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Paper No. 6
Presentation Time: 2:50 PM

GEOARCHAEOLOGY OF THE LATE BRONZE AGE IN SOUTHERN UKRAINE: PRELIMINARY RESULTS


FADEM, Cynthia M.1, MIDDLEBROOKS, Zoe T.2, GILLESPIE, P. Geer2, GERSHKOVICH, Yakiv P.3, GORBENKO, Kiril G.4, FILATOV, Dmitry4 and EFREMOV-KENDALL, Nicholas5, (1)Department of Geosciences, Earlham College, 801 National Rd W, Campus Drawer 132, Richmond, IN 47374, (2)Geosciences, Earlham College, 801 National Rd W, Campus Drawer 132, Richmond, IN 47374, (3)Institute of Archaeology/Інст. Aрхеології, Ukrainian Academy of Sciences/Нац. Академія На , вул.Героїв Сталінгра, Kyiv/м.Київ, 04210, Ukraine, (4)Institute of History & Law/Iнcт. Icтоpії та Пpава, Mikolayiv State University/Mикoлаївcький Д. У, пл. Комунарів, 1, кімн. 1, Mikolayiv/м. Mикoлаїв, 54003, Ukraine, (5)Department of Anthropology, Washington University, 1 Brookings Dr, St Louis, MO 63130, fademcy@earlham.edu

Current work in southern Ukraine seeks to elicit the ecological circumstances of the Bronze Age-Iron Age transition. Traditionally thought to be represented by a cultural shift from sedentism to nomadism, this transition is poorly represented archaeologically. This summer’s fieldwork at the Late Bronze Age (3.5-2.5 ka) sites of Rozanivka/Розанівка, Reprinka/Репринка, and Dikij Sahd/Дикий Сад revealed relatively fertile alfisols. The soil parent at Rozanivka and Reprinka is the Archaean granulite-gneiss of the Ukrainian Shield/Український щит, while soils at Dikij Sahd are sourced in alluvial sand deposits. Though pollen records from other sites indicate a drying trend for the terminal Bronze Age, our initial results indicate relative stability in soil-forming processes from occupation to the present. Geochemical and geomorphological analyses are also underway for each site.
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