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硫化物作为深海热液喷口虾的化学刺激物。

Sulfide as a Chemical Stimulus for Deep-Sea Hydrothermal Vent Shrimp.

作者信息

Renninger G H, Kass L, Gleeson R A, Van Dover C L, Battelle B-A, Jinks R N, Herzog E D, Chamberlain S C

出版信息

Biol Bull. 1995 Oct;189(2):69-76. doi: 10.2307/1542456.

Abstract

Organisms dependent on deep-sea hydrothermal vents for their existence face extinction when their vents expire, unless they can establish populations on neighboring vents or on new vent sites. Propagules, including larvae and motile adults, are readily dispersed broadly by seafloor currents, but how they recognize active hydrothermal sites is problematical. Compelling evidence that vent organisms can find and colonize hydrothermal sites has been provided by a series of observations on the East Pacific Rise (1). New hydrothermal vents created there following a volcanic eruption on the seafloor in March 1991 were colonized by sessile invertebrates in less than one year. On the Mid-Atlantic Ridge, shrimp that normally cluster on sulfide surfaces have been observed to swim directly back to the surfaces when displaced from them. How do vent animals locate new or existing vents? Passive transport by currents (2) or active swimming without guidance by some physical cue is not likely to result in success (3). Chemicals present in hydrothermal fluids have been proposed as attractants. We provide the first evidence of a chemosensory response in a vent invertebrate to sulfides, which are prevalent in vent fluids and provide the energy,for chemosynthetic primary production at vents.

摘要

依赖深海热液喷口生存的生物,当其所在的喷口消失时便面临灭绝,除非它们能够在邻近的喷口或新的喷口区域建立种群。包括幼虫和能活动的成体在内的繁殖体很容易被海床水流广泛扩散,但它们如何识别活跃的热液区域仍是个问题。对东太平洋海隆的一系列观察提供了有力证据,表明喷口生物能够找到并在热液区域定殖(1)。1991年3月海底火山喷发后在那里形成的新热液喷口,不到一年就被固着无脊椎动物定殖。在中大西洋海脊,通常聚集在硫化物表面的虾被观察到从硫化物表面移开后能直接游回。喷口动物是如何定位新的或现有的喷口的呢?靠水流被动运输(2)或在没有某种物理线索引导的情况下主动游动不太可能成功(3)。热液流体中存在的化学物质已被提出作为引诱剂。我们首次提供了喷口无脊椎动物对硫化物产生化学感应反应的证据,硫化物在喷口流体中普遍存在,并为喷口处的化学合成初级生产提供能量。

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