Utilisation of dissolved organic carbon from different sources by pelagic bacteria in an acidic mining lake

N. Kamjunke, Chris Bohn, J. Grey
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引用次数: 17

Abstract

We compared growth rates and efficiencies of pelagic bacteria from an extremely acidic mining lake (pH 2.6, mean depth 4.6 m) supplied with different sources of carbon: (1) excreted by phytoplankton, (2) derived from benthic algae, (3) entering the lake via ground water, and (4) leached from leaf litter. Bacteria exhibited high growth rate and efficiency on exudates of pelagic and benthic algae. In contrast, they showed a lower growth rate and efficiency with organic carbon from ground water, and grew at a very high rate but a very low efficiency on leaf leachate. Results from stable isotope analyses indicate a greater importance of benthic exudates and leaf leachate for bacteria in the epilimnion, and a higher impact of ground water sources in the hypolimnion. Given the magnitude of differential source inputs into the lake, we suggest that benthic primary production was the most important carbon source for pelagic bacteria. The benthic-pelagic coupling seems to be more relevant in this shallow acidic lake with low pelagic carbon dioxide concentrations than in neutral lakes.
酸性采矿湖中浮游细菌对不同来源的溶解有机碳的利用
我们比较了一个极酸性采矿湖(pH值2.6,平均深度4.6 m)中浮游细菌的生长速度和效率,这些湖泊提供了不同的碳来源:(1)浮游植物排出的碳,(2)底栖藻类产生的碳,(3)通过地下水进入湖泊,(4)从凋落叶中浸出的碳。细菌在远洋和底栖藻类分泌物中表现出较高的生长速度和效率。相反,它们对地下水有机碳的生长速率和效率较低,对叶片渗滤液的生长速率很高,但效率很低。稳定同位素分析的结果表明,底栖生物渗出物和树叶渗滤液对土壤中细菌的影响更大,而地下水对土壤中细菌的影响更大。考虑到不同来源输入湖泊的规模,我们认为底栖生物初级生产是中上层细菌最重要的碳源。与中性湖泊相比,海底-远洋耦合似乎在这种低远洋二氧化碳浓度的浅酸性湖泊中更为相关。
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