Details
| Original language | English |
|---|---|
| Pages (from-to) | 85-103 |
| Number of pages | 19 |
| Journal | PHYTOCOENOLOGIA |
| Volume | 28 |
| Issue number | 1 |
| Publication status | Published - 24 Mar 1998 |
Abstract
The banks of the lower Havel valley exhibit grassland vegetation zonation comprising communities of the alliances Plantagini-Festucion, Cnidion, Potentillion anserinae, Magnocaricion and Phragmition. Their zonation reflects the frequency and duration of flooding intervals, soil moisture and dryness, as determined by topographic microrelief and pedology. Palynological results show that open habitats have existed there for the last 9000 yrs. The reconstruction of their vegetation can roughly be outlined.
Keywords
- Flood swards, Floodplain reeds, Grasslands in eurysaleutic habitats, Inundation, Landscape history, Open land, Palynology, Semiarid grasslands
ASJC Scopus subject areas
- Agricultural and Biological Sciences(all)
- Plant Science
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In: PHYTOCOENOLOGIA, Vol. 28, No. 1, 24.03.1998, p. 85-103.
Research output: Contribution to journal › Review article › Research › peer review
}
TY - JOUR
T1 - A historical and plant sociological appraisal of floodplain meadows in the lower Havel valley, northeast Germany
AU - Burkart, M.
AU - Küster, H.
AU - Schelski, A.
AU - Pötsch, J.
PY - 1998/3/24
Y1 - 1998/3/24
N2 - The banks of the lower Havel valley exhibit grassland vegetation zonation comprising communities of the alliances Plantagini-Festucion, Cnidion, Potentillion anserinae, Magnocaricion and Phragmition. Their zonation reflects the frequency and duration of flooding intervals, soil moisture and dryness, as determined by topographic microrelief and pedology. Palynological results show that open habitats have existed there for the last 9000 yrs. The reconstruction of their vegetation can roughly be outlined.
AB - The banks of the lower Havel valley exhibit grassland vegetation zonation comprising communities of the alliances Plantagini-Festucion, Cnidion, Potentillion anserinae, Magnocaricion and Phragmition. Their zonation reflects the frequency and duration of flooding intervals, soil moisture and dryness, as determined by topographic microrelief and pedology. Palynological results show that open habitats have existed there for the last 9000 yrs. The reconstruction of their vegetation can roughly be outlined.
KW - Flood swards
KW - Floodplain reeds
KW - Grasslands in eurysaleutic habitats
KW - Inundation
KW - Landscape history
KW - Open land
KW - Palynology
KW - Semiarid grasslands
UR - http://www.scopus.com/inward/record.url?scp=0031872007&partnerID=8YFLogxK
U2 - 10.1127/phyto/28/1998/85
DO - 10.1127/phyto/28/1998/85
M3 - Review article
AN - SCOPUS:0031872007
VL - 28
SP - 85
EP - 103
JO - PHYTOCOENOLOGIA
JF - PHYTOCOENOLOGIA
SN - 0340-269X
IS - 1
ER -