The Relation of Concretions to Coal Seams
@article{FelicianoTheRO, title={The Relation of Concretions to Coal Seams}, author={J. Feliciano}, journal={The Journal of Geology}, volume={32}, pages={230 - 239} }
Coal balls and roof-nodules are the most important concretions occurring with coal seams. Coal balls have been known for a long time in Europe, but have been only recently discovered in the United States and in Australia. They are formed in situ and contain plant remains which, because of their excellent preservation, yield much valuable paleobotanical information. The shale beds above the coal carry another type of concretion called roof-nodules which are generally formed in situ by the actipn…
7 Citations
The Formation and Significance of Carboniferous Coal Balls
- Environmental Science, Geography
- 1985
The preservation of cell contents, plant apices, gametophytes, etc., demonstrates the contemporaneous or early diagenetic formation of coal balls, which supported arguments for a marine source for the carbonate.
American coal-ball floras
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This brief review of American coal-ball floras points out current lines of research and what may be expected during the next decade or two to contribute notably to an understanding of the evolution of certain pteridophytic groups and the early seed plants.
Contributions to Pennsylvanian Paleobotany
- Geology
- 2004
PREFACE Applied research on coal has revealed the fact that there is a dearth of fundamental information regarding the nature of the original plant material from which the coal was derived. I t is…
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This work describes the interpretation of animal-containing-coal balls as homogeneous-mixed and faunal coal balls, and the results confirmed that both types of coal balls have similar physical and biological properties.