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首页> 外文期刊>Journal of paleolimnology >Do changes in water depth and water level influence the diatom diversity of Yunlong Lake, in Yunnan Province, Southwest China?
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Do changes in water depth and water level influence the diatom diversity of Yunlong Lake, in Yunnan Province, Southwest China?

机译:水深和水位的变化会影响云龙湖的硅藻多样性,云南省中国云南省?

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摘要

Exploring whether diatom diversity in a lake sediment core is representative of that of the entire lake is important for determining the response of lake diatom diversity to global climatic warming. In this study, Yunlong Lake, an alpine lake located in Yunnan Province, Southwest China, was investigated to explore this question over both space and time. Spatially, we investigated diatom diversity patterns in 62 surface sediment samples from different locations and depth zones of Yunlong lake and found essentially constant diatom diversity across the entire lake basin. Temporally, we studied a well-dated sediment core from the lake center to explore whether long-term water-level changes influenced diatom diversity over the last similar to 100 years. Changes in the annual average sediment accumulation rates indicate that the water level of Yunlong Lake increased substantially after the construction of a dam. However, there is no obvious relationship between diatom diversity and water-level changes, which suggests at this site long-term water-level changes did not influence diatom diversity. Comparative analysis of the results for Yunlong Lake with those for other lakes indicates that for relatively strongly mixed lakes with a simple morphology and uniform shoreline microhabitat, such as Yunlong Lake, differences in water depth and changes in water level may not influence diatom diversity. In such cases, the diatom diversity from a sediment core is likely to be representative of that of the entire lake during specific time intervals. Therefore, such lakes may be optimal for studies of changes in past diatom diversity using sediment cores.
机译:探索湖泊沉积物核心的硅藻多样性代表整个湖泊的代表,对于确定硅藻湖多样性对全球气候变暖的反应非常重要。在这项研究中,位于中国西南部云南省的高山湖云龙湖被调查,在两个空间和时间上探索这个问题。在空间上,我们研究了来自云龙湖的不同地点和深度区域的62个表面沉积物样本中的硅藻分集模式,并在整个湖泊盆地中发现基本恒定的硅藻多样性。在暂时,我们研究了来自湖中心的日期沉积物核心,探索长期的水位变化是否影响到100年的最后一个相似的硅藻多样性。年平均沉积物积累率的变化表明,云龙湖的水位大幅增加了一个大坝的建设后大幅增加。然而,硅藻多样性与水位变化之间没有明显的关系,这在该网站上表明长期水位变化不会影响硅藻多样性。对其他湖泊云龙湖的结果的比较分析表明,对于相对强烈的湖泊,具有简单的形态和均匀的海岸线微藻,如云龙湖,水深的差异和水位的变化可能不会影响硅藻多样性。在这种情况下,来自沉积物核心的硅藻分集可能在特定时间间隔内代表整个湖泊的代表。因此,使用沉积物芯的过去硅藻多样性的改变可能是最佳的最佳选择。

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