首页> 外文期刊>Journal of Molluscan Studies >Thyasirid bivalves from the methane seep community off Paramushir Island (Sea of Okhotsk) and their nutrition
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Thyasirid bivalves from the methane seep community off Paramushir Island (Sea of Okhotsk) and their nutrition

机译:帕拉默希尔岛(鄂霍次克海)附近甲烷渗流社区的Thyasirid双壳类及其营养

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The present study focuses on two apparent species: the giant thyasirid Conchocele bisecta (Conrad, 1849), which is the dominant species of the benthic community in a gas hydrate area with cold-water methane-rich vents at a depth of about 800 m on the slope off Paramushir Island (Kuril Islands, Sea of Okhotsk) and small unidentified thyasirid bivalves from this same community. An examination of the shell morphology of these thyasirids showed that the small bivalves were in fact young specimens of C. bisecta, characterized by a high individual and age variability. A transmission electron microscopic study of C. bisecta revealed gills with 'Type 3' filaments, which were extended abfrontally and had a distinct bacteriocyte zone with extracellular symbionts. The symbiotic bacteria found were spherical, similar to thiotrophic symbionts of other thyasirids. The isotopic delta C-13 values of C. bisecta soft tissues (from -39.6 to -33.8%) were much heavier than those of methane in the Paramushir gas-hydrate area and matched the range characteristic of symbiotrophic bivalves harbouring sulphur-oxidizing chemoautotrophic bacteria. The variations in delta C-13 and delta N-15 recorded for large and small C. bisecta can be related to ontogenetic differences in life habit: small individuals are totally buried in the sediment, while large ones are half-buried. Data from fatty acid (FA) analysis indicate that sulphur-oxidizing symbionts constitute almost the entire nutrition of C. bisecta, with no significant contribution of symbiotic or free-living methanotrophs. Furthermore, neither FA nor isotopic compositions provided evidence for photosynthetic sources as food items for C. bisecta through filter feeding.
机译:本研究着眼于两个明显的物种:巨型thyasirid Conchocele bisecta(Conrad,1849年),它是天然气水合物区底栖动物群落的优势物种,在天然气水合物区域,深水甲烷排放口约在800 m处。帕拉默希尔岛(Kuril岛,鄂霍次克海)附近的斜坡,以及来自同一社区的小型不知名的锡西里德双壳类动物。对这些甲壳动物的壳形态进行检查后发现,这些小双壳类动物实际上是双壳梭菌的年轻标本,其个体和年龄差异很大。透射电镜对双歧杆菌的研究表明,with具有“ 3型”细丝,a向前方延伸,并具有明显的带有胞外共生菌的细菌细胞区。发现的共生细菌是球形的,类似于其他thyasirids的硫营养共生菌。二裂衣原体软组织的同位素δC-13值(从-39.6至-33.8%)比甲烷气水合物区域中的甲烷重得多,并且与带有硫氧化性化学自养细菌的共生双壳类的范围特征相符。 。大和小的双歧梭菌记录的δC-13和δN-15的变化可能与生活习惯的个体发育差异有关:小个体被完全埋在沉积物中,大个体被半埋。脂肪酸(FA)分析的数据表明,硫氧化共生菌几乎构成了C. bisecta的全部营养,而没有共生或自由生活的甲烷营养菌。此外,FA和同位素组合物均不能通过滤料喂养提供光合作用的证据,作为双歧杆菌的食物。

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