium in skeletal clacium carbonate of cephalopods, gastropods, and brachiopods from the Kendrick Shale appears to be the same in spite of the different feeding habits of these animals.en_US
dc.format.extent722994 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.titleThe Isotopic Composition of Strontium in Fossils from the Kendrick Shale, Kentuckyen_US


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