Biber-Danube interglacial
The Biber-Danube interglacial (
erosion phase, that followed the Biber and preceded the Danube glacial. Thus, it represented the gap between the depositions that are ascribed to the two cold periods.[1]
Modern research has found that both Biber and Danube correspond to many glacial cycles, as identified by approximately 80
marine isotope stages (MIS), making the term Biber-Danube superfluous. The term is not used in the 2016 version of the detailed stratigraphic table by the German Stratigraphic Commission.[2]
See also
References
The cold and warm periods of the Quaternary in the Alpine region | ||
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