Peat depositional environments, the sites where and conditions under which peat
accumulates, significantly influence a resultant coal's physical properties, chemical …

▪ Abstract Late Carboniferous and Early Permian strata record the transition from a cold
interval in Earth history, characterized by the repeated periods of glaciation and deglaciation …

Nonmarine biostratigraphic/biochronologic schemes have been created for all or parts of the
late Carboniferous–Middle Triassic using palynomorphs, megafossil plants, conchostracans …

There have been at least ten English-language textbooks of palaeobotany since DH Scott
published the first edition of Studies inFossilBotany in 1900. Most have been written by …

Premise of research. The Late Paleozoic Ice Age was the last extensive pre-Pleistocene ice
age. It includes many climate changes of different intensities, permitting examination of …

ABSTRACT A change to global greenhouse conditions following deglaciation occurred
during the late Paleozoic. The deep-past data set preserved in the stratigraphic record can …

Quantitative analysis of Pennsylvanian coal-swamp vegetation provides a means of inferring
organization and structure of communities. Distribution of these communities further …

Improved regional and interregional stratigraphic correlations of Pennsylvanian strata permit
comparisons of vegetational changes in Euramerican coal swamps. The coal-swamp …

The climatic influences on vegetation in the present world can serve as an excellent model
for the Permian, there being approximately the same level of floral differentiation and the …

Diverse wetland vegetation flourished at the margins of the Midland Basin in north-central
Texas during the Pennsylvanian Period. Extensive coastal swamps and an ever-wet, tropical …