Supplemental Material: Terrestrial paleoclimate transition associated with continental weathering and drift during the Aptian–Albian of East Asia
Table S1: Climate indicators from element and isotope geochemistry, and clay and carbonate minerals from boreholes FY-2, FY-1, and DY-1 in the Fuxin Basin. Table S2: Palynomorph assemblage from borehole FY-2 in the Fuxin Basin. Figure S1: Correlated sequence stratigraphy and sedimentary facies with positions of measured samples in the Fuxin Basin from borehole FY-2 in the west (A), FY-1 in the center (B), and DY-1 in the east (C) (modified after Jia et al., 2021). Figure S2: Diagrams of Al2O3 and TiO2 and δ13C and δ18O values for organic-rich mudrocks from boreholes FY-2 (A, D), FY-1 (B, E), and DY-1 (C, F). Figure S3. Microscopic characteristics of carbonate minerals observed in SEM (A) and thin section images (B) of organic-rich mudrocks from borehole FY-2.