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首页> 外文期刊>Marine Geology >Comments on the paper of Gay et al. (2006) Seafloor fades related to upward methane flux within a Giant Pockmark of the Lower Congo Basin. Marine Geology 226:81-95
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Comments on the paper of Gay et al. (2006) Seafloor fades related to upward methane flux within a Giant Pockmark of the Lower Congo Basin. Marine Geology 226:81-95

机译:对盖伊等人论文的评论。 (2006)海床褪色与下刚果盆地大麻点内的甲烷向上通量有关。海洋地质226:81-95

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The paper by Gay et al. describes a giant pockmark on the basis of geological and biological data collected during ROV dives. The description of seep communities based on a transect across the pockmark includes some mistakes. Part of the description of the fauna is attributed to Olu-Le Roy et al. (2003) and includes data that have not been presented in this oral communication. An "evolutive model" is proposed, based on these data and on an incorrect interpretation of symbiotic species requirements (classification of methane vs sulfide dependent species). In this note, I would like to point out the mistakes of this paper and express why their model cannot be used to describe the reality of the seabed.
机译:盖伊等人的论文。根据ROV潜水期间收集的地质和生物学数据,描述了一个巨大的麻点。基于痘痕上横断面的渗透社区的描述包含一些错误。动物区系的部分描述归因于Olu-Le Roy等人。 (2003年),并包括尚未在本次口头交流中提供的数据。基于这些数据和对共生物种需求(甲烷与硫化物依赖性物种的分类)的错误解释,提出了“进化模型”。在本文中,我想指出本文的错误,并说明为什么不能使用其模型来描述海床的现实情况。

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