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Correlation of Plio-Pleistocene deposits of the lower Rhine basin (north-west Germany) and the Valle Ricca pits (central Italy)

Auteurs :
ARIAS, C.
BIGAZZI, G.
BONADONNA, F.
BRUNNACKER, K.
URBAN, B.

Description :
Around the Reunion subchronozone, vegetation in the Valle Ricca was dominated by a mountain forest type pointing to cool climatic conditions. In the Lower Rhine Basin vegetation had a slightly warmer character, but was also dominated strongly by a mountain type of forest vegetation, characteristic of cooler summers and higher precipitation than at present. Two warmer periods have been determined in the Central Italian profiles| the youngest around the Olduvai reversal, should correspond to the youngest Tiglian beds of the Lower Rhine Basin.


Type de document :
Article de périodique

Source :
Quaternary science reviews Oxford, 1984, vol. 3, n°. 1, p. 73-89, Références bibliographiques : 26 réf.

Date :
1984

Langue :
Anglais
Droits :
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