Various paleoclimatic records from ice cores, deep sea sediments, speleothems, continental paleobotanical data, and loesses show similar abrupt climate events, which are consistent with Younger Dryas events, during the terminations of the last four glacial periods.
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Raymo ( 2005 ) used measurements of ? 18 O in benthic foraminifera from 57 globally distributed deep sea sediment cores, taken as a proxy for the total global mass of glacial ice sheets, to reconstruct the climate for the past five million years.
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""'Chryseobacterium profundimaris " "'is a Gram-negative, strictly aerobic, rod-shaped and non-motile bacteria from the genus of Chryseobacterium which has been isolated from deep sea sediments from the Atlantic Ocean.
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