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Deepest and hottest hydrothermal activity in the Okinawa Trough: the Yokosuka site at Yaeyama Knoll

机译:冲绳海槽最深最热的热液活动:八重山丘陵的横须贺站

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摘要

Since the initial discovery of hydrothermal vents in 1977, these ‘extreme’ chemosynthetic systems have been a focus of interdisciplinary research. The Okinawa Trough (OT), located in the semi-enclosed East China Sea between the Eurasian continent and the Ryukyu arc, hosts more than 20 known vent sites but all within a relatively narrow depth range (600–1880 m). Depth is a significant factor in determining fluid temperature and chemistry, as well as biological composition. However, due to the narrow depth range of known sites, the actual influence of depth here has been poorly resolved. Here, the Yokosuka site (2190 m), the first OT vent exceeding 2000 m depth is reported. A highly active hydrothermal vent site centred around four active vent chimneys reaching 364°C in temperature, it is the hottest in the OT. Notable Cl depletion (130 mM) and both high H2 and CH4 concentrations (approx. 10 mM) probably result from subcritical phase separation and thermal decomposition of sedimentary organic matter. Microbiota and fauna were generally similar to other sites in the OT, although with some different characteristics. In terms of microbiota, the H2-rich vent fluids in Neuschwanstein chimney resulted in the dominance of hydrogenotrophic chemolithoautotrophs such as Thioreductor and Desulfobacterium. For fauna, the dominance of the deep-sea mussel Bathymodiolus aduloides is surprising given other nearby vent sites are usually dominated by B. platifrons and/or B. japonicus, and a sponge field in the periphery dominated by Poecilosclerida is unusual for OT vents. Our insights from the Yokosuka site implies that although the distribution of animal species may be linked to depth, the constraint is perhaps not water pressure and resulting chemical properties of the vent fluid but instead physical properties of the surrounding seawater. The potential significance of these preliminary results and prospect for future research on this unique site are discussed.
机译:自1977年首次发现热液喷口以来,这些“极端”化学合成系统一直是跨学科研究的重点。冲绳海槽(OT)位于欧亚大陆和琉球弧之间的半封闭东海中,拥有20多个已知的喷发点,但都位于相对较窄的深度范围内(600-1880 m)。深度是决定流体温度和化学性质以及生物组成的重要因素。但是,由于已知地点的深度范围较窄,此处对深度的实际影响难以解决。在这里,横须贺站(2190 m)被报道,这是第一个OT深度超过2000 depthm的通风口。一个高活性的热液喷口,以四个活动的烟囱为中心,温度达到364°C,是OT中最热的一个。明显的Cl消耗(130 mM)以及高H2和CH4浓度(约10 mM)可能是由于亚临界相分离和沉积有机物的热分解所致。微生物群和动物区系总体上与旧约中的其他地点相似,尽管具有一些不同的特征。就微生物群而言,新天鹅堡烟囱中富含H2的排泄液导致了氢营养型化学自养生物如硫代还原剂和脱硫细菌的优势。对于动物区系,由于其他附近的通风孔通常以双歧杆菌(B. platifrons)和/或日本血吸虫(B. japonicus)为主,而深海贻贝(Bathymodiolus aduloides)的优势令人吃惊,而OT通风孔则以Poecilosclerida为主的周边海绵场是罕见的。我们从横须贺厂区获得的见解表明,尽管动物物种的分布可能与深度有关,但制约因素可能不是水压和最终排放物的化学性质,而是周围海水的物理性质。讨论了这些初步结果的潜在意义以及对该独特站点的未来研究前景。

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