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A new bathymodioline mussel symbiosis at the Juan de Fuca hydrothermal vents

机译:胡安·德·富卡热液喷口处的一种新的盐基二碘甲烷贻贝共生

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Until recently, the only major hydrothermal vent biogeographic province not known to include bathymodioline mussels was the spreading centers of the northeast Pacific, but deep-sea dives using DSV Alvin on the Endeavor segment of the Juan de Fuca Ridge (47°56N 129°06W; ~2,200 m depth) in August 1999 yielded the only recorded bathymodioline mytilids from these northeastern Pacific vents. One specimen in good condition was evaluated for its relatedness to other deep-sea bathymodioline mussels and for the occurrence of chemoautotrophic and/or methanotrophic symbionts in the gills. Phylogenetic analyses of the host cytochrome oxidase I gene show this mussel shares evolutionary alliances with hydrothermal vent and cold seep mussels from the genus Bathymodiolus, and is distinct from other known species of deep-sea bathymodiolines, suggesting this mussel is a newly discovered species. Ultrastructural analyses of gill tissue revealed the presence of coccoid bacteria that lacked the intracellular membranes observed in methanotrophic symbionts. The bacteria may be extracellular but poor condition of the fixed tissue complicated conclusions regarding symbiont location. A single gamma-proteobacterial 16S rRNA sequence was amplified from gill tissue and directly sequenced from gill tissue. This sequence clusters with other mussel chemoautotrophic symbiont 16S rRNA sequences, which suggests a chemoautotrophic, rather than methanotrophic, symbiosis in this mussel. Stable carbon (δ~(13)C = -26.6%) and nitrogen (δ~(15)N = +5.19%) isotope ratios were also consistent with those reported for other chemoautotroph-mussel symbioses. Despite the apparent rarity of these mussels at the Juan de Fuca vent sites, this finding extends the range of the bathymodioline mussels to all hydrothermal vent biogeographic provinces studied to date.
机译:直到最近,唯一未知的主要热液喷口生物地理省份是东北太平洋的扩散中心,但在胡安德富卡海岭的奋进段上使用DSV Alvin进行深海潜水(47°56N 129°06W ;〜2,200 m深度)(1999年8月),从这些东北太平洋喷口中获得了唯一记录的贝氏莫氏类til虫。评估一个状况良好的标本与其他深海贝氏莫氏贻贝的相关性,以及the中化学自养和/或甲烷营养共生体的发生。宿主细胞色素氧化酶I基因的系统发育分析表明,该贻贝与来自水线虫属的热液喷口和冷渗水贻贝具有进化联盟,并且与其他已知的深海线虫病物种不同,表明该贻贝是新发现的物种。对g组织的超微结构分析表明,存在球菌,其缺乏在甲烷营养菌共生体中观察到的细胞内膜。细菌可能在细胞外,但固定组织的状况较差,有关共生体位置的结论很复杂。从g组织中扩增出单个γ-变形细菌16S rRNA序列,并直接从directly组织中测序。此序列与其他贻贝化学自养共生生物16S rRNA序列聚类,这表明该贻贝具有化学自养而不是甲烷营养共生。稳定的碳(δ〜(13)C = -26.6%)和氮(δ〜(15)N = + 5.19%)同位素比率也与其他化学自养贻贝共生体的同位素比率一致。尽管在胡安·德富卡喷口处这些贻贝明显稀少,但这一发现将深水二碘化贻贝的范围扩展到了迄今为​​止研究的所有热液喷口生物地理省。

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