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Chelidonichthys Kumu
The bluefin gurnard or Pacific red gurnard (''Chelidonichthys kumu'') is a species of marine ray-finned fishes belonging to the family Triglidae, the gurnards and sea robins. Its Māori names are Kumukumu and Pūwahaiau. It is found in the western Indian Ocean and the western Pacific Ocean, being common around Australia and New Zealand at depths down to . This fish is edible for humans. Taxonomy The bluefin gurnard was first formally described in 1829 by the French zoologist Georges Cuvier with the type locality given as New Zealand. Within the genus '' Chelidonichthys'' this species is classified in the nominate subgenus. The specific name ''kumu'' is a latinisation of ''koumou'', a name Cuvier said was used locally for this fish New Zealand. Description The bluefin gurnard is a bottom-dwelling fish known for its bright red body and large, colourful pectoral fins with a large black eye-spot in the center and surrounded by a bright blue edge. Its natural colour is a splo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Georges Cuvier
Jean Léopold Nicolas Frédéric, Baron Cuvier (; 23 August 1769 – 13 May 1832), known as Georges Cuvier, was a French natural history, naturalist and zoology, zoologist, sometimes referred to as the "founding father of paleontology". Cuvier was a major figure in natural sciences research in the early 19th century and was instrumental in establishing the fields of comparative anatomy and paleontology through his work in comparing living animals with fossils. Cuvier's work is considered the foundation of vertebrate paleontology, and he expanded Linnaean taxonomy by grouping classes into phylum, phyla and incorporating both fossils and living species into the classification. Cuvier is also known for establishing extinction as a fact—at the time, extinction was considered by many of Cuvier's contemporaries to be merely controversial speculation. In his ''Essay on the Theory of the Earth'' (1813) Cuvier proposed that now-extinct species had been wiped out by periodic catastrophi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Latinisation Of Names
Latinisation (or Latinization) of names, also known as onomastic Latinisation, is the practice of rendering a ''non''-Latin name in a Latin style. It is commonly found with historical proper names, including personal names and toponyms, and in the standard binomial nomenclature of the life sciences. It goes further than romanisation, which is the transliteration of a word to the Latin alphabet from another script (e.g. Cyrillic). For authors writing in Latin, this change allows the name to function grammatically in a sentence through declension. In a scientific context, the main purpose of Latinisation may be to produce a name which is internationally consistent. Latinisation may be carried out by: * transforming the name into Latin sounds (e.g. for ), or * adding Latinate suffixes to the end of a name (e.g. for '' Meibom),'' or * translating a name with a specific meaning into Latin (e.g. for Italian ; both mean 'hunter'), or * choosing a new name based on some attribut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helicometra
''Helicometra'' is a genus of trematodes in the class Opecoelidae. It is synonymous with ''Allostenopera'' Baeva, 1968, ''Metahelicometra'' Yamaguti, 1971, and ''Stenopera'' Manter, 1933. Its type species is ''H. fasciata'' (Rudolphi, 1819). They are distinguished by their unique spiral uterus, from which their name is derived. Species *'' Helicometra aegyptensis'' Hassanine, 2007 *'' Helicometra antarcticae'' Holloway & Bier, 1968 *'' Helicometra aposinuata'' Pritchard, 1966 *'' Helicometra bassensis'' Woolcock, 1935 *'' Helicometra borneoensis'' Fischthal & Kuntz, 1965 *'' Helicometra boseli'' Nagaty, 1956 *'' Helicometra dalianensis'' (Li, Qiu & Zhang, 1989) *'' Helicometra dorabi'' (Mamaev & Oshmarin, 1966) *'' Helicometra equilata'' (Manter, 1933) *'' Helicometra fasciata'' (Rudolphi, 1819) *'' Helicometra filamentosa'' Madhavi, 1975 *'' Helicometra fusiformis'' Wang, Wang & Zhang, 1992 *'' Helicometra gibsoni'' Meenakshi, Madhavi & Swarnkumari, 1993 *''Helicometra gomphosi'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Fur Seal
''Arctocephalus forsteri'' (common names include the Australasian fur seal, South Australian fur seal, New Zealand fur seal, Antipodean fur seal, or long-nosed fur seal) is a species of fur seal found mainly around southern Australia and New Zealand. The name ''New Zealand fur seal'' is used by English speakers in New Zealand; ''kekeno'' is used in the Māori language. , the common name long-nosed fur seal has been proposed for the population of seals inhabiting Australia. Although the Australian and New Zealand populations show some genetic differences, their morphologies are very similar, and thus they remain classed as a single species. After the arrival of humans in New Zealand, and particularly after the arrival of Europeans in Australia and New Zealand, hunting reduced the population to near-extinction. Description Males have been reported as large as 160 kg; their average weight is about 126 kg.Harcourt, R.G., (2001)"Advances in New Zealand mammalogy 1990–20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foveaux Strait
The Foveaux Strait, (, or , ) separates Stewart Island, New Zealand's third largest island, from the South Island. The strait is about 130 km long (from Ruapuke Island to Little Solander Island), and it widens (from 14 km at Ruapuke Island to 50 km at Te Waewae Bay) and deepens (from 20 to 120 m) from east to west. The strait lies within the continental shelf area of New Zealand, and was probably dry land during the Pleistocene epoch. Three large bays, Te Waewae Bay, Oreti Beach and Toetoes Bay, sweep along the strait's northern coast, which also hosts Bluff township and harbour. Across the strait lie the Solander Islands, Stewart Island, Dog Island and Ruapuke Island. According to a Maori legend, the strait was created by Kewa the obedient whale when traditional Maori ancestor Kiwa summoned the whale to create a waterway. History During the Last Glacial Period when sea levels were over 100 metres lower than current levels, the South Island and Stewart Is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banks Peninsula
Banks Peninsula is a peninsula of volcanic origin on the east coast of the South Island of New Zealand. It has an area of approximately and encompasses two large harbours and many smaller bays and coves. The South Island's largest city, Christchurch, is immediately north of the peninsula. Geology Banks Peninsula forms the most prominent volcanic feature of the South Island, similar to — but more than twice as large as — the older Dunedin volcano (Otago Peninsula and Harbour) to the southwest. Geologically, the peninsula comprises the eroded remnants of two large (Lyttelton formed first, then Akaroa), and the smaller Mt Herbert Volcanic Group. These formed due to intraplate volcanism between approximately eleven and eight million years ago (Miocene) on a continental crust. The peninsula formed as offshore islands, with the volcanoes reaching to about 1,500 m above sea level. Two dominant craters formed Lyttelton and Akaroa Harbours. The Canterbury ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hawke Bay
Hawke Bay ( mi, Te Matau-a-Māui), formerly named ''Hawke's Bay'', is a large bay on the east coast of the North Island of New Zealand, surrounded by the Hawke's Bay region. It stretches from Māhia Peninsula in the northeast to Cape Kidnappers / Te Kauwae-a-Māui in the southwest, a distance of some . Captain James Cook, sailing in HMS ''Endeavour'', entered the bay on 12 October 1769. After exploring it, he named it for Sir Edward Hawke, First Lord of the Admiralty, on 15 October 1769, describing it as some 13 leagues (about ) across. Hawke had decisively defeated the French at the Battle of Quiberon Bay in 1759. This part of the New Zealand coast is subject to tectonic uplift, with the land being raised out of the sea. For this reason, the coastal land in this area has significant marine deposits, with both marine and land dinosaur fossils having been found inland. The Napier earthquake of 3 February 1931 resulted in several parts of the seabed close to the city of Nap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Plenty
The Bay of Plenty ( mi, Te Moana-a-Toi) is a region of New Zealand, situated around a bight of the same name in the northern coast of the North Island. The bight stretches 260 km from the Coromandel Peninsula in the west to Cape Runaway in the east. The Bay of Plenty Region, governed by the Bay of Plenty Regional Council, incorporates several large islands in the bay, in addition to the mainland area. Called ''Te Moana-a-Toi'' (the Sea of Toi) in the Māori language after Toi, an early ancestor, the name 'Bay of Plenty' was bestowed by James Cook in 1769 when he noticed the abundant food supplies at several Māori villages there, in stark contrast to observations he had made earlier in Poverty Bay. History According to local Māori traditions, the Bay of Plenty was the landing point of several migration canoes that brought Māori settlers to New Zealand. These include the ''Mātaatua'', ''Nukutere'', ''Tākitimu'', '' Arawa'' and ''Tainui'' canoes. Many of the de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kermadec Islands
The Kermadec Islands ( mi, Rangitāhua) are a subtropical island arc in the South Pacific Ocean northeast of New Zealand's North Island, and a similar distance southwest of Tonga. The islands are part of New Zealand. They are in total area and uninhabited, except for the permanently manned Raoul Island Station, the northernmost outpost of New Zealand. The islands are listed with the New Zealand outlying islands. The islands are an immediate part of New Zealand, but not part of any region or district, but instead an ''Area Outside Territorial Authority''. Toponymy The islands were named after the Breton captain Jean-Michel Huon de Kermadec, who visited the islands as part of the d'Entrecasteaux expedition in the 1790s. The topographic particle "Kermadec" is of Breton origin and is a lieu-dit in Pencran in Finistère where '' ker'' means village, residence and madec a proper name derived from '' mad'' (which means 'good') with the suffix '' -ec'', used to form adjectives in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chatham Islands
The Chatham Islands ( ) (Moriori: ''Rēkohu'', 'Misty Sun'; mi, Wharekauri) are an archipelago in the Pacific Ocean about east of New Zealand's South Island. They are administered as part of New Zealand. The archipelago consists of about ten islands within an approximate radius, the largest of which are Chatham Island and Pitt Island (Rangiauria). They include New Zealand's easternmost point, the Forty-Fours. Some of the islands, formerly cleared for farming, are now preserved as nature reserves to conserve some of the unique flora and fauna. The islands were uninhabited when the Moriori people arrived around 1500 CE and developed a peaceful way of life. In 1835 members of the Ngāti Mutunga and Ngāti Tama Māori iwi from the North Island of New Zealand invaded the islands and nearly exterminated the Moriori, enslaving the survivors. Later during the period of European colonisation of New Zealand, the New Zealand Company claimed that the British Crown had never include ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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