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首页> 外文期刊>Lakes & Reservoirs >Six years’ (1992–1997) evolution of phytoplankton communities after recovery by liming in Lake Orta, northern Italy
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Six years’ (1992–1997) evolution of phytoplankton communities after recovery by liming in Lake Orta, northern Italy

机译:在意大利北部的奥尔塔湖上撒石灰恢复后的六年(1992–1997)浮游植物群落的演变

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摘要

Lake Orta became heavily polluted in 1926 by ammonium sulphate and copper. After a couple of years the biological communities became extremely simplified and were composed of a few resistant species. This acute copper pollution was followed by a chronic acidification of the water, brought about by in-lake biochemical oxidation of ammonium. Since the 1960s, heavy metals discharged from some plating factories became an additional source of pollution. After the reduction of ammonium discharge in 1982 and from May 1989 to June 1990 the lake was limed: the pH at overturn increased from pH 4.4 to 5.9, the metals’ concentration decreased and the number of planktonic taxa rapidly increased.The present paper deals with the recent (1992–1997) evolution of the phytoplankton communities analysed by sample clustering: the cluster analysis indicates the separation of two large groups of samples (1992–1993 and 1995–1997). Such clustering is because of the gradual decline of the chlorophytes (for a long period the most important group in Lake Orta) between 1992 and 1994, followed by their marked decrease between 1995 and 1997, during which they were replaced by blue–green algae.Also noticeable was the increase in diatoms, which had disappeared from the phytoplankton community from the 1930s until 1994, but during spring and summer 1997 they amounted to 40% of community abundance. Although it is now possible to describe a phytoplanktonic seasonal succession in Lake Orta, the dissimilarities shown by the cluster analysis seem to indicate the existence of a certain year-to-year variability inside the dominant species assemblage, meaning that the phytoplankton community is still evolving.In spite of the phytoplankton’s fast recovery after liming, it is only since 1994 that the algal community started to change toward a phytoplankton assemblage more typical of deep subalpine lakes.
机译:1926年,奥尔塔湖被硫酸铵和铜污染严重。几年后,生物群落变得极为简化,由一些抗性物种组成。在这种严重的铜污染之后,水的慢性酸化是由于湖内生化氧化铵引起的。自1960年代以来,从某些电镀厂排放的重金属已成为另一种污染源。 1982年铵盐排放量减少之后,从1989年5月到1990年6月,该湖被灰化了:倾翻处的pH从pH 4.4增加到5.9,金属的浓度降低,浮游生物群的数量迅速增加。最近通过样本聚类分析了浮游植物群落(1992-1997年)的演变:聚类分析表明两组大样本是分开的(1992-1993年和1995-1997年)。这种聚集的原因是,1992年至1994年间,绿藻类植物(长期以来是奥尔塔湖中最重要的种群)逐渐减少,随后在1995年至1997年间,它们的数量明显减少,在此期间它们被蓝绿色藻类所取代。同样值得注意的是硅藻的增加,从1930年代到1994年,硅藻从浮游植物群落中消失了,但是在1997年的春季和夏季,硅藻占了群落丰富度的40%。尽管现在可以描述奥尔塔湖中浮游植物的季节性演替,但聚类分析显示的差异似乎表明优势物种集合内部存在一定的逐年变异性,这意味着浮游植物群落仍在演化尽管浮游植物在成泥后迅速恢复,但直到1994年,藻类群落才开始向深亚高山湖泊更典型的浮游植物组合转变。

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