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深海热液喷口流体的海底孵化实验揭示了压力和滞后时间对自养微生物群落的影响。

Seafloor Incubation Experiment with Deep-Sea Hydrothermal Vent Fluid Reveals Effect of Pressure and Lag Time on Autotrophic Microbial Communities.

机构信息

Department of Biology, Widener University, Chester, Pennsylvania, USA.

Joint Institute for the Study of Atmosphere and Ocean, University of Washington, Seattle, Washington, USA.

出版信息

Appl Environ Microbiol. 2021 Apr 13;87(9). doi: 10.1128/AEM.00078-21.

DOI:10.1128/AEM.00078-21
PMID:33608294
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC8091007/
Abstract

Depressurization and sample processing delays may impact the outcome of shipboard microbial incubations of samples collected from the deep sea. To address this knowledge gap, we developed a remotely operated vehicle (ROV)-powered incubator instrument to carry out and compare results from and shipboard RNA stable isotope probing (RNA-SIP) experiments to identify the key chemolithoautotrophic microbes and metabolisms in diffuse, low-temperature venting fluids from Axial Seamount. All the incubations showed microbial uptake of labeled bicarbonate primarily by thermophilic autotrophic that oxidized hydrogen coupled with nitrate reduction. However, the seafloor incubations showed higher abundances of transcripts annotated for aerobic processes, suggesting that oxygen was lost from the hydrothermal fluid samples prior to shipboard analysis. Furthermore, transcripts for thermal stress proteins such as heat shock chaperones and proteases were significantly more abundant in the shipboard incubations, suggesting that depressurization induced thermal stress in the metabolically active microbes in these incubations. Together, the results indicate that while the autotrophic microbial communities in the shipboard and seafloor experiments behaved similarly, there were distinct differences that provide new insight into the activities of natural microbial assemblages under nearly native conditions in the ocean. Diverse microbial communities drive biogeochemical cycles in Earth's ocean, yet studying these organisms and processes is often limited by technological capabilities, especially in the deep ocean. In this study, we used a novel marine microbial incubator instrument capable of experimentation to investigate microbial primary producers at deep-sea hydrothermal vents. We carried out identical stable isotope probing experiments coupled to RNA sequencing both on the seafloor and on the ship to examine thermophilic, microbial autotrophs in venting fluids from an active submarine volcano. Our results indicate that microbial communities were significantly impacted by the effects of depressurization and sample processing delays, with shipboard microbial communities being more stressed than seafloor incubations. Differences in metabolism were also apparent and are likely linked to the chemistry of the fluid at the beginning of the experiment. Microbial experimentation in the natural habitat provides new insights into understanding microbial activities in the ocean.

摘要

减压和样品处理延迟可能会影响从深海采集的样品的船上微生物培养的结果。为了解决这一知识空白,我们开发了一种遥控车辆(ROV)驱动的孵育器仪器,以进行和比较结果,并进行船上 RNA 稳定同位素探测(RNA-SIP)实验,以确定轴向海山漫射,低温通风流体中的关键化学自养微生物和代谢物。所有的孵育都表明微生物主要通过氧化氢与硝酸盐还原偶联的嗜热自养菌吸收标记的碳酸氢盐。然而,海底孵育显示出更多与有氧过程相关的转录物丰度,这表明在船上分析之前,热水流体样品中的氧气已经损失。此外,热应激蛋白如热休克伴侣和蛋白酶的转录物在船上孵育中明显更丰富,这表明在这些孵育中,减压会对代谢活跃的微生物产生热应激。总的来说,结果表明,尽管船上和海底实验中的自养微生物群落表现相似,但存在明显差异,这为在海洋中几乎自然条件下研究自然微生物组合的活动提供了新的见解。多样的微生物群落驱动着地球海洋的生物地球化学循环,但研究这些生物体和过程通常受到技术能力的限制,尤其是在深海中。在这项研究中,我们使用了一种新型的海洋微生物孵育器仪器,能够进行实验,以研究深海热液喷口的微生物初级生产者。我们在海底和船上进行了相同的稳定同位素探测实验,结合 RNA 测序,以检查来自活跃海底火山的通风流体中的嗜热微生物自养生物。我们的结果表明,微生物群落受到减压和样品处理延迟的影响显著,船上微生物群落的压力比海底孵育更大。代谢差异也很明显,可能与实验开始时流体的化学性质有关。在自然栖息地进行微生物实验为理解海洋中微生物的活动提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bbfd/8091007/941758930062/AEM.00078-21-f0007.jpg
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