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首页> 外文期刊>Palaeontographica, Abteilung A. Palaozoologie-Stratigraphie >Microorganisms associated with the seed fern Lyginopteris oldbamia (Binney) H. Potonié (Lyginopteridales) from the Carboniferous of Great Britain
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Microorganisms associated with the seed fern Lyginopteris oldbamia (Binney) H. Potonié (Lyginopteridales) from the Carboniferous of Great Britain

机译:与英国石炭纪种子蕨Lyginopteris oldbamia(Binney)H.Potonié(Lyginopteridales)相关的微生物

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摘要

Several types of microbial filaments and isolated reproductive units occur in structurally preserved Lyginopteris oldbamia stems and pinna axes from the Lower Coal Measures (Lower Pennsylvanian) of Great Britain. One common type of filament is narrow, tubular, and forms clusters or coils in host cells, while another type is wide and characterized by irregular swellings. Reproductive units are mostly spheroid, but differ from one another in size and wall thickness. This assemblage probably represents a community of saprotrophs. Concentrations of microbial filaments around the cortical sclerotic bars of the pinna axes and in the stalks of multicellular glands may suggest that these structures served as sites of entry into the plant. Although the systematic affinities of the microbial remains in L. oldbamia cannot be precisely determined, their discovery contributes to a more comprehensive understanding of the diversity and biological roles of microorganisms in Carboniferous continental ecosystems.
机译:几种微生物细丝和分离的生殖单位出现在英国下层煤系(宾夕法尼亚州下层)的结构保存的Lyginopteris oldbamia茎和pinna轴上。一种常见的细丝是窄的,管状的,并在宿主细胞中形成簇或线圈,而另一种细的丝是宽的,并且具有不规则的溶胀。生殖单位大多为球状,但大小和壁厚互不相同。这种组合可能代表着腐臭菌的群落。耳廓轴皮层硬化条周围以及多细胞腺茎中的微生物细丝集中可能表明这些结构可作为进入植物的位点。尽管无法精确确定旧巴氏杆菌中微生物的系统亲和力,但它们的发现有助于人们更全面地了解石炭纪大陆性生态系统中微生物的多样性和生物学作用。

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