“…The arthropod inclusions in Zhangpu amber and plant fossil assemblage both suggest that the middle Miocene Zhangpu biota is a megathermal (currently "tropical") rainforest biome (Wang et al, 2021a). The plant fossil assemblage consists of Osmundaceae, Schizaeaceae, Smilacaceae, Altingiaceae, Anacardiaceae, Annonaceae, Burseraceae, Clusiaceae, Coriariaceae, Dipterocarpaceae, Elaeocarpaceae, Euphorbiaceae, Fagaceae, Lauraceae, Leguminosae, Magnoliaceae, Melastomataceae, Moraceae, Myrtaceae, Myristicaceae, Rhamnaceae, Salicaceae, Urticaceae, Trapaceae, and Nelumbonaceae (Shi & Li, 2010;Shi et al, 2014b;Jacques et al, 2015;Lin et al, 2015;Wang et al, 2017Wang et al, , 2019aWang et al, , 2019bWang et al, , 2019cWang et al, , 2019dWang et al, , 2020Wang et al, , 2021aWang et al, , 2021bWang et al, , 2022aWang et al, , 2022bDong et al, 2018aDong et al, , 2018bDong et al, , 2021Dong et al, , 2022Beurel et al, 2023;Wu et al, 2023;Yin et al, 2023). Paleoclimate estimates based on leaf physiognomy also reveal that the middle Miocene flora in Zhangpu represents a tropical seasonal rainforest with a mean annual temperature of ~22.5°C, a warm month mean temperature of ~27.1°C, a cold month mean temperature of ~17.2°C, nearly 12-month growing seasons, and growing season precipitation of ~1929 mm (Wang et al, 2021a).…”