Provenance evolution of the northern Weihe Basin as an indicator of environmental changes during the Quaternary

AbstractThe Weihe Basin is an intracontinental rift basin in central China that provides an ideal location for studying the interactions between regional tectonics and monsoonal climate change. In this paper, we present detrital zircon U–Pb ages from sediments from Core LYH drilled in the northern margin of the basin. We use these to illuminate changing sediment transport processes, provenance and palaeo-environments during the Quaternary. The sediments are dominated by zircon age groups of 100–400 Ma and 400–550 Ma, and three secondary age peaks at 700–1100 Ma, 1700–2100 Ma and 2400–2600 Ma. Multidimensional scaling plots support the conclusion that the Central Loess Plateau and the Luo River are the dominant sources of sediments to the core site. Before c. 1.06 Ma, the Qinling Mountains and the Wei River, as well as the Yellow River, had minor influence on the sedimentation at the core site. These results are consistent with the existence of a palaeolake prior to 1.06 Ma, which allowed sediments supplied to the south and east edge of the basin to be reworked to the northern side of the Weihe Basin. Subsequently, the Luo River has provided a steady source of sediments to the northern Weihe Basin.</jats:p

Lithic production strategies during the late Middle Pleistocene at Dali, Shaanxi Province, China: implications for understanding late archaic humans

The Dali hominid site is well known as it contains a human cranium associated with stone artefacts and animal bones. Dating efforts have provided an age range of ~ 300–247 ka for these remains. Renewed study of the cranium in recent years has revealed a mix of archaic traits in the neurocranium and derived features in the face, and thus, this specimen may provide insight into our understanding of modern human evolution in China. However, the technological behaviour possessed by these people has remained unclear due to a lack of new and detailed research. In this paper, we re-examine the lithic assemblages from Dali, originally excavated in 1978 and 1980, and for the first time, we now provide a sound assemblage by removing those geofacts that have been used in past archaeological reports. Although the total number of artefacts is now smaller, our results show that core reduction strategies at Dali are primarily expedient, dominated by simple unifacial unidirectional flaking. In contrast, the formal tools exhibit relatively advanced technology, with artefacts that are diverse in type and characterized by a relatively standardized production strategy. In contrast to the widely accepted model for slow and conservative technological development in Chinese Palaeolithic technology, pre 40 ka, here, we suggest that there is evidence for gradual technological changes from the Early to Middle and early Late Pleistocene.The Chinese Academy of Sciences Pioneer Hundred Talents Program and the Chinese Academy of Sciences Strategic Priority Research Program Grant (No. XDPB05). MGL would like to acknowledge funding support provided by the National Research Foundation (NRF) of South Africa and the Palaeontological Scientific Trust (PAST) with its Scatterings of Africa programs.https://link.springer.com/journal/125202020-05-01hj2018Anthropology and Archaeolog