首页> 外文期刊>Journal of Vegetation Science >Sampling soil wood charcoals at a high spatial resolution: a new methodology to investigate the origin of grassland plant communities.
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Sampling soil wood charcoals at a high spatial resolution: a new methodology to investigate the origin of grassland plant communities.

机译:以高空间分辨率对土壤木炭进行采样:一种研究草原植物群落起源的新方法。

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Questions: (i) Can sampling of soil wood charcoals at high spatial resolution produce new evidence concerning the presence of chalk grassland before or during the Neolithic, Bronze and Iron Ages? (ii) Are there correlations between vegetation history and archeological data during these periods at this particular site? Location: The chalk hillsides of Saint-Adrien in the lower Seine Valley, Upper Normandy, northwest France. Methods: The study was carried out at a high spatial resolution in chalk grassland using soil wood charcoal analysis, in which charcoals found in the soil were identified and dated in an area of several hundred square meters. Results: Late-successional woody species (Fagus sylvatica, Quercus sp.) were still present in the study site in an area inconsistent with the existence of large chalk grassland herbaceous plant communities (several hectares) in the Neolithic (6500-3800 BP) and Bronze Age (3800-2700 BP). Conclusions: The presence of late-successional woody species on the studied hillside suggests that fires in the Neolithic were linked to forest clearance for pastoral activities, as already demonstrated for similar ecosystems in eastern France and Germany. Nevertheless, our methodology clearly demonstrates that palaecological studies need to take into account the spatial organisation of plant communities as a complementary element to validate their potential existence in former times.
机译:问题:(i)在新石器时代,青铜时代和铁器时代之前或期间,以高空间分辨率对土壤木炭进行采样能否产生有关白垩草原存在的新证据? (ii)在这段时期内,该特定地点的植被历史与考古数据之间是否存在相关性?位置:法国西北部上诺曼底塞纳河谷下部的圣阿德瑞安粉笔山坡。方法:利用土壤木炭分析技术,在白垩草原上进行了高空间分辨率的研究,对土壤中发现的木炭进行了鉴定,并注明了其年代为几百平方米。结果:在该研究地点仍然存在晚成功的木本物种(西格纳斯迷迭香(Fagus sylvatica), Quercus sp。)。 (几公顷)在新石器时代(6500-3800 BP)和青铜时代(3800-2700 BP)。结论:在研究过的山坡上存在较晚的木本物种,这表明新石器时代的大火与森林的放牧活动有关,正如法国东部和德国类似生态系统所证明的那样。然而,我们的方法论清楚地表明,古生物学研究需要考虑植物群落的空间组织,作为补充元素,以验证其在以前的潜在存在。

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