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Fig. 16.7
Comparison between the grain size index (GSI) records in Nussloch (P3 and P4 sequences) (After Rousseau et al.
2007b
) and in Stayky (Rousseau
et al.
2011
). Identification of similar cycles (marked by the
green arrows
) and proposed correlation between the two continental records, supported by IRSL
dates, and pollen characteristics (arboreal pollen (AP) percentages) of the embryonic soils. Correlation between the Greenland GRIP dust record (Johnsen et al.
2001
) and the Nussloch record according to Rousseau et al. (
2007b
), with GIS 8 correlated with the Nussloch Lohner Boden (LB). H3 and H2 correspond to
marine Heinrich events 3 and 2 in the Greenland and European records. G1-7 and IG5-9 are the identified tundra gleys or oxidized horizons in Nussloch (From
Rousseau et al.
2011
)
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