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Origin, history, management and plant species composition of grasslands in Central Europe - a review

机译:中欧草原的起源,历史,管理和植物种类 - 评论

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Until now, relatively little attention has been paid to the origin and history of grasslands in Central Europe and to the sources of information that can be used for such study. The aim of this review was to discuss the origin of natural and semi-natural grasslands in Central Europe. Without any written records, grassland history can be studied using the pollen and macrorem-nant analysis of different sediments and by soil charcoal analysis. An indicator of grasslands is the ratio of non-arboreal/arboreal pollen and species such as Plantago lanceolata and Urtica dioica in sediments. Pastures can be indicated by Juniperus communis pollen or by its charcoals. Insect-pollinated species can be studied using cesspit sediments and vessels in graves, because of their pollen in honey which was used as a sweetener. In Central Europe, natural grasslands occurred even before the start of agricultural activities in the Early Neolithic (5500 BC), but their area was relatively small and grassland patches were rather fragmentary in the forested landscape. Large-scale enlargement of grasslands can not be expected to have occurred before the Iron Age. The first scythes come from the 5th century BC, therefore, hay meadows did not develop before this time. From the start of the agriculture until the 18th century, pastures and pasture forests were dominant sources of forage in Central Europe. Large scale enlargement of hay meadows and decline of pastures in many regions occurred from the 18th century, when livestockwere predominantly moved into barns because of higher demand for organic fertilizers that were used to increase crop production on arable land. In some mountain areas, there are no records of large-scale deforestation and enlargement of grasslands untilthe Middle Ages, in the 14th century, and the peak of the agriculturally used area was recorded for the period from the 18th to the first half of the 20th century. Mountain grasslands were converted into arable land during the wars and, in contrast, grasslands replaced arable land after the collapse of agriculture in many regions of former communist countries following the change of the political regime in the 1990s. The dynamics of the grassland area reflect the development of human society, because grasslands are an integral part of the cultural landscape in Central Europe.
机译:到目前为止,在中欧草原的起源和历史上,对这些研究可用于此类研究的信息来源,对草原的起源和历史相对较少。本综述的目的是讨论中欧中欧洲自然和半天然草原的起源。如果没有任何书面记录,可以使用不同沉积物的花粉和宏观分析和土壤木炭分析来研究草地历史。草原指标是非植物/植物花粉和物种的比率,如沉积物中的植物植物和荨麻酶二恶英。牧场可以由杜松犬Comparen或其木炭表示。昆虫授粉物种可以使用泥浆沉积物和坟墓中的血管进行研究,因为它们在蜂蜜中的花粉作为甜味剂。在中欧,即使在新石器时代早期(5500年)的农业活动开始之前,天然草地也发生了,但他们的地区是相对较小的,草原斑块在森林景观中相当零碎。在铁时代之前,不能预期草原的大规模扩大。第一个Scythes来自于公元前5世纪,因此,干草草甸在这次之前没有发展。从农业开始到18世纪,牧场和牧场森林是中欧中部牧草的主导来源。大规模扩大了干草草甸和许多地区牧场的衰落发生在18世纪,因为牲畜主要被搬进谷仓,因为对用于增加耕地上的作物生产的有机肥料的需求较高。在一些山区,在14世纪,18世纪到第20届至上半年的期间,没有大规模森林砍伐和草原扩大的记录,直到14世纪,录制了农业使用的地区的峰值。世纪。在战争期间,山地草地被转化为耕地,相比之下,草原在20世纪90年代政治制度改变后,在前共产主义国家的许多地区在农业崩溃后替代耕地。草地地区的动态反映了人类社会的发展,因为草原是中欧文化景观的一个组成部分。

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