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Boreas An International Journal of Quaternary Research, Volume 36 Issue 3 2007

ISSN: 1502-3885 (electronic) 0300-9483 (paper)
Publication Frequency: 4 issues per year

The circumstances under which this title is published have changed:

Reason for change: Changed Publisher
Now published by: Wiley Blackwell
Date of change: 2008

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Original Articles
The surface geometry of the Last Glacial Maximum ice sheet in the Andøya–Skånland region, northern Norway, constrained by surface exposure dating and clay mineralogy
Atle Nesje;  Svein Olaf Dahl;  Henriette Linge;  Colin K. Ballantyne;  Danny McCarroll;  Edward J. Brook;  Grant M. Raisbeck; Francoise Yiou
Pages 227 – 239
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Holocene denudation of the northwest sector of Iceland as determined from accumulation of sediments on the continental margin
John T. Andrews
Pages 240 – 252
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High-resolution stratigraphy of the northernmost concentric raised bog in Europe: Sellevollmyra, Andøya, northern Norway
Karl-Dag Vorren;  Maarten Blaauw;  Stefan Wastegård;  Johannes Van Der Plicht; Christin Jensen
Pages 253 – 277
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Younger Dryas cirque glaciers in western Spitsbergen: smaller than during the Little Ice Age
Jan Mangerud; Jon Y. Landvik
Pages 278 – 285
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Dynamics of the Late Weichselian ice sheet on Svalbard inferred from high-resolution sea-floor morphology
Dag Ottesen;  Julian A. Dowdeswell;  Jon Y. Landvik; Juergen Mienert
Pages 286 – 306
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Timing of the last deglaciation in Belarus
Vincent R. Rinterknecht;  Irina E. Pavlovskaya;  Peter U. Clark;  Grant M. Raisbeck;  Françoise Yiou; Edward J. Brook
Pages 307 – 313
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Luminescence and radiocarbon ages from laminated Lateglacial aeolian sediments in western Jutland, Denmark
Else Kolstrup;  Andrew Murray; Göran Possnert
Pages 314 – 325
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The lithostratigraphy of the Les Echets basin, France: tentative correlation between cores
Daniel Veres;  Barbara Wohlfarth;  Valérie Andrieu-Ponel;  Svante Björck;  Jacques-Louis De Beaulieu;  Gunnar Digerfeldt;  Philippe Ponel;  Linda Ampel;  Siwan Davies;  Emmanuel Gandouin; Soumaya Belmecheri
Pages 326 – 340
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