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Loess-paleosol sequencesin South Germany were used to reconstruct the evolution ofthe paleoclimate and the chronology of river terraces formation. It was demonstrated that theclassical Riβ glacial period issubdividedintoat least 3 glacial/interglacial cycles. In consequence,it is probable that the Holsteinian t Loess-paleosol sequences in South Germany were used toreconstruct the evolution of the paleoclimate and the chronology of river terraces formation. It wasdemonstrated that the classical Riβ glacial period issubdividedintoatleast3 glacial/interglacialcycles. In consequence, it is probable that the Holsteinian period can be classified as the isotopestage 11.
Loess-paleosol sequences in South Germany were used to reconstruct the evolution of the paleoclimate and the chronology of river terraces formation. It was demonstrated that theclassical Riβ glacial period issubdividedintoat least 3 glacial / interglacial cycles. In consequence, it is probable that the Holsteinian t Loess- paleosol sequences in South Germany were used toreconstruct the evolution of the paleoclimate and the chronology of river terraces formation. It wasdemonstrated that the classical Riβ glacial period issubdividedintoatleast3 glacial / interglacialcycles. In consequence, it is probable that the Holsteinian period can be classified as the isotopestage 11.