Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)

A Pliocene alluvial fan sequence of soils and sediments with 24 fossil soils in the northeastern part of the Granada Basin was investigated. The reddish brown to red soils and the (soil-)sediments substantiate a multiple alternation of sedimentation and (differently intensive) soil formation. Accumu...

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Main Authors: N. Günster, A. Skowronek, L. Pfeiffer, S. Stephan, M. Veerhoff
Format: Article
Language:deu
Published: Copernicus Publications 1998-01-01
Series:Eiszeitalter und Gegenwart
Online Access:https://www.eg-quaternary-sci-j.net/48/57/1998/egqsj-48-57-1998.pdf
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author N. Günster
A. Skowronek
L. Pfeiffer
S. Stephan
M. Veerhoff
author_facet N. Günster
A. Skowronek
L. Pfeiffer
S. Stephan
M. Veerhoff
author_sort N. Günster
collection DOAJ
description A Pliocene alluvial fan sequence of soils and sediments with 24 fossil soils in the northeastern part of the Granada Basin was investigated. The reddish brown to red soils and the (soil-)sediments substantiate a multiple alternation of sedimentation and (differently intensive) soil formation. Accumulation took place during dry and morphodynamic active periods without vegetation cover and soil formation during wet and morphodynamic stable periods with vegetation. Hence a high number of climatic changes has to he postulated to this - still not defined – part of the Pliocene.
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spelling doaj.art-ea67f82a48de4dd5995ad7e4a249351d2022-12-22T01:34:19ZdeuCopernicus PublicationsEiszeitalter und Gegenwart0424-71162199-90901998-01-0148576610.3285/eg.48.1.06Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)N. GünsterA. SkowronekL. PfeifferS. StephanM. VeerhoffA Pliocene alluvial fan sequence of soils and sediments with 24 fossil soils in the northeastern part of the Granada Basin was investigated. The reddish brown to red soils and the (soil-)sediments substantiate a multiple alternation of sedimentation and (differently intensive) soil formation. Accumulation took place during dry and morphodynamic active periods without vegetation cover and soil formation during wet and morphodynamic stable periods with vegetation. Hence a high number of climatic changes has to he postulated to this - still not defined – part of the Pliocene.https://www.eg-quaternary-sci-j.net/48/57/1998/egqsj-48-57-1998.pdf
spellingShingle N. Günster
A. Skowronek
L. Pfeiffer
S. Stephan
M. Veerhoff
Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
Eiszeitalter und Gegenwart
title Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
title_full Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
title_fullStr Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
title_full_unstemmed Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
title_short Zur Paläopedologie pliozäner Schwemmfächersedimente im Becken von Granada (Hochandalusien)
title_sort zur palaopedologie pliozaner schwemmfachersedimente im becken von granada hochandalusien
url https://www.eg-quaternary-sci-j.net/48/57/1998/egqsj-48-57-1998.pdf
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