globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2012.10.026
Scopus记录号: 2-s2.0-84870156464
论文题名:
The chronological position of the Lohne Soil in the Nussloch loess section - re-evaluation for a European loess-marker horizon
作者: Kadereit A.; Kind C.-J.; Wagner G.A.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2013
卷: 59
起始页码: 67
结束页码: 86
语种: 英语
英文关键词: Chronology ; Loess ; Lohne Soil ; Palaeosols ; Pedostratigraphic marker horizon ; Southern Germany ; Upper Palaeolithic ; Weichselian Pleniglacial
Scopus关键词: Chronology ; Loess ; Palaeosols ; Pedostratigraphic marker horizon ; Southern Germany ; Upper Palaeolithic ; Weichselian Pleniglacial ; Weathering ; Soils ; chronology ; chronostratigraphy ; interglacial ; Last Glacial ; loess ; paleoenvironment ; paleosol ; radiocarbon dating ; reconstruction ; soil horizon ; Weichselian ; anatomy ; correlation ; data processing ; soil analysis ; Baden-Wurttemberg ; Germany ; Nussloch
英文摘要: The loess section of Nussloch in southwestern Germany is a key profile for the reconstruction of the terrestrial palaeo-environment of central Europe at the time of the Last Glacial and Interglacial. Recently, the significance of the site for palaeo-environmental and geoarchaeological research increased additionally, with the discovery of unique Palaeolithic cultural remains from anatomically and culturally modern humans that invaded southwestern Germany during the Weichselian (Würmian) Pleniglacial period. At Nussloch, a chrono-stratigraphical key position is taken by a Middle Pleniglacial Cambisol remain which, under the designation Lohne Soil, serves as an important pedostratigraphic marker horizon for the greater area. Repeatedly, Greenland interstadial (GIS) 8 was suggested as a likely period of soil formation for the Lohne Soil. This interpretation is yet not justified on the basis of published chronometric data. Critical assessment of the data points to a later period of soil formation, likely during GIS7 to GIS5. This conclusion is supported by a new set of radiocarbon ages for the Nussloch site which are presented here for the first time. Consequences of a revised chronology for correlations of Pleniglacial Cryosols below and above the Lohne Soil with Greenland interstadials are discussed. The implications are important for European loess research as the Nussloch section serves as a reference base for loess sections throughout Europe. © 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/60761
Appears in Collections:过去全球变化的重建

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作者单位: Geographisches Institut, Universität Heidelberg, Im Neuenheimer Feld 348, D-69120 Heidelberg, Germany; Regierungspräsidium Stuttgart, Landesamt für Denkmalpflege, Berliner Str. 12, D-73728 Esslingen, Germany

Recommended Citation:
Kadereit A.,Kind C.-J.,Wagner G.A.. The chronological position of the Lohne Soil in the Nussloch loess section - re-evaluation for a European loess-marker horizon[J]. Quaternary Science Reviews,2013-01-01,59
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