STABLE ISOTOPIC PALEOHYDROLOGY OF PEDOGENIC CARBONATE NODULES FROM PLIOCENE PALEOSOLS IN THE MEADE BASIN, SOUTHWESTERN KANSAS
In this study, we utilize cathodoluminescence (CL) imagery to guide a micro-sampling campaign for stable isotopic analyses (δ13C and δ18O) of carbonate components that have discrete luminescence characteristics mapped at the thin section scale. Pedogenic carbonate nodules from five discrete superimposed paleosols were investigated from one Pliocene-aged lithostratigraphic section in the Meade Basin.
CL images indicate that all paleosol samples have undergone some degree of phreatic overprinting. Isotopic results reveal different diagenetic trends in C and O space that provide information about paleohydrologic processes. These trends include meteoric calcite lines (MCL) that indicate early meteoric diagenesis and positive linear covariant trends (PLCT) that reveal evaporative effects during carbonate precipitation.
In three of the samples, four discrete MCLs were identified with δ18O values of -9.36, -9.38, -9.46, and -9.64‰ VPDB, suggesting subtle variations in either the δ18O value of meteoric water or temperature during carbonate formation. Variations in δ13C values between the different MCLs (-4.48 to +0.55‰ total range) suggest different dissolved inorganic carbon sources in the groundwater systems. Four PLCT patterns were also apparent and differ from their respective MCLs by between 0.61 and 1.46‰, indicating slightly different degrees of evaporative enrichment. Two other samples are characterized by relatively invariant carbon and oxygen isotopic values. Nonetheless, clear differentiation is apparent between components with different CL characteristics.
Ongoing petrographic work will enable us to characterize the morphology of different carbonate components and further delineate and interpret diagenetic features.