TY - JOUR
T1 - A new skeleton of Palaeosinopa didelphoides (Mammalia, Pantolesta) from the early Eocene Fossil Butte Member, Green River Formation (Wyoming), and skeletal ontogeny in Pantolestidae
AU - Rose, Kenneth D.
AU - Dunn, Rachel H.
AU - Grande, Lance
N1 - Funding Information:
For valuable information, discussion, and other assistance, we thank R. J. Asher, V. B. DeLeon, R. Z. German, W. von Koenigswald, W. P. Luckett, M. R. Sánchez-Villagra, B. H. Smith, and T. Smith. G. Gruber (HLMD) kindly provided measurements of Buxolestes minor. We are grateful to M. Albano, K. Koenig, and D. Ruben at the Johns Hopkins University School of Medicine for taking the radiographs. At the Field Museum, M. Peters prepared the new skeleton and J. Weinstein assisted with photography. We thank W. von Koenigswald, R. Stucky, and associate editor T. Martin for constructive comments that improved the manuscript. Initial research on pantolestid skeletons was supported by an award from the Alexander von Humboldt Foundation to K.D.R.
PY - 2014/6/7
Y1 - 2014/6/7
N2 - A new subadult partial skeleton of a pantolestid is reported from the late early Eocene Fossil Butte Member of the Green River Formation. Although the specimen displays a full permanent dentition, the presence of unfused elbow epiphyses (typically the first epiphyses to close), together with a short skull, shallow dentaries, and incompletely erupted third molars, indicates that it was a young juvenile. This adds to evidence that pantolestids had relatively early eruption of permanent premolars and late epiphyseal closure. Based on molar size and morphology, including presence of a well-developed paraconid, the specimen is attributed to Palaeosinopa didelphoides. Despite differences in skeletal size and robustness among the three known Fossil Butte pantolestid skeletons, all of which are skeletally subadult, similarity in molar size (and morphology, to the extent that it is visible) suggests that the three skeletons represent three growth stages of P. didelphoides. If this interpretation is correct, it has implications for recognition of fossil species based on such traits as jaw depth, presence/absence of diastemata, and relative robustness of skeletal features.
AB - A new subadult partial skeleton of a pantolestid is reported from the late early Eocene Fossil Butte Member of the Green River Formation. Although the specimen displays a full permanent dentition, the presence of unfused elbow epiphyses (typically the first epiphyses to close), together with a short skull, shallow dentaries, and incompletely erupted third molars, indicates that it was a young juvenile. This adds to evidence that pantolestids had relatively early eruption of permanent premolars and late epiphyseal closure. Based on molar size and morphology, including presence of a well-developed paraconid, the specimen is attributed to Palaeosinopa didelphoides. Despite differences in skeletal size and robustness among the three known Fossil Butte pantolestid skeletons, all of which are skeletally subadult, similarity in molar size (and morphology, to the extent that it is visible) suggests that the three skeletons represent three growth stages of P. didelphoides. If this interpretation is correct, it has implications for recognition of fossil species based on such traits as jaw depth, presence/absence of diastemata, and relative robustness of skeletal features.
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U2 - 10.1080/02724634.2013.822876
DO - 10.1080/02724634.2013.822876
M3 - Article
AN - SCOPUS:84903986290
SN - 0272-4634
VL - 34
SP - 932
EP - 940
JO - Journal of Vertebrate Paleontology
JF - Journal of Vertebrate Paleontology
IS - 4
ER -