Vegetation recovery patterns in early volcanic succession [at Japanese island]

Permanent plots were monitored from 1983 to the present on Mount Usu after the eruptions of 1977-78 which destroyed the pre-eruption vegetation by 1-3 m thick accumulations of ash and pumice in order to clarify the processes and mechanisms of succession. Until now, 163 species were recorded in the s...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of plant research 1995-06, Vol.108 (1090), p.241-248
1. Verfasser: Tsuyuzaki, S. (Niigata Univ. (Japan))
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Permanent plots were monitored from 1983 to the present on Mount Usu after the eruptions of 1977-78 which destroyed the pre-eruption vegetation by 1-3 m thick accumulations of ash and pumice in order to clarify the processes and mechanisms of succession. Until now, 163 species were recorded in the summit area. Most of these species were derived from vegetative reproduction throughout the volcanic deposits. Vegetative reproduction plays a major role on increases in cover. Although long-distance seed-dispersal species could immigrate to the crater basin, their cover increase was slow. Seedbank species only established in gullies where the original topsoil was exposed by erosion. Most annuais were supplied by the seedbank in the original topsoil and woody species originated via immigration, suggesting that the source greatly determines the species composition of establishing vegetation. Annual seedlings showed low survival, while overwintering perennial seedlings steadily established. Ground surface movements strongly restricted increases in plant cover and the distance from source vegetation was the principal determinant of plant density. Due to differences in disturbance intensity, successional rates were higher in the stable substrates outside gullies and lower on the exposed original topsoil in some gullies.
ISSN:0918-9440
1618-0860
DOI:10.1007/bf02344349