MORPHOMETRICS AND SYSTEMATICS OF HYOPSODUS (MAMMALIA, CONDYLARTHRA) FROM THE WASATCHIAN AND BRIDGERIAN EOCENE OF THE GREEN RIVER BASIN, WYOMING
In Wa-7, the first appearance of the small-sized H. minusculus is reported alongside H. miticulus, both of which continue into the Gardnerbuttean Zone, Br-1a. Evidence from the premolar series is suggestive of a continuation of the still larger H. walcottianus into Br-1a. Additionally, a last occurrence of H. miticulus is noted at the end of Br-1a, with H. minusculus continuing as the sole representative of the genus in the Early Blacksforkian Zone (Br-1b). The Late Blacksforkian Zone (Br-2) sediments preserve H. minusculus, the first appearance of H. paulus (the type species of Hyopsodus), and a possible precocious occurrence of the large-sized H. marshi (previously known from Br-3). Sample sizes from Br-3 are small, but the available evidence suggests that two smaller species of Hyopsodus accompany H. marshi, perhaps continuations of H. minusculus and H. paulus.
The presence of only one Hyopsodus species of small body size in Br-1b and the appearance of two additional species and an overall increase in body size among all lineages in Br-2 and Br-3 may be a reflection of climatic deterioration in the later Bridgerian.Geographic variation in Hyopsodus dentitions is also evident in this study. In the Br-2, body size is the smallest in specimens from localities near the basin-margin and increases toward the basin-center. In Br-1a, accessory cusps on the lower molars are variably present only in part of the basin-center of the Green River Basin.