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海底地壳生物膜生态学

Ecology of Subseafloor Crustal Biofilms.

作者信息

Ramírez Gustavo A, Garber Arkadiy I, Lecoeuvre Aurélien, D'Angelo Timothy, Wheat C Geoffrey, Orcutt Beth N

机构信息

Graduate School of Oceanography, University of Rhode Island, Narragansett, RI, United States.

Division of Biological Sciences, University of Montana, Missoula, MT, United States.

出版信息

Front Microbiol. 2019 Aug 28;10:1983. doi: 10.3389/fmicb.2019.01983. eCollection 2019.

Abstract

The crustal subseafloor is the least explored and largest biome on Earth. Interrogating crustal life is difficult due to habitat inaccessibility, low-biomass and contamination challenges. Subseafloor observatories have facilitated the study of planktonic life in crustal aquifers, however, studies of life in crust-attached biofilms are rare. Here, we investigate biofilms grown on various minerals at different temperatures over 1-6 years at subseafloor observatories in the Eastern Pacific. To mitigate potential sequence contamination, we developed a new bioinformatics tool - . We explore ecological factors driving community structure and potential function of biofilms by comparing our sequence data to previous amplicon and metagenomic surveys of this habitat. We reveal that biofilm community structure is driven by temperature rather than minerology, and that rare planktonic lineages colonize the crustal biofilms. Based on 16S rRNA gene overlap, we partition metagenome assembled genomes into planktonic and biofilm fractions and suggest that there are functional differences between these community types, emphasizing the need to separately examine each to accurately describe subseafloor microbe-rock-fluid processes. Lastly, we report that some rare lineages present in our warm and anoxic study site are also found in cold and oxic crustal fluids in the Mid-Atlantic Ridge, suggesting global crustal biogeography patterns.

摘要

洋壳海底是地球上探索最少且面积最大的生物群落。由于栖息地难以到达、生物量低以及存在污染挑战,对洋壳生物的研究颇具难度。海底观测站促进了对洋壳含水层中浮游生物的研究,然而,对附着在洋壳上的生物膜中的生物研究却很少。在此,我们对东太平洋海底观测站不同温度下在各种矿物质上生长1至6年的生物膜展开研究。为减轻潜在的序列污染,我们开发了一种新的生物信息学工具—— 。通过将我们的序列数据与该栖息地先前的扩增子和宏基因组调查进行比较,我们探索了驱动生物膜群落结构和潜在功能的生态因素。我们发现生物膜群落结构受温度而非矿物学驱动,并且罕见的浮游生物谱系定殖在洋壳生物膜上。基于16S rRNA基因重叠,我们将宏基因组组装基因组划分为浮游生物和生物膜部分,并表明这些群落类型之间存在功能差异,强调需要分别对每种类型进行研究以准确描述海底微生物 - 岩石 - 流体过程。最后,我们报告在我们温暖且缺氧的研究地点存在的一些罕见谱系,在大西洋中脊寒冷且有氧的洋壳流体中也有发现,这表明存在全球洋壳生物地理学模式。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9b1a/6736579/701c888cd976/fmicb-10-01983-g001.jpg

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