对保加利亚里拉山西北部全新世晚期植被史的贡献:斯卡卡维察湖的花粉记录

M. Lazarova, S. Tonkov, D. Ivanov
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引用次数: 0

摘要

对从里拉山西北部斯卡卡维萨湖(海拔 2170 米)泥炭质湖岸获得的全新世晚期沉积物岩芯进行了花粉分析。在详细的放射性碳年代学支持下进行的植被重建揭示了研究地区过去 4000 年森林发展和人类影响的新信息。4000 至 3000 年前,该地区分布着以欧洲赤松(Pinus sylvestris)、白松(Abies alba)、欧洲赤松(Pinus peuce)和一些欧洲冷杉(Picea abies)为主的茂密针叶林,在它们下面则生长着孤立的法桐(Fagus)。森林植被随后发生的变化包括:2500 年至 800 年前针叶林带云杉的入侵,以及 1500 年前山毛榉群落的扩大。在过去的 700 年里,有证据表明人类进行了密集的放牧和作物种植活动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Contribution to the Late Holocene Vegetation History of the Northwestern Rila Mountain, Bulgaria: the Pollen Record of Lake Skakavitsa
Pollen analysis was conducted on a Late Holocene sediment core obtained from the peaty shore of Lake Skakavitsa (2170 m) in the Northwestern Rila Mountain. The vegetation reconstruction supported by detailed radiocarbon chronology revealed new information about the forest development and human impact in the study area for the last 4000 years. Dense coniferous forests dominated by Pinus sylvestris, Abies alba, Pinus peuce and some Picea abies were distributed between 4000 and 3000 years ago and below them thrived isolated stands of Fagus. The subsequent transformations in the forest cover include the invasion of spruce in the coniferous belt between 2500 and 800 years ago and the enlargement of beech communities since 1500 years ago. Evidence of intensive human activities related to livestock-grazing and crop cultivation is registered for the last 700 years.
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