Fig. 4From: Characteristics and evolution of inertinite abundance and atmospheric pO2 during China’s coal-forming periodsReconstruction map of global palaeogeographic environment during Middle–Late Jurassic (175–146 Ma) (Li and Jiang 2013). Note: The time node of plate reconstruction is 160 Ma. Orogenic belt (Golonka 2011); Shallow sea (Golonka 2011); Ocean currents (Scotese 2002); Paleoclimate (Sellwood and Valdes 2008)Back to article page