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Results from palynological studies of Lower Pennsylvanian coal beds and adjacent strata from the proposed Pennsylvanian system stratotype in Virginia and West Virginia

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6386456
The Lower Pennsylvanian Series of the stratotype is composed of the Pocahontas and New River Formations. One hundred twelve samples of roof rock, coal, and seat rock were collected from 29 localities in these formations. Palynological data from samples of 19 of the 29 collecting localities provide evidence to support the continuity of important range zones and establish the first Pennsylvanian occurrence of Laevigatosporites near the top of the New River Formation close to the New River-Kanawha boundary that separates Lower and Middle Pennsylvanian. This occurrence may help in the placement of the boundary in the Appalachian Basin and elsewhere. Fungal remains and other previously unobserved microfossils were found in four samples. Palynomorphs and other organic matter observed in this study have been exposed to a high degree of thermal alteration. The alteration of the palynomorphs is most pronounced in the coal beds of the Pocahontas Formation and the lower half of the New River Formation. Palynomorphs from the Pocahontas Formation are brown to black and more difficult to identify than those from the New River Formation which are a lighter brown color. Palynomorphs preserved in non-coal strata, such as roof and seat rocks, are much less thermally altered than palynomorphs preserved in coal. Consequently, the Pocahontas Formation, the primary data were obtained from non-coal samples.
Research Organization:
Denver Federal Center, CO (USA)
OSTI ID:
6386456
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English