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Depth-distribution of surface sediment diatoms in Lake Tovel, Italy

机译:意大利托维尔湖表面沉积物硅藻的深度分布

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摘要

Surface sediment, which covers large parts of lake bottoms, is a widespread microhabitat for which specific algae quantification procedures have been developed (Eaton & Moss 1966). Sediment habitat can promote selection of diatom taxa with specific characteristics such as motility, which is required to avoid being buried and losing access to light (Wetzel 2001). Diatoms inhabiting the surface sediment of lakes have also been shown to perform vertical migrations in the upper portion of the sediment; cell numbers on the surface start to increase before sunrise and reach a maximum at about midmorning (Wetzel 2001). Notwithstanding these peculiarities, the ecology of depth distribution of surface sediment diatoms in lakes is a topic which has received limited attention (Round 1956, Round 1961, Bradbury & Winter 1976, Stevenson & Stoermer 1981, Gaiser & Johansen 2000). An aspect explored to some extent is the analysis of the depth distribution of taphocoenoses, a field of study needed to develop training sets to reconstruct lake-level fluctuations (Lotter 1988, Yang & Duthie 1995) often linked to climate change in the Holocene (Bigler 2001). However, ecological aspects, particularly the identification of the most influential factors by means of mul-tivariate analysis, have been only seldom considered (Wolin & Duthie 1999).
机译:覆盖湖底大部分区域的地表沉积物是一种广泛的微生境,已针对其开发了特定的藻类定量程序(Eaton&Moss 1966)。沉积物的生境可以促进硅藻类群的选择,使其具有诸如运动性等特定特征,这是避免被掩埋和失去光照的必要条件(Wetzel 2001)。居住在湖泊表层沉积物中的硅藻也被证明在沉积物上部进行垂直迁移。在日出之前,表面的细胞数量开始增加,并在大约中午达到最大值(Wetzel 2001)。尽管有这些特殊性,但湖泊中表层沉积物硅藻深度分布的生态学问题仍然受到关注(Round 1956,Round 1961,Bradbury&Winter 1976,Stevenson&Stoermer 1981,Gaiser&Johansen 2000)。在一定程度上探讨了一个方面,即对胡同的深度分布进行了分析,这是开发训练集以重建通常与全新世(Bigler)气候变化有关的湖面波动(Lotter 1988,Yang&Duthie 1995)所需要的研究领域。 2001)。但是,很少考虑生态方面的问题,尤其是通过多变量分析来确定最有影响力的因素(Wolin&Duthie 1999)。

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