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Exploring the influence range of early cities is significant for understanding the mechanisms behind ancient settlement systems and human-environment interactions. Due to a lack of effective research methods, the evolution processes and impact mechanisms of the influence ranges of prehistoric cities are still ambiguous. In this study, we chose the Songshan Mountain region for research, which witnessed the origin and development of Chinese civilization. Using GIS spatial analyses such as the 'average nearest neighbor' and 'Thiessen polygon', we explored the spatial-temporal distributions and influence ranges of Neolithic-Bronze Age cities in the region. The roles of human culture and the natural environment in the process were also investigated. The results indicated that the spatial distributions of early cities were random during the Yangshao (7000–5000 BP) and Longshan (5000–4000 BP) cultures. During the Erlitou culture (3800–3500 BP) and Shang Dynasty (3600–3046 BP), the spatial distributions changed into dispersed models. During the Zhou Dynasty (3046–2256 BP), the spatial distribution model was random again. Correspondingly, the influence range of early cities during the Erlitou culture is the largest, followed by those of the Longshan culture, Yangshao culture, Shang Dynasty, and Zhou Dynasty. This is different from the conventional view that the ancient city's influence range continuously expands as time advances. Both the natural environment and human culture are believed to impact this evolutional process. Specifically, the Holocene climate variation and the consequent cyclic river downcutting and silting affect the city site selection and thus the spatial-temporal distribution and influence range of early cities. The enfeoffment system occurring during the Erlitou culture should also have played a vital role in this evolution. In general, the natural environment is more important for the spatial distribution and influence range of early cities during Yangshao, Longshan, and Erlitou cultures, while human culture represented by the enfeoffment system plays a dominant role during Shang and Zhou Dynasties when the natural environment is relatively stable. [ABSTRACT FROM AUTHOR]

The introduction of wheat into China between ~4500 and 4000 cal. a BP is thought to have restructured the ancient Chinese agricultural system and contributed to the formation and development of Chinese civilization. However, the spatial variation in agricultural development before and after the introduction of exotic crops across the Yellow River valley has not yet been discussed in detail. Here, we report new archaeobotanical data and radiocarbon dates from 25 sites in Sanmenxia, Henan Province, which was a hub for human migration in the middle reach of the Yellow River. Integrating our data with those of other archaeobotanical studies in northern China confirms that spatial cropping patterns in the Yellow River valley changed significantly around 4000 cal. a BP in the context of trans-Eurasia exchanges. From 7000 to 4000 cal. a BP, millet crops in the upper and middle Yellow River valley dominated the agricultural system, while mixed millet and rice agriculture developed in the lower Yellow River valley. In the subsequent period (4000–2200 cal. a BP), the cropping system in the upper Yellow River valley changed predominantly to barley and wheat agriculture, supplemented with millets. The contemporaneous cropping system in the middle and lower Yellow River valley, however, was dominated by millets, supplemented with wheat and rice. We argue that technological innovation and its dissemination in the context of trans-Eurasian cultural exchanges provided the basis for changes in the agricultural systems in northern China during the Bronze Age. Additionally, the trajectory of agricultural development was influenced by the natural environment and social change in different regions of the Yellow River valley. [ABSTRACT FROM AUTHOR]

The literature in the field of archaeological predictive models has grown in the last years, looking for new factors the most effective methods to introduce. However, where predictive models are used for archaeological heritage management, they could benefit from using a more speedy and consequently useful methods including some well-consolidated factors studied in the literature. In this paper, an operative archaeological predictive model is developed, validated and discussed, in order to test its effectiveness. It is applied to Yangshao period (5000–3000 BC) in the Songshan area, where Chinese civilization emerged and developed, and uses 563 known settlement sites. The satisfactory results herein achieved clearly suggest that the model herein proposed can be reliably used to predict the geographical location of unknown settlements. [ABSTRACT FROM AUTHOR]

The continuous development of the Neolithic to Bronze-Age cultures on China's Central Plains is well contested by archaeological and historical research. Environmental factors that sustained such an exceptionally long cultural continuity are, however, poorly understood. The evolution of fluvial landscapes and its relationship with cultural developments are key to disentangle the close interaction between the environment and civilizational discourse on the Central Plains. Here, we present OSL and AMS 14C ages and other environmental data collected from a range of typical geomorphological locations in the Shuangji River valley, which is situated at the heartland of the Central Plains and long considered to be one of the most important regions for the rise of the Chinese civilization. Combining the OSL and 14C dates, results of particle size and soil/sediment micromorphological analyses, and geoarchaeological field observations, we reconstructed the evolution of Holocene geomorphological landscape in the Shuangji River valley. The results show that the Neogene alluvial fan was incised into a wide valley during the early Pleistocene. Subsequent alluvial processes were constrained within this general framework of regional landform. The period of 20 ka BP and 10–8 ka BP saw two episodes of basin-scale alluvial incision, which created two alluvial terraces (i.e., T4 and T3), respectively. Despite the occurrence of episodic floods and some large-scale alluvial siltation during 8–3 ka BP, the alluvial surfaces remained stable for a prolonged period of time and thus provided optimal living conditions for prehistoric inhabitation. We argue that the geomorphological foundation and prolonged landscape stability were instrumental to the continuous cultural developments on the Central Plains as seen in the Shuangji River valley as a representative of such long-term human-environment interactions. Our geoarchaeological survey for the first time reveals basin-scale evidence on the mechanism responsible for this distinctive relationship between alluvial landscape and cultural development, in which the terrace-surface stability, alongside many other cultural factors, profoundly shaped the celebrated cultural continuity on prehistoric Central Plains. • Holocene fluvial landscape evolution was reconstructed in Shuangji River valley. • Regional rivers never overflowed the tops of high terraces after incision in 8 kaBP. • Landscape stability guaranteed the continuous cultural developments in Central China. [ABSTRACT FROM AUTHOR]