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首页> 外文期刊>Canadian Journal of Fisheries and Aquatic Sciences >Long-term assessments of ecological effects of anthropogenic stressors on aquatic ecosystems from paleoecological analyses: challenges to perspectives of lake management
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Long-term assessments of ecological effects of anthropogenic stressors on aquatic ecosystems from paleoecological analyses: challenges to perspectives of lake management

机译:从古生态分析对人为应激源对水生生态系统生态影响的长期评估:对湖泊管理观点的挑战

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摘要

Paleolimnological techniques are important for determining background ecological conditions and ecosystem responses to stressors when long- term data sets are absent. Research at the Dorset Environmental Sciences Centre (Ontario, Canada) has included paleolimnological studies to determine the effects of anthropogenic stressors on shield lakes, including eutrophication, acidic deposition, and climate change. Diatom- based total phosphorus (TP) inferences suggest that [TP] has declined in some lakes, despite increased inputs from anthropogenic sources. When coupled with siliceous algae- based pH inferences that suggest landscape- scale long- term acidification, these results indicate that the ecological effects of anthropogenic P inputs are being masked by the cumulative effects of multiple stressors. Detailed stratigraphic analyses of lakes that have experienced severe anthropogenic disturbances indicate that despite measured and inferred recovery in epilimnetic [TP] to predisturbance concentrations, pelagic communities have not recovered to predisturbance community composition; profundal communities and the variables associated with water quality (e. g., hypolimnetic oxygen) have also not recorded recovery. This suggests that (i) typical modeling approaches to quantify the effects of anthropogenic inputs on lake water [TP] should be used with caution and (ii) lake management approaches that follow the paradigm of "water quality recovery = biological recovery" may not be applicable to ecosystems being affected by multiple anthropogenic stressors.
机译:当缺乏长期数据集时,古生物学技术对于确定背景生态条件和生态系统对压力源的响应非常重要。多塞特郡环境科学中心(加拿大安大略省)的研究包括古脂学研究,以确定人为胁迫因素对盾构湖的影响,包括富营养化,酸性沉积和气候变化。基于硅藻的总磷(TP)推断表明,尽管来自人为来源的投入增加,但某些湖泊的[TP]有所下降。当结合硅藻藻的pH推断表明景观规模的长期酸化时,这些结果表明人为磷输入的生态效应被多种胁迫源的累积效应所掩盖。对遭受严重人为干扰的湖泊进行的详细地层分析表明,尽管上表皮[TP]的测量和推断恢复程度达到扰动前的浓度,但远洋群落并未恢复到扰动前的群落组成。底层社区和与水质相关的变量(例如,低氧氧气)也没有记录到恢复。这表明(i)应谨慎使用用于量化人为输入对湖水[TP]的影响的典型建模方法,并且(ii)遵循“水质恢复=生物恢复”范式的湖泊管理方法可能不适用。适用于受到多种人为压力源影响的生态系统。

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