The science of paleoceanography analyzes variations in the relative abundance of stable isotopes of oxygen preserved within the carbonate shells found in deep sea sediment, which allows them to interpret The rate that marine snow is being deposited on the sea floor Changes in the temperature of surface and deep water over time Changes in the amount of terrigenous sediment being deposited by wind The rate that cosmogenous sediment is deposited over time The abundance of diatoms and radiolaria that are lithified in the marine sediment

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