Palaeoclimatic estimates for the late pliocene based on leaf physiognomy from Western Yunnan, China

Based on leaf physiognomy of the Late Pliocene Tuantian megaflora from the Mangbang Formation of Tengchong County in western Yunnan, a quantitative reconstruction of palaeoclimate was performed with Leaf Margin Analysis (LMA) methodology and the Climate–Leaf Analysis Multivariate Program (CLAMP).