在某些时期，世界海洋的底层来自遥远的北大西洋下沉的寒冷、稠密的水。
During some periods, the bottom layer of the world's oceans comes from cold, dense water sinking in the far North Atlantic.
在这一时期，谷物和其他固体货物被装在由非粘土材料制成的集装箱里穿过 Remain 海洋。
During the period, grain and other solid cargo was shipped across the Remain Sea in containers made from material other than clay.
相比于大陆冰川沉积物，海洋沉积物提供了更完整的更新世时期的地质记录。
Ocean sediments presented a much more complete geologic record of the Pleistocene than continental glacial deposits did.
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