Response of Hypolimnetic Water and Bottom Sediment Microbial Communities to Freshwater Salinization—A Microcosm Experiment

Jean-Christophe Gagnon, Valérie Turcotte Blais, C. Lazar
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Abstract

The introduction of NaCl in freshwater caused by winter runoffs is a problem whose consequences are still little understood. We sought to analyze the effect of NaCl addition on microbial communities of the hypolimnion and bottom sediments of a Canadian lake. Using microcosms comprising a salinity gradient varying between 0.01 and 3.22 ppt (10–3220 mg/L−1) NaCl, we investigated the effect of salinity on prokaryotic absolute abundance and diversity, following a three- and six-week exposure, and detected the presence of a salinity threshold for microbial communities’ differentiation. We observed a significant decline of bacterial diversity after six weeks in hypolimnetic samples. In the sediments, no clear effect of NaCl was observed on abundance or diversity, despite the presence of variations throughout the salinity gradient. The implication of nutrient fluctuations as well as the co-occurrence of species and inter-domain interactions is likely and would strongly contribute to the development of salt-exposed prokaryotic communities. In hypolimnetic water and sediments, the archaeal and eukaryotic communities differed significantly from 0.93 ppt (930 mg/L−1), while only conclusive at 1.9 ppt (1900 mg/L−1) NaCl in bacteria, meaning that the regulations in place are possibly suitable for the protection of the microbial communities in the hypolimnion and sediment lake layers.
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低盐度水体和底泥微生物群落对淡水盐碱化的响应——一个微观实验
冬季径流引起的淡水中NaCl的引入是一个其后果仍然知之甚少的问题。我们试图分析NaCl添加对加拿大一个湖泊低磷离子和底部沉积物微生物群落的影响。在盐度梯度为0.01 ~ 3.22 ppt (10-3220 mg/L−1)NaCl的环境中,研究了盐度对原核生物绝对丰度和多样性的影响,并检测了微生物群落分化的盐度阈值的存在。我们观察到,在低酶样品中,6周后细菌多样性显著下降。在沉积物中,尽管在整个盐度梯度中存在变化,但NaCl对丰度和多样性没有明显的影响。营养物的波动、物种的共存和区域间的相互作用可能对盐暴露的原核生物群落的发展有很大的促进作用。在低盐度水体和沉积物中,古细菌和真核生物群落在0.93 ppt (930 mg/L−1)之间存在显著差异,而细菌群落在1.9 ppt (1900 mg/L−1)NaCl下存在显著差异,说明现有的规定可能适用于低盐度水体和沉积物湖层微生物群落的保护。
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