TY - JOUR UR - http://lib.ugent.be/catalog/pug01:8543740 ID - pug01:8543740 LA - eng TI - The younger Dryas and Preboreal landscape in the Moervaart area (northwestern Belgium) and the apparent decrease in human occupation PY - 2018 JO - (2018) VEGETATION HISTORY AND ARCHAEOBOTANY SN - 0939-6314 PB - 2018 AU - Bos, Johanna AU - Gelorini, Vanessa UGent 001995434587 801001965016 AU - Van der Meeren, Thijs WE11 002002361603 AU - Peleman, Jolien AU - Court-Picon, Mona AU - Demiddele, Hendrik AU - De Smedt, Philippe LA20 002002229641 802000150788 0000-0002-7230-4965 AU - Boudin, Mathieu AU - Verniers, Jacques WE13 801000298131 0000-0002-2939-7684 AU - Boeckx, Pascal LA24 001986067825 AU - Crombé, Philippe AB - This paper presents the results of multi-disciplinary research carried out on the deposits of a residual channel (“Peerdemeers”) of the Kale/Durme River in the Moervaart depression, NW Belgium. The combination of physical, botanical, zoological and chemical analyses allowed a detailed reconstruction of the channel ecosystem and the vegetation in the surrounding landscape during the Younger Dryas and Early Holocene. A chronology for the record was provided by radiocarbon dating. Vegetation patterns were influenced by major climate changes that occurred during this period. During the early Younger Dryas, the river channel was active and vegetation was open with scattered birch copses, shrubs, grasses and herbs. The channel was cut-off in the late Younger Dryas, while some heath developed in the area. The Friesland Phase is characterised by a lithological change and increase in water level in the residual channel. Dwarf birch disappeared and boreal forests developed. The area however, remained relatively open compared to other coversand areas in NW Europe. The Rammelbeek Phase is considered as a drier, more continental climate phase in which forest expansion was temporarily interrupted and grasslands became more abundant. Also at the “Peerdemeers” site an increase in grasses is recorded. During the entire period (ca. 1,000 years)there is no hard evidence for human activity. The absence of archaeological evidence is in sharp contrast with the preceding (Allerød) and succeeding periods (Boreal). This suggests that environmental conditions during the YD and PB were probably too unfavourable for hunter-gatherers to remain in the Moervaart area. ER -Download RIS file
| 00000nam^a2200301^i^4500 | |||
| 001 | 8543740 | ||
| 005 | 20181113145128.0 | ||
| 008 | 180104s2018------------------------eng-- | ||
| 022 | a 0939-6314 | ||
| 024 | a 000440822100004 2 wos | ||
| 024 | a 1854/LU-8543740 2 handle | ||
| 024 | a 10.1007/s00334-017-0666-3 2 doi | ||
| 040 | a UGent | ||
| 245 | a The younger Dryas and Preboreal landscape in the Moervaart area (northwestern Belgium) and the apparent decrease in human occupation | ||
| 260 | c 2018 | ||
| 520 | a This paper presents the results of multi-disciplinary research carried out on the deposits of a residual channel (“Peerdemeers”) of the Kale/Durme River in the Moervaart depression, NW Belgium. The combination of physical, botanical, zoological and chemical analyses allowed a detailed reconstruction of the channel ecosystem and the vegetation in the surrounding landscape during the Younger Dryas and Early Holocene. A chronology for the record was provided by radiocarbon dating. Vegetation patterns were influenced by major climate changes that occurred during this period. During the early Younger Dryas, the river channel was active and vegetation was open with scattered birch copses, shrubs, grasses and herbs. The channel was cut-off in the late Younger Dryas, while some heath developed in the area. The Friesland Phase is characterised by a lithological change and increase in water level in the residual channel. Dwarf birch disappeared and boreal forests developed. The area however, remained relatively open compared to other coversand areas in NW Europe. The Rammelbeek Phase is considered as a drier, more continental climate phase in which forest expansion was temporarily interrupted and grasslands became more abundant. Also at the “Peerdemeers” site an increase in grasses is recorded. During the entire period (ca. 1,000 years)there is no hard evidence for human activity. The absence of archaeological evidence is in sharp contrast with the preceding (Allerød) and succeeding periods (Boreal). This suggests that environmental conditions during the YD and PB were probably too unfavourable for hunter-gatherers to remain in the Moervaart area. | ||
| 598 | a A1 | ||
| 100 | a Bos, Johanna | ||
| 700 | a Gelorini, Vanessa u UGent 0 001995434587 0 801001965016 0 977519869729 9 F7884FDC-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Van der Meeren, Thijs u WE11 0 002002361603 0 802000139472 9 F8C0A246-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Peleman, Jolien 0 000060352083 9 0230D7CE-F0EE-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Court-Picon, Mona u WE13 0 802000444014 9 1C353A84-F0EE-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Demiddele, Hendrik | ||
| 700 | a De Smedt, Philippe u LA20 0 002002229641 0 802000150788 0 0000-0002-7230-4965 9 FBF59098-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Boudin, Mathieu | ||
| 700 | a Verniers, Jacques u WE13 0 801000298131 0 0000-0002-2939-7684 9 F39D70C8-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Boeckx, Pascal u LA24 0 001986067825 0 801000894275 9 F4AEF482-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 700 | a Crombé, Philippe u LW02 0 801000753627 9 F478F97C-F0ED-11E1-A9DE-61C894A0A6B4 | ||
| 650 | a History and Archaeology | ||
| 650 | a Earth and Environmental Sciences | ||
| 653 | a Late-glacial/early Holocene transition | ||
| 653 | a Multi-proxy analyses | ||
| 653 | a Palynology | ||
| 653 | a Climate | ||
| 653 | a Hunter-gatherers | ||
| 653 | a Belgium | ||
| 653 | a PLEISTOCENE-HOLOCENE TRANSITION | ||
| 653 | a MULTI-PROXY | ||
| 653 | a EVENT STRATIGRAPHY | ||
| 653 | a CLIMATIC CHANGES | ||
| 653 | a NW BELGIUM | ||
| 653 | a LAKE | ||
| 653 | a ASSEMBLAGES | ||
| 653 | a NETHERLANDS | ||
| 653 | a RECORD | ||
| 653 | a RECONSTRUCTION | ||
| 773 | t VEGETATION HISTORY AND ARCHAEOBOTANY g Veg. Hist. Archaeobot. 2018. 27 (5) p.697-715 q 27:5<697 | ||
| 856 | 3 Full Text u https://biblio.ugent.be/publication/8543740/file/8543744 z [ugent] y Bos et al., VHA 2017.pdf | ||
| 920 | a article | ||
| Z30 | x LW 1 LW02 | ||
| 922 | a UGENT-LW | ||
| Z30 | x WE 1 WE13 | ||
| 922 | a UGENT-WE | ||
| Z30 | x WE 1 WE11 | ||
| 922 | a UGENT-WE | ||
| Z30 | x BW 1 LA20 | ||
| 922 | a UGENT-BW | ||
| Z30 | x BW 1 LA24 | ||
| 922 | a UGENT-BW | ||
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