Preface "Evolutionary and geological history of the Balkan lakes Ohrid and Prespa"
Preface "Evolutionary and geological history of the Balkan lakes Ohrid and Prespa"
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序言“巴尔干奥赫里德湖和普雷斯帕湖的演化和地质历史”
DOI：
10.5194/bg-8-995-2011
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发表时间：
2011
期刊：
影响因子：
4.9
通讯作者：
T. Wilke
中科院分区：
文献类型：
--
作者：
B. Wagner;T. Wilke
全世界只有极少数淡水湖具有悠久的地质历史，往往导致了高度的地方性生物多样性。例如位于西伯利亚的贝加尔湖、南美洲的的喀喀湖以及东非大裂谷的坦噶尼喀湖和马拉维湖。大多数此类“古老”湖泊都有构造起源，并且位于构造仍然活跃的地区。欧洲此类湖泊的两个著名代表是巴尔干半岛上的小型“姐妹湖”普雷斯帕湖和奥赫里德湖。奥赫里德湖如今的表面积为 358 km2，最大水深为 289 m，平均水深为 155 m，体积为 55 km3（Matzinger 等，2006）。邻近的普雷斯帕湖表面积仅为 254 km2，最大和平均水深分别为 58 m 和 14 m，体积为 3.6 km3（Matzinger 等，2006；Albrecht 和 Wilke，2008）。两个湖之间的最短直线距离为 9 公里，普雷斯帕湖（海拔 849 米）通过地下喀斯特通道与奥赫里德湖（海拔 693 米）在水文上相连。
Worldwide only very few freshwater lakes exist that are characterised by a long geological history, often leading to an outstanding degree of endemic biodiversity. Examples include Lake Baikal located in Siberia, Lake Titicaca in South America, and lakes Tanganyika and Malawi in the East African Rift. Most of such “old” lakes have a tectonic origin and are located in regions, wich are still tectonically active. Two famous representatives of such lakes in Europe are the small “sister lakes” Prespa and Ohrid on the Balkan Peninsula. Lake Ohrid has today a surface area of 358 km2, a maximum water depth of 289 m, a mean water depth of 155 m, and a volume of 55 km3 (Matzinger et al., 2006). The surface area of neighbouring Lake Prespa is only 254 km2, its maximum and mean water depths are 58 m and 14 m, respectively, and its volume is 3.6 km3 (Matzinger et al., 2006; Albrecht and Wilke, 2008). The shortest straight line distance between the two lakes is 9 km and Lake Prespa (altitude 849 m a.s.l.) is connected hydrologically with Lake Ohrid (altitude 693 m a.s.l.) via underground karstic channels.
普雷斯帕湖和奥赫里德湖沉积物记录了过去约 50 年来巴尔干地区的环境变化
影响因子：
4.9
作者：
Wagner B;Vogel H;Zanchetta G;Sulpizio R
通讯作者：
Sulpizio R