Supporting information for: Paleosol-based reconstruction indicates decoupling of mean annual precipitation and precipitation intensity during the Paleocene-Eocene Thermal Maximum in the Uinta Basin, Utah

Supporting materials for Slawson et al. 2024 "Paleosol-based reconstruction indicates decoupling of mean annual precipitation and precipitation intensity during the Paleocene-Eocene Thermal Maximum in the Uinta Basin, Utah." Figure S1. Paleosol-based composite measured section from Nine Mile Canyon. The pedotypes are listed to the right of the associated paleosols. Table S1. d13C/12C of the dispersed organic carbon in floodplain deposits. The unit of measurement is per mille relative to the VPBD standard. Table S2. Major elemental oxide data for the paleosol samples listed by stratigraphic height (m). Table S3. Mass balance calculations and mean annual precipitation (MAP) estimates for the collected paleosol samples. MAP estimates using the CIA-K, RF-MAP 2.0, and PPM1.0 climofunctions are included.