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含水层沉积物中硝酸盐还原条件下病毒产生与碳矿化之间的相关性。

Correlation between viral production and carbon mineralization under nitrate-reducing conditions in aquifer sediment.

作者信息

Pan Donald, Watson Rachel, Wang Dake, Tan Zheng Huan, Snow Daniel D, Weber Karrie A

机构信息

School of Biological Sciences, University of Nebraska-Lincoln, Lincoln, NE, USA.

Water Sciences Laboratory, University of Nebraska-Lincoln, Lincoln, NE, USA.

出版信息

ISME J. 2014 Aug;8(8):1691-703. doi: 10.1038/ismej.2014.38. Epub 2014 Mar 27.

Abstract

A variety of microbially mediated metabolic pathways impact biogeochemical cycling in terrestrial subsurface environments. However, the role that viruses have in influencing microbial mortality and microbial community structure is poorly understood. Here we investigated the production of viruses and change in microbial community structure within shallow alluvial aquifer sediment slurries amended with (13)C-labeled acetate and nitrate. Biostimulation resulted in production of viruses concurrent with acetate oxidation, (13)CO2 production and nitrate reduction. Interestingly, change in viral abundance was positively correlated to acetate consumption (r(2)=0.6252, P<0.05) and (13)CO2 production (r(2)=0.6572, P<0.05); whereas change in cell abundance was not correlated to acetate consumption or (13)CO2 production. Viral-mediated cell lysis has implications for microbial community structure. Betaproteobacteria predominated microbial community composition (62% of paired-end reads) upon inoculation but decreased in relative abundance and was negatively correlated to changes in viral abundance (r(2)=0.5036, P<0.05). As members of the Betaproteobacteria decreased, Gammaproteobacteria, specifically Pseudomonas spp., increased in relative abundance (82% of paired-end reads) and was positively correlated with the change in viral abundance (r(2)=0.5368, P<0.05). A nitrate-reducing bacterium, Pseudomonas sp. strain Alda10, was isolated from these sediments and produced viral-like particles with a filamentous morphology that did not result in cell lysis. Together, these results indicate that viruses are linked to carbon biogeochemistry and community structure in terrestrial subsurface sediments. The subsequent cell lysis has the potential to alter available carbon pools in subsurface environments, additionally controlling microbial community structure from the bottom-up.

摘要

多种微生物介导的代谢途径影响着陆地地下环境中的生物地球化学循环。然而,病毒在影响微生物死亡率和微生物群落结构方面所起的作用却鲜为人知。在此,我们研究了在添加了¹³C标记的乙酸盐和硝酸盐的浅层冲积含水层沉积物浆液中病毒的产生以及微生物群落结构的变化。生物刺激导致病毒的产生与乙酸盐氧化、¹³CO₂产生和硝酸盐还原同时发生。有趣的是,病毒丰度的变化与乙酸盐消耗呈正相关(r² = 0.6252,P < 0.05)以及与¹³CO₂产生呈正相关(r² = 0.6572,P < 0.05);而细胞丰度的变化与乙酸盐消耗或¹³CO₂产生无关。病毒介导的细胞裂解对微生物群落结构有影响。接种时β-变形菌在微生物群落组成中占主导地位(双端读数的62%),但相对丰度下降,且与病毒丰度的变化呈负相关(r² = 0.5036,P < 0.05)。随着β-变形菌成员数量减少,γ-变形菌,特别是假单胞菌属,相对丰度增加(双端读数的82%),且与病毒丰度的变化呈正相关(r² = 0.5368,P < 0.05)。从这些沉积物中分离出一种硝酸盐还原细菌,假单胞菌属菌株Alda10,它产生了具有丝状形态的类病毒颗粒,但并未导致细胞裂解。总之,这些结果表明病毒与陆地地下沉积物中的碳生物地球化学和群落结构有关。随后的细胞裂解有可能改变地下环境中可用的碳库,此外还能从下至上控制微生物群落结构。

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