The map shows landcover and vegetation impact of the Hunga Tonga Hunga Haápai volcanic eruption on the Tonga Island group.
While acknowledging their diversity, the IPCC Third
Assessment Report (TAR) also noted that small island states
share many similarities (e.g., physical size, proneness to natural disasters and climate extremes, extreme openness of their economies, low adaptive capacity) that enhance their vulnerability and reduce their resilience to climate variability and change.
Available online|(* NB these materials are also available on the workshop CDROM deposited with the IRC NBSAP workshop Nadi, Feb 2009)
Call Number: [EL]
The main topographical features of Samoa are rugged mountains of volcanic origin, surrounded by flat and rolling coastal plains. All the islands of Samoa were formed by volcanic activity. Savai'i is regarded as still volcanically active with its most recent eruption producing lava flows between 1905 and 1911. A large percentage of Samoan soils are porous, shallow and clay in texture.
Also available online|A PICCAP-GEF funded project
Call Number: 551.6 UNI [EL],302.2 GOV,VF 2682,INT-CON
Physical Description: xi, 50 p. ; 29 cm
The designation of geographical entities in this book, and the presentation of the material, do not imply
the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country,
territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries.
A contribution to the global invasive species programme
Call Number: 628.16 CLA [EL],SPE
ISBN/ISSN: 2-8317-0548-7
Physical Description: xvi, 138 p. ; 29 cm
What are the decapod crustacea known from French Polynesia? The answer to this, apparently simple question, would be very helpful for determinating the species collected during ecological studies. Moreover, from a biogeographical point of view, a check list of the species reaching this area, at the eastern limit of the Indo-West Pacific province, would be very interesting.
The islands of French Polynesia are scattered throughout a considerable oceanic area located on the eastern boundary of the Indo-Pacific Province. This area stretches from 134°28' W (Temoe Island) to 154°40' W longitude (Stilly Island), and from 7°50' S (Motu one Island) to 27°36' S latitude (Rapa Island). Out of the 118 islands constituting French Polynesia, 35 are high volcanic islands and 83 are low-relief islands or atolls. Altogether, the territory of French Polynesia represents an area of 4000 km2 of dry land, 12,000 km2 of lagoonal water and a huge
Matter and energy budgets for coral reefs, their components, and the world around them can, do, and must balance in a theorical context (Smith and Kinsey, 1988). In this paper, we will try to
establish nitrogen, phosphorus and silica budgets between ocean and lagoon waters of Tikehau atoll in the purpose to learn more about the functioning of coral reef lagoons. Nutrient concentrations (dissolved components and particulate organic matter) were measured in the lagoon and in the surrounding oceanic surface waters between 1983 and 1987.
Available online