During the Permian, all the Earth's major landmasses were collected into a single supercontinent known as Pangaea, with the microcontinental terranes of Cathaysia to the east.

Wikipedia contributors. (2023, November 13). Permian. In Wikipedia, The Free Encyclopedia. Retrieved November 17, 2023, from https://en.wikipedia.org/w/index.php?title=Permian&oldid=1184912510

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Permian (Wikipedia) The Permian (/ˈpɜːrmi.ən/ PUR-mee-ən) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period 298.9 million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia.

During the Permian, all the Earth’s major landmasses were collected into a single supercontinent known as Pangaea, with the microcontinental terranes of Cathaysia to the east.

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