Abstract:Beginning with the earliest organized habitation sites the options provided by the regional environment have largely or partially governed the location and relocation of human settlements. The settlement system in second millennium BCE Henan Province, China, evolved during a period of significant climatic change and shifting river courses but relative soil stability. Human-environment interactions across the landscape have left ample remains for investigation by scholars of social and cultural change and by na… Show more
“…Shang moved its capitals five times in the lower Yellow River region. Post-Shang records state that at least one capital was moved following destruction by a catastrophic flood (Rapp and Jing 2011).…”
Section: History Of the Yellow River Floodsmentioning
We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.
“…Shang moved its capitals five times in the lower Yellow River region. Post-Shang records state that at least one capital was moved following destruction by a catastrophic flood (Rapp and Jing 2011).…”
Section: History Of the Yellow River Floodsmentioning
We analyze 4000-year flood history of the lower Yellow River and the history of agricultural development in the middle river by investigating historical writings and quantitative time series data of environmental changes in the river basin. Flood dynamics are characterized by positive feedback loops, critical thresholds of natural processes, and abrupt transitions caused by socio-economic factors. Technological and organizational innovations were dominant driving forces of the flood history. The popularization of iron plows and embankment of the lower river in the 4th century BC initiated a positive feedback loop on levee breaches. The strength of the feedback loop was enhanced by farming of coarse-sediment producing areas, steep hillslope cultivation, and a new river management paradigm, and finally pushed the flood frequency to its climax in the seventeenth century. The co-evolution of river dynamics and Chinese society is remarkable, especially farming and soil erosion in the middle river, and central authority and river management in the lower river.
“…The oracle bones and other early historical texts reveal that the unpredictability of the natural world greatly concerned Shang and Zhou dynastic kings (Keightly, ; Needham, Wang, & Lu, ). Shang kings frequently consulted the oracle bones to divine potentially dangerous floods that could significantly damage Shang dynasty urban centers and, more importantly, endanger the year's harvest (Rapp & Jing, ; Keightly, , ). “Beautiful land was ordered land” to the Shang kings because it represented the stability of an agricultural lifeway and the kings’ rule (Keightly, :119).…”
Section: Discussionmentioning
confidence: 99%
“…Shang kings frequently consulted the oracle bones to divine potentially dangerous floods that could significantly damage Shang dynasty urban centers and, more importantly, endanger the year's harvest (Rapp & Jing, 2011;Keightly, 2000Keightly, , 2013. "Beautiful land was ordered land" to the Shang kings because it represented the stability of an agricultural lifeway and the kings' rule (Keightly, 2000:119).…”
Section: Discussionmentioning
confidence: 99%
“…The majority of the population lived in rural areas and presumably would have required water management technology to support agricultural production and protect against potentially devastating floods. Some of the only published evidence of nonurban water management technology include the “water‐ditches” found outside of Xiaodun, Anyang, but an inadequate amount of work has been done to reveal their function (Rapp & Jing, :127).…”
Section: Regional Backgroundmentioning
confidence: 99%
“…Archaeologists have tried to overcome the limitations of such deeply buried archaeological deposits through national archaeological surveys (see Wagner et al., ), but many of the archaeological sites identified through these surveys are close to the modern land surface. Recent geoarchaeological investigations have revealed that at least 10 m of Yellow River alluvium has buried a series of ancient land surfaces dating to the early, middle, and late Holocene (Kidder, Liu, Xu, & Li ; Jing, Rapp, & Gao, , ; Rapp & Jing, ). These discoveries make the integration of alluvial geoarchaeology into traditional archaeological research design essential (Brown, ).…”
Section: Excavations At Anshang Town Neihuang County Henan Provincementioning
The development of irrigation is a politically important technology that enabled agricultural societies to intensify agricultural production. In the North China Plain, the historical record suggests a long tradition of irrigation, but archaeologists have found scant evidence of these technologies outside of urban areas. In 2012, 2015, and 2016, our excavations at the Anshang site, Neihuang County, Henan Province, China, revealed several archaeological features that we interpret as evidence of Late Shang dynasty (ca. 1200–1046 B.C.) canal construction in a nonurban context. By using a range of geological methods, including particle size, loss on ignition, magnetic susceptibility, and micromorphology, we suggest that these ancient canals and the subsequent construction phases found at Anshang not only influenced the development of local geomorphic conditions, but also were part of early dynastic attempts to restructure the natural landscape to facilitate agricultural productivity. These irrigation canals found at Anshang may be representative of broader trends of human‐environmental interactions in the North China Plain.
The heartlands of many of the world's civilizations are situated within alluvial plains, where thick alluvial sediments obscure much of the archaeological record. However, the use of alluvial geoarchaeology remains patchy, particularly in the world's largest alluvial basins. We present results from our geoarchaeological survey at Neihuang County, Henan Province, China, as an example for alluvial geoarchaeological research in the North China Plain and to develop a generalized framework for landscape evolution in the area during the Holocene. We reconstruct the alluvial history of the area around Neihuang County by synthesizing stratigraphic data from seven outcrops into distinct depositional units. Our findings suggest that much of the archaeological record in the North China Plain is buried by meters of sediment or eroded away by the ancient channels of the Yellow River and other tributary streams. Therefore, the presence of buried archaeological sites and river scour in recorded outcrops suggests that the nonsystematic archaeological surveys that are commonly used to interpret cultural changes are not accurate reflections of archaeological site distributions. From the results of this case study, we recommend that archaeologists and paleoclimatologists should exercise more caution when using settlement distribution data gathered through nonsystematic pedestrian surveys to make inferences about ancient processes of cultural change or social dynamics in the North China Plain.
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