PNG Threatened Endemic Plants and Animals Species. This was published as part of the 5th CBD National Report.
Fifth National Report on Species Richness of PNG and World Higher Vertebrates
The total area under Conservation in PNG is approximately 3.8% of the total land area.
The 15 countries reporting largest primary forest area (in 1000 ha) to FRA 2015 (representing 90% of the global primary forest area reported to FRA, 2015). PNG has a deforestation rate of 0.49%.
Figures are for wild and ranched species of both freshwater and saltwater crocodiles
Submission for UNFCCC Technical Assessment in 2017 by Climate Change and Development Authority
National Report to the United Nations Framework Convention on Climate Change
Papua New Guinea’s (PNG) has been one of the fastest growing economies globally this century with average growth rates above 6%. This rapid growth has been driven primarily by the expansion of foreign investment within the natural gas sector and high prices for PNG’s central exports many of which are transported to rapidly growing Asian economies. This growth has built on a long history of natural resources being at the centre of the PNG economy with exports and employment dominated by mining, natural gas, logging and agriculture. While this rapid growth has
In urban areas, responsibility for providing piped water and sewerage services in the nation’s capital, Port Moresby, lies with Eda Ranu, and for the remaining provincial and district towns with Water PNG (formerly the PNG Water Board). Service provision to these areas are estimated to be 89% access to safe water (little change from 87% in 1990), and 57% access to safe sanitation (down from 89% in 1990)1. Access to services in urban areas struggle to keep up in the face of rapid urban population expansion.
The New Guinea region evolved within the obliquely and rapidly converging Australian and Pacific plate boundary zone. It is arguably one of the most tectonically complex regions of the world, and its geodynamic evolution involved microplate formation and rotation, lithospheric rupture to form ocean basins, arc-continent collision, subduction olarity reversal, collisional orogenesis, ophiolite obduction, and exhumation of (ultra)high-pressure metamorphic rocks.