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首页> 外文期刊>Global change biology >Hemispheric-scale patterns of climate-related shifts in planktonic diatoms from North American and European lakes.
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Hemispheric-scale patterns of climate-related shifts in planktonic diatoms from North American and European lakes.

机译:来自北美和欧洲湖泊的浮游硅藻与气候有关的转变的半球模式。

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摘要

A synthesis of over 200 diatom-based paleolimnological records from nonacidifiedonenriched lakes reveals remarkably similar taxon-specific shifts across the Northern Hemisphere since the 19th century. Our data indicate that these diatom shifts occurred in conjunction with changes in freshwater habitat structure and quality, which, in turn, we link to hemispheric warming trends. Significant increases in the relative abundances of planktonic Cyclotella taxa (P<0.01) were concurrent with sharp declines in both heavily silicified Aulacoseira taxa (P<0.01) and benthic Fragilaria taxa (P<0.01). We demonstrate that this trend is not limited to Arctic and alpine environments, but that lakes at temperate latitudes are now showing similar ecological changes. As expected, the onset of biological responses to warming occurred significantly earlier (P<0.05) in climatically sensitive Arctic regions (median age=AD 1870) compared with temperate regions (median age=AD 1970). In a detailed paleolimnological case study, we report strong relationships (P<0.005) between sedimentary diatom data from Whitefish Bay, Lake of the Woods (Ontario, Canada), and long-term changes in air temperature and ice-out records. Other potential environmental factors, such as atmospheric nitrogen deposition, could not explain our observations. These data provide clear evidence that unparalleled warming over the last few decades resulted in substantial increases in the length of the ice-free period that, similar to 19th century changes in high-latitude lakes, likely triggered a reorganization of diatom community composition. We show that many nonacidified, nutrient-poor, freshwater ecosystems throughout the Northern Hemisphere have crossed important climatically induced ecological thresholds. These findings are worrisome, as the ecological changes that we report at both mid- and high-latitude sites have occurred with increases in mean annual air temperature that are less than half of what is projected for these regions over the next half century.
机译:从未酸化/未富集的湖泊中合成的200多种基于硅藻的古湖泊学记录表明,自19世纪以来,整个北半球的分类群特异性变化非常相似。我们的数据表明,这些硅藻移动与淡水栖息地结构和质量的变化有关,而这又与半球变暖趋势相关。浮游性 P 分类群的相对丰度( P <0.01)显着增加,而重度硅化的 Aulacoseira 分类群( P <0.01)和底栖的草莓属分类群( P <0.01)。我们证明了这种趋势不仅限于北极和高山环境,而且温带纬度的湖泊现在也显示出类似的生态变化。不出所料,与温带地区(中位年龄= AD 1970)相比,在气候敏感的北极地区(中位年龄= AD 1870),对变暖的生物学反应发生的时间明显更早( P <0.05)。在详细的古湖泊学案例研究中,我们报告了来自伍兹湖(加拿大安大略省)的怀特菲什湾的沉积硅藻数据与长期气温变化之间的强相关性( P <0.005)冻结记录。其他潜在的环境因素,例如大气中的氮沉积,无法解释我们的观察结果。这些数据提供了明确的证据,表明过去几十年来无与伦比的变暖导致无冰期长度的显着增加,这与19世纪高纬度湖泊的变化类似,可能引发了硅藻群落组成的重组。我们显示,整个北半球许多非酸化,营养贫乏的淡水生态系统已经跨越了重要的气候诱发生态阈值。这些发现令人担忧,因为我们报告的中高纬度地区都发生了生态变化,年平均气温升高幅度还不到下半个世纪这些地区的预期水平的一半。

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