Lava injected into deep sea sediments is baking sediments and driving out greenhouse gases.
深海下的极热熔岩会把海底有机沉积物烤干同时释放出温室气体。
Such a study provides a basis for understanding palaeoclimate shifts by investigation of organic carbon isotopic composition in the deep sea sediments.
从而为利用深海沉积有机质碳同位素组成研究古气候变迁提供了依据。
Most of those events were found in the glacial and deep sea sediments, mainly occurring on the high latitudes of the Northern Hemisphere.
指出这些事件大部分首先发现于冰川和深海沉积物中，且集中在北半球的高纬度地带。
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