globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2012.10.037
Scopus记录号: 2-s2.0-84870810103
论文题名:
Lateglacial/early Holocene fluvial reactions of the Jeetzel river (Elbe valley, northern Germany) to abrupt climatic and environmental changes
作者: Turner F.; Tolksdorf J.F.; Viehberg F.; Schwalb A.; Kaiser K.; Bittmann F.; von Bramann U.; Pott R.; Staesche U.; Breest K.; Veil S.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2013
卷: 60
起始页码: 91
结束页码: 109
语种: 英语
英文关键词: Biostratigraphy ; Climatic fluctuations ; Elbe ; Late Palaeolithic ; Lateglacial ; Palaeochannels ; River system development
Scopus关键词: Climatic fluctuations ; Elbe ; Late Palaeolithic ; Lateglacial ; Palaeochannels ; River systems ; Biostratigraphy ; Dynamics ; Glacial geology ; Landforms ; Vegetation ; Rivers ; biostratigraphy ; climate variation ; climatology ; coniferous forest ; environmental conditions ; fossil record ; herb ; Holocene ; human settlement ; lake level ; late glacial ; paleochannel ; paleoclimate ; paleoecology ; paleohydrology ; Paleolithic ; proxy climate record ; reconstruction ; river system ; shrub ; valley ; vegetation cover ; Germany ; Jeetze River ; Ostracoda
英文摘要: Mechanisms of climatic control on river system development are still only partially known. Palaeohydrological investigations from river valleys often lack a precise chronological control of climatic processes and fluvial dynamics, which is why their specific forces remain unclear. In this multidisciplinary case study from the middle Elbe river valley (northern Germany) multiple dating of sites (palynostratigraphy, radiocarbon- and OSL-dating) and high-resolution analyses of environmental and climatological proxies (pollen, plant macro-remains and ostracods) reveal a continuous record of the environmental and fluvial history from the Lateglacial to the early Holocene. Biostratigraphical correlation to northwest European key sites shows that river system development was partially out of phase with the main climatic shifts. The transition from a braided to an incised channel system predated the main phase of Lateglacial warming (∼14.6 ka BP), and the meandering river did not change its drainage pattern during the cooling of the Younger-Dryas period. Environmental reconstructions suggest that river dynamics were largely affected by vegetation cover, as a vegetation cover consisting of herbs, dwarf-shrubs and a few larger shrubs seems to have developed before the onset of the main Lateglacial warming, and pine forests appear to have persisted in the river valley during the Younger Dryas. In addition, two phases of high fluvial activity and new channel incision during the middle part of the Younger Dryas and during the Boreal were correlated with changes from dry towards wet climatic conditions, as indicated by evident lake level rises. Lateglacial human occupation in the river valley, which is shown by numerous Palaeolithic sites, forming one of the largest settlement areas of that period known in the European Plain, is assigned to the specific fluvial and environmental conditions of the early Allerød. © 2012 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60735
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作者单位: Institut für Geobotanik, Leibniz-Universität Hannover, Nienburger Straße 17, D-30167 Hannover, Germany; Seminar für Vor- und Frühgeschichte, Philipps-Universität Marburg, Biegenstraße 11, D-35032 Marburg, Germany; Institut für Geologie und Mineralogie, Universität Köln, Zülpicher Str. 49a, D-50674 Köln, Germany; Institut für Geosysteme und Bioindikation, Technische Universität Braunschweig, Langer Kamp 19c, D-38106 Braunschweig, Germany; Deutsches GeoForschungsZentrum GFZ, Telegrafenberg, D-14473 Potsdam, Germany; Niedersächsisches Institut für historische Küstenforschung, Viktoriastraße 26/28, D-26382 Wilhelmshaven, Germany; Niedersächsisches Landesmuseum Hannover, Willy-Brandt-Allee 5, D-30169 Hannover, Germany

Recommended Citation:
Turner F.,Tolksdorf J.F.,Viehberg F.,et al. Lateglacial/early Holocene fluvial reactions of the Jeetzel river (Elbe valley, northern Germany) to abrupt climatic and environmental changes[J]. Quaternary Science Reviews,2013-01-01,60
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