首页> 外文期刊>Journal of plankton research >Climate-induced input of turbid glacial meltwater affects vertical distribution and community composition of phyto- and zooplankton
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Climate-induced input of turbid glacial meltwater affects vertical distribution and community composition of phyto- and zooplankton

机译:气候引起的混浊冰川融水的输入影响浮游植物和浮游植物的垂直分布和群落组成

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摘要

Receding glaciers are among the most obvious changes caused by global warming, and glacial meltwater entering lakes generally forms plumes of particles. By taking vertical samples along a horizontal gradient from such a particle source, we found that photosynthetically active radiation (PAR) and ultraviolet radiation (UVR) attenuated 20-25% faster close to the inflow of suspended particles compared with the more transparent part of the gradient. All sampled stations had a deep chlorophyll a (Chl a) maximum at 15-20 m which was more distinct in the transparent part of the horizontal gradient. Picocyanobacteria increased in abundance in more transparent water and their numbers were tightly correlated with the intensity of the deep Chl a maxima. Motile species of phytoplankton had a deeper depth distribution in transparent versus less transparent water. Yet other species, like Chrysochromulina parva, that can withstand high PAR intensities and low nutrient concentrations, increased in abundance as the water became more transparent. Also copepods increased in abundance, indicating that they are more successful in transparent water. We conclude that sediment input into lakes creates horizontal gradients in PAR and UVR attenuation which strongly affect both distribution and behavior of phyto- and zooplankton. The input of glacial flour creates a subhabitat that can function as a refuge for species that are sensitive to high PAR and UVR exposure. When the glacier has vanished, this habitat may disappear. During the melting period, with heavy sediment input, we predict that competitive species in transparent waters, like Chrysocromulina, picocyanobacteria and copepods, will become less common. The deep Chl a maxima is also likely to become less developed. Hence, glacier melting will probably have profound effects on both species composition and behavior of several planktonic taxa with potential effects on the food web.
机译:后退冰川是全球变暖引起的最明显变化之一,进入湖泊的冰川融水通常形成颗粒羽流。通过从这样的粒子源沿水平梯度采集垂直样本,我们发现与悬浮粒子的更透明部分相比,光合有效辐射(PAR)和紫外线(UVR)在接近悬浮粒子流入处的衰减速度快20-25%。梯度。所有采样站在15-20 m处都有一个深的叶绿素a(Chl a)最大值,这在水平梯度的透明部分更为明显。在更透明的水中,蓝藻细菌的数量大量增加,并且它们的数量与深部最大的Chl a max的强度紧密相关。游动性浮游植物在透明水与不透明水中的深度分布较深。随着水变得更加透明,可以承受高PAR强度和低养分浓度的其他物种,如金绿藻,会增加其丰度。 co足类的数量也增加了,表明它们在透明水中更成功。我们得出的结论是,输入湖泊的沉积物会在PAR和UVR衰减中产生水平梯度,从而强烈影响浮游植物和浮游动物的分布和行为。冰粉的输入会产生一个亚生境,可作为对高PAR和UVR暴露敏感的物种的避难所。冰川消失后,这种栖息地可能会消失。在融化期间,随着大量泥沙的输入,我们预测透明水域中的竞争性物种(如金眼鲷,微小蓝细菌和co足类)将变得不那么普遍。深的Chl最大值也可能变得不那么发达。因此,冰川融化将可能对几种浮游生物分类的物种组成和行为产生深远影响,并对食物网产生潜在影响。

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