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Stone age vegetation in Uppland, Southeastern Svealand, Sweden

机译:瑞典东南斯韦兰地区乌普兰的石器时代植被

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A compilation has been done of 12 pollen diagrams from the county of Uppland, southeastern Sweden, in order to describe the earliest vegetational history in the Uppland archipelago. All diagrams cover the Middle and the Late Neolithic (3300-2300 BC), while nine of them date back to the Early Neolithic (3900-3300 BC) and four to the Late Mesolithic (5500-3900 BC). The main part of the sites has been investigated in connection with archaeological projects. The pollen studies carried out so far are not detailed enough to trace the farming history in Uppland, but some important results are obtained: (i) One site indicates weak signs of clearance and cultivation from the Late Mesolithic. (ii) From the Early Neolithic possible traces of cattle breeding occur at one site. (iii) More obvious but sparse finds of human indicators start during the Middle and the Late Neolithic, with possible cattle breeding from five sites and cultivation from four sites. Cattle breeding seems not to have been applied in the archipelago during the Stone Age, but was initiated when the sites were connected with the mainland. (iv) Palynological indications may verify that the maritime deciduous forest zone in the Stockholm archipelago is of natural origin. (v) The elm decline can be traced in more than 50% of the diagrams and occur c. 2500 BC. (vi) In seven diagrams from the Early Neolithic and 10 from the Middle and Late Neolithic, pollen of Picea occur in the sediments, indicating either limited spruce stands in the vicinity or windblown pollen, possibly from the eastern coast of the Baltic.
机译:为了描述Uppland群岛的最早植被历史,已经对来自瑞典东南部Uppland县的12个花粉图进行了汇编。所有图都涵盖了新石器时代中期和晚期(公元前3300年至2300年),其中九幅可以追溯到新石器时代早期(3900-3300 BC),另外四幅则可以追溯到中石器晚期(公元前5500-3900年)。已对遗址的主要部分进行考古研究。迄今为止进行的花粉研究不够详尽,无法追踪乌普兰的耕作历史,但获得了一些重要结果:(i)一个地点表明中石器时代晚期清除和耕种的迹象较弱。 (ii)从新石器时代早期开始,一个地方就可能出现牛繁殖的痕迹。 (iii)在新石器时代中期和晚期开始发现人类指标更为明显但稀疏,可能是从五个地点繁殖牛,并从四个地点进行耕种。石器时代似乎没有在群岛上进行牛育种,但牛场育种是在地点与大陆相连时开始的。 (iv)孢粉学迹象可证实斯德哥尔摩群岛的海洋落叶林带是自然起源的。 (v)榆树的下降可以追溯到50%以上的图表中并发生c。西元前2500年。 (vi)在新石器时代早期的七幅图中和新石器时代中期和晚期的十幅图中,云杉的花粉出现在沉积物中,表明附近云杉林有限,或者可能是波罗的海东海岸的风花粉。

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