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Bewani Mountains
The Bewani Mountains form a mountain range in northwestern Papua New Guinea. Together with the Torricelli Mountains and Prince Alexander Mountains it forms the North Coastal Range of Papua New Guinea.Birdlife International: North Papuan mountains retrieved 11 August 2010 The highest point of the mountains is at 1,960 m. The Bewani languages and various other are spoken in the region. Geology The Bewani-Torricelli-Prince Alexander Mountains, are presumed to have been formed as an island arc in the Late[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope Carbon-13, 13C in the atmosphere was exceptionally low in comparison with the more common isotope Carbon-12, 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Popigai impact structure, Siberia and in what is now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tree-kangaroo
Tree-kangaroos are marsupials of the genus ''Dendrolagus'', adapted for arboreal locomotion. They inhabit the tropical rainforests of New Guinea and far northeastern Queensland, along with some of the islands in the region. All tree-kangaroos are considered threatened due to hunting and habitat destruction. They are the only true arboreal macropods. Evolutionary history The evolutionary history of tree-kangaroos possibly begins with a rainforest floor-dwelling pademelon-like ancestor. This ancestor possibly evolved from an arboreal possum-like ancestor as is suspected of all macropodid marsupials in Australia and New Guinea. During the late Eocene, the Australian/New Guinean continent began a period of drying that caused a retreat in the area of rainforest, which forced the ancestral pademelons to begin living in a dryer, rockier environment. After some generations of adaptation to the new environment, the pademelons may have evolved into rock-wallabies (''Petrogale'' spp.), w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene Oceania
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and end of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Papua New Guinea
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bewani-Wutung Onei Rural LLG
Bewani/Wutung Onei Rural LLG is a local-level government (LLG) of Sandaun Province, Papua New Guinea. Bewani languages and Skou languages are spoken in the LLG. Wards *01. Wutung (Wutung language speakers) *02. Musu (Wutung language speakers: Musu dialect) *03. Yaukono (Wutung language speakers: Nyao dialect) *04. Yako *05. Waromo (Dumo speakers) *06. Lido *07. Ningra ( Ningera language speakers) *08. Rawo *09. Poko *10. Nowake *11. Laitre (Rawo language speakers) *12. Puari *13. Onei (Womo language Womo and Sumararu are a Papuan language of Papua New Guinea. The two varieties are sufficiently divergent that Usher counts them as distinct languages. Womo is spoken in Onei village () of Bewani/Wutung Onei Rural LLG in Sandaun Province Sand ... speakers) *14. Osol *15. Krisa (I'saka language speakers) *16. Ossima (Kilmeri language speakers) *17. Kilipau *18. Ilup *19. Amoi *20. Somboi *21. Ituly *22. Skotiaho *23. Ainbai (Ainbai language speakers) *24. Sumumini *25. Imbio 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bewani River
The Bewani River is a river in Western New Guinea, Indonesia. Bewani Riverat Geonames.org (cc-by) post updated 2014-03-05; database downloaded on 2015-11-27 See also *List of rivers of Western New Guinea This is a partial list of rivers of Western New Guinea in Indonesia.''Map of Indonesia''. Peta Indonesia. Wawasan Nusantara. CV. Indo Prima Sarana. Accessed 29 Juli 2017. In alphabetical order By mouth location From west to east: North coast ... References Rivers of Papua (province) {{Indonesia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bewani Range Languages
The Border or Upper Tami languages are an independent family of Papuan languages in Malcolm Ross's version of the Trans–New Guinea proposal. Unlike the neighboring Sepik languages and many other Papuan language families of northern New Guinea, Border languages do not have grammatical gender or number (dual and plural forms). Name The Border family is named after the Indonesia – Papua New Guinea border, which it spans. Other than the Border languages, the Skou, Senagi, Pauwasi, Anim, and Yam families also span the Indonesia – Papua New Guinea border. Classification history Cowan (1957) tentatively proposed a "Tami" family, named after the Tami River, that included the modern Border and Sko language families. Some of the previously unclassified languages did turn out to be Sko, and were added to that family; the remainder (including the languages of the upper Tami) constitute the Border family. Languages Laycock classified Morwap as an isolate, but noted pronominal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Choerophryne Longirostris
''Choerophryne longirostris'' is a species of frog in the family Microhylidae. It is endemic to Mount Menawa in the Bewani Mountains of Papua New Guinea Papua New Guinea (abbreviated PNG; , ; tpi, Papua Niugini; ho, Papua Niu Gini), officially the Independent State of Papua New Guinea ( tpi, Independen Stet bilong Papua Niugini; ho, Independen Stet bilong Papua Niu Gini), is a country i .... It inhabits the interior and edges of closed-canopy rainforest. References longirostris Amphibians of Papua New Guinea Endemic fauna of Papua New Guinea Taxonomy articles created by Polbot Amphibians described in 2001 {{Microhylidae-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cophixalus Bewaniensis
''Cophixalus bewaniensis'' is a species of frog in the family Microhylidae. It is endemic to Mount Menawa in the Bewani Mountains, West Sepik Province, mainland Papua New Guinea. The specific name refers to its type locality. Description The type series In biology, a type is a particular specimen (or in some cases a group of specimens) of an organism to which the scientific name of that organism is formally attached. In other words, a type is an example that serves to anchor or centralizes t ... consists of two adult males measuring in snout–vent length. No other specimens are known. The snout is truncate. The tympanum is very indistinct and there is a weak supratympanic fold. The eyes are moderately large. The fingers and the toes bear small discs, except for the first finger that is greatly reduced and lacks a disc. The first toe is also reduced but bears a tiny disc. No webbing is present. The dorsum has reddish-tan ground color. There is a large, black blotch beh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endemic
Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found elsewhere. For example, the Cape sugarbird is found exclusively in southwestern South Africa and is therefore said to be ''endemic'' to that particular part of the world. An endemic species can be also be referred to as an ''endemism'' or in scientific literature as an ''endemite''. For example '' Cytisus aeolicus'' is an endemite of the Italian flora. '' Adzharia renschi'' was once believed to be an endemite of the Caucasus, but it was later discovered to be a non-indigenous species from South America belonging to a different genus. The extreme opposite of an endemic species is one with a cosmopolitan distribution, having a global or widespread range. A rare alternative term for a species that is endemic is "precinctive", which applies to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tenkile
The tenkile (''Dendrolagus scottae''), also known as Scott's tree-kangaroo, is a species of tree-kangaroo in the family Macropodidae. It is endemic to a very small area of the Torricelli Mountains of Papua New Guinea. Flannery, Tim: ''Mammals of New Guinea'', Chatswood, 1995 Its natural habitat is subtropical or tropical dry forests. It is threatened by habitat loss and by hunting. The tenkile is listed as endangered due to hunting and logging activities in Papua New Guinea. The tenkile is hunted for its meat, and is the main protein source for the residents of Papua New Guinea. The population of Papua New Guinea has increased in recent years due to improvements in healthcare; therefore increasing need in tenkile meat which means that more tenkiles are being hunted. Additionally, tenkiles are poached for their fur and are captured and sold as a part of the illegal pet trade. Domesticated dogs also hunt tenkiles. Deforestation in Papua New Guinea affects all tree-kangaroos, however ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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