The Museum of Evolution of Polish Academy of Sciences (Polish : Muzeum Ewolucji Instytutu Paleobiologii Polskiej Akademii Nauk) is the display area of the natural history museum in Warsaw, Poland. [1] It is the public front of the Muzeum i Instytut Zoologii or Zoology Museum and the Instytut Paleobiologii or Paleobiology Institute. It is based at the Palace of Culture and Science. [2]
In the halls of the Palace of Culture and Science in Warsaw, professor Zofia Kielan-Jaworowska organised an exhibition named "Dinosaurs of the Gobi Desert" in 1968. It was open until 1984 and featured the discoveries of Polish-Mongolian palaeontological missions to the Gobi Desert. [3]
The Museum of Evolution was founded in 1984 when the Institute of Paleobiology took over the exhibition halls that the Institute of Zoology, Polish Academy of Sciences, had been using in the Youth Palace (a section of the Palace of Culture of Science). The public was first given access to the "Evolution on Land" permanent exhibition in 1985, which was created by Zofia Kielan-Jaworowska with support from Andrzej Sulimski and a group from the Institute of Paleobiology. Many specimens gathered during the excursions to Mongolia were on display in the show. A section of the exhibit was also devoted to contemporary creatures, especially insects and birds, with specimens from the Institute and Museum of Zoology's collections on display. [1]
A new display showcasing the Late Triassic amphibians and reptiles found in Krasiejów close to Opole opened in 2001. Both actual fossil material from the Krasiejów site and life-size replicas of both land and marine species discovered there are included in the display.
A life reconstruction of the Australopithecus specimen "Lucy" was added to the museum's anthropology section in 2003.
The Museum of Evolution's gallery underwent additional development in 2005. The two new skeletal reconstructions of the Mongolian dinosaurs Tarbosaurus and Opisthocoelicaudia, based on the most recent scientific knowledge of their anatomy, were among the notable contributions.
In 2009, to commemorate the 150th anniversary of the publication of Charles Darwin's "On the Origin of Species," the permanent exhibition of the Museum of Evolution was substantially expanded. [4]
The majority of the exhibit's dinosaur skeletons were discovered during Polish-Mongolian expeditions to the Gobi Desert in the 1960s and 1970s under the direction of Zofia Kielan-Jaworowska. The gigantic skeletal replica of the enormous plant-eating sauropod dinosaur Opisthocoelicaudia fills practically the whole main exhibition hall at the Museum of Evolution. Nemegtosaurus, a separate sauropod dinosaur from the Gobi, whose skull was put on this skeletal reconstruction, was discovered a few kilometres from Opisthocoelicaudia's skeleton. However, other palaeontologists claim that the skull and the skeleton belong to the same species. [5]
Other specimens from the Gobi, besides Opisthocoelicaudia, can be found in the museum's largest exhibition hall, including fossilised dinosaur eggs, the remains of early horned (ceratopsian) and armoured (ankylosaur) dinosaurs, as well as the tiny skulls of Cretaceous mammals that coexisted with the giant dinosaurs and lived in their shadow. [5]
The skulls and skeletons of enormous carnivorous dinosaurs found in the Cretaceous rocks of the Gobi Desert are also among the exhibits at the museum, and they are on show in a separate exhibition hall. The main attraction is two skeletal mounts of the Tarbosaurus, an Asian relative of the well-known Tyrannosaurus rex. The present understanding of the anatomy of this dinosaur is reflected in the first mount, which depicts the animal with its backbone parallel to the ground. The second historical mount depicts Tarbosaurus in a stance reminiscent of a kangaroo, in line with past theories of dinosaur mobility. These two dissimilar mounts serve as a great illustration of how far dinosaur knowledge has come in the last 50 years. The massive front limbs of Deinocheirus were discovered in the Gobi Desert in 1965, and its identity was unknown until more complete skeletons were discovered in 2014, proving that Deinocheirus was a large ostrich-like dinosaur. [5]
A group of young scientists led by professor Jerzy Dzik made some of Poland's main palaeontological discoveries in Krasiejów, close to Opole, where they uncovered a cemetery of Late Triassic reptiles and amphibians in 1993. [6]
The Krasiejów locality's actual "gemstone" turned revealed to be Silesaurus, a prehistoric relative of dinosaurs. The second major focus of the Museums' exhibition is on the skeletons of various terrestrial and marine species, as well as live reconstructions of such animals.
The Museum also has other Polish fossils on exhibit, including the oldest frog skeleton ever discovered, which was revealed in Triassic rocks from the area of Cracow. [7]
The casts of pterosaurs and early birds from the renowned German Jurassic Solnhofen limestone, which are some of the best fossil specimens confirming Darwin's theory of evolution, are among the other displays. The Mammal Evolution Hall has a realistic reconstruction of the Australopithecus 'Lucy,' which was made by sculptor Marta Szubert under the direction of Karol Sabath, a Polish evolutionary popularizer. [5] [8] [9] [10] [11]
Tarbosaurus is a genus of tyrannosaurine theropod dinosaur that lived in Asia about 70 million years ago, during the Maastrichtian age at the end of the Late Cretaceous period, considered to contain a single known species: Tarbosaurus bataar. Fossils have been recovered from the Nemegt Formation of Mongolia, with more fragmentary remains found further afield in the Subashi Formation of China.
Sinobaatar is a genus of extinct mammal from the Lower Cretaceous of China. It is categorized within the also extinct order Multituberculata and among these it belongs to the plagiaulacid lineage. Sinobaatar was a small herbivore during the Mesozoic era, commonly called "the age of the dinosaurs". The genus was named by Hu Y. and Wang Y. in 2002. Three species have been described.
Sloanbaataridae is a family of fossil mammals within the extinct order Multituberculata. Remains are known from the Upper Cretaceous of Mongolia. These small herbivores lived during the "age of the dinosaurs". This family is part of the suborder Cimolodonta. The family Sloanbaataridae was named by Kielan-Jaworowska, Z. in 1974.
Kamptobaatar is a Mongolian mammal genus from the Upper Cretaceous. It lived at the same time as the later dinosaurs. This animal was a member of the extinct order Multituberculata within the suborder Cimolodonta and family Sloanbaataridae.
Bulganbaatar is a Central Asian mammal genus from the Upper Cretaceous. It existed in the company of dinosaurs. This animal was a member of the extinct order Multituberculata. It's within the suborder Cimolodonta and is a member of the superfamily Djadochtatherioidea. The genus Bulganbaatar was named by Kielan-Jaworowska Z. in 1974.
Nemegtbaatar is a genus of mammal from the Upper Cretaceous Period of what is now Mongolia. It existed in the company of much larger dinosaurs, found together in the Nemegt Basin. This creature was a member of the extinct order Multituberculata. It is within the suborder Cimolodonta and is a member of the superfamily Djadochtatherioidea. It was a hopping, gerboa-like species.
Catopsbaatar is a genus of multituberculate, an extinct order of rodent-like mammals. It lived in what is now Mongolia during the late Campanian age of the Late Cretaceous epoch, about 72 million years ago. The first fossils were collected in the early 1970s, and the animal was named as a new species of the genus Djadochtatherium in 1974, D. catopsaloides. The specific name refers to the animal's similarity to the genus Catopsalis. The species was moved to the genus Catopsalis in 1979, and received its own genus in 1994. Five skulls, one molar, and one skeleton with a skull are known; the last is the genus' most complete specimen. Catopsbaatar was a member of the family Djadochtatheriidae.
Kryptobaatar, also known as Gobibaatar or Tugrigbaatar, is an extinct mammalian genus dating from the Upper Cretaceous Period and identified in Central Asia. This animal was a member of the extinct order of Multituberculata within the suborder Cimolodonta, and was a member of the family Djadochtatheriidae. It lived contemporaneously with some of the dinosaurs. Its skull had a length of perhaps 3 cm.
Deinocheirus is a genus of large ornithomimosaur that lived during the Late Cretaceous around 70 million years ago. In 1965, a pair of large arms, shoulder girdles, and a few other bones of a new dinosaur were first discovered in the Nemegt Formation of Mongolia. In 1970, this specimen became the holotype of the only species within the genus, Deinocheirus mirificus; the genus name is Greek for "horrible hand". No further remains were discovered for almost fifty years, and its nature remained a mystery. Two more complete specimens were described in 2014, which shed light on many aspects of the animal. Parts of these new specimens had been looted from Mongolia some years before, but were repatriated in 2014.
Saurolophus is a genus of large hadrosaurid dinosaur from the Late Cretaceous period of Asia and North America, that lived in what is now the Horseshoe Canyon and Nemegt formations about 70 million to 66 million years ago. It is one of the few genera of dinosaurs known from multiple continents. The type species, S. osborni, was described by Barnum Brown in 1912 from Canadian fossils. A second valid species, S. angustirostris, is represented by numerous specimens from Mongolia, and was described by Anatoly Konstantinovich Rozhdestvensky.
Nemegtosaurus was a sauropod dinosaur from the Late Cretaceous Period of what is now Mongolia. It was named after the Nemegt Basin in the Gobi Desert, where the remains — a single skull — were found. The skull resembles diplodocoids in being long and low, with pencil-shaped teeth. However, recent work has shown that Nemegtosaurus is in fact a titanosaur, closely related to animals such as Saltasaurus, Alamosaurus and Rapetosaurus.
Opisthocoelicaudia is a genus of sauropod dinosaur of the Late Cretaceous Period discovered in the Gobi Desert of Mongolia. The type species is Opisthocoelicaudia skarzynskii. A well-preserved skeleton lacking only the head and neck was unearthed in 1965 by Polish and Mongolian scientists, making Opisthocoelicaudia one of the best known sauropods from the Late Cretaceous. Tooth marks on this skeleton indicate that large carnivorous dinosaurs had fed on the carcass and possibly had carried away the now-missing parts. To date, only two additional, much less complete specimens are known, including part of a shoulder and a fragmentary tail. A relatively small sauropod, Opisthocoelicaudia measured about 11.4–13 m (37–43 ft) in length. Like other sauropods, it would have been characterised by a small head sitting on a very long neck and a barrel shaped trunk carried by four column-like legs. The name Opisthocoelicaudia means "posterior cavity tail", alluding to the unusual, opisthocoel condition of the anterior tail vertebrae that were concave on their posterior sides. This and other skeletal features lead researchers to propose that Opisthocoelicaudia was able to rear on its hindlegs.
Bagaceratops is a genus of small protoceratopsid dinosaurs that lived in Asia during the Late Cretaceous, around 72 to 71 million years ago. Bagaceratops remains have been reported from the Barun Goyot Formation and Bayan Mandahu Formation. One specimen may argue the possible presence of Bagaceratops in the Djadochta Formation.
Tylocephale is a genus of pachycephalosaurid dinosaur, a group of dome-headed, herbivorous ornithischians, that lived during the Late Campanian stage of the Late Cretaceous in what is now Mongolia. It is known from a partial skull and associated mandible that were unearthed in 1971 by a Polish-Mongolian Expedition to the Barun Goyot Formation of the Gobi Desert. The specimen was described in 1974 by Polish paleontologists Teresa Maryańska and Halszka Osmólska as a new genus and species.
Gobipteryx is a genus of prehistoric bird from the Campanian Age of the Late Cretaceous Period. 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.
The Djadochta Formation is a highly fossiliferous geological formation situated in Central Asia, Gobi Desert, dating from the Late Cretaceous period, about 75 million to 71 million years ago. The type locality is the Bayn Dzak locality, famously known as the Flaming Cliffs. Reptile and mammal remains are among the fossils recovered from the formation.
Teresa Maryańska was a Polish paleontologist who specialized in Mongolian dinosaurs, particularly pachycephalosaurians and ankylosaurians. Peter Dodson states that in 1974 Maryanska together with Halszka Osmólska were among the first "women to describe new kinds of dinosaurs". She is considered not only as one of Poland's but also one of the world's leading experts on dinosaurs.
Karol Sabath was a Polish biologist, paleontologist and paleoartist. He was employed by the Instytut Paleobiologii of the Polska Akademia Nauk - Institute of Paleobiology, Polish Academy of Sciences, Warsaw. He also worked for National Geographic magazine, the Museum of the Polish Geological Institute, the European edition of Scientific American, and various other publishing houses in Poland. He authored many popular-science books for children, did translations, and wrote popular-science articles for Polish national newspapers. He was a scientific advisor for many popular-science events, including reconstructions of paleobiological environment and specimens.
Zofia Kielan-Jaworowska was a Polish paleobiologist. In the mid-1960s, she led a series of Polish-Mongolian paleontological expeditions to the Gobi Desert. She was the first woman to serve on the executive committee of the International Union of Geological Sciences. The most notable dinosaur species she discovered include: Deinocheirus and Gallimimus while Kielanodon and Zofiabaatar were named in her honour.
The "Gurlin Tsav" skull is a currently unnamed carnivorous metatherian fossil from the Nemegt Formation of Mongolia. Composed of a single semi-complete skull, this specimen is notable in regards to the evolution and systematics of Metatheria as a whole, and thus nigh-omnipresent in phylogenetic analyses of this group.
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