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The Arctic’s glacial history has classically been interpreted from marine records in terms of the fluctuations of the Eurasian and North American ice sheets. However, the extent and timing of the East Siberian Ice Sheet (ESIS) have remained uncerta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2423::da31f2a4416070d4401cebb4b540741a
http://urn.fi/urn:nbn:fi-fe202301031295
http://urn.fi/urn:nbn:fi-fe202301031295
Autor:
Lyså, A. (Astrid), Benediktsson, ĺ. Ö. (ĺvar Örn), Emery, A. (Andy), Gregoire, L. (Lauren), Jennings, A. (Anne), Morigi, C. (Caterina), Müller, J. (Juliane), O’Regan, M. (Matt), Sarala, P. (Pertti), Stokes, C. (Chris), Szczuciński, W. (Witold), Winsborrow, M. (Monica)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2423::622d712895d015bbe292b747d611e6aa
http://urn.fi/urn:nbn:fi-fe2019102534805
http://urn.fi/urn:nbn:fi-fe2019102534805