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    This chapter has been cited by the following publications. This list is generated based on data provided by CrossRef.

    Emry, Robert J. and Korth, William W. 2012. Early Chadronian (late Eocene) rodents from the Flagstaff Rim area, central Wyoming. Journal of Vertebrate Paleontology, Vol. 32, Issue. 2, p. 419.

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  • Print publication year: 1996
  • Online publication date: July 2010

19 - Cylindrodontidae

Summary

ABSTRACT

The rodent family Cylindrodontidae reached its greatest diversity in North America in Chadronian time, and cylindrodonts are among the most common rodents in White River faunas of Chadronian age. This chapter provides a general systematic summary of all Chadronian cylindrodont rodents, but focuses on those from the White River Group. We describe two new species, Cylindrodon natronensis and C. solarborus, from the early to middle Chadronian of the Flagstaff Rim area, Wyoming. Previously undescribed material affords much new information on the cranial and mandibular morphology of Cylindrodon and prompts a reinterpretation of its zygomasseteric structure.

INTRODUCTION

The earliest record of cylindrodontid rodents is Dawsonomys woodi from the Wasatchian of Wyoming (Korth, 1984). The family reached its greatest diversity in the Chadronian, where four genera and 13 species have been recognized, but before the end of Chadronian time the family became extinct in North America. Two subfamilies, the Cylindrodontinae and Jaywilsonomyinae, are recognized on the basis of dental characters (Wood, 1974), and can be traced back to the Bridgerian and Uintan, respectively; the subfamilial allocation of the Wasatchian Dawsonomys is uncertain, but is probably to Cylindrodontinae.

Outside North America, cylindrodontids are rare. The genus Ardynomys (originally referred to the Ischyromyidae) was first described from the latest Eocene or earliest Oligocene Ardyn Obo Formation of Mongolia by Matthew and Granger (1925). From the same deposits, Shrevyreva (1972) later named Morosomys silentiumis, which she classified as a cylindrodont; we consider Morosomys a synonym of Tsaganomys, and not a cylindrodont.

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The Terrestrial Eocene-Oligocene Transition in North America
  • Online ISBN: 9780511665431
  • Book DOI: https://doi.org/10.1017/CBO9780511665431
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