深海热液系统对深海环境的环境生态影响

M. Sunamura, T. Noguchi, Hiroyuki Yamamoto, K. Okamura
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引用次数: 2

摘要

热液循环为深海提供了大量的化学物质。高温热液中释放的化学物质99%以上流入深海,形成深海热液柱。对热液羽流的观测引导了对深海热液喷口的研究,如确定深海热液喷口的位置、确定深海火山喷发的位置以及计算海底到深海的地球化学通量。热液羽流通过提供许多还原性化学物质来影响深海微生物群落,这些还原性化学物质可能是趋化岩石营养微生物的能量来源。本文(1)综述了热液羽流的物理、化学和生物学研究;(2)讨论了新的野外调查技术和海底对深海环境的生态影响。
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Environmental and Ecological Impact on Deep-sea Environment from Deep-sea Hydrothermal System
Hydrothermal circulations supply a huge amount of chemical species into the deep sea. More than 99% of chemical species emitted from high-temperature hydrothermal fluids flow into the deep sea and construct deep-sea hydrothermal plumes. Observations of hydrothermal plumes have led studies of deep-sea hydrothermal vents, such as locating deep-sea hydrothermal vents, locating deep-sea volcanic eruptions, and calculating geochemical fluxes from sub-seafloor to deep ocean. Hydrothermal plumes affect the microbial community in deep seas by supplying many reduced chemicals, which are possible energy sources of chemolithotrophic microbes. This paper (1) reviews physical, chemical, biological studies of hydrothermal plumes and (2) discusses novel field survey technology and ecological infection of sub-seafloor to the deep-sea environment.
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