Abstract
The Permian Period represents both a transition and a beginning in global paleoclimate. Continental glaciation, which peaked in the Late Carboniferous, declined and ceased during the Permian, and climate typical of the Pangean (Permian through Middle Jurassic; Parrish 1992) megamonsoon (Kutzbach and Gallimore 1989) began. The purpose of this chapter is to provide a global paleoclimatic context for this Volume, by summarizing current information about the development of global climate during the Permian Period.
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CITATION STYLE
Parrish, J. T. (1995). Geologic Evidence of Permian Climate. In The Permian of Northern Pangea (pp. 53–61). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-78593-1_4
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