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New Occurrence of Paleocene Mammals in the Evanston Formation, Southwestern Wyoming

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dc.contributor.author Gazin, C. L. en
dc.date.accessioned 2007-07-31T16:24:13Z
dc.date.available 2007-07-31T16:24:13Z
dc.date.issued 1969
dc.identifier.citation Gazin, C. L. 1969. <em><a href="https://doi.org/10.5479/si.00810266.2.1">New Occurrence of Paleocene Mammals in the Evanston Formation, Southwestern Wyoming</a></em>. Washington, D.C.: Smithsonian Institution. <a href="https://doi.org/10.5479/si.00810266.2.1">https://doi.org/10.5479/si.00810266.2.1</a> en
dc.identifier.uri http://hdl.handle.net/10088/1935
dc.identifier.uri http://dx.doi.org/10.5479/si.00810266.2.1
dc.description.abstract A new fossil horizon and locality for the Evanston formation, near Little Muddy Creek in the Fossil Basin of southwestern Wyoming, has yielded remains of a mammalian faunule of middle Paleocene age. Relationships are shown to the two widely separated classic occurrences: the upper Lebo of the Montana Fort Union and the New Mexico Torrejon. A correlation is also indicated with the Battle Mountain and Rock Bench occurrences in the more local Wyoming region. The known faunule is comprised of essentially small Mammalia representing the orders Multituberculata, Insectivora, Primates, Creodonta, and Condylarthra. The material consists for the most part of isolated teeth, hence identifications are necessarily tentative in nature. en
dc.format.extent 9694493 bytes
dc.format.extent 845817 bytes
dc.format.mimetype application/pdf
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.title New Occurrence of Paleocene Mammals in the Evanston Formation, Southwestern Wyoming en
dc.type Book, Whole en
dc.identifier.srbnumber 113434
dc.identifier.eISSN 1943-6688
dc.identifier.doi 10.5479/si.00810266.2.1
dc.description.SIUnit SISP en
dc.relation.url https://doi.org/10.5479/si.00810266.2.1


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