GSA Annual Meeting in Denver, Colorado, USA - 2016

Paper No. 281-5
Presentation Time: 9:15 AM


MATMON, Ari1, HIDY, Alan J.2, VAINER, Shlomy3, CROUVI, Onn4, FINK, David5, EREL, Yigal3, ASTER, Team6, HORWITZ, Liora K.7 and CHAZAN, Michael8, (1)The Fredy and Nadine Harrmann Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram campus, Jerusalem, 91904, Israel, (2)Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, 7000 East Avenue, Livermore, CA 94550, (3)The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University, Givat Ram, Jerusalem, 91904, Israel, (4)Geological Survey of Israel, 30 Malkhe Israel St, Jerusalem, 95501, Israel, (5)Australian Nuclear Science and Technology Organization, PMB1, Menai, NSW 2234, Australia, (6)ASTER - CEREGE, CNRS-Aix-Marseille University, UMR 6635, BP 80,, Aix en Provence, 13 545 Cedex 4, France, (7)National Natural History Collections, Faculty of Life Science, Hebrew University, Berman Building, The Hebrew University, Jerusalem, Jerusalem, 91904, Israel, (8)Department of Anthropology, University of Toronto, 19 Russell Street, Toronto, ON M5S 2S2, Canada,

Kalahari Group sediments accumulated in the Kalahari basin, which started forming during the breakup of Gondwana in the early Cretaceous. These sediments cover an extensive part of southern Africa and form a low-relief landscape. Current models assume that the Kalahari Group accumulated throughout the entire Cenozoic. However, chronology has been restricted to early-middle Cenozoic biostratigraphic correlations and to OSL dating of only the past ~300 ka. We present a new chronological framework that reveals a dynamic nature of sedimentation in the southern Kalahari. Cosmogenic burial ages obtained from a 55 m section of Kalahari Group sediments from the Mamatwan Mine, southern Kalahari, indicate that the majority of deposition at this location occurred rapidly at 1–1.2 Ma. This Pleistocene sequence overlies the Archaean basement, forming a significant hiatus that permits the possibility of many Phanerozoic cycles of deposition and erosion no longer preserved in the sedimentary record. Calcretes that cement conglomerates and sands throughout the sequence are dated with U-series to range between 300-500 ka, much younger than previously assumed. Our data also establish the existence of a shallow water body that persisted for >450 ka prior to this rapid period of deposition and is associated with early-middle Pleistocene high-density hominin occupation.