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Upper Pennsylvanian Steubenville Coal-Ball Flora

Please use this identifier to cite or link to this item: http://hdl.handle.net/1811/23241

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dc.creator Rothwell, Gar W. en_US
dc.date.accessioned 2006-07-07T02:25:08Z
dc.date.available 2006-07-07T02:25:08Z
dc.date.issued 1988-03 en_US
dc.identifier.citation The Ohio Journal of Science. v88, n1 (March, 1988), 61-65 en_US
dc.identifier.issn 0030-0950 en_US
dc.identifier.uri http://hdl.handle.net/1811/23241
dc.description Author Institution: Department of Botany, Ohio University en_US
dc.description.abstract The Upper Pennsylvanian (Conemaugh Group) Duquesne Coal west of Steubenville, Ohio represents a deltaic peat-accumulating swamp, and is one of the best known of coal swamp floras. In a few places, the peat was infiltrated and permineralized by calcium carbonate prior to coalification, thus producing coal balls in which both morphological and anatomical structure of the constituent plant parts are preserved. The plant material represents primarily the community that inhabited the peat-accumulating environment, but some remains from near-swamp environments also are represented. The flora is relatively diverse, consisting of over 55 megafossil taxa of isolated organs that were produced by at least 25 species of plants. All five major groups of Pennsylvanian coal-swamp plants (i.e., Lycopsida, Sphenopsida, Pteridopsida, Pteridospermopsida and Cordaitales) are represented. en_US
dc.format.extent 2022417 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.title Upper Pennsylvanian Steubenville Coal-Ball Flora en_US