کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
5786627 | 1640773 | 2017 | 16 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Multiple oscillations during the Lateglacial as recorded in a multi-proxy, high-resolution record of the Moervaart palaeolake (NW Belgium)
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
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چکیده انگلیسی
During the Lateglacial, vegetation and geomorphology of the landscape in general changed from a tundra landscape to a boreal forest. The vegetation development, however, was interrupted by a number of cold reversals. Three centennial-scale cold oscillations are present in the record: 1) the so-called Older Dryas corresponding to GI-1d in the Greenland ice-cores, 2) a short and pronounced cold event during the early Allerød, which could be correlated to GI-1c2 and 3) a cooling event during the late Allerød probably corresponding to the Intra Allerød Cold Period (IACP) or GI-1b. The latter most likely was responsible for the disappearance of the Moervaart palaeolake.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary Science Reviews - Volume 162, 15 April 2017, Pages 26-41
Journal: Quaternary Science Reviews - Volume 162, 15 April 2017, Pages 26-41
نویسندگان
Johanna A.A. Bos, Philippe De Smedt, Hendrik Demiddele, Wim Z. Hoek, Roger Langohr, Vera Marcelino, Nelleke Van Asch, Dirk Van Damme, Thijs Van der Meeren, Jacques Verniers, Pascal Boeckx, Mathieu Boudin, Mona Court-Picon, Peter Finke, Vanessa Gelorini,