The nature of MIS 3 stadial–interstadial transitions in Europe: New insights from model–data comparisons

Autor: Van Meerbeeck, C.J. ^{a, ∗}, Renssen, H. ^a, Roche, D.M. ^{a, b}, Wohlfarth, B. ^c, Bohncke, S.J.P. ^a, Bos, J.A.A. ^a, Engels, S. ^a, Helmens, K.F. ^d, Sánchez-Goñi, M.F. ^e, Svensson, A. ^f, Vandenberghe, J. ^a

Publikováno v: In Quaternary Science Reviews 2011 30(25):3618-3637

Tropical snowline changes at the last glacial maximum: A global assessment

Autor: Mark, B.G. ^{a, b, c, ⁎}, Harrison, S.P. ^{a, d}, Spessa, A. ^a, New, M. ^e, Evans, D.J.A. ^{b, f}, Helmens, K.F. ^g

Publikováno v: In Quaternary International 2005 138:168-201

Interglacial temperatures in northern Scandinavia during the Last Glacial Maximum

Autor: Helmens, K.F., Bos, J.A.A., Engels, S., van Meerbeeck, C.J.V.C., Bohncke, S.J.P., Renssen, H., Heiri, O., Brooks, S.J., Seppa, H., Birks, H.J.B., Wohlfarth, B.

Publikováno v: Geology, 35(11), 987-990. Geological Society of America
Helmens, K F, Bos, J A A, Engels, S, van Meerbeeck, C J V C, Bohncke, S J P, Renssen, H, Heiri, O, Brooks, S J, Seppa, H, Birks, H J B & Wohlfarth, B 2007, ' Interglacial temperatures in northern Scandinavia during the Last Glacial Maximum. ', Geology, vol. 35, no. 11, pp. 987-990 . https://doi.org/10.1130/G23995A.1

Scandinavia is generally considered to have been covered extensively with ice throughout marine isotope stages (MIS) 4-2 between 75 and 10 ka. Here we present evidence for ice-free, warm conditions in the central area of the Scandinavian glaciations

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7226fbdb11d28d059c3adb6c39dbe685
https://research.vu.nl/en/publications/9fc134a5-ab46-44f0-a8a8-a8820e5c7757

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