Yingjun Lin , Xinxin Zuo 左昕昕 , Lin Fu , Yunming Huang , Jun Yang , Weiwei Liu , Shuo Zhang , Jinqi Dai , Hui Xie , Lin Ren , Yongjun Huang , Zekai Hu
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引用次数: 0
Abstract
Late Neolithic cultures in the southeastern mountainous region of China were diverse and frequently interacted with surrounding areas. Understanding the emergence of agriculture and its relationship with the regional cultural background is crucial for comprehending the development of societies. This study combined detailed phytolith analysis with archaeological and historical data and examined Late Neolithic sites in the inland mountainous area of Fujian. The results revealed the presence of various rice phytoliths from the Niubishan to Maling period (5300–3800 cal BP), indicating that rice cultivation occurred in this region at least 5000 years ago. Furthermore, the earliest millet phytoliths emerged in the Upper Niubishan Culture layers 4500 years ago. These findings provide a comprehensive understanding of the agricultural development in this region. This study suggests that the emergence of rice and millet in the southeastern mountainous areas of China may be linked to interactions between prehistoric cultures in different regions. The initial emergence of rice at approximately 7500 cal BP likely spread from the lower Yangtze River along the coastal route. Between 5500 and 3500 cal BP, the gradual opening of land routes facilitated the southward dispersal of agriculture from the middle and lower Yangtze River, creating interconnected land and sea routes. This integration possibly led to the formation of a mixed rice-millet agricultural system that spread to Southeast Asia. Additionally, environmental factors, such as early to mid-Holocene sea level rise and mid to late Holocene drought, appear to have played a crucial role in the emergence and spread of agriculture in this region. Overall, These findings provide significant insights into the emergence, development, and dispersal of prehistoric agriculture and its relationship with cultural exchange and environmental changes in this region.
中国东南部山区新石器时代晚期文化多样,并与周边地区频繁互动。了解农业的出现及其与区域文化背景的关系对于理解社会的发展至关重要。本研究将详细的植物岩分析与考古和历史资料结合起来,考察了福建内陆山区的新石器时代晚期遗址。研究结果表明,在牛壁山至马陵时期(5300-3800 cal BP)存在多种水稻植物岩,表明该地区至少在5000年前就出现了水稻种植。此外,最早的谷子植物岩出现在距今4500年前的牛壁山上文化层。这些发现对该地区的农业发展提供了一个全面的认识。这项研究表明,中国东南部山区水稻和小米的出现可能与不同地区的史前文化之间的相互作用有关。水稻的最初出现大约在7500 cal BP,可能是从长江下游沿着沿海路线传播的。在5500 - 3500 cal BP之间,陆路的逐渐开放促进了农业从长江中下游向南扩散,形成了相互连接的陆海通道。这种整合可能导致形成了一种混合的水稻-谷子农业系统,并传播到东南亚。此外,全新世早期至中期的海平面上升和全新世中后期的干旱等环境因素在该地区农业的出现和传播中发挥了至关重要的作用。总的来说,这些发现对史前农业的出现、发展和传播及其与该地区文化交流和环境变化的关系提供了重要的见解。
期刊介绍:
Journal of Archaeological Science: Reports is aimed at archaeologists and scientists engaged with the application of scientific techniques and methodologies to all areas of archaeology. The journal focuses on the results of the application of scientific methods to archaeological problems and debates. It will provide a forum for reviews and scientific debate of issues in scientific archaeology and their impact in the wider subject. Journal of Archaeological Science: Reports will publish papers of excellent archaeological science, with regional or wider interest. This will include case studies, reviews and short papers where an established scientific technique sheds light on archaeological questions and debates.