Ocean sediments presented a much more complete geologic record of the Pleistocene than continental glacial deposits did.

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。

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In the normal water phase, the remaining Phosphorus makes its way, settles to the bottom of the ocean, and gets mixed into ocean sediments.

在正常的水相中，残留的磷会自己移动，沉淀到海洋底部，并混合到海洋沉积物中。

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After millions of years, powerful geological forces, like underwater volcanoes lift up the ocean sediments to form new land.

数百万年后，强大的地质力量，比如海底火山，会掀起海洋沉积物，形成新的陆地。

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These proxies include coral, ice cores, mineral deposits in caves, lake and ocean sediments, as well as a few historical records like grape harvest dates.

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