The eomyid rodent Paradjidaumo Burke from the late Eocene White River Formation, Flagstaff Rim area, Wyoming

Emry, Robert J.; Korth, William W.

doi:10.2988/0006-324X-126.2.178

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other| July 01 2013

The eomyid rodent Paradjidaumo Burke from the late Eocene White River Formation, Flagstaff Rim area, Wyoming

Robert J. Emry;

Robert J. Emry

(RJE) Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, D.C. 20013, U.S.A., e-mail: [email protected];

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William W. Korth

(WWK) Rochester Institute of Vertebrate Paleontology, 265 Carling Road, Rochester, New York 14610, U.S.A.

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Proceedings of the Biological Society of Washington (2013) 126 (2): 178–186.

https://doi.org/10.2988/0006-324X-126.2.178

Abstract

Two species of the eomyid rodent Paradjidaumo are recognized from the Chadronian (latest Eocene) White River Formation in the Flagstaff Rim area of Wyoming: P. hansonorum from early Chadronian levels and P. nanus, new species, from higher levels representing the middle Chadronian.

2013

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The eomyid rodent Paradjidaumo Burke from the late Eocene White River Formation, Flagstaff Rim area, Wyoming

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The eomyid rodent Paradjidaumo Burke from the late Eocene White River Formation, Flagstaff Rim area, Wyoming