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宏转录组分析揭示了冲积含水层生物地球化学热点中出人意料的多样微生物代谢。

Metatranscriptomic Analysis Reveals Unexpectedly Diverse Microbial Metabolism in a Biogeochemical Hot Spot in an Alluvial Aquifer.

作者信息

Jewell Talia N M, Karaoz Ulas, Bill Markus, Chakraborty Romy, Brodie Eoin L, Williams Kenneth H, Beller Harry R

机构信息

Earth and Environmental Sciences, Lawrence Berkeley National Laboratory Berkeley, CA, USA.

出版信息

Front Microbiol. 2017 Jan 25;8:40. doi: 10.3389/fmicb.2017.00040. eCollection 2017.

Abstract

Organic matter deposits in alluvial aquifers have been shown to result in the formation of naturally reduced zones (NRZs), which can modulate aquifer redox status and influence the speciation and mobility of metals, affecting groundwater geochemistry. In this study, we sought to better understand how natural organic matter fuels microbial communities within anoxic biogeochemical hot spots (NRZs) in a shallow alluvial aquifer at the Rifle (CO) site. We conducted a 20-day microcosm experiment in which NRZ sediments, which were enriched in buried woody plant material, served as the sole source of electron donors and microorganisms. The microcosms were constructed and incubated under anaerobic conditions in serum bottles with an initial N headspace and were sampled every 5 days for metagenome and metatranscriptome profiles in combination with biogeochemical measurements. Biogeochemical data indicated that the decomposition of native organic matter occurred in different phases, beginning with mineralization of dissolved organic matter (DOM) to CO during the first week of incubation, followed by a pulse of acetogenesis that dominated carbon flux after 2 weeks. A pulse of methanogenesis co-occurred with acetogenesis, but only accounted for a small fraction of carbon flux. The depletion of DOM over time was strongly correlated with increases in expression of many genes associated with heterotrophy (e.g., amino acid, fatty acid, and carbohydrate metabolism) belonging to a strain that accounted for a relatively large percentage (~8%) of the metatranscriptome. This strain also expressed genes indicative of chemolithoautotrophy, including CO fixation, H oxidation, S-compound oxidation, and denitrification. The pulse of acetogenesis appears to have been collectively catalyzed by a number of different organisms and metabolisms, most prominently pyruvate:ferredoxin oxidoreductase. Unexpected genes were identified among the most highly expressed (>98th percentile) transcripts, including acetone carboxylase and cell-wall-associated hydrolases with unknown substrates (numerous lesser expressed cell-wall-associated hydrolases targeted peptidoglycan). Many of the most highly expressed hydrolases belonged to a . Bathyarchaeota strain and may have been associated with recycling of bacterial biomass. Overall, these results highlight the complex nature of organic matter transformation in NRZs and the microbial metabolic pathways that interact to mediate redox status and elemental cycling.

摘要

冲积含水层中的有机物沉积已被证明会导致天然还原带(NRZs)的形成,这会调节含水层的氧化还原状态,并影响金属的形态和迁移性,进而影响地下水地球化学。在本研究中,我们试图更好地了解天然有机物如何为科罗拉多州莱夫尔(Rifle)地区浅层冲积含水层中缺氧生物地球化学热点区域(NRZs)内的微生物群落提供能量。我们进行了一项为期20天的微观实验,其中富含埋藏木本植物材料的NRZ沉积物作为电子供体和微生物的唯一来源。微观实验在血清瓶中于厌氧条件下构建和培养,初始顶空为氮气,每5天取样一次,用于宏基因组和宏转录组分析,并结合生物地球化学测量。生物地球化学数据表明,天然有机物的分解分不同阶段进行,在培养的第一周开始于溶解有机物(DOM)矿化生成二氧化碳,随后在2周后出现占主导地位的产乙酸脉冲,主导了碳通量。产甲烷脉冲与产乙酸同时发生,但仅占碳通量的一小部分。随着时间的推移,DOM的消耗与许多与异养相关基因(如氨基酸、脂肪酸和碳水化合物代谢)的表达增加密切相关,这些基因属于一个在宏转录组中占比较大(约8%)的菌株。该菌株还表达了指示化学无机自养的基因,包括二氧化碳固定、氢气氧化、硫化合物氧化和反硝化作用。产乙酸脉冲似乎是由多种不同的生物体和代谢共同催化的,最显著的是丙酮酸:铁氧化还原蛋白氧化还原酶。在表达量最高(>第98百分位数)的转录本中鉴定出了一些意想不到的基因,包括丙酮羧化酶和底物未知的细胞壁相关水解酶(许多表达量较低的细胞壁相关水解酶靶向肽聚糖)。许多表达量最高的水解酶属于一个深古菌门菌株,可能与细菌生物量的循环利用有关。总体而言,这些结果突出了NRZs中有机物转化的复杂性以及相互作用以介导氧化还原状态和元素循环的微生物代谢途径。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/747d/5264521/986e34528486/fmicb-08-00040-g0001.jpg

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