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跨粒度、深度和氧浓度的定量微生物分类学。

Quantitative microbial taxonomy across particle size, depth, and oxygen concentration.

作者信息

Huanca-Valenzuela Paulina, Fuchsman Clara A, Tully Benjamin J, Sylvan Jason B, Cram Jacob A

机构信息

University of Maryland Center for Environmental Science Horn Point Laboratory, Cambridge, MD, United States.

Center for Dark Energy Biosphere Investigations, University of Southern California, Los Angeles, CA, United States.

出版信息

Front Microbiol. 2025 May 23;16:1552305. doi: 10.3389/fmicb.2025.1552305. eCollection 2025.

Abstract

INTRODUCTION

Marine particles form in the ocean surface sink through the water column into the deep ocean, sequestering carbon. Microorganisms inhabit and consume carbon in these particles. The East Pacific Rise (EPR) harbors both an Oxygen Deficient Zone (ODZ) and a non-buoyant plume region formed from hydrothermal vents located on the ocean floor, allowing us to explore relationships between microbial community and particle size between a range of environments.

METHODS

In this study, we quantified microbial diversity using a fractionation method that separated particles into seven fine scale fractions (0.2-1.2, 1.2-5, 5-20, 20-53, 53-180,180-500, >500 μm), and included a spike-in standard for sequencing the 16S rRNA gene. Size fractionated organic carbon into the same fractions enabled the calculation of bacterial 16S rRNA copies per μg C and per liter.

RESULTS

There was a large increase in the bacterial 16S rRNA copies/ug C and copies/L on particles >180 μm between the upper water column and the deep water column. Though the total concentration of organic C in particles decreased in the deep water column, the density of bacteria on large particles increased at depth. The microbial community varied statistically significantly as a function of particle size and depth. Quantitative abundance estimates found that ostensibly obligate free-living microbes, such as SAR11 and Thaumarcheota, were more abundant in the free-living fraction but also common and abundant in the particulate size fractions. Conversely, ostensibly obligate particle attached bacteria such as members of Bacteroidetes and Planctomycetes, while most abundant on particles, were also present in the free living fraction. Total bacterial abundance, and the abundance of many taxonomic groups, increased in the ODZ region, particularly in the free-living fraction. Contrastingly, in the non-buoyant plume, there were highly abundant bacteria in the 5-20 and 20-53 μm fractions but reduced bacteria present in the 53-180 and 180-500 μm fractions.

CONCLUSION

Quantitative examination of microbial communities highlights the distribution of microbial taxa unburdened by compositional effects. These data are congruent with existing models which suggest high levels of exchange between particle-attached and free-living communities.

摘要

引言

海洋颗粒在海洋表层形成,通过水柱沉入深海,从而封存碳。微生物栖息于这些颗粒中并消耗其中的碳。东太平洋海隆(EPR)既有缺氧区(ODZ),又有由位于海底的热液喷口形成的非浮力羽状流区域,这使我们能够探索一系列环境中微生物群落与颗粒大小之间的关系。

方法

在本研究中,我们使用一种分级方法对微生物多样性进行了量化,该方法将颗粒分离为七个精细尺度的级分(0.2 - 1.2、1.2 - 5、5 - 20、20 - 53、53 - 180、180 - 500、>500 μm),并纳入了用于对16S rRNA基因进行测序的加标标准。将有机碳按相同级分进行分级,从而能够计算每微克碳和每升中的细菌16S rRNA拷贝数。

结果

在上层水柱和深水柱之间,>180 μm颗粒上的细菌16S rRNA拷贝数/微克碳和拷贝数/升大幅增加。尽管深水柱中颗粒有机碳的总浓度有所下降,但大颗粒上细菌的密度在深度上增加了。微生物群落随颗粒大小和深度的变化在统计学上有显著差异。定量丰度估计发现,表面上专性自由生活的微生物,如SAR11和奇古菌门,在自由生活级分中更为丰富,但在颗粒大小级分中也常见且丰富。相反,表面上专性附着于颗粒的细菌,如拟杆菌门和浮霉菌门的成员,虽然在颗粒上最为丰富,但在自由生活级分中也存在。总细菌丰度以及许多分类群的丰度在缺氧区增加,特别是在自由生活级分中。相比之下,在非浮力羽状流中,5 - 20和20 - 53 μm级分中有大量细菌,但53 - 180和180 - 500 μm级分中的细菌数量减少。

结论

对微生物群落的定量研究突出了不受组成效应影响的微生物分类群的分布。这些数据与现有模型一致,这些模型表明附着于颗粒的群落和自由生活的群落之间存在高水平的交换。

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