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U.S. Department of Energy
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Palynology of selected coal beds in the proposed Pennsylvanian System stratotype in West Virginia

Technical Report ·
OSTI ID:6421135
Investigation of coals from sections of the proposed Pennsylvanian System stratotype provided the opportunity to examine changes in palynomorph content through a number of coals from the New River Formation to the basal part of the Monongahela Formation. The rank of most coals of the Pocahontas and New River Formations of West Virginia does not permit extraction of palynomorphs with current laboratory maceration techniques. Because of this, the data of some possibly equivalent lower rank Pennsylvanian coals from adjacent parts of southern Ohio and eastern Kentucky have been included. The coals examined from the Kanawha Formation, Charleston Sandstone, and Monongahela Formations of West Virginia have yielded abundant and well-preserved palynomorphs. The coal is a significant resource in Pennsylvanian rocks, and the correlation of coals is an important consideration in the area of the stratotype in West Virginia and in adjacent states. The approximate range zones of some important taxa have been established. The range zones of some important taxa from Lower to Upper Pennsylvanian coals are: Densosporites irregularis Hacquebard and Barss, Stenozonotriletes lycosporoids (Butterworth and Williams) Smith and Butterworth, Schulzospora rara Kosanke, Laevigatosporites spp., Radiizonates spp., Torispora securis Balme, Zosterosporites triangularis Kosanke, Thymospora pseudothiessenii (Kosanke) Wilson and Venkatachala, Schopfites dimorphus Kosanke, and Thymospora thiessenii (Kosanke) Wilson and Venkatachala. 44 refs., 9 figs., 22 tabs.
Research Organization:
Geological Survey, Reston, VA (USA)
OSTI ID:
6421135
Report Number(s):
USGS-PP-1318; ON: TI86900258
Country of Publication:
United States
Language:
English