{"refrec":{"BRefID":302329,"RR":"<b>Uenzelmann-Neben, G.; Gohl, K.</b> (2012). Amundsen Sea sediment drifts: Archives of modifications in oceanographic and climatic conditions. <i>Mar. Geol. 299-302</i>: 51-62. <a href=\"https://dx.doi.org/10.1016/j.margeo.2011.12.007\" target=\"_blank\">https://dx.doi.org/10.1016/j.margeo.2011.12.007</a>","BEntID":294573,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Mar. Geol. 299-302</i>: 51-62. <a href=\"https://dx.doi.org/10.1016/j.margeo.2011.12.007\" target=\"_blank\">https://dx.doi.org/10.1016/j.margeo.2011.12.007</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Uenzelmann-Neben, G.; Gohl, K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Uenzelmann-Neben, G.; Gohl, K.","Englishabstract":"Drift deposits document stages of particular dynamic bottom-currents and associated sedimentary transport activities. The analysis of seismic reflection data from the Amundsen Sea, southern Pacific Ocean, reveals sediment drift formation already in Eocene/Oligocene times. This observation indicates bottom current activity and hence a cold climate for the late Palaeogene in an area, which today lies under the influence of Antarctic Bottom Water (AABW) originating in the Ross Sea. 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