Final answer:
The supercontinent Pangaea existed around 300 to 200 million years ago and included all of Earth's continental crust. Alfred Wegener proposed the theory of continental drift, supporting it with evidence like similar fossils on separated continents. Pangaea's breakup, due to plate tectonics, facilitated distinct evolutionary paths for species on the resulting continents.
Step-by-step explanation:
The concept of Pangaea refers to the supercontinent that existed during the late Paleozoic and early Mesozoic eras, about 300 to 200 million years ago (Ma). It was during this time when nearly all of Earth's continental crust was assembled into this gigantic landmass. The geological evidence and scientific consensus support the notion that the breaking up of Pangaea, due to plate tectonics, led to the formation of the seven continents as we know them today.
German scientist Alfred Wegener is credited with the hypothesis of continental drift, which he proposed in 1915. Wegener compiled evidence suggesting that the continents were once conjoined, citing similar fossils found on distant continents, congruent coastlines, and matching geological structures across oceans. While initially controversial, Wegener's theory laid the groundwork for the modern theory of plate tectonics, which was only widely accepted in the 1960s.
During the existence of Pangaea, the Earth experienced extreme climates and habitat changes that greatly influenced biodiversity and evolution. The structure of Pangaea itself limited marine diversity by reducing shallow coastal habitats, contributing to the end-Permian mass extinction. Following the breakup, distinct biogeographical patterns emerged, with unique species developing on the derivatives of the supercontinent, such as Laurasia and Gondwana.