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Earth Pennsylvanian PeriodThe Pennsylvanian time period lasted from 325 to 286
million years ago, a time span of 39 million years. The term Pennsylvanian
was first used in the late 1800s to describe a sequence of rocks in, of
all places, Pennsylvania. In Europe the time period just above the Devonian
was named the Carboniferous because of the abundant coal beds found in
them. However, in the United States geologists divided the Carboniferous
into two periods, the Mississippian and the Pennsylvanian. These Pennsylvanian
rocks were defined based on a particular type of fossil assemblage contained
within them. They are located above the rocks of the Mississippian
System and below the rocks of the Permian System.
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