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

Robert J. Emry; William W. Korth

doi:10.2988/0006-324X-126.2.178

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Robert J. Emry,¹ William W. Korth²

¹(RJE) Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, P.O.
²(WWK) Rochester Institute of Vertebrate Paleontology, 265 Carling Road, Rochester, New York 14610, U

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.

Citation Download Citation

Robert J. Emry and William W. Korth "The eomyid rodent Paradjidaumo Burke from the late Eocene White River Formation, Flagstaff Rim area, Wyoming," Proceedings of the Biological Society of Washington 126(2), 178-186, (1 July 2013). https://doi.org/10.2988/0006-324X-126.2.178

Published: 1 July 2013