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Detection and Identification of the Latent Microorganisms in the Altered Layers of Ancient Bronze Mirrors

机译:古铜镜蚀变层中潜在微生物的检测与鉴定

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We obtained ancient bronze mirrors and carried out: scanning electron microscopy (SEM) of fractured altered layers; biologic microscopic observation of Gram-stained samples; and DNA analyses of samples removed from altered sites. Fine particles about 2 mu m in length were confirmed in the altered layer by SEM. Microorganisms of identical size were observed in the Gram-stained sample removed from the altered layer through a biologic microscope. Fine particles observed under SEM were considered to be microorganisms. Many fine particles were confirmed, particularly in the altered sites, by SEM. Certain types of microorganisms may have played a part in the alteration (deterioration) of the ancient bronze mirrors while the latter were buried in soil. From the base sequences obtained by DGGE analysis, two types of microorganisms were present in the altered layer of the mirror. One was 94.7 percent homologous to the 16S rDNA of the uncultured bacterium (accession number: AY 053488). It was also highly homologous to the sequence derived from the 16S rDNA of the Xanthomonadaceae family (e.g., Stenotrophomonas, Xanthomona). That is, the sequence was derived from a strain belonging to the Xanthomonadaceae family. The other base sequence was 97.4 percent homologous to the 16S rDNA of the Bacteroidales order such as uncultured Bacteroidales bacterium (accession number: AY 859647). That is, the sequence was derived from a strain belonging to the Bacteroidales order. Genes of microorganisms, presumed to belong to the Acetobacter and Gluconacetobacter genera and the Fe(III)-reducing bacterium, Shewanella algae, were detected from base sequence analysis by cloning. Microbial activity around the mirrors was assumed to be high. The alteration containing corrosion mechanism of bronze mirrors appears complex, but several types of microbes that possibly altered the bronze mirrors were verified.
机译:我们获得了古铜镜,并进行了:断裂蚀变层的扫描电子显微镜(SEM);革兰氏染色样品的生物学显微镜观察;以及从改变的位点取出的样品的DNA分析。通过扫描电镜在蚀变层中确认了约2μm长的细颗粒。通过生物显微镜从蚀变层中取出的革兰氏染色样品中观察到大小相同的微生物。在SEM下观察到的细颗粒被认为是微生物。通过SEM确认了许多细颗粒,特别是在改变的部位。某些类型的微生物可能在古代铜镜被埋在土壤中的变化(退化)中发挥了作用。根据通过DGGE分析获得的碱基序列,在镜面的变化层中存在两种类型的微生物。一种是与未培养细菌的16S rDNA同源的94.7%(登录号:AY 053488)。它也与源自黄单胞菌科的16S rDNA的序列(例如,嗜单胞菌,黄单胞菌)高度同源。即,该序列衍生自属于黄单胞菌科的菌株。另一个碱基序列与拟杆菌属(例如未培养的拟杆菌属细菌)的16S rDNA具有97.4%的同源性(登录号:AY 859647)。即,该序列衍生自属于拟杆菌科的菌株。通过克隆从碱基序列分析中检测到了推测为属于醋杆菌属和葡糖杆菌属以及减少Fe(III)的细菌希瓦氏菌属的微生物的基因。镜子周围的微生物活动被认为是很高的。包含铜镜的腐蚀机理的蚀变看起来很复杂,但已验证了可能改变铜镜的几种微生物。

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