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The loess-palaeosol sequence of Datthausen, SW Germany: Characteristics, chronology, and implications for the use of the Lohne Soil as a marker soil.
by
Sauer
,
D
.
,
Kadereit, A.
,
Kühn, P.
,
Kosel, M.L.
,
Miller, C.E.
,
Shinonaga, T.
,
Kreutzer, S.
,
Herrmann, L.
,
Fleck, W.
,
Starkovich, B.M.
,
Stahr, K.
Published in
CATENA
(2016)
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Related Subjects
Chronometric marker
Loess-palaeosol sequence
Lohne soil
MIS3/MIS2 boundary
Middle to Upper Pleniglacial boundary
Pedostratigraphic marker
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