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现代分子生物学技术为蓝藻的生物多样性研究提供了更多信息和证据.单细胞蓝藻——双囊藻属（Geminocystis）是2009年从集胞藻（Synechocystis）分离出来的新属.2017年5月从青海湖的封闭子湖——月牙湖采集分离到一株单细胞蓝藻藻株，16S rRNA基因序列显示此藻株和双囊藻的藻种显示出最高的相似性，都在97%以上，并且在分子系统树聚为一束.此株的细胞结构以及超微结构显示，细胞纵轴具有窝式结构以及类囊体不规则的排列等双囊藻属所具有的特征.双囊藻是我国蓝藻的新报道纪录属，本研究还对双囊藻的分类和生态进行了讨论. 相似文献
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微生物岩的原始定义指底栖微生物主导形成的沉积体或岩石体。笔者对该概念进行了扩充,认为微生物岩除了包括叠层石、凝块石、纹层石、核形石、均一石之外,还应该包括微生物骨架岩、微生物粘结岩、非钙化浮游或漂浮微生物形成的模铸岩、矿化浮游或漂浮微生物形成的颗粒岩和泥粒岩。P-T界线地层微生物岩的特征是具有由较粗矿物晶体(主要是方解石,其次是白云石)组成的斑点状、树枝状、网状结构的灰岩。这3种结构分别称为斑点状体、树枝状体、网状体,在露头上呈暗色,在薄片中呈浅色,一般由无定形的亮晶充填体和其间的微亮晶组成。亮晶充填体是指无定形的孔洞被不同成岩期形成的矿物充填形成的结构体,因成岩作用各异,造成不同层位、不同地点的亮晶充填体内部的矿物类型和充填顺序存在差异;所有的亮晶充填体都不具有壁,故不是钙化化石。通过形态、大小和生态比较,以及形成演化分析,认为亮晶充填体的前身是漂浮蓝细菌微囊菌,胶鞘是微囊菌形成模铸化石的关键因素。亮晶充填体是表层水漂浮生活的微囊菌沉入海底后,被泥晶沉积物掩埋或者被早期海底胶结物胶结,在泥晶沉积物半固结或固结之后腐烂留下的孔洞被后期成岩作用形成的矿物充填形成的。P-T界线地层微生物岩段顶部遭受成岩作用程度高,树枝状体和网状体中的亮晶充填体的轮廓基本都被破坏,变成微亮晶和亮晶,以前被学者解释为凝块石;但斑点状体、树枝状体、网状体是成岩流体沿着亮晶充填体或其他化石丰富的地方运移形成较粗的晶体而造成的,并不符合凝块石的定义。同时,少数学者把树枝状体本身当成底栖生物,也是没有充分认识树枝状体的矿物组成而做的解释。该微生物岩段含有钙化的小球状化石和同心层状化石,但它们不是组成微生物岩的主体。 相似文献
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微生物岩的原始定义指底栖微生物主导形成的沉积体或岩石体。笔者对该概念进行了扩充,认为微生物岩除了包括叠层石、凝块石、纹层石、核形石、均一石之外,还应该包括微生物骨架岩、微生物粘结岩、非钙化浮游或漂浮微生物形成的模铸岩、矿化浮游或漂浮微生物形成的颗粒岩和泥粒岩。P-T界线地层微生物岩的特征是具有由较粗矿物晶体(主要是方解石,其次是白云石)组成的斑点状、树枝状、网状结构的灰岩。这3种结构分别称为斑点状体、树枝状体、网状体,在露头上呈暗色,在薄片中呈浅色,一般由无定形的亮晶充填体和其间的微亮晶组成。亮晶充填体是指无定形的孔洞被不同成岩期形成的矿物充填形成的结构体,因成岩作用各异,造成不同层位、不同地点的亮晶充填体内部的矿物类型和充填顺序存在差异;所有的亮晶充填体都不具有壁,故不是钙化化石。通过形态、大小和生态比较,以及形成演化分析,认为亮晶充填体的前身是漂浮蓝细菌微囊菌,胶鞘是微囊菌形成模铸化石的关键因素。亮晶充填体是表层水漂浮生活的微囊菌沉入海底后,被泥晶沉积物掩埋或者被早期海底胶结物胶结,在泥晶沉积物半固结或固结之后腐烂留下的孔洞被后期成岩作用形成的矿物充填形成的。P-T界线地层微生物岩段顶部遭受成岩作用程度高,树枝状体和网状体中的亮晶充填体的轮廓基本都被破坏,变成微亮晶和亮晶,以前被学者解释为凝块石;但斑点状体、树枝状体、网状体是成岩流体沿着亮晶充填体或其他化石丰富的地方运移形成较粗的晶体而造成的,并不符合凝块石的定义。同时,少数学者把树枝状体本身当成底栖生物,也是没有充分认识树枝状体的矿物组成而做的解释。该微生物岩段含有钙化的小球状化石和同心层状化石,但它们不是组成微生物岩的主体。 相似文献
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Species in the cyanobacterial genus Merismopedia are present in freshwaters at different trophic levels, with some species even as the components of cyanobacterial blooms. However, species diversity in this genus was not fully verified by molecular investigation and polyphasic taxonomic studies. In this study, Merismopedia-like strain tenuissima CHAB 7021 was isolated from Ganjiang River in Jiangxi Province, China, and polyphasic characterization of this strain was performed by morphological observation, ultrastructural examination, chemical detection of pigments and phylogenetic analysis based on 16 S rRNA gene sequences. Morphological identification of the strain was supported by the ultrastructural features, as the tiny species Merismopedia tenuissima Lemmermann. The phylogeny based on 16 S rRNA gene sequences revealed at least three clades formed by the strains of Merismopedia. The three M. tenuissima strains including M. tenuissima CHAB 7021 was gathered in clade III with distant relationship to the clade I formed by the six Merismopedia strains including the type species M. punctata, and such a genetic distance may propose Merismopedia tenuissima to separate from Merismopedia genus. However intermixture relationship in between strains of M. punctate and M. glauca in the phylogenetic tree still complicated the taxonomic status in the genus Merismopedia. The process for taxonomic revision in the Merismopedia genus still await for examination and further information on more strains of type species M. punctata. 相似文献
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以前的微生物岩识别和分类只根据裸眼可见的中观结构,而对显微镜下的微观结构未予使用。微生物的显微结构有什么基本特征,是否可以用于微生物岩的识别和分类是本文关注的焦点。作者从微生物岩形成机制和实际材料的观察来探讨这个问题。在诱导钙化实验中观察到,蓝藻鞘丝藻Lyngbya的胶鞘表面有碳酸盐矿物形成: 先是在胶鞘表面形成点状碳酸盐颗粒,后来碳酸盐几乎包裹整个丝体,形成一个矿物壳。微生物岩形成的模式推演表明,微生物岩一般都有微生物留下的孔(模孔)和包围模孔的矿物壳2种基本单元。对3个地点的现代微生物碳酸盐岩和1个地点的古代(寒武纪)微生物岩的观察,发现在显微尺度上都具有模孔,此外还可能有矿物壳或胶结物。模孔的形状、大小、排列方式是微生物碳酸盐岩显微结构研究的核心内容,在今后的研究中可以用于微生物岩的识别和分类,以及作为分析形成机制和形成环境的基础。 相似文献
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The morphological and molecular detection for the presence of toxic Cylindrospermopsis(Nostocales,Cyanobacteria) in Beijing city,China 总被引：1，自引：0，他引：1
Cylindrospermopsis raciborskii and its highly similar relatives R aphidiopsis species have been recognized as globally invasive and expansive filamentous cyanobacteria causing water blooms. Reports on C. raciborskii/Raphidiopsis species and their harmful metabolites such as hepatotoxic cylindrospermopsins(CYNs) in Chinese waters have been increasing, but mostly restricted to the southern regions of China. To further explore the existence and distribution of C. raciborskii in China, six water samples from Beijing city were morphologically and molecularly examined. Five samples of the six were shown to have C ylindrospermopsis filaments with straight and spiral morphotypes. PCR detection targeting on Cylindrospermopsis/Raphidiopsis specific 16 S r RNA gene region also showed the positive amplification, and such amplifications were confirmed by sequencing and phylogenetic analysis. As well, three of the five Cylindrospermopsis containing samples were shown to have c yr J — a gene of CYN synthesis gene cluster. The results represented the presence of toxic C ylindrospermopsis at the most northern line in China so far, indicating rapid expansion of this harmful invasive cyanobacterium. It is strongly suggested that the monitoring on C. raciborskii/R aphidiopsis species and their production of cylindrospermopsin should be emphasized in Beijing and even more northern parts of China. 相似文献
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