Multiple oscillations during the Lateglacial as recorded in a multi-proxy, high-resolution record of the Moervaart palaeolake (NW Belgium)

• Main Authors: Crombé, Philippe, De Smedt, Philippe, Serbruyns, Lynn, Bos, Johanna A.A., Heiri, Oliver, Gelorini, Vanessa, Verniers, Jacques, Court-Picon, Mona, Boeckx, Pascal, Finke, Peter, Marcelino, Vera, Gobert, Stefan, Martens, Koen, Langohr, Roger, Hoek, Wim Z., Van Damme, Dirk, Van Asch, Nelleke, Van Strydonck, Mark, Mostaert, Frank, Van Der Meeren, Thijs, Demiddele, Hendrik, Boudin, Mathieu
• Format: Text
• Language: English
• Published: Elsevier 2017
• Subjects: 580 Plants Botany; Greenland; Greenland ice cores; Tundra
• Online Access: https://dx.doi.org/10.7892/boris.99417; http://boris.unibe.ch/99417/

This paper presents the results of multi-disciplinary research carried out on the deposits of Moervaart depression, NW Belgium, one of the largest palaeolakes (∼25 km2) that existed during the Lateglacial interstadial in NW Europe. The multi-proxy study, including physical (organic matter and calcium carbonate, magnetic susceptibility, micromorphological), botanical (pollen, macrofossils, diatoms), zoological (ostracods, molluscs, chironomids) and chemical analyses (stable carbon and oxygen isotopes) has resulted in a detailed reconstruction of the Lateglacial landscape as well of the local conditions that prevailed in the lake itself. A chronology of the record was provided by radiocarbon dating and comparison with radiocarbon dates of the nearby Rieme site. These yielded a good match with the regional biostratigraphy. 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.