Historical Influence of Man on the Vegetation Record in the Prášilské Lake Sediments (Bohemian Forest, Czech Republic)

E. Břízová
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引用次数: 2

Abstract

Abstract The Prášilské Lake is the glacial lake in the Bohemian Forest (Šumava Mts) located on the Czech side in the elevation of 1,079 m above sea level. The lake area is 4 ha, the maximal depth is 15.5 m. The lake catchment area is situated in the sub-alpine zone. The studied area has never been the object of forest or agricultural farming in the history because of its inaccessibility. The sediment dating was carried out by means of lead isotope 210Pb. The oldest layer established by this isotope in the Prášilské Lake was in the depth of 0.47 m. This dating was used for the deepest layer of sediment and its age was dated to the year of 1843 (depth 0.11 m) and a base of this profile to the medieval age (depth 0.47 m), which corresponds to about the 12th-13th century A.D. The analysed profile (0-0.47 m) can be divided into the local pollen assemblage zones PRI-1 (depth 0.37-0.47 m), PRI-2 (depth 0.25-0.37 m), PRI-3 (depth 0.12- 0.25 m), PRI-4 (depth 0.06-0.12 m), PRI-5 (depth 0.02-0.06 m), PRI-6 (depth 0-0.02 m). On the basis of dating by the 210Pb method the age of sediment (0-0.11 m) is established into the range of 1843 to 1994. It is noticeable in the pollen spectrum that it concerns a locality situated already above the forest border, the pollen curves of stratigraphical important taxons (mainly woody species) do not change markedly. The rich woody component is formed mainly by pollen grains of Picea and Fagus. The herbaceous component (NAP) is very diverse; however, in a general way the pollen grains of woody species (AP) predominate due to the above mentioned deciduous forests. A representation of the herbaceous component (NAP) is very varied as far as species are concerned, human influence is very visible here (e.g. occurrence of cereals Cerealia, Zea mays, Fagopyrum-type, weed: Centaurea cyanus, Agrostemma githago etc.). The dating of this part also corresponds to the results of the pollen analysis. Of the plants producing spores the findings of lesser clubmoss (Selaginella-type cf. Selaginella selaginoides) and water plant quillwort (Isoëtes), whose nearest contemporary place of the finding in our territory is in the Černé and Plešné Lake and Wielki Staw (the Giant Mts), were quite interesting. The most of spores were recorded at the family Polypodiaceae and green alga Botryococcus, which indicate cold and humid conditions of the occurrence.
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人类对Prášilské湖泊沉积物植被记录的历史影响(捷克波希米亚森林)
Prášilské湖是波希米亚森林(Šumava Mts)中的冰川湖,位于捷克一侧,海拔1079米。湖泊面积4公顷,最大水深15.5米。湖泊集水区位于亚高山地带。由于交通不便,研究区在历史上从未成为森林或农业耕作的对象。沉积物年代测定采用铅同位素210Pb。该同位素在Prášilské湖中建立的最古老的地层深度为0.47 m。这个约会是用于最深的沉积物层及其年龄是追溯到1843年(深度0.11米)和一个基地这个概要文件的中世纪时代(深度0.47米),对应于约公元12至13日世纪分析概要(0 - 0.47)可分为本地花粉组合区PRI-1(深度0.37 - -0.47米),PRI-2(深度0.25 - -0.37米),PRI-3(深度0.12 - 0.25米),PRI-4(深度0.06 - -0.12米),PRI-5(深度0.02 - -0.06米),在210Pb测年的基础上,确定沉积物年龄(0 ~ 0.11 m)为1843 ~ 1994年。值得注意的是,在花粉谱中,它涉及的地方已经位于森林边界之上,地层重要分类群(主要是木本种)的花粉曲线没有明显变化。丰富的木质成分主要由云杉和Fagus的花粉粒组成。草本成分(NAP)非常多样化;然而,在一般情况下,由于上述落叶森林,木本物种(AP)的花粉粒占主导地位。就物种而言,草本成分(NAP)的表现非常多样化,人类的影响在这里非常明显(例如,谷类、玉米、荞麦类、杂草:Centaurea cyanus、Agrostemma githago等)。这部分的年代测定也与花粉分析的结果相吻合。在产生孢子的植物中,发现了较小的杆藓(卷叶卷苔类,如卷叶卷苔)和水生植物刺茅(Isoëtes),其在我国领土上最近的当代发现地点是Černé和Plešné湖和Wielki Staw(巨人山),这是相当有趣的。孢子主要分布在水蛭科和绿藻芽孢球菌中,表明其发生在寒冷潮湿的环境中。
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