Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) is a Homo sapiens partial calvaria from site GvJm-22 at Lukenya Hill, Kenya, associated with Later Stone Age (LSA) archaeological deposits. KNM-LH 1 is securely dated to the Late Pleistocene, and samples a time and region important for understanding the origins of modern human diversity. A revised chronology based on 26 accelerator mass spectrometry radiocarbon dates on ostrich eggshells indicates an age range of 23,576–22,887 y B.P. for KNM-LH 1, confirming prior attribution to the Last Glacial Maximum. Additional dates extend the maximum age for archaeological deposits at GvJm-22 to >46,000 y B.P. (>46 kya). These dates are consistent with new analyses identifying both Middle Stone Age and LSA lithic technologies at the site, making GvJm-22 a rare eastern African record of major human behavioral shifts during the Late Pleistocene. Comparative morphometric analyses of the KNM-LH 1 cranium document the temporal and spatial complexity of early modern human morphological variability. Features of cranial shape distinguish KNM-LH 1 and other Middle and Late Pleistocene African fossils from crania of recent Africans and samples from Holocene LSA and European Upper Paleolithic sites.

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The late Middle Palaeolithic (MP) settlement patterns in the Levant included the repeated use of caves and open landscape sites. The fossil record shows that two types of hominins occupied the region during this period—Neandertals and Homo sapiens. Until recently, diagnostic fossil remains were found only at cave sites. Because the two populations in this region left similar material cultural remains, it was impossible to attribute any open-air site to either species. In this study, we present newly discovered fossil remains from intact archaeological layers of the open-air site ‘Ein Qashish, in northern Israel. The hominin remains represent three individuals: EQH1, a nondiagnostic skull fragment; EQH2, an upper right third molar (RM3); and EQH3, lower limb bones of a young Neandertal male. EQH2 and EQH3 constitute the first diagnostic anatomical remains of Neandertals at an open-air site in the Levant. The optically stimulated luminescence ages suggest that Neandertals repeatedly visited ‘Ein Qashish between 70 and 60 ka. The discovery of Neandertals at open-air sites during the late MP reinforces the view that Neandertals were a resilient population in the Levant shortly before Upper Palaeolithic Homo sapiens populated the region.

Studying the distribution of lithic raw materials around prehistoric sites, their procurement, transport, and use, are important for understanding organizational decisions of hunter-gatherers. Here we examine lithic technological organization in two stratigraphic subunits B4 and B1 (dated ß 68 and ß 55 ka, respectively) at the Neanderthal site of Amud Cave. The lithic assemblages are made exclusively of flint. An ArcGIS model is used to create a predictive model for daily exploitation territories (DETs) around the site. Using a battery of statistical methods (ANOVA, principal component analysis, and cluster analysis), we link flint visual types with geochemical characteristics (obtained through inductively coupled plasma (ICP) mass spectrometry and ICP atomic emission spectrometry) of both geological and archaeological flints. Results indicate that local materials are abundant in both subunits. Nonlocal raw materials (from areas beyond the modeled DET) amount to 30-40% across all technological categories, suggesting long-distance transport. The technological patterns of the nonlocal raw material differ between the two subunits. Pending results of additional work, we suggest that nonlocal flint types were likely obtained from distances >60 km. Mobility patterns inferred from this study suggest that Amud Cave was a focal location within its settlement system during both occupation periods, but the manner of site use and mobility patterns changed through time. C 2016 Wiley Periodicals, Inc.

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