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Uncoupling of Bacterial and Terrigenous Dissolved Organic Matter Dynamics in Decomposition Experiments

机译:分解实验中细菌和陆源溶解有机物动力学的解耦

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摘要

The biodegradability of terrigenous dissolved organic matter (tDOM) exported to the sea has a major impact on the global carbon cycle, but our understanding of tDOM bioavailability is fragmentary. In this study, the effects of preparative tDOM isolation on microbial decomposition were investigated in incubation experiments consisting of mesocosms containing mesohaline water from the Baltic Sea. Dissolved organic carbon (DOC) consumption, molecular DOM composition, bacterial activities, and shifts in bacterial community structure were compared between mesocosms supplemented with riverine tDOM, either as filtered, particle-free river water or as a concentrate obtained by lyophilization/tangential ultrafiltration, and those containing only Baltic Sea water or river water. As shown using ultra-high-resolution mass spectrometry (15 Tesla Fourier-transform ion cyclotron resonance mass spectrometry, FT-ICR-MS) covering approximately 4600 different DOM compounds, the three DOM preparation protocols resulted in distinct patterns of molecular DOM composition. However, despite DOC losses of 4–16% and considerable bacterial production, there was no significant change in DOM composition during the 28-day experiment. Moreover, tDOM addition affected neither DOC degradation nor bacterial dynamics significantly, regardless of the tDOM preparation. This result suggested that the introduced tDOM was largely not bioavailable, at least on the temporal scale of our experiment, and that the observed bacterial activity and DOC decomposition mainly reflected the degradation of unknown, labile, colloidal and low-molecular weight DOM, both of which escape the analytical window of FT-ICR-MS. In contrast to the different tDOM preparations, the initial bacterial inoculum and batch culture conditions determined bacterial community succession and superseded the effects of tDOM addition. The uncoupling of tDOM and bacterial dynamics suggests that mesohaline bacterial communities cannot efficiently utilize tDOM and that in subarctic estuaries other factors are responsible for the removal of imported tDOM.
机译:出口到海洋的陆源溶解有机物(tDOM)的生物降解性对全球碳循环具有重大影响,但是我们对tDOM生物利用度的理解是零碎的。在这项研究中,在孵育实验中研究了制备性tDOM分离对微生物分解的影响,该实验由来自波罗的海的含有中卤水的中胚层组成。比较了补充有河流tDOM的中膜作为过滤的无颗粒河水或通过冻干/切向超滤获得的浓缩物的溶解性有机碳(DOC)消耗量,分子DOM组成,细菌活性和细菌群落结构的变化,以及仅包含波罗的海水或河水的水。如使用超高分辨率质谱法(15 Tesla傅立叶变换离子回旋共振质谱法,FT-ICR-MS)所显示的,该质谱法涵盖大约4600种不同的DOM化合物,这三种DOM制备方案导致了分子DOM组成的不同模式。但是,尽管DOC损失了4%至16%,并且细菌产生量很大,但在28天的实验中,DOM的组成没有明显变化。而且,无论使用何种tDOM,添加tDOM都不会显着影响DOC降解或细菌动力学。该结果表明,引入的tDOM至少在我们的实验时间尺度上基本上没有生物利用度,并且观察到的细菌活性和DOC分解主要反映了未知,不稳定,胶体和低分子量DOM的降解,这两种逃脱了FT-ICR-MS的分析窗口。与不同的tDOM制剂不同,初始细菌接种物和分批培养条件决定了细菌群落的继承,并取代了添加tDOM的作用。 tDOM和细菌动力学的解耦表明,中盐细菌群落无法有效利用tDOM,在弧下河口中,其他因素也导致了进口tDOM的去除。

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