Depositional History and Performance of a Permian Bell Canyon Sandstone Reservoir, Ford-Geraldine Field, West Texas

Author(s):  
Robert W. Ruggiero
2017 ◽  
Vol 155 (7) ◽  
pp. 1507-1522 ◽  
Author(s):  
STIG M. BERGSTRÖM ◽  
ANNALISA FERRETTI

AbstractOlistostromes with calcareous olistoliths are rare components in the Ordovician successions in NW Europe and North America, having been described from only a small number of localities. One of the best exposed, but least known, is in the Garn Formation in coastal outcrops in Anglesey in northwestern Wales. Here, in the graptolite-bearing shales of the Garn Formation, there are numerous limestone olistoliths that are derived from an otherwise unknown ‘ghost’ formation whose original depositional site remains an enigma. These olistoliths contain a Baltoscandian type of conodont fauna that is otherwise unknown in Wales and England. It represents the Baltoniodus variabilis Subzone of the Amorphognathus tvaerensis Zone. Similar, but slightly older, conodont faunas are recorded from olistoliths in the Tweeddale Member of the Shinnel Formation in southern Scotland and in probable olistoliths of the Cobbs Arm Limestone in northeasternmost Newfoundland. Approximately coeval conodont faunas are present in calcareous olistoliths in the Woods Hollow Shale of West Texas and the Womble Shale in the Ouachita Mountains of Arkansas, USA. Lithological and conodont evidence indicates that the calcareous olistoliths were derived from carbonate sediments deposited in relatively shallow water. It is concluded that the study of ‘ghost’ formation olistoliths may provide otherwise unavailable but important data bearing on the marine depositional history of a particular region.


Geosphere ◽  
2018 ◽  
Vol 14 (5) ◽  
pp. 2206-2244 ◽  
Author(s):  
Thomas M. Lehman ◽  
Steven L. Wick ◽  
Heather L. Beatty ◽  
William H. Straight ◽  
Jonathan R. Wagner

2007 ◽  
Vol 1 (1) ◽  
pp. 75-85 ◽  
Author(s):  
J. William Carey ◽  
Marcus Wigand ◽  
Steve J. Chipera ◽  
Giday WoldeGabriel ◽  
Rajesh Pawar ◽  
...  

HortScience ◽  
1999 ◽  
Vol 34 (3) ◽  
pp. 503D-503
Author(s):  
W.A. Mackay ◽  
D. Sankhla ◽  
T.D Davis ◽  
N. Sankhla

Racemes of Big Bend bluebonnet (Lupinus havardii Wats.), a winter annual native to far west Texas with attractive blue flowers, are currently being produced commercially as a specialty cut-flower crop. Our studies indicated that the key determinants of postharvest longevity and performance are flower abscission and flower senescence, both of which can be influenced by ethylene. Therefore, this study was undertaken to evaluate the role of some ethylene biosynthesis inhibitors (aminooxy acetic acid = AOA; cobalt = CO++; salicylic acid = SA) and an ethylene action inhibitor (silver thiosulfate = STS) on flower abscission and flower senescence of bluebonnet racemes. Depending on the concentration used (10 μM - 1 mM), AOA and CO++ exhibited variable effects on flower abscission, flower senescence and vaselife. SA (10-100 μM) slightly delayed senescence but did not affect abscission, while higher levels of SA (500 μM - 2 mM) slightly promoted abscission and also significantly enhanced the senescence of flowers on cut racemes. The effects of SA were found to be pH-dependent. However, STS nearly eliminated flower abscission and enhanced vaselife. The results also demonstrated that the abscission of bluebonnet flowers, in particular, is highly sensitive to ethylene.


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