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(Article of periodic en Anglais - 1984)

Document title

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

Authors(s) and Affiliation(s)

ARIAS C. ; BIGAZZI G. ; BONADONNA F. ; BRUNNACKER K. ; URBAN B. ;

Abstract

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.

Source

Article of periodic

published at : Quaternary science reviews Oxford

Editor :

Millesime : 1984, vol. 3, no1 [pp. 73-89]

Bibliographic references : 26 réf.

Language

Anglais

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