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首页> 外文期刊>Vegetation History and Archaeobotany >New insights into vegetation dynamics and settlement history in Hummling, north-western Germany, with particular reference to the Neolithic
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New insights into vegetation dynamics and settlement history in Hummling, north-western Germany, with particular reference to the Neolithic

机译:关于德国西北部Hummling植被动态和沉降历史的新见解,特别是新石器时代

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摘要

Palynological investigations on two well-dated peat profiles provide insights into Neolithic vegetation and settlement history from Hummling in north-western Germany. The site selections allow comparisons between local and regional vegetation changes and are used to estimate the extent of Neolithic influence on the vegetation. The interpretation of the fossil spectra relied on radiocarbon dating, evaluation of pollen indicator taxa, non-pollen palynomorphs and multivariate techniques. During the late Mesolithic the vegetation was dominated by mixed oak forests while openings in forest cover were detected, with a decline in elm reflected in the regional pollen record around 4250 cal. b.c. The presence of humans is shown by settlement indicators that are first recorded at ca. 3800 cal. b.c. Vegetation changes were small between 4300 and 3600 cal. b.c. This suggests that regional vegetation was relatively resilient to small-scale disturbances. Possible indications of grazing were recorded in the spectra of the local pollen profile but there is no clear-cut evidence for Neolithic activity. Between 3520 and 2260 cal. b.c. decreases in forest cover were inferred from both profiles and increases in settlement indicators reflect farming activity. These changes coincide with the emergence in the area of the Funnel Beaker Culture and the subsequent Single Grave Culture. Both profiles suggest that settlement probably ceased between ca. 3230 and 3050 cal. b.c. This lull or cessation in activity was probably regional in character. After 2260 cal. b.c. human impact on the vegetation decreases and woodlands regenerate. The longevity of the regeneration phase-ca. 690 years-was probably connected with the low resilient capability of the vegetation on the poor soils
机译:对两种日期合适的泥炭剖面的孢粉学调查提供了德国西北部Hummling的新石器时代植被和定居历史的见解。选址可以比较本地和区域的植被变化,并用于估计新石器时代对植被的影响程度。化石光谱的解释依赖于放射性碳年代测定法,对花粉指示物分类群的评估,非花粉质变体和多变量技术。在中石器时代晚期,植被被混合的橡树林为主,同时发现了森林覆盖的空缺,榆树的减少反映在大约4250 cal的区域花粉记录中。公元前。人类的存在由沉降指标显示,该指标最初记录在约。 3800卡路里公元前。在4300至3600 cal之间,植被变化很小。公元前。这表明区域植被对小规模干扰具有相对的抵抗力。在局部花粉轮廓的光谱中记录了可能的放牧迹象,但尚无明确的新石器时代活动证据。在3520和2260之间公元前。从这两个方面推断出森林覆盖率的下降,而定居​​指标的增加则反映了农业活动。这些变化与漏斗烧杯文化和随后的单坟文化的出现相吻合。两种情况都表明,沉降可能在大约2个月之间停止。 3230和3050卡路里公元前。活动的这种平息或停止可能具有区域性。 2260卡路里后公元前。人类对植被的影响减少,林地再生。再生相的寿命ca。 690年可能与贫瘠土壤上植被的低复原力有关

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