Introduction: Individual grains and small lithic clasts in thin-sectioned suevitic breccia samples from the International Continental Scientific Drilling Program (ICDP) Bosumtwi impact crater drillcore LB07A were examined petrographically to evaluate the occurrence , abundance, and characteristics of unshocked and shock-metamorphosed quartz. The analyzed samples were taken across a ~42-m-long (...

Age-estimates ranging from 50 to 70 ky were obtained for the Mousterian deposits of Amud Cave in Israel from thermoluminescence measurements performed on 19 burnt flints. The late dates obtained for the stratigraphic layers bearing hominid remains confirm the evidence for the late presence of Neanderthals in the Levant. The dates enable a more effective comparison of the lithic assemblages from...

There are multiple hypotheses for human responses to glacial cycling in the Late Pleistocene, including changes in population size, interconnectedness, and mobility. Lithic technological analysis informs us of human responses to environmental change because lithic assemblage characteristics are a reflection of raw material transport, reduction, and discard behaviors that depend on hunter-gather...

The human settlement of Europe during Pleistocene times was sporadic and several stages have been recognized, both from paleaoanthropological and archaeological records. If the first phase of hominin occupation (as early as 1.4 Ma) seems mainly restricted to the southern part of the continent, the second phase, characterized by specific lithic tools (handaxes), is linked to Acheulean settlement...

Sibudu in KwaZulu-Natal (South Africa) with its rich and high-resolution archaeological sequence provides an ideal case study to examine the causes and consequences of short-term variation in the behavior of modern humans during the Middle Stone Age (MSA). We present the results from a technological analysis of 11 stratified lithic assemblages which overlie the Howiesons Poort deposits and all ...

Ab stract Klissoura Cave 1 is lo cated in the north east ern edge of the Argive Plain, Peloponnese, at the en trance of the Berbadiotis river gorge. The cave com prises a col lapsed cave cham ber and a rockshelter area. The strati graphic anal y sis and micromorphological study of the sed i ments elu ci dated the main pro cesses in volved in the for ma tion of the site and its depositional his ...