Sustainable Land Use Policy (SLUP) is a systematic and iterative procedure carried out in order to create an enabling environment for sustainable development (Wehrmann.B, 2011). It assess the physical, socio-economic, institutional and legal potentials and constraints with respect to an optimal and sustainable use of land resources and empowers people to make decisions about how to allocate those resources.
At 463,000 square kilometers, Papua New Guinea (PNG) is the largest Pacific island state. Located in the South
West Pacific, it is bound by the Gulf of Guinea and the Coral Sea to the south, Indonesia to the west, the Solomon
Sea to the east, and the Bismarck Sea to the northeast. PNG comprises the eastern half of New Guinea island, four additional islands (Manus, New Ireland, New Britain, and Bougainville), and 600 smaller islets and atolls to the north and east. PNG is home to a diverse range of ecosystems, including mountain glaciers, humid tropical
Papua New Guinea, the land of diversity and last frontier for Biodiversity Conservation. Situated north of Australia, Papua New Guinea is a Pacific Island country that comprises the eastern half of the Island of New Guinea and four islands bordered by the Solomon Islands to the east and Indonesia to the west. It is one of the largest tropical islands on earth, New Guinea remains covered by the 3rd largest rainforest in the world, after the Amazon and the Congo Basin.
Papua New Guinea, the land of diversity and last frontier for Biodiversity Conservation. Situated north of Australia, Papua New Guinea is a Pacific Island country that comprises the eastern half of the Island of New Guinea and four islands bordered by the Solomon Islands to the east and Indonesia to the west. It is one of the largest tropical islands on earth, New Guinea remains covered by the 3rd largest rainforest in the world, after the Amazon and the Congo Basin.
Papua New Guinea, the land of diversity and last frontier for Biodiversity Conservation. Situated north of Australia, Papua New Guinea is a Pacific Island country that comprises the eastern half of the Island of New Guinea and four islands bordered by the Solomon Islands to the east and Indonesia to the west. It is one of the largest tropical islands on earth, New Guinea remains covered by the 3rd largest rainforest in the world, after the Amazon and the Congo Basin.
Coral bleaching
Coral bleaching
Marine fisheries
Tuna Fishery Report Card 2018
PNG Energy Supply & Demand Outlook published by APEC. Capture data on PNG:
- Economy
- Energy resources & infrastructure
- Energy policies
- Business-as-usual (BAU) outlook
- Challenges and implications of BAU
- Alternative scenarios
The 2020 State of Environment Report is the first for Papua New Guinea.
Coupled climate and sea-level changes deduced from Huon Peninsula coral terraces of the last ice age
Huon Peninsula, Papua New Guinea, is a tectonically unstable, uplifting shoreline ringed by emergent coral terraces. The terraces were formed during episodes of rapid sea-level rise when corals constructed large, discrete coral platforms that were subsequently uplifted. Uranium series ages of four prominent Huon Peninsula last glacial (OIS 3) coral terraces coincide with the timing of major North Atlantic climate reversals at intervals of 6000^7000 yr between 30 000 yr and 60 000 yr ago.
An analysis of cultural change and generation gaps in the local community of the Nungon ethnic group in the state of Papua New Guinea will be the subject of the study. This ethnic group came into contact with Europeans for the first time in the mid-1930s. The pace of cultural changes within the community has been gradually increasing.
In days gone by some of the Motu-speaking peoples around Port Moresby used to go on annual trading expeditions to the Gulf of Papua. There they would exchange with the inhabitants of that area pots and other valuables for sago and canoe logs. These expeditions were called hiri, and were not only spectacular in terms of the number, nature and size of the sailing craft involved and the cargoes they carried but also very important economically and in other ways to the Motu and others directly or indirectly involved.
Peatlands are common in montane areas above 1,000 m in New Guinea and become extensive above 3,000 m in the subalpine zone. In the montane mires, swamp forests and grass or sedge fens predominate on swampy alley bottoms. These mires may be 4–8 m in depth and up to 30,000 years in age. In Papua New Guinea (PNG) there is about 2,250 km2 of montane peatland, and Papua Province (the Indonesian western half of the island) probably contains much more. Above 3,000 m, peat soils form under blanket bog on slopes as well as on valley floors.
Two of the unanswered questions of Papua New Guinea prehistory are: (1) whether agriculture was present
in the mid-Holocene not only in the highlands but also in the lowlands and Bismarck Archipelago and (2)whether the presence of agriculture might have been influenced by interaction between these regions. This paper addresses these questions through an analysis of prehistoric stone mortars, pestles and figures, which hold information on both style and function.