The authors are grateful to IPEV, the captain and the crew of the Marion Dufresne and to the scientific party of the IMAGES P.I.C.A.S.S.O cruise. We also thank Dag Inge Blindheim and Rune Søraas at Uni Research for help with sample preparation and stable isotope analyses and Eva Bjørseth at Department of Earth Science for help with the map construction. This work is a contribution of the European Science Foundation EuroMARC program, through the AMOCINT project (grant number 187166), funded through grants from the Research Council of Norway, and RCN Frinatek project NOCWARM (grant number 205524), and contributes to EU-FP7 IP Past4Future. U. Ninnemann received funding for this study from a University of Bergen Meltzer research grant.
Department of Earth Science, University of Bergen, Allégaten 41, Bergen, Norway; Bjerknes Centre for Climate Research, Bergen, Norway; Discipline of Geography, National University of Ireland, University Road, Galway, Ireland; Institute of Marine and Coastal Sciences and Department of Geology Rutgers, The State University of New Jersey, 71 Dudley Road, New Brunswick, NJ, United States
Recommended Citation:
Irvalı N.,Ninnemann U.S.,Kleiven H.K.F.,et al. Evidence for regional cooling, frontal advances, and East Greenland Ice Sheet changes during the demise of the last interglacial[J]. Quaternary Science Reviews,2016-01-01,150