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{{Short description|Extinct genus of mammals}}
{{Italic title}}
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'''''Pliohyrax''''', is a genus of hyracoidshyracoid, (thea cavy-likeclade group of animalsof mostmammals closely related to [[elephants]] and [[manatees]]). It grew to sizes greatlylargely exceeding those of any living [[hyrax]], thoughbut it was by no means the largest member of thisits family.
 
[[File:PliohyraxDB22.jpg|thumb|left|[[Life restoration]]]]
Fossils of this [[Miocene]]-[[Pliocene]], [[Arboreal locomotion|scansorial]] [[herbivore]] have been found inthroughout Afghanistan,Southern France,Europe and TurkeyWestern Asia.<ref>{{Cite web | title = Pliohyrax | publisher = Paleobiology Database | url = http://paleodb.org/cgi-bin/bridge.pl?a=basicTaxonInfo&taxon_no=43305 | accessdate = 25 August 2012}}</ref>
In Spain, ''Pliohyrax graecus'' is among the large mammals species found in the [[Almenara, Castellón|Almenara]] site, deposited during the [[Messinian salinity crisis]], together with ''[[Macaque|Macaca]]'' sp., [[Bovidae]] indet., cf. ''[[Nyctereutes]]'' sp., and [[Felidae]] indet.<ref>{{Cite journal | last1 = Agustí | first1 = Jordi | last2 = Garcés | first2 = Miguel | last3 = Krijgsman | first3 = Wout | title = Evidence for African–Iberian exchanges during the Messinian in the Spanish mammalian record | journal = Palaeogeography, Palaeoclimatology, Palaeoecology | year = 2006 | volume = 238 | issue = 1–4 | pages = 5–14 | url = http://www.geo.uu.nl/~forth/publications/Agusti_2006.pdf | doi = 10.1016/j.palaeo.2006.03.013| bibcode = 2006PPP...238....5A }}</ref>
 
==History==
 
[[File:Leptodon Gaudry 1867.png|thumb|left|HolotypeType mandible of ''Pliohyrax graecus'']]
 
In 1853, following a field trip in [[Cyprus]], French palaeontologist and geologist [[Albert Gaudry]] stopped in [[Greece]] on his way back to [[France]], and, on the invitation of the [[List of ambassadors of France to Greece|ambassador of France to Greece]] [[Alexandre de Forth-Rouen]], visited a local fossil site at [[Pikermi]], in the [[Attica]] peninsula, near [[Athens]], first visited by German scientists. Gaudry immediatly recognized the importance of the deposits and led, in 1855 and in 1860, two excavation campaigns in Attica under the commission of the [[French Academy of Science]]. In Pikermi, Gaudry excavated the fossils of a diverse fauna whose preservation was almost unprecedented in the Neogene of Europe. Among those discoveries figured two large but isolated mandibles belonging to the same adult individual of a yet unknown large species of mammal. In a seminal book published in 1862, Gaudry described these incomplete remains under the name ''Leptodon graecus'', after the slender shape of its molars. At the time of Gaudry, [[Hyracoid]]s, [[Proboscidean]]s, [[Perissodactyl]]s and [[Artiodactyl]]s were classified together within the order [[Pachydermata]]. Gaudry speculated that ''Leptodon'' was an extinct member of a clade including the modern [[rhinoceros]] and [[hyrax]]es.<ref name=Gaudry1862>{{cite book |last1=Gaudry|first1=A. |date=1862-1867|title=Animaux fossiles et géologie de l'Attique, d'après les recherches faites en 1855, 1856 et 1860 par Albert Gaudry|publisher=F. Savy (Paris) |orig-date= |pages=474 p.}}
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In 1995, a study by [[Gary T. Schwartz]], [[David Tab Rasmussen]] and [[Richard J. Smith]] estimated the size of extinct hyracoids based on the of their dentition and proposed that ''P. chardini'' weighed between 900 and 1432 kg.<ref name=Schwartz1995>{{cite journal|first1=G.T.|last1=Schwartz|first2=D.|last2=Tab Rasmussen|first3=R.J.|last3=Smith|title=Body-size diversity and community structure of fossil hyracoids|date=1995|journal=Journal of Mammalogy|volume=76(4)|pages=1088-1099}}</ref> In 1996, [[Zong Guanfu]] described a new species of ''Postschizotherium'', ''P. tibetensis'', from the [[Hengduan Mountains]] of [[Sichuan]], China, based on a maxilla and two mandibles, and referred to the genus an additional maxilla from the same site.<ref name=Zong1996>{{cite book |last=Zong|first=G.F.|date=1996|editor-last1=Zong|editor-first1=G.F.|editor-last2=Chen|editor-first2=W.Y.|editor-last3=Huang|editor-first3=X.S.|title=Cenozoic Mammals and Environment of Hengduan Mountains Region|pages=61-80|chapter=Hyracoidea Huxley|isbn=}}</ref>
In 2002, Qiu, [[Wei Qi]], [[Pei Shuwen]] and [[Chen Zheying]] redescribed ''P. intermedium'' on the basis of two new crania associated with their mandibles collected by Wei and Chen between 1981 and 1983 in the locality 81018, in [[Tianzhen County]], [[Shanxi]]. Additionaly, they considered that the holotype of ''P. licenti'' had been misidentified and that it was therefore a junior synonym of ''P. chardini'', and that most of the material referred to ''Postschizotherium'' by Zong in 1996 belonged in reality to [[Schizotheriinae|schizotheres]], although the maxilla designated as type for ''P. tibetensis'' was genuine.<ref name=Qiu2002>{{cite journal|first1=Z.|last1=Qiu|first2=Q.|last2=Wei|first3=S.|last3=Pei|first4=Z.|last4=Chen|title=Preliminary report on Postschizotherium (Mammalia: Hyarcoidea) material from Tianzhen, Shanxi, China|date=2002|journal=Vertebrata PalAsiatica|volume=40(2)|pages=146-160}}</ref> In 2003, [[Chen Guanfang]] erected ''P. tibetensis'' as its own genus, ''[[Hengduanshanhyrax]]''.<ref name=Chen2003>{{cite journal|first1=G.|last1=Chen|title=A new genus of Pliohyracinae (Hyracoidea, Mammalia) from the Late Pliocene of Dege, Sichuan, China|date=2003|journal=Vertebrata PalAsiatica|volume=41(3)|pages=240-248}}</ref>
 
In 2009, [[Nakaya Hideo]], [[Takai Masanaru]], [[Fukuchi Akira]] and [[Ogino Shintaro]] reported the first fossil remains of ''Postschizotherium'' outside of China. The material, consisting in several associated teeth, were collected near [[Udunga]], [[Buryatia]], in [[Transbaikal|Transbaikalian]] [[Russia]], and was originally described as ''Postschizotherium'' cf. ''chardini''.<ref name=Nakata2009>{{cite journal|first1=H.|last1=Nakaya|first2=M.|last2=Takai|first3=A.|last3=Fukuchi|first4=S.|last4=Ogino|title=A preliminary report on some fossil mammals (Equidae, Perissodactyla and Hyracoidea) from the Pliocene Udunga fauna, Transbaikalia, Russia|date=2009|journal=Asian Paleoprimatology|volume=5|pages=99-104}}</ref>
 
=Prohyrax=
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From 1961 to 1967, expeditions organized by [[Yale University]] to the [[Fayoum]] uncovered a rich diversity of fossil taxa from the [[Jebel Qatrani Formation]]. Among the remains were a vast array of fragmentary dentaries and associated postcranial remains belonging to a new type of hyracoid, collected between 1962 and 1967 in the quarries G, M and I. In 1973, [[Grant E. Meyer]], who had participated in the expeditions, described formally the remains as the new genus and species that he named ''Thyrohyrax domorictus'', based on the only fragmentary right mandible collected in Quarry M during the last year of the expeditions by Meyer himself. Meyer noted the great resemblance between ''Thyrohyrax'' and ''[[Meroehyrax]]'', then placed among the [[Pliohyracinae]], and proposed that ''T. domorictus'', while a [[Sagatheriinae]], was closely related to the last common ancestor of the more derived pliohyracins.<ref name=Meyer1973>{{cite journal|first1=G.E.|last1=Meyer|title=A new Oligocene hyrax from the Jebel el Qatrani Formation, Fayum, Egypt|date=1973|journal=Postilla|volume=1653|pages=1-11}}</ref> In 1978, in an overview of the fossil African hyraxes, Meyer still excluded ''Thyrohyrax'' from Pliohyracinae, but speculated that it was at least closely related in its dental anatomy to the earliest stage of a lineage leading directly to ''Pliohyrax'' through ''Meroehyrax''. He also transfered in the same chapter ''M. pygmaeus'' to the genus ''[[Pachyhyrax]]''.<ref name=Meyer1978>{{cite book |last=Meyer|first=G.E.|date=1978|editor-last1=Maglio|editor-first1=V.J.|editor-last2=Cooke|editor-first2=H.B.S.|title=Evolution of African Mammals|publisher=Harvard University Press|pages=284-314|chapter=Hyracoidea|isbn=}}</ref>
 
In 1988, [[David Tab Rasmussen]] and [[Elwyn L. Simons]], describing the hyracoid remains collected in the [[Jebel Qatrani Formation]] of the Fayum between 1977 and 1984, finally transfered to ''Thyrohyrax'' ''P. pygmaeus'', and referred another isolated molar to the species ; he also referred a great number of specimens to the more abundant type species ''T. domorictus'', and mentioned the presence of a third smaller species, ''T.'' sp., known from a few isolated teeth and a fragmentary mandible.<ref name=TabRasmussen1988>{{cite journal|first1=D.|last1=Tab Rasmussen|first2=E.L.|last2=Simons|title=New Oligocene hyracoids from Egypt|date=1988|journal=Journal of Vertebrate Paleontology|volume=8(1)|pages=67-83}}</ref> In 1990, Tab Rasmussen, [[Mario Gagnon]] and Simons signaled the collection of several isolated hyracoid [[astragalus (bone)|astragali]], including one of small size, found in the newly exploited quarry L-41 of the Jebel Qatrani Formation, and tentatively attributable to ''Thyrohyrax'' or ''Saghatherium''.<ref name=TabRasmussen1990>{{cite journal|first1=D.|last1=Tab Rasmussen|first2=M.|last2=Gagnon|first3=E.L.|last3=Simons|title=Taxeopody in the carpus and tarsus of Oligocene Pliohyracidae (Mammalia: Hyracoidea) and the phyletic position of Hyraxes|date=1990|journal=Proceedings of the National Academy of Sciences of the United States of America|volume=87|pages=4688-4691}}</ref> The next year, 1991, Tab Rasmussen and Simons described, among several new hyracoid taxa, two new species of ''Thyrohyrax'' from Quarry L-41 : the smaller ''T. meyeri'', based on CGM 41882, a partial mandible, to which they referred several fragmentary mandibles, a partial skull, and speculated that some postcranial elements found in the same quarry belonged to the new species, the name honouring Grant E. Meyer, the founder of the genus ; and the larger ''T. litholagus'', based on CGM 41880, a partial mandible, to which they referred four other mandibles, two maxilla and two cranial fragments, the species name, based on the greek prefix "'lithos'" ("rock"), and the suffix "'lagos'", ("rabbit"), meaning "rock rabbit", a translation of the common name used for hyraxes by modern Egyptians.<ref name=TabRasmussen1991>{{cite journal|first1=D.|last1=Tab Rasmussen|first2=E.L.|last2=Simons|title=The Oldest Egyptian Hyracoids (Mammalia: Pliohyracidae): New Species of Saghatherium and Thyrohyrax from the Fayum|date=1991|journal=Neues Jahrbuch für Geologie und Paläontologie|volume=182(2)|pages=187-209}}</ref> In 1995, a study by [[Gary T. Schwartz]], Tab Rasmussen and [[Richard J. Smith]] estimated the size of extinct hyracoids based on the of their dentition and proposed that the smaller ''T. meyeri'', weighing between 4.6 and 7.1 kg, was barely larger than modern hyraxes ; ''T. domorictus'' weighed between 6.9 and 12.6 kg, and the larger ''T. litholagus'' weighed between 13.7 and 23.1 kg.<ref name=Schwartz1995>{{cite journal|first1=G.T.|last1=Schwartz|first2=D.|last2=Tab Rasmussen|first3=R.J.|last3=Smith|title=Body-size diversity and community structure of fossil hyracoids|date=1995|journal=Journal of Mammalogy|volume=76(4)|pages=1088-1099}}</ref>
 
The genus name, ''Thyrohyrax'', is formed from the [[Ancient Greek|Greek]] prefix "''thyra-''", meaning "window", and the suffix "''-hyrax''", referring to the internal fenestra in the mandible of the presumed females. The type species name is formed from the Greek "''domos-''", meaning "house" and the [[Latin]] ''-ramus'', meaning "jaws", referring to the chambered jaws of the type species.<ref name=Meyer1973/>
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'''''Naranbulagornis''''' is an [[extinct]] [[monotypic]] [[genus]] of basal [[waterfowl]]. Its type and only known species, ''N. khun'', is known from two Late [[Paleocene]] localities in Southern [[Mongolia]].
 
==History and Etymology==
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==Description==
 
''Naranbulagornis'' is a quite large waterfowlfowl, a fourth larger than the contemporary ''[[Anatalavis]]'' ; it was presumably one of the largest anseriform of its time, reaching almost the size of the modern [[coscoroba swan]]. The [[holotype]], the proximal end of a right [[carpometacarpus]], reached 58 mm in length ; most notably, and contrarily to all other anseriforms, its pisiform process was positioned at the level of the proximal margin of the extensor process.
 
==Paleontology==