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Which European subsystems are used to divide the Carboniferous Period?
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Carboniferous Period
Distribution of landmasses, mountainous regions, shallow seas, and deep ocean basins during the late Carboniferous Period. Included in the paleogeographic reconstruction are the locations of the interval's subduction zones.
In Europe, the Carboniferous Period is traditionally subdivided into two subsystems: the Dinantian and the succeeding Silesian.1
It is important to note that this European classification differs from the internationally accepted division of the Carboniferous into the Mississippian and Pennsylvanian subsystems. Specifically, the boundary between the Dinantian and Silesian divisions occurs below the internationally recognized boundary between the Mississippian and Pennsylvanian.21