Climate variability in the Upper Jordan Valley around 0.78 Ma, inferences from time-series stable isotopes of Viviparidae, supported by mollusc and plant palaeoecology

The Early-Middle Pleistocene lacustrine sediments at Gesher Benot Ya'aqov (GBY) in the Upper Jordan Valley span ca. 100 Ka across the Matuyama-Brunhes Boundary (MBB) at 780 Ka and oxygen isotope stages (OISs) 20 to 18, provide a continuous record of their sedimentary history and prevailing climate. The lacustrine environment is investigated using ecological and stable isotope characteristics of gastropods belonging to the family Viviparidae supplemented by other molluscan and floral indicators. The sedimentary framework of the 34 in thick sequence is bounded by channel conglomerates at its base and top, and consists of six sedimentary cycles Each one starts with shore sediments (coquina and sand) and ends with deeper water sediments (black mud or gray mud) Time series of delta O-18 and delta C-13 values were determined in individual shells belonging to two sympatric genera of viviparid gastropods: Viviparus apameae gahleae and Bellamya sp found in the sedimentary cycles 2 through 5. The total overall range of delta O-18 in the time series of all the shells is from -10 5 parts per thousand to -5 2 parts per thousand (VPDB), and the delta C-13 from -9.2 parts per thousand to -4 8 parts per thousand (VPDB). The delta C-13 values of shells recovered from black mud are lower than those from the other sediment types suggesting a higher proportion of carbon of organic origin. The delta C-18 values show only a weak relation with sediment type. The time series of the individual shells indicate a relative constancy in the water delta C-18 and temperature whilst the variation in delta C-13 could be related to the annual productivity cycle (growth and decay of aquatic plants) of the lake. The delta C-13 patterns in the time series and winter rings indicate that the rate of growth of the individual snails was ca. 15-30 mm/year. The isotopic characteristics of the Viviparid shells from these beds indicate diverse sedimentary environments and suggest that above the MBB (cycles 2-5) the GBY lake received constant and isotopically consistent water inflow. Our integrated data, isotopic and ecological of molluscs. and ecological of plants. indicates that the geophysical-magnetic phenomenon of MBB coincides with an environmental change from a relatively cold dry climate towards a warmer temperate subtropical climate in this region. This change coincides with the occurrence of hominin artifacts, which were found mainly in layers of the sedimentary cycles 3-5. (C) 2009 Elsevier B.V. All rights reserved.