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Contrasting local and regional Holocene histories of Abies alba in the Czech Republic in relation to human impact: Evidence from forestry, pollen and anthracological data

机译:与人类影响有关的捷克共和国白冷杉的地方和区域全新世历史对比:来自林业,花粉和人类学数据的证据

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摘要

After the last glaciation, around 4000 bc, silver fir (Abies alba Mill.) spread to the area that is now the Czech Republic. This spread was not restricted to high mountains, but also took place across both highland and lowland landscapes. Historical forestry records from around ad IS00 mention a massive expansion of Abies alba, favoured by forest pasturing, litter raking and selective tree cutting. According to the current interpretation of these historical records, this expansion in Czech forests was extensive and lasted until ad 1800. On the other hand, pollen data coming mostly from the Alps consider silver fir as a species that is extremely sensitive to human impact. In this paper, we compare historical forestry reports with pollen and charcoal data from the Czech Republic. Both pollen and charcoal records show that Abies alba reached its maximum during the Bronze (2200-800/750 bc) and Iron Ages (800/750 bc-ad 0). While charcoal records indicate that silver fir wood was important also during the High Medieval, pollen data show that the High Medieval and Modern times were periods of a general decline in Abies. Our data suggest that the expansion of silver fir documented by historical records was not general but rather fragmented, probably according to actual form and the intensity of human impact, as well as environmental conditions. These historical records have contributed much evidence regarding the wider ecological tolerance of Abies.
机译:在最后一次冰川消融之后,大约在公元前4000年,白枞(Abies alba Mill。)扩散到了现在的捷克共和国。这种传播不仅限于高山,而且还发生在高地和低地景观上。来自广告IS00周围的历史林业记录提到白冷杉的大规模扩张,这受到森林放牧,枯草耙和选择性砍伐的青睐。根据对这些历史记录的当前解释,捷克森林的这种扩张是广泛的,一直持续到公元1800年。另一方面,大部分来自阿尔卑斯山的花粉数据都将银杉视为对人类影响极为敏感的物种。在本文中,我们将历史林业报告与捷克共和国的花粉和木炭数据进行了比较。花粉和木炭记录均显示,白冷杉(Abies alba)在青铜时代(2200-800 / 750 bc)和铁器时代(800/750 bc-ad 0)达到了最大值。木炭记录表明,银枞木在中世纪期间也很重要,但花粉数据显示,中世纪和近代是冷杉的普遍下降时期。我们的数据表明,历史记录记载的银杉的扩张不是一般性的,而是分散的,可能是根据实际形式和人类影响的强度以及环境条件而定。这些历史记录为有关冷杉的更广泛的生态耐受性提供了许多证据。

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