Lithology and pollen record of 4 profiles from the Bavaria, southern Germany

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1. Verfasser: Hahne, Jürgen
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Sprache:en
Veröffentlicht: PANGAEA 2009
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author Hahne, Jürgen
author_facet Hahne, Jürgen
collection Datos científicos de ciencias marinas y ambientales
contents Palynological investigations of sediments from northern Bavaria (Rhön, Grabfeld, Lange Berge) reveal the Late Glacial and Postglacial history of the regional vegetation. The older sedirnents were found in the Rhön (Schwarzes Moor) and date back into the Bölling Period. At the end of that period pine spread into the Grabfeld. In both areas Lacher Tuff has been found. A radiocarbon date of 10,300 BP was found for the Late Glacial - Postglacial transition and one of 9300 BP for the Preboreal - Boreal transition. Hazel reached its highest values in the Rhön around 7,400 BP. During the Atlanticum a deciduous mixed oak forest covered the Rhön and Grabfeld regions. Beech dominated since the Subatlanticum. In the Lange Berge region, however, a mixed forest with Fagus, Picea, Pinus and Abies developed. In the Rhön first anthropogenic influence was found during the Latene Period. The boundary between zone IX and X has been dated at 820 A.D., and the start of extensive forest clearances at 1000 A. D. A culmination of landuse was found for the Medieval Period. At the end of that period however the Rhön was deserted. New forest clearances started around 1500 A.D., but were interrupted by the 'Thirty Years War'. Afterwards the Rhön got its present appearance.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_726009
institution PANGAEA
language en
publishDate 2009
publisher PANGAEA
record_format pangaea
spellingShingle Lithology and pollen record of 4 profiles from the Bavaria, southern Germany
Hahne, Jürgen
Beug_pollen-archive; Moor bei Rappershausen, Grabfeld; PROFILE; Profile sampling; RAPERSH1; RAPERSH2; Rappershausen-1; Rappershausen-2; Rottenburg; Rottenburg, NO Coburg; Sampling on land; SchwarzesMoor; Schwarzes Moor/Rhön
Palynological investigations of sediments from northern Bavaria (Rhön, Grabfeld, Lange Berge) reveal the Late Glacial and Postglacial history of the regional vegetation. The older sedirnents were found in the Rhön (Schwarzes Moor) and date back into the Bölling Period. At the end of that period pine spread into the Grabfeld. In both areas Lacher Tuff has been found. A radiocarbon date of 10,300 BP was found for the Late Glacial - Postglacial transition and one of 9300 BP for the Preboreal - Boreal transition. Hazel reached its highest values in the Rhön around 7,400 BP. During the Atlanticum a deciduous mixed oak forest covered the Rhön and Grabfeld regions. Beech dominated since the Subatlanticum. In the Lange Berge region, however, a mixed forest with Fagus, Picea, Pinus and Abies developed. In the Rhön first anthropogenic influence was found during the Latene Period. The boundary between zone IX and X has been dated at 820 A.D., and the start of extensive forest clearances at 1000 A. D. A culmination of landuse was found for the Medieval Period. At the end of that period however the Rhön was deserted. New forest clearances started around 1500 A.D., but were interrupted by the 'Thirty Years War'. Afterwards the Rhön got its present appearance.
title Lithology and pollen record of 4 profiles from the Bavaria, southern Germany
topic Beug_pollen-archive; Moor bei Rappershausen, Grabfeld; PROFILE; Profile sampling; RAPERSH1; RAPERSH2; Rappershausen-1; Rappershausen-2; Rottenburg; Rottenburg, NO Coburg; Sampling on land; SchwarzesMoor; Schwarzes Moor/Rhön
url https://doi.org/10.1594/PANGAEA.726009