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海洋、中盐度和低盐度细菌群落对陆源碳添加的差异响应。

Differential responses of marine, mesohaline and oligohaline bacterial communities to the addition of terrigenous carbon.

作者信息

Herlemann D P R, Manecki M, Dittmar T, Jürgens K

机构信息

Leibniz Institute for Baltic Sea Research Warnemünde (IOW), Biological Oceanography, Seestrasse 15, Rostock, D-18119, Germany.

Research Group for Marine Geochemistry, Institute for Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University Oldenburg, Carl-von-Ossietzky-Str, Oldenburg, 9-11 D-26129, Germany.

出版信息

Environ Microbiol. 2017 Aug;19(8):3098-3117. doi: 10.1111/1462-2920.13784. Epub 2017 May 29.

Abstract

In response to global warming, increasing quantities of tDOM are transported through estuaries from land to the sea. In this study, we investigated microbial responses to increased tDOM concentrations in three salinity regimes (salinity: 32, 7 and 3) characteristic of the Baltic Sea. Mesocosm experiments performed in May and November revealed low (0-6%) dissolved organic carbon (DOC) utilisation. Molecular DOM analyses using ultrahigh-resolution mass spectrometry identified the terrigenous signal in the tDOM manipulation, but the molecular changes in DOM levels over the course of the experiment were subtle. However, tDOM had significant stimulatory effects on bacterial production in the oligohaline mesocosms. The shift in the bacterial community composition was especially prominent in the tDOM-amended marine and mesohaline mesocosms, but not in the oligohaline mesocosms after 7 and 11 days of incubation. These results suggested the inherent ability of oligohaline bacterial communities to adapt to high tDOM concentrations and therefore to use tDOM. The higher rates of bacterial activity and DOC removal in mesocosms containing UV-pretreated tDOM supported the increased bioavailability of photoinduced, modified tDOM. The overall low rates of microbial tDOM utilisation highlights the importance of abiotic factors in determining the distribution and dynamics of tDOM in estuaries.

摘要

为应对全球变暖,越来越多的陆源溶解性有机物(tDOM)通过河口从陆地输送到海洋。在本研究中,我们调查了波罗的海三种盐度状态(盐度分别为32、7和3)下微生物对tDOM浓度增加的反应。5月和11月进行的中宇宙实验显示,溶解性有机碳(DOC)利用率较低(0 - 6%)。使用超高分辨率质谱进行的分子DOM分析确定了tDOM处理中的陆源信号,但实验过程中DOM水平的分子变化很细微。然而,tDOM对低盐度中宇宙中的细菌生产有显著的刺激作用。在tDOM添加的海洋和中盐度中宇宙中,细菌群落组成的变化尤为显著,但在低盐度中宇宙中培养7天和11天后则不明显。这些结果表明,低盐度细菌群落具有适应高tDOM浓度并因此利用tDOM的内在能力。含有紫外线预处理tDOM的中宇宙中细菌活性和DOC去除率较高,这支持了光诱导、改性tDOM生物可利用性的增加。微生物对tDOM的总体低利用率凸显了非生物因素在决定河口tDOM分布和动态中的重要性。

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