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Diversity of Mire Origin and History in Latvia

机译:拉脱维亚泥潭起源和历史的多样性

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摘要

Latvia is located in the western part of the East European Plain between 55 deg 40' and 58 deg 05' Northern latitude and 20 deg 58' and 28 deg 14' Eastern longitude. The area of Latvia covers 64,635 sq. km of which approximately 10 percent is covered by peatlands and mires. The climate, with higher precipitation over evaporation, slightly undulated relief and impermeable deposits in the bottoms of many depressions favours development of diverse mire types, such as fens and raised bogs. They have been formed under different paleoeco-logical conditions and time. The greater part of them is overgrown by trees and shrubs due to draining of the area and the surrounding lands; some areas are used for agricultural purposes. Therefore, just 4.9 percent of the total area is in natural conditions and occupied by fen, transition or bog biotopes.
机译:拉脱维亚位于东欧平原的西部,介于北纬55度40'和58度05'和东经20度58'和28度14'之间。拉脱维亚的面积为64,635平方公里,其中约10%被泥炭地和泥潭覆盖。气候,降水多于蒸发,起伏略微起伏以及许多洼地底部的不渗透性沉积物,有利于多种泥潭类型的开发,例如和高沼地。它们是在不同的古生态条件和时间下形成的。由于该地区和周围土地的排干,大部分树木和灌木丛生。有些地区用于农业目的。因此,只有4.9%的面积处于自然条件下,并被fen,transition或bog生物群落占据。

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