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Bachitherium

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1307: 3735: 4549: 5097: 4759: 5432: 611: 4729:, which engage in aquatic escape behaviours from predators by running into a water source and swimming. They can swim with only the upper half of their heads out of the water and can even completely submerge, although the behaviours prove to be exhaustive for the small ruminants. In comparison, this behaviour is not as common in pecorans, supporting the hypothesis that the Tragulidae retains such rare escape behaviours because they diverged within the Ruminantia at an early stage. The oldest tragulid, known from the Krabi Basin of southern 4908: 1507: 4604: 4276: 3764:, where the P is evolutionarily lost, thus explaining why it has one less premolar in its upper jaw than its lower jaw. There are also no upper incisors recorded from the skeleton or other related specimens, typical of ruminant traits. The upper canine is curved in a hook-like manner and strong but relatively short since it does not exceed the height of the upper edge of the mandible. The lower canine is also short similar to the upper canine and the lower incisors but is incisiform in shape. In terms of 136: 1528: 4802: 4691: 1079: 5253: 3585: 620: 115: 5733: 4953: 4397:
long with an articular surface being almost perpendicular to the body of the bone. The fusions of the bones appear to be an advanced trait since it is also present in pecoran evolution while the fusions are not always represented in the Tragulidae. Because of this, the Bachitheriidae are considered "advanced" in phylogenetic traits compared to similar tragulines but more "primitive" than early pecorans or their predecessors.
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superfamily Traguloidea is sometimes used in systemic palaeontological diagnoses, plus Janis and Jessica M. Theodor defined Hypertraguloidea as a valid superfamily consisting of the Hypertragulidae and Praetragulidae based on the fusion of the magnum and trapezoid bones in the carpus, a trait unseen in other artiodactyls. The two superfamilies are not often mentioned in research papers on members of the Tragulina, however.
5451:, and all Paleogene European nimravids, the latter of which are suggested to have gone extinct by 28 Ma. These faunal changes brought an end to the dominance of feliforms in Europe in favor of caniforms (amphicyonids and ursids), the complete extinction of the palaeotheres, and the extirpations of the entelodonts and amynodonts from Europe, potentially correlating with increased aridity in Europe. 1586:
and Asian "Gelocidae" (a known wastebasket family), Bachitheriidae, late Oligocene or early Miocene Pecora of ambiguous affinities, Lophiomerycidae, Tragulidae, Leptomerycidae, Archaeomerycidae, and Hypertragulidae. Below are two phylogenetic trees of the defined Oligocene ruminants, the first based on a 50% majority consensus and the second based on a strict consensus:
4679:, the last surviving species of the Bachitheriidae, likely lived in more open environments than preceding species based on the significant elongation of the metacarpals for locomotion, coinciding with the large transition from forested environments to more open environments by MP28, correlated with major climatic and faunal events. All species of 1278:), or some 20 Ma. It is the oldest-recognized instance of island endemism within the region (fossils dating to the Eocene are known although rare, but the faunas do not display endemism since the landmass had not separated from the European plate yet). In his previous 1999 list of the large mammals of the early Miocene of Sardinia, he listed 4409:, he and Jean-Noël Martinez used the dimensions of the astragali of Paleogene artiodactyls to estimate their body masses, since the astragalus is the most frequently postcranial bone in fossil assemblages from its reduction of vulnerability to fragmentation due to its stocky shape and compact structure. Four known 4966:
faunal turnover in western Europe, in which faunal immigrants from Asia disperse there as a result of the closing of seaways previously separating western Europe from the rest of Eurasia. The Grande Coupure also marks the first European appearances of the later anthracotheres, gelocids, lophiomerycids, and
5826:'s management sought to promote conservation of the Oligocene-aged phosphorite deposits in part by educating nearby inhabitants to understand the generally niche palaeontological heritage in their areas to become the locality's future guarantors. In 2021, the Geopark's management commissioned the sculptor 1354:
animal." He also defined the etymologies of the species names, "curtum" and "insigne" translating in Latin to "shortened" and "distinguished" respectively, "vireti" being in honor of Jean Viret, "guirounetensis" being unknown, and "lavocati" being in honor of Lavocati for studying the lower dentition of
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was the last bachitheriid species to exist in Europe. Its near-exclusivity to the MP28 zonation unit means that the species was short-lived, existing for only ~300,000 years. The Late Oligocene Warming event, which marks large increases in surface temperatures, not only marked the final speciation of
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by MP28. The speciation changes coincide in part with the Late Oligocene Warming, a period lasting ~26 to 24 Ma (MP26 and MP28), which caused a reversal of climates towards warmer surface temperatures similar to those observed in the late Eocene. This is evident in part by a 2 Â°C (36 Â°F) to
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The Eocene-Oligocene transition of western Europe, as a result of the global climatic conditions, is marked by a transition from tropical and subtropical forests to more open, temperate or mixed deciduous habitats with adaptations to increased seasonality. The extinction event also marks a coincident
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mammalian faunas of western Europe were therefore mostly isolated from other continents including Greenland, Africa, and eastern Eurasia, allowing for endemism to occur within western Europe. The European mammals of the late Eocene (MP17 - MP20) were mostly descendants of endemic middle Eocene groups
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In 2014, Takehisa Tsubamoto reexamined the relationship between astragalus size and estimated body mass based on extensive studies of extant terrestrial mammals, reapplying the methods to Paleogene artiodactyls previously tested by Sudre and Martinez. The researcher used linear measurements and their
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formations that were found during extensive geographical mapping by drilling. The basal breccia-conglomerate-sandstone formation's exact age, although known to be of Eocene age, has an unknown exact age that cannot be possible to deduce because of factors such as a lack of biostratigraphically useful
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in the short but gradual extinction process as a result of the Mi-1 Glaciation event, an immediate event occurring after the Late Oligocene Warming that marked a reversal to colder climates and aridification from the latest Oligocene to the earliest Miocene (why aridification occurred in both events
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Although the Eocene-Oligocene transition marked long-term drastic cooling global climates, western Eurasia was still dominated by humid climates, albeit with dry winter seasons in the Oligocene. Europe during the Oligocene had environments largely adapted to winter-dry seasons and humid seasons that
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The spinal processes are short on C3 and C4 but lengthen from C5 to D1. The lengths of the spinal processes are more or less constant up to D7. The spine is slightly curved backwards from vertebrae C7-D2, then straight on D3-D4, and finally slightly inclined forward until D9. In the spine, there are
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In 2015, Bastien Mennecart and Grégoire Métais created a hypothesis on the phylogenetic relationships of Oligocene ruminants by compiling a matrix of 40 dental, cranial, and postcranial features known from them. The taxa included in the analysis are 20 ruminant species representative of the European
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or as sister taxa of the Bachitheriidae, favouring the former hypothesis over the latter. The Bachitheriidae are considered the sister family to the Tragulidae and are thus phylogenetically within the crown Ruminantia, seemingly supported in part thanks to the Eocene-aged remains recently described
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Several researchers such as Innessa Anatolevna Vislobokova have considered the two superfamilies within the infraorder, the Traguloidea (Tragulidae, Gelocidae, Leptomerycidae, Archaeomerycidae, Lophiomerycidae, Bachitheriidae) and Hypertraguloidea (Hypertragulidae, Praetragulidae), to be valid. The
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are also typical Eocene faunas of typically Asian origins that are present in eastern Europe prior to the Grande Coupure, although the exact ages of the formations that they appeared in are not well-established due to the difficulties in estimating them in eastern European formations. These faunas
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are missing, the former trait being suggested as an autapomorphy of the Bachitheriidae since the skeleton specimen is excellently preserved that the bones being missing could not have been an accident. The first phalanges of the back feet are short compared to the second, while the third are very
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in various phylogenetic trees of Paleogene ruminants, most of which were done by hand. Despite having a complete skeleton, the phylogenetic position of the Bachitheriidae with respect to the "crown" Ruminantia (i.e. below or above the Tragulidae) remained unstable. They suggested that basicranial
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is not found in Asia). This is especially evident after the abrupt Grande Coupure extinction event within the MP20-MP21 boundary (which includes the Eocene-Oligocene boundary), which marks the base of the Rupelian at 33.9 Ma. The first true ruminants to appear in western Europe, the Gelocidae and
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Land-based connections to the north of the developing Atlantic Ocean were interrupted around 53 Ma, meaning that North America and Greenland were no longer well-connected to western Europe. From the early Eocene up until the Grande Coupure extinction event (56 Ma - 33.9 Ma), the western Eurasian
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Although artiodactyls of the Paleogene are not as popular in palaeobiological research as their Neogene counterparts, there has been efforts in recent decades to contextualize the palaeobiologies of Paleogene ruminants in relation to those of Neogene and modern ruminants. The relatively abundant
7610:
Hutchinson, David K.; Coxall, Helen K.; Lunt, Daniel J.; Steinthorsdottir, Margret; De Boer, Agatha M.; Baatsen, Michiel L.J.; Von der Heydt, Anna S.; Huber, Matthew; Kennedy-Asser, Alan T.; Kunzmann, Lutz; Ladant, Jean-Baptiste; Lear, Caroline; Moraweck, Karolin; Pearson, Paul; Piga, Emanuela;
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and other factors causing a 60% extinction rate of western European mammalian lineages while Asian faunal immigrants replaced them. The Grande Coupure is often marked by palaeontologists as part of the Eocene-Oligocene boundary as a result at 33.9 Ma, although some estimate that the event began
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Mennecart and MĂ©tais stated that the systematic position of the monogeneric family Bachitheriidae is somewhat problematic since the uncertain phylogenetic position of the Bachitheriidae with other Oligocene ruminants is due to its postcranial and dental features being similar to other ruminant
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is the earliest-known ruminant to have appeared in the European fossil record, originating in eastern Europe during the late Eocene and migrating to western Europe by the early Oligocene after major seaway barriers fell. The genus remained endemic to the continent and survived several waves of
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The causes of the abrupt extinctions are debated, with suggested causes being climatic and environmental deterioration following late Eocene-early Oligocene glaciations, intensified competition from Asian faunas resulting from seaways previously separating western Europe from other landmasses
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was first reported in 1986 by Jean Sudre at Le Garouillas in France and has since been found in multiple sites in France and Italy. He also defined the etymology of the genus, the prefix "Bach" referring to the old collections of the Quercy site and the suffix "therium" meaning "wild beast or
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of the Neogene) and Bachitheriidae are defined by special traguline-shaped lower premolars that feature a lack of metaconids and two elongated parallel cristids forming the edges of the back valley of the cusp. The lower molars are derived, having relatively selenodont cusps, typical of most
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or early Priabonian (late Eocene). Within the locality, Mennecart et al. reported the oldest Paleogene ruminant from Europe as well as the earliest one known from outside Asia and North America, dating well before the Grande Coupure faunal event in western Europe which dated back to the
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stood out to Sudre, the paraconid being offset lingually and close to the protoconid, but the palaeontologist speculated that the slight difference is not significant enough for a certain allocation to a different species since it could be interpreted as a variation in the more common
573:, weighing up to 36 kg (79 lb), was more cursorial and therefore built for more open forested environments and a diet consisting mainly of leaves. The morphological differences between the species, combined with their frequent appearances in the same fossil deposits, imply 592:
climatic changes of the Oligocene without evolving into a new genus. The Microbunodon Event in the late Oligocene, however, led to its extinction as it faced a combination of a warming climate plus subsequent habitat turnover and competition from a new wave of migrating species.
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Mennecart, Bastien; Wazir, Wasim Abass; Sehgal, Ramesh K.; Patnaik, Rajeev; Singh, Ningthoujam P.; Kumar, Navin; Nanda, Avinash C. (2021). "New remains of Nalamaeryx (Tragulidae, Mammalia) from the Ladakh Himalaya and their phylogenetical and palaeoenvironmental implications".
4773:(or the suborder Euprimates) appeared already by the early Eocene, diversifying rapidly and developing dentitions specialized for folivory. The omnivorous forms mostly either switched to folivorous diets or went extinct by the middle Eocene (47 - 37 Ma) along with the archaic " 1055:), although the specimens from southern Germany were thought to characterize the lower Oligocene. In the palaeontological locality of Itardies in Quercy, two species were determined by Sudre to have characterized the 19th-century Quercy collections of the site: the abundant 5866:. The mayors of the villages approved of the commissioned statues to represent the locations. In addition to serving as palaeontological icons for village inhabitants, the sculptures are intended to interest visitors in the geological histories surrounding the areas. 8710:
Musalizi, Sarah; Schnyder, Johann; Segalen, Loic; Rössner, Gertrud E. (2022). "Early and Middle Miocene Tragulidae of the Napak Region (Uganda) including the Oldest African tragulids: Taxonomic revision, stratigraphical background, and biochronological framework".
4647:, a small-sized species, would have lived in warm, humid environments that were either wooded or semi-aquatic in characteristics, evident by its shorter limb proportions. Therefore, its palaeobiogical niches would have been equvivalent to modern-day chevrotains or 5124:
and Greater Caucasus Basin, thus separating southeastern Europe from western Europe. It was not until ~31 Ma (ca. MP23) that the Paratethys Sea branch of the Tethys Ocean became shallower and eventually disappeared. The disappearance of the seaway barrier allowed
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PeignĂ©, StĂ©phane; Vianey-Liaud, Monique; PĂ©lissiĂ©, Thierry; SigĂ©, Bernard (2014). "Valbro : un nouveau site Ă  vertĂ©brĂ©s de l'OligocĂšne infĂ©rieur (MP22) de France (Quercy). I – Contexte gĂ©ologique ; Mammalia : Rodentia, Hyaenodontida, Carnivora".
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sculpture in front of the village's town hall was completed on November 12, 2022. By that time, the village mayor Patrick Valette, Causses du Quercy Geopark president Catherine Marlas, and Patrick Médéric held an inauguration there to celebrate its completion.
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fold (or similar cuspid structures) on the lower molars, and bunoselenodont dentition on the molars. The Tragulidae (its members commonly known as "chevrotains" or "mouse deer") is the only extant family of the infraorder and are, as a result, considered
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habitats. When alarmed, the species is reported to rush to the nearest river and submerge, swimming upstream, and coming to the surface beneath water banks or overhanging vegetation. Although not as often observed, this behaviour is also reported in
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closing, or some combination of the two. Either way, the post-Grande Coupure faunas of Europe had few endemic representatives, the Asian faunal immigrants that were better-adapted for the Oligocene becoming the dominant faunal assemblages.
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decreases and an estimated drop of ~70 m (230 ft) in sea level. Alexis Licht et. al suggested that the Grande Coupure could have possibly been synchronous with the Oi-1 glaciation (33.5 Ma), which records a decline in atmospheric
4821:, the first ruminant to appear in eastern Europe, in regions like modern-day Bulgaria during the middle-late Eocene. Fossil evidence indicates that the late Eocene mammals of eastern Europe during the Priabonian age include the palaeothere 983:
in the Leptomerycidae. They first reviewed the basic diagnosis of the hypertragulids, a primitive ruminant family with numerous characteristics distinct from other ruminants such as sharp cutting premolars and loss of the mesostyle in the
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remains supporting the criteria on which the species were based (dental dimensions and diastemas of the P-P) were not variable and did not reflect any dimorphism in between species, thereby supporting the distinction between the smaller
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ruminants, as well as possessing no cingulum. The upper molars of the Bachitheriidae do not possess any aligned paracone and metacone. Some more recently described dental autapomorphies of the Bachitheriidae are the diastema between P
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Costa, Elisenda; GarcĂ©s, Miguel; SĂĄez, Alberto; Cabrera, LluĂ­s; LĂłpez-Blanco, Miguel (2011). "The age of the "Grande Coupure" mammal turnover: New constraints from the Eocene–Oligocene record of the Eastern Ebro Basin (NE Spain)".
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In 2021, Bastien Mennecart et al. reused the morphological matrix of some 40 characters from 2015 by Mennecart and MĂ©tais (as explained above) to produce a hypothesis regarding the phylogenetic affinities of the Oligocene tragulid
4930:, an abrupt shift from a greenhouse world characterizing much of the Paleogene to a coolhouse/icehouse world of the early Oligocene onwards. The massive drop in temperatures stems from the first major expansion of the Antarctic 4640:. Therefore, the different sizes of the fossil specimens can be explained as belonging to different species that fill different palaeoecological niches from each other and the many other artiodactyls that coexisted with them. 5120:) were unable to fully disperse to western Europe (modern-day Spain, France, Germany, Belgium, and England) from eastern Europe because of deep water barriers resulting from the Northern Alpine water basin connecting to the 8192:
Scherler, Laureline; Lihoreau, Fabrice; Becker, Damien (2018). "To split or not to split Anthracotherium? A phylogeny of Anthracotheriinae (Cetartiodactyla: Hippopotamoidea) and its palaeobiogeographical implications".
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contrast strongly with western Europe due to the stronger endemism in the western landmass and great difficulties for mammals of Asian affinities in crossing to the landmass prior to the latest Eocene-early Oligocene.
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The Grande Coupure, translating in French to "the great break," is one of the largest extinction and faunal turnover events in the Cenozoic palaeontological record, occurring in Europe within MP20-MP21 as a result of
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By MP24, a faunal turnover event occurred, likely caused by environmental changes resulting from the Oi-2 glaciation and European sea regressions. The extinction event resulted in the extinctions of the rhinocerotid
1397:, the assigned names are to be taken with caution since the materials are generally fragmented and mainly based on postcranial remains, which most often are prone to insular adaptations from the now-extinct animals. 1135:, which she felt was less likely than the alternate hypothesis that it is a derived character state, which would involve three independent evolutions of the character in the Hypertragulidae, the Leptomerycidae, and 8314:
Solé, Floréal; Fischer, Valentin; Le Verger, Kévin; Mennecart, Bastien; Speijer, Robert P.; Peigné, Stéphane; Smith, Thierry (2022). "Evolution of European carnivorous mammal assemblages through the Paleogene".
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Ducrocq, Stéphane; Soe, Aung Naing; Chavasseau, Olivier; Sein, Chit; Chaimanee, Yaowalak; Lazzari, Vincent; Jaeger, Jean-Jacques (2019). "New basal ruminants from the Eocene of the Pondaung Formation, Myanmar".
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is also a focus of further recent efforts within France to promote palaeontological heritage, including as a representation of the post-Grande Coupure faunas of the Quercy fossil record. More specifically, the
5615:. The immigrant pecorans were able to live in the arid and open habitats because they were better-adapted to mixed feeding diets and cursoriality compared to the European tragulines. The complete extinctions of 5558:
but eventually its extinction. In part, the event brought changes in vegetation towards more open habitats like savannahs that were adjusted to drier and more seasonal climates. Although postcranial remains of
8611:
Harzhauser, Mathias; Daxner-Höck, Gudrun; López-Guerrero, Paloma; Maridet, Olivier; Oliver, Adriana; Piller, Werner E.; Richoz, Sylvain; Erbajeva, Margarita A.; Neubauer, Thomas A.; Göhlich, Ursula B. (2016).
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was selected to represent the village of Bach in the program, which was known as "Mon village, mon fossile" ("My village, my fossil"). The other animals chosen to represent other areas were the chalicothere
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is the type and only genus of the family Bachitheriidae within the infraorder Tragulina in the artiodactyl suborder Ruminantia. Tragulina is more basal than Pecora and is characterized by doglike astragalus
1151:" fold ("fold on the posterolingual face of the metaconid") and the posterior lower premolars possessing primitive ruminant conditions of elongated, posteriorly directed metaconids. The hypoconulid of the M 7338:
Badiola, Ainara; Perales-Gogenola, Leire; Astibia, Humberto; Suberbiola, Xabier Pereda (2022). "A synthesis of Eocene equoids (Perissodactyla, Mammalia) from the Iberian Peninsula: new signs of endemism".
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Palaeobiogeography of eastern Eurasian ruminants during the late Eocene-early Oligocene with dispersal routes to western Europe during the Grande Coupure (33.9 Ma) and Bachitherium Dispersal Event (31 Ma).
4227:, of which the anterior member is much shorter than the posterior one. The axis's body is short, but the axis itself is noted to be remarkable for the vertical and especially caudal extension of its high 6531:
Licht, Alexis; MĂ©tais, GrĂ©goire; Coster, Pauline; Ä°bilioğlu, Deniz; Ocakoğlu, Faruk; Westerweel, Jan; Mueller, Megan; Campbell, Clay; Mattingly, Spencer; Wood, Melissa C.; Beard, K. Christopher (2022).
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or western Europe, which became isolated from North America and Greenland by the later early Eocene and thereby had faunas that evolved in the form of distinct endemism compared to the rest of Eurasia (
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from previous decades. He documented the biostratigraphical distribution of western European ruminants during the early-middle Oligocene by Mammal Paleogene zones. In the distribution chart, he listed
4651:(tribe Cephalophini/subfamily Cephalophinae), both of which live in humid wooded habitats in Africa and/or southern Asia with freshwater bank sources. Based on dental microwear analysis, the diet of 7199:
Métais, Grégoire; Chaimanee, Yaowalak; Jean-Jacques, Jaeger; Ducrocq, Stéphane (2001). "New remains of primitive ruminants from Thailand: Evidence of the early evolution of the Ruminantia in Asia".
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For much of the Eocene, a hothouse climate with humid, tropical environments with consistently high precipitations prevailed. Modern mammalian orders including the Perissodactyla, Artiodactyla, and
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was thought to be separate from the leptomerycids based on derived characteristics more similar to "gelocids" and its lack of derived features with the leptomerycids. Unlike the leptomerycids, the I
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Obergfell, Friedlinde A. (1957). "Vergleichende Untersuchungen an Dentitionen und Dentale Altburdigaler Cerviden von Wintershof-West in Bayern und rezenter Cerviden (Eine phylogenetische Studie)".
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Pélissié, Thierry; Orliac, Maëva J.; Antoine, Pierre-Olivier; Biot, Vincent; Escarguel, Gilles (2021). "Beyond Eocene and Oligocene Epochs: The Causses du Quercy Geopark and the Grande Coupure".
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Mennecart, Bastien; Zoboli, Daniel; Costeur, LoĂŻc; Pillola, Gian Luigi (2017). "Reassessment of the latest Oligocene ruminant from Sardara, the last non-insular mammal from Sardinia (Italy)".
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is distinguished by its dentition that is closer to the Tragulina than other artiodactyls but are distinct enough to justify it belonging to its own family. The dental formula of the genus is
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allow for distinguishing it as a distinct family compared to other members of the Tragulina infraorder such as the Gelocidae, Lophiomerycidae, Hypertragulidae, Leptomerycidae, and Tragulidae.
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from the Balkans. Below is an updated tree based on the 2015 phylogenetic trees by Mennecart and MĂ©tais resulting from the cladistic analysis of 41 dental, cranial, and postcranial specimens:
4916:, an iconic genus of the Western European endemic fauna from the late Eocene to the early Oligocene. It died out by the Eocene-Oligocene transition due to the Grande Coupure extinction event. 1365:
per van der Made in 2008, stating that the species is based only on postcranial remains and that the association of characteristics does not allow for a strict attribution of the remains to
1100:, in which the recent discovery of the complete skeleton of the genus and her investigation of the European dental material of it could enable a reassessment of the ruminant. Janis verified 6300:
Sudre, Jean (1995). "Le Garouillas et les sites contemporains (OligocÚne, MP 25) des phosphorites du Quercy (Lot, Tarn-et-Garonne, France) et leurs faunes de vertébrés: 12. Artiodactyles".
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Although Paleogene mammals are incomplete in the fossil record in eastern Europe compared to western Europe, there is enough fossil evidence indicating which mammals likely coexisted with
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Jean Sudre wrote a research article chapter on the Oligocene artiodactyls of the Quercy collections of France in 1995, including the Bachitheriidae. He said that recent diagnoses of many
8900: 3618:. The premaxillary, being edentulous (lacking teeth), upright, and short, comes into contact with long nasals, broadened behind and ending towards the front. There is a small gap in the 3557:, allowing for more thorough diagnoses for the Bachitheriidae. Unfortunately, the skeleton is strongly flattened transversely, limiting observations of it to only its left side. The 8838: 3811:" fold on the molars. It is also different from other traguline genera by the straight outline of the lower mandible and the elongated diastema being highly constricted just after P 569:, weighing 7 kg (15 lb) to 8 kg (18 lb), was well-adapted to closed forest environments and ate a mix of leaves, fruit, and herbages. In comparison, the larger 8386:"On the morphology of the astragalus and calcaneus of the amphicyonids (Carnivora, Mammalia) from the Paleogene of Europe: implications for the ecology of the European bear-dogs" 4579:, however, was unusually large in comparison to not just other bachitheriid species but also other Paleogene tragulines, being estimated to weigh up to 36 kg (79 lb). 5795: 5145: 2864:
are classified as outgroups within the Artiodactyla due to not falling within the Ruminantia suborder. However, the 2021 phylogenetic tree also adds the enigmatic artiodactyl
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Janis, Christine Marie (1987). "Grades and Clades in Hornless Ruminants Evolution: the Reality of the Gelocidae and the Systematic Position of Lophiomeryx and Bachitherium".
5799: 8046:"New data on the earliest European ruminant (Mammalia, Artiodactyla): A revision of the fossil mandible from Rusce in the Pčinja basin (late Eocene, Southeastern Serbia)" 6186:"Un squelette complet de Bachitherium (Artiodactyla, Mammalia) de l'OligocĂšne de CĂ©reste (Alpes de Haute-Provence). Remarques sur la systĂ©matique des Ruminants primitifs" 8868: 5823: 1286:, basing the species etymology on the island. He based it off of postcranial remains that have the general morphologies of primitive ruminants and sizes intermediate to 1112:, the palaeontologist argued, could be excluded from the Tragulidae and Hypertragulidae families because of a combination of features of its limb anatomy. Nonetheless, 7945:
Solé, Floréal; Fischer, Fischer; Denayer, Julien; Speijer, Robert P.; Fournier, Morgane; Le Verger, Kévin; LadevÚze, Sandrine; Folie, Annelise; Smith, Thierry (2020).
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Lophiomerycidae, were immigrant taxa that dispersed from Asia while most mammal lineages of western Europe, most of which were endemic to the continent, disappeared.
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frog, a complete but currently undescribed shell of a turtle with associated skeletal remains, an almost complete skull and postcranial skeleton of the alligatoroid
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to create seven sculptures of Eocene-Oligocene animals whose genus/species names or synonymized names derive from a particular village as mascots of the locations.
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The researchers also reviewed reports of the supposed previously oldest Bachitheriidae from the German localities of Herrlingen1, Möhren13, Ronheim1, and Weinheim (
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Peigné, Stéphane (2003). "Systematic review of European Nimravinae (Mammalia, Carnivora, Nimravidae) and the phylogenetic relationships of Palaeogene Nimravidae".
4777:." By the late Eocene (approx. 37 - 33 Ma), most of the ungulate form dentitions shifted from bunodont cusps to cutting ridges (i.e. lophs) for folivorous diets. 4388:
II and IV (or long bones of the feet) are partially fused (fused except at their distal extremities without a groove (or furrow) on the anterior face) while the
1024: 5827: 4848: 3673:
The horizontal region of the mandible increases in height towards the back, the lower edge having two concavities. Of the two concavities, one is in front of P
8023:"Insect bone-modification and palaeoecology of Oligocene mammal-bearing sites in the Doupov Mountains,northwestern Bohemia. Dvérce, Detan, Valec (NW Bohemia)" 8271:
Solé, Floréal; Dubied, Morgane; Le Verger, Kévin; Mennecart, Bastien (2018). "Niche partitioning of the European carnivorous mammals during the paleogene".
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tribe by MN2, thus bringing the end of the post-Grande Coupure faunas. The tragulines were completely absent from Europe as a result of the extinctions of
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Estimated body masses (kg) of Paleogene artiodactyls based on recalculated trochlear widths (Li1) in comparison to estimates from Martinez and Sudre (1995)
4535:
products with adjusted correction factors. The recalculations resulted in somewhat lower estimates compared to the 1995 results (with the exception of the
8538:"Ursidae (Mammalia, Carnivora) from the Late Oligocene of the "Phosphorites du Quercy" (France) and a reappraisal of the genus Cephalogale Geoffroy, 1862" 6802:
Mennecart, Bastien; Métais, Grégoire (2015). "Mosaicomeryx gen. nov., a ruminant mammal from the Oligocene of Europe and the significance of 'gelocids'".
5563:
suggest that it was better-adapted towards open habitats compared to its predecessors, it may have been unable to adapt to further changes in vegetation.
7164:
Meijaard, Erik; Arifin, Umilaela; Wijeyeratne, Gehan de Silva (2010). "Aquatic escape behaviour in mouse-deer provides insight into tragulid evolution".
5798:
in 1991. The park management, intending to allow the skeleton to be displayed for public display and education, gave the ownership of the fossil to the
7291:"Western European middle Eocene to early Oligocene Chiroptera: systematics, phylogeny and palaeoecology based on new material from the Quercy (France)" 7107:"The European Ruminants during the "Microbunodon Event" (MP28, Latest Oligocene): Impact of Climate Changes and Faunal Event on the Ruminant Evolution" 6902:
Geraads, Denis; Bouvrain, GeneviÚve; Sudre, Jean (1987). "Relations phylétiques de Bachitherium Filhol, Ruminant de l'OligocÚne d'Europe occidentale".
6111:
The Ruminantia (Mammalia, Cetartiodactyla) from the Oligocene to the Early Miocene of Western Europe: systematics, palaeoecology and palaeobiogeography
5027: 3642:
appears to be absent from the skull, the lacrimal hole instead opening inside the orbit which is small and closed posteriorly by a complete and robust
585:
and was likely better adapted to open forested environments than other species of its genus, coinciding with major climatic and faunal restructurings.
6944:
Martinez, Jean-Noël; Sudre, Jean (1995). "The astragalus of Paleogene artiodactyls: comparative morphology, variability and prediction of body mass".
6343:
van der Made, Jan (2008). "New endemic large mammals from the Lower Miocene of Oschiri (Sardinia): Observations on evolution in insular environment".
8746:
Coster, Pauline; Legal, Stéphane (2021). "An Early Oligocene Fossil LagerstÀtten from the Lacustrine Deposits of the Luberon UNESCO Global Geopark".
7382:
Nikolov, Ivan; Heissig, Kurt (1985). "Fossile SĂ€ugetiere aus dem ObereozĂ€n und UnteroligozĂ€n Bulgariens und ihre Bedeutung fĂŒr die PalĂ€ogeographie".
6428:"Discovery of the oldest European ruminant in the late Eocene of Bulgaria: Did tectonics influence the diachronic development of the Grande Coupure?" 5849: 5320: 5117: 4735: 3304: 3152: 2569: 2425: 1957: 1770: 1387:
separated from the mainland by the early Miocene, in which then the Sandinian insular Neogene fossils represented the oldest case of endemism in the
787: 6729:
Draz, Omer; Ni, Xijun; Samiullah, Khizar; Yasin, Riffat; Fazal, Rana Mehroz; Naz, Sakeela; Akhtar, Saleem; Gillani, Mahpara; Ejaz, Muzammil (2020).
1569:
is technically considered a mammal of Asian origin based on its geographical origins being that of eastern Europe as opposed to the Eocene landmass
5332: 5033: 4835: 1243:
series. The mandible fragment was referred to the species with some reservation based on its slightly smaller size compared to those attributed to
940: 543: 9098: 5684: 5408: 5182: 5766:
site for its well-preserved flora and fauna fossils. The site contains hundreds of species of fossil plants, fossil fish a skeletal remain of a
4231:
which reaches the level of C4. The unusual traits of the cervical vertebrae could be connected with the strong development of the large oblique
1000:
being developed into a tusk similar to leptomerycids, it was very reduced unlike them, therefore not belonging to the family due to the lack of
8909: 7660:
Toumoulin, Agathe; Tardif, Delphine; Donnadieu, Yannick; Licht, Alexis; Ladant, Jean-Baptiste; Kunzmann, Lutz; Dupont-Nivet, Guillaume (2022).
5586: 5435:
Africa today largely consists of tropical savannahs with dry conditions, making it slightly similar to Europe during the middle-late Oligocene.
5314: 5056: 4841: 4392:
III and IV (or long bones of the hands coming after wrist bones) are unfused. The lateral metacarpals appear to be absent and all of the front
3595: 3576:, the major differences between the two species are the former species' smaller teeth, diastema, and postcranial bones compared to the latter. 3376: 3352: 3280: 2651: 2634: 2552: 2063: 2046: 1940: 479:, is currently pending reassessment. The genus name derives from "Bach", the French locality where its first fossils were found, and the Greek 4961:, a rhinocerotid that appeared in Europe during the Grande Coupure extinction-faunal turnover event and lived there for most of the Oligocene. 1063:, which was much rarer. At the Pech Desse locality in Quercy (the most recent site at the former province at the time), a second new species, 6234:
Sudre, Jean (1986). "Le genre Bachitherium Filhol 1882 (Mammalia, Artiodactyla): diversite specifique, phylogenie, extension chronologique".
5695: 5230: 3328: 2977: 2668: 2357: 1974: 1702: 808: 8773: 7023:
Blondel, CĂ©cile (1997). "Les ruminants de Pech Desseet de Pech du Fraysse (Quercy; MP28); Ă©volution des ruminants de l'oligocĂšne d'Europe".
6629:"Unearthing deep-time biodiversity changes: The Palaeogene mammalian metacommunity of the Quercy and Limagne area (Massif Central, France)" 5537: 5276:
or purely broadleaved deciduous forests aligning with the northernmost belt between 40°N and 50°N, the middle belt of warmth-adapted mixed
5236: 5162: 5047: 3169: 2866: 2528: 2442: 1916: 1787: 827: 1369:. The shape of the postcranial remains resembling those of primitive ruminants could potentially be due to insular effects similar to the 1306: 526:
in France in 1981, which helped palaeontologists understand its morphology compared to other ruminants. The complete fossil revealed that
7846:"Ruminants reveal Eocene Asiatic palaeobiogeographical provinces as the origin of diachronous mammalian Oligocene dispersals into Europe" 7447:"Eocene–Oligocene mammalian faunal turnover in the Hampshire Basin, UK: calibration to the global time scale and the major cooling event" 5712: 5592: 4829: 3247: 3230: 2307: 2290: 1837: 1820: 5998:"Iberomeryx minor (Mammalia, Artiodactyla) from the Early Oligocene of Soulce (Canton Jura, NW Switzerland): systematics and palaeodiet" 8425:
O'Brien, Charlotte Lucy; Huber, Matthew; Thomas, Ellen; Pagani, Mark; Super, James; Elder, Leanne Elizabeth; Hull, Pincelli M. (2020).
5791: 5743: 4870: 2324: 1628: 1493:, the cingulum is only more emergent. Therefore, the actual oldest record of the Bachitheriidae in western Europe is ca. 31 Ma (MP23). 1131:
is a primitive ruminant character would entail the loss of the character twice within the evolution of ruminants in the Tragulidae and
7703:"Age and driving mechanisms of the Eocene–Oligocene transition from astronomical tuning of a lacustrine record (Rennes Basin, France)" 996:, validating the previous reassignment from the Hypertragulidae. However, Bouvrain and Garaads also observed that although it shared I 5977:
Bouvrain, GeneviĂšve; Geraads; Sudre, Jean (1986). "RĂ©vision taxonomique de quelques Ruminants oligocĂšnes desphosphorites du Quercy".
5052: 4362:
are shorter than the hind limbs, but the difference is smaller than in tragulids. The limb proportions are similar to the musk deer (
3001: 2384: 1729: 668: 8934: 8671:"New records of Dorcatherium guntianum (Tragulidae), stratigraphical framework, and diphyletic origin of Miocene European tragulids" 7611:
Pound, Matthew J.; Salzmann, Ulrich; Scher, Howie D.; Sijp, Willem P.; ƚliwiƄska, Kasia K; Wilson, Paul A.; Zhang, Zhongshi (2021).
7239:"Mountain uplift explains differences in Palaeogene patterns of mammalian evolution and extinction between North America and Europe" 5920:
Catalogue of the Fossil Mammalia in the British Museum, (Natural History): Part II. Containing Order Ungulata, Suborder Artiodactyla
9182: 9085: 9031: 4687:
and thereby more adaptable for semi-open habitats as indicated by their elongated cannon bones relative to their metacarpal bones.
4311:
present within the humerus. In the distal area of the humerus, the diameter of the condyle is lower than that of the trochlea. The
7575:
Venczel, Márton; Codrea, Vlad; FărcaƟ, Cristina (2011). "A new palaeobatrachid frog from the early Oligocene of Suceag, Romania".
4263:
of the bachitheriid are wide, short, and straight, contrasting with the later ribs that are thin, long, and curved. The number of
8344:"A new early Late Oligocene (MP 26) continental vertebrate fauna from Saint-Privat-des-Vieux (Ales Basin, Gard, Southern France)" 6509:
Erfurt, Jörg; Métais, Grégoire (2007). "Endemic European Paleogene Artiodactyls". In Prothero, Donald R.; Foss, Scott E. (eds.).
1321:
Bastien Mennecart reviewed the post-Grande Coupure artiodactyls of Europe in his 2012 PhD thesis, including all known species of
8846: 7662:"Evolution of continental temperature seasonality from the Eocene greenhouse to the Oligocene icehouse –a model–data comparison" 9197: 8484:
Assemat, Alexandre; Mourlam, Mickaël J.; Weppe, Romain; Maugoust, Jacob; Antoine, Pierre-Olivier; Orliac, Maeva Judith (2020).
8099:"Oligocene vegetation of Europe and western Asia-Diversity change and continental patterns reflected by plant functional types" 4998:
have all entered the European continent during the Grande Coupure, abruptly making carnivorans the dominant carnivorous group.
4567:, a common species at the Pech Desse locality in France, had any dimorphism, indicating that it was homogenous in nature. Both 8875: 6628: 6493: 3561:
of the skull, as a result, are little or cannot be observed. Nonetheless, the complete skeleton and various other remains of
7063:
Blondel, Cécile (1998). "Le squelette appendiculaire de sept ruminants oligocÚnes d'Europe; implications paléoécologiques".
9177: 8140:"Palaeoclimatic reconstruction for the Late Oligocene La Val fossil site (Estadilla, Huesca, Spain) based on CLAMP and LMA" 4986:) as well as eulipotyphlans (Erinaceidae) were also Grande Coupure arrivals of Asian origins. Carnivorans representing the 4575:
have been estimated to weigh 7 kg (15 lb) - 8 kg (18 lb), consistent with the idea of similar weights.
8097:
Utescher, Torsten; Erdei, Boglårka; François, Louis; Henrot, Alexandra-Jane; Mosbrugger, Volker; Popova, Svetlana (2020).
5284:
broadleaved forests aligning between 40°N and 30°N, and the last belt containing tropical vegetation aligning below 30°N.
866:
teeth, leaving a valley on the tip from the protoconid to the entostylid. In 1971, LĂ©onard Ginsburg created a genus named
750:" synonyms of because the specimens appeared to have belonged to the same species (notably, Filhol described the species " 9202: 9157: 7495:
Legendre, Serge; Mourer-Chauviré, Cécile; Hugueney, Marguerite; Maitre, Elodie; Sigé, Bernard; Escarguel, Gilles (2006).
6770:
Janis, Christine M.; Theodor, Jessica M. (2014). "Cranial and postcranial morphological data in ruminant phylogenetics".
6427: 1187:(also known as the talus bone or ankle bone). As a result, Christine Janis suggested that the it should be placed as a 944: 8384:
Fournier, Morgane; LadevÚze, Sandrine; Le Verger, Kévin; Fischer, Valentin; Speijer, Robert P.; Solé, Floréal (2020).
5312:
along with all other rhinocerotoids and anthracotheres. MP24 also involves the first appearances of the stem pecorans
4591:
offers hints of different ecological niches being filled by them within the European continent, as the larger size of
979:), and until then, it only had jaws for fossil remains. The researchers discussed Webb and Taylor's 1980 placement of 9192: 9172: 4927: 4299:
is slightly marked, and the tuberosity (prominence where muscles and connective tissues attach) of the tendon of the
1431: 633: 8956: 7947:"The upper Eocene-Oligocene carnivorous mammals from the Quercy Phosphorites (France) housed in Belgian collections" 6128:
Lavocat, René (1946). "Observations sur le genre Bachitherium et sur l'extension géographique des Hypertragulidés".
4781:
continent was separated into three landmasses, the former two of which were isolated by seaways: western Europe (an
2840:
morphological analyses will provide key features to better understanding the evolutionary history of bachitheriids.
8342:
Vianey-Liaud, Monique; Comte, Bernard; Marandat, Bernard; Peigné, Stéphane; Rage, Jean-Claude; Sudre, Jean (2014).
7613:"The Eocene-Oligocene transition: A review of marine and terrestrial proxy data, models and model-data comparisons" 7497:"Dynamique de la diversité des mammifÚres et des oiseaux paléogÚnes du Massif Central (Quercy et Limagnes, France)" 5762:, a palaeontological site for terrestrial communities dating to the early Oligocene that is considered a Konservat- 5129:
and rodents associated with it to disperse from southeastern Europe into the western European region. The tragulid
5088:. The faunas of this locality are consistent enough with those representative of the post-Grande Coupure deposits. 2831:
and traguloid-shaped astragali, but the selenodont molars and fusion of the carpal bones were probably a result of
1123:
was more similar to hypertragulids than those of the Leptomerycidae which was characterized by their more conical P
5596:, all of which were Asiatic immigrants. Additional carnivorans appear during this time as well, namely the ursids 9167: 5488:, after long periods of existence in Europe, finally disappeared by the end of MP27, where they were replaced by 1466: 1145:
was discerned to have a mixture of primitive and derived dental characteristics, the lower molars retaining the "
1086: 1047:, which then had just two species in its name and were reported additionally in Italy, Switzerland, and Germany. 7903:"Earliest record of rhinocerotoids (Mammalia: Perissodactyla) from Switzerland: systematics and biostratigraphy" 6924:
Métais, Grégoire; Vislobokova, Inessa (2007). "Basal Ruminants". In Prothero, Donald R.; Foss, Scott E. (eds.).
5893:"Découverte de quelques nouveaux genres de MammifÚres fossiles, dans les dépÎts de phosphate de chaux du Quercy" 4739:, dates back to the late Eocene, further supporting the Tragulidae being the most basal extant ruminant family. 1071:
by the size of the diastema between the P and P. He also reviewed the systematics of the genus, confirming that
9187: 8086:(in French). École Pratique des Hautes Études-Sciences de la Vie et de la Terre, Montpellier. pp. 769–850. 3734: 2835:. The convergent traits, the researchers suggested, caused misinterpretations of the phylogenetic relations of 5940:
Recherches Sur Les Phosphorites Du Quercy: Étude Des Fossiles Qu'on Y Rencontre Et SpĂ©cialement Des MammifĂšres
7403:"First occurrence of Palaeotheriidae (Perissodactyla) from the late–middle Eocene of eastern Thrace (Greece)" 4632:
species indicates that virtually none display any signs of sexual dimorphism, although it is unknown whether
4595:
likely means that it lived in a different habitat and had slightly different eating habits compared to them.
1216: 518:
was only known from incomplete remains, making assessments difficult. However, a nearly complete skeleton of
460: 6534:"Balkanatolia: The insular mammalian biogeographic province that partly paved the way to the Grande Coupure" 9162: 897: 6476:
Janis, Christine M. (1984). "Tragulids as Living Fossils". In Eldridge, Niles; Stanley, Steven M. (eds.).
5263:. Anthracotheres, rhinocerotoids, and ruminants were the dominant assemblages of Eurasia in the Oligocene. 4327:. The pelvis does not have any peculiar traits except for the elongation of the acetabular portion of the 3795:
The Bachitheriidae is defined as a traguline family that possesses a narrow and "pinched" hypoconulid on M
3553:
is also known by a complete skeleton from the limestone deposits of Cereste, France that is attributed to
900:
angle of the tooth. Because of this and other dental traits of the species, the taxon was reclassified to
8343: 8080:
Aguilar, Jean-Pierre; Legendre, Serge; Michaux, Jacques (1997). "SynthÚses et tableaux de corrélations".
7701:
Boulila, Slah; Dupont-Nivet, Guillaume; Galbrun, Bruno; Bauer, Hugues; ChĂąteauneuf, Jean-Jacques (2021).
5786:, and fossil insects. Mammal fossils are rare within the site, however, making the discovery of the only 4765:
of Europe and Asia during the middle Eocene with possible artiodactyl and perissodactyl dispersal routes.
3785: 1469:) that date back to 32.5 Ma (MP22). The German ruminant fossils were reclassified to the gelocid species 135: 4545:, which as a shorter astragalus proportion than most other artiodactyls), displayed in the below graph: 3646:. The back of the skull, which is slightly inclined with respect to the face, is surmounted by a strong 4706:
The primitive natures of modern chevrotains also provide clues to early ruminant behaviour. The modern
4433:) were analyzed using two different methods of medial weight estimations: the astragalus size and the M 4813:
appeared in Europe by the late Eocene (MP17a) and existed there for up to the earliest Miocene (MP30).
4563:, the latter species considered to be the potential ancestor of the former. There is no evidence that 4548: 3681:. The upward angular region of the mandible is wide, its posterior edge connecting to the neck of the 766:
was known only by some portions of the mandible and maxilla, that it was said to be closely allied to
5133:, known first in the Eocene of eastern Asia, dispersed into southwestern Asia (modern-day Turkey and 799: 530:
had cursorial limb builds unlike typical tragulines and like smaller-sized members of the infraorder
6731:"New Fossil Remains of Artiodactyla from Dhok Pathan Formation, Middle Siwaliks of Punjab, Pakistan" 5892: 5790:
skeleton significant. It was first discovered by a private collector in 1981 within the locality of
4671:
was the largest species and likely lived in light forested habitats, where it would have had a more
1450:
near the border of Bulgaria and Turkey. The species was described as small and differing from other
1235:
sp., which was also known from Le Garouillas based on six astragali and probably a mandible of the P
9022: 3615: 8229:"Evolutionary history of hoofed mammals during the Oligocene–Miocene transition in Western Europe" 5918: 3666:, visible for a short distance, is oblique forwards and backwards and is pierced by several small 8781: 5955: 5794:. The specimen was sold to a German collector in 1984 who held on to it before selling it to the 5497:
only existed for one unit, MP28. The French locality of Pech Desse, an MP28-dated location with
5096: 4758: 1434:. The researchers decided that the fossil material belongs to a new species for which they named 971:, France in addition to previously collected Quercy materials. The skeleton was referred to as a 9049: 5474:) making their first appearances within the continent. The faunas of this time suggest woodland- 4215:(or "wings") that terminate posteriorly at a point exceeding the level of articulation with the 9129: 8984: 5343:
The Le Garouillas locality in France, dating to MP25, contains two, possibly three, species of
4748: 3639: 1477:
because they have bifurcated and shortened postentocristids that are close to the diagnosis of
1400:
In June 2018, Bastien Mennecart et al. described the earliest known European ruminant from the
9103: 7518:
Sun, Jimin; Ni, Xijun; Bi, Shundong; Wu, Wenyu; Ye, Jie; Meng, Jin; Windley, Brian F. (2014).
6772:
Zitteliana Reihe B: Abhandlungen der Bayerischen Staatssammlung fĂŒr PalĂ€ontologie und Geologie
5570:", which occurred between 24.8 and 24 Ma and marks the appearances of the small anthracothere 5431: 4267:
is not determinable because of the transversely flattened state of the sub-complete skeleton.
9124: 9116: 9044: 5428:
in Europe existed only in this locality, suggesting just a short period of existence there.
4949:, boosting the Antarctic glaciation that already started by the Eocene-Oligocene transition. 4823: 3765: 684:
in that the newer genus had all compressed lower premolars whereas only the last premolar of
8614:"Stepwise onset of the Icehouse world and its impact on Oligo-Miocene Central Asian mammals" 7520:"Synchronous turnover of flora, fauna, and climate at the Eocene-Oligocene Boundary in Asia" 5627:
could therefore also potentially be the result of competition with the "advanced" pecorans.
4211:, also known in the anatomy of the neck vertebrae as C1, possesses wide, rounded anatomical 4195:
skeleton is short and robust, its total length measuring less than that of the head. On the
1314: 1313:
maxillae originally from Tarn-et-Garonne, France dating to the Oligocene, now stored at the
696:
immediately following them was strong. Based on these traits, Filhol erected the genus name
8625: 8585: 8438: 8280: 8151: 7857: 7805: 7766: 7714: 7673: 7624: 7531: 7461: 7414: 7348: 7302: 7173: 7118: 7072: 7032: 6953: 6811: 6695: 6640: 6588: 6545: 6442: 6352: 6309: 6269: 5680: 4300: 4280: 1267: 680:, with the posterior edge extending as a deep furrow. It was therefore differentiated from 6747: 6730: 8: 7237:
Eronen, Jussi T.; Janis, Christine M.; Chamberlain, Charles Page; Mulch, Andreas (2015).
5326: 5176:, rodents (theridomyids, sciurids, eomyids, cricetids, murids, and glirids), hyaenodonts 3662:) apophysis (normal developmental outgrowth of a bone) by a mastoid of unknown size. The 8629: 8589: 8442: 8284: 8155: 7861: 7809: 7770: 7718: 7677: 7628: 7535: 7465: 7418: 7352: 7306: 7177: 7122: 7076: 7036: 6957: 6815: 6699: 6644: 6592: 6549: 6446: 6356: 6313: 6273: 3549:
and most other Paleogene ruminants are typically known mostly or only from jaw remains,
1223:, differing from other species by a few astragali whose dimensions are between those of 9152: 8874:(Report) (in French). Parc Naturel RĂ©gional des Causses du Quercy. 2022. Archived from 8820: 8728: 8692: 8646: 8613: 8557: 8510: 8485: 8461: 8426: 8407: 8366: 8296: 8250: 8169: 8120: 8083:
Actes du CongrĂšs Bio-chroM'97. MĂ©moires et Travaux de l'EPHE Institut de Montpellier 21
8003: 7968: 7924: 7878: 7845: 7844:
Mennecart, Bastien; Aiglstorfer, Manuela; Li, Yikun; Li, Chunxiao; Wang, Shiqi (2021).
7823: 7794:"Hogs, hippos or bears? Paleodiet of European Oligocene anthracotheres and entelodonts" 7732: 7642: 7592: 7552: 7519: 7477: 7364: 7320: 7263: 7238: 7216: 7141: 7106: 7002: 6965: 6863: 6827: 6752: 6711: 6458: 6325: 6019: 4308: 4188: 3590: 2832: 574: 378: 130: 7792:
Rivals, Florent; Belyaev, Ruslan I.; Basova, Vera B.; Prilepskaya, Natalya E. (2023).
7778: 7751: 7384:
Mitteilungen der Bayerischen Staatssammlung fĂŒr PalĂ€ontologie und historische Geologie
7084: 7044: 6148:"The phylogeny of hornless ruminants and a description of the cranium of Archaeomeryx" 1262:
In 2008, Jan van der Made reviewed the Oschiri fauna from the Mediterranean island of
610: 9111: 8824: 8732: 8696: 8651: 8561: 8515: 8466: 8411: 8300: 8254: 8173: 8124: 8081: 8022: 7999: 7972: 7883: 7827: 7736: 7646: 7596: 7557: 7496: 7481: 7446: 7368: 7268: 7212: 7146: 6867: 6756: 6715: 6667: 6489: 6462: 6329: 5134: 4987: 4695: 4212: 3686: 2852: 1549: 1388: 459:. The genus was erected in 1882 by Henri Filhol based on fossil remains found in the 8402: 8385: 8370: 8007: 7928: 7324: 7220: 7006: 6831: 6558: 6533: 6321: 6185: 6023: 5493:
4 Â°C (39 Â°F) increase in marine temperature. Unlike its two predecessors,
4907: 4623:, making the former adapted to more open habitats and the latter to closed habitats. 4441:
Comparisons (g and oz) of medial weight estimates from the astragalus size and the M
2850:
using additional remains from the genus. Similar to the research article from 2015,
8816: 8812: 8759: 8755: 8720: 8682: 8641: 8633: 8593: 8549: 8505: 8497: 8456: 8446: 8397: 8358: 8324: 8288: 8240: 8202: 8159: 8110: 8057: 7995: 7958: 7914: 7873: 7865: 7813: 7774: 7722: 7681: 7632: 7584: 7547: 7539: 7469: 7422: 7356: 7310: 7258: 7250: 7208: 7181: 7136: 7126: 7080: 7040: 6992: 6961: 6855: 6819: 6779: 6742: 6703: 6648: 6604: 6596: 6553: 6481: 6450: 6387: 6360: 6317: 6281: 6277: 6216: 6208: 6159: 6009: 5121: 5006: 4707: 4389: 4385: 4248: 4244: 4240: 3780:
are recorded to be lengthy. The complex of front teeth being very distant from the
3663: 3558: 1486: 1172: 727: 8724: 7360: 6859: 6707: 5462:, and most other typical Oligocene European faunas, with additional amphicyonids ( 4603: 3840:
and a shallow external postprotocristid that is not linked to the prehypocristid.
1211:. After reviewing the previous species, Sudre ascertained that another species of 676:
of the genus was 3:1:3:3, and the genus was characterized by its compressed lower
9007: 8597: 8328: 8164: 8139: 7818: 7793: 7588: 7185: 7131: 6823: 6600: 6454: 6364: 5938: 5687: 5258: 4967: 4922: 4857: 4853: 4790: 4762: 4536: 4208: 3643: 3607: 1534: 1421:
fossils. Since the terrestrial formation is overlain by two marine formations of
1093: 928: 539: 508: 500: 495:
has historically been assigned to various families within the ruminant infrorder
225: 8227:
Scherler, Laureline; Mennecart, Bastien; Hiard, Florent; Becker, Damien (2013).
8206: 6485: 6391: 5806:, located in the village of VachĂšres, was renovated and was chosen to house the 4319:(the other type of long bone found in the forearm) along its entire length. The 4275: 924: 838:
In 1957, the palaeontologist Friedlinde A. Obergfell erected a newer species of
9076: 7869: 7427: 7402: 6652: 6109: 5268:
were composed of three separate vegetational belts by latitude, with temperate
5202: 5014: 4975: 4971: 4943: 4786: 4216: 3781: 3651: 3647: 1562: 1104:
not belonging to the Hypertragulidae in that despite the tusk-like caniniform P
770:
but differed by its first lower premolar. He stated that the dental formula of
693: 673: 551: 534:. In addition, its dentition differs from other traguline families such as the 8687: 8670: 8245: 8228: 7919: 7902: 7315: 7290: 6426:
Mennecart, Bastien; Geraads, Denis; Spassov, Nikolai; Zagorchev, Ivan (2018).
6014: 5997: 5763: 5671:
followed by MP30. The last Oligocene-spanning artiodactyls and perissodactyls
5137:) and also arrived at western Europe where it took the same southern route as 3610:, although just slightly above the M, is as far from the anterior edge of the 1506: 9146: 8138:
Moreno-DomĂ­nguez, Rafael; Postigo-Mijarra, JosĂ© MÂȘ.; BarrĂłn, Eduardo (2021).
6783: 5515: 5398: 4912: 4866: 4801: 4715: 4316: 4204: 3772:
of similar size for wearing and the frontal teeth. The diastemas of C-P and P
3635: 3417: 3400: 2944: 2610: 2593: 2250: 2015: 1998: 1669: 1425:
age, however, the basal formation could be estimated to date from the latest
985: 821:. In 1986, however, GeneviĂšve Bouvrain, Denis Geraads and Jean Sudre revised 72: 8451: 7727: 7702: 7473: 4690: 1527: 8655: 8519: 8470: 7887: 7686: 7661: 7637: 7612: 7561: 7272: 7254: 7150: 6209:"Miocene Leptomerycidae (Artiodactyla, Ruminantia) and Their Relationships" 5779: 5737: 5691: 5572: 5394: 4957: 4393: 4344: 4332: 4224: 3655: 3631: 3619: 2896: 2859: 2202: 1604: 1570: 1513: 1401: 1147: 1078: 1001: 963:
as a genus in 1984, examining the cast of a sub-complete skeleton from the
647: 559: 468: 256: 247: 8610: 8427:"The enigma of Oligocene climate and global surface temperature evolution" 8292: 7752:"The Eocene-Oligocene ungulates from Western Europe and their environment" 6997: 6980: 4655:
was closest to those of selective browsers, consuming leaves, fruits, and
3759: 3756: 1361:
Additionally, Mennecart made a brief mention of the Sardinian artiodactyl
780: 777: 9016: 7963: 7946: 5858: 5598: 5361: 5273: 5252: 4894: 4889: 4782: 4774: 4656: 3584: 3014: 2827:
is phylogenetically related to other tragulines based on its caniniform P
2800: 2397: 2028: 1742: 1370: 1275: 1108:, the former was more advanced based on dental and postcranial evidence. 939:) teeth, and in 1980, S. David Webb and Beryl E. Taylor placed it in the 896:, closed on the rear; it instead turns inward and opens at the posterior 868: 651: 187: 47: 8908:(Map). Parc Naturel RĂ©gional des Causses du Quercy. 2023. Archived from 8902:
Les Causses du Quercy: Biking for our Fossils! Let's Travel Back in Time
7337: 619: 9090: 9036: 6057: 5783: 5732: 5470: 5439:
MP25 (middle Oligocene) records the last appearances of the entelodont
5309: 5277: 5208: 4991: 4983: 4931: 4885: 4876: 4336: 4315:, or one type of long bone found in the forearm, is separated from the 4264: 4256: 3658:
is the auditory hole, separated from a strong paramastoid (or near the
3623: 3611: 3081: 3018: 2927: 2882: 2788: 2781: 2776: 2411: 2401: 2233: 2165: 2158: 2153: 1756: 1746: 1652: 1422: 1294: 1184: 1018: 846:
from the German locality of Wintershof-West. He said that it resembled
735: 724: 535: 114: 92: 57: 8637: 8553: 8501: 8362: 7543: 6668:"Evolution and classification of Tragulina (Ruminantia, Artiodactyla)" 6609: 4785:), Balkanatolia, and eastern Eurasia (Balkanatolia was in between the 4559:, according to its dental traits, was barely larger as a species than 988:. In comparison, the only dental trait the hypertragulids shared with 523: 8137: 7494: 7445:
Hooker, Jerry J.; Collinson, Margaret E.; Sille, Nicholas P. (2004).
6220: 6163: 6058:"Un ruminant nouveau des faluns miocĂšnesde la Touraine et de l'Anjou" 5611: 5281: 5196: 5191: 4794: 4721: 4684: 4540: 4376: 4370: 4355: 4348: 4324: 4320: 3799:, a strong presence of a distally isolated posterolabial cristid on P 3119: 3102: 2846: 2377: 1722: 1426: 1417: 1379: 1192: 1188: 964: 920: 855: 851: 701: 677: 663: 632:
left ramus of a mandible in an 1885 fossil mammals catalogue for the
496: 486: 456: 448: 207: 147: 97: 41: 34: 8978: 8537: 8115: 8098: 7609: 9070: 9001: 5897:
Comptes rendus hebdomadaires des séances de l'Académie des sciences
5475: 5168: 5156:. The two species were found in the same locality as the marsupial 4979: 4952: 4770: 4730: 4714:) lives in tropical African habitats including swampy habitats and 4672: 4328: 4228: 4200: 3690: 3667: 1409: 1374: 1288: 1263: 1052: 1009: 936: 555: 197: 167: 87: 82: 67: 62: 52: 7198: 6147: 3606:
is the great development of its face, as the anterior edge of the
2870:, which is typically considered to be either next to the outgroup 1383:. In 2017, Mennecart et al. said that the islands of Sardinia and 1179:
is also excluded from the Pecora by the presence of a caniniform P
1096:
wrote a journal questioning and revising traguline clades such as
654:
genera from the lime phosphate deposits of the French province of
8062: 8045: 5775: 5759: 5607: 5464: 5269: 5010: 4995: 4881: 4648: 4364: 4304: 4296: 4232: 4196: 3682: 3659: 3627: 1384: 1271: 968: 689: 547: 102: 77: 8486:"The ossicular chain of Cainotheriidae (Mammalia, Artiodactyla)" 8383: 6425: 5996:
Mennecart, Bastien; Becker, Damien; Berger, Jean-Pierre (2010).
4335:, although it is still shorter than that of the Tragulidae. The 8341: 7700: 5810:
skeleton, where it is considered a significantly unique piece.
4252: 3209: 2805: 2793: 2170: 2032: 1447: 1413: 1405: 1132: 662:
epoch in 1882. He thought that the first genus belonged to the
659: 655: 531: 452: 177: 157: 30: 8935:"BouziĂšs. RĂ©ception des sculptures "Mon village, mon fossile"" 8709: 8574: 8044:
Mennecart, Bastien; Radović, Predrag; Marković, Zoran (2018).
7791: 4926:
33.6-33.4 Ma. The event correlates directly with or after the
4528:
14,104 g (497.5 oz) - 23,808 g (839.8 oz)
876:
is the type species. He acknowledged the similarities between
8313: 7659: 6377: 5923:. London, Printed by order of the Trustees. pp. 155–159. 5767: 4619:
was larger and more cursorial based on limb proportions than
4511:
4,906 g (173.1 oz) - 12,202 g (430.4 oz)
4340: 4220: 3746:
from Pech Desse, France (2-3) and Gaimersheim, Germany (4-9).
831:
for which the type and only confirmable species would become
785:, that the upper cheek of the genus closely resemble that of 577:
based on their different ecological niches. The last species
480: 8424: 8270: 8226: 6380:
Neues Jahrbuch fĂŒr Geologie und PalĂ€ontologie - Abhandlungen
5758:
was found in the commune of CĂ©reste in the French region of
5144:
The Itardies locality of France is dated to MP23, after the
4659:
that would have been common in humid forested environments.
4495:
4,772 g (168.3 oz) - 6,959 g (245.5 oz)
4479:
4,089 g (144.2 oz) - 5,229 g (184.4 oz)
1565:, since they had changed little in the evolutionary record. 8483: 8096: 7236: 6844: 6130:
Comptes Rendus sommaires de la Société Géologique de France
5956:"Eine Zeitschrift FĂŒr Anatomie Und Entwickelungsgeschichte" 5854: 5478:
environments with forested areas and tree-shrub savannahs.
5173: 4935: 4312: 4260: 1485:. The fossils also have upper molars that possess a strong 1438:. The holotype and only specimen is a right mandible with P 1051:
was considered to have characterized the middle Oligocene (
6627:
Escarguel, Gilles; Legendre, Serge; Sigé, Bernard (2008).
6530: 5706:
since MP29 until the appearances of the Neogene tragulids
4173:
20.4 mm (0.80 in) - 22.5 mm (0.89 in)
4148:
30.5 mm (1.20 in) - 35.7 mm (1.41 in)
1155:
is narrow and somewhat "pinched" in appearance similar to
954: 738:(chevrotains/mouse-deer/tragulids) and listed the species 704:," a location of phosphorite deposits. The first species, 8802: 7944: 7163: 5750:
skeleton, indicating co-existence by the early Oligocene.
5454:
The faunas of MP26 were similar to preceding units, with
3950:
Measurements (mm & in) of the teeth and diastemas of
1127:
teeth. Janis said that the hypothesis that a caniniform P
1004:
shared with them. Furthermore, the C is reduced and the P
8043: 7843: 6684: 5017:, dating to MP21 or MP22, indicates the co-existence of 4255:
is short because it does not exceed the cavities of the
4199:(or shoulder blade), the spine ends in a strong, hooked 4111:
19.5 mm (0.77 in) - 22 mm (0.87 in)
4064:
23 mm (0.91 in) - 25.2 mm (0.99 in)
4061:
18 mm (0.71 in) - 18.2 mm (0.72 in)
1171:
fold" is retained in the lower molars, and the internal
546:
by a combination of a tusklike but reduced bottom first
475:; five more species have since been named although one, 5813: 5359:
sp. The locality has also recorded multiple nimravids (
4583:
overlapping in the MP zones with other species such as
4176:
26 mm (1.0 in) - 32.4 mm (1.28 in)
4120:
26.5 mm (1.04 in) - 28 mm (1.1 in)
4114:
50.5 mm (1.99 in) - 51 mm (2.0 in)
911:
As a result of the perceived closeness of the genus to
8774:"The village of VachĂšres and the Pierre MARTEL Museum" 8191: 8187: 8185: 8183: 8079: 6577: 6062:
Bulletin du Muséum Nationald'Histoire Naturelle, Paris
5943:(in French). Vol. 2. G. Masson. pp. 456–463. 5774:, fossil remains of birds that could be identified as 5724: 4117:
20 mm (0.79 in) - 22 mm (0.87 in)
4055:
10 mm (0.39 in) - 15 mm (0.59 in)
1404:, which is located mostly within the European area of 1067:
was recognized by the palaeontologist, differing from
688:, which has four premolars total, was compressed. The 6981:"Estimating body mass from the astragalus in mammals" 6626: 5995: 5630:
Other typical Oligocene faunas would eventually join
4223:
of the atlas reach dorsally almost to the top of the
7444: 6901: 6728: 5976: 4683:
seem, regardless of their preferred habitats, to be
4429:
nov. sp. (the last of which would later be known as
4170:
51 mm (2.0 in) - 52 mm (2.0 in)
4167:
32 mm (1.3 in) - 34 mm (1.3 in)
4145:
26 mm (1.0 in) - 28 mm (1.1 in)
4058:
40 mm (1.6 in) - 42 mm (1.7 in)
1446:, which was found south of the Bulgarian village of 1301: 360: 271: 263: 8180: 7574: 6928:. Johns Hopkins University Press. pp. 189–212. 4405:In September 1995, prior to Sudre's publication on 4323:of the ulna is wide and located in the axis of the 4287:), a deer species whose cursorial limb proportions 3784:, probably in relation to the strengthening of the 1195:, for which she named the family "Bachitheriidae." 7065:Comptes Rendus de l'AcadĂ©mie des Sciences de Paris 6236:Comptes Rendus de l'AcadĂ©mie des Sciences de Paris 6190:Comptes Rendus de l'AcadĂ©mie des Sciences de Paris 6152:Bulletin of the American Museum of Natural History 5979:Comptes Rendus de l'AcadĂ©mie des Sciences de Paris 850:from the phosphorite sites of Quercy based on the 8144:Palaeogeography, Palaeoclimatology, Palaeoecology 7798:Palaeogeography, Palaeoclimatology, Palaeoecology 7759:Palaeogeography, Palaeoclimatology, Palaeoecology 6923: 6581:Palaeogeography, Palaeoclimatology, Palaeoecology 6513:. Johns Hopkins University Press. pp. 59–84. 6435:Palaeogeography, Palaeoclimatology, Palaeoecology 6295: 6293: 6291: 6255: 6253: 6251: 6249: 6141: 6139: 5746:. The skeleton was found in the same area as the 5566:MP28 marks a faunal turnover event known as the " 1282:, in which he would eventually erect the species 9144: 5719: 4351:is robust but is shorter than that of camelids. 1183:tooth and the possession of a traguloid type of 8431:Proceedings of the National Academy of Sciences 7839: 7837: 7394: 7100: 7098: 7096: 7094: 7058: 7056: 7054: 6919: 6917: 6801: 6797: 6795: 6793: 6526: 6524: 6522: 6520: 6480:. Casebooks in Earth Sciences. pp. 87–94. 6421: 6183: 5501:, also has fossil remains of the lophiomerycid 5091: 1043:By 1986, Jean Sudre conducted a close study of 943:by diagnosis of a large mastoid fissure of the 931:in 1946 based on the bachitheriid's tusk-like P 8839:"Cherchez Les 7 Sculptures d'Animaux Disparus" 8668: 8531: 8529: 8266: 8264: 7381: 6939: 6937: 6935: 6419: 6417: 6415: 6413: 6411: 6409: 6407: 6405: 6403: 6401: 6288: 6246: 6136: 5340:was able to cross through the turnover event. 3709:Front of premaxilla to top of occipital crest 3596:Smithsonian National Museum of Natural History 1358:and thereby advancing knowledge of the genus. 1219:from the locality of Le Garouillas in France, 959:Genevieve Bouvrain and Denis Geraads reviewed 7284: 7282: 6943: 6897: 6103: 6101: 6099: 6097: 6095: 4437:area, both results shown in the below table: 451:ruminants that lived in Europe from the late 8869:Les Causses du Quercy: Bilan d'ActivitĂ© 2021 8020: 7834: 7440: 7438: 7232: 7230: 7091: 7051: 6914: 6895: 6893: 6891: 6889: 6887: 6885: 6883: 6881: 6879: 6877: 6790: 6769: 6517: 6508: 6342: 6184:Bouvrain, GeneviĂšve; Geraads, Denis (1985). 6093: 6091: 6089: 6087: 6085: 6083: 6081: 6079: 6077: 6075: 4753: 1391:. However, they also warned that except for 708:, was determined to be a large animal while 8745: 8669:Rössner, Gertrud E.; Heissig, Kurt (2013). 8526: 8261: 8021:Fejfar, Oldƙich; Kaiser, Thomas M. (2005). 7940: 7938: 6932: 6665: 6398: 6179: 6177: 6175: 6173: 5108:and associated rodents coexisting with it ( 692:, he observed, were quite small, while the 666:family and must be closely affiliated with 565:Based on its dental and limb morphologies, 125:skeleton, Pierre Martel Museum of VachĂšres 8090: 7279: 6622: 6620: 6206: 6145: 5744:National Museum of Natural History, France 5247: 3768:, the C is lodged between the caniniform P 3712:Front of nasals to top of occipital crest 113: 8686: 8645: 8509: 8460: 8450: 8401: 8317:Biological Journal of the Linnean Society 8244: 8222: 8220: 8218: 8216: 8195:Zoological Journal of the Linnean Society 8163: 8114: 8061: 7962: 7918: 7877: 7817: 7743: 7726: 7685: 7636: 7551: 7517: 7435: 7426: 7400: 7314: 7262: 7227: 7140: 7130: 6996: 6978: 6874: 6746: 6608: 6557: 6207:Taylor, Beryl E.; Webb, S. David (1976). 6146:Webb, S. David; Taylor, Beryl E. (1980). 6107: 6072: 6036: 6013: 5953: 5912: 5910: 4303:is strong and oval. There is neither any 3706:Front of premaxilla to occipital condyle 1489:that surrounds the protocone, whereas in 1036:, which has a strong C and a caniniform P 8957:"Bach. Une nouvelle sculpture inaugurĂ©e" 8535: 7935: 7104: 6666:Vislobokova, Innessa Anatolevna (2001). 6170: 6055: 5932: 5930: 5916: 5731: 5430: 5251: 5095: 4951: 4906: 4800: 4757: 4689: 4602: 4547: 4274: 3733: 3583: 1552:, a lack of posterolingual cristids on P 1537:, who created the family Bachitheriidae. 1305: 1077: 8845:(in French). 2022-01-26. Archived from 7749: 7062: 7022: 7018: 7016: 6617: 6502: 6127: 5576:and pecorans of uncertain affinities: " 4636:sp. represents a distinct species from 4343:is moderately elevated compared to the 3788:, constitutes the main autapomorphy of 955:Modern revisions of Paleogene ruminants 9145: 8213: 7985: 7900: 7401:MĂ©tais, GrĂ©goire; Sen, Sevket (2017). 7288: 6573: 6571: 6569: 5936: 5907: 5890: 3742:from Mailhat, France (Specimen 1) and 1349:from MP25-26. According to Mennecart, 1032:. These traits strongly contrast with 813:, as described by Filhol in 1877, and 8983: 8982: 8075: 8073: 6475: 6299: 6259: 6233: 5927: 4902: 4182: 3815:. The European Tragulidae (including 3697:Cranial lengths (mm & in) of the 1416:. The area is known for having three 1092:In 1987, the British palaeontologist 716:but larger than the smallest species 7013: 4219:of the cervical vertebrae (C2). The 3844:Dental lengths (mm & in) of the 1075:(Filhol 1877) was the type species. 1008:tooth is small and separated by the 798:In 1886, the German palaeontologist 640:mandible at the same museum (right). 7577:Journal of Systematic Palaeontology 6804:Journal of Systematic Palaeontology 6748:10.17582/journal.pjz/20181028131031 6566: 758:" in 1877 prior to the erection of 514:For much of its taxonomic history, 13: 8070: 7243:Proceedings of the Royal Society B 6966:10.1111/j.1502-3931.1995.tb01423.x 6688:Journal of Vertebrate Paleontology 6262:Journal of Vertebrate Paleontology 4675:diet consisting mostly of leaves. 4295:In bachitheriids, the neck of the 4105:Old collections of Quercy, France 4077:Old collections of Quercy, France 1022:, the later leptomerycids such as 791:. Additionally, he also confirmed 499:, but was reclassified to its own 14: 9214: 8780:. 26 January 2018. Archived from 7454:Journal of the Geological Society 5160:(multiple species), nyctitheriid 4663:would have been a counterpart to 4384:are a little less elongated. The 1496: 1454:species by the structure of its P 1302:Increased role of biostratigraphy 1175:is retained in the upper molars. 672:. According to Filhol, the lower 634:British Museum of Natural History 8778:Parc naturel rĂ©gional du Luberon 8000:10.1046/j.1463-6409.2003.00116.x 7213:10.1046/j.0300-3256.2001.00071.x 5804:Pierre Martel Museum of VachĂšres 4742: 4598: 4460:Astragalus Size Weight Estimate 4380:), although the distal limbs in 3598:in a close-up view of the skull. 1526: 1505: 618: 609: 600: 522:was uncovered in the commune of 134: 45: 9183:Prehistoric Artiodactyla genera 8949: 8927: 8893: 8861: 8831: 8796: 8766: 8739: 8703: 8662: 8604: 8568: 8477: 8418: 8403:10.5252/geodiversitas2020v42a18 8377: 8335: 8307: 8131: 8037: 8014: 7979: 7894: 7785: 7694: 7653: 7603: 7568: 7511: 7488: 7375: 7331: 7192: 7157: 6972: 6838: 6763: 6722: 6678: 6659: 6559:10.1016/j.earscirev.2022.103929 6469: 6371: 6336: 6227: 6200: 6121: 5005:The site locality Detan of the 1467:Palaeontological Museum, Munich 1256:, found in the same deposit as 1087:Natural History Museum of Basel 923:, although the palaeontologist 919:was normally placed within the 8817:10.30486/gcr.2021.1913051.1050 8760:10.30486/GCR.2021.1915524.1068 7295:Swiss Journal of Palaeontology 6282:10.1080/02724634.1987.10011653 6117:(PhD). UniversitĂ© de Fribourg. 6049: 6030: 5989: 5970: 5947: 5884: 5683:. The Paleogene ursids of the 5021:cf. curtum with the marsupial 4809:in a subtropical environment. 4525:18,647 g (657.8 oz) 4522:12,913 g (455.5 oz) 4291:is suggested to be similar to. 4027:>14 mm (0.55 in) 3848:skeleton from Cereste, France 3701:skeleton from Cereste, France 3540: 658:that he thought indicated the 1: 9198:Fossil taxa described in 1882 8725:10.1080/08912963.2022.2144285 7779:10.1016/S0031-0182(00)00252-2 7361:10.1080/08912963.2022.2060098 7085:10.1016/S1251-8050(98)80081-5 7045:10.1016/S0016-6995(97)80123-4 6985:Acta Palaeontologica Polonica 6926:The Evolution of Artiodactyls 6860:10.1080/08912963.2021.2014479 6708:10.1080/02724634.2019.1722682 6511:The Evolution of Artiodactyls 6302:Palaeontographica Abteilung A 5877: 5720:Palaeontological significance 5647:became extinct by MP29 while 5544: 5148:, and has fossil evidence of 4628:fossil evidence of different 4508:7,722 g (272.4 oz) 4505:6,905 g (243.6 oz) 4492:6,114 g (215.7 oz) 4489:6,905 g (243.6 oz) 4476:4,553 g (160.6 oz) 4473:4,736 g (167.1 oz) 4439: 3948: 3842: 3695: 1217:Quercy Phosphorites Formation 562:traits unique to the genus. 471:, and another species called 461:Quercy Phosphorites Formation 8675:Swiss Journal of Geosciences 8598:10.1016/j.annpal.2013.11.002 8233:Swiss Journal of Geosciences 8165:10.1016/j.palaeo.2021.110302 7907:Swiss Journal of Geosciences 7819:10.1016/j.palaeo.2022.111363 7589:10.1080/14772019.2012.671790 7186:10.1016/j.mambio.2009.05.007 7132:10.1371/journal.pone.0116830 6979:Tsubamoto, Takehisa (2014). 6824:10.1080/14772019.2014.948505 6601:10.1016/j.palaeo.2011.01.005 6455:10.1016/j.palaeo.2018.01.011 6365:10.1016/j.quaint.2007.09.036 6002:Swiss Journal of Geosciences 5862:, and two bats of the genus 5796:Luberon Regional Nature Park 5308:both survived the event and 5146:Bachitherium Dispersal Event 5092:Bachitherium Dispersal Event 4978:, and amynodonts). Rodents ( 4400: 4142:57.6 mm (2.27 in) 4139:27.5 mm (1.08 in) 3943:62.5 mm (2.46 in) 3940:33.4 mm (1.31 in) 3937:27.7 mm (1.09 in) 3934:27.2 mm (1.07 in) 3928:56.5 mm (2.22 in) 3925:30.2 mm (1.19 in) 3922:25.7 mm (1.01 in) 3729: 1016:in early leptomerycids like 734:provisionally in the family 487: 354:Species pending reassessment 7: 9178:Oligocene mammals of Europe 6735:Pakistan Journal of Zoology 6486:10.1007/978-1-4613-8271-3_9 6108:Mennecart, Bastien (2012). 5800:Luberon UGGp Geology Museum 5639:remains unknown, however). 5104:During the Grande Coupure, 4928:Eocene-Oligocene transition 3931:7.8 mm (0.31 in) 3832:being longer than that of P 3677:while the other is behind M 1432:Eocene-Oligocene transition 1329:as ranging from MP22-MP27, 1221:Bachitherium guirounetensis 1012:of the canine as with the P 892:" is not, at least on the P 700:, basing its etymology on " 646:The French palaeontologist 595: 331:Bachitherium guirounetensis 10: 9219: 9203:Taxa named by Henri Filhol 9158:Cenozoic mammals of Europe 8329:10.1093/biolinnean/blac002 8050:Palaeontologia Electronica 8027:Palaeontologia Electronica 7870:10.1038/s41598-021-96221-x 7428:10.1016/j.crpv.2017.01.001 7105:Menncart, Bastien (2015). 6653:10.1016/j.crte.2007.11.005 6056:Ginsburg, LĂ©onard (1971). 5917:Lydekker, Richard (1885). 5814:"Mon village, mon fossile" 5300:. The two other ruminants 4746: 4247:(probably sacral), and 17 4089:25 mm (0.98 in) 4033:18 mm (0.71 in) 3723:197 mm (7.8 in) 3720:208 mm (8.2 in) 3717:183 mm (7.2 in) 3572:is commonly confused with 3153:Archaeotragulus krabiensis 2426:Archaeotragulus krabiensis 1771:Archaeotragulus krabiensis 1458:being similar to that of P 1215:could be erected from the 884:" but noticed that unlike 554:, caniniform first bottom 481: 9060: 8991: 8688:10.1007/s00015-013-0132-x 8246:10.1007/s00015-013-0140-x 8207:10.1093/zoolinnean/zly052 7920:10.1007/s00015-009-1330-4 7316:10.1007/s13358-014-0069-3 6633:Comptes Rendus Geoscience 6322:10.1127/pala/236/1995/205 6213:American Museum Novitates 6015:10.1007/s00015-010-0034-0 5824:Causses du Quercy Geopark 5690:were replaced by similar 4754:Pre-Grande Coupure Europe 4462: 4459: 4452: 4449: 4161:Pech Desse (Lot, France) 4092:37 mm (1.5 in) 4086:63 mm (2.5 in) 4083:38 mm (1.5 in) 4049:Nassiet (Landes, France) 4000: 3990: 3980: 3970: 3967: 3964: 3961: 3958: 3942: 3939: 3936: 3933: 3930: 3927: 3924: 3921: 3919:41 mm (1.6 in) 3918: 3906: 3896: 3886: 3875: 3864: 3861: 3858: 3855: 3852: 3740:Bachitherium cf. lavocati 3738:The various specimens of 3722: 3719: 3716: 3711: 3708: 3705: 3622:probably bordered by the 3414: 3397: 3390: 3373: 3366: 3349: 3342: 3325: 3318: 3305:Prodremotherium elongatum 3301: 3294: 3277: 3270: 3244: 3227: 3220: 3213: 3166: 3149: 3142: 3116: 3099: 3092: 3085: 3058: 3043: 3036: 3029: 3022: 2998: 2991: 2974: 2967: 2941: 2924: 2917: 2910: 2893: 2886: 2773: 2665: 2648: 2631: 2624: 2607: 2590: 2583: 2570:Prodremotherium elongatum 2566: 2549: 2542: 2525: 2518: 2494: 2479: 2472: 2465: 2439: 2422: 2415: 2405: 2381: 2371: 2354: 2347: 2321: 2304: 2287: 2280: 2273: 2247: 2230: 2223: 2216: 2199: 2192: 2150: 2060: 2043: 2036: 2012: 1995: 1988: 1971: 1958:Prodremotherium elongatum 1954: 1937: 1930: 1913: 1906: 1882: 1867: 1860: 1834: 1817: 1810: 1784: 1767: 1760: 1750: 1726: 1716: 1699: 1692: 1666: 1649: 1642: 1625: 1618: 1601: 1594: 384: 377: 292: 287: 262: 255: 131:Scientific classification 129: 121: 112: 23: 9193:Eocene first appearances 9173:Eocene mammals of Europe 8805:Geoconservation Research 8748:Geoconservation Research 8578:Annales de PalĂ©ontologie 8536:de Bonis, Louis (2013). 7750:Blondel, CĂ©cile (2001). 6345:Quaternary International 5960:Morphologisches Jahrbuch 5869:The installation of the 5802:. In 1995, the regional 5756:Bachitherium cf. insigne 5726:Bachitherium cf. insigne 5420:, and the lophiomerycid 4819:Bachitherium thraciensis 4270: 4136:Middle Oligocene (MP25) 3846:Bachitherium cf. insigne 3699:Bachitherium cf. insigne 3579: 3555:Bachitherium cf. insigne 2945:Hypertragulus calcaratus 2251:Hypertragulus calcaratus 1670:Hypertragulus calcaratus 1516:, who erected the genus 1471:Gelocus villebramarensis 1436:Bachitherium thraciensis 977:Bachitherium cf. insigne 817:synonyms of the species 762:). Lydekker stated that 636:(left) and a photo of a 342:Bachitherium thraciensis 123:Bachitherium cf. insigne 16:Extinct genus of mammals 8963:(in French). 2022-11-18 8937:(in French). 2022-08-13 8452:10.1073/pnas.2003914117 7901:Becker, Damien (2009). 7728:10.5194/cp-17-2343-2021 7474:10.1144/0016-764903-091 7289:Maitre, Elodie (2014). 6672:Paleontological Journal 6392:10.1127/njgpa/2017/0688 5954:Schlosser, Max (1886). 5549:By the late Oligocene, 5248:Europe in the Oligocene 4657:dicotyledonous herbages 4052:Early Oligocene (MP23) 1394:Sardomeryx oschiriensis 975:species of large size ( 888:, the tooth valley of " 854:being connected to the 447:is an extinct genus of 346:Mennecart et al., 2018 9168:Oligocene Artiodactyla 7687:10.5194/cp-18-341-2022 7638:10.5194/cp-17-269-2021 7407:Comptes Rendus Palevol 7255:10.1098/rspb.2015.0136 6784:10.5282/ubm/epub.22383 5937:Filhol, Henri (1877). 5891:Filhol, Henri (1882). 5751: 5436: 5264: 5101: 4962: 4917: 4814: 4766: 4749:Mammal Paleogene zones 4703: 4643:During the Oligocene, 4624: 4553: 4292: 4164:Late Oligocene (MP28) 4133:Le Garouillas, France 4108:Oligocene (MP23-MP27) 4080:Oligocene (MP23-MP27) 3747: 3599: 3353:Dremotherium feignouxi 2978:Lophiomeryx chalaniati 2652:Dremotherium feignouxi 2358:Lophiomeryx chalaniati 2064:Dremotherium feignouxi 1703:Lophiomeryx chalaniati 1318: 1266:, which dates back to 1231:. He also mentioned a 1089: 1059:and the newer species 967:limestone locality of 712:was much smaller than 581:probably evolved from 560:evolutionarily derived 9188:Oligocene extinctions 9125:Paleobiology Database 9045:Paleobiology Database 8293:10.2110/palo.2018.022 6998:10.4202/app.2011.0067 6538:Earth-Science Reviews 6132:(in French): 115–117. 5735: 5434: 5255: 5099: 4994:, Amphicyonidae, and 4955: 4910: 4827:, the anthracotheres 4804: 4789:of the north and the 4761: 4747:Further information: 4693: 4606: 4551: 4501:Bachitherium lavocati 4457:Area Weight Estimate 4278: 3819:of the Paleogene and 3737: 3650:protruding above the 3587: 3418:Amphitragulus quercyi 3401:Amphitragulus elegans 3329:Pseudomeryx gobiensis 2669:Pseudomeryx gobiensis 2611:Amphitragulus quercyi 2594:Amphitragulus elegans 2016:Amphitragulus quercyi 1999:Amphitragulus elegans 1975:Pseudomeryx gobiensis 1309: 1094:Christine Marie Janis 1081: 1025:Pseudoparablastomeryx 742:, for which he made " 723:In 1885, the English 650:described two fossil 320:Bachitherium lavocati 29:Temporal range: Late 7964:10.20341/gb.2020.006 4934:that caused drastic 4892:, and the marsupial 4849:Brachydiastematerium 4712:Hyemoschus aquaticus 4463:Weight Limit Values 4301:infraspinatus muscle 4281:southern red muntjac 3786:adductor musculature 3281:Mosaicomeryx quercyi 3061:Bachitherium insigne 2897:Archaeomeryx optatus 2553:Mosaicomeryx quercyi 2497:Bachitherium insigne 2203:Archaeomeryx optatus 1941:Mosaicomeryx quercyi 1885:Bachitherium insigne 1605:Archaeomeryx optatus 1083:Bachitherium insigne 795:as a valid species. 298:Bachitherium insigne 9163:Eocene Artiodactyla 8630:2016NatSR...636169H 8590:2014AnPal.100....1P 8443:2020PNAS..11725302O 8437:(41): 25302–25309. 8285:2018Palai..33..514S 8156:2021PPP...56710302M 7862:2021NatSR..1117710M 7810:2023PPP...61111363R 7771:2001PPP...168..125B 7719:2021CliPa..17.2343B 7707:Climate of the Past 7678:2022CliPa..18..341T 7666:Climate of the Past 7629:2021CliPa..17..269H 7617:Climate of the Past 7536:2014NatSR...4E7463S 7466:2004JGSoc.161..161H 7419:2017CRPal..16..382M 7353:2022HBio...34.1623B 7307:2014SwJP..133..141M 7178:2010MamBi..75..471M 7123:2015PLoSO..1016830M 7077:1998CRASE.326..527B 7037:1997Geobi..30..573B 6958:1995Letha..28..197M 6816:2015JSPal..13..581M 6700:2019JVPal..39E2682D 6645:2008CRGeo.340..602E 6593:2011PPP...301...97C 6550:2022ESRv..22603929L 6447:2018PPP...498....1M 6357:2008QuInt.182..116V 6314:1995PalAA.236..205S 6274:1987JVPal...7..200J 5772:Diplocynodon rateli 5645:Paenanthracotherium 5507:Paenanthracotherium 5330:, and rhinocerotid 5327:Paenanthracotherium 5240:, and the tragulid 4839:, the brontotheres 4805:Old restoration of 4793:of the south). The 4485:Bachitherium curtum 4469:Bachitherium vireti 4446: 3955: 3849: 3702: 3120:Nalameryx sulaimani 3046:Bachitherium curtum 2482:Bachitherium curtum 1870:Bachitherium curtum 1311:Bachitherium curtum 1284:Bachitherium sardus 992:is the caniniform P 819:Cryptomeryx gaudryi 748:Bachitherium medium 740:Bachitherium curtum 638:Bachitherium curtum 630:Bachitherium curtum 465:Bachitherium curtum 407:Bachitherium medium 365:Bachitherium sardus 309:Bachitherium vireti 276:Bachitherium curtum 8713:Historical Biology 8618:Scientific Reports 8490:Journal of Anatomy 8103:Geological Journal 7850:Scientific Reports 7524:Scientific Reports 7341:Historical Biology 6848:Historical Biology 5752: 5568:Microbunodon Event 5437: 5381:, rhinocerotoids ( 5265: 5102: 4982:, Cricetidae, and 4963: 4918: 4903:The Grande Coupure 4815: 4767: 4704: 4625: 4554: 4440: 4309:deltoid tuberosity 4293: 4189:cervical vertebrae 4183:Vertebrae and ribs 3954:species holotypes 3949: 3843: 3748: 3696: 3614:as it is from the 3602:A unique trait of 3600: 3591:Tragulus javanicus 3377:Dremotherium guthi 3231:Notomeryx besensis 2833:parallel evolution 2635:Dremotherium guthi 2291:Notomeryx besensis 2047:Dremotherium guthi 1821:Notomeryx besensis 1319: 1315:MusĂ©um de Toulouse 1090: 1085:mandible remains, 815:Bachitherium minus 806:for which he made 802:erected the genus 575:niche partitioning 369:van der Made, 2008 9140: 9139: 9112:Open Tree of Life 8985:Taxon identifiers 8719:(12): 2456–2503. 8638:10.1038/srep36169 8554:10.5252/g2013n4a4 8502:10.1111/joa.13190 8363:10.5252/g2014n4a4 7988:Zoologica Scripta 7951:Geologica Belgica 7544:10.1038/srep07463 7503:. 1 (in French). 7201:Zoologica Scripta 7166:Mammalian Biology 6854:(12): 2295–2303. 6639:(9–10): 602–614. 6495:978-1-4613-8273-7 6039:Palaeontographica 5966:. Carl Gegenbaur. 5832:B. guirounetensis 5353:B. guirounetensis 5084:, and hyaenodont 5064:, anthracotheres 5009:of the region of 4988:Amphicynodontidae 4861:, the hyracodont 4696:lesser mouse-deer 4638:B. guirounetensis 4589:B. guirounetensis 4532: 4531: 4431:B. guirounetensis 4407:B. guirounetensis 4368:) or small deer ( 4285:Muntiacus muntjak 4180: 4179: 4126:B. guirounetensis 4021:Sladun, Bulgaria 3947: 3946: 3727: 3726: 3687:condyloid process 3654:. Forward of the 3537: 3536: 3528: 3527: 3519: 3518: 3510: 3509: 3501: 3500: 3492: 3491: 3483: 3482: 3474: 3473: 3465: 3464: 3456: 3455: 3447: 3446: 3438: 3437: 3429: 3428: 3259: 3258: 3248:Indomeryx cotteri 3199: 3198: 3190: 3189: 3181: 3180: 3131: 3130: 3103:Nalameryx savagei 3071: 3070: 2956: 2955: 2928:Leptomeryx evansi 2872:Amphirhagatherium 2853:Amphirhagatherium 2819: 2818: 2770: 2769: 2761: 2760: 2752: 2751: 2743: 2742: 2734: 2733: 2725: 2724: 2716: 2715: 2707: 2706: 2698: 2697: 2689: 2688: 2680: 2679: 2529:Gobiomeryx dubius 2507: 2506: 2454: 2453: 2336: 2335: 2325:Miomeryx altaicus 2308:Indomeryx cotteri 2262: 2261: 2234:Leptomeryx evansi 2184: 2183: 2147: 2146: 2138: 2137: 2129: 2128: 2120: 2119: 2111: 2110: 2102: 2101: 2093: 2092: 2084: 2083: 2075: 2074: 1917:Gobiomeryx dubius 1895: 1894: 1849: 1848: 1838:Indomeryx cotteri 1799: 1798: 1681: 1680: 1653:Leptomeryx evansi 1629:Miomeryx altaicus 1389:Mediterranean Sea 1339:B. guirounetensis 1254:B. guirounetensis 1245:B. guirounetensis 1229:B. guirounetensis 1191:genus within the 951:(incisor) teeth. 927:placed it in the 491:meaning "beast". 440: 439: 433: 423: 411: 403: 393: 370: 355: 347: 336: 325: 314: 303: 251: 229: 9210: 9133: 9132: 9120: 9119: 9107: 9106: 9094: 9093: 9081: 9080: 9079: 9053: 9052: 9040: 9039: 9027: 9026: 9025: 9012: 9011: 9010: 8980: 8979: 8973: 8972: 8970: 8968: 8953: 8947: 8946: 8944: 8942: 8931: 8925: 8924: 8922: 8920: 8914: 8907: 8897: 8891: 8890: 8888: 8886: 8880: 8873: 8865: 8859: 8858: 8856: 8854: 8843:Le Petit Journal 8835: 8829: 8828: 8800: 8794: 8793: 8791: 8789: 8784:on July 24, 2023 8770: 8764: 8763: 8743: 8737: 8736: 8707: 8701: 8700: 8690: 8666: 8660: 8659: 8649: 8608: 8602: 8601: 8572: 8566: 8565: 8533: 8524: 8523: 8513: 8481: 8475: 8474: 8464: 8454: 8422: 8416: 8415: 8405: 8381: 8375: 8374: 8348: 8339: 8333: 8332: 8311: 8305: 8304: 8268: 8259: 8258: 8248: 8224: 8211: 8210: 8189: 8178: 8177: 8167: 8135: 8129: 8128: 8118: 8094: 8088: 8087: 8077: 8068: 8067: 8065: 8041: 8035: 8034: 8018: 8012: 8011: 7983: 7977: 7976: 7966: 7942: 7933: 7932: 7922: 7898: 7892: 7891: 7881: 7856:(17710): 17710. 7841: 7832: 7831: 7821: 7789: 7783: 7782: 7765:(1–2): 125–139. 7756: 7747: 7741: 7740: 7730: 7713:(6): 2343–2360. 7698: 7692: 7691: 7689: 7657: 7651: 7650: 7640: 7607: 7601: 7600: 7572: 7566: 7565: 7555: 7515: 7509: 7508: 7492: 7486: 7485: 7451: 7442: 7433: 7432: 7430: 7398: 7392: 7391: 7379: 7373: 7372: 7347:(8): 1623–1631. 7335: 7329: 7328: 7318: 7286: 7277: 7276: 7266: 7234: 7225: 7224: 7196: 7190: 7189: 7161: 7155: 7154: 7144: 7134: 7102: 7089: 7088: 7060: 7049: 7048: 7020: 7011: 7010: 7000: 6976: 6970: 6969: 6941: 6930: 6929: 6921: 6912: 6911: 6904:Palaeovertebrata 6899: 6872: 6871: 6842: 6836: 6835: 6799: 6788: 6787: 6767: 6761: 6760: 6750: 6741:(5): 1955–1967. 6726: 6720: 6719: 6682: 6676: 6675: 6663: 6657: 6656: 6624: 6615: 6614: 6612: 6575: 6564: 6563: 6561: 6528: 6515: 6514: 6506: 6500: 6499: 6473: 6467: 6466: 6432: 6423: 6396: 6395: 6375: 6369: 6368: 6340: 6334: 6333: 6308:(1–6): 205–256. 6297: 6286: 6285: 6257: 6244: 6243: 6231: 6225: 6224: 6204: 6198: 6197: 6181: 6168: 6167: 6143: 6134: 6133: 6125: 6119: 6118: 6116: 6105: 6070: 6069: 6053: 6047: 6046: 6034: 6028: 6027: 6017: 5993: 5987: 5986: 5974: 5968: 5967: 5951: 5945: 5944: 5934: 5925: 5924: 5914: 5905: 5904: 5888: 5754:The skeleton of 5535:, and the ursid 5505:, anthracothere 5416:, anthracothere 5373:), the feliform 5324:, anthracothere 5224:, anoplotheriid 5186:, amphicynodont 5158:Amphiperatherium 5122:Carpathian Basin 5110:Pseudocricetodon 5041:, lophiomerycid 5028:Pseudocricetodon 5023:Amphiperatherium 5007:Doupov Mountains 4708:water chevrotain 4700:Tragulus kanchil 4607:Restorations of 4447: 4390:metacarpal bones 4386:metatarsal bones 4331:compared to the 4249:caudal vertebrae 4245:lumbar vertebrae 4241:dorsal vertebrae 3956: 3850: 3807:, and a strong " 3763: 3762: 3761: 3758: 3703: 3664:squamosal suture 3393: 3392: 3369: 3368: 3345: 3344: 3321: 3320: 3297: 3296: 3273: 3272: 3223: 3222: 3216: 3215: 3170:Iberomeryx minor 3145: 3144: 3095: 3094: 3088: 3087: 3039: 3038: 3032: 3031: 3025: 3024: 3002:Gelocus communis 2994: 2993: 2970: 2969: 2920: 2919: 2913: 2912: 2889: 2888: 2879: 2878: 2808: 2803: 2796: 2791: 2784: 2779: 2627: 2626: 2586: 2585: 2545: 2544: 2521: 2520: 2475: 2474: 2468: 2467: 2443:Iberomeryx minor 2418: 2417: 2408: 2407: 2385:Gelocus communis 2374: 2373: 2350: 2349: 2283: 2282: 2276: 2275: 2226: 2225: 2219: 2218: 2195: 2194: 2188: 2187: 2173: 2168: 2161: 2156: 2039: 2038: 1991: 1990: 1933: 1932: 1909: 1908: 1863: 1862: 1813: 1812: 1788:Iberomeryx minor 1763: 1762: 1753: 1752: 1730:Gelocus communis 1719: 1718: 1695: 1694: 1645: 1644: 1621: 1620: 1597: 1596: 1590: 1589: 1530: 1509: 1475:Gelocus communis 1351:Bachitherium sp. 1347:Bachitherium sp. 1274:, or within the 1258:Bachitherium sp. 1118: 874:A. andegaviensis 833:Iberomeryx minor 825:as a synonym of 784: 783: 782: 779: 756:Gelocus insignis 728:Richard Lydekker 622: 613: 490: 484: 483: 467:was defined the 431: 429:Gelocus insignis 418: 409: 401: 388: 368: 362: 353: 345: 334: 323: 312: 301: 273: 265: 246: 239: 224: 219: 139: 138: 117: 107: 44: 21: 20: 9218: 9217: 9213: 9212: 9211: 9209: 9208: 9207: 9143: 9142: 9141: 9136: 9128: 9123: 9115: 9110: 9102: 9097: 9089: 9084: 9075: 9074: 9069: 9056: 9048: 9043: 9035: 9030: 9021: 9020: 9015: 9006: 9005: 9000: 8987: 8977: 8976: 8966: 8964: 8955: 8954: 8950: 8940: 8938: 8933: 8932: 8928: 8918: 8916: 8912: 8905: 8899: 8898: 8894: 8884: 8882: 8878: 8871: 8867: 8866: 8862: 8852: 8850: 8837: 8836: 8832: 8801: 8797: 8787: 8785: 8772: 8771: 8767: 8744: 8740: 8708: 8704: 8667: 8663: 8609: 8605: 8573: 8569: 8534: 8527: 8482: 8478: 8423: 8419: 8396:(18): 305–325. 8382: 8378: 8346: 8340: 8336: 8312: 8308: 8279:(11): 514–523. 8269: 8262: 8225: 8214: 8190: 8181: 8136: 8132: 8116:10.1002/gj.3830 8095: 8091: 8078: 8071: 8042: 8038: 8019: 8015: 7984: 7980: 7943: 7936: 7899: 7895: 7842: 7835: 7790: 7786: 7754: 7748: 7744: 7699: 7695: 7658: 7654: 7608: 7604: 7573: 7569: 7516: 7512: 7493: 7489: 7449: 7443: 7436: 7399: 7395: 7380: 7376: 7336: 7332: 7287: 7280: 7235: 7228: 7197: 7193: 7162: 7158: 7103: 7092: 7061: 7052: 7021: 7014: 6977: 6973: 6942: 6933: 6922: 6915: 6900: 6875: 6843: 6839: 6800: 6791: 6768: 6764: 6727: 6723: 6694:(6): e1722682. 6683: 6679: 6664: 6660: 6625: 6618: 6587:(1–4): 97–107. 6576: 6567: 6529: 6518: 6507: 6503: 6496: 6474: 6470: 6430: 6424: 6399: 6376: 6372: 6341: 6337: 6298: 6289: 6258: 6247: 6232: 6228: 6205: 6201: 6182: 6171: 6144: 6137: 6126: 6122: 6114: 6106: 6073: 6054: 6050: 6035: 6031: 5994: 5990: 5975: 5971: 5952: 5948: 5935: 5928: 5915: 5908: 5889: 5885: 5880: 5850:Pseudamphimeryx 5847:, amphimerycid 5828:Patrick MĂ©dĂ©ric 5816: 5730: 5722: 5653:Anthracotherium 5625:Prodremotherium 5547: 5511:Prodremotherium 5418:Anthracotherium 5321:Prodremotherium 5290:Epiaceratherium 5259:Anthracotherium 5256:Restoration of 5250: 5220:, rhinocerotid 5118:Melissodontinae 5094: 5082:Pseudocyonopsis 5072:, rhinocerotid 5066:Anthracotherium 4947: 4939: 4923:climate forcing 4905: 4858:Forstercooperia 4854:paraceratheriid 4791:Neotethys Ocean 4763:Palaeogeography 4756: 4751: 4745: 4736:Archaeotragulus 4601: 4456: 4444: 4436: 4403: 4273: 4229:spinous process 4203:, reaching the 4185: 4008: 4004: 3998: 3994: 3988: 3984: 3978: 3974: 3914: 3910: 3904: 3900: 3894: 3890: 3883: 3879: 3872: 3868: 3839: 3835: 3831: 3827: 3814: 3806: 3802: 3798: 3779: 3775: 3771: 3755: 3754: 3732: 3680: 3676: 3644:postorbital bar 3616:occipital crest 3582: 3543: 3538: 3529: 3520: 3511: 3502: 3493: 3484: 3475: 3466: 3457: 3448: 3439: 3430: 3260: 3200: 3191: 3182: 3132: 3072: 2957: 2830: 2820: 2811: 2810: 2806: 2801: 2798: 2794: 2789: 2786: 2782: 2777: 2771: 2762: 2753: 2744: 2735: 2726: 2717: 2708: 2699: 2690: 2681: 2508: 2455: 2337: 2263: 2185: 2176: 2175: 2171: 2166: 2163: 2159: 2154: 2148: 2139: 2130: 2121: 2112: 2103: 2094: 2085: 2076: 1896: 1850: 1800: 1682: 1555: 1542: 1541: 1540: 1539: 1538: 1535:Christine Janis 1531: 1522: 1521: 1520: 1510: 1499: 1461: 1457: 1445: 1441: 1345:from MP28, and 1304: 1250: 1242: 1238: 1207:and the larger 1182: 1167:is small, the " 1166: 1154: 1130: 1126: 1122: 1116: 1107: 1039: 1031: 1015: 1007: 999: 995: 957: 950: 934: 929:Hypertragulidae 904:as the species 895: 865: 861: 788:Prodremotherium 776: 775: 644: 643: 642: 641: 625: 624: 623: 615: 614: 603: 598: 550:, strong upper 540:Hypertragulidae 509:Christine Janis 436: 425: 424: 414: 395: 394: 373: 357: 356: 283: 280: 269: 245: 237: 223: 217: 133: 108: 106: 105: 100: 95: 90: 85: 80: 75: 70: 65: 60: 55: 50: 39: 38: 27: 17: 12: 11: 5: 9216: 9206: 9205: 9200: 9195: 9190: 9185: 9180: 9175: 9170: 9165: 9160: 9155: 9138: 9137: 9135: 9134: 9121: 9108: 9095: 9082: 9066: 9064: 9058: 9057: 9055: 9054: 9041: 9028: 9023:Bachitheriidae 9013: 8997: 8995: 8993:Bachitheriidae 8989: 8988: 8975: 8974: 8948: 8926: 8892: 8860: 8830: 8795: 8765: 8754:(2): 604–612. 8738: 8702: 8681:(2): 335–347. 8661: 8603: 8567: 8548:(4): 787–814. 8525: 8496:(2): 250–262. 8476: 8417: 8376: 8357:(4): 565–622. 8334: 8323:(4): 734–753. 8306: 8260: 8239:(2): 349–369. 8212: 8179: 8130: 8109:(2): 628–649. 8089: 8069: 8036: 8013: 7994:(3): 199–229. 7978: 7934: 7913:(3): 489–504. 7893: 7833: 7784: 7742: 7693: 7672:(2): 341–362. 7652: 7623:(1): 269–315. 7602: 7583:(2): 179–189. 7567: 7530:(7463): 7463. 7510: 7487: 7460:(2): 161–172. 7434: 7413:(4): 382–396. 7393: 7374: 7330: 7301:(2): 141–242. 7278: 7226: 7207:(4): 231–248. 7191: 7172:(5): 471–473. 7156: 7090: 7071:(7): 527–532. 7050: 7031:(4): 573–591. 7012: 6991:(2): 259–265. 6971: 6952:(3): 197–209. 6931: 6913: 6873: 6837: 6810:(7): 581–600. 6789: 6762: 6721: 6677: 6658: 6616: 6565: 6516: 6501: 6494: 6478:Living Fossils 6468: 6397: 6370: 6351:(1): 116–134. 6335: 6287: 6268:(2): 200–216. 6245: 6226: 6215:(2596): 1–22. 6199: 6169: 6135: 6120: 6071: 6068:(5): 996–1002. 6048: 6029: 5988: 5969: 5946: 5926: 5906: 5882: 5881: 5879: 5876: 5843:"), marsupial 5841:Limognitherium 5815: 5812: 5748:B. cf. insigne 5729: 5723: 5721: 5718: 5546: 5543: 5523:, cainotheres 5447:, palaeothere 5445:Cadurcotherium 5391:Cadurcotherium 5377:, palaeothere 5375:Stenoplesictis 5333:Molassitherium 5292:and ruminants 5249: 5246: 5228:, cainotheres 5216:, palaeothere 5203:Stenoplesictis 5114:Paracricetodon 5093: 5090: 5080:, amphicyonid 5034:Paracricetodon 5015:Czech Republic 4968:rhinocerotoids 4945: 4937: 4904: 4901: 4836:Prominatherium 4787:Paratethys Sea 4755: 4752: 4744: 4741: 4600: 4597: 4530: 4529: 4526: 4523: 4520: 4513: 4512: 4509: 4506: 4503: 4497: 4496: 4493: 4490: 4487: 4481: 4480: 4477: 4474: 4471: 4465: 4464: 4461: 4458: 4454: 4451: 4442: 4434: 4402: 4399: 4272: 4269: 4184: 4181: 4178: 4177: 4174: 4171: 4168: 4165: 4162: 4159: 4156: 4150: 4149: 4146: 4143: 4140: 4137: 4134: 4131: 4128: 4122: 4121: 4118: 4115: 4112: 4109: 4106: 4103: 4100: 4094: 4093: 4090: 4087: 4084: 4081: 4078: 4075: 4072: 4066: 4065: 4062: 4059: 4056: 4053: 4050: 4047: 4044: 4038: 4037: 4034: 4031: 4028: 4025: 4022: 4019: 4016: 4014:B. thraciensis 4010: 4009: 4006: 4002: 3999: 3996: 3992: 3989: 3986: 3982: 3979: 3976: 3972: 3969: 3966: 3965:Type Locality 3963: 3960: 3945: 3944: 3941: 3938: 3935: 3932: 3929: 3926: 3923: 3920: 3916: 3915: 3912: 3908: 3905: 3902: 3898: 3895: 3892: 3888: 3885: 3881: 3877: 3874: 3870: 3866: 3863: 3860: 3857: 3854: 3837: 3833: 3829: 3825: 3812: 3804: 3800: 3796: 3777: 3773: 3769: 3731: 3728: 3725: 3724: 3721: 3718: 3714: 3713: 3710: 3707: 3678: 3674: 3652:occipital face 3648:sagittal crest 3640:lacrimal fossa 3581: 3578: 3542: 3539: 3535: 3534: 3531: 3530: 3526: 3525: 3522: 3521: 3517: 3516: 3513: 3512: 3508: 3507: 3504: 3503: 3499: 3498: 3495: 3494: 3490: 3489: 3486: 3485: 3481: 3480: 3477: 3476: 3472: 3471: 3468: 3467: 3463: 3462: 3459: 3458: 3454: 3453: 3450: 3449: 3445: 3444: 3441: 3440: 3436: 3435: 3432: 3431: 3427: 3426: 3423: 3422: 3413: 3410: 3409: 3406: 3405: 3396: 3391: 3389: 3386: 3385: 3382: 3381: 3372: 3367: 3365: 3362: 3361: 3358: 3357: 3348: 3343: 3341: 3338: 3337: 3334: 3333: 3324: 3319: 3317: 3314: 3313: 3310: 3309: 3300: 3295: 3293: 3290: 3289: 3286: 3285: 3276: 3271: 3269: 3266: 3265: 3262: 3261: 3257: 3256: 3253: 3252: 3243: 3240: 3239: 3236: 3235: 3226: 3221: 3219: 3214: 3212: 3206: 3205: 3202: 3201: 3197: 3196: 3193: 3192: 3188: 3187: 3184: 3183: 3179: 3178: 3175: 3174: 3165: 3162: 3161: 3158: 3157: 3148: 3143: 3141: 3138: 3137: 3134: 3133: 3129: 3128: 3125: 3124: 3115: 3112: 3111: 3108: 3107: 3098: 3093: 3091: 3086: 3084: 3078: 3077: 3074: 3073: 3069: 3068: 3065: 3064: 3057: 3054: 3053: 3050: 3049: 3042: 3037: 3035: 3030: 3028: 3023: 3021: 3011: 3010: 3007: 3006: 2997: 2992: 2990: 2987: 2986: 2983: 2982: 2973: 2968: 2966: 2963: 2962: 2959: 2958: 2954: 2953: 2950: 2949: 2940: 2937: 2936: 2933: 2932: 2923: 2918: 2916: 2911: 2909: 2906: 2905: 2902: 2901: 2892: 2887: 2885: 2877: 2828: 2817: 2816: 2813: 2812: 2799: 2787: 2775: 2774: 2772: 2768: 2767: 2764: 2763: 2759: 2758: 2755: 2754: 2750: 2749: 2746: 2745: 2741: 2740: 2737: 2736: 2732: 2731: 2728: 2727: 2723: 2722: 2719: 2718: 2714: 2713: 2710: 2709: 2705: 2704: 2701: 2700: 2696: 2695: 2692: 2691: 2687: 2686: 2683: 2682: 2678: 2677: 2674: 2673: 2664: 2661: 2660: 2657: 2656: 2647: 2644: 2643: 2640: 2639: 2630: 2625: 2623: 2620: 2619: 2616: 2615: 2606: 2603: 2602: 2599: 2598: 2589: 2584: 2582: 2579: 2578: 2575: 2574: 2565: 2562: 2561: 2558: 2557: 2548: 2543: 2541: 2538: 2537: 2534: 2533: 2524: 2519: 2517: 2514: 2513: 2510: 2509: 2505: 2504: 2501: 2500: 2493: 2490: 2489: 2486: 2485: 2478: 2473: 2471: 2466: 2464: 2461: 2460: 2457: 2456: 2452: 2451: 2448: 2447: 2438: 2435: 2434: 2431: 2430: 2421: 2416: 2414: 2406: 2404: 2394: 2393: 2390: 2389: 2380: 2372: 2370: 2367: 2366: 2363: 2362: 2353: 2348: 2346: 2343: 2342: 2339: 2338: 2334: 2333: 2330: 2329: 2320: 2317: 2316: 2313: 2312: 2303: 2300: 2299: 2296: 2295: 2286: 2281: 2279: 2274: 2272: 2269: 2268: 2265: 2264: 2260: 2259: 2256: 2255: 2246: 2243: 2242: 2239: 2238: 2229: 2224: 2222: 2217: 2215: 2212: 2211: 2208: 2207: 2198: 2193: 2191: 2186: 2182: 2181: 2178: 2177: 2164: 2152: 2151: 2149: 2145: 2144: 2141: 2140: 2136: 2135: 2132: 2131: 2127: 2126: 2123: 2122: 2118: 2117: 2114: 2113: 2109: 2108: 2105: 2104: 2100: 2099: 2096: 2095: 2091: 2090: 2087: 2086: 2082: 2081: 2078: 2077: 2073: 2072: 2069: 2068: 2059: 2056: 2055: 2052: 2051: 2042: 2037: 2035: 2025: 2024: 2021: 2020: 2011: 2008: 2007: 2004: 2003: 1994: 1989: 1987: 1984: 1983: 1980: 1979: 1970: 1967: 1966: 1963: 1962: 1953: 1950: 1949: 1946: 1945: 1936: 1931: 1929: 1926: 1925: 1922: 1921: 1912: 1907: 1905: 1902: 1901: 1898: 1897: 1893: 1892: 1889: 1888: 1881: 1878: 1877: 1874: 1873: 1866: 1861: 1859: 1856: 1855: 1852: 1851: 1847: 1846: 1843: 1842: 1833: 1830: 1829: 1826: 1825: 1816: 1811: 1809: 1806: 1805: 1802: 1801: 1797: 1796: 1793: 1792: 1783: 1780: 1779: 1776: 1775: 1766: 1761: 1759: 1751: 1749: 1739: 1738: 1735: 1734: 1725: 1717: 1715: 1712: 1711: 1708: 1707: 1698: 1693: 1691: 1688: 1687: 1684: 1683: 1679: 1678: 1675: 1674: 1665: 1662: 1661: 1658: 1657: 1648: 1643: 1641: 1638: 1637: 1634: 1633: 1624: 1619: 1617: 1614: 1613: 1610: 1609: 1600: 1595: 1593: 1588: 1563:living fossils 1553: 1532: 1525: 1524: 1523: 1511: 1504: 1503: 1502: 1501: 1500: 1498: 1497:Classification 1495: 1459: 1455: 1443: 1439: 1333:from MP23-27, 1303: 1300: 1248: 1240: 1236: 1180: 1164: 1152: 1128: 1124: 1120: 1119:s caniniform P 1105: 1037: 1029: 1028:losing their P 1013: 1005: 997: 993: 956: 953: 948: 947:and enlarged I 941:Leptomerycidae 932: 893: 863: 859: 752:Gelocus curtus 744:Gelocus curtum 674:dental formula 627: 626: 617: 616: 608: 607: 606: 605: 604: 602: 599: 597: 594: 544:Leptomerycidae 520:B. cf. insigne 505:Bachitheriidae 438: 437: 435: 434: 417: 416: 415: 413: 412: 404: 399:Gelocus curtus 387: 386: 385: 382: 381: 375: 374: 372: 371: 352: 351: 350: 349: 348: 337: 326: 315: 304: 290: 289: 288:Other species 285: 284: 281: 267:Gelocus curtus 260: 259: 253: 252: 235: 231: 230: 221:Bachitheriidae 215: 211: 210: 205: 201: 200: 195: 191: 190: 185: 181: 180: 175: 171: 170: 165: 161: 160: 155: 151: 150: 145: 141: 140: 127: 126: 119: 118: 110: 109: 101: 96: 91: 86: 81: 76: 71: 66: 61: 56: 51: 46: 40:37.71–24  28: 15: 9: 6: 4: 3: 2: 9215: 9204: 9201: 9199: 9196: 9194: 9191: 9189: 9186: 9184: 9181: 9179: 9176: 9174: 9171: 9169: 9166: 9164: 9161: 9159: 9156: 9154: 9151: 9150: 9148: 9131: 9126: 9122: 9118: 9113: 9109: 9105: 9100: 9096: 9092: 9087: 9083: 9078: 9072: 9068: 9067: 9065: 9063: 9059: 9051: 9046: 9042: 9038: 9033: 9029: 9024: 9018: 9014: 9009: 9003: 8999: 8998: 8996: 8994: 8990: 8986: 8981: 8962: 8958: 8952: 8936: 8930: 8915:on 2023-07-24 8911: 8904: 8903: 8896: 8881:on 2023-07-24 8877: 8870: 8864: 8849:on 2022-05-26 8848: 8844: 8840: 8834: 8826: 8822: 8818: 8814: 8810: 8806: 8799: 8783: 8779: 8775: 8769: 8761: 8757: 8753: 8749: 8742: 8734: 8730: 8726: 8722: 8718: 8714: 8706: 8698: 8694: 8689: 8684: 8680: 8676: 8672: 8665: 8657: 8653: 8648: 8643: 8639: 8635: 8631: 8627: 8623: 8619: 8615: 8607: 8599: 8595: 8591: 8587: 8583: 8580:(in French). 8579: 8571: 8563: 8559: 8555: 8551: 8547: 8543: 8542:Geodiversitas 8539: 8532: 8530: 8521: 8517: 8512: 8507: 8503: 8499: 8495: 8491: 8487: 8480: 8472: 8468: 8463: 8458: 8453: 8448: 8444: 8440: 8436: 8432: 8428: 8421: 8413: 8409: 8404: 8399: 8395: 8391: 8390:Geodiversitas 8387: 8380: 8372: 8368: 8364: 8360: 8356: 8352: 8351:Geodiversitas 8345: 8338: 8330: 8326: 8322: 8318: 8310: 8302: 8298: 8294: 8290: 8286: 8282: 8278: 8274: 8267: 8265: 8256: 8252: 8247: 8242: 8238: 8234: 8230: 8223: 8221: 8219: 8217: 8208: 8204: 8200: 8196: 8188: 8186: 8184: 8175: 8171: 8166: 8161: 8157: 8153: 8150:(3): 110302. 8149: 8145: 8141: 8134: 8126: 8122: 8117: 8112: 8108: 8104: 8100: 8093: 8085: 8084: 8076: 8074: 8064: 8059: 8055: 8051: 8047: 8040: 8032: 8028: 8024: 8017: 8009: 8005: 8001: 7997: 7993: 7989: 7982: 7974: 7970: 7965: 7960: 7957:(1–2): 1–16. 7956: 7952: 7948: 7941: 7939: 7930: 7926: 7921: 7916: 7912: 7908: 7904: 7897: 7889: 7885: 7880: 7875: 7871: 7867: 7863: 7859: 7855: 7851: 7847: 7840: 7838: 7829: 7825: 7820: 7815: 7811: 7807: 7803: 7799: 7795: 7788: 7780: 7776: 7772: 7768: 7764: 7760: 7753: 7746: 7738: 7734: 7729: 7724: 7720: 7716: 7712: 7708: 7704: 7697: 7688: 7683: 7679: 7675: 7671: 7667: 7663: 7656: 7648: 7644: 7639: 7634: 7630: 7626: 7622: 7618: 7614: 7606: 7598: 7594: 7590: 7586: 7582: 7578: 7571: 7563: 7559: 7554: 7549: 7545: 7541: 7537: 7533: 7529: 7525: 7521: 7514: 7506: 7502: 7498: 7491: 7483: 7479: 7475: 7471: 7467: 7463: 7459: 7455: 7448: 7441: 7439: 7429: 7424: 7420: 7416: 7412: 7408: 7404: 7397: 7389: 7386:(in German). 7385: 7378: 7370: 7366: 7362: 7358: 7354: 7350: 7346: 7342: 7334: 7326: 7322: 7317: 7312: 7308: 7304: 7300: 7296: 7292: 7285: 7283: 7274: 7270: 7265: 7260: 7256: 7252: 7248: 7244: 7240: 7233: 7231: 7222: 7218: 7214: 7210: 7206: 7202: 7195: 7187: 7183: 7179: 7175: 7171: 7167: 7160: 7152: 7148: 7143: 7138: 7133: 7128: 7124: 7120: 7116: 7112: 7108: 7101: 7099: 7097: 7095: 7086: 7082: 7078: 7074: 7070: 7067:(in French). 7066: 7059: 7057: 7055: 7046: 7042: 7038: 7034: 7030: 7027:(in French). 7026: 7019: 7017: 7008: 7004: 6999: 6994: 6990: 6986: 6982: 6975: 6967: 6963: 6959: 6955: 6951: 6947: 6940: 6938: 6936: 6927: 6920: 6918: 6909: 6906:(in French). 6905: 6898: 6896: 6894: 6892: 6890: 6888: 6886: 6884: 6882: 6880: 6878: 6869: 6865: 6861: 6857: 6853: 6849: 6841: 6833: 6829: 6825: 6821: 6817: 6813: 6809: 6805: 6798: 6796: 6794: 6785: 6781: 6778:(32): 15–31. 6777: 6773: 6766: 6758: 6754: 6749: 6744: 6740: 6736: 6732: 6725: 6717: 6713: 6709: 6705: 6701: 6697: 6693: 6689: 6681: 6673: 6669: 6662: 6654: 6650: 6646: 6642: 6638: 6634: 6630: 6623: 6621: 6611: 6606: 6602: 6598: 6594: 6590: 6586: 6582: 6574: 6572: 6570: 6560: 6555: 6551: 6547: 6543: 6539: 6535: 6527: 6525: 6523: 6521: 6512: 6505: 6497: 6491: 6487: 6483: 6479: 6472: 6464: 6460: 6456: 6452: 6448: 6444: 6440: 6436: 6429: 6422: 6420: 6418: 6416: 6414: 6412: 6410: 6408: 6406: 6404: 6402: 6393: 6389: 6386:(1): 97–104. 6385: 6381: 6374: 6366: 6362: 6358: 6354: 6350: 6346: 6339: 6331: 6327: 6323: 6319: 6315: 6311: 6307: 6304:(in French). 6303: 6296: 6294: 6292: 6283: 6279: 6275: 6271: 6267: 6263: 6256: 6254: 6252: 6250: 6242:(8): 749–754. 6241: 6238:(in French). 6237: 6230: 6222: 6218: 6214: 6210: 6203: 6195: 6192:(in French). 6191: 6187: 6180: 6178: 6176: 6174: 6165: 6161: 6157: 6153: 6149: 6142: 6140: 6131: 6124: 6113: 6112: 6104: 6102: 6100: 6098: 6096: 6094: 6092: 6090: 6088: 6086: 6084: 6082: 6080: 6078: 6076: 6067: 6064:(in French). 6063: 6059: 6052: 6044: 6041:(in German). 6040: 6033: 6025: 6021: 6016: 6011: 6007: 6003: 5999: 5992: 5985:(2): 101–104. 5984: 5981:(in French). 5980: 5973: 5965: 5962:(in German). 5961: 5957: 5950: 5942: 5941: 5933: 5931: 5922: 5921: 5913: 5911: 5902: 5899:(in French). 5898: 5894: 5887: 5883: 5875: 5872: 5867: 5865: 5861: 5860: 5856: 5852: 5851: 5846: 5842: 5838: 5837:Schizotherium 5833: 5829: 5825: 5820: 5811: 5809: 5805: 5801: 5797: 5793: 5789: 5785: 5781: 5777: 5773: 5769: 5765: 5761: 5757: 5749: 5745: 5741: 5739: 5734: 5727: 5717: 5715: 5714: 5709: 5705: 5701: 5697: 5693: 5689: 5686: 5685:Cephalogalini 5682: 5678: 5674: 5670: 5666: 5662: 5658: 5657:Amphitragulus 5654: 5650: 5646: 5642: 5637: 5633: 5628: 5626: 5622: 5618: 5614: 5613: 5609: 5605: 5601: 5600: 5595: 5594: 5589: 5588: 5583: 5579: 5578:Amphitragulus 5575: 5574: 5569: 5564: 5562: 5557: 5552: 5542: 5540: 5539: 5534: 5531:, hyaenodont 5530: 5526: 5522: 5518: 5517: 5516:Amphitragulus 5512: 5508: 5504: 5500: 5496: 5491: 5487: 5483: 5479: 5477: 5473: 5472: 5467: 5466: 5461: 5457: 5452: 5450: 5446: 5442: 5433: 5429: 5427: 5426:Schizotherium 5423: 5419: 5415: 5412:, cainothere 5411: 5410: 5409:Metriotherium 5406:, dichobunid 5405: 5401: 5400: 5399:Schizotherium 5396: 5392: 5388: 5384: 5380: 5376: 5372: 5371:Dinailurictis 5368: 5364: 5363: 5358: 5354: 5350: 5346: 5341: 5339: 5335: 5334: 5329: 5328: 5323: 5322: 5317: 5316: 5311: 5307: 5303: 5299: 5295: 5291: 5285: 5283: 5279: 5275: 5271: 5262: 5260: 5254: 5245: 5243: 5239: 5238: 5233: 5232: 5227: 5223: 5219: 5215: 5211: 5210: 5205: 5204: 5199: 5198: 5193: 5189: 5185: 5184: 5183:Thereutherium 5179: 5175: 5171: 5170: 5165: 5164: 5159: 5155: 5151: 5147: 5142: 5140: 5136: 5132: 5128: 5123: 5119: 5115: 5111: 5107: 5098: 5089: 5087: 5083: 5079: 5075: 5071: 5067: 5063: 5060:, entelodont 5059: 5058: 5054: 5050: 5049: 5045:, cainothere 5044: 5040: 5036: 5035: 5030: 5029: 5024: 5020: 5016: 5012: 5008: 5003: 4999: 4997: 4993: 4989: 4985: 4981: 4977: 4973: 4972:rhinocerotids 4969: 4960: 4959: 4954: 4950: 4948: 4940: 4933: 4929: 4924: 4915: 4914: 4913:Anoplotherium 4909: 4900: 4897: 4896: 4891: 4887: 4883: 4879: 4878: 4873: 4872: 4868: 4864: 4860: 4859: 4855: 4851: 4850: 4845: 4843: 4838: 4837: 4832: 4831: 4826: 4825: 4820: 4812: 4808: 4803: 4799: 4798:as a result. 4796: 4792: 4788: 4784: 4778: 4776: 4772: 4764: 4760: 4750: 4743:Palaeoecology 4740: 4738: 4737: 4732: 4728: 4724: 4723: 4717: 4713: 4709: 4701: 4697: 4692: 4688: 4686: 4682: 4678: 4674: 4670: 4666: 4662: 4658: 4654: 4650: 4646: 4641: 4639: 4635: 4631: 4622: 4618: 4614: 4610: 4605: 4599:Palaeobiology 4596: 4594: 4590: 4586: 4582: 4578: 4574: 4570: 4566: 4562: 4558: 4550: 4546: 4544: 4542: 4538: 4537:anoplotheriid 4527: 4524: 4521: 4518: 4515: 4514: 4510: 4507: 4504: 4502: 4499: 4498: 4494: 4491: 4488: 4486: 4483: 4482: 4478: 4475: 4472: 4470: 4467: 4466: 4448: 4438: 4432: 4428: 4424: 4420: 4416: 4412: 4408: 4398: 4395: 4391: 4387: 4383: 4379: 4378: 4373: 4372: 4367: 4366: 4361: 4357: 4352: 4350: 4346: 4342: 4338: 4334: 4330: 4326: 4322: 4318: 4314: 4310: 4306: 4302: 4298: 4290: 4286: 4282: 4277: 4268: 4266: 4262: 4258: 4254: 4250: 4246: 4242: 4236: 4235:of the head. 4234: 4230: 4226: 4222: 4218: 4214: 4210: 4206: 4205:glenoid fossa 4202: 4198: 4194: 4190: 4175: 4172: 4169: 4166: 4163: 4160: 4157: 4155: 4152: 4151: 4147: 4144: 4141: 4138: 4135: 4132: 4129: 4127: 4124: 4123: 4119: 4116: 4113: 4110: 4107: 4104: 4101: 4099: 4096: 4095: 4091: 4088: 4085: 4082: 4079: 4076: 4073: 4071: 4068: 4067: 4063: 4060: 4057: 4054: 4051: 4048: 4046:UCBL FSL9672 4045: 4043: 4040: 4039: 4035: 4032: 4029: 4026: 4023: 4020: 4018:NMNHS FM3320 4017: 4015: 4012: 4011: 3957: 3953: 3917: 3853:C-P diastema 3851: 3847: 3841: 3822: 3818: 3810: 3793: 3791: 3787: 3783: 3767: 3752: 3745: 3741: 3736: 3715: 3704: 3700: 3694: 3692: 3688: 3684: 3671: 3669: 3665: 3661: 3657: 3653: 3649: 3645: 3641: 3637: 3633: 3629: 3625: 3621: 3617: 3613: 3609: 3605: 3597: 3593: 3592: 3586: 3577: 3575: 3571: 3566: 3564: 3560: 3556: 3552: 3548: 3533: 3532: 3524: 3523: 3515: 3514: 3506: 3505: 3497: 3496: 3488: 3487: 3479: 3478: 3470: 3469: 3461: 3460: 3452: 3451: 3443: 3442: 3434: 3433: 3425: 3424: 3421: 3420: 3419: 3412: 3411: 3408: 3407: 3404: 3403: 3402: 3395: 3394: 3388: 3387: 3384: 3383: 3380: 3379: 3378: 3371: 3370: 3364: 3363: 3360: 3359: 3356: 3355: 3354: 3347: 3346: 3340: 3339: 3336: 3335: 3332: 3331: 3330: 3323: 3322: 3316: 3315: 3312: 3311: 3308: 3307: 3306: 3299: 3298: 3292: 3291: 3288: 3287: 3284: 3283: 3282: 3275: 3274: 3268: 3267: 3264: 3263: 3255: 3254: 3251: 3250: 3249: 3242: 3241: 3238: 3237: 3234: 3233: 3232: 3225: 3224: 3218: 3217: 3211: 3208: 3207: 3204: 3203: 3195: 3194: 3186: 3185: 3177: 3176: 3173: 3172: 3171: 3164: 3163: 3160: 3159: 3156: 3155: 3154: 3147: 3146: 3140: 3139: 3136: 3135: 3127: 3126: 3123: 3122: 3121: 3114: 3113: 3110: 3109: 3106: 3105: 3104: 3097: 3096: 3090: 3089: 3083: 3080: 3079: 3076: 3075: 3067: 3066: 3063: 3062: 3056: 3055: 3052: 3051: 3048: 3047: 3041: 3040: 3034: 3033: 3027: 3026: 3020: 3016: 3013: 3012: 3009: 3008: 3005: 3004: 3003: 2996: 2995: 2989: 2988: 2985: 2984: 2981: 2980: 2979: 2972: 2971: 2965: 2964: 2961: 2960: 2952: 2951: 2948: 2947: 2946: 2939: 2938: 2935: 2934: 2931: 2930: 2929: 2922: 2921: 2915: 2914: 2908: 2907: 2904: 2903: 2900: 2899: 2898: 2891: 2890: 2884: 2881: 2880: 2876: 2873: 2869: 2868: 2863: 2861: 2856: 2854: 2849: 2848: 2841: 2838: 2834: 2826: 2815: 2814: 2809: 2804: 2797: 2792: 2785: 2780: 2766: 2765: 2757: 2756: 2748: 2747: 2739: 2738: 2730: 2729: 2721: 2720: 2712: 2711: 2703: 2702: 2694: 2693: 2685: 2684: 2676: 2675: 2672: 2671: 2670: 2663: 2662: 2659: 2658: 2655: 2654: 2653: 2646: 2645: 2642: 2641: 2638: 2637: 2636: 2629: 2628: 2622: 2621: 2618: 2617: 2614: 2613: 2612: 2605: 2604: 2601: 2600: 2597: 2596: 2595: 2588: 2587: 2581: 2580: 2577: 2576: 2573: 2572: 2571: 2564: 2563: 2560: 2559: 2556: 2555: 2554: 2547: 2546: 2540: 2539: 2536: 2535: 2532: 2531: 2530: 2523: 2522: 2516: 2515: 2512: 2511: 2503: 2502: 2499: 2498: 2492: 2491: 2488: 2487: 2484: 2483: 2477: 2476: 2470: 2469: 2463: 2462: 2459: 2458: 2450: 2449: 2446: 2445: 2444: 2437: 2436: 2433: 2432: 2429: 2428: 2427: 2420: 2419: 2413: 2410: 2409: 2403: 2399: 2396: 2395: 2392: 2391: 2388: 2387: 2386: 2379: 2376: 2375: 2369: 2368: 2365: 2364: 2361: 2360: 2359: 2352: 2351: 2345: 2344: 2341: 2340: 2332: 2331: 2328: 2327: 2326: 2319: 2318: 2315: 2314: 2311: 2310: 2309: 2302: 2301: 2298: 2297: 2294: 2293: 2292: 2285: 2284: 2278: 2277: 2271: 2270: 2267: 2266: 2258: 2257: 2254: 2253: 2252: 2245: 2244: 2241: 2240: 2237: 2236: 2235: 2228: 2227: 2221: 2220: 2214: 2213: 2210: 2209: 2206: 2205: 2204: 2197: 2196: 2190: 2189: 2180: 2179: 2174: 2169: 2162: 2157: 2143: 2142: 2134: 2133: 2125: 2124: 2116: 2115: 2107: 2106: 2098: 2097: 2089: 2088: 2080: 2079: 2071: 2070: 2067: 2066: 2065: 2058: 2057: 2054: 2053: 2050: 2049: 2048: 2041: 2040: 2034: 2030: 2027: 2026: 2023: 2022: 2019: 2018: 2017: 2010: 2009: 2006: 2005: 2002: 2001: 2000: 1993: 1992: 1986: 1985: 1982: 1981: 1978: 1977: 1976: 1969: 1968: 1965: 1964: 1961: 1960: 1959: 1952: 1951: 1948: 1947: 1944: 1943: 1942: 1935: 1934: 1928: 1927: 1924: 1923: 1920: 1919: 1918: 1911: 1910: 1904: 1903: 1900: 1899: 1891: 1890: 1887: 1886: 1880: 1879: 1876: 1875: 1872: 1871: 1865: 1864: 1858: 1857: 1854: 1853: 1845: 1844: 1841: 1840: 1839: 1832: 1831: 1828: 1827: 1824: 1823: 1822: 1815: 1814: 1808: 1807: 1804: 1803: 1795: 1794: 1791: 1790: 1789: 1782: 1781: 1778: 1777: 1774: 1773: 1772: 1765: 1764: 1758: 1755: 1754: 1748: 1744: 1741: 1740: 1737: 1736: 1733: 1732: 1731: 1724: 1721: 1720: 1714: 1713: 1710: 1709: 1706: 1705: 1704: 1697: 1696: 1690: 1689: 1686: 1685: 1677: 1676: 1673: 1672: 1671: 1664: 1663: 1660: 1659: 1656: 1655: 1654: 1647: 1646: 1640: 1639: 1636: 1635: 1632: 1631: 1630: 1623: 1622: 1616: 1615: 1612: 1611: 1608: 1607: 1606: 1599: 1598: 1592: 1591: 1587: 1583: 1579: 1576: 1572: 1568: 1564: 1559: 1551: 1546: 1536: 1529: 1519: 1518:Bachitherium. 1515: 1508: 1494: 1492: 1488: 1484: 1480: 1476: 1472: 1468: 1463: 1453: 1449: 1437: 1433: 1428: 1424: 1419: 1415: 1411: 1407: 1403: 1398: 1396: 1395: 1390: 1386: 1382: 1381: 1376: 1372: 1368: 1364: 1359: 1357: 1352: 1348: 1344: 1340: 1336: 1332: 1328: 1324: 1316: 1312: 1308: 1299: 1297: 1296: 1291: 1290: 1285: 1281: 1280:Bachitherium? 1277: 1273: 1269: 1265: 1260: 1259: 1255: 1246: 1234: 1230: 1226: 1222: 1218: 1214: 1210: 1206: 1201: 1196: 1194: 1190: 1186: 1178: 1174: 1170: 1162: 1158: 1150: 1149: 1144: 1140: 1138: 1134: 1115: 1111: 1103: 1099: 1095: 1088: 1084: 1080: 1076: 1074: 1070: 1066: 1062: 1058: 1054: 1050: 1046: 1041: 1035: 1027: 1026: 1021: 1020: 1011: 1003: 991: 987: 982: 978: 974: 970: 966: 962: 952: 946: 945:temporal bone 942: 938: 930: 926: 922: 918: 914: 909: 907: 903: 899: 891: 887: 883: 879: 875: 871: 870: 858:on both the P 857: 853: 849: 845: 841: 836: 834: 830: 829: 824: 820: 816: 812: 810: 805: 801: 800:Max Schlosser 796: 794: 790: 789: 773: 769: 765: 761: 757: 753: 749: 745: 741: 737: 733: 729: 726: 721: 719: 715: 711: 707: 703: 699: 695: 691: 687: 683: 679: 675: 671: 670: 665: 661: 657: 653: 649: 639: 635: 631: 621: 612: 601:Early history 593: 590: 586: 584: 580: 576: 572: 568: 563: 561: 557: 553: 549: 545: 541: 537: 533: 529: 525: 521: 517: 512: 510: 506: 502: 498: 494: 489: 478: 474: 470: 466: 462: 458: 454: 450: 446: 445: 430: 427: 426: 422: 408: 405: 400: 397: 396: 392: 383: 380: 376: 367: 366: 359: 358: 344: 343: 338: 333: 332: 327: 322: 321: 316: 311: 310: 305: 302:Filhol, 1877 300: 299: 294: 293: 291: 286: 278: 277: 268: 261: 258: 254: 249: 244: 243: 236: 233: 232: 227: 222: 216: 213: 212: 209: 206: 203: 202: 199: 196: 193: 192: 189: 186: 183: 182: 179: 176: 173: 172: 169: 166: 163: 162: 159: 156: 153: 152: 149: 146: 143: 142: 137: 132: 128: 124: 120: 116: 111: 104: 99: 94: 89: 84: 79: 74: 69: 64: 59: 54: 49: 43: 36: 32: 26: 22: 19: 9062:Bachitherium 9061: 8992: 8965:. Retrieved 8960: 8951: 8939:. Retrieved 8929: 8917:. Retrieved 8910:the original 8901: 8895: 8883:. Retrieved 8876:the original 8863: 8851:. Retrieved 8847:the original 8842: 8833: 8808: 8804: 8798: 8786:. Retrieved 8782:the original 8777: 8768: 8751: 8747: 8741: 8716: 8712: 8705: 8678: 8674: 8664: 8624:(1): 36169. 8621: 8617: 8606: 8581: 8577: 8570: 8545: 8541: 8493: 8489: 8479: 8434: 8430: 8420: 8393: 8389: 8379: 8354: 8350: 8337: 8320: 8316: 8309: 8276: 8272: 8236: 8232: 8198: 8194: 8147: 8143: 8133: 8106: 8102: 8092: 8082: 8063:10.26879/883 8053: 8049: 8039: 8030: 8026: 8016: 7991: 7987: 7981: 7954: 7950: 7910: 7906: 7896: 7853: 7849: 7801: 7797: 7787: 7762: 7758: 7745: 7710: 7706: 7696: 7669: 7665: 7655: 7620: 7616: 7605: 7580: 7576: 7570: 7527: 7523: 7513: 7504: 7500: 7490: 7457: 7453: 7410: 7406: 7396: 7387: 7383: 7377: 7344: 7340: 7333: 7298: 7294: 7246: 7242: 7204: 7200: 7194: 7169: 7165: 7159: 7114: 7110: 7068: 7064: 7028: 7024: 6988: 6984: 6974: 6949: 6945: 6925: 6907: 6903: 6851: 6847: 6840: 6807: 6803: 6775: 6771: 6765: 6738: 6734: 6724: 6691: 6687: 6680: 6671: 6661: 6636: 6632: 6584: 6580: 6541: 6537: 6510: 6504: 6477: 6471: 6438: 6434: 6383: 6379: 6373: 6348: 6344: 6338: 6305: 6301: 6265: 6261: 6239: 6235: 6229: 6212: 6202: 6193: 6189: 6155: 6151: 6129: 6123: 6110: 6065: 6061: 6051: 6042: 6038: 6032: 6005: 6001: 5991: 5982: 5978: 5972: 5963: 5959: 5949: 5939: 5919: 5900: 5896: 5886: 5871:Bachitherium 5870: 5868: 5863: 5857: 5848: 5844: 5840: 5836: 5831: 5819:Bachitherium 5818: 5817: 5808:Bachitherium 5807: 5788:Bachitherium 5787: 5780:hummingbirds 5771: 5755: 5753: 5747: 5738:Diplocynodon 5736: 5725: 5711: 5708:Dorcatherium 5707: 5703: 5700:Bachitherium 5699: 5692:hemicyonines 5679:died out by 5676: 5672: 5668: 5664: 5660: 5656: 5652: 5649:Microbunodon 5648: 5644: 5641:Ronzotherium 5640: 5636:Bachitherium 5635: 5631: 5629: 5624: 5620: 5617:Bachitherium 5616: 5610: 5603: 5597: 5591: 5587:Dremotherium 5585: 5581: 5577: 5573:Microbunodon 5571: 5565: 5560: 5556:Bachitherium 5555: 5550: 5548: 5536: 5532: 5528: 5524: 5520: 5514: 5510: 5506: 5502: 5498: 5494: 5489: 5485: 5481: 5480: 5469: 5463: 5459: 5455: 5453: 5449:Plagiolophus 5448: 5444: 5443:, amynodont 5440: 5438: 5425: 5421: 5417: 5413: 5407: 5404:Doliochoerus 5403: 5397: 5395:chalicothere 5390: 5386: 5383:Ronzotherium 5382: 5379:Plagiolophus 5378: 5374: 5370: 5366: 5360: 5356: 5352: 5348: 5345:Bachitherium 5344: 5342: 5337: 5331: 5325: 5319: 5315:Mosaicomeryx 5313: 5305: 5302:Bachitherium 5301: 5297: 5293: 5289: 5286: 5266: 5257: 5241: 5235: 5229: 5225: 5222:Ronzotherium 5221: 5218:Plagiolophus 5217: 5213: 5212:), nimravid 5207: 5201: 5195: 5190:, enigmatic 5188:Amphicynodon 5187: 5181: 5177: 5167: 5166:, erinaceid 5161: 5157: 5153: 5149: 5143: 5139:Bachitherium 5138: 5130: 5127:Bachitherium 5126: 5113: 5109: 5106:Bachitherium 5105: 5103: 5085: 5081: 5077: 5074:Ronzotherium 5073: 5069: 5065: 5061: 5057:Doliochoerus 5055: 5046: 5042: 5038: 5032: 5026: 5022: 5019:Bachitherium 5018: 5004: 5000: 4964: 4958:Ronzotherium 4956: 4919: 4911: 4893: 4875: 4869: 4863:Prohyracodon 4862: 4856: 4847: 4842:Sivatitanops 4840: 4834: 4828: 4824:Plagiolophus 4822: 4818: 4816: 4810: 4806: 4779: 4768: 4734: 4726: 4720: 4711: 4705: 4699: 4681:Bachitherium 4680: 4676: 4668: 4664: 4660: 4652: 4644: 4642: 4637: 4634:Bachitherium 4633: 4630:Bachitherium 4629: 4626: 4620: 4616: 4612: 4608: 4592: 4588: 4584: 4580: 4576: 4572: 4568: 4564: 4560: 4556: 4555: 4539: 4533: 4517:Bachitherium 4516: 4500: 4484: 4468: 4430: 4426: 4422: 4418: 4414: 4411:Bachitherium 4410: 4406: 4404: 4382:Bachitherium 4381: 4375: 4369: 4363: 4360:Bachitherium 4359: 4353: 4345:femoral head 4294: 4289:Bachitherium 4288: 4284: 4259:. The first 4237: 4225:neural canal 4193:Bachitherium 4192: 4186: 4153: 4125: 4102:MNHN Qu3917 4097: 4074:MNHN QU4258 4069: 4041: 4024:Late Eocene 4013: 3952:Bachitherium 3951: 3845: 3821:Dorcatherium 3820: 3816: 3809:Dorcatherium 3808: 3794: 3790:Bachitherium 3789: 3751:Bachitherium 3750: 3749: 3743: 3739: 3698: 3672: 3656:nuchal lines 3620:ethmoid bone 3604:Bachitherium 3603: 3601: 3589: 3588:Skeleton of 3573: 3569: 3567: 3563:Bachitherium 3562: 3554: 3551:Bachitherium 3550: 3547:Bachitherium 3546: 3544: 3416: 3415: 3399: 3398: 3375: 3374: 3351: 3350: 3327: 3326: 3303: 3302: 3279: 3278: 3246: 3245: 3229: 3228: 3168: 3167: 3151: 3150: 3118: 3117: 3101: 3100: 3060: 3059: 3045: 3044: 3000: 2999: 2976: 2975: 2943: 2942: 2926: 2925: 2895: 2894: 2871: 2865: 2860:Merycoidodon 2858: 2851: 2845: 2842: 2837:Bachitherium 2836: 2825:Bachitherium 2824: 2821: 2667: 2666: 2650: 2649: 2633: 2632: 2609: 2608: 2592: 2591: 2568: 2567: 2551: 2550: 2527: 2526: 2496: 2495: 2481: 2480: 2441: 2440: 2424: 2423: 2383: 2382: 2356: 2355: 2323: 2322: 2306: 2305: 2289: 2288: 2249: 2248: 2232: 2231: 2201: 2200: 2062: 2061: 2045: 2044: 2014: 2013: 1997: 1996: 1973: 1972: 1956: 1955: 1939: 1938: 1915: 1914: 1884: 1883: 1869: 1868: 1836: 1835: 1819: 1818: 1786: 1785: 1769: 1768: 1728: 1727: 1701: 1700: 1668: 1667: 1651: 1650: 1627: 1626: 1603: 1602: 1584: 1580: 1575:Bachitherium 1574: 1571:Balkanatolia 1567:Bachitherium 1566: 1558:Dorcatherium 1557: 1545:Bachitherium 1544: 1543: 1517: 1514:Henri Filhol 1512:Portrait of 1491:Bachitherium 1490: 1483:Bachitherium 1482: 1478: 1474: 1470: 1464: 1452:Bachitherium 1451: 1435: 1402:Thrace Basin 1399: 1392: 1378: 1367:Bachitherium 1366: 1362: 1360: 1356:Bachitherium 1355: 1350: 1346: 1342: 1338: 1334: 1330: 1326: 1323:Bachitherium 1322: 1320: 1310: 1293: 1287: 1283: 1279: 1261: 1257: 1253: 1244: 1233:Bachitherium 1232: 1228: 1224: 1220: 1213:Bachitherium 1212: 1208: 1204: 1200:Bachitherium 1199: 1197: 1177:Bachitherium 1176: 1169:Dorcatherium 1168: 1161:Bachitherium 1160: 1156: 1148:Dorcatherium 1146: 1143:Bachitherium 1142: 1141: 1137:Bachitherium 1136: 1114:Bachitherium 1113: 1110:Bachitherium 1109: 1102:Bachitherium 1101: 1098:Bachitherium 1097: 1091: 1082: 1072: 1068: 1064: 1060: 1056: 1049:Bachitherium 1048: 1045:Bachitherium 1044: 1042: 1034:Bachitherium 1033: 1023: 1017: 1002:autapomorphy 990:Bachitherium 989: 981:Bachitherium 980: 976: 973:Bachitherium 972: 961:Bachitherium 960: 958: 925:RenĂ© Lavocat 917:Bachitherium 916: 912: 910: 905: 901: 889: 886:Bachitherium 885: 881: 877: 873: 867: 847: 843: 840:Bachitherium 839: 837: 832: 826: 822: 818: 814: 807: 803: 797: 792: 786: 772:Bachitherium 771: 767: 764:Bachitherium 763: 760:Bachitherium 759: 755: 751: 747: 743: 739: 732:Bachitherium 731: 722: 717: 713: 709: 705: 698:Bachitherium 697: 685: 681: 667: 648:Henri Filhol 645: 637: 629: 628:Sketch of a 589:Bachitherium 588: 587: 582: 578: 570: 566: 564: 558:, and other 528:Bachitherium 527: 519: 516:Bachitherium 515: 513: 504: 493:Bachitherium 492: 476: 472: 469:type species 464: 455:to the late 444:Bachitherium 443: 442: 441: 432:Filhol, 1877 428: 420: 419:Synonyms of 410:Filhol, 1882 406: 402:Filhol, 1877 398: 390: 389:Synonyms of 364: 363: 341: 340: 335:Sudre, 1995 330: 329: 324:Sudre, 1986 319: 318: 313:Sudre, 1986 308: 307: 297: 296: 282:Filhol, 1877 275: 274: 266: 257:Type species 242:Bachitherium 241: 240: 220: 204:Infraorder: 188:Artiodactyla 122: 25:Bachitherium 24: 18: 9017:Wikispecies 8811:(2): 1–13. 8584:(1): 1–45. 8201:(2): 1–24. 8056:(3): 1–12. 7117:(2): 1–28. 6910:(2): 43–73. 6196:(2): 75–78. 6008:: 115–132. 5859:Palaeotodus 5845:Peratherium 5764:LagerstĂ€tte 5704:Lophiomeryx 5696:Hemicyonini 5632:Lophiomeryx 5621:Lophiomeryx 5599:Phoberogale 5561:B. lavocati 5551:B. lavocati 5525:Plesiomeryx 5509:, pecorans 5503:Lophiomeryx 5499:B. lavocati 5495:B. lavocati 5490:B. lavocati 5424:. Notably, 5422:Lophiomeryx 5362:Quercylurus 5336:. Notably, 5306:Lophiomeryx 5274:broadleaved 5231:Plesiomeryx 5078:Cephalogale 5043:Lophiomeryx 5037:), gelocid 5025:, rodents ( 4976:eggysodonts 4895:Peratherium 4890:Erinaceidae 4783:archipelago 4775:condylarths 4702:) foraging. 4677:B. lavocati 4611:(left) and 4569:B. lavocati 4565:B. lavocati 4557:B. lavocati 4158:UM PDS1330 4154:B. lavocati 3744:B. lavocati 3689:similar to 3638:bones. The 3541:Description 2862:culbertsoni 1533:Picture of 1408:as well as 1371:Pleistocene 1343:B. lavocati 1341:from MP25, 1276:Burdigalian 1270:(the early 1159:. However, 1157:Lophiomeryx 1065:B. lavocati 902:Andegameryx 872:, of which 869:Andegameryx 823:Cryptomeryx 809:Lophiomeryx 804:Cryptomeryx 652:artiodactyl 579:B. lavocati 9147:Categories 8961:La DĂ©pĂȘche 8033:(1): 1–11. 7804:: 111363. 7507:: 275–282. 6610:2445/34510 6544:: 103929. 5903:: 138–139. 5878:References 5784:passerines 5742:skeleton, 5728:exhibition 5604:Cyonarctos 5545:Extinction 5538:Cyonarctos 5529:Caenomeryx 5471:Brachycyon 5460:B. insigne 5414:Caenomeryx 5298:Iberomeryx 5278:mesophytic 5270:needleleaf 5242:Iberomeryx 5237:Caenomeryx 5209:Palaeogale 5163:Darbonetus 5131:Iberomeryx 5048:Paroxacron 4992:Nimravidae 4984:Castoridae 4932:ice sheets 4886:Cricetidae 4877:Cadurcodon 4867:amynodonts 4865:, and the 4673:folivorous 4669:B. insigne 4661:B. insigne 4617:B. insigne 4613:B. insigne 4593:B. insigne 4581:B. insigne 4577:B. insigne 4423:B. insigne 4337:trochanter 4307:curve nor 4265:sternebrae 4257:acetabulum 4130:UM GAR441 4070:B. insigne 3971:Diastema P 3817:Iberomeryx 3782:cheekbones 3612:premaxilla 3574:B. insigne 3082:Tragulidae 3019:Ruminantia 2883:Ruminantia 2867:Stenomeryx 2823:lineages. 2783:Ruminantia 2412:Tragulidae 2402:Ruminantia 2160:Ruminantia 1757:Tragulidae 1747:Ruminantia 1423:Priabonian 1331:B. insigne 1295:Hyemoschus 1209:B. insigne 1185:astragalus 1019:Leptomeryx 878:B. insigne 848:B. insigne 828:Iberomeryx 793:B. insigne 736:Tragulidae 725:naturalist 714:B. insigne 706:B. insigne 571:B. insigne 536:Tragulidae 473:B. insigne 421:B. insigne 198:Ruminantia 194:Suborder: 9153:Tragulina 9008:Q21290936 8825:243764500 8733:254625390 8697:132558321 8562:131561629 8412:220714559 8301:134345822 8255:128585686 8174:233968947 8125:216198894 7973:224860287 7828:254801829 7737:244097729 7647:234099337 7597:129158241 7482:140576090 7369:248164842 6868:245480633 6757:208647044 6716:216324257 6674:: 69–145. 6463:134845249 6330:247399047 6221:2246/5473 6164:2246/1042 6045:: 71–166. 5864:Vaylatsia 5713:Dorcabune 5673:Eggysodon 5669:Hyaenodon 5665:Babameryx 5612:Amphictis 5593:Babameryx 5533:Hyaenodon 5486:B insigne 5482:B. curtum 5456:B. curtum 5441:Entelodon 5387:Eggysodon 5349:B. curtum 5347:, namely 5338:B. curtum 5310:speciated 5282:evergreen 5226:Diplobune 5197:Stenogale 5192:feliforms 5178:Hyaenodon 5154:B. vireti 5150:B. curtum 5086:Hyaenodon 5062:Entelodon 4830:Bakalovia 4811:Hyaenodon 4807:Hyaenodon 4795:Holarctic 4722:Moschiola 4685:cursorial 4665:B. curtum 4653:B. curtum 4645:B. curtum 4621:B. curtum 4615:(right). 4609:B. curtum 4585:B. curtum 4573:B. curtum 4561:B. curtum 4541:Diplobune 4519:nov. sp. 4419:B. curtum 4415:B. vireti 4413:species, 4401:Body mass 4394:phalanges 4377:Hyelaphus 4371:Muntiacus 4356:forelimbs 4349:calcaneus 4325:diaphysis 4321:olecranon 4213:processes 4098:B. curtum 4042:B. vireti 3962:Holotype 3884:diastema 3873:diastema 3766:occlusion 3730:Dentition 3628:maxillary 3570:B. curtum 3545:Although 2847:Nalameryx 2378:Gelocidae 1723:Gelocidae 1556:teeth, a 1550:trochleas 1427:Bartonian 1418:Paleogene 1380:Myotragus 1363:B. sardus 1337:in MP23, 1335:B. vireti 1327:B. curtum 1225:B. curtum 1205:B. curtum 1193:Tragulina 1189:monotypic 1073:B. curtum 1069:B. curtum 1061:B. vireti 1057:B. curtum 965:Oligocene 921:Gelocidae 856:metaconid 852:entoconid 710:B. medium 678:premolars 664:Moschidae 583:B. curtum 567:B. curtum 511:in 1987. 501:monotypic 497:Tragulina 477:B. sardus 457:Oligocene 449:Paleogene 391:B. curtum 208:Tragulina 154:Kingdom: 148:Eukaryota 35:Oligocene 9077:Q3632528 9071:Wikidata 9002:Wikidata 8967:July 24, 8941:July 24, 8919:July 24, 8885:July 24, 8853:July 24, 8788:July 24, 8656:27897168 8520:32255213 8471:32989142 8371:85908676 8008:86827900 7929:67817430 7888:34489502 7562:25501388 7390:: 61–79. 7325:84066785 7273:26041349 7249:(1809). 7221:85647031 7151:25692298 7111:PLOS ONE 7007:54686160 6832:56365084 6024:73655017 5792:Pichovet 5716:by MN4. 5677:Elomeryx 5606:and the 5476:savannah 5402:, suoid 5367:Nimravus 5214:Nimravus 5169:Tetracus 5076:, ursid 5070:Elomeryx 4980:Eomyidae 4871:Amynodon 4771:Primates 4731:Thailand 4727:Tragulus 4716:riparian 4450:Species 4329:hip bone 4201:acromion 3959:Species 3691:camelids 3668:foramina 3636:lacrimal 2855:weigelti 1487:cingulum 1481:and not 1410:Bulgaria 1375:Holocene 1289:Tragulus 1264:Sardinia 1173:cingulum 1053:Stampian 1010:diastema 937:premolar 906:A. serum 890:B. serum 882:B. serum 844:B. serum 718:B. minus 690:incisors 596:Taxonomy 556:premolar 379:Synonyms 214:Family: 178:Mammalia 168:Chordata 164:Phylum: 158:Animalia 144:Domain: 33:to Late 9117:3615965 9104:1195021 9091:4835226 9037:8639107 8647:5126638 8626:Bibcode 8586:Bibcode 8511:7369187 8462:7568263 8439:Bibcode 8281:Bibcode 8273:PALAIOS 8152:Bibcode 7879:8421421 7858:Bibcode 7806:Bibcode 7767:Bibcode 7715:Bibcode 7674:Bibcode 7625:Bibcode 7553:4264005 7532:Bibcode 7462:Bibcode 7415:Bibcode 7349:Bibcode 7303:Bibcode 7264:4590438 7174:Bibcode 7142:4334963 7119:Bibcode 7073:Bibcode 7033:Bibcode 7025:Geobios 6954:Bibcode 6946:Lethaia 6812:Bibcode 6696:Bibcode 6641:Bibcode 6589:Bibcode 6546:Bibcode 6443:Bibcode 6441:: 1–8. 6353:Bibcode 6310:Bibcode 6270:Bibcode 5776:trogons 5760:Luberon 5740:ratelii 5694:of the 5661:quercyi 5608:ailurid 5582:quercyi 5521:quercyi 5465:Cynelos 5294:Gelocus 5135:Georgia 5039:Gelocus 5013:in the 5011:Bohemia 4996:Ursidae 4882:Muridae 4649:duikers 4365:Moschus 4339:of the 4305:triceps 4297:humerus 4233:muscles 4197:scapula 4191:of the 3760:3.1.4.3 3757:0.1.3.3 3683:condyle 3660:mastoid 3632:frontal 3594:at the 3559:sutures 1479:Gelocus 1385:Corsica 1272:Miocene 1247:. Its P 1040:tooth. 969:Cereste 913:Gelocus 898:lingual 811:gaudryi 781:3.1.3.3 778:?.?.3.3 768:Gelocus 754:" and " 746:" and " 730:placed 686:Gelocus 682:Gelocus 669:Gelocus 548:incisor 524:CĂ©reste 503:family 488:therium 234:Genus: 184:Order: 174:Class: 9050:184981 8823:  8731:  8695:  8654:  8644:  8560:  8518:  8508:  8469:  8459:  8410:  8369:  8299:  8253:  8172:  8123:  8006:  7971:  7927:  7886:  7876:  7826:  7735:  7645:  7595:  7560:  7550:  7501:STRATA 7480:  7367:  7323:  7271:  7261:  7219:  7149:  7139:  7005:  6866:  6830:  6755:  6714:  6492:  6461:  6328:  6022:  5782:, and 5667:, and 5623:, and 5590:, and 5355:, and 5261:magnum 4880:. The 4852:, the 4667:since 4425:, and 4347:. The 4317:radius 4253:sacrum 4251:. The 4221:joints 4207:. The 3634:, and 3568:Since 3210:Pecora 3017:  2807:Pecora 2795:Pecora 2400:  2172:Pecora 2033:Pecora 2031:  1745:  1448:Sladun 1414:Greece 1406:Turkey 1377:bovid 1133:Pecora 986:molars 842:named 694:canine 660:Eocene 656:Quercy 552:canine 542:, and 532:Pecora 453:Eocene 250:, 1882 248:Filhol 228:, 1987 31:Eocene 9130:42605 9099:IRMNG 8913:(PDF) 8906:(PDF) 8879:(PDF) 8872:(PDF) 8821:S2CID 8729:S2CID 8693:S2CID 8558:S2CID 8408:S2CID 8367:S2CID 8347:(PDF) 8297:S2CID 8251:S2CID 8170:S2CID 8121:S2CID 8004:S2CID 7969:S2CID 7925:S2CID 7824:S2CID 7755:(PDF) 7733:S2CID 7643:S2CID 7593:S2CID 7478:S2CID 7450:(PDF) 7365:S2CID 7321:S2CID 7217:S2CID 7003:S2CID 6864:S2CID 6828:S2CID 6753:S2CID 6712:S2CID 6459:S2CID 6431:(PDF) 6326:S2CID 6158:(3). 6115:(PDF) 6020:S2CID 5768:ranid 5688:tribe 5513:and " 5053:suoid 4543:minor 4445:area 4341:femur 4333:ilium 4271:Limbs 4209:atlas 3803:and P 3685:in a 3624:nasal 3608:orbit 3580:Skull 3015:Crown 2802:Crown 2398:Crown 2029:Crown 1743:Crown 1117:' 880:and " 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Index

Eocene
Oligocene
Ma
PreꞒ
Ꞓ
O
S
D
C
P
T
J
K
Pg
N

Scientific classification
Edit this classification
Eukaryota
Animalia
Chordata
Mammalia
Artiodactyla
Ruminantia
Tragulina
Bachitheriidae
Janis
Bachitherium
Filhol
Type species

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