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Magnetosome-containing bacteria living as symbionts of bivalves

机译:作为双壳类共生体的含磁小体的细菌

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Bacteria containing magnetosomes (protein-bound nanoparticles of magnetite or greigite) are common to many sedimentary habitats, but have never been found before to live within another organism. Here, we show that octahedral inclusions in the extracellular symbionts of the marine bivalve Thyasira cf. gouldi contain iron, can exhibit magnetic contrast and are most likely magnetosomes. Based on 16S rRNA sequence analysis, T. cf. gouldi symbionts group with symbiotic and free-living sulfur-oxidizing, chemolithoautotrophic gammaproteobacteria, including the symbionts of other thyasirids. T. cf. gouldi symbionts occur both among the microvilli of gill epithelial cells and in sediments surrounding the bivalves, and are therefore facultative. We propose that free-living T. cf. gouldi symbionts use magnetotaxis as a means of locating the oxic-anoxic interface, an optimal microhabitat for chemolithoautotrophy. T. cf. gouldi could acquire their symbionts from near-burrow sediments (where oxic-anoxic interfaces likely develop due to the host's bioirrigating behavior) using their superextensile feet, which could transfer symbionts to gill surfaces upon retraction into the mantle cavity. Once associated with their host, however, symbionts need not maintain structures for magnetotaxis as the host makes oxygen and reduced sulfur available via bioirrigation and sulfur-mining behaviors. Indeed, we show that within the host, symbionts lose the integrity of their magnetosome chain (and possibly their flagellum). Symbionts are eventually endocytosed and digested in host epithelial cells, and magnetosomes accumulate in host cytoplasm. Both host and symbiont behaviors appear important to symbiosis establishment in thyasirids.
机译:含细菌的磁小体(与磁铁矿或钙铁矿结合的蛋白质纳米颗粒)在许多沉积生物中很常见,但从未发现存在于另一生物体内。在这里,我们显示八面体包含在海洋双壳类Thyasira cf.的细胞外共生体中。 gouldi含有铁,可以显示出磁性对比,并且很可能是磁小体。基于16S rRNA序列分析,T。古迪(Gouldi)共生菌群具有共生和自由生存的硫氧化性,化学自养型γ-变形杆菌,包括其他胸腺类共生菌。 T.比照古尔迪共生体同时存在于g上皮细胞的微绒毛和双壳类动物周围的沉积物中,因此是兼性的。我们建议自由生活T。古尔迪共生体利用趋磁性定位有氧-缺氧界面,这是化石自养的最佳微生境。 T.比照古尔迪可以用它们的超伸脚从附近的洞穴沉积物中获得共生体(由于宿主的生物灌溉行为而可能产生有氧-缺氧的界面),这可能会使共生体缩回地幔腔后将其转移到g表面。一旦与它们的宿主结合,共生体就不需要维持趋磁结构,因为宿主通过生物灌溉和硫磺开采行为使氧气和还原的硫可利用。确实,我们表明,在宿主体内,共生体失去了它们的磁小体链(可能还有鞭毛)的完整性。共生体最终在宿主上皮细胞中被内吞和消化,并且磁小体在宿主细胞质中积累。宿主和共生体的行为都对共生关系起着重要的作用。

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