The loess-palaeosol sequence of Datthausen, SW Germany: Characteristics, chronology, and implications for the use of the Lohne Soil as a marker soil
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- 作者：Daniela Sauera ; daniela.sauer@geo.uni-goettingen.de" class="auth_mail" title="E-mail the corresponding author ; Annette Kadereitb ; Peter Kü ; hnc ; Michael Kö ; seld ; Christopher E. Millere ; Taeko Shinonagaf ; Sebastian Kreutzerg ; Ludger Herrmannh ; Wolfgang Fleckd ; Britt M. Starkoviche ; i ; Karl Stahrh
- 关键词：Loess-palaeosol sequence ; Middle to Upper Pleniglacial boundary ; MIS3/MIS2 boundary ; Lohne soil ; Pedostratigraphic marker ; Chronometric marker
- 刊名：Catena
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：146
- 期：Complete
- 页码：10-29
- 全文大小：4655 K
文摘
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Presentation of new loess-palaeosol sequence on upper Danube in SW-Germany
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Middle/Upper Pleniglacial (MPG/UPG) and MIS3/MIS2 boundaries match in this profile.
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Palaeosol with Lohne Soil habitus younger than at Schwalbenberg II and Nussloch
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Loess-accumulation rates and topographic position control soil formation.
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Lohne Soil is suitable as pedostratigraphic marker but not as chronometric marker.