Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß

Prerequisite for the estimation of age and paleoecological interpretation of paleosols in loess is the cognizance of relief and landscape position. Examples from Southern Germany show that already by this properties (like hydromorphy or a change of soil depth and humus contents) can be explained tha...

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Main Author: K. E. Bleich
Format: Article
Language:deu
Published: Copernicus Publications 1998-01-01
Series:Eiszeitalter und Gegenwart
Online Access:https://www.eg-quaternary-sci-j.net/48/50/1998/egqsj-48-50-1998.pdf
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author K. E. Bleich
author_facet K. E. Bleich
author_sort K. E. Bleich
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description Prerequisite for the estimation of age and paleoecological interpretation of paleosols in loess is the cognizance of relief and landscape position. Examples from Southern Germany show that already by this properties (like hydromorphy or a change of soil depth and humus contents) can be explained that, in ignoring the situation, were used as criteria for character and length of climatic influences. For the comparison of loess/pa-leosol sequences, the quantitative determination of intensity and extent of soil formation (in kg per m²) concerning suitable fossil and recent soils of the same landscape is reasonable. This requires the limitation on completely preserved soils in plateau position, but does not necessarily imply the imagination of a monotypically developed soil-landscape. These soils, too, have been alternated by periglacial features. The different importance of soil horizons for the reconstruction of the paleoclimate is put out finally.
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spelling doaj.art-97c24a8a34f1451f9e4c1e74c0b382922022-12-21T18:10:03ZdeuCopernicus PublicationsEiszeitalter und Gegenwart0424-71162199-90901998-01-0148505610.3285/eg.48.1.05Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) LößK. E. BleichPrerequisite for the estimation of age and paleoecological interpretation of paleosols in loess is the cognizance of relief and landscape position. Examples from Southern Germany show that already by this properties (like hydromorphy or a change of soil depth and humus contents) can be explained that, in ignoring the situation, were used as criteria for character and length of climatic influences. For the comparison of loess/pa-leosol sequences, the quantitative determination of intensity and extent of soil formation (in kg per m²) concerning suitable fossil and recent soils of the same landscape is reasonable. This requires the limitation on completely preserved soils in plateau position, but does not necessarily imply the imagination of a monotypically developed soil-landscape. These soils, too, have been alternated by periglacial features. The different importance of soil horizons for the reconstruction of the paleoclimate is put out finally.https://www.eg-quaternary-sci-j.net/48/50/1998/egqsj-48-50-1998.pdf
spellingShingle K. E. Bleich
Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
Eiszeitalter und Gegenwart
title Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
title_full Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
title_fullStr Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
title_full_unstemmed Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
title_short Zur Deutung und Bedeutung von Paläoböden im (süddeutschen) Löß
title_sort zur deutung und bedeutung von palaoboden im suddeutschen loss
url https://www.eg-quaternary-sci-j.net/48/50/1998/egqsj-48-50-1998.pdf
work_keys_str_mv AT kebleich zurdeutungundbedeutungvonpalaobodenimsuddeutschenloß