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Volume 80—2000

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Several Microvertebrate Fossils from the Washita Local Fauna

Henry Kirkland, Shane Norris, Jeanette Bartow, Julie Hughes, Jerri Devine, Samuel Maxwell Adu-Lartey, and Nicki Wollison

Department of Biology, Southwestern Oklahoma State University, Weatherford, OK 73096

In the 1998-1999 academic year, we excavated several microvertebrate fossils from Washita Local Fauna. This site is located 7.5 miles south of Weatherford, OK (T11N, R14W, Sec 18, SW 1/4, NE 1/4,). We removed the fossils from a Pleistocene deposit of light gray, silty clay measuring approximately 18 meters long and 2.3 meters deep. This deposit rests unconformibly on Permian sandstone of the Cloud Chief Formation. A gradual color change marks the end of the older Permian and the beginning of Pleistocene sediments. To obtain an accurate age of the deposit, three previously excavated bone samples from Washita Local Fauna were sent to Geochron Laboratories in Cambridge, Massachusetts for radiocarbon dating. These samples include Bison cf. occidentalis, GX-16060-A (18,295± 270 yr) (1), Equus excelsus, GX-22604-A (16,440 ± 730 yr) (1), and Bootherium bombifrons GX-19196 (16,350 ± 190 yr) (2). These dates place the deposit in the late Pleistocene Epoch (3).

We used a screenwashing method described by Rixon (4) to isolate fossils from the sediment collected. A right mandible with an incisor and three molars of Reithrodontomys montanus, K-143, were recovered (Fig. 1). Identification was accomplished using a binocular stereoscopic microscope and a digital caliper to make measurements for comparison. The specimen recovered had the distinctive shape and characteristics of the Reithrodontomys genus (Table 1)(5).

We also found in screenwashing a left molar of a second small mammal, K-144 (Fig. 2). Its identification was made by comparing it to previously excavated fossils in the Southwestern Oklahoma State University (SWOSU) collection, in particular specimen K-138 (6). We also compared measurements of its dentine tract (7) on the labial surface of the M1 (8) to those of the species Neotoma micropus, N. floridana, and N. albigula (Table 2). The M1 of these species are characterized by a development of a dentine tract height of less than 0.2 mm. The dentine tract of the specimen recovered from Washita Local Fauna is 0.18 mm. In addition, the following measurements were made. The midlength (3.79 mm), base of lingual fold 1 to base of lingual fold 2 (1.20 mm), and base of lingual fold 2 to anterior face (2.77 mm). All measurements were within the range of those characteristic of N. floridana.

The third microvertebrate recovered was a fragmented right mandible of Sorex hoyi, K-14 (5). It contains two teeth, the M1 and M2, and has a total length of 4.87 mm. The total length of the right mandible of S. hoyi is 5.6-6.2 mm (9). The sample was also identified via comparison with the fossil shrews housed at SWOSU, K-142.

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The fourth specimen excavated was a lower left mandible of Sorex cf. cinereus, K-146. It was identified by comparison with specimens in the collection at SWOSU, K-141. The anterior part of the mandible is fragmented, thus only the M2 and M3 are present. The length of M2 is 1.05 mm and the length of M3 is 1.07 mm. These measurements fall within the range of the S. cinereus (10).

Other species recovered from screenwashing are Microtus cf. ochragaster, K-151 and K-153, and Synaptomys cf. cooperi, K-152. These fossil rodents were taken to the Natural History Museum at the University of Oklahoma for identification by Nicholas Czaplewski. They were also compared to specimens K-116 and K-139 in the SWOSU collection.

Microtus cf. ochragaster is represented by a right mandible with the incisor and M1 and M2 present, K-151. The left M1 Microtus cf. ochragaster, K-153, is also present. Synaptomys cf. cooperi is represented at the Washita Local Fauna by the left M1, K-152.

Measurements of the Microtus cheek teeth (K-151 & K-153) were obtained using the methods described by Martin (11). The M1 is the best tooth for identifying Microtus ochragaster (11).

Measurements taken from the M1 of K-151, the right mandible of Microtus cf. ochragaster, include occlusal length (L) 2.86 mm, relative length of the anterconid complex (W'/W) 83.3 mm, the ratio of the width of the dentine isthmus connecting T4/T5 and the anterior cap to the width of the anteroconid complex (B/W) 29.75 mm, and the ratio of the width of the dentine isthmus connecting T4/T5 to the width of the anteroconid complex (C/W) 25.6 mm. All of these measurements fall within specification of Microtus ochragastor (Table 3).

The measurements obtained from M2 of K-151 provided the ratio of width of the dentine isthmus connecting T3/T4 to the greatest width across T3/T4 (Cl/W).

Measurements of the M1 of Microtus cf. ochragaster, K-153, were taken in the same fashion as those from the M1 of K-151. They are: L 2.73 mm, A/L 58.97 mm, W'/W 98.97 mm, B/W 28.34 mm, and C/W 24.6 mm. Once again all measurements closely match measurements for the identification of the Microtus ochragaster (Table 4).

The left M1 of Synaptomys cf. cooperi, K-152, measures 3.17 mm x 4.36 mm (L x W) (12). These measurements compare favorably to those of Synaptomys cooperi.

ACKNOWLEDGMENTS

This study was supported by a Southwestern Oklahoma State University faculty research grant. Thanks to Nicholas Czaplewski, of the Oklahoma Museum of Natural History for identification. We also thank the landowner Lola Littlebird, for allowing removal of the fossils and Russell Pfau for the drawings.

REFERENCES

1.   Kirkland H Jr, Dill J, Selfridge W. Some late pleistocene vertebrates for western Oklahoma. Proc Okla Acad Sci, 1991;71:55.

2.   Kirkland H, Hilliard J. An extinct pleistocene musk ox from western Oklahoma. Southwest Nat. 1996;41:246-279.

3.   Levin HL. The earth through time. Philadelphia: Saunders; 1988. 593 p.

4.   Rixon AE. Fossil animal remains: their preparation and conservation. Humanities Press, NJ; 1976. 304 p.

5.   Dalquest WW, Schultz GE. Ice age mammals of northwestern Texas. Wichita Falls (TX): Midwestern State University Press; 1992. 309 p.

6.   Kirkland H, Davis M, Wood J, Devine D, Giblet K. Some late Pleistocene fossils from the Washita local fauna. Proc Okla Acad 1997;77:113-115.

7.   Zakrzewski RJ. Morphological change in woodrat (Rodentia: Cricetedae) molars. In: Martin RA, Barnosky AD, editors. Morphological change in Quaternary mammals of North America. Boston: Cambridge University Press; 1993. p 392-490.

8.   Harris AH. Neotoma in the late Pleistocene of New Mexico and Chihuahua. Special Pub. Carnegie Mus Nat His 1991;8:164-178.

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9.   Mullican TR, Carraway LN. Shrew remains from Moo and Middle Butte, Caves, Idaho. J Mammal 1990;71:351-356.

10.   Van Zyll, De Jong CG. Relationships of amphiberingian shrews of the Sorex cinereus group. Can J Zoo 1982;60:1580-1586.

11.   Martin RA. A new middle Pleistocene species of Microtus (Pedomys) from the southern United States, with comments on the taxonomy and early evolution of Pedomys and Pitymys in North America. Journ Vert Paleo 1995;15:171-186.

12.   Clark MK, Mitchel MS, Karriker KS. Notes on the geographical and ecological distribution of relict populations of Synaptomys cooperi (Rodentia: Arvi-colidae) from eastern North Carolina. Brimleyena. 1993;19:155-167

Received: January 6, 2000; Accepted: September 11, 2000

(Table 1)

(Table 2)

(Table 3)

(Table 4)