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一株岩石放线菌对碳酸钙形貌的影响北大核心CSCD
引用本文:褚玥,曹成亮,连宾. 一株岩石放线菌对碳酸钙形貌的影响北大核心CSCD[J]. 微生物学报, 2016, 56(7): 1123-1131
作者姓名:褚玥  曹成亮  连宾
作者单位:南京师范大学生命科学学院, 江苏省功能微生物与功能基因组学重点实验室, 江苏省微生物工程技术研究中心, 江苏 南京 210023,中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵州 贵阳 550001,南京师范大学生命科学学院, 江苏省功能微生物与功能基因组学重点实验室, 江苏省微生物工程技术研究中心, 江苏 南京 210023
基金项目:国家自然科学基金(41373078);国家重大科学研究计划(2013CB956702);江苏高校优势学科建设工程(PAPD)
摘    要:【目的】微生物诱导成矿是近年来地质微生物学领域研究中的热点之一。采用一株分离自喀斯特地区的岩生放线菌DHS C013^T菌株,研究该菌株及其代谢产物在由NaHCO3、Ca(NO3)2.4H2O组成的成矿体系中对CaCO3生成及形貌的影响。【方法】将在葡萄糖麦芽酵母提取物(MGYP)培养液中培养的放线菌上清液、菌丝球、发酵液以及无菌的MGYP培养液和超纯水分别加入成矿体系,SEM观察不同处理成矿体系中的底部沉淀物。【结果】在超纯水成矿体系中只形成标准菱面体方解石,而在添加放线菌及其代谢产物甚至含有机质的培养液则可形成形态各异的CaCO3晶体,如球形、哑铃以及表面具有鳞片状的柱形。这些特殊形态的CaCO3晶体的形成,可能是在放线菌的菌丝球和菌丝片段以及胞外分泌物上成核和逐渐生长的结果。【结论】放线菌菌丝体及代谢产物对调控和影响CaCO3的晶体形貌有重要作用。研究结果对进一步认识放线菌及其代谢产物诱导生物成矿提供了新的证据。

关 键 词:岩生放线菌  成矿体系  CaCO3
收稿时间:2015-09-28
修稿时间:2015-12-09

Effect on calcium carbonate morphology by a strain of rock actinomycete
Yue Chu,Chengliang Cao and Bin Lian. Effect on calcium carbonate morphology by a strain of rock actinomycete[J]. Acta microbiologica Sinica, 2016, 56(7): 1123-1131
Authors:Yue Chu  Chengliang Cao  Bin Lian
Affiliation:Jiangsu Key Laboratory of Microbes and Functional Genomics, Jiangsu Engineering and Technology Research Center for Microbiology, College of Life Science, Nanjing Normal University, Nanjing 210023, Jiangsu Province, China,State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550001, Guizhou Province, China and Jiangsu Key Laboratory of Microbes and Functional Genomics, Jiangsu Engineering and Technology Research Center for Microbiology, College of Life Science, Nanjing Normal University, Nanjing 210023, Jiangsu Province, China
Abstract:[Objective] Microbes-induced mineralization is one of the hottest issues in the field of geomicrobiology. Strain DHS C013T isolated from the surfaces of rocks in the Karst region was used to investigate microbial influence on the formation of carbonate and its morphology in the metallogenic system consisting NaHCO3 and Ca(NO3)2·4H2O. [Methods] Strain DHS C013T was inoculated into malt extract-glucose-yeast extract peptone (MGYP) liquid medium. After cultivation we put the fermented solution, supernatant, hypha pellets, sterile MGYP liquid medium and ultrapure water into the metallogenic system separately. Scanning electronic microscope was applied to observe the crystals at the bottom of the petri dishes. [Results] In the metallogenic system with ultrapure water, only standard calcite of rhombohedron was found. However, special morphology of CaCO3, such as dumbbelllike, spherulite and scaly cylindrical shapes, were found in the metallogenic system with actinomycetes, hyphae fragment and their cell metabolism products. These calcium carbonates of special morphology might be resulted from their nucleation on smaller hypha pellets, hyphae fragment or extracellular secretion. [Conclusion] Actinomycetes can induce the formation of CaCO3, and the mycelium and metabolites have important effects on regulating and influencing CaCO3 morphology. Our data provide new evidence for further understanding of the biological mineralization mediated by actinomycete and its metabolic products.
Keywords:actinomycete  metallogenic system  CaCO3
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