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Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy)

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Standard

Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy). / Arias, Claudio; Bigazzi, Giulio; Bonadonna, Francescopaolo et al.
in: Quaternary Science Reviews, Jahrgang 3, Nr. 1, 1984, S. 73-89.

Publikation: Beiträge in Zeitschriften › Zeitschriftenaufsätze › Forschung › begutachtet

Harvard

Arias, C, Bigazzi, G, Bonadonna, F, Brunnacker, K & Urban, B 1984, 'Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy)', Quaternary Science Reviews, Jg. 3, Nr. 1, S. 73-89. https://doi.org/10.1016/0277-3791(84)90005-2

APA

Arias, C., Bigazzi, G., Bonadonna, F., Brunnacker, K., & Urban, B. (1984). Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy). Quaternary Science Reviews, 3(1), 73-89. https://doi.org/10.1016/0277-3791(84)90005-2

Vancouver

Arias C, Bigazzi G, Bonadonna F, Brunnacker K, Urban B. Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy). Quaternary Science Reviews. 1984;3(1):73-89. doi: 10.1016/0277-3791(84)90005-2

Bibtex

@article{0f132e6362cd4513a6551a3d49078638,
title = "Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy)",
abstract = "Biostratigraphic and palaeomagnetic research has been carried out on selected profiles in North-Western Germany and Central Italy in order to correlate Plio-Pleistocene sections. Around the R{\'e}union 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. Deposits older than the R{\'e}union subzone have not been found in the Valle Ricca. In the Lower Rhine Basin, on the other hand, the Gauss-Matuyama boundary is located between the uppermost Pliocene, the Reuverian C and the Praetiglian.",
keywords = "Ecosystems Research",
author = "Claudio Arias and Giulio Bigazzi and Francescopaolo Bonadonna and Karl Brunnacker and Brigitte Urban",
year = "1984",
doi = "10.1016/0277-3791(84)90005-2",
language = "English",
volume = "3",
pages = "73--89",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier Ltd",
number = "1",

}

RIS

TY - JOUR

T1 - Correlation of Plio-Pleistocene deposits of the Lower Rhine Basin (North-West Germany) and the Valle Ricca pits (Central Italy)

AU - Arias, Claudio

AU - Bigazzi, Giulio

AU - Bonadonna, Francescopaolo

AU - Brunnacker, Karl

AU - Urban, Brigitte

PY - 1984

Y1 - 1984

N2 - Biostratigraphic and palaeomagnetic research has been carried out on selected profiles in North-Western Germany and Central Italy in order to correlate Plio-Pleistocene sections. Around the Réunion 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. Deposits older than the Réunion subzone have not been found in the Valle Ricca. In the Lower Rhine Basin, on the other hand, the Gauss-Matuyama boundary is located between the uppermost Pliocene, the Reuverian C and the Praetiglian.

AB - Biostratigraphic and palaeomagnetic research has been carried out on selected profiles in North-Western Germany and Central Italy in order to correlate Plio-Pleistocene sections. Around the Réunion 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. Deposits older than the Réunion subzone have not been found in the Valle Ricca. In the Lower Rhine Basin, on the other hand, the Gauss-Matuyama boundary is located between the uppermost Pliocene, the Reuverian C and the Praetiglian.

KW - Ecosystems Research

UR - http://www.scopus.com/inward/record.url?scp=0021620027&partnerID=8YFLogxK

U2 - 10.1016/0277-3791(84)90005-2

DO - 10.1016/0277-3791(84)90005-2

M3 - Journal articles

AN - SCOPUS:0021620027

VL - 3

SP - 73

EP - 89

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

IS - 1

ER -

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