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Icarops
''Icarops'' is an extinct, possibly paraphyletic genus of mystacine bat with three described species. The genus is known from fossils found at Riversleigh, north-western Queensland, Bullock Creek, Northern Territory, and Lake Ngapakaldi to Lake Palankarinna Fossil Area South Australia Australia. The fossils date from the late Oligocene to early Miocene. The name was derived from a figure of Greek mythology, Icarus, who the authors noted, "flew towards the sun, in reference to the ancient mystacinid that flew eastwards from Australia to New Zealand". A study describing the genus ''Vulcanops'' renders ''Icarops'' paraphyletic towards the rest of Mystacinidae, with ''I. paradox'' being closer to New Zealand mystacines than to other Australian mystacines, which form an independent clade. The described species are * ''Icarops'' :*''Icarops aenae'' :*''Icarops breviceps'' :*''Icarops paradox'' Terrestriality Like its modern relatives, the '' Mystacina ''short-tailed bats, ''I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mystacine
__NOTOC__ Mystacinidae is a family of unusual bats, the New Zealand short-tailed bats. There is one living genus, ''Mystacina'', with two species, one of which could have possibly become extinct in the 1960s. They are medium-sized bats, about in length, with grey, velvety fur. Species and range The origins of this family go back to the Late Oligocene of Australia, with the genus ''Icarops''. Several fossil species are also known from the contemporary Saint Bathans Fauna in New Zealand. The oldest unambiguous fossils of the living genus date to the Miocene of New Zealand. A second extinct genus, ''Vulcanops'', lived sympatrically with ''Mystacina'' in New Zealand from the Miocene until its extinction during the Pleistocene. The study describing ''Vulcanops'' also renders ''Icarops'' paraphyletic in regards to the rest of the family. Mystacines appear to have been an old Gondwanan lineage; they diverged from other bat groups within Noctilionoidea (a primarily Gondwanan group otherw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mystacinidae
__NOTOC__ Mystacinidae is a family of unusual bats, the New Zealand short-tailed bats. There is one living genus, '' Mystacina'', with two species, one of which could have possibly become extinct in the 1960s. They are medium-sized bats, about in length, with grey, velvety fur. Species and range The origins of this family go back to the Late Oligocene of Australia, with the genus '' Icarops''. Several fossil species are also known from the contemporary Saint Bathans Fauna in New Zealand. The oldest unambiguous fossils of the living genus date to the Miocene of New Zealand. A second extinct genus, '' Vulcanops'', lived sympatrically with ''Mystacina'' in New Zealand from the Miocene until its extinction during the Pleistocene. The study describing ''Vulcanops'' also renders ''Icarops'' paraphyletic in regards to the rest of the family. Mystacines appear to have been an old Gondwanan lineage; they diverged from other bat groups within Noctilionoidea (a primarily Gondwanan group o ... [...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] |
Vulcanops
''Vulcanops jennyworthyae'' is an extinct species of bat that lived during the Miocene in New Zealand, a large burrowing microchiropteran that probably ate arthropods and plant material around twenty million years before present. It is the type and only described species of the genus ''Vulcanops''. Taxonomy and etymology ''Vulcanops jennyworthyae'' was described in 2018 from fossilized teeth and bone fragments. The new genus and species were placed within the family Mystacinidae, commonly called the burrowing bats. The genus name "''Vulcanops''" is derived from the Roman god of fire and volcanoes, Vulcan. The suffix "-ops" is commonly used for bat genera. "Vulcan" was chosen in homage to the tectonic nature of New Zealand, as well as a historic hotel, Vulcan Hotel, in the mining town of Saint Bathans. The eponym for the specific epithet "''jennyworthyae''" is Jennifer P. Worthy "in recognition of her pivotal role in revealing the diversity of the St Bathans Fauna." Jennifer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prehistoric Bat Genera
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oligocene Bats
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 of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene Bats
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene Mammals Of Australia
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monotreme
Monotremes () are prototherian mammals of the order Monotremata. They are one of the three groups of living mammals, along with placentals (Eutheria), and marsupials (Metatheria). Monotremes are typified by structural differences in their brains, jaws, digestive tract, reproductive tract, and other body parts, compared to the more common mammalian types. In addition, they lay eggs rather than bearing live young, but, like all mammals, the female monotremes nurse their young with milk. Monotremes have been considered members of Australosphenida, a clade that contains extinct mammals from the Jurassic and Cretaceous of Madagascar, South America, and Australia, though this is disputed. The only surviving examples of monotremes are all indigenous to Australia and New Guinea, although there is evidence that they were once more widespread, as ''Monotrematum'' is known from the Paleocene of South America. The extant monotreme species are the platypus and four species of echidnas. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsupial
Marsupials are any members of the mammalian infraclass Marsupialia. All extant marsupials are endemic to Australasia, Wallacea and the Americas. A distinctive characteristic common to most of these species is that the young are carried in a pouch. Marsupials include opossums, Tasmanian devils, kangaroos, koalas, wombats, wallabies, bandicoots, and the extinct thylacine. Marsupials represent the clade originating from the last common ancestor of extant metatherians, the group containing all mammals more closely related to marsupials than to placentals. They give birth to relatively undeveloped young that often reside in a pouch located on their mothers' abdomen for a certain amount of time. Close to 70% of the 334 extant species occur on the Australian continent (the mainland, Tasmania, New Guinea and nearby islands). The remaining 30% are found in the Americas—primarily in South America, thirteen in Central America, and one species, the Virginia opossum, in North America, n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mystacina
''Mystacina'' is the sole surviving genus of the family Mystacinidae. The New Zealand lesser short-tailed bat is the only member of this group confirmed to survive today, since the closely related New Zealand greater short-tailed bat The New Zealand greater short-tailed bat (''Mystacina robusta'') is one of two species of New Zealand short-tailed bats, a family (Mystacinidae) unique to New Zealand. Larger than the New Zealand lesser short-tailed bat, there have been no confi ... possibly went extinct as recently as 1965. A third species, '' Mystacina miocenalis'', is known from the Middle Miocene some 19-16 million years ago. References {{Taxonbar, from= Q368565 Bat genera Mammal genera with one living species Taxa named by John Edward Gray Mystacinidae Mammals of New Zealand Endemic fauna of New Zealand Endemic mammals of New Zealand ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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