{"refrec":{"BRefID":207160,"RR":"<b>Berger, W.H.</b> (2011). Geologist at sea: Aspects of ocean history, <b><i>in</i></b>: Carlson, C.A. <i>et al.</i> <i>Ann. Rev. Mar. Sci. 3. Annual Review of Marine Science,</i> 3: pp. 1-34. <a href=\"https://dx.doi.org/10.1146/annurev-marine-120709-142831\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-120709-142831</a>","BEntID":199219,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Carlson, C.A. <i>et al.</i> <i>Ann. Rev. Mar. Sci. 3. Annual Review of Marine Science,</i> 3: pp. 1-34. <a href=\"https://dx.doi.org/10.1146/annurev-marine-120709-142831\" target=\"_blank\">https://dx.doi.org/10.1146/annurev-marine-120709-142831</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Berger, W.H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Berger, W.H.","Englishabstract":"Ocean history is largely read from deep-sea sediments, using microscopic fossils, notably foraminifers. Ice age fluctuations in the ocean's sediments provided for a new geologic understanding of climate change. The discovery of rapid decay of ice masses at the end of glacial periods was especially important, yielding rates of sea level rise reaching values of 1 to 2 m per century for millennia. Thanks to deep-ocean drilling, the overall planetary cooling trend in the Cenozoic was recognized as occurring in three large steps. 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