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首页> 外文期刊>Limnology and Oceanography >Regeneration, recycling, and trophic transfer of trace metals by microbial food-web organisms in the pelagic surface waters of Lake Erie
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Regeneration, recycling, and trophic transfer of trace metals by microbial food-web organisms in the pelagic surface waters of Lake Erie

机译:伊利湖中上层地表水中微生物食物网微生物对微量金属的再生,再循环和营养转移

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Rapid regeneration of ~(109)Cd and ~(65)Zn from their picoplankton prey into the dissolved phase by micro-zooplankton was observed in water sampled from the pelagic surface waters of Lake Erie (summer 1994 and 1995). Trace metals were added to grazing (lake water < 210 μm) and control (lake water < 0.2 μm) treatments in the form of radiolabeled Synechococcus. Picoplankton (0.2-3 μm) were grazed heavily by consumers in the nanoplankton (3-20 μm) and microplankton (20-210 μm) size classes (collectively referred to as micro-zooplankton) as confirmed by dilution assays used to independently measure grazing activity. Most consumed trace metals were regenerated into the dissolved phase (< 0.2 μm), but some trophic transfer of ~(109)Cd and ~(65)Zn from radiolabeled prey into the nanoplankton and microplankton did occur: ~(65)Zn was transferred 2.5 times more efficiently into the microplankton and 2.9 times more efficiently into the nanoplankton than was ~(109)Cd. Recycling of regenerated ~(109)Cd back into plankton biomass was greater than that for ~(65)Zn. Grazing by microzooplankton influenced the molecular size distribution of regenerated trace metal in the dissolved phase (77±6% ~(109)Cd < 5,000 MW; 8±24% ~(65)Zn < 5,000 MW). These results show that microzooplankton grazing tends to prolong the residence times of metals such as Cd and Zn in the pelagic surface waters of large lakes.
机译:在伊利湖浮游地表水采样的水中(1994年夏季和1995年),观察到〜(109)Cd和〜(65)Zn从它们的微微浮游生物迅速再生成溶解相,并溶解到溶解相中。痕量金属以放射性标记的Synechococcus的形式加入放牧(湖水<210μm)和对照(湖水<0.2μm)处理中。消费者在纳米浮游生物(3-20μm)和微型浮游生物(20-210μm)大小级别(统称为微型浮游动物)中大量放食了浮游生物(0.2-3μm),这通过用于独立测量放牧的稀释测定法得以证实活动。大部分消耗的痕量金属再生为溶解相(<0.2μm),但是〜(109)Cd和〜(65)Zn从放射性标记的猎物向纳米浮游生物和微浮游生物的营养转移确实发生了:〜(65)Zn转移了与〜(109)Cd相比,进入微浮游生物的效率高2.5倍,进入纳米浮游生物的效率高2.9倍。再生的〜(109)Cd循环回浮游生物质的能力大于〜(65)Zn。微浮游动物放牧影响了溶解相中再生微量金属的分子大小分布(77±6%〜(109)Cd <5,000 MW; 8±24%〜(65)Zn <5,000 MW)。这些结果表明,微浮游动物的放牧倾向于延长金属(例如镉和锌)在大湖中上层地表水中的停留时间。

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