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苏打湖细菌群落对模拟降雨的生长响应。

Growth response of soda lake bacterial communities to simulated rainfall.

作者信息

Krammer M, Velimirov B, Fischer U, Farnleitner A H, Herzig A, Kirschner A K T

机构信息

Center of Anatomy and Cell Biology, Medical University Vienna, Waehringerstr. 10, 1090 Vienna, Austria.

出版信息

Microb Ecol. 2008 Feb;55(2):194-211. doi: 10.1007/s00248-007-9267-5. Epub 2007 Jul 6.

Abstract

Moderately saline soda lakes harbor extremely abundant and fast growing bacterial communities. An interesting phenomenon of an explosive bacterial growth in shallow soda lakes in Eastern Austria after dilution with rainwater, concomitantly with a significant decrease in temperature was observed in a former study. In the present study, we tried to identify the factors being responsible for this enhanced bacterial growth in laboratory batch cultures. Three experiments were performed with water taken from two different lakes at different seasons. Natural soda lake water was diluted with distilled water, artificial lake water, sterile filtered soda lake water, and grazer-free water to test (1) for the influence of compatible solutes released to the environment and reduced salt stress after osmotic down-shock, (2) for the influence of nutrients, which may be washed in from the dry areas of the lake bottom after rainfall and (3) for the decrease of grazing pressure due to dilution. The potential influence of (4) viruses was indirectly deduced. The response of the bacterial community to the manipulations was measured by changes in bacterial numbers, the incorporation of (3)H-leucine and the concomitant determination of the amount of (3)H-leucine uptaking bacteria by microautoradiography. The influence of the environmental factors enhancing bacterial growth after a simulated rainfall event showed variations between the lakes and over the seasons. The addition of nutrients was, in all experiments, the main factor triggering bacterial growth. The decrease in grazing pressure and viral lysis after dilution was of significant importance in two of three experiments. In the experiment with the highest salinity, we could show that either compatible solutes released after osmotic down-shock and used as a source of nutrients for the soda lake bacterial populations or reduced salt stress were most probably responsible for the observed marked enhancement of bacterial growth.

摘要

中度盐碱化的苏打湖拥有极其丰富且生长迅速的细菌群落。在之前的一项研究中,观察到奥地利东部浅苏打湖在被雨水稀释后,细菌出现爆发性生长,同时温度显著下降这一有趣现象。在本研究中,我们试图在实验室分批培养中确定导致细菌生长增强的因素。使用取自两个不同湖泊在不同季节的水进行了三个实验。用蒸馏水、人工湖水、无菌过滤的苏打湖水和无食草动物的水稀释天然苏打湖水,以测试:(1) 渗透休克后释放到环境中的相容性溶质以及盐胁迫减轻的影响;(2) 降雨后可能从湖底干燥区域冲刷进来的养分的影响;(3) 稀释导致的捕食压力降低。(4) 病毒的潜在影响是间接推断出来的。通过细菌数量的变化、³H-亮氨酸的掺入以及通过微放射自显影法同时测定摄取³H-亮氨酸的细菌数量,来衡量细菌群落对这些操作的反应。模拟降雨事件后促进细菌生长的环境因素的影响在不同湖泊和不同季节之间存在差异。在所有实验中,添加养分是引发细菌生长的主要因素。稀释后捕食压力的降低和病毒裂解在三个实验中的两个中具有重要意义。在盐度最高的实验中,我们可以表明,渗透休克后释放并用作苏打湖细菌种群养分来源的相容性溶质或减轻的盐胁迫很可能是观察到的细菌生长显著增强的原因。

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