Geomorphologische Lage, Deckschichten und Molluskenführung letztinterglazialer Hochflutlehme im Neckartal (Baden-Württemberg)

Erhard Bibus & Wolfgang Rähle
Terrace relicts from the Riss Period with terminal high-flood loams and superficial layers from the Wurm Period are described for two sites in the Neckar Valley. Due to the mollusc layers and the stage of development of the palaeosoils, one can state that the high-flood loams represent various sections of the last inter-glacial period. The results from palaeontological and palaeopedological analyses show a high degree of correlation. Conclusions, which differ greatly from previous results, have...