The distribution and relative amounts of six genera of lycophyte microspores, Lycospora, Densosporites, Crassispora, Cirratriradites, Endosporites and Cadiospora, are compared in the Pennsylvanian coals from the Dobrudzha and Forest of Dean coalfields, clastic sediments from the Glace Bay borehole in the Cape Breton Coalfield, and the southern crop of the South Wales coalfield. Inverse relationships are shown between Lycospora and Densosporites and between Lycospora and Crassispora in samples from all of the coalfields. The changes in microspore assemblages suggest there were at least five different communities of lycophyte plants growing in the Pennsylvanian swamps. Changes in microspore assemblages at the Asturian/Cantabrian boundary mirr...
Sites yielding Pennsylvanian (late Carboniferous) coal floras are well known across Europe and North...
By maceration of coal it is possible to extract microfossils that consist of various plant parts. Th...
Includes bibliographical references."Reprinted from the Journal of geology, vol. 50, no. 3, 1947.
The distribution and relative amounts of six genera of lycophyte microspores, Lycospora, Densosporit...
Plant fossils are recorded and described from Duckmantian clastic strata associated with coal seams ...
Plant fossils are recorded and described from Duckmantian clastic strata associated with coal seams ...
Author Institution: Department of Botany, Ohio UniversityThe Upper Pennsylvanian (Conemaugh Group) D...
Pennsylvanian System of North America. Int. J. Coal Geol., 5: 43—109. Quantitative analysis of Penns...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
Large leafy calamite stems are very rare in the fossil record. One such leafy stem is described as a...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
Large leafy calamite stems are very rare in the fossil record. One such leafy stem is described as a...
Sites yielding Pennsylvanian (late Carboniferous) coal floras are well known across Europe and North...
By maceration of coal it is possible to extract microfossils that consist of various plant parts. Th...
Includes bibliographical references."Reprinted from the Journal of geology, vol. 50, no. 3, 1947.
The distribution and relative amounts of six genera of lycophyte microspores, Lycospora, Densosporit...
Plant fossils are recorded and described from Duckmantian clastic strata associated with coal seams ...
Plant fossils are recorded and described from Duckmantian clastic strata associated with coal seams ...
Author Institution: Department of Botany, Ohio UniversityThe Upper Pennsylvanian (Conemaugh Group) D...
Pennsylvanian System of North America. Int. J. Coal Geol., 5: 43—109. Quantitative analysis of Penns...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
Large leafy calamite stems are very rare in the fossil record. One such leafy stem is described as a...
The link between vegetation and climate change during the Pennsylvanian Subperiod is of significant...
Large leafy calamite stems are very rare in the fossil record. One such leafy stem is described as a...
Sites yielding Pennsylvanian (late Carboniferous) coal floras are well known across Europe and North...
By maceration of coal it is possible to extract microfossils that consist of various plant parts. Th...
Includes bibliographical references."Reprinted from the Journal of geology, vol. 50, no. 3, 1947.