中国新石器时代晚期中原地区的水生景观与城墙遗址的出现——来自古城寨遗址的考古和地质考古证据

Pub Date : 2023-03-01 DOI:10.1016/j.ara.2022.100428
Yijie Zhuang , Xiaohu Zhang , Junjie Xu
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引用次数: 0

摘要

中国中原地区出现了许多新石器时代晚期和青铜时代早期的城墙遗址,与一些突出的全新世气候事件相吻合。近年来对古城寨最大遗址之一的发掘和地质考古调查,为探讨史前中原晚期水生景观形成与社会演化之间的长期关系提供了重要的资料。我们从一系列现场和现场外的环境中收集了细粒度的古环境和考古证据,重建了城墙遗址周围的晚全新世古环境,并研究了其大型护城河的建造、维护和废弃过程。研究结果表明,全新世晚期存在许多小到大的水体,这些水体与当地河流共同构成了遗址的主要水源。古城寨人口被吸引到靠近河流和其他水文条件最优的水体的低洼地带。在使用期间,护城河可能与附近的湿地和/或河流相连。水文系统由温和但相对含沙的水流主导,其间穿插着几次高能洪水事件。当护城河不再作为主要的水流通道时,护城河使用期间沉积的淡黄色泥沙和带有一些人为包裹体的沙子被富含有机质的快速淤积所取代,尽管附近继续发生其他土地利用活动,如火灾(土地清理?)。重建的护城河“生活史”表明,随着气候变得越来越干燥,居住在古城寨的人口越来越多,面临着日益严峻的挑战。护城河的修建和运营标志着古城寨的技术创新和水资源管理的加强,形成了水文最佳环境下大型水利基础设施特色鲜明的水生景观。我们认为,这是许多当代或后期中原城墙遗址的共同特征或趋势。
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Aquatic landscape and the emergence of walled sites in late Neolithic Central Plains of China: Integrating archaeological and geoarchaeological evidence from the Guchengzhai site

The emergence of many late-Neolithic and early Bronze-Age walled sites on China's Central Plains coincided with some prominent Holocene climate events. Recent excavation and geoarchaeological investigation at one of the largest walled sites of Guchengzhai provide important data to examine some of the questions concerning the long-term relationship between the formation of aquatic landscape and social evolution in late prehistoric Central Plains. We collected fine-grained paleo-environmental and archaeological evidence from a range of on- and off-site contexts to reconstruct the late-Holocene paleo-environment surrounding the walled site, and examine the construction, maintenance and abandonment processes of its large-size moat. Our results show that there existed many small-to-large-sized waterbodies during the late Holocene, which, together with local rivers, were the main source of water to the site. The Guchengzhai population was drawn to the low-lying land near the river and other waterbodies with an optimal hydrological condition. During its use, the moat might have been linked to the nearby wetlands and/or rivers. The hydrological regime was dominated by gentle but relatively sediment-laden flow, being punctuated by several high-energy flood events. The sedimentation of light yellowish silt and sand with some anthropogenic inclusions during the use of the moat gave way to a quick siltation with the deposition of rich organic matter when the moat ceased to function as a main channel for water flow, although other land-use activities such as fire (land clearance?) continued to occur in the vicinity. The reconstructed ‘life-history’ of the moat demonstrates the increasingly acute challenge facing the growing population living at Guchengzhai as the climate was becoming drier. The construction and operation of the moat signified technological innovations and intensified water management at Guchengzhai, which led to the formation of distinctive aquatic landscape that featured large-scale hydraulic infrastructures in a hydrologically optimal environment. We contend that such was a common characteristic or trend shared by many contemporary or later-period walled sites on the Central Plains.

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