87 Stratigraphy and Geochronology (Posters)
Wednesday, 30 July 2003
1:30 PM - 4:30 PM
NEW DATING OF EUROPEAN ICE SHEETS IMPROVES THE QUATERNARY OF THE RHINE REGION
Paper number: 87-17
Program: Technical Sessions
Time: 1:30 PM – 4:30 PM
Authors
Abstract
Reconstruction of the settlement enables the election of a core without severe sediment disturbances: V28-239. Its record, "based on oxygen isotope data from marine fossils that reflect the size of continental ice sheets" (SCHRAG 2002:23) is proportional to the known sequence of European ice sheets.
An application to the Rhine region shows more details: The largest sheets touched the Lower Rhine in the stages 22 (850 kyr), 16 (550 kyr) and 12 (300 kyr). In different stages ice sheets had different size and duration. Crustal movement, river erosion and volcanism were mobilized most in the stages 22 and 16, less in 12, still less in the other. Overridden sheets are distinguishable.
SHACKLETON NJ, OPDYKE ND (1973) Quaternary Research 3:39-55 IMBRIE J, HAYS JD, MARTINSON DG et al. (1984) NATO ASI Series C Vol. 126 pp 269-305 SCHRAG DP (2000) Nature 404:23 THOME KN (1997) Springer Berlin Heidelberg New York ISBN 3-540-62932-7 pp 25-26, 41-55, 69-111, 188-209 --(2000) Decheniana (Bonn) 153:241-259 ISSN 0366-872 X --(2001) DGG14:211-212 ISSN 1616-0606, ISBN 3-932537-14-9 --(2002a) Terra Nostra 2002/6:364-374 DEUQUA ISSN 0946-8978 --(2002b) GeoArchaeoRhein 4 Münster ISBN 3-8258-6009-4