Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 27-58 |
| Seitenumfang | 32 |
| Fachzeitschrift | Annali di Botanica |
| Jahrgang | 55 |
| Publikationsstatus | Veröffentlicht - 1997 |
Abstract
When studying the natural development in the evolution of beechwood forests in Central Europe after the last glaciation, it is necessary to look at the warm periods prior to the last Weichselian glaciation. The Eem interglacial period has already been studied in great detail in Europe; it is evidend with similar climatic conditions as the current Holocene. At that time nearly all of Europe was more or less completely covered with forests. As laminated sediments and datings indicate, the Eem interglacial period lasted from approximately 125000 to 113000 years before today. The types of trees were generally the same as those of the present, except for the beech (Fagus) which was missing due to its delayed re-migration and was replaced by the hornbeam (Carpinus). It was not until the present time following the glaciation-periods that Fagus sylvatica could be found again widespread throughout the woodland vegetation covering Central Europe. The Holocene expansion and re-colonisation of Fagus sylvatica from its refuges during the glacial periods will be described in great detail, based on the most recent pollen analytic proofs.
ASJC Scopus Sachgebiete
- Agrar- und Biowissenschaften (insg.)
- Pflanzenkunde
Zitieren
- Standard
- Harvard
- Apa
- Vancouver
- BibTex
- RIS
in: Annali di Botanica, Jahrgang 55, 1997, S. 27-58.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Invasion of beech and e stablishment of beech forests in Europe
AU - Pott, Richard
PY - 1997
Y1 - 1997
N2 - When studying the natural development in the evolution of beechwood forests in Central Europe after the last glaciation, it is necessary to look at the warm periods prior to the last Weichselian glaciation. The Eem interglacial period has already been studied in great detail in Europe; it is evidend with similar climatic conditions as the current Holocene. At that time nearly all of Europe was more or less completely covered with forests. As laminated sediments and datings indicate, the Eem interglacial period lasted from approximately 125000 to 113000 years before today. The types of trees were generally the same as those of the present, except for the beech (Fagus) which was missing due to its delayed re-migration and was replaced by the hornbeam (Carpinus). It was not until the present time following the glaciation-periods that Fagus sylvatica could be found again widespread throughout the woodland vegetation covering Central Europe. The Holocene expansion and re-colonisation of Fagus sylvatica from its refuges during the glacial periods will be described in great detail, based on the most recent pollen analytic proofs.
AB - When studying the natural development in the evolution of beechwood forests in Central Europe after the last glaciation, it is necessary to look at the warm periods prior to the last Weichselian glaciation. The Eem interglacial period has already been studied in great detail in Europe; it is evidend with similar climatic conditions as the current Holocene. At that time nearly all of Europe was more or less completely covered with forests. As laminated sediments and datings indicate, the Eem interglacial period lasted from approximately 125000 to 113000 years before today. The types of trees were generally the same as those of the present, except for the beech (Fagus) which was missing due to its delayed re-migration and was replaced by the hornbeam (Carpinus). It was not until the present time following the glaciation-periods that Fagus sylvatica could be found again widespread throughout the woodland vegetation covering Central Europe. The Holocene expansion and re-colonisation of Fagus sylvatica from its refuges during the glacial periods will be described in great detail, based on the most recent pollen analytic proofs.
KW - Beech-woods
KW - Fagus sylvatica
KW - Holocene expansion
KW - Pleistocene refuges
UR - http://www.scopus.com/inward/record.url?scp=0003175865&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0003175865
VL - 55
SP - 27
EP - 58
JO - Annali di Botanica
JF - Annali di Botanica
SN - 0365-0812
ER -