The Pennsylvanian is a subperiod of the Carboniferous period lasting from roughly 318.1± 1.3  to 299± 0.8 Ma (million years ago). As with most other geologic periods, the rock beds that define the period are well identified, but the exact date of the start and end are uncertain by a few million years. The Pennsylvanian is named after the state of Pennsylvania, where rocks from this age are widespread.

Generalized geographic map of the United States in Middle Pennsylvanian time.

In North America, where the early Carboniferous beds are primarily marine limestones, the Pennsylvanian is treated as a full fledged geologic period between the Mississippian and the Permian. In Europe, the Mississippian and Pennsylvanian are one more-or-less continuous sequence of lowland continental deposits and are grouped together as the Carboniferous period.

All modern classes of fungi were present in the Late Carboniferous (Pennsylvanian Epoch).^[1]

External links

The references used in this article may be clearer with a different or consistent style of citation, footnoting, or external linking.

• http://www.scotese.com/late.htm Provides a picture of the world from this time period.
• http://www.ucmp.berkeley.edu/carboniferous/carboniferous Information on stratigraphies, localities, tectonics, and life.
• http://www.palaeos.com/Paleozoic/Carboniferous/Pennsylvanian.htm

 This geochronology article is a stub. You can help Wikipedia by expanding it.