Gf. Gunnell, PALEOCENE MAMMALS AND FAUNAL ANALYSIS OF THE CHAPPO TYPE LOCALITY (TIFFANIAN), GREEN RIVER BASIN, WYOMING, Journal of vertebrate paleontology, 14(1), 1994, pp. 81-104
The Chappo Type Locality in southwestern Wyoming has produced an exten
sive Tiffanian (late Paleocene) mammalian fauna. Thirty-three genera a
nd 39 species of mammals are represented at Chappo, including three ne
wly recognized taxa, a ?lipotyphlan insectivore Palaeoryctes cruoris,
sp. nov., an erinaceomorph insectivore Cedrocherus aceratus, sp. nov.,
and an arctocyonid condylarth Lambertocyon gingerichi, sp. nov. Compa
rison with other middle and late Tiffanian localities suggests that Ch
appo represents a transitional Ti3-Ti4 fauna. The presence of mature p
aleosol horizons at Chappo indicates deposition on a distal floodplain
. Faunal analysis (including body size distribution, trophic structure
, and taxonomic diversity) indicates that the Chappo sample consists o
f small- to medium-sized mammals dominated by omnivores and insectivor
es. The relatively low frequency of frugivores indicates less forested
, more open conditions. Diversity indices suggest that middle Tiffania
n mammalian diversity was only slightly lower than comparable early an
d late Tiffanian diversity, but diversity distribution was uneven, wit
h a few taxa dominating the fauna. Cenogram analysis of the Chappo fau
na indicates that the paleoenvironmental setting at Chappo was one of
open woodlands and relatively dry, seasonal conditions.