基瓦人类居住的古生态和考古证据的比较

Pub Date : 2012-01-01 DOI:10.3176/arch.2012.supv1.10
V. Lang, A. Heinsalu, S. Veski
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引用次数: 0

摘要

在Keava(公元前4世纪至公元13世纪初)史前定居中心最近的一个非常小的盆地,Verevainu的前沼泽,用古生态方法,即花粉,木炭,点火损失分析和放射性碳定年,研究了泥炭记录。该研究旨在确定该地区史前人类的面貌,重建当地植被历史和人类对定居中心周围环境的影响。根据古生态学证据,在青铜时代晚期的沉积物中出现了第一批零星的谷物花粉粒。作为表土侵蚀指标的泥炭燃烧残留物值和花粉证据都表明,前罗马铁器时代的森林砍伐、景观开放和谷物种植。大约在公元350-500年间,人类对环境的影响显著增加。古生态资料与人类居住的考古证据比较,既有较大的吻合,也有一定的差异。1
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A COMPARISON OF PALAEO-ECOLOGICAL AND ARCHAEOLOGICAL EVIDENCE OF HUMAN HABITATION AT KEAVA
Peat record from a very small basin, the former mire of Verevainu, in the nearest vicinity of the prehistoric settlement centre at Keava (4th century BC – early 13th century AD), was investigated by palaeo-ecological means, namely by pollen, charcoal, and loss-on-ignition analyses and radiocarbon dating. The study aimed at ascertaining the appearance of prehistoric man in the area and reconstructing the local vegetation history and human impact on the environment around the settlement centre. According to palaeo-ecological evidence the first sporadic cereal pollen grains appeared in the sediments in the Late Bronze Age. Both peat ignition residue values as indicators of topsoil erosion and pollen evidence suggest forest clearance, opening of landscape, and cultivation of cereals from the Pre-Roman Iron Age. Approximately at AD 350–500 the rate of human impact upon environment increased notably. The comparison of palaeo-ecological data with archaeological evidence of human inhabitation displays not only large coincidences but also some discrepancies. 1
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