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Nanantius
''Nanantius'' is a genus of extinct enantiornithean avialan ("bird" in the broad sense of the word) known from the Early Cretaceous (Albian, c. 100–112 mya) of Australia. Specimens and species The only valid species of ''Nanantius'' is ''Nantantius eos,' '' which was first described in 1986. A supposed second species, ''Nanantius valifanovi,'' has turned out to be a synonym of '' Gobipteryx minuta''. ''N. eos'' was initially only known from an incomplete but elongated tibiotarsus and a cervical (neck) vertebra hailing from the Toolebuc Formation stratum. This holotype tibiotarsus ( QM F12992) was found at Warra Station near Boulia, in Queensland. In 1997, additional fossils from Canary Station in the same area of Australia were also placed into the genus ''Nanantius.'' One of these was a cervical (neck) vertebra, QM F12991, which was assigned to ''Nanantius eos''. The other bone was a partial left tibiotarsus (QM F31813) which was assigned to ''Nanantius'' but not placed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gobipteryx Minuta
''Gobipteryx'' (from Gobi eferring to the Gobi Desert where it was first discovered and Greek pteryx "wing") is a genus of prehistoric bird from the Campanian Age of the Late Cretaceous Period.Elżanowski, A. (1974)"Preliminary note on the Palaeognthous bird from the Upper Cretaceous of Mongolia"''Palaeontologia Polonica'' 30:103-109, plates 32-33. It is not known to have any direct descendants. Like the rest of the enantiornithes clade, ''Gobipteryx'' is thought to have gone extinct near the end of the Cretaceous.Padian, K. (2004). "Basal Avialae". chptr 11, in Weishampel, D.B., Dodson, P. and Osmólska, H. (eds.): ''The Dinosauria'' 2nd Edition. University of California Press, Berkeley . Description Based on a skull length of 45 millimeters, ''Gobipteryx'' has been estimated to be approximately the size of a partridge.Elżanowski, A. (1976): Palaeognathous bird from the Cretaceous of Central Asia ''Nature'' 264: 51-53. Its bones are fibrolamellar.Chinsamy, A., Elżanowski, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toolebuc Formation
The Toolebuc Formation is a geological Formation (geology), formation that extends from Queensland across South Australia and the Northern Territory in Australia, whose strata date back to the Albian stage of the Early Cretaceous. Dinosaurs,Weishampel ''et al.'', 2004, pp.573-574 pterosaurs, plesiosaurs, ichthyosaurs, protostegid turtles, sharks, chimaeroids and bony fish remains are among the fossils that have been recovered from the formation. Description Deposition occurred in a cool to temperate inland sea setting and the present lithology is dominantly made up of limey shales with abundant ''Inoceramus'' bivalve shells. Ichthyosaurs and protostegid turtles were the most common marine reptiles at this time in the Eromanga Sea, in contrast to older Aptian deposits such as the Bulldog Shale of South Australia, which show that plesiosaurs were previously more abundant and also more diverse. The Toolebuc Formation is one of the richest known sources of Mesozoic vertebrate fossi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Enantiornithes
The Enantiornithes, also known as enantiornithines or enantiornitheans in literature, are a group of extinct Avialae, avialans ("birds" in the broad sense), the most abundant and diverse group known from the Mesozoic era. Almost all retained teeth and clawed fingers on each wing, but otherwise looked much like modern birds externally. Over seventy species of Enantiornithes have been named, but some names represent only single bones, so it is likely that not all are valid. The Enantiornithes became extinct at the Cretaceous–Paleogene boundary, along with Hesperornithes and all other non-avian dinosaurs. Discovery and naming The first Enantiornithes to be discovered were incorrectly referred to modern bird groups. For example, the first known species of Enantiornithes, ''Gobipteryx minuta'', was originally considered a paleognath related to ostriches and tinamou. The Enantiornithes were first recognized as a distinct lineage, or "subclass" of birds, by Cyril A. Walker in 1981. W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Cretaceous
The Early Cretaceous (geochronology, geochronological name) or the Lower Cretaceous (chronostratigraphy, chronostratigraphic name) is the earlier or lower of the two major divisions of the Cretaceous. It is usually considered to stretch from 143.1 Megaannum#SI prefix multipliers, Ma to 100.5 Ma. Geology Proposals for the exact age of the Barremian–Aptian boundary ranged from 126 to 117 Ma until recently (as of 2019), but based on drillholes in Svalbard the defining Anoxic event#Cretaceous, early Aptian Oceanic Anoxic Event 1a (OAE1a) was dated to 123.1±0.3 Ma, limiting the possible range for the boundary to c. 122–121 Ma. There is a possible link between this anoxic event and a series of Early Cretaceous large igneous provinces (LIP). The Ontong Java Plateau, Ontong Java-Manihiki Plateau, Manihiki-Hikurangi Plateau, Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Onto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apsaravis
''Apsaravis'' is a Mesozoic avialan genus from the Late Cretaceous. The single known species, ''Apsaravis ukhaana'', lived about 78 million years ago, in the Campanian age of the Cretaceous period. Its fossilized remains were found in the Camel's Humps sublocality of the Djadokhta Formation, at Ukhaa Tolgod in the Gobi Desert of Mongolia. They were collected in the 1998 field season by the Mongolian Academy of Sciences/American Museum of Natural History Paleontological Expeditions. It was described by Norell and Clarke (2001).Norell, Mark A., Clarke, Julia A. (2001). "Fossil that fills a critical gap in avian evolution". ''Nature'' Vol. 409 11 January 2001 pp.181-184. Its habitat was presumably very arid open landscape much like it is today, perhaps hotter still and with more (but nonetheless intermittent) rain. Permanent freshwater would have been scarce. Implications ''Apsaravis'' is important in avian paleontology. It has provided evidence that is directly relevant to at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queensland
Queensland ( , commonly abbreviated as Qld) is a States and territories of Australia, state in northeastern Australia, and is the second-largest and third-most populous state in Australia. It is bordered by the Northern Territory, South Australia and New South Wales to the west, south-west and south, respectively. To the east, Queensland is bordered by the Coral Sea and the Pacific Ocean; to the state's north is the Torres Strait, separating the Australian mainland from Papua New Guinea, and the Gulf of Carpentaria to the north-west. With an area of , Queensland is the world's List of country subdivisions by area, sixth-largest subnational entity; it List of countries and dependencies by area, is larger than all but 16 countries. Due to its size, Queensland's geographical features and climates are diverse, and include tropical rainforests, rivers, coral reefs, mountain ranges and white sandy beaches in its Tropical climate, tropical and Humid subtropical climate, sub-tropical c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous–Paleogene Extinction Event
The Cretaceous–Paleogene (K–Pg) extinction event, also known as the K–T extinction, was the extinction event, mass extinction of three-quarters of the plant and animal species on Earth approximately 66 million years ago. The event caused the extinction of all non-avian dinosaurs. Most other tetrapods weighing more than also became extinct, with the exception of some ectothermic species such as sea turtles and crocodilians. It marked the end of the Cretaceous period, and with it the Mesozoic era, while heralding the beginning of the current era, the Cenozoic. In the geologic record, the K–Pg event is marked by a thin layer of sediment called the Cretaceous–Paleogene boundary, K–Pg boundary or K–T boundary, which can be found throughout the world in marine and terrestrial rocks. The boundary clay shows unusually high levels of the metal iridium, which is more common in asteroids than in the Earth's crust. As originally proposed in 1980 by a team of scientists le ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vorona
''Vorona berivotrensis'' ( ; Malagasy for "bird", ''berivotrensis'', "from Berivotra") is a monotypic genus of prehistoric birds. It was described from fossils found in a Maevarano Formation quarry near the village of Berivotra, Mahajanga Province, Madagascar. The age of the fossilised specimen is Late Cretaceous, probably Maastrichtian (72.1-66.0 mya). ''V. berivotrensis'' is known from scattered remains, possibly from a single individual ( UA 8651 and FMNH PA715). The phylogenic affinity of ''Vorona'' is hard to determine due to the fragmentary nature of the remains, mainly because the fossil shows a mix of basal avian features as well as some that seem very derived. ''Vorona'' might be a primitive ornithuromorph. At least two studies recovered it as part of Enantiornithes, however. ''Vorona'' is sometimes confused with the dromaeosaur '' Rahonavis ostromi'', a fossil of which was found in the same location. This confusion has led to the common misconception that ''Voro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarsometatarsus
The tarsometatarsus is a bone that is only found in the lower leg of birds and some non-avian dinosaurs. It is formed from the fusion of several bird bones found in other types of animals, and homologous to the mammalian tarsus (ankle bones) and metatarsal bones (foot). Despite this, the tarsometatarsus of flying types is often referred to as just the shank, tarsus or metatarsus. Tarsometatarsal fusion occurred in several ways and extents throughout bird evolution. Paticularly, in Neornithes (modern birds), although the bones are joined along their entire length, the fusion is most thorough at the distal (metatarsal) end. In the Enantiornithes, a group of Mesozoic avialans, the fusion was complete at the proximal (tarsal) end, but the distal metatarsi were still partially distinct. While these fused bones are best known from birds and their relatives, avians are neither the only group nor the first to possess tarsometatarsi. In a remarkable case of parallel evolution, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warra Station
Warra is a rural town and locality in the Western Downs Region, Queensland, Australia. In the , the locality of Warra had a population of 180 people. Geography Warra is on the Darling Downs, a farming area in Queensland. It is on the Warrego Highway, north west of the state capital, Brisbane. The locality is bounded to the north by Haystack Road and Seigmeiers Road and to the south-west by the Condamine River. The town is located to the west of centre of the locality. The Warrego Highway and Western railway line enter the locality from the south-east ( Macalister), pass through the town, and exit to the west (Brigalow). Warra railway station serves the town (). The highway is known as Thorne Street within the town. Haystack is a neighbourhood in the north-west of the locality on the boundary with Tuckerang (). The land use is a mixture of dry and irrigated cropping with some grazing on native vegetation. History The town takes its name from the Warra Warra pastoral r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grabauornis
''Grabauornis'' is an extinct genus of enantiornitheans from the Early Cretaceous of China. The type species, ''Grabauornis lingyuanensis'', was named and described in 2014 by Johan Dalsätt, Per Ericson and Zhou Zhonghe. The genus name combines a reference to Amadeus William Grabau with the Greek word , which means bird. The specific name refers to the place where it was found; the city of Lingyuan in the Lianoning province of China. Dalsät already referred to the descriptive article in 2012, before it was published, in his dissertation and the name ''Grabauornis'' was mentioned with it. However it was still an invalid ''nomen ex dissertatione''. In addition, he explicitly stated that he did not want to perform naming acts, if they are not performed validly. The fossil, holotype IVPP V14595, was found in a layer of the Yixian Formation which dates to the Aptian, at an age of 125 million years. The holotype consists of a well-preserved skeleton, compressed onto a single plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
