Deglaciation of the Eurasian ice sheet complex.

• Published in: Quaternary Science Reviews
• Main Authors: Patton, H., Hubbard, A., Andreassen, K., Auriac, A., Whitehouse, P.L., Stroeven, A., Shackleton, C., Winsborrow, M., Heyman, J., Hall, A.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Elsevier 2017
• Subjects: Barents Sea; Franz Josef Land; Svalbard; Fennoscandia; Ice Sheet; North Atlantic; Novaya Zemlya
• Online Access: http://dro.dur.ac.uk/22213/; http://dro.dur.ac.uk/22213/2/22213.pdf; http://dro.dur.ac.uk/22213/1/22213.pdf; https://doi.org/10.1016/j.quascirev.2017.05.019

The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic sea-level lowering. Whilst recent terrestrial and marine empirical insights have improved understanding of the chronology, patt...