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Rising social complexity, agricultural intensification, and the earliest rice paddies on the Loess Plateau of northern China

机译:中国北方黄土高原的社会复杂性,农业集约化和最早的稻​​田

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Geoarchaeological studies of landscapes immediately adjacent to archaeological sites can contribute information on the direct impact of small-scale societies on their associated landscapes. This direct connection allows us to understand aspects of the motivations, economic decision-making and agricultural strategies and how they affected local site catchments. The origin and spreading of farming communities onto the Loess Plateau of northern China provides a good example of this. We recorded sediment profiles that were immediately adjacent to the site of Huizui in the Yiluo River Basin. Here we identified evidence for human land-use beginning with the early Mid-Holocene deposits which are consistent with stable hillslope soils, indicating that the first mixed forager-millet farmers of the Peiligang Neolithic had a very light ecological footprint on the landscape. This is in contrast to the later middle Neolithic Yangshao Period farmers. Sediments from the Yangshao Period revealed paleolandscape and phytolith evidence for the earliest Neolithic paddy farming well outside of the natural habitat of wild rice. In addition to evidence for massive deforestation and soil erosion, a 15 m deep sediment sequence containing sets of gravels (beginning ca. 7200 cal BP) and gleyed soils dating from ca. 6600 cal BP, contained rice phytoliths, archaeological waste suggesting manuring, and micromorphological data indicating trampling. These signs of intensive landscape management go hand-in-hand with rapidly increasing social complexity. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:对紧邻考古遗址的景观进行地理考古研究可以提供有关小规模社会对其相关景观的直接影响的信息。这种直接联系使我们能够了解动机,经济决策和农业策略的各个方面,以及它们如何影响当地的集水区。中国北方黄土高原上农业社区的起源和传播就是一个很好的例子。我们记录了与伊洛河流域回族遗址紧邻的沉积物剖面。在这里,我们确定了人类早期土地利用的证据,该时期始于全新世中期的沉积物,与稳定的山坡土壤相一致,这表明培里岗新石器时代最早的混合饲草-粟农在景观上的生态足迹非常轻。这与后来的新石器时代仰韶中期农民形成鲜明对比。仰韶时期的沉积物揭示了古陆景观和植物石器证据,表明野生稻自然栖息地以外最早的新石器时代稻田耕作良好。除了大规模毁林和水土流失的证据外,还有一个深达15 m的沉积物序列,其中包含砾石集(始于大约7200 cal BP)和可追溯至大约1200年的带泥土。 6600 cal BP,包含水稻植石,表明粪便的考古废物和表明践踏的微观形态数据。加强景观管理的这些迹象与迅速增加的社会复杂性息息相关。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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