Timing of the Northern Prince Gustav Ice Stream retreat and the deglaciation of northern James Ross Island, Antarctic Peninsula during the last glacial–interglacial transition

• Published in: Quaternary Research
• Main Authors: Nývlt, Daniel, Braucher, Régis, Engel, Zbyněk, Mlčoch, Bedřich, Team, ASTER
• Other Authors: Ministry of the Environment of the Czech Republic, Czech Science Foundation, European Social Fund, Czech Republic, INSU/CNRS, French Ministry of Research and Higher Education, IRD, CEA
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2014
• Subjects: Antarctic; The Antarctic; Antarctic Peninsula; Ross Island; Prince Gustav Channel; Lachman; Cape Lachman; Antarc*; Antarctica; Ice Sheet; Ice Shelf; James Ross Island
• Online Access: http://dx.doi.org/10.1016/j.yqres.2014.05.003; http://api.elsevier.com/content/article/PII:S0033589414000672?httpAccept=text/xml; http://api.elsevier.com/content/article/PII:S0033589414000672?httpAccept=text/plain; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S003358940000082X

Abstract The Northern Prince Gustav Ice Stream located in Prince Gustav Channel, drained the northeastern portion of the Antarctic Peninsula Ice Sheet during the last glacial maximum. Here we present a chronology of its retreat based on in situ produced cosmogenic 10 Be from erratic boulders at Cape...