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首页> 外文期刊>Quaternary International >Linking the vicissitude of Neolithic cities with mid Holocene environment and climate changes in the middle Yangtze River, China
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Linking the vicissitude of Neolithic cities with mid Holocene environment and climate changes in the middle Yangtze River, China

机译:将新石器时代城市的变迁与中全新世环境和长江中游的气候变化联系起来

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摘要

This study investigated fifteen Neolithic cities distributed in a crescent-shaped belt along the middle Yangtze River from the period between ~ 4750 and 3050 BC (~ 6.7-5.0 cal. ka BP). The belt consists of a low-lying medial alluvial plain surrounded by hills more than 50 m a.s.l. (above sea level). The Neolithic cities within this belt occupied three distinct topographies, the highlands of alluvial plains, the lower foothills, and the surrounding hills. All the cities were situated adjacent to the lowest level tributaries or smallest lakes, and had complex trench defense systems, with rivers and lakes interlinking the trenches, and most of the cities had defensive moats. Construction peaks of defensive fortifications occurred during the Daxi (4550-3050 BC) and Qujialing cultures (3050-2650 BC), while most Neolithic cities were abandoned in the late Shijiahe period (~2250 BC). Based on assessments on the locality, age, construction, and the detailed information on the geographical characteristics of the Neolithic cities, the sites of Neolithic cities were tightly associated with the development history of East civilization, and the rise of the cities is well correlated with the warm and humid climate in mid-Holocene (~ 5.2 cal. ka BP, or ~ 3250 BC), while the decline of the ancient cities is related with the dry and cold climate in mid-late Holocene (~4.2 cal. ka BP, or ~2250 BC). The development and decline of these cities were also well linked with water accessibility, topography, and the occurrence of droughts, floods and other extreme events during the mid-Holocene. Such environment conditions and climate changes played significant roles for the ancient people to determine the location, structure, and morphology of the cities. Although the military considerations were also important, we cannot simply consider the prehistoric city construction in the middle Yangtze River was a passive defense against foreign invasion.
机译:这项研究调查了15个新石器时代的城市,这些城市分布在公元前4750年至公元前3050年(约6.7-5.0 cal。BP)之间,分布在长江中游的月牙形带中。该带由低洼的内侧冲积平原组成,周围环绕着超过50 m a.s.l.的山丘。 (高于海平面)。该带内的新石器时代城市占据了三个截然不同的地形,即冲积平原的高地,较低的山麓丘陵和周围的山丘。所有城市都与最低支流或最小的湖泊相邻,并具有复杂的trench沟防御系统,河流和湖泊将the沟相互连接,并且大多数城市都具有防御性的护城河。防御工事的建设高峰发生在大溪(公元前4550至3050年)和屈家岭文化(公元前3050至2650年),而大多数新石器时代的城市则在石家河末期(公元前2250年)被废弃。根据对新石器时代城市的地区,年龄,建筑和详细地理信息的评估,新石器时代城市的遗址与东方文明的发展历史紧密相关,并且城市的兴起与全新世中期(〜5.2 cal。BP,或〜3250 BC)的温暖湿润气候,而古代城市的衰落与全新世中期(〜4.2 cal。ka BP)的干冷气候有关,或〜2250 BC)。这些城市的发展和衰落还与水的可获取性,地形以及全新世中期干旱,洪水和其他极端事件的发生密切相关。这种环境条件和气候变化对古代人确定城市的位置,结构和形态起着重要作用。尽管军事考虑也很重要,但我们不能简单地认为长江中游的史前城市建设是对外国入侵的被动防御。

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  • 来源
    《Quaternary International》 |2014年第13期|22-28|共7页
  • 作者单位

    School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China;

    Hubei Provincial Institute of Cultural Relic and Archaeology, Wuhan 430077, China;

    College of Territorial Resources and Tourism, Anhui Normal University, Wuhu 241003, China;

    Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA 70803, USA;

    School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China;

    State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, CAS, Nanjing 210008, China,Nanjing Institute of Geology and Palaeontology, CAS. No 39 East Beijing Road, Nanjing 210008, China;

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