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首页> 外文期刊>Northeastern Naturalist >Physicochemical Controls on Spatiotemporal Distribution and Benthic Mat Severity of Didymosphenia geminata in Pine Creek, an Unregulated Watershed in Northern Pennsylvania
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Physicochemical Controls on Spatiotemporal Distribution and Benthic Mat Severity of Didymosphenia geminata in Pine Creek, an Unregulated Watershed in Northern Pennsylvania

机译:北宾夕法尼亚州北部的丁香磷磷尼磷磷尼磷磷尼磷磷的近年磷钛席位严重程度的物理化学对照

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Didymosphenia geminata (Didymo) is a benthic freshwater diatom that has been globally expanding its range and extracellular stalk production in freshwater ecosystems. Didymo has been observed in reaches downstream of hypolimnetic reservoir releases in the northeastern US since 2007. This study focused on a newly observed (2013) Didymo occurrence in Pine Creek, a highly forested and unregulated watershed in north-central Pennsylvania. Study objectives included comparing contemporary distribution with historical data to provide insight on historical occurrence, quantifying physicochemical controls on Didymo distribution and benthic mat severity, and examining historical changes in water chemistry that might affect habitat suitability. At present, Didymo cellular distribution is limited to upper reaches of Pine Creek where median soluble reactive phosphorus (SRP) is 2.7 mu g/L; median SRP was 4.8 mu g/L at sites where Didymo was absent. At the epicenter of distribution in Pine Creek where SRP was consistently 2 mu g/L, increased streamflow flashiness and water temperature were associated with decreased benthic mat severity. My results suggest SRP thresholds for Didymo proliferation may vary depending on whether streams are regulated by reservoirs with hypolimnetic releases. Mann-Kendall trends tests of a similar to 20-y water chemistry dataset show that orthophosphate and sulfate concentrations decreased while pH increased within Pine Creek, which may have implications for Didymo habitat suitability. Further research is warranted to determine whether improving water quality following the industrial era may facilitate Didymo colonization.
机译:兼奥米奥奥尼亚奥奥米亚(Didymo)是一种底栖淡水硅藻,在淡水生态系统中一直在全球扩大其范围和细胞外茎生成。自2007年以来,在美国东北部的低辐射水库释放下,达摩了达摩了。本研究专注于新观察到的(2013年)在宾夕法尼亚州北部中部高度森林植物和未降级的流域。研究目标包括将当代分配与历史数据进行比较,以了解历史事件的洞察力,量化兼闺族分布和底栖席严重程度的物理化学控制,以及检查水化学的历史变化可能影响栖息地适用性。目前,DidyMo细胞分布仅限于杉木溪的上游,其中中值可溶性反应性磷(SRP)为2.7μg/ l;中位数SRP在Didymo缺席的地点是4.8亩。在松树溪的分布震中,其中SRP一致&2μg/ l,流出闪烁和水温的提高与底层垫严重程度降低有关。我的结果表明DIDYMO增殖的SRP阈值可能因流储层是否受到低估释放的储层而异。 Mann-Kendall趋势试验类似于20-Y水化学数据集显示,正磷酸盐和硫酸盐浓度在Pine Creek内的pH增加时降低,这可能对DidyMo栖息地适合有影响。有权进一步研究,以确定工业时代后的水质是否可促进戴姆诺殖民化。

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