Unraveling the paleoclimatic proxy signatures embedded in paleosols during the Late Triassic

Documents vertical progression in the major paleosol types in response to regional tectonics and long-term climate change

Providing evidence for the northward migration of equatorial Pangea from dry subtropical latitudes toward humid, wet equatorial, possibly monsoonal, paleoclimatic zone during the Late Triassic

Plinthite/laterite indicating the prevalence of a wet equatorial climate characterized by extensive chemical weathering