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Par Collection Par Auteur- THORNTON, I. W. B., (Editeur scientifique) (4)
- WHITTAKER, R. J. (2)
- ASQUITH, N. M. (1)
- BUSH, M. B. (1)
- HILL, J. (1)
- MIRMANTO, E. (1)
- RICHARDS, K. (1)
- WALDEN, J. (1)
- WHITTAKER, R. J. (1)
- PARTOMIHARDJO, T. (1)
- SELF, S. (1)
- 1992 (4)
- Analyse des groupes ; Analyse multivariée ; Biogéographie ; Cendre volcanique ; Dynamique de la végétation ; Eruption volcanique ; Géochimie ; Ile ; Indonésie ; Propriété du sol ; Pyroclastique ; Sol ; Stratigraphie ; Volcanisme (1)
- Biogeography ; Cluster analysis ; Geochemistry ; Indonesia ; Island ; Multivariate analysis ; Pyroclastic ; Soil ; Soil properties ; Stratigraphy ; Vegetation dynamics ; Volcanic ash ; Volcanic eruption ; Volcanism (1)
- Biogeography ; Ecology ; Fauna ; Forest ; Indonesia ; Island ; Population dynamics ; Vegetation ; Volcanic eruption ; Volcanism (1)
- Biogeography ; Ecosystem ; Indonesia ; Island ; Population dynamics ; Vegetation ; Volcanic eruption ; Volcanism (1)
- Biogéographie ; Dynamique des populations ; Ecologie ; Eruption volcanique ; Faune ; Forêt ; Ile ; Indonésie ; Volcanisme ; Végétation (1)
- Biogéographie ; Dynamique des populations ; Ecosystème ; Eruption volcanique ; Ile ; Indonésie ; Volcanisme ; Végétation (1)
- Eruption volcanique ; Géochimie ; Indonésie ; Magma ; Pyroclastique ; Tsunami ; Volcanisme (1)
- Geochemistry ; Indonesia ; Magma ; Pyroclastic ; Tsunami ; Volcanic eruption ; Volcanism (1)
- Krakatau. A century of change (4)
- Anak Krakatau's vegetation and flora circa 1991, with observations on a decade of development and change (1)
- Ecological aspects of plant colonisation of the Krakatau Islands (1)
- Krakatau revisited : the course of events and interpretation of the 1883 eruption (1)
- Post-1883 ash fall on Panjang and Sertung and its ecological impact (1)
- , with the aim of assessing spatial variation in ash fall history across Panjang and Sertung. Most sites on both islands showed evidence of a number of distinct ash-falls in both the early 1930s and 1952/53 periods, of a highly disruptive nature. Sites nearest
- that the cause of both is most likely related to the sudden emission of large pulses of magma that led to formation of the Krakatau ignimbrite.
- The major aims of this contribution are to describe the state of vegetation and flora in the period 1989 to 1991 and to re-assess the development of both over the last ten years in comparison with data from earlier surveys. In addition, the paper
- Species assemblage data from the Krakatau Islands are presented for the period 1883 to 1989. With the exception of the strand-line, no component of the Krakatau flora or vegetation has yet approached a stable composition. Both floral and faunal