Сообщество, посвящённое ра Below are the 10 most recent journal entries recorded in the "Сообщество, посвящённое ра" journal:
November 27th, 2014
08:06 pm
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Eurazhdarcho

 Eurazhdarcho is a genus of pterodactyloid pterosaur from the Late Cretaceous Transylvanian Basin of Romania.

 In 2009, Mátyás Vremir at Lancrăm near Sebeş-Glod in Transylvania at the SbG-B site uncovered the remains of a pterosaur. He donated these to the Erdélyi Múzeum, of the Societății Muzeului Ardelean (Transylvanian Museum Society). Subsequent excavations by Vremir discovered additional bones of the same individual animal and were added by him to the collection of the Babeș-Bolyai University.

 In 2013, Vremir, Alexander Wilhelm Armin Kellner, Darren Naish, and Gareth Dyke named and described the type species Eurazhdarcho langendorfensis. The generic name combines the name of Europe with that of the related form Azhdarcho. The specific name refers to Langendorf, the name of Lancrǎm in the language of the German ethnic minority in Romania. The article appeared in the electronic journal PLoS ONE without an accompanying printed version; it nevertheless validly names the taxon under the new rules of the ICZN.

 The holotype, EME VP 312, was found in a layer of the Sebeş Formation dating from the upper Early Maastrichtian, about 69 million years old. It consists of a partial skeleton lacking the skull. It includes three neck vertebrae among which the almost complete third and the fourth; the third and fourth right metacarpal; the upper part of the first phalanx of the wing finger; the lower part of the second phalanx; a lower phalanx of one of the other fingers and a number of undetermined fragments. The Babeș-Bolyai University material is included within this enumeration and is not indicated by a separate inventory number. Generally the quality of the bones is poor with much of the outer cortex broken or eroded and internal structures present as (impressions of) natural moulds. The fossils have not been completely flattened, preserving three-dimensionality, but compression has caused some distortion. The carcass had probably by flooding been deposed on its back in mud near a riverbank. Afterwards it was exposed to the air, weathering and being scavenged as proven by circular bite-marks inflicted by the conical teeth of some member of the Crocodyliformes. Later covered by a thin layer of dirt, it was damaged by beetles and termites.

 The authors noted that from the same Romanian layers the related giant form Hatzegopteryx is known; the known fossil material from both genera does not overlap. The authors considered an identity to be unlikely because the much smaller EME VP 312 seems to represent an adult individual.

 Eurazhdarcho is a medium-sized azhdarchid. The authors estimated its wingspan at three metres, extrapolating from an estimated length for the fourth metacarpal of about twenty-five centimetres.

 The authors established some distinctive traits, all present in the cervical vertebrae. The third neck vertebra has three-quarters of the length of the fourth vertebra, whereas 60% would be normal with azhdarchids. The necks of the prezygapophyses, the front joint processes, are well-developed and elongated, obliquely pointing forwards and outwards under an angle of 30° with the long axis of the vertebra. The preexapophysis, a secondary joint process on the side of the prezygapophysis, is well-developed with a forward pointing articulation facet and separated from a process, itself the remains of the diapophysis and possibly a neck rib, on the outer base of the prezygapophysis, by a deep trough on its underside. The pneumatic openings, the entrance holes for the air sacks, at the sides of the neural arch are small and placed in a low position.

 Eurazhdarcho was by the authors assigned to the Azhdarchidae, based on the method of comparative anatomy; a cladistic analysis was not performed.

 The area where Eurazhdarcho was found, in the Upper Cretaceous was localised on the Hațeg Island, part of the European Archipelago. The SbG-B site, though encompassing a surface of just 200 m³, has yielded several distinct animal species among which the turtle Kallokibotion bajazidi, the hadrosaur Telmatosaurus and a form referred to the titanosaur Magyarosaurus. This terrestrial fauna suggests that Eurazdarcho was not a coastal piscivore catching fish on the wing, affirming the "superstork" model for azhdarchids, in which they are terrestrial stalkers snatching small prey animals while walking on all fours.

 If Eurazhdarcho was indeed distinct from Hatzegopteryx, its discovery implies the presence of two azhdarchid forms in the Hațeg fauna, the one gigantic, the other medium-sized. This suggests a niche partitioning between them, although it is as yet unclear how this correlates with differences in prey preference and hunting techniques. This reflects a pattern seen in other Late Crataceous faunae which also show a combination of a large azhdarchid species with a smaller one. The Javalina Formation from the Maastrichtian of Texas has brought forth the giant Quetzalcoatlus northropi but also a smaller Quetzalcoatlus sp. and the azhdarchoid represented by specimen TMM 42489-2. The Two Medicine Formation fauna from the Campanian of Montana includes the smaller Montanazhdarcho minor, with a wingspan of 2.5 metres, but also fragments of larger forms with a span of eight metres. In the coeval Dinosaur Park Formation of Canada the smaller specimen RTMP 92.83 was discovered with a wingspan of five to six metres but also the large specimen PMA P.80.16.1367 indicating a ten metre wide animal.

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November 19th, 2014
02:53 pm
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Volgadraco

 Volgadraco ("Volga River dragon") is a genus of azhdarchid pterodactyloid pterosaur from the Upper Cretaceous of European Russia. It is known from lower beak (holotype SGU, no. 46/104a) and postcranial fragments from the early Campanian-age Rybushka Formation of Saratov, Russia. The size of this animal, and the development of blood supply in the lower jaw, are intermediate between older Santonian or Turonian azhdarchids like Azhdarcho and Bakonydraco and later Maastrichtian azhdarchids like Quetzalcoatlus. Volgadraco was described in 2008 by Averianov, Arkhangelsky, and Pervushov. The type species is V. bogolubovi, the specific name honouring Russian paleontologist Nikolai Nikolaevich Bogolubov. The authors consider the earlier named genus Bogolubovia to be a nomen dubium that in fact might be identical to Volgadraco.

 Ученые из Саратовского государственного технического университета во время полевых работ в верхнемеловых отложениях южной части саратовского правобережья обнаружили кости летающих ящеров-птерозавров. 

"По мнению ведущего российского специалиста по птерозаврам профессора Александра Аверьянова (Зоологический институт РАН, Санкт-Петербург), кости относятся к представителям семейства аждархид. Это самые крупные летающие создания на нашей планете, обитавшие в конце мелового периода. 

 Как выяснилось, ранее останки Volgadraco bogolubovi «Волжский дракон Боголюбова» уже находили. Они являлись самыми крупными летающими созданиями на нашей планете, обитавшими в конце мелового периода. Их размах крыльев был более 10 метров и пропитание они добывали, пикируя на поверхностью водоемов, высматривая рыбу плавающую на небольшой глубине.

 Новые находки были сделаны доцентом кафедры "Геоэкология и инженерная геология" Саратовского технического университета Максимом Архангельским и участником исследовательской группы "Искатели" Сергеем Меркуловым. 

 "Вместе с останками птерозавров обнаружены и кости морских рептилий - плезиозавров, мозазавров и черепах. В ближайшее время экспедиционные работы по сбору ископаемых останков мезозойских рептилий будут продолжены", - цитирует сообщение РИА "Новости".


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 Сравнение размеров с другими аждархидами и человеком, обозначен буквой I:


 


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01:32 pm
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Zhejiangopterus

 Zhejiangopterus is a genus of azhdarchid pterosaur known from one species, which lived in China during the late Cretaceous Period.

 The genus was named in 1994 by Chinese paleontologists Cai Zhengquan and Wei Feng. The type species is Zhejiangopterus linhaiensis. The genus name refers to Zhejiang Province and a Latinised Greek pteron, "wing". The specific name refers to the city of Linhai.

 In 1986 a young chalkstone quarry worker named Xu Chengfa, found a large fossil near the village of Aolicun. Xu by letter informed the director of the Zhejiang Museum of Natural History at Hangzhou, Ming Hua, who from it understood the remains were those of an unknown pterosaur. Therefore he sent a team consisting of the describers and Wu Weitang to investigate. They secured the fossil, instructing the local population to be alert for possible further finds. Xu himself managed to find three more specimens before being killed in an accident in 1988; another worker found a complete skull.

 In the early nineties in total six larger fossils had been recovered from the Tangshang Formation, an 81.5 million year old layer from the Campanian. Among those was the holotype, ZMNH M1330, the impression of the skull of a juvenile individual. Several paratypes were referred: ZMNH M1325, a skeleton lacking the skull; ZMNH M1328, an almost complete skeleton and ZMNH M1329, a fragmentary skeleton.

 Zhejiangopterus was a moderately large pterosaur. Its wingspan was first estimated at 5 metres (16.4 feet). Later estimates reduced this to about 3.5 metres (11.5 ft). Its skull was long, low, perfectly arched, and lacked a "keel" or any other crest sometimes seen in related species. The nasal opening and the large opening typically present between the nose and eye openings of archosaurs (the "antorbital fenestra") had joined together in species such as this to create a single oval opening that occupied nearly one half the length of the skull. The beak was long, thin, sharply pointed, and lacked teeth. The cervical vertebrae were elongated. The first six dorsal vertebrae had fused into a notarium. Several pairs of belly ribs were preserved. Its upper leg bone was half the size of its upper arm bone, and strong and thin. The wings were short but robust.

 Zhejiangopterus was by the original describers classified as a member of the Nyctosauridae, because of the two edentulous pterosaurs they possessed good descriptions of, Pteranodon and Nyctosaurus, it showed the most resemblance to the latter. They deplored lacking good data on Quetzalcoatlus. Indeed in 1997 David Unwin determined that Zhejiangopterus was more closely related to this giant American form and thus belonged to the Azhdarchidae. No other azhdarchid is known from such complete skeletal material.


 Репродукции (1, 2, 3, 4, 5, 6):


 


 


 


 


 


 


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October 23rd, 2014
04:11 pm
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Quetzalcoatlus

 Кетцалькоа́тль (Quetzalcoatlus) — крупнейший известный на сегодня представитель отряда птерозавров (Pterosauria). Типовой вид — Quetzalcoatlus northropi Lawson, 1975. Размах крыльев точно не известен из-за неполной сохранности останков, но по пропорциям птерозавров других видов оценивается приблизительно в 11 метров (по мнению некоторых палеонтологов — до 15 м). Обнаружен в позднемеловых отложениях Северной Америки. Время обитания — поздний меловой период, 68—65,5 миллионов лет назад.

 Весил, по разным оценкам, от 85 до 250 кг. Окаменелости кетцалькоатля обнаружены в Северной Америке. Название дано в честь ацтекского бога. В настоящее время кетцалькоатль вместе с другими гигантскими птерозаврами (Hatzegopteryx) являеся самым крупным известным летающим существом за всю историю жизни на планете. Кетцалькоатль и хатцегоптерикс были примерно одинакового размера, только первый был немного более массивным. Кетцалькоатль летал над сушей и питался падалью и мелкими позвоночными. Возможно, он мог поймать и небольшого динозавра весом до 30 килограммов.

 Изначально размах крыльев оценили в 15,9 метров, усреднив оценку через пропорции других птерозавров. Однако в ходе исследования 1981 года оценочный размер уменьшили до 11—12 метров. Более поздние исследования ещё уменьшили размер Q. до 10—11 метров.

 Оценить массу гигантских аждархидов очень сложно, поскольку нет существующих видов схожего размера или строения, поэтому в разных публикациях результаты разнятся. В то время как некоторые исследования традиционно указывают крайне низкую оценочную массу, как например 70 кг для 10-и метровой особи, большинство оценок, опубликованных с начала 2000-х, указывают на массу в районе 200 кг.

 О жизненном укладе Q. существует несколько предположений. Поскольку кости были найдены в сотнях километров от береговой линии, и не было найдено следов больших рек или глубоких озёр, Дуглас Лоусон в 1975 году отверг рыболовную натуру Q., предположив, что животное питалось падалью подобно африканскому марабу. Лоусон нашел останки гигантского птерозавра во время поисков костей аламозавра, бывшего важной частью экосистемы.

 В 1996 году Томас Леман и Лангстон указали, что строение нижней челюсти отличается от таковой у типичных птиц-падальщиков. Они предположили, что длинная шея и длинные беззубые челюсти позволяли Q. питаться примерно как современные водорезы, ловя рыбу во время полета над водой, прочесывая волны клювом.

 Исследование 2007 года показало, что для такого большого птерозавра подобный полет был бы слишком энергозатратным из-за сильного лобового сопротивления.

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Репродукции (1, 2, 3, 4, 5, 6, 7, 8, 9, 10, 11, 12):


 


 



 


 


 

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 Размеры тела в сравнении с человеком:


 


 

 Ископаемые останки и реплики (1, 2, 3):


 


 


 


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October 11th, 2014
02:40 pm
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Phosphatodraco
 
 Phosphatodraco (meaning "phosphate dragon", in reference to the phosphates of Morocco, the country where it was found) is a genus of azhdarchid pterodactyloid pterosaur from a late Maastrichtian-age Upper Cretaceous portion of the Oulad (or Qualad) Abdoun Phosphatic Basin, Grand Doui, near Khouribga, central Morocco.

 Phosphatodraco is based on holotype OCP DEK/GE 111, found in 2000, which is composed of five associated, though disarticulated and compressed, damaged cervical vertebrae and a bone of unknown origin. The cervical vertebrae are thought to be a series from the fifth (the longest with a length of thirty centimeters) to the ninth. The individual to which the neck belonged would have had a wingspan of about five meters (16.4 feet). It is unusual among azhdarchids for having elongate vertebrae at the base of the neck (also with neural spines), interpreted as modified dorsal vertebrae; the neck is also one of the most complete known for azhdarchids. It was one of the last pterosaurs before the Cretaceous–Paleogene extinction event that finished off the group, and is the first azhdarchid found in northern AfricaP. mauritanicus is the type and only known species. The specific name refers to Mauretania.


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                                             Вместе с саркозухом.


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September 27th, 2014
04:45 pm
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Montanazhdarcho
 
 Montanazhdarcho is a genus of azhdarchid pterosaur from the late Cretaceous Period (Campanian stage) of North America, known from only one species, M. minor.

 The genus was named in 1993 by Kevin PadianArmand de Ricqlès, and Jack Horner, again published by the same authors in 1995 and fully described in 2002.

 The type species is Montanazhdarcho minor. The genus name refers to Montana and to the related species Azhdarcho. The specific name means "the smaller one" in Latin, a reference to the relatively small size in comparison to closely related forms.

 The holotypeMOR 691 (Museum of the Rockies), was found by Robert W. Harmon inGlacier County, in the territory of the Blackfoot, in sandstone of the Upper Two Medicine Formation, a layer about 74 million years old. The fossil is largely uncompressed and that of an adult exemplar, as established by a study of the bone by de Ricqlès. It consists of a partial left wing, lacking the outer three wing finger phalanges, a complete shoulder girdle, a crushed cervical vertebra and two fragments of the symphysis of the mandible. The jaws were edentulous, i.e.: they lacked teeth.

 Montanazhdarcho was by the authors assigned to the Azhdarchidae, mainly based on the elongated form of the neck vertebra. Compared to other azhdarchids, it was small; the fragments of humerusradius, and carpal suggest an animal with a 2.5 meter wingspan (eight feet). Its ulna was longer than the wing metacarpal, which is atypical for azhdarchids.


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May 30th, 2014
07:38 pm
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Hatzegopteryx

 Hatzegopteryx (рум. Hațeg — название румынского города, πτέρυξ — крыло) — род аждархидовых птерозавров, известный по останкам, найденным в Трансильвании в 2002 году. Черепные фрагменты, левая плечевая кость, и другие ископаемые останки указывают на то, что Hatzegopteryx был одним из самых крупных птерозавров.

 Род был назван в 2002 году французским палеонтологом Eric Buffetaut и румынскими палеонтологами Dan Grigorescu и Zoltan Csiki. Включает в себя только один вид Hatzegopteryx thambema. Название рода образовано от румынского города Хацег (кости Hatzegopteryx были найдены в районе так называемого «Hațeg Island (англ.)») и греч. πτέρυξ «крыло». Видовое название thambema образовано от греч. "монстр" и отсылает к размерам Hatzegopteryx.

 Останки Hatzegopteryx относятся к Densus Ciula Formation в западной Румынии, которая датируется поздним маастрихтом (верхний мел, приблизительно 65 млн лет назад). Голотип, FGGUB R 1083A, состоит из задней части черепа и поврежденной проксимальной части левой плечевой кости. 38,5-сантиметровый диафиз бедренной кости, найденный поблизости (FGGUB R1625), может тоже принадлежать Hatzegopteryx.

 Hatzegopteryx, предположительно, имел крепкий расширяющийся в задней части череп и массивные челюсти. Многие ископаемые кости Hatzegopteryx сильно схожи с костями Quetzalcoatlus sp., но у Hatzegopteryx был намного более тяжелый череп и другое сочленение челюстей, похожее на таковое у птеранодона. Сравнивая с черепами других птерозавров: Nyctosaurus и Anhanguera, Buffetaut с коллегами, при описании найденных образцов дают оценку длины черепа Hatzegopteryx до 3 м, что больше, чем у кетцалькоатля.

 Авторы оценивали размер Hatzegopteryx, сравнивая фрагмент плечевой кости длиной 23,6 см, с плечевой костью кетцалькоатля, считавшегося ранее самым крупным известным птерозавром. Образец кетцалькоатля TMM 41450-3 имеет плечевую кость длиной 54,4 см. Фрагмент плечевой кости Hatzegopteryx меньше половины целой, поэтому она, скорее всего, была немного длиннее кости кетцалькоатля. Размах крыльев последнего был в 1981 году оценен в 11—12 метров, более ранние оценки же говорили о 15—20 метрах. Отсюда авторы заключили, что оценка размаха крыла в 12 метров достаточно скромна, «если его плечевая кость была действительно длиннее, чем таковая у Q. northropi». В 2003 году оценки были пересмотрены: размах крыльев  Hatzegopteryx был оценен приблизительно в 12 метров, а длина черепа — свыше 2,5 метра. В 2010 году Mark Witton заявил, что кажущееся превосходство размеров плечевой кости Hatzegopteryx вызвано её деформацией после отложения в породе, так что, вероятно, размах крыльев Hatzegopteryx был не больше, чем размах крыльев кетцокоатля, сегодня обычно оцениваемый в 10—11 метров.

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 Репродукции (1, 2, 3, 4, 5, 6, 7, 8, 9):


 


 


 


 


 

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 Размеры тела в сравнении с человеком и жирафом:


 


 


 Ископаемые останки:


 


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April 30th, 2014
12:54 pm
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Azhdarcho

 Azhdarcho /ɑːʒˈdɑrx/ is a genus of pterodactyloid pterosaur from the late Cretaceous Period of the Bissekty Formation (middle Turonian stage, about 92 million years ago) of Uzbekistan. It is known from fragmentary remains including the distinctive, elongated neck vertebrae that characterizes members of the family Azhdarchidae, which also includes such giant pterosaurs as Quetzalcoatlus. The name Azhdarcho comes from the Uzbek word azhdarkho [adʒˈdarχɒ], the name of a dragon in Uzbek mythology. The type species is Azhdarcho lancicollis. The specific epithet lancicollis is derived from the Latin words lancea (meaning "lance" or "spear") and collum ("neck").

 The fossil remains of Azhdarcho were recovered in the Kyzyl Kum desert (from the Taykarshinskaya unit of the Bissekty Formation) by Lev A. Nesov during expeditions to Central Asia in 1974-1981. The type specimen, given the catalog number TsNIGRmuzey 1/11915, consists of an anterior neck vertebra. Twelve paratypes were referred, including several other neck vertebrae, elements from the wing and leg, and pieces of the jaw. These specimens, along with other vertebrate fossils collected during the expeditions, were deposited at the F.N. Chernyshev Central Geologic Exploration Museum in St. Petersberg.

 In his description of the type specimen of Azhdarcho lancicollis, Nesov noted its distinctive neck vertebrae, which are extremely elongated and round in cross section at mid-length. He pointed out similar characteristics in several other pterosaurs, and used them to erect the new subfamily Azhdarchinae, within the Pteranodontidae. Nesov also referred Quetzalcoatlus and Arambourgiania (then known as Titanopteryx) to this subfamily, which was subsequently re-classified as the family Azhdarchidae. He also suggested that similar, thin-walled pterosaur bones from the Lance Formation of Wyoming could be assigned to a species of Azhdarcho, using this as evidence of commonalities between the fauna of Late Cretaceous central Asia and western North America. However, subsequent research has not followed this suggestion, and A. lancicollis is the only currently recognized species of Azhdarcho.

 In the original description of Azhdarcho, Nesov noted that because of the way the vertebrae articulated, the pterosaur would have had very limited flexibility in the neck. Azhdarcho could not rotate its neck at all, though it could flex the neck vertically to a certain degree. Nesov suggested that pterosaurs like Azhdarcho may have fed in a manner similar to the modern Skimmer, with their long necks allowing them to scoop prey from the water's surface and small depths without needing to dive. However, recent research has shown that skimming requires more energy and anatomical specializations than previously thought, and that large pterosaurs like Azhdarcho probably were not capable of skimming. The long neck would also have allowed azhdarchids to hunt for food in the water or on the bottom while swimming, or to hunt poorly-flying vertebrates in the air, though Nesov also suggested that the animal would have needed stable weather conditions to fly well, and suggested azhdarchid habitats needed to be dominated by even, mild winds.

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 Репродукции (1, 2, 3, 4):

 

 


 


 


 


 Ископаемые останки (1, 2, 3, 4):


 


 


 


 


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April 23rd, 2014
12:56 pm
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Arambourgiania

 Arambourgiania is a pterosaur from the Late Cretaceous (Maastrichtian) of Jordan. It was one of the largest members of this group.

 In the early forties, a railway worker during repairs on the Amman-Damascus railroad near Russeifa found a two feet long fossil bone. In 1943 this was acquired by the director of a nearby phosphate mine, Amin Kawar, who brought it to the attention of a British archeologist, Fielding, after the war. This generated some publicity — the bone was even shown to Abdullah I of Jordan — but more importantly, it made the scientific community aware of the find.

 In 1953 the fossil was sent to Paris, where it was examined by Camille Arambourg of the Muséum national d'histoire naturelle. In 1954, he concluded the bone was the wing metacarpal of a giant pterosaur. In 1959, he named a new genus and species: Titanopteryx philadelphiae. The genus name meant "titan wing" in Greek; the specific name refers to the name of Amman in Antiquity: Philadelphia. Arambourg let a plaster cast be made and then sent the fossil back to the phosphate mine; this last aspect was later forgotten and the bone was assumed lost.

 In 1975 Douglas A. Lawson, studying the related Quetzalcoatlus, concluded the bone was not a metacarpal but a cervical vertebra.

 In the eighties, Russian paleontologist Lev Nesov was informed by an entomologist that the name Titanopteryx had already been given by Günther Enderlein to a fly from the Simulidae family in 1934. Therefore, in 1987 he renamed the genus into Arambourgiania, honouring Arambourg. However, the name "Titanopteryx" was informally kept in use in the West, partially because the new name was assumed by many to be a nomen dubium.

 Early 1995, paleontologists David Martill and Eberhard Frey traveled to Jordan in an attempt to clarify matters. In a cupboard of the office of the Jordan Phosphate Mines Company they discovered some other pterosaur bones: a smaller vertebra and the proximal and distal extremities of a wing phalanx — but not the original find. However, after their departure to Europe engineer Rashdie Sadaqah of the mine investigated further and in 1996 established it had been bought from the company in 1969 by geologist Hani N. Khoury who had donated it in 1973 to the University of Jordan; it was still present in the collection of this institute and now could be restudied by Martill and Frey.

The holotype, VF 1, consists of a very elongated cervical vertebra, probably the fifth. Today the middle section is missing; the original find was about 62 centimetres long, but had been sawed into three parts. Most of the fossil consists of an internal infilling or mould; the thin bone walls are missing on most of the surface. The find had not presented the whole vertebra; a piece was absent from its posterior end as well. Frey and Martill estimated the total length to have been 78 centimetres, using for comparison the relative position of the smallest shaft diameter of the fifth cervical vertebra of Quetzalcoatlus. From this again the total neck length was extrapolated at about three metres. From the relatively slender vertebra the length dimension was then selected to be compared to that of Quetzalcoatlus, estimated at 66 centimeters long, resulting in a ratio of 1.18. Applying that ratio to the overall size, Frey and Martill in 1998 concluded that the wingspan of Arambourgiania had been twelve to thirteen metres, compared with the ten to eleven metres of Quetzalcoatlus, and that Arambourgiania was thus the largest pterosaur then known. Later estimates have been more moderate, sometimes as low as seven metres.

 Frey and Martill rejected the suggestion that Arambourgiania was a nomen dubium or identical to Quetzalcoatlus and affirmed its validity in relation to "Titanopteryx".

 Nesov in 1984 had placed the species within Azhdarchinae, part of the Pteranodontidae; the same year Kevin Padian placed it within Titanopterygidae. Both concepts have fallen into disuse now that such forms are commonly assigned to the Azhdarchidae.


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10:48 am
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Alanqa

 Alanqa (от араб. «Al Anqa» — феникс) — вымерший род птеродактелей, обитавший в меловом периоде примерно 95 млн лет назад. Ископаемые останки были найдены в отложениях сеноманского яруса в Марокко и описаны в 2010 году. Единственный известный вид — Alanqa saharica Ibrahim et a., 2010.

 Название птеродактиля Alanqa saharica происходит от арабского слова «Al Anqa», которое означает «Феникс», а видовое название saharica указывает на то, что данный вид был обнаружен в пустыне Сахара.

 Описание A. saharica основано на исследовании челюстной кости длиной 344 мм, составленной из трёх отдельных фрагментов. Также были найдены фрагменты шейных позвонков, принадлежавших, вероятно, A. saharica. Длина птеродактеля составляла примерно шесть метров. Отличительной особенностью A. saharica является отсутствие зубов. Является одним из древнейших известных представителей семейства аждархид.

 Окаменелости птерозавра находились на территории древней Гондваны (на территории современного Марокко), однако подавляющее большинство сравнимых по возрасту экземпляров аждархид было обнаружено на землях бывшей Лавразии. Так же рядом с останками Alanqa были обнаружены 2 других вида птерозавров, что свидетельствует о тесном соседстве разных видов птерозавров на одной территории и на одном промежутке времени.

 Aided by local villagers, a team of paleontologists had been excavating at several locations in the Kem Kem Beds during April, and November to December 2008, uncovering remains of several different pterosaurs. The material was fragmentary, and the type locality for Alanqa is Aferdou N'Chaft, near the village of Begaa and 10 km to the north-east of Taouz.

 Alanqa is known only from five fragments of the front upper and lower jaws, and possibly a neck vertebra, representing the single type species Alanqa saharica. Two of these fragments were first described, but not named, by Wellnhofer and Buffetaut in 1999. Three additional jaw specimens, including a better preserved upper jaw, were described and named by Ibrahim and colleagues in 2010. The jaws were straight and pointed, like those of Quetzalcoatlus and Zhejiangopterus, so while it was originally proposed as a pteranodontid, it is more likely Alanqa was an azhdarchid. Based on comparison to related species, the Alanqa saharica the individuals known from jaw specimens probably had wingspans of about 4 meters (about 13 ft). However, according to Ibrahim and colleagues, the vertebra (which probably belonged to the same species) appeared to come from a larger individual, measuring about 6 meters (about 20 ft) in wingspan.

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