adj.热液的;热水的
网络 水热法; 热水的; 水热合成
It all began in 1977 with the exploration of hydrothermal vents on the ocean floor.
一切始于1977年的一次海底上深海热泉的探索。
Hydrothermal vents are cracks in the Earth´s surface that occur, the ones we are talking about here are found deep at the bottom of the ocean.
深海热泉是地球表面出现的裂缝,我们在这里提到的裂缝是在海底深处发现的。
Some of the large sedentary organisms associated with vents are also found at ordinary deep-sea temperatures many meters from the nearest hydrothermal sources.
在距离最近的热液源几米远的深海温度下,也发现了一些与火山口有关的大型静止生物。
However, near hydrothermal vents, areas of the ocean where warm water emerges from subterranean sources, live remarkable densities of huge clams, blind crabs, and fish.
然而,在海底热液喷口附近,也就是温暖海水从地下涌出的地方,生活着大蛤、盲蟹和鱼类,数量非常庞大。
As we said, these hydrothermal vents are releasing into the ocean depth this intensely hot water that contains a chemical called hydrogen sulfide, and also a gas, carbon dioxide.
正如我们所说,这些热液喷口正在向海洋深处释放这种强热的水,含有一种叫做硫化氢的化学物质,和一种气体,二氧化碳。