Department of Biology, Memorial University of Newfoundland, St John's, Newfoundland A1B 3X9, Canada.
Department of Physics and Physical Oceanography, Memorial University of Newfoundland, St John's, Newfoundland A1B 3X7, Canada.
ISME J. 2014 Dec;8(12):2453-62. doi: 10.1038/ismej.2014.93. Epub 2014 Jun 10.
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.
含有磁小体(磁铁矿或硫铁矿的蛋白结合纳米颗粒)的细菌在许多沉积栖息地中很常见,但以前从未在其他生物体中发现过。在这里,我们表明,海洋双壳类 Thyasira cf. gouldi 的细胞外共生体中的八面体内含物含有铁,可表现出磁对比,并且很可能是磁小体。基于 16S rRNA 序列分析,T. cf. gouldi 共生体与共生和自由生活的硫氧化、化能自养γ变形菌聚在一起,包括其他 thyasirids 的共生体。T. cf. gouldi 共生体既存在于鳃上皮细胞的微绒毛之间,也存在于贝类周围的沉积物中,因此是兼性的。我们提出,自由生活的 T. cf. gouldi 共生体可能利用趋磁性作为定位好氧-缺氧界面的一种手段,这是化能自养的最佳小生境。T. cf. gouldi 可以利用其超长的脚从近洞沉积物(由于宿主的生物灌溉行为,可能在那里形成好氧-缺氧界面)中获得共生体,当它们缩回外套腔时,这些脚可以将共生体转移到鳃表面。然而,一旦与宿主相关联,共生体就不必维持趋磁性结构,因为宿主通过生物灌溉和硫矿化行为提供氧气和还原硫。事实上,我们表明,在宿主内,共生体失去了磁小体链的完整性(可能还有它们的鞭毛)。共生体最终被宿主上皮细胞内吞和消化,磁小体在宿主细胞质中积累。宿主和共生体的行为似乎对 thyasirids 共生体的建立都很重要。