Permo-Pennsylvanian Stratigraphy of Western Colorado Plateau and Eastern Great Basin Regions

Author(s):  
KENNETH G. BRILL
PeerJ ◽  
2019 ◽  
Vol 7 ◽  
pp. e8039 ◽  
Author(s):  
M. Andrew Johnston

The genus Trogloderus LeConte, 1879, which is restricted to dunes and sandy habitats in the western United States, is revised using morphological and molecular information. Six new species are described from desert regions: Trogloderus arcanus New Species (Lahontan Trough); Trogloderus kandai New Species (Owens Valley); Trogloderus major New Species (Mohave Desert); Trogloderus skillmani New Species (eastern Great Basin and Mohave Desert); Trogloderus verpus New Species (eastern Colorado Plateau); and Trogloderus warneri New Species (western Colorado Plateau). A molecular phylogeny is presented for the genus and used to infer its historical biogeography. The most recent common ancestor of Trogloderus is dated to 5.2 mya and is inferred to have inhabited the Colorado Plateau. Current species most likely arose during the mid-Pleistocene where the geographic features of the Lahontan Trough, Bouse Embayment and Kaibab Plateau were significant factors driving speciation.


1979 ◽  
Vol 44 (4) ◽  
pp. 711-722 ◽  
Author(s):  
David B. Madsen

A satisfactory and explicit definition of the Fremont has not been produced in over 50 years of research—a failure which suggests that no comprehensive entity exists. Attempts to define a Fremont through the use of trait lists have failed, although such lists have provided the basis for three apparently conflicting theories of origin. Analyses of subsistence economies and settlement patterns suggest that no comprehensive entity exists and that all three origin theories may possibly be valid. A Sevier "culture," based on marsh collecting and supplemented by corn agriculture, can be defined in the eastern Great Basin. A Fremont "culture," based on corn agriculture and supplemented by hunting, can be defined on the Colorado Plateau. A third unnamed, but possibly Plains-related, culture may be defined to the north of these. These "cultures" are distinctive enough to be separated on the same taxonomic level as are the Anasazi and the Sinagua.


2000 ◽  
Vol 5 (2) ◽  
pp. 269
Author(s):  
M. Guy Bishop ◽  
Kimball T. Harper ◽  
Larry L. St. Clair ◽  
Kaye H. Thorne ◽  
Wilford M. Hess

1985 ◽  
Vol 50 (4) ◽  
pp. 819-824 ◽  
Author(s):  
Karl J. Reinhard ◽  
J. Richard Ambler ◽  
Magdalene McGuffie

AbstractAnalysis of 100 desiccated feces of the Desha Complex (6800–4800 B.C.) from Dust Devil Cave near Navajo Mountain in southern Utah shows high proportions of Chenopodium seed and an absence of parasitic round-worms. Conversely, fecal remains from other sites in the Great Basin and Colorado Plateau show high incidences of parasite infection and low frequencies of Chenopodium. The implications of Chenopodium as a vermifuge are discussed.


2020 ◽  
Vol 85 (3) ◽  
pp. 573-590
Author(s):  
Jesse W. Tune

The central Colorado Plateau contains an exceptional density of cultural resources. Historically, however, archaeological investigations have overlooked the late Pleistocene and early Holocene record of this region. As such, there is currently a biased understanding of the earliest human occupations and adaptations. The regional Paleoindian record is reviewed here to assess the nature of initial human occupation of the area. Projectile point typologies, toolstone selection, and site distributions are used to characterize the land use patterns used by the region's earliest inhabitants. Results suggest that as early as circa 13,000 cal BP Clovis groups were familiar with the lithic landscape and habitually made use of local materials. Subsequent Paleoindian populations maintained relatively consistent levels of occupation throughout the Pleistocene-Holocene transition. Finally, the presence of classic Southwest, High Plains, and Great Basin–related lithic technologies suggests that the central Colorado Plateau was part of early interregional land use strategies.


Lithosphere ◽  
10.1130/l79.1 ◽  
2010 ◽  
Vol 2 (4) ◽  
pp. 221-231 ◽  
Author(s):  
S.E. Tindall ◽  
L.P. Storm ◽  
T.A. Jenesky ◽  
E.L. Simpson

1982 ◽  
Vol 60 (10) ◽  
pp. 2424-2433 ◽  
Author(s):  
Henri Goulet ◽  
Bernard R. Baum

This is a continuation of a study on geographical variation of the Elaphrus americanus Dejean species complex. This paper is devoted to E. finitimus Casey, which includes at least seven populations: White Mountains of California, Colorado Plateau, western Great Basin, western Arizona, central California, southern California, and southern Sierra Nevada. Three main groups of populations were recognized by means of numerical taxonomic analyses: White Mountains of California (one population), Intermontane (Colorado Plateau and western Great Basin), and southwestern (remaining four populations). The above groups were discerned from clustering by UPGMA (unweighted pair group using arithmetic averages) of Mahalanobis distances, and are characterized in a discriminant analysis. Other geographically distinct populations were recognized by univariate analysis of nominal characters. All seven populations are allopatric and are isolated presently from one another by vast expanses of dry regions (prairies and piñon–juniper woodlands), or by different life zones with altitude. We postulated that during the glacial phases of the Pleistocene similar barriers existed, though the gaps were narrower than at present. The reconstructed glacial ranges of these populations offer a hypothesis as to the origin of some populations, and direction of limited gene flow between some populations.


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