Climate variabilities at the intra-HC, HC, IC, and LC scales were interpreted from sedimentary and paleosol evidence. Four prominent climatic shifts are present: 1) from the humidx2013;subhumid to highly-variable subhumidx2013;semiarid conditions at the beginning of Sakamarian; 2) from highly-variable subhumidx2013;semiarid to humidx2013;subhumid conditions across the Artinskian-Capitanian unconformity; 3) from humidx2013;subhumid to highly-variable subhumidx2013;semiarid conditions at early Induan; and 4) from the highly-variable subhumidx2013;semiarid to humidx2013;subhumid conditions across the Olenekian-Anisian unconformity. The stable humidx2013;subhumid condition from Lopingian to early Induan implies that paleoclimate change may not have been the cause of the end-Permian terrestrial mass extinction. A close documentation of the pace and timing of the extinction and exploration of other causes are needed. In addition, the semiaridx2013;subhumid conditions from Sakamarian to Artinskianx2013;Kungurian (?) and from middle Induan to end of Olenekian are in conflict with modern mid-latitude east coast meso- and macrothermal humid climate. Extreme continentality, regional orographic effect, and/or abnormal circulation of Paleo-Tethys maybe are possible causes. Our work serves as a rare data point at mid-latitude NE Pangea for climate modeling to seek explanations on the origin(s) of climate variability in NE Pangea from latest Carboniferous to Early Triassic.