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Fiji, New Caledonia, Vanuatu, Solomon Islands, Samoa and Tuvalu report monitoring data for this report, with data from a broad range of observers (scientists, students, dive guides and communities); Nauru has not conducted recent monitoring; Coral cover has changed since the 2004 report due to effective management (positive), or local disturbances, coral predation and natural disasters (negative). Average coral cover at monitoring sites was 45% in Fiji; 27% in New Caledonia; 43% in Samoa; 30% in Solomon Islands; 65% in Tuvalu; and 26% in Vanuatu; Monitoring observations over 9-10 years in Fiji and New Caledonia indicate that these reefs have coped reasonably well with natural and human stressors without catastrophic changes; Densities of edible fish and invertebrates remained generally low (0-10/100m2) in 4 countries reflecting high subsistence and commercial fishing pressure. Butterflyfish, parrotfish, surgeonfish and damselfish were generally most dominant. High densities of parrotfish were reported from 4 countries; Socioeconomic monitoring is conducted in Fiji, Samoa and Solomon Islands. Greatest activity is by the Fiji Locally Marine Managed Area (FLMMA) network at 270 villages across all Fiji provinces. Most households harvest marine resources for subsistence and partially for sale, with few commercial fishers. In Samoa, more people eat canned fish than fresh fish, possibly because of decreased fish stocks in the last 10 years. In the Solomon Islands, some traditional managed systems have collapsed due to poor understanding of fisheries and resource management issues or poor national regulations. Mangrove destruction and greater fishing pressure are reducing family incomes;

The Upper Navua River cuts a narrow gorge through the province of Serua in the central highlands of Viti Levu. The Navua River represents Fiji's third largest freshwater drainage. The gorge is approximately 75 meters deep and varies in width from 5 to 25 meters. The Upper Navua Conservation Area (UNCA) encompasses tins never gorge and approximately 58% of die entire catchment area. Lush highland rainforest surrounds the entire drainage and provides a host of botanical cures diat are utilized by die indigenous peoples of the area. The forest, over and associated biodiversity provide die necessary supplies and food required for daily living and a wide range of ecosystem services to the entire catchment area including flood control for lower areas.

The Apia Catchment is Samoa's selected IWRM demonstration project zone. It accommodates Lake Lanoto'o and its two main tributaries - Vaisigano and Fuluasou Rivers, which are very important water sources for drinking water, hydropower, bio-diversity and tourism. Unfortunately, with increasing population and development pressures over the years, this catchment area has become significantly degraded from problems such as soil erosion, siltation, water pollution/contamination and water shortages, causing major concern to the Government.

The Action Strategy for Nature Conservation in the Pacific Islands Region for 2003-2007, arose out of the 7th Pacific Islands Conference on Nature Conservation and Protected Areas which was held in Rarotonga, Cook Islands, in July 2002. It was then endorsed by the member country representatives of the Secretariat of the Pacific Regional Environment Programme (SPREP) at the September 2003 SPREP Meeting and it was meant to represent a consensus on the priority concerns for conservation and ways in which these can be addressed.

The intentional and unintentional transfer of species from one water body to another around the world has boomed in recent decades. Many seas and regions have been invaded by a high number of non-native species. Some of these species thrive in their new habitats, out-competing native species and changing ecosystems, sometimes dramatically. Alien Invasive Species (AIS) are currently perceived to be one of the primary threats to biological diversity. Throughout the world, marine resource managers are in the process of setting up marine protected areas (MPAs), sanctuaries, estuarine reserves and fishing closures as a means to preserve our marine biodiversity and living resources. Given the high ecological value of these areas, the efforts undertaken and the funds disbursed to conserve it, biodiversity loss in such places is even more dramatic than in others.

A project team composed of staff of the various division of MNREM was formed as a Technical Team to assist the Project Manager in the implementation of project activities. The Project Team and Manager were able to compile a Summary Report of Existing Information on Lake Lanoto’o, organized and started the initial detail surveys on the site’s flora and fauna ecologies; and prepare a list of stakeholders for engagement in the formulation of an effective management/development plan for the site.

A project team composed of staff of the various division of MNREM was formed as a Technical Team to assist the Project Manager in the implementation of project activities. The Project Team and Manager were able to compile a Summary Report of Existing Information on Lake Lanoto’o, organized and started the initial detail surveys on the site’s flora and fauna ecologies; and prepare a list of stakeholders for engagement in the formulation of an effective management/development plan for the site.

The marine environment and its resources have always been an important part in the way of life for small Pacific Island countries such as Samoa. A vast majority of Samoa's population inhabit the coastal fringes of the islands, thus depending largely on coastal marine resources and ecosystems for daily sustenance. Coastal waters support some of the most productive ecosystems such as mangrove forests, coral reefs and seagrass beds, which are all interrelated features crucial to marine wildlife and their habitats. In addition to playing extremely important ecological roles, marine ecosystems provide coastline protection, and sustain resources that contribute significantly to the country's economy.

Mangrove systems occur extensively on low gradient tropical shorelines, where sedimentation enables resilience during sea-level rise (SLR). Within mangroves, inundation frequencies across the intertidal slope cause zonation of different species with elevation. This tight sea-level control of the seaward margin and zones within mangroves has been demonstrated by precise EDM survey. Hence species zones in mangroves are definitive indicators of sea-level position, and pollen distributions record the locations of different zones in the sedimentary record. Pollen stratigraphic records can be used to reconstruct Holocene sea-levels and show mangrove response to change. Mangrove response to sea-level rise has been investigated in Bermuda, the Cayman Islands, Tonga and southern New Guinea. Radiocarbon dating of stratigraphy determined a sediment accretion rate of 1 mm a1for the low island locations, and up to 1.5 mm a"1 in two estuaries of southern New Guinea. The IPCC SLR projections of 9-88 cm by 2100 equate to a rate of 0.9-8.8 mm a"1. Mangrove recession events and replacement by lagoon environments are shown to occur during more rapid sea-level rise. In Bermuda rates of SLR exceed 2 mm a1and the largest mangrove area having existed for the last 2000 years lost 26% area in retreat of its seaward edge during the last century. In Tonga, a large mangrove swamp persisted 7000-5500 yr BP during SLR of 1.2 mm a1, then retreated when the rate increased. In Cayman 20 km of mangroves died back between 4080 and 3230 yr BP, during SLR of 2.8-3.3 mm a1, to become a lagoon. In extensive swamps of southern New Guinea gradual Late Holocene retreat of mangrove zones occurred with SLR of 0.67 mm a1. Hence while low island mangroves are likely to be the most sensitive to projected SLR, continental margin mangroves will also suffer disruption and retreat.