Human Settlement Distribution Patterns During The Longshan And Xinzhai-Erlitou Periods And Their Hydrogeomorphic Contexts In The Central Plains, China

The Central Plains of China witnessed a crucial cultural transformation towards the end of the Longshan period from a chiefdom-like society to a state-level society that has been speculated to be associated with regionally favorable environmental conditions. However, this speculation has not yet been substantiated. We first compiled the information on human migrations and extreme floods during the late Longshan period and then compared the relationships of human settlements with hydrogeomorphic settings in the Central Plains between the Longshan and Xinzhai-Erlitou periods. Our comparison shows that the course of the Yellow River was relatively stable during the Longshan period in the eastern Central Plains, where abundant highlands might have existed for human dwellings. However, geologically and archaeologically documented extreme floods that occurred at similar to 4000 cal. yr BP changed hydrogeomorphic settings in key locations along the Yellow River. The northern Henan area and the bordering area of Henan, Shandong and Anhui Provinces were subjected to frequent crevasses from flooding of the Yellow River at similar to 4000 cal. yr BP, which might have forced human migrations. Consequently, the northern Henan area and the bordering area of the three provinces lacked human settlements, whereas the western Central Plains contained concentrated human settlements during the Xinzhai-Erlitou period. We propose that the success of the above-mentioned cultural transformation was likely causally associated with hydrogeomorphic setting changes in the lower Yellow River Basin. Specifically, the frequent crevasses from flooding of the Yellow River at similar to 4000 cal. yr BP in the eastern alluvial plain regions made the western hilly and mountainous regions of present-day Henan Province the "refuge" for eastern immigrants during the late Longshan period. After the floods, human reoccupation and subsequent population increase beyond the local optimum carrying capacity within the Luoyang Basin during the Erlitou period might be a key driver of local social complexity.