2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)

Paper No. 292-12
Presentation Time: 11:25 AM


BEVERLY, Emily J., Terrestrial Paleoclimatology Research Group, Department of Geology, Baylor University, One Bear Place #97354, Waco, TX 76798-7354, DRIESE, Steven G., Terrestrial Paleoclimatology Research Group, Dept. of Geosciences, Baylor University, One Bear Place #97354, Waco, TX 76798-7354, PEPPE, Daniel J., Department of Geology, Baylor University, One Bear Place #97354, Waco, TX 76798-7354, FAITH, J. Tyler, School of Social Science, University of Queensland, Michie Building (#9), Brisbane, 4072, Australia, TRYON, Christian A., Department of Anthropology, Harvard University, Cambridge, MA 02138, ROURE-JOHNSON, Cara A., Department of Anthropology, University of Connecticut, U-2176, Storrs, CT 06269, MICHEL, Lauren A., Perot Museum of Nature and Science, 2201 N. Field Street, Dallas, TX 75201 and SHARP, Warren D., Berkeley Geoochronology Center, 2455 Ridge Road, Berkeley, CA 94709

Although the effects of changing paleoclimate and paleoenvironment on the evolution of Pleistocene Homo sapiens continues to be heavily debated, few data from equatorial East Africa are available prior to the Last Glacial Maximum (LGM). Lake Victoria (LV) spans the equator between the eastern and western branches of the East African Rift and is the largest tropical freshwater lake by surface area (~64,400 km2) but is only 68 m deep. The shallow depth and dependence on direct precipitation to maintain lake levels makes LV sensitive to changes in precipitation. Middle to Late Pleistocene deposits on the shoreline of eastern LV preserve an abundance of vertebrate fossils and Stone Age artifacts, and riverine tufas identified at the base of the deposits are ideal for paleoenvironmental reconstructions. Here we present new data on tufas identified at Rusinga Island and on the mainland near Karungu, Kenya. Tufas were described and sampled for micromorphology, mineralogy, bulk geochemistry, stable isotopes and U-series at four sites: Nyamita, Aringo, Kisaaka, and Onge. Additional dates are in progress but Aringo has a U-series age of 455±45 ka (95% CI). Seven carbonate facies and three clastic facies cemented by syn-depositional calcite were identified. Poor sorting of clastic sediments indicates flashy, ephemeral discharge, but barrage tufas and paludal areas with δ13C values of ~-10‰ are indicative of C3 macrophyes (e.g., Typha). Other sites have a mixed C3/C4 signature that suggests a semi-arid C4 grassland surrounding these spring-fed rivers. The δ18O of tufa from Nyamita is on average ~1‰ more negative than calcite precipitated from modern rainfall in the LV Basin, which suggests less contribution of catchment rainfall and more enriched monsoonal input similar to the LGM. Positive increases in both δ13C and δ18O at other sites suggest increased evaporation or CO2 degassing. Both Nyamita and Aringo (~40 km apart) record cyclicity in isotopic composition and stromatolite lamina type likely tied to sub-Milankovitch cycles, such as El Niño. The tufas indicate that climate was significantly drier than modern LV, but the presence of spring-fed rivers would have afforded animals a more reliable water source (aquifer vs. precipitation), allowing for a more diverse plant and animal community in an otherwise arid environment.