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- https://geo.libretexts.org/Courses/Fullerton_College/Introduction_to_Geology/08%3A_Earth_HistoryFrom the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a gener...From the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a general understanding of these changes can put present change into a more rounded perspective. The rocks are Permian in age and formed in the desert conditions that dominated North America toward the end of the Paleozoic through the middle Mesozoic.
- https://geo.libretexts.org/Courses/Fullerton_College/Introduction_to_Earth_Science_(Ikeda)/08%3A_Earth_HistoryFrom the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a gener...From the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a general understanding of these changes can put present change into a more rounded perspective. The rocks are Permian in age and formed in the desert conditions that dominated North America toward the end of the Paleozoic through the middle Mesozoic.
- https://geo.libretexts.org/Courses/Gettysburg_College/Book%3A_An_Introduction_to_Geology_(Johnson_Affolter_Inkenbrandt_and_Mosher)/15%3A_Earth_HistoryFrom the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a gener...From the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a general understanding of these changes can put present change into a more rounded perspective. The rocks are Permian in age and formed in the desert conditions that dominated North America toward the end of the Paleozoic through the middle Mesozoic.
- https://geo.libretexts.org/Courses/California_State_University_Los_Angeles/Book%3A_An_Introduction_to_Geology_(Johnson_Affolter_Inkenbrandt_and_Mosher)/10.0%3A_Earth_HistoryFrom the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a gener...From the oxygenation of the atmosphere, the progression of life forms, the assembly and deconstruction of several supercontinents, to the extinction of more life forms than exist today, having a general understanding of these changes can put present change into a more rounded perspective. The rocks are Permian in age and formed in the desert conditions that dominated North America toward the end of the Paleozoic through the middle Mesozoic.
