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 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

Tonga has a small open economy with squash, coconuts and vanilla the main export crops that make up two thirds of total exports. A high proportion of food is imported, mainly from New Zealand. Remittances are important to the economy, as is tourism. Private sector development is emphasized in its Strategic Development Plan and there is a reasonably sound basic infrastructure and well-developed social services. Fisheries and tourism are considered as having the most potential for further economic growth.

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

Environment The Solomon Islands is part to various treaties and conventions related to environmental protection, including the United Nations Framework Convention on Climate Change (UNFCCC) and the Kyoto Protocol. A communication to UNFCCC, including greenhouse gas emissions and vulnerability to climate change, is expected to be submitted during 2004.

Available online|This report is based on data gathered by a PIREP team consisting of John Korinihone, Morgan Wairiu, John Vos and Peter Johnston

Call Number: 333.79415953 JOH (EL)

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

PNG has two distinct economies: i) a modem, cash economy dominated by mining, timber, gas and oil. and agricultural expoits (coffee, cocoa, tea. oil palm and copra): and ii) the traditional subsistence economy and semi-subsistence fanning, with most villages producing little or no surplus for trading. Economic growth has varied considerably but averaged less than 3% annually in real terms since independence in 1975. with per capita income less in 2002 than at Independence. The government expects real growth to average 2.1% from 2003-2008.

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

Palau lias an equatorial, marine environment. No cyclones have been recorded though near passages are not unusual when high waves can be a problem. Palau has a strong program for preserving the environment, particularly that of the major tourist attractions including the Rock Islands and the reefs where some of the best diving in the world is found. Marine biodiversity is high and land biodiversity moderate. Strict USA

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

Environmental issues have a high priority. The people of Nine have taken positive action to maintain the environment for future generations. The low population density has allowed large areas of the island's interior to remain as natural forests and this natural state has become a tourist attraction along with the exotic coral formations, caves and other natural attractions of the island. In general water quality and air quality are very good. Periods of drought occur that can cause loss of crops and hardship for residents.

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

The climate is equatorial marine in nature. There are 110 cyclones though rainfall is cyclic and periodic droughts are a serious problem with one year having a recorded rainfall of only 280 nun. The land biodiversity is limited with only

 Secretariat of the Pacific Regional Environment Programme (SPREP),  Pacific Islands Renewable Energy Project (PIREP)

The Republic of the Marshall Islands consists of two groups of atolls and islands: Ralik in the west and Ratak to the east, within a rectangle extending 1150 km north-south and 1300 km east- west. about 3200 kilometers from Honolulu and Tokyo. Twenty-two of 29 atolls, and four of the five small raised coral islands are inhabited. The islands are typically several km long and rarely over 200 meters in width.

 University of Guam

This report is an assessment of the status of coral reef ecosystems in Guam from 2002 to 2004. Data on coral reef ecosystems were synthesized from assessments and monitoring programs conducted by local and federal organizations. Included in the report are assessments of the environmental and anthropogenic stressors affecting coral reefs, information on data gathering activities and the condition of coral reef ecosystem resources, a description of current conservation management activities, and overall conclusions and recom-

 Pacific Islands Forum Secretariat

With these decisions in mind, the Pacific Plan identifies initiatives within an implementation framework that extends to 10 years. Some of this work is already underway. The Plan provides a framework for effective and enhanced engagement
between Forum countries and Pacific territories and with their non-state actors and development partners. It does not limit the sovereign right of Forum Member countries to determine their own national goals and priorities. It may also guide but does not restrict bilateral development programmes and activities.

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 SPREP Pacific Environment Information Network (PEIN)

Following the United Nations Conference on Environment and Development, the governments of the Asian and Pacific region have, within certain limitations and constraints, drawn up and implemented national strategies, action plans and programmes to attain the objectives of sustainable development. The international, regional and subregional organizations have developed their respective action programmes to assist the governments in their efforts. There were also some common problems and transboundary issues that lent themselves to action at the regional and subregional levels.

 Smithsonian Institution

The colonization of the lagoon by coral reef fish larvae was compared between two islands of French Polynesia, the atoll of Rangiroa and the high volcanic island of Moorea. In both cases the larval flux coming into the lagoon followed a daily cycle.

 Smithsonian Institution

Ten caves in the makatea limestone of Mangaia, Cook Islands were explored and mapped, totalling over 3.7 km of passage. Of these, there was an apparent grouping by elevation that corresponds with previously described sea-level terraces in the makatea. Four caves have major level sections 10-20 m above sea-level, corresponding with a 14.5 m Pleistocene terrace. The high dimensions of these caves indicate downcutting during

 Smithsonian Institution

The Republic of the Marshall Islands requested a natural and cultural biodiversity survey of 6 northern atolls (Bok-ak, Pikaar, Toke, Wotto, Rondik, Adkup) and one reef island (Jemo) which was accomplished over 17 days in September 1988. This report covers the results of the survey of the reefs and corals during the expedition. Ninety-five marine sites were snorkeled and the shorelines of all island were surveyed during the

 Smithsonian Institution

The recorded flora of the raised phosphatic limestone island of Nauru in the equatorial Pacific Ocean consists of approximately 493 species. Only 59 are possibly indigenous, none of which are endemic. The balance is composed of ornamentals, weedy exotics, food plants, and a limited number of other useful cultigens. Twelve of the recorded species are either extinct or were never successfully established on Nauru.

 Smithsonian Institution

This paper lists the vascular flora of the three atolls (Canton, Gardner, Hull) and five small islands (Birnie, Enderbury, McKean, Phoenix, Sydney) of the Phoenix Group,
located in the arid equatorial belt of the Central Pacific, based on extensive collections made in 1973 and 1975 and on previous records and collections. The flora includes 87
species in 36 families. Only 28 of the species (32%) are considered native. A further 60 species have been recorded in the literature, many of them deliberate introductions which

 Smithsonian Institution

This paper describes the channels known as hoa which are characteristic of atoll land rims and of some islands on barrier reefs, where they often dissect previously more continuous reef-top sediment accumulations and conglomerate platforms. They are

 Smithsonian Institution

Nukutipipi atoll (5 km2), of volcanic origin 16-17 million years old on the Pitcairn (hot spot) Hereheretue line, presents a land flora and fauna of low diversity but with a Pisonia forest and hundreds of resident red-tailed tropic birds. Nukutipipi suffered from the 1983 hurricanes : destruction of vegetation and motu as well as sand lagoon mollusc populations. The north and south rims present original geomorphological structures.

 Smithsonian DC

Washington Island (Teraina) in the Northern Line Islands is a small atoll with a land area of 14.2 sq. km. situated at 4° 4 3'N, 160° 25'W. The Northern Line Island archipelago is comprised of four islands alined on an axis which runs from Christmas Island, just north of the equator, to Palmyra Island in the northwest (Figure 1). Washington Island, and its nearest neighbor Fanning Island, about 150 kilometers to the south east, have had close economic and social ties for most of their recent history.

 Smithsonian Institution

During the period 1958-1964, the authors undertook soil and vegetation studies in the northern Marshall Islands as part of the University of Washington Radiation Biology Laboratory surveillance team. This team was responsible for monitoring levels of radiation in various components of the island environment and any effects on plant and animal life. The authors of this report were charged with the soils and vegetation components but assisted with collections in the aquatic ecosystems and some food plant materials.

 Smithsonian Institution

Phosphatic limestones and associated soils occur on eight of the nine islands of Tuvalu, central Pacific. Deposits range from gram-size to >500,000 tons. Carbonate hydroxyapatite, dahllite, forms crustose cement about calcareous bioclasts which it sometimes replaces. Precise genetic relationship of rock to soil is unclear. Consolidated rock occurs as hardpan within phosphatic soil profiles, with unconsolidated phosphatic layers above and below. Phosphatization has occurred either as a continuous or episodic process within the vadose zone for at least 4000 years.