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海洋沉积物中微生物的预测分泌组及其靶向底物。

Predicted microbial secretomes and their target substrates in marine sediment.

机构信息

Department of Earth and Environmental Sciences, Paleontology & Geobiology, Ludwig-Maximilians-Universität München, 80333, Munich, Germany.

GeoBio-CenterLMU, Ludwig-Maximilians-Universität München, 80333, Munich, Germany.

出版信息

Nat Microbiol. 2018 Jan;3(1):32-37. doi: 10.1038/s41564-017-0047-9. Epub 2017 Oct 23.

Abstract

Scientific drilling has identified a biosphere in marine sediments , which contain many uncultivated microbial groups known only by their DNA sequences . Recycling of organic matter in sediments is an important component of biogeochemical cycles because marine sediments are critical for long-term carbon storage . Turnover of carbon is hypothesized to be driven by the secretion of enzymes by microbial organisms , which act to break down macromolecules into constitutive monomers that can be transported into cells. As such, the nature of the microbial secretome often influences the function of a community . However, the microbial groups involved in this process and the biochemistry they encode is poorly understood. Here, we show that expressed genes from 5 to 159 meters below the seafloor (mbsf) encode numerous candidate peptidases and carbohydrate-active enzymes ('CAZymes') targeted for secretion. The majority (90-99%) were assigned to Bacteria, of which 12% shared the highest sequence similarity with candidate phyla . The remaining putatively secreted proteins shared highest sequence similarity with archaeal and fungal enzymes, which peak in two redox transition zones . In the shallower redox zone at 30 mbsf, 20% of the transcripts encoding putative secreted peptidases were assigned to lineages of uncultivated Archaea. The target compounds of the predicted secreted proteome show a preference for necromass in the form of microbial cell envelopes as well as plankton and algal detritus. The predicted fungal secreted proteome encodes CAZymes not present in the predicted bacterial or archaeal secreted proteomes, indicating that fungi putatively play a minimal but specialized role in subseafloor carbohydrate recycling.

摘要

科学钻探在海洋沉积物中发现了一个生物圈,其中包含许多仅通过其 DNA 序列可知的未培养微生物群体。沉积物中有机物的再循环是生物地球化学循环的一个重要组成部分,因为海洋沉积物对于长期碳储存至关重要。碳的周转被假设是由微生物生物体分泌的酶驱动的,这些酶作用于将大分子分解为组成单体,这些单体可以被运输到细胞中。因此,微生物分泌组的性质通常会影响群落的功能。然而,参与这个过程的微生物群体及其编码的生物化学物质还知之甚少。在这里,我们表明,从海底以下 5 到 159 米(mbsf)处的表达基因编码了许多候选肽酶和碳水化合物活性酶(“CAZymes”),这些酶被靶向分泌。大多数(90-99%)被分配给细菌,其中 12%与候选门具有最高的序列相似性。其余假定分泌的蛋白质与古菌和真菌酶具有最高的序列相似性,这些酶在两个氧化还原过渡区达到峰值。在较浅的氧化还原区(30 mbsf),编码假定分泌肽酶的转录本中有 20%被分配给未培养古菌的谱系。预测分泌蛋白质组的靶化合物优先选择以微生物细胞包膜形式存在的腐殖质,以及浮游生物和藻类碎屑。预测的真菌分泌蛋白质组编码了预测的细菌或古菌分泌蛋白质组中不存在的 CAZymes,这表明真菌在海底碳水化合物再循环中可能发挥着最小但专业化的作用。

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