قراءة كتاب Records of the Fossil Mammal Sinclairella, Family Apatemyidae, From the Chadronian and Orellan
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Records of the Fossil Mammal Sinclairella, Family Apatemyidae, From the Chadronian and Orellan
Chadronian age referable to Sinclairella dakotensis have been discovered subsequently at a locality in Nebraska and fossils of Orellan age, also referable to S. dakotensis, have been collected at two localities in Colorado. The sample from each locality is described separately.
Sioux County, northwestern Nebraska
Material.—RAM-UCR nos. 381, left M1; 598, left m2; 1000, right m1; 1001, right m2; 1079, right m2; 1674, right M2; and 3013, left m2.
Locality and stratigraphy.—These Chadronian fossils were discovered by Raymond Alf and members of his field parties in several harvester ant mounds built in exposures of the Chadron Formation in Sec. 26, T 33 N, R 53 W, Sioux County, Nebraska (Alf, 1962, and Hough and Alf, 1958). This is UCR locality V5403. The collectors carefully considered the possibility that some of the fossils found in the ant mounds were collected from younger strata by the harvester ants and concluded this was unlikely (Alf, personal communication).
Description and comments.—The cusps of RAM-UCR no. 381, a left M1, are sharp and the wear-facets resulting from occlusion with the lower dentition are small. The paraconule is a low, ill-defined cusp on the anterior margin of the crown; a metaconule is not present. A smooth stylar shelf is present labial to the metacone. The crown was supported by three roots. There are no interradicular crests.
The crown of RAM-UCR no. 1674, a right M2, is heavily abraded and many morphological details of the cusps have been destroyed. Low interradicular crests linked the three roots of the tooth with a low, central prominence. As was the case with RAM-UCR no. 381, no significant differences could be found in comparisons with illustrations of the teeth preserved in Princeton no. 13585.
RAM-UCR nos. 598, 1001, 1079, and 3013 all appear to be m2's. The talonids of these teeth are not elongated, their trigonids have quadrilateral outlines, and the paraconids are small but prominent, bladelike cusps. The trigonid of RAM-UCR 1000 is elongated and the paraconid is a minute cusp; the tooth closely resembles the m1 of the type of Sinclairella dakotensis.
Logan County, northeastern Colorado
Material.—KU no. 11210 (fig. 1), a fragment of a left maxillary containing P4 and M1-2.
Locality and stratigraphy.—The fossil was found in the center of the W-1/2, Sec. 21, T 11 N, R 53 W, Logan County, Colorado, " ... in the bed below Agnotocastor bed, Cedar Creek Member...." (Ronald H. Pine, 1958, field notes on file at the University of Kansas). The bed so defined is part of unit 3 in the lower division of the Cedar Creek Member, as subdivided by Galbreath (1953:25) in stratigraphic section XII. The fauna obtained from unit 3 is of Orellan age.
Fig. 1. Sinclairella dakotensis Jepsen, KU no. 11210, fragment of left maxillary with P4 and M1-2; Orellan, Logan County, Colorado; drawings by Mrs. Judith Hood: a, labial view; b, occlusal view; both approximately × 9.
