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东地中海深海沉积物微生物群落的比较

Comparison of deep-sea sediment microbial communities in the Eastern Mediterranean.

作者信息

Heijs Sander K, Laverman Anniet M, Forney Larry J, Hardoim Pablo R, van Elsas Jan Dirk

机构信息

Department of Microbial Ecology, Center for Ecological and Evolutionary Studies, University of Groningen, AA Haren, The Netherlands.

出版信息

FEMS Microbiol Ecol. 2008 Jun;64(3):362-77. doi: 10.1111/j.1574-6941.2008.00463.x. Epub 2008 Apr 14.

Abstract

Bacterial and archaeal communities in sediments obtained from three geographically-distant mud volcanoes, a control site and a microbial mat in the Eastern Mediterranean deep-sea were characterized using direct 16S rRNA gene analyses. The data were thus in relation to the chemical characteristics of the (stratified) habitats to infer community structure-habitat relationships. The bacterial sequences in the different habitats were related to those of Actinobacteria, Bacilli, Chloroflexi, Alpha-, Beta-, Gamma-, Delta- and Epsilonproteobacteria and unclassified bacteria, including the JS1 group. The archaeal sequences found were affiliated with those of the Methanosarcinales, Thermoplasmales, Halobacteriales and Crenarchaea belonging to marine benthic group I and B, as well as MCG group archaea. In each sample, the communities were diverse and unique at the phylotype level. However, at higher taxonomic levels, similar groups were found in different sediments, and similar depth layers tended to contain similar communities. The sequences that dominated in all top layers (as well as in the mat) probably represented organisms involved in aerobic heterotrophy, sulfide-based chemoautotrophy and methanotrophy and/or methylotrophy. Sequences of organisms most likely involved in anaerobic methane oxidation, sulfate reduction and anaerobic heterotrophy were predominantly found in deeper layers. The data supported the notion of (1) uniqueness of each habitat at fine taxonomic levels, (2) stratification in depth and (3) conservation of function in the sediments.

摘要

利用直接16S rRNA基因分析方法,对从地中海东部深海的三个地理位置遥远的泥火山、一个对照站点及一个微生物垫采集的沉积物中的细菌和古菌群落进行了特征描述。这些数据与(分层的)栖息地的化学特征相关,以推断群落结构与栖息地的关系。不同栖息地中的细菌序列与放线菌、芽孢杆菌、绿弯菌、α-、β-、γ-、δ-和ε-变形菌以及未分类细菌(包括JS1组)的序列相关。发现的古菌序列与甲烷八叠球菌目、嗜热质体目、盐杆菌目以及属于海洋底栖生物第一组和B组的泉古菌以及MCG组古菌的序列相关。在每个样本中,群落类型水平上是多样且独特的。然而,在较高分类水平上,不同沉积物中发现了相似的类群,并且相似的深度层往往包含相似的群落。在所有表层(以及微生物垫)中占主导地位的序列可能代表参与好氧异养、基于硫化物的化学自养以及甲烷氧化和/或甲基营养的生物体。最有可能参与厌氧甲烷氧化、硫酸盐还原和厌氧异养的生物体序列主要在较深层中发现。这些数据支持了以下观点:(1)每个栖息地在精细分类水平上的独特性;(2)深度分层;(3)沉积物中功能的保守性。

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