From one to seven individuals are represented by each of these names except Odocoileus, which accounts for the great majority of the specimens. We conclude that the people who were responsible for this deposit lived, while at this site, on a diet in which venison, probably from the Mule Deer (Odocoileus hemionus), predominated. There are surprisingly few Bison bones, and just one specimen each of “Elk” and Bighorn.

All of this fauna still lived in the same general area in historic times; it is a Recent fauna. The symbol (†) marks genera and species known to occur in the fauna of the Piney Creek alluvium (Hunt, 1954, p. 114-117).[5] These elements of the Piney Creek fauna have previously been reported from the nearby Denver area by Hunt (1954, p. 118), and have been identified by the Upper Cenozoic Research Group in the collections made by Scott[6] from the nearby Kassler area, and by Hunt[7] from the dark-colored, sandy and silty alluvium that occurs along Strain Gulch near the Sanger Site. It seems reasonable to believe that the age of the main deposit in the shelter, below the ceramic occupation layer, is approximately equivalent to the age of the dark-colored, sandy, silty alluvium and that of the Piney Creek alluvium.

Classification used in this report:

TABLE VII—Faunal Remains, LoDaisKa

 A   B   C   D   E   F   G   H 
12 24 3648 60 7284 95   108
Amphibian 2 1
Reptile 2
Bird 3 2 11
Lagomorphs, sp. undet.  4 1
Lepus 18
Rodentia, undet. 2
Cynomys 4 11 203 1
Citellus 31
Tamias and Eutamias 1 2
Thomomys 2
Castor (canadensis) 2
Peromyscus ?3
Microtine 2 4
Carnivore, undet. 1 1
Canis 1
Mephites 1
Taxidea 1 1
Felis 3
Cervus 1
Odocoileus 26 1832 42 4470 17
?Bos 6
Bison (bison) 4 5 711
Ovis (canadensis) 1 1

Plant Remains from the LoDaisKa Site

By Walton C. Galinat

(Below Dr. Galinat has identified key specimens from the site from which data table was completed).