{"refrec":{"BRefID":257860,"RR":"<b>Hodgson, D.; Verleyen, E.; Vyverman, W.; Sabbe, K.; Leng, M.; Pickering, M.; Keely, B.</b> (2009). A geological constraint on relative sea level in Marine Isotope Stage 3 in the Larsemann Hills, Lambert Glacier region, East Antarctica (31 366-33 228 cal yr BP). <i>Quat. Sci. Rev. 28(25-26)</i>: 2689-2696. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2009.06.006\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2009.06.006</a>","BEntID":249870,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Quat. Sci. Rev. 28(25-26)</i>: 2689-2696. <a href=\"https://dx.doi.org/10.1016/j.quascirev.2009.06.006\" target=\"_blank\">https://dx.doi.org/10.1016/j.quascirev.2009.06.006</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hodgson, D.; Verleyen, E.; Vyverman, W.; Sabbe, K.; Leng, M.; Pickering, M.; Keely, B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hodgson, D. <i>et al.</i>","Englishabstract":"In this paper we present geological evidence from the Larsemann Hills (Lambert Glacier - Amery Ice Shelf region, East Antarctica) of marine sediments at an altitude of c. 8 m a.s.l., as revealed by diatom, pigment and geochemical proxies in a lake sediment core. The sediments yielded radiocarbon dates between c. 26 650 and 28 750 <sup>14</sup>Cyr BP (31 366-33 228 cal yr BP). This information can be used to constrain relative sea level adjacent to the Lambert Glacier at the end of Marine isotope Stage 3. 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