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首页> 外文期刊>Quaternary International >The origins of a Nardus stricta grassland through soil charcoal analyses: Reconstructing the history of a mountain cultural landscape (Mont Lozere, France) since the Neolithic
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The origins of a Nardus stricta grassland through soil charcoal analyses: Reconstructing the history of a mountain cultural landscape (Mont Lozere, France) since the Neolithic

机译:通过土壤木炭分析得出纳尔达斯草原的起源:重建新石器时代以来山区​​文化景观的历史(法国蒙特罗泽尔)

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This paper presents the use of soil charcoal analyses in order to identify the origin of a Nardus stricta grassland in a mountain system (Mont Lozere, France), and the use of environmental resources and the construction of a cultural landscape. Two opposing theories have been proposed to explain the origin of this open landscape (1450-1700 m altitude): natural or anthropogenic. The identification and radiocarbon dates of charcoal fragments of Fagus sylvatica, which were found in all of the pits located in the current grassland area and dated to 3695-3633 cal BC, demonstrate that this species has been present on the upper part of Mont Lozere since the Middle Neolithic. In addition, the presence of pioneer species (Betula, Salix, Corylus avellana), as well as mid- (Prunus cf avium) and late-successional species (F. sylvatica) supports the hypothesis that the grassland contained both pioneer and mature phases of forest landscapes. The C-14 dates, ranging from c. 4200 cal BC to 1200 cal AD, show that fire events occurred with different climatic influences. Fire events may correspond to one or several fires in a short period at the scale of the slope. Moreover, the dates coincide with the early and extensive human impact detected in the Massif Central and Mont Lozere. To explain the regular occurrences of fire events from the Middle Neolithic to the Central Middle Ages, agro-pastoral clearings have been postulated, as have been identified in other areas in the Pyrenees and in the Alps. Such human impact may have been magnified, or least facilitated, by climatic conditions. Comparison with additional data (pollen, archaeology, ecology) demonstrates that this grassland area is not natural and corresponds to an ancient forested system that has been used and transformed by societies since the Neolithic, although climate change may have certainly affected this transformation. The aim of this research is to promote this cultural heritage in collaboration with the National Park of the Cevennes in order to protect its future. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:本文介绍了使用土壤木炭分析来确定山区系统(法国蒙罗泽尔)上的纳尔达斯草原的起源,以及环境资源的利用和文化景观的建设。已经提出了两种相反的理论来解释这种开放景观(海拔1450-1700 m)的起源:自然的或人为的。在当前草地地区所有凹坑中发现的青冈木炭碎片的鉴定和放射性碳日期可追溯到公元前3695-3633年,证明该物种自从那时起就已经存在于Mont Lozere的上部。新石器时代中期。此外,存在先驱物种(桦木,柳树,欧洲榛)以及中(Prunus cf avium)和后成功物种(F. sylvatica)也支持了这样的假设,即草原既有先驱阶段又有成熟阶段。森林景观。 C-14日期,范围从c。公元前4200年至公元1200年之间,表明火灾事件是在不同气候影响下发生的。火灾事件可能在短时间内对应于坡度范围内的一场或几场火灾。此外,这些日期与在Massif Central和Mont Lozere发现的早期人类广泛影响相吻合。为了解释从新石器时代中期到中中世纪时期火灾的定期发生,已经提出了农业和牧草的清理方法,在比利牛斯山和阿尔卑斯山的其他地区也发现了这种情况。这种人类影响可能已被气候条件放大,或至少得到了促进。与其他数据(花粉,考古学,生态学)的比较表明,该草原区不是自然的,并且对应于自新石器时代以来已被社会使用和改造的古老森林系统,尽管气候变化肯定会影响这种转化。这项研究的目的是与塞文山脉国家公园合作,促进这种文化遗产,以保护其未来。 (C)2014 Elsevier Ltd和INQUA。版权所有。

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