The Triassic-Jurassic (T-J) transition interval (ca. 200 Ma) is characterized by a major mass extinction in which major biotic turnover occurred in both marine and terrestrial realms. However, studies on the terrestrial response to this event are still limited, especially in the eastern Tethys region of eastern Asia.
Click here for original story, Study reveals palaeovegetation and palaeoclimate changes across Triassic-Jurassic transition in south China
Source: Phys.org