P. Török, M. Janišová, Anna A. Kuzemko, Solvita, Rūsiņa, Z. Stevanović
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引用次数: 34
摘要
东欧地区包括中欧和东欧(不包括东德和俄罗斯的欧洲部分)和巴尔干国家(不包括希腊和土耳其)的后社会主义国家(图4.1)。该地区总面积为2,154,005平方公里,其特点主要是北部和东北部的广泛低地地区,以及该地区中部(喀尔巴阡山脉)和南部(巴尔干山脉,克里米亚山脉)的相当多的山区。该地区是凉爽的大陆性气候,地中海对南部的影响越来越大(Peel et al., 2007)。根据Metzger et al.(2005)提供的欧洲环境分层系统(European Environmental Stratification system),东欧大部分平原和低地以及巴尔干半岛的高地和低山位于大陆环境带(Continental Environmental Zone, CON),自然以落叶林、混交林和针叶林为主。在低地地区,草原形成于细粒或粗粒的冲积和河流沉积物上,其特点是受大河及其支流的高度影响。的
Grasslands, their Threats and Management in Eastern Europe
The Eastern European region covers the post-socialist countries of central and eastern Europe (excluding East Germany and the European part of Russia) and the Balkan countries (excluding Greece and Turkey) (Fig. 4.1). The total area of the region is 2,154,005 km2, characterized mostly by extensive lowland regions to the north and north-east and with considerable mountainous regions in the central (Carpathians) and the southern (Balkan mountains, Crimean mountains) parts of the region. The region experiences a cool continental climate with increasing Mediterranean influence to the south (Peel et al., 2007). Based on the European Environmental Stratification system provided by Metzger et al. (2005), most of the Eastern European plains and lowlands and the uplands and low mountains of the Balkan Peninsula are situated in the Continental Environmental Zone (CON), naturally dominated by deciduous, mixed and coniferous forests. In the lowland regions, grasslands were formed on fine or coarse-grained alluvial and fluvial deposits and are characterized by the high influence of large rivers and their tributaries. The