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Quaternary Landforms and Basin Morphology Control the Natural Eutrophy of Boreal Lakes and Their Sensitivity to Anthropogenic Forcing

机译:第四纪地貌和盆地形态控制着北方湖泊的自然富营养化及其对人为强迫的敏感性

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Both natural and anthropogenic changes in boreal lakes have been studied utilizing paleolimnological methods, but the spatial variation in the natural conditions of lakes and its connection to geological factors has drawn less attention. Our aims were to examine the spatial distribution of naturally eutrophic lakes on the previously glaciated terrain of central-eastern Finland and the relationship between pre-human disturbance water quality and geological factors related to the basins and their catchments. Furthermore, we studied the pre- to post-human disturbance changes in the diatom assemblages and water quality of 48 lakes (51 sampling sites) across the pre-disturbance phosphorus gradient by using the top-bottom sampling approach and multivariate statistics. According to our results, naturally eutrophic boreal lakes are more common than previously thought, occurring on fine-grained and organic Quaternary landforms, including fine-grained till. Our study emphasizes the importance of the previously overlooked matter of till grain-size variation as a driver behind the spatial variation in the natural trophic states of boreal lakes. The location of a lake in the hydrologic landscape and basin morphology appear to be important factors as well. Shallow, naturally eutrophic lakes with short water residence times and high catchment area to lake area and volume ratios have been particularly sensitive to anthropogenic forcing. Our results indicate that cultural eutrophication is not the only water protection challenge for the relatively remote and dilute boreal lakes, but salinization and alkalinization are also serious threats that should be taken into account. Therefore, it is crucial to consider the notable variation in the natural conditions of boreal lakes in addition to mitigating the effects of anthropogenic forcing, such as nutrient loading, catchment erosion, salt pollution, and climate change, in order to achieve efficient water protection.
机译:北部湖泊的自然变化和人为变化都已通过古湖泊学方法进行了研究,但是湖泊自然条件的空间变化及其与地质因素的联系引起了较少的关注。我们的目的是研究芬兰中东部先前冰川化地区自然富营养化湖泊的空间分布,以及人类前干扰水质量与与盆地及其流域有关的地质因素之间的关系。此外,我们使用上下采样方法和多元统计数据研究了人类在扰动前磷梯度范围内48个湖泊(51个采样点)的硅藻组合和水质之前的扰动变化。根据我们的结果,自然富营养化的北方湖泊比以前认为的要普遍得多,发生在细粒和有机第四纪地貌上,包括细粒耕作地。我们的研究强调了以前忽略的耕种直到晶粒大小变化这一问题的重要性,因为它是北方湖泊自然营养状态的空间变化背后的驱动力。湖泊在水文景观和盆地形态中的位置似乎也是重要因素。浅水,自然富营养化的湖泊,其水停留时间短,流域面积与湖泊面积和体积比高,对人为强迫特别敏感。我们的结果表明,富营养化不是相对偏僻和稀疏的北方湖泊面临的唯一水保护挑战,但是盐碱化和碱化也是严重的威胁,应予以考虑。因此,至关重要的是,除了减轻人为强迫的影响(如营养素负荷,集水区侵蚀,盐污染和气候变化)以外,还必须考虑北方湖泊自然条件的显着变化,以实现有效的水保护。

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