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A cold seep (sometimes called a cold vent) is an area of the ocean floor where hydrogen sulfide, methane and other hydrocarbon-rich fluid seepage occurs, often in the form of a brine pool. "Cold" does not mean that the temperature of the seepage is lower than that of the surrounding sea water. On the contrary, its temperature is often slightly higher.〔 p. 20.〕 Cold seeps constitute a biome supporting several endemic species. Cold seeps develop unique topography over time, where reactions between methane and seawater create carbonate rock formations and reefs. These reactions may also be dependent on bacterial activity. Ikaite, a hydrous calcium carbonate, can be associated with oxidizing methane at cold seeps. == Types == Types of cold seeps can be distinguished according to the depth, as shallow cold seeps and deep cold seeps.〔 Cold seeps can also be distinguished in detail, as follows: * oil/gas seeps〔 * gas seeps:〔 methane seeps * gas hydrate seeps〔 * brine seeps〔 are forming brine pools * pockmarks〔 * mud volcanos〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Cold seep」の詳細全文を読む スポンサード リンク
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