I. R. Jónsson, G. S. Jónsson, J. Ólafsson, S. Einarsson, Þ. Antonsson
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引用次数: 2
摘要
双硅藻属(Didymosphenia geminata)自20世纪90年代初以来,M. Smith一直在冰岛的一些河流中形成有害的生长(JONSSON et al. 2000)。这种藻类覆盖在多石的河床上,像灰色的羊毛状覆盖物,可以消灭大型植物和苔藓。当该物种首次在冰岛被发现时,其他国家类似的大规模发展的文献信息很少,但从那时起,D. geminata的令人讨厌的外观在全球范围内扩大,入侵行为已经被认识到(SPAULDING & ELWELL 2007)。冰岛是一个火山岛,主要由第四纪和第三纪的玄武岩组成。使用基岩类型作为陆地区域分类的标准(GuoJONSSON 1990),电导率通常在新火山带内的河流和源于植被丰富的高地集水区的直接径流长的河流中最高,而第三系玄武岩组的短径流河流的电导率较低(ÜISLASON et al. 1998, JONSSON et al. 2000)。从植被繁茂的荒野和河流中流出的河流
The colonization of the invasive diatom Didymosphenia geminata in Icelandic rivers
The diatom species Didymosphenia geminata (Lyngb.) M. Smith has been forming nuisance growths in some rivers in Iceland since the early 1990s (JONSSON et al. 2000). The algae covers stony river bed as a grayish, woolen cover and can eliminate macrophytes and moss. When the species was first found in Iceland, information from the literature of similar mass development in other countries was sparse, but since then time the nuisance appearance of D. geminata has been expanding on the global scale and the invasive behaviour has been recognized (SPAULDING & ELWELL 2007). lceland is a volcanic island predominantly formed of basaltic rock of Quaternary and Tertiary age. Using the type ofthe bedrock as a criteria for land zone classification (GuoJONSSON 1990), conductivity is generally highest in rivers within the neovolcanic zone and in long direct run-off rivers originating in well-vegetated highland catchments, whereas conductivity is lower in short run-off rivers of the Tertiary basalt formation (ÜISLASON et al. 1998, JONSSON et al. 2000). Rivers running from well-vegetated moors and rivers