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Species diversity and spatial structure of pelagic zooplankton in a lake of glacial origin during summer stratification

机译:夏季地层冰川期湖泊浮游浮游动物的物种多样性和空间结构

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摘要

Lake South Volos (55° 37′ N, 27° 08′ E, area 1.2 km2, max. depth 40.4 m) is a stratificated mesotrophic lake with some features of oligotrophy. From May to September 200 0, 54 Rotifera, 11 Copepoda and 17 Cladocera species were recorded in the pelagic zone. A substantional increase in the depth of the thermocline took place from May to July. It was accompanied by a rise in species richness of the zooplankton (Rotifera and Crustacea). Increase in the number of non-overlapping niches was observed with the increase in rotifer species richness. It was shown, that maximum species density was related to temperature, and ecological groups of the species developed in water layers of certain temperatures, though this may not always be indicative of thermopreference. Species dominance in a particular water layer in the column was caused by a combination of factors (“sliced functioning”) influencing the zooplankton community. No active diurnal movements between the layers (epi-, meta- and, hypolimnion, and the upper hypolimnion/clinolimnion) were demonstrated by the majority of crustacean species.
机译:南沃洛斯湖(北纬55°37′,东经27°08′,面积1.2 km2 ,最大深度40.4 m)是一种层状的中营养湖,具有一些低营养的特征。从200年5月至9月,在中上层带记录了54种轮虫,11种Co足类和17种角须藻。从5月到7月,温床的深度大大增加。伴随着浮游动物(轮虫和甲壳纲)物种丰富度的增加。随着轮虫种类丰富度的增加,观察到非重叠生态位的数量增加。结果表明,最大物种密度与温度有关,物种的生态群在一定温度的水层中发育,尽管这可能并不总是表明热偏好。列中特定水层中的物种优势是由影响浮游动物群落的多种因素(“分割功能”)共同引起的。大多数甲壳类动物没有表现出层间(上层,下层和次层水层,以及上层次层水层/斜层水层)之间的活跃的昼间运动。

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