Maps showing drift patterns along the north-central Texas coast, 1973-1974

10.3133/mf714 ◽  
1975 ◽  
Keyword(s):  
Texas Coast ◽  
North Central ◽  
The North ◽  
North Central Texas ◽  
Central Texas

scholarly journals Fusulinids from the Howe Limestone Member (Red Eagle Limestone, Council Grove Group) in Northeastern Kansas and Their Significance to the North American Carboniferous (Pennsylvanian)-Permian Boundary

2010 ◽  
pp. 1-13
Author(s):  
Gregory P. Wahlman ◽  
Ronald R. West
Keyword(s):  
New Mexico ◽  
North American ◽  
Early Permian ◽  
North Central ◽  
The North ◽  
West Texas ◽  
North Central Texas ◽  
Central Texas ◽  
First Time

Fusulinids from the Howe Limestone Member (upper part of the Red Eagle Limestone, lower part of the Council Grove Group) are described here for the first time. The Howe fauna is particularly significant because it represents the earliest fusulinids known to occur above the new conodont-based Carboniferous (Pennsylvanian)-Permian boundary at the Glenrock Limestone Member-Bennett Shale Member contact (Red Eagle Limestone) in northeastern Kansas. The Howe fusulinid assemblage is composed entirely of species of the genus Leptotriticites. The species L. hughesensis and L. glenensis were originally described from just beneath the new systemic boundary horizon in the Hughes Creek Shale Member and Glenrock Limestone Member, respectively. L. wetherensis is a species from the Stockwether Limestone Member of north-central Texas, which is thought to directly overlie the new systemic boundary in that region. L. gracilitatus is a species reported from below and above the boundary in west Texas and New Mexico. Therefore, the Howe Limestone Member fusulinid fauna is quite transitional in character. The first typical and diagnostic early Permian (Wolfcampian Series) fusulinids in the midcontinent section appear in steps through the stratigraphically higher Neva Limestone Member of the Grenola Limestone (Paraschwagerina kansasensis), and the Cottonwood and Morrill Limestone Members of the overlying Beattie Limestone (Schwagerina jewetti, S. vervillei). This offset of conodont and fusulinid faunal changes should be taken into account in regional and interregional biostratigraphic correlations of the new systemic boundary.

scholarly journals Evaluation of Vitis Species Found in Selected Locations of Texas and New Mexico

HortScience ◽  
1996 ◽  
Vol 31 (4) ◽  
pp. 621a-621
Author(s):  
J. Kim Pittcock ◽  
Richard E. Durham
Keyword(s):  
New Mexico ◽  
Morphological Characteristics ◽  
Current Status ◽  
Vitis Species ◽  
North Central ◽  
North West ◽  
The North ◽  
Rich Diversity ◽  
North Central Texas ◽  
Central Texas

North American Vitis species and hybrids thereof have been the source of rootstocks for V. vinifera for the last century. Collection and evaluation of native Vitis in north-central Texas, western Texas, and New Mexico have been made to determine their current status. Known geographical pockets of grapevines were visited, with specimens taken and identified by comparison to herbarium collections and published descriptions. In locals where more than one species existed, many natural hybrids with varying morphological characteristics have become established. In North Central Texas, two areas were visited. The first was Tarrant, Parker and Wise counties where three grapevine species (V. mustangensis, V. cinerea var. helleri, and V. vulpina) and many hybrids were observed. The second was Wilbarger County where V. acerifolia was found growing in the south while V. ×doaniana was found growing in the north. West Texas was primarily populated with V. acerifolia with the exception of the Silver Falls Canyon area in Crosby County where hybrids of V. acerifolia, V. arizonica and V. riparia were observed. In New Mexico, two areas were visited: San Miquel County (North Central region), where V. acerifolia, V. arizonica, and V. riparia were observed and Eddy County (southern New Mexico) where V. arizonica was observed. A rich diversity of Vitis germplasm appears to remain in these habitats.

Being “Regionable”: A Key to Training Success

1986 ◽  
Vol 15 (4) ◽  
pp. 383-388
Author(s):  
Barbara Carpenter
Keyword(s):  
Training Programs ◽  
Financial Resources ◽  
High Quality ◽  
North Central ◽  
The North ◽  
North Central Texas ◽  
Central Texas ◽  
Training Success

Drawing on the success of a project initiated by the North Central Texas Council of Governments, the author describes the advantages—in terms of costs, time, and transportability—of establishing a regional consortium of public jurisdictions to develop high-quality, easily adaptable training programs in a climate of constricting financial resources.

scholarly journals Cretaceous δ13C stratigraphy and the age of dolichosaurs and early mosasaurs

2005 ◽  
Vol 84 (3) ◽  
pp. 257-268 ◽  
Author(s):  
L.L. Jacobs ◽  
K. Ferguson ◽  
M.J. Polcyn ◽  
C. Rennison
Keyword(s):  
Large Scale ◽  
Eastern Mediterranean ◽  
Eastern Mediterranean Region ◽  
Global Scale ◽  
North Central ◽  
The North ◽  
Depositional Settings ◽  
Isotopic Analyses ◽  
North Central Texas ◽  
Central Texas

AbstractSediments in north-central Texas, ranging in age from >117 to 85 Ma, represent a variety of terrestrial and marine depositional settings. Isotopic analyses of wood fragments found throughout the section allow correlation to the standard secular marine δ13C curve because of characteristic peaks at the Aptian-Albian and Cenomanian-Turonian boundaries. Consistency of the north-central Texas δ13C curve with the marine standard facilitates correlation among non-marine and marine environments on a global scale. Radiometrically dated ammonite zones recognised in Texas provide calibration for the Cenomanian and Turonian portions of the section. Cenomanian and Turonian sediments in north-central Texas preserve the oldest (96 Ma) and the youngest (<85 Ma) well-documented Coniasaurus, a dolichosaur also known from the southern North Sea Basin during that interval. Haasiasaurus, the oldest known well-documented early mosasaur, is found at ‘Ein Yabrud, Israel (98 Ma), followed by other poorly dated Cenomanian taxa from the eastern Mediterranean region, and then by Dallasaurus turneri and Russellosaurus coheni in Texas (92 Ma) and Tethysaurus (90.5 Ma) in Morocco. Neither shifts in δ13C nor large-scale sea level change seem to have influenced dolichosaur or mosasaur evolution in substantial ways during the Cenomanian and Turonian stages.

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