View source for Amphicyon

{{Short description|Extinct genus of carnivores}}
{{Automatic taxobox
| fossil_range = Early Miocene to Late Miocene ~{{fossilrange|23|7}}
| image = Amphicyon AMNH.jpg
| image_upright = 1.15
| image_caption = ''Amphicyon ingens'' reconstructed skeleton, [[American Museum of Natural History]]
| taxon = Amphicyon
| authority = [[Édouard Lartet|Lartet]], 1836
| type_species = {{extinct}}'''''Amphicyon major'''''
| type_species_authority = Blainville, 1841
| subdivision_ranks = Other species
| subdivision = {{species list
|{{extinct}}'''''A. giganteus?'''''|Schinz, 1825
|{{extinct}}'''''A. palaeindicus?'''''|Lydekker, 1876
|{{extinct}}'''''A. gutmanni'''''|Kittl, 1891
|{{extinct}}'''''A. lydekkeri?'''''|Pilgrim, 1910
|{{extinct}}'''''A. shahbazi'''''|Pilgrim, 1912
|{{extinct}}'''''A. frendens'''''|Matthew, 1924
|{{extinct}}'''''A. ingens'''''|Matthew, 1924
|{{extinct}}'''''A. reinheimeri?'''''|Cook, 1926
|{{extinct}}'''''A. lactorensis'''''|Astre, 1928
|{{extinct}}'''''A. eppelsheimensis'''''|Weitzel, 1930
|{{extinct}}'''''A. pontoni?'''''|Simpson, 1930
|{{extinct}}'''''A. cooperi'''''|Pilgrim, 1932
|{{extinct}}'''''A. pithecophilus'''''|Pilgrim, 1932
|{{extinct}}'''''A. sindiensis'''''|Pilgrim, 1932
|{{extinct}}'''''A. confucianus?'''''|Young, 1937
|{{extinct}}'''''A. riggsi?'''''|McGrew, 1939
|{{extinct}}'''''A. tairumensis?'''''|Colbert, 1939
|{{extinct}}'''''A. longiramus'''''|White, 1942
|{{extinct}}'''''A. astrei'''''|Kuss, 1962
|{{extinct}}'''''A. olisiponensis?'''''|Antunes & Ginsburg, 1977
|{{extinct}}'''''A. pannonicus'''''|Kretzoi, 1985
|{{extinct}}'''''A. laugnacensis'''''|Ginsburg, 1989
|{{extinct}}'''''A. ulungurensis'''''|Qi, 1989
|{{extinct}}'''''A. lathanicus'''''|Ginsburg, 2000
|{{extinct}}'''''A. galushai'''''|Hunt, 2003
|{{extinct}}'''''A. zhanxiangi'''''|Jiangzuo et al, 2019
}}
| synonyms = * '''''Arctamphicyon?''''' <small>Pilgrim, 1932</small>
* '''''Megamphicyon?''''' <small>Kuss, 1965</small>
* '''''Hubacyon''''' <small>Kretzoi, 1985</small>
* '''''Euroamphicyon?''''' <small>Viranta, 1996</small>
}}
'''''Amphicyon''''' is an extinct [[genus]] of large [[carnivorans]] belonging to the family [[Amphicyonidae]] (known colloquially as "bear-dogs"), [[subfamily]] [[Amphicyoninae]], from the [[Miocene]] epoch. Members of this family received their vernacular name for possessing bear-like and dog-like features. They ranged over [[North America]], [[Europe]], [[Asia]], and [[Africa]].
==Taxonomy==
{{multiple image
| align = left
| width = 125
| image1=Amphicyon major Blainvaille 1.jpg
| image2=Amphicyon major Blainvaille 2.jpg
| image3=Amphicyon minor Hemicyon sansaniensis Blainville.jpg
| footer = Sketches of fossil bones determined as belonging to ''Amphicyon'' by [[Henri Marie Ducrotay de Blainville]] in his 1841 iconography of living mammal skeletons and fossil mammal fossils. (1) and (2): ''Amphicyon major'', the type genus. (3) "''Amphicyon? minor''," which was reclassified to ''[[Hemicyon]] sansaniensis'' in 1851.
}}
In a note dated back to May 16, 1836, French geologist [[Alexandre Leymerie]] wrote of a letter in April that he requested from French palaeontologist [[Édouard Lartet]], which provided details of his exploits in palaeontological sites in the French [[departments of France|department]] of [[Gers]], in particular the [[Communes of France|commune]] [[Sansan, Gers|Sansan]]. Lartet described his finds of fossil taxons that he found within the sites, including "''[[Mammut|Mastodonte]]''" (species assigned to it were later reclassified to another [[Mammutidae|mammutid]] ''[[Zygolophodon]]'' and the [[gomphothere]] ''[[Gomphotherium]]''), "''Dinotherium''" (its species eventually reclassified as either ''[[Deinotherium]]'' or ''[[Prodeinotherium]]''), "''[[Rhinoceros (genus)|Rhinoceros]]''" (reclassified as an [[Aceratheriinae|aceratherine rhinocerotid]] ''[[Hoploaceratherium]]''), and "''[[Palaeotherium]]''" (the referred equid species now known as belonging to an [[Anchitheriinae|anchitherine]] ''[[Anchitherium]]''). He also recalled finding fossil "[[deer]]" species of which he said that the largest ones were the size of extant deer in [[France]] while the smallest ones were the size of small [[antelope]]. The palaeontologist noted that the "peaceful [[ruminants]]" coexisted with a "formidable" large [[carnivore]] he provisionally named ''Amphicyon'' based on two half-jaws and bones that he sent to a museum. He described it as having unilobed [[incisors]] and compressed [[canine (tooth)|canines]] similar to [[raccoons]] but also a carnivorous [[molar (tooth)|molar]] and its first two [[Cusp (anatomy)|tubercles]] conforming those to [[dogs]]. Lartet then stated that the genus's most distinct trait was the existence of a third tubercle at the upper jaw, which was not known in any other carnivore. The genus name appears to be derived from the [[Ancient Greek]] terms ἀμφί ("on both sides") and κύων ("dog"), but Lartet did not define the genus's etymology.<ref name="lartet">{{cite journal|last=Lartet|first=Édouard|year=1836|title=Nomenclature des mammifères et des coquilles qu'il a trouvés dans un terrain d'eau douce près de Simorre et de Sansan (Gers)|journal=Bulletin de la Société Géologique de France|language=french|volume=7|pages=217–220}}</ref>
[[File:Amphicyon major.jpg|thumb|left|''Amphicyon major'' cranium and mandible, [[National Museum of Natural History, France]]]]
Despite the initial status of the genus name ''Amphicyon'' as nonpermanent, French anatomist [[Henri Marie Ducrotay de Blainville]], a peer who Lartet had regularly discussed his fossil findings with, had sketched mammal skeletons and fossils in 1841, where he recognized the 2 species "''Amphicyon major''" and "''Amphicyon? minor''."<ref name="lartet"/><ref>{{cite book|last=de Blainville|first=Henri Marie Ducrotay|year=1841|title=Osteographie, ou, Description iconographique comparee du squelette et du systeme dentaire des mammiferes recents et fossiles pour servir de base a la zoologie et a la geologie|publisher=J.B. Baillière|language=french}}</ref> In 1851, Lartet reviewed the fossil carnivoran genera from Sansan. Among them were ''Amphicyon'', in which it was reconfirmed as a carnivorous mammal the size of extant [[bears]] that was discovered in Sansan in 1835. He recalled that its single-lobed incisors and its canines of serrated [[Dental anatomy#ridges|ridges]] are similar to the raccoon while the molars were similar to that of a dog. He confirmed the fossil specimens along with the third tubercle in the upper jaw (of which he said that it only exists in the extant [[bat-eared fox]] (then known as "''Canis megalotis''")) as belonging to the species ''Amphicyon major''. The palaeontologist described it as also having an [[anatomy]] of [[plantigrade]] locomotion similar to extant bears with few differences in form. Blainville was mentioned as speculating that it must have had a long and very strong tail. The species "''Amphicyon minor''" was reclassified as a separate genus ''[[Hemicyon]]'', which he described as a carnivore larger than a European [[wolf]] that was closer in form to a dog than ''Amphicyon'' and had [[dentition]] similar to [[mustelids]]. He also described a newer genus ''[[Pseudocyon]]'', which he misidentified as being [[digitigrade]] and described as being smaller than ''Amphicyon'' and coming closest to canids based on its dentition and bones. All three genera, Lartet said, had canines that retained finely serrated edges, implying that they were some of the top coexisting predators of the [[Miocene]] in modern-day France.<ref>{{cite book|last=Lartet|first=Édouard|year=1851|title=Notice sur la colline de Sansan, suivie d'une récapitulation des diverses espèces d'animaux vertébrés fossiles, trouvés soit à Sansan, soit dans d'autres gisements du terrain tertiaire miocène dans le bassin sous-Pyrénéen|publisher=J. - A. Portes|language=French|pages=16}}</ref>
==Species==
=== European species ===
[[File:Paléosite de Sansan 2021 14 - Amphicyon (cropped).jpg|300px|thumb|''Amphicyon major'' reconstructed skeleton, [[Sansan paleontological site|Site paléontologique de Sansan]]]]
*'''''Amphicyon astrei'''''
:The oldest known species of the genus, ''A. astrei'' is known from the Early Miocene sites Gardouch and Paulhiac in France, which date to MN1 (or "Mammal Neogene 1" as part of the [[Mammal Neogene zones]]). The species was originally described by Kuss in 1962, however, he also noted that its features do not completely match any known genus, and later moved it to the genus ''Pseudocyon'', as subspecies of ''P. sansanienis'', and considered it to be ancestral to ''P. s. intermedius'' (which has since then been moved to the separate genus ''[[Crassidia]]'').<ref name=":3">{{Cite book |last=Kuss |first=Sigfried Ernst |url=https://books.google.com/books?id=usKpBgAAQBAJ |title=Revision der europäischen Amphicyoninae: (Canidae, Carnivora, Mamm.) ausschließlich der voroberstampischen Formen |date=1965 |publisher=Springer-Verlag |isbn=978-3-642-99886-7 |language=de}}</ref> Ginsburg and Antunes later reassigned it to ''Amphicyon'', which was followed by other authors, and suggested that it was ancestral to later species of the genus.<ref name=":11">{{Cite book |last1=Rössner |title=The Miocene Land Mammals of Europe |last2=Heissig |publisher=Pfeil |year=1999 |location=Munich |pages=109–148 |chapter=Order Carnivora}}</ref><ref name=":32">{{Cite journal |last1=Jiangzuo |first1=Qigao |last2=Li |first2=Chunxiao |last3=Wang |first3=Shiqi |last4=Sun |first4=Danhui |date=2018-11-02 |title=Amphicyon zhanxiangi, sp. nov., a new amphicyonid (Mammalia, Carnivora) from northern China |url=https://doi.org/10.1080/02724634.2018.1539857 |journal=Journal of Vertebrate Paleontology |volume=38 |issue=6 |pages=e1539857 |doi=10.1080/02724634.2018.1539857 |bibcode=2018JVPal..38E9857J |s2cid=91998860 |issn=0272-4634}}</ref> Unlike later members of the genus, it did not possess enlarged posterior molars.<ref name=":03" />
*'''''Amphicyon lactorensis'''''
:This species was originally described by Astre on the basis of a single molar, from the French locality Le Mas d’Auvignon, which dates to MN4/5. Ginsburg referred more material from MN4-5 of France to this species, and assigned it to the subgenus ''Euroamphicyon''. Its M2 is peculiar, as it is anteroposteriorly shortened but transversely elongated.<ref name=":32" /> Kuss synonymized it with ''A. depereti'', which has since been moved to ''[[Ysengrinia]],'' although later authors generally consider it to be a valid species of ''Amphicyon''.<ref name=":3" /><ref name=":32" /><ref name=":9"/>
*'''''Amphicyon major'''''
:''A. major'', which was named by De Blainville in 1841, is both the type species of the genus but also the best known, as various cranial and even postcranial remains have been discovered across Western and Central Europe as well as Turkey.<ref>{{Cite journal |last1=Sabol |first1=Martin |last2=Holec |first2=Peter |date=2002 |title=Temporal and spatial distribution of Miocene mammals in the Western Carpathians (Slovakia) |url=https://www.researchgate.net/publication/266227379 |journal=Geologica Carpathica |volume=53 |issue=4 |pages=269–279 |via=researchgate}}</ref><ref>{{Cite journal |last1=Mayda |first1=Serdar |last2=Koufos |first2=George D. |last3=Kaya |first3=Tanju |last4=Gul |first4=Arzu |date=2015-01-01 |title=New carnivore material from the Middle Miocene of Turkey. Implications on biochronology and palaeoecology |url=https://www.sciencedirect.com/science/article/pii/S0016699514000965 |journal=Geobios |language=en |volume=48 |issue=1 |pages=9–23 |doi=10.1016/j.geobios.2014.11.001 |bibcode=2015Geobi..48....9M |issn=0016-6995}}</ref> It first appeared in MN4 and lasted until at least MN6. Amphicyonid remains from La Grive Saint-Alban, dating back to MN7/8, have also been assigned to this species.<ref name=":6" /> Others point out the differences between these fossils and the type material of ''A. major'', suggesting that they may belong to a separate species.<ref name=":32" /> It is likely closely related to the geologically younger ''A. eppelsheimensis'', ''A. gutmanni'' and ''A. pannonicus'', the first two of which had previously been assigned to ''A. major'' as subspecies.<ref name=":18">{{Cite journal |last1=Morlo |first1=Michael |last2=Nagel |first2=Doris |last3=Bastl |first3=Katharina |date=2020-09-01 |title=Evolution of the carnivoran (Carnivora, Mammalia) guild structure across the Middle/Upper Miocene boundary in Germany |url=https://www.sciencedirect.com/science/article/pii/S0031018220302467 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=553 |pages=109801 |doi=10.1016/j.palaeo.2020.109801 |bibcode=2020PPP...553j9801M |s2cid=219451746 |issn=0031-0182}}</ref><ref name=":15">{{Cite journal |last1=Agustí |first1=Jordi |last2=Cabrera |first2=Lluís |last3=Garcés |first3=Miguel |date=2013-01-01 |title=The Vallesian Mammal Turnover: A Late Miocene record of decoupled land-ocean evolution |url=https://www.sciencedirect.com/science/article/pii/S0016699513000065 |journal=Geobios |language=en |volume=46 |issue=1 |pages=151–157 |doi=10.1016/j.geobios.2012.10.005 |bibcode=2013Geobi..46..151A |issn=0016-6995}}</ref><ref name=":16">{{Cite book |url=http://www.rhinoresourcecenter.com/pdf_files/146/1468237570.pdf |title=Vösendorf: ein Lebensbild aus dem Pannon des Wiener Beckens |date=1954 |language=de}}</ref><ref name=":3" />
*'''''Amphicyon eppelsheimensis'''''
:A mandible and a mandibular fragment belong to ''A. eppelsheimensis'' were originally discovered at the locality Eppelsheim in Germany, and described by Weitzel in 1930. Other remains have since been found at Gau-Weinheim, which is located in close proximity to Eppelsheim, and the Spanish Valles de Fuentidueña. All these localities date to MN9-10.<ref name=":18" /><ref>{{Cite journal |last1=Ginsburg |last2=Morales |last3=Soria |date=1981 |title=Nuevos datos sobre los carnivoros de Los Valles de Fuentiduena (Segovia). |url=https://www.researchgate.net/publication/285250563 |journal=Estudios Geológicos |volume=37 |pages=383–415}}</ref> The taxonomic status of this species is controversial, with Kuss and several other authors considering this taxon to be a subspecies or synonym of A. major. Later authors however suggest that the two species are distinct, with ''A. eppelsheimensis'' possibly being the last representative of the ''A. major'' lineage. Notably, the p4 is more strongly reduced than in ''A. major'', and it is also slightly larger.<ref name=":3" /><ref name=":32" />
*'''''Amphicyon gutmanni'''''
:''A. gutmanni'' was described by Kittl in 1891 on the basis of a single, robust and low-crowned lower carnassial. Kuss considered it to be a subspecies of ''A. major'', but Kretzoi argued for its validity, based on the contour of its talonid, and even erected the separate genus ''Hubacyon'', with ''H. gutmanni'' as type species.<ref name=":3" /><ref name=":17">{{Cite journal |last=Kretzoi |first=M. |date=1985 |title=Neuer Amphicyonide aus dem Altpannon von Pécs (Südungarn) |url=http://publication.nhmus.hu/annales/cikkreszletes.php?idhoz=2450 |journal=Annales Musei historico-naturalis hungarici |volume=77 |pages=65–68}}</ref> Viranta followed his arguments for the distinction of this species, but did not consider ''Hubacyon'' to be a valid genus. The highest point of its hypoconid is located more posterior than in other members of this genus, and a line drawn from the posterolingual corner to the posterobuccal corner possesses a greater angle on the buccal side, due to the extended posterobuccal corner. Both of these features are similar to those seen in thaumastocyonines. Its type locality Mannersdorf, in Austria, is of uncertain age, but the presence of hipparionine horses shows that it is no older than MN9. Viranta also tentatively assigns molars from Kohfidisch, previously referred to cf. ''A. giganteus'', to this species. As this locality dates to MN11, this would make it one of the youngest members of the family.<ref name=":6" /> This species is likely closely related to ''A. major''.<ref name=":15" /><ref name=":16" />
*'''''Amphicyon pannonicus'''''
:The molar of this species was discovered in the Danitzpuszta sandpit in [[Pécs]], southern Hungary, and originally described by Kretzoi in 1985 as ''Hubacyon (Kanicyon) pannonicus''.<ref name=":17" /> Some authors state that locality of where it was found has been considered to date to MN11-12, which would make it one of the youngest known amphicyonids, although its exact dating is unclear.<ref name=":6" /><ref name=":13">{{Citation |last=Werdelin |first=Lars |title=Carnivore Behavior, Ecology, and Evolution |chapter=17. Carnivoran Ecomorphology: A Phylogenetic Perspective |date=2019-05-15 |chapter-url=https://www.degruyter.com/document/doi/10.7591/9781501745829-024/html |pages=582–624 |access-date=2023-04-08 |publisher=Cornell University Press |language=en |doi=10.7591/9781501745829-024 |isbn=978-1-5017-4582-9|s2cid=240701960 }}</ref> However, the terrestrial assemblage of the sandpit generally points towards an Early Pannonian (Vallesian) age, as which is in agreement with Kretzoi's original description.<ref>{{Cite book |last=Gasparik |first=Mihály |url=https://www.academia.edu/49838346 |title=Programme, Abstracts and Field Trip Guidebook of the 6th Workshop on the Neogene of Central and South-Eastern Europe |year=2015 |pages=102–124 |chapter=Neogene stratigraphy in the Mecsek region.}}</ref> This species is potentially hypercarnivorous, and only known from a single, fragmentary tooth, which is smaller, more slender and gracile than that of ''A. gutmanni'', as well as considerably more brachydont.<ref name=":17" /> Just like ''A. gutmanni'', it is considered to be closely related to ''A. major''.<ref name=":13" /><ref name=":15" /><ref name=":16" />
*'''''Amphicyon carnutense'''''
:''A. carnutense'', known from the MN3 of France and possibly Czechia, is a large species with a confusing taxonomic history. The type material from Chilleurs-aux-Boiwas was originally described a subspecies of ''A. giganteus'', ''A. g. carnutense'', and considered ancestral to the nominal subspecies ''A. g. giganteus''. The subspecies was discarded later on, but other authors considered ''A. carnutense'' distinct enough for it to be classified as a separate species. Adding to the confusion is the status of ''Megamphicyon'', to which ''A. carnutense'' is referred, which is variously considered to be synonymous with ''Amphicyon'', a subgenus of the former or a separate genus altogether. Furthermore, ''Amphicyon lathanicus'', originally described in 2000 on basis of isolated teeth from Beilleaux à Hommes, France, which date to MN3, with further remains reported across France, is likely synonymous with ''A. carnutense''.<ref>{{Cite journal |date=2001 |title=Les faunes de mammifères terrestres du Miocène moyen des Faluns du bassin de Savigné-sur-Lathan (France) |url=https://sciencepress.mnhn.fr/fr/periodiques/geodiversitas/23/3/les-faunes-de-mammiferes-terrestres-du-miocene-moyen-des-faluns-du-bassin-de-savigne-sur-lathan-france |journal=Geodiversitas |language=fr |volume=23 |issue=3 |pages=381–394}}</ref><ref name=":32" /><ref name=":20">{{Cite journal |last1=Morales |last2=Fejfar |last3=Heizmann |last4=Wagner |last5=Valenciano |last6=Abella |date=2021 |title=The Amphicyoninae (Amphicyonidae, Carnivora, Mammalia) Of The Early Miocene From Tuchořice, The Czech Republic |url=https://zenodo.org/record/7167294 |journal=Fossil Imprint |volume=77 |issue=1 |pages=126–144|doi=10.37520/fi.2021.011 |s2cid=245032640 |doi-access=free }}</ref>
[[File:Amphicyon giganteus mandible.JPG|left|thumb|Mandible of ''A. giganteus'']]
*'''''Amphicyon giganteus'''''
:''A. giganteus'' was originally described by Schinz in 1825, and in 1965 Kuss erected the genus ''Megamphicyon'' for this species, based on differences in its dentition and size between it and ''A. major''.<ref name=":3" /> Subsequent authors generally disregarded this assignment, with Ginsburg considering ''Megamphicyon'' a subgenus of ''Amphicyon''.<ref name=":32" /><ref name=":6" /><ref>{{Cite journal |last1=Peigné |first1=S. |last2=Salesa |first2=M. J. |last3=Antón |first3=M. |last4=Morales |first4=J. |date=2006-12-30 |title=New data on carnivores from the Middle Miocene (Upper Aragonian, MN 6) of Arroyo del Val area (Villafeliche, Zaragoza Province, Spain) |url=https://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/31 |journal=Estudios Geológicos |language=es |volume=62 |issue=1 |pages=359–374 |doi=10.3989/egeol.0662131 |issn=1988-3250|doi-access=free |hdl=10261/22441 |hdl-access=free }}</ref><ref name=":25" /><ref name=":11" /> Siliceo et al. revived the genus in 2020, a classification that was followed by some authors.<ref name=":10" /><ref name=":9" /><ref>{{Cite journal |last1=Březina |first1=Jakub |last2=Alba |first2=David M. |last3=Ivanov |first3=Martin |last4=Hanáček |first4=Martin |last5=Luján |first5=Àngel H. |date=2021-08-01 |title=A middle Miocene vertebrate assemblage from the Czech part of the Vienna Basin: Implications for the paleoenvironments of the Central Paratethys |url=https://www.sciencedirect.com/science/article/pii/S0031018221002583 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=575 |pages=110473 |doi=10.1016/j.palaeo.2021.110473 |bibcode=2021PPP...575k0473B |s2cid=236600984 |issn=0031-0182}}</ref> Others, however, reject the reclassification in favour of the older classification ''A. giganteus''.<ref name=":12" /><ref>{{Cite journal |last1=Morlo |first1=M. |last2=Friscia |first2=A. |last3=Miller |first3=E. |last4=Locke |first4=Ellis M. |last5=Nengo |first5=I. |date=2021 |title=Systematics and paleobiology of Carnivora and Hyaenodonta from Buluk, Early Miocene, Kenya |journal=Acta Palaeontologica Polonica |volume=66 |doi=10.4202/APP.00794.2020 |s2cid=236655608 |language=en|doi-access=free }}</ref> ''A. giganteus'' was a widespread European species that lived during the late [[Burdigalian]] to late [[Serravallian|Seravallian]], corresponding to the MN4-MN7/8.<ref name=":12">{{Cite journal |last1=van der Hoek |first1=Julien |last2=Karabaşoğlu |first2=Aslı |last3=Mayda |first3=Serdar |last4=van den Hoek Ostende |first4=Lars W. |date=2022-06-01 |title=Caught in travertine: computed tomography reveals the youngest record of Amphicyon giganteus from the travertine deposits of Karacalar (late middle Miocene, central Anatolia, Turkey) |url=https://doi.org/10.1007/s12542-022-00610-0 |journal=PalZ |language=en |volume=96 |issue=2 |pages=385–402 |doi=10.1007/s12542-022-00610-0 |issn=1867-6812 |pmc=8857634 |pmid=35221381}}</ref><ref name=":9">{{Cite journal |last1=Solé |first1=Floréal |last2=Lesport |first2=Jean-François |last3=Heitz |first3=Antoine |last4=Mennecart |first4=Bastien |date=2022-06-15 |title=A new gigantic carnivore (Carnivora, Amphicyonidae) from the late middle Miocene of France |journal=PeerJ |language=en |volume=10 |pages=e13457 |doi=10.7717/peerj.13457 |pmid=35726261 |pmc=9206431 |issn=2167-8359 |doi-access=free }}</ref> Most remains were found in Western Europe, although the youngest known record of the species is from Turkey, possibly suggesting the species survived in Anatolia after it had already gone extinct in Europe. Fossils from this species are also known from Bosnia and Herzegovina as well as the locality Arrisdrift in Namibia.<ref name=":25">{{Cite journal |last1=Bastl |first1=Katharina |last2=Nagel |first2=Doris |last3=Morlo |first3=Michael |last4=Göhlich |first4=Ursula B. |date=2020-06-01 |title=The Carnivora (Mammalia) from the middle Miocene locality of Gračanica (Bugojno Basin, Gornji Vakuf, Bosnia and Herzegovina) |journal=Palaeobiodiversity and Palaeoenvironments |language=en |volume=100 |issue=2 |pages=307–319 |doi=10.1007/s12549-018-0353-0 |s2cid=133767653 |issn=1867-1608|doi-access=free }}</ref><ref name=":0">{{cite journal |last1=Morales, J. |last2=Pickford, M. |last3=Soria, D. |last4=Fraile, S. |year=1998 |title=New carnivores from the basal Middle Miocene of Arrisdrift, Namibia |journal=Eclogae Geologicae Helvetiae |volume=91 |pages=27–40}}</ref><ref name=":1">{{cite journal |last1=Morales, J. |last2=Pickford, M. |last3=Fraile, S. |last4=Salesa, M. J. |last5=Soria, D. |year=2003 |title=Creodonta and Carnivora from Arrisdrift, early Middle Miocene of southern Namibia |journal=Memoirs of the Geological Survey of Namibia |volume=19 |pages=177–194}}</ref> It has also been referred to fossil specimens from Moghra in Egypt, but the referral of these fossils remains controversial.<ref name=":24">{{Cite journal |date=2019 |title=New Amphicyonids (Mammalia, Carnivora) from Moghra, Early Miocene, Egypt |url=https://sciencepress.mnhn.fr/en/periodiques/geodiversitas/41/21 |journal=Geodiversitas |language=en |volume=41 |issue=21 |pages=731–745|doi=10.5252/geodiversitas2019v41a21 |s2cid=208284245 |last1=Morlo |first1=Michael |last2=Miller |first2=Ellen R. |last3=Bastl |first3=Katharina |last4=Abdelgawad |first4=Mohamed K. |last5=Hamdan |first5=Mohammed |last6=El-Barkooky |first6=Ahmed N. |last7=Nagel |first7=Doris |doi-access=free }}</ref><ref name=":2">{{Cite journal |last1=Morales|first1=Jorge|last2=Pickford|first2=Martin|date=2022 |title=The taxonomic status of "Ysengrinia" ginsburgi Morales et al. 1998 (Amphicyonidae, Carnivora) from the basal middle Miocene of Arrisdrift, Namibia. |url=https://www.mme.gov.na/files/publications/b07_CommsGSN24pp1_16Morales_Pickford2022.pdf |journal=Communications of the Geological Survey of Namibia |volume=24 |pages=1–16 |via=Google Scholar}}</ref> It has furthermore been reported from Pakistans lower Vihowa Formation.<ref name=":21">{{Citation |last1=Antoine |first1=Pierre-Olivier |title=Chapter 16. Mammalian Neogene Biostratigraphy of the Sulaiman Province, Pakistan |date=2013-05-14 |url=https://www.degruyter.com/document/doi/10.7312/wang15012-016/html |pages=400–422 |access-date=2023-04-09 |publisher=Columbia University Press |language=en |doi=10.7312/wang15012-016 |isbn=978-0-231-52082-9 |last2=Métais |first2=Gregoire |last3=Orliac |first3=Maeva J. |last4=Crochet |first4=J.-Y. |last5=Flynn |first5=Lawrence J. |last6=Marivaux |first6=Laurent |last7=Rajpar |first7=Abdul Rahim |last8=Roohi |first8=G. |last9=Welcomme |first9=Jean-Loup}}</ref> It differs from ''A. major'' through its larger size, bigger premolars, shorter diastemata, a P4 that possesses a larger and lingually extended protocone and the presence of a paracone, that is very large and high paracone in comparison with its metacone, on its elongated M1. ''A. eibiswaldensis'' is generally considered to be a junior synonym of this species.<ref name=":32" />
*'''''Amphicyon laugnacensis'''''
:Originally described as subspecies of ''A. giganteus'', ''A. laugnacensis'' was elevated to species level by Ginsburg in 1999. It is the oldest known member of the ''A. giganteus'' lineage, with both its type locality Laugnac and possible remains from Gérand-le-Puy and Grépiac dating to MN2.<ref>{{Cite journal |last1=Ginsburg |last2=Cheneval |last3=Janvier |last4=Pouit |last5=Sen |date=2000 |title=Les Vertébrés des sables continentaux d'âge orléanien inférieur (MN 3) de Mauvières à Marcilly-sur-Maulne (Indre-et-Loire), La Brosse à Meigné-le-Vicomte (Maine-et-Loire) et Chitenay (Loir-et-Cher) |url=https://sciencepress.mnhn.fr/sites/default/files/articles/pdf/g2000n4a8.pdf |journal=Geodiversitas |volume=22 |issue=4 |pages=597–631}}</ref><ref>{{Cite journal |last=Ginsburg |date=2011 |title=Les Grands Mammifères du Burdigalien (MN3; Miocène) d'Estrepouy (Gers, France): liste faunique actualisée|url=https://www.researchgate.net/publication/270079655 |journal=Estudios Geológicos |language=en |volume=67 |issue=2 |pages=411–417 |doi=10.3989/egeol.40714.197|doi-access=free }}</ref> Its holotype is a maxilla, previously referred to ''A. astrei'', possesses a parastyle and a more posteriorly located protocone.<ref name=":32" />
*'''''Amphicyon olisiponensis'''''
:''A. olisiponensis'' was described by Antunes and Ginsburg in 1977 on the basis of a mandible discovered near Lisbon. Isolated teeth belonging to this species have also been reported from Buñol in Spain.<ref>{{Cite journal |last1=García |first1=Margarita Belinchón |last2=Romero |first2=Jorge Morales |date=1989 |title=Los carnívoros del Mioceno Inferior de Buñol (Valencia, España) |url=http://www.sepaleontologia.es/revista/anteriores/REP%20(1989)%20vol.%204/00.%20Belinchon%20&%20Morales.pdf |journal=Spanish Journal of Palaeontology |volume=4 |issue=1 |pages=3–8 |issn=2255-0550}}</ref> Both these localities date to MN4, although there is a possible report from La Retama, which dates to MN5, but the remains from there are as of yet undescribed. Differences in dentition, most notably the reduction of its premolars, led Viranta to erect the separate genus ''Euroamphicyon'' for this species.<ref name=":6" /> This proposal of a separate genus is followed by some authors.<ref name=":9" /><ref name=":20" /> Others, however, do not recognize "''Euroamphicyon''" as a distinct genus and instead still use ''A. olisiponensis''.<ref name=":32" /><ref name=":19" /><ref>{{Cite journal |last1=Peign |first1=Stphane |last2=Salesa |first2=Manuel J. |last3=Antn |first3=Mauricio |last4=Morales |first4=Jorge |title=A New Amphicyonine (Carnivora: Amphicyonidae) from the Upper Miocene of Batallones-1, Madrid, Spain |date=2008 |journal=Palaeontology |language=en |volume=51 |issue=4 |pages=943–965 |doi=10.1111/j.1475-4983.2008.00788.x|bibcode=2008Palgy..51..943P |s2cid=55334897 |doi-access=free }}</ref>
:
=== Asian species ===
*'''''Amphicyon ulungurensis'''''
:''A. ulungurensis'' is known from the early Langhian in the Halamagai Formation, near the Ulungur River from which it derives its name.<ref name=":26">{{Citation |last1=Qiu |first1=Zhan-Xiang |title=Chapter 1. Neogene Land Mammal Stages/Ages of China: Toward the Goal to Establish an Asian Land Mammal Stage/Age Scheme |date=2013-05-14 |url=https://www.degruyter.com/document/doi/10.7312/wang15012-001/html |pages=29–90 |access-date=2023-04-03 |publisher=Columbia University Press |language=en |doi=10.7312/wang15012-001 |isbn=978-0-231-52082-9 |last2=Qiu |first2=Zhu-Ding |last3=Deng |first3=Tao |last4=Li |first4=Chuan-Kui |last5=Zhang |first5=Zhao-Qun |last6=Wang |first6=Ban-Yue |last7=Wang |first7=Xiaoming}}</ref> Due to the lack of observation on the characteristics of the upper molars, there is neither evidence for including it nor for excluding it from the genus, in which it is placed mostly on the basis of its very large size.<ref name=":32" /> the holotype of this species is a fragmentary right hemimandible, but postcranial remains belonging to this species have also been described, including a comparatively small calcaneum and cuboid, possibly indicating sexual dimorphism.<ref name=":14">{{Cite journal |last1=Peigné |first1=Stéphane |last2=Chaimanee |first2=Yaowalak |last3=Yamee |first3=Chotima |last4=Tian |first4=Pannipa |last5=Jaeger |first5=Jean-Jacques |date=2006-04-01 |title=A new amphicyonid (Mammalia, Carnivora, Amphicyonidae) from the late middle Miocene of northern Thailand and a review of the amphicyonine record in Asia |url=https://www.sciencedirect.com/science/article/pii/S1367912004002093 |journal=Journal of Asian Earth Sciences |language=en |volume=26 |issue=5 |pages=519–532 |doi=10.1016/j.jseaes.2004.11.003 |bibcode=2006JAESc..26..519P |issn=1367-9120}}</ref><ref>{{Cite journal |last1=Jiangzuo |first1=Qigao |last2=Li |first2=Chunxiao |last3=Zhang |first3=Xiaoxiao |last4=Wang |first4=Shiqi |last5=Ye |first5=Je |last6=Li |first6=Yu |date=2020-02-07 |title=Diversity of Amphicyonidae (Carnivora, Mammalia) in the Middle Miocene Halamagai formation in Ulungur River area, Xinjiang, Northwestern China |url=https://doi.org/10.1080/08912963.2018.1477142 |journal=Historical Biology |volume=32 |issue=2 |pages=187–202 |doi=10.1080/08912963.2018.1477142 |s2cid=90842601 |issn=0891-2963}}</ref>
*'''''Amphicyon zhanxiangi'''''
:The only Asian amphicyonid which definitely belongs to the genus Amphicyon'', A. zhanxiangi'' was described in 2018 based on a maxillary fragment from the Zhang’enbao Formation in Ningxia, China. The Yinziling subfauna to which it belongs dates to the late Shanwangian, roughly corresponding to MN5.<ref name=":32" /> It has also been reported from the slightly younger locality Lagou, part of the Hujialiang Formation, in the Linxia Basin, dating to the Tunggurian, which is equivalent to MN6.<ref name=":5">{{Cite journal |last1=Sun |first1=Zhiqian |last2=Han |first2=Aili |last3=Li |first3=Yan |last4=Jiangzuo |first4=Qigao |last5=Wang |first5=Shiqi |last6=Li |first6=Shijie |date=2022-05-04 |title=New material of Amphicyon zhanxiangi from laogou, linxia basin suggests a possible southern dispersal with increasing omnivory |url=https://doi.org/10.1080/08912963.2021.1949009 |journal=Historical Biology |volume=34 |issue=5 |pages=857–864 |doi=10.1080/08912963.2021.1949009 |s2cid=237803060 |issn=0891-2963}}</ref> ''A. zhanxiangi'' is medium-sized, comparable to ''A. major'', and closely related to ''A. giganteus''.<ref name=":32" /> Over time, the diet of the species adapted towards omnivory as it moved towards more southern and humid areas, where greater amounts of plant material were available. The Lagou specimen showing greater adaptions to omnivory than the older one from Ningxia, which lived farther to the north, in a more arid terrain. This trend likely continued, with ''A. zhanxiangi'' being the probable ancestor of ''Arctamphicyon''.<ref name=":5" />
*'''''Amphicyon lydekkeri'''''
:''A. lydekkeri'' is known from the [[Dhok Pathan]] horizon in [[Pakistan]] and was described by Pilgrim in 1910, who later attributed it to its own genus, ''Arctamphicyon''. However, Pilgrim identified the holotype as first m1 and then as M1, despite it actually being a M2, making the diagnosis invalid. It has furthermore been argued that the differences between “''Arctamphicyon''” and ''Amphicyon'' are negligible, with the former being a junior synonym of the latter.<ref name=":14" /> Other authors consider the differences distinct enough for the separation of the two genera.<ref name=":32" /> Fossils from Yuanmou in Yunnan, and the Lower Irrawaddy Formation in Myanmar, show affinities to this species, and have been assigned to ''Arctamphicyon''.<ref name=":5" /> As the locality Hasnot, where ''A. lydekkeri'' was found, has been dated to the latest Miocene (7-5 Ma), this species is one of the youngest amphicyonids known.<ref>{{Cite journal |last1=Khan |first1=Muhammad Akbar |last2=Akhtar |first2=Muhammad |last3=Iliopoulos |first3=George |date=2014-09-01 |title=Cervid remains from the middle Siwaliks of Hasnot (Late Miocene), Pakistan |url=https://doi.org/10.1007/s12594-014-0139-6 |journal=Journal of the Geological Society of India |language=en |volume=84 |issue=3 |pages=352–360 |doi=10.1007/s12594-014-0139-6 |s2cid=128757418 |issn=0974-6889}}</ref>
*'''''Amphicyon cooperi'''''
:This species is only definitely known from its holotype, a single m1, discovered in rocks of the Bugi Hills probably dating to the early Miocene, although possible remains have been reported from the zones 4 and 6 of the Dera Bugti synclinal.<ref name=":14" /><ref>{{Cite journal |last1=Welcomme |first1=Jean-Loup |last2=Ginsburg |first2=Léonard |date=1997-12-01 |title=Mise en évidence de l'Oligocène sur le territoire des Bugti (Balouchistan, Pakistan) |url=https://www.sciencedirect.com/science/article/pii/S1251805097823816 |journal=Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science |language=fr |volume=325 |issue=12 |pages=999–1004 |doi=10.1016/S1251-8050(97)82381-6 |bibcode=1997CRASE.325..999W |issn=1251-8050}}</ref> It was described by Pilgrim in 1932. He noted that the tooth is very similar to that of ''A. shahbazi'', although ''A. cooperi'' lacks an external cingulum, and that it may actually belong to that species.<ref name=":22" />
[[File:Amphicyon.JPG|thumb|Skull and mandible of ''Amphicyon'', [[Palaeontological Museum, Munich|Paläontologisches Museum München]]]]
*'''''Amphicyon palaeindicus'''''
:''A. palaeindicus'' was described by [[Richard Lydekker]] in 1876 on the basis of an isolated M2 collected at Kushalgarh in the Potwar Plateau.<ref>{{Cite book |last=Lydekker |first=Richard |url=https://books.google.com/books?id=-17hpBh19RoC |title=Molar Teeth and Other Remains of Mammalia |date=1876 |publisher=Office of Superintendent of Government Printing |language=en}}</ref> Later authors referred a fragmentary mandible from Chinji, isolated teeth from the Chinji and the Nagri zones, and the Dang Valley, to this species.<ref name=":22">{{Cite book |last=Pilgrim |first=Guy Ellcock |url=https://books.google.com/books?id=plkaqAAACAAJ |title=The Fossil Carnivora of India |date=1932 |publisher=Government of India, Central Publication Branch |language=en}}</ref><ref name=":42">{{Cite journal |last=Colbert |first=Edwin H. |date=1935 |title=Siwalik Mammals in the American Museum of Natural History |url=https://www.jstor.org/stable/1005467 |journal=Transactions of the American Philosophical Society |volume=26 |pages=i–401 |doi=10.2307/1005467 |jstor=1005467 |issn=0065-9746}}</ref><ref>{{Cite journal |last1=West |first1=Robert M. |last2=Lukacs |first2=John R. |last3=Munthe |first3=Jens |last4=Hussain |first4=S. Taseer |date=1978 |title=Vertebrate Fauna from Neogene Siwalik Group, Dang Valley, Western Nepal |url=https://www.jstor.org/stable/1303847 |journal=Journal of Paleontology |volume=52 |issue=5 |pages=1015–1022 |jstor=1303847 |issn=0022-3360}}</ref> The exact age of the Chinji specimens cannot be defined, as the fossil-bearing localities in this region stretch from ca. 15 to 9 Ma, although the correlation of the Dang Valley fauna suggests that they're of late middle Miocene age, whereas the Nagri fauna dates to the [[Vallesian]].<ref name=":14" /><ref name=":7">{{Cite journal |last1=Nanda |first1=A. C. |last2=Sehgal |first2=R. K. |last3=Chauhan |first3=P. R. |date=2018-08-15 |title=Siwalik-age faunas from the Himalayan Foreland Basin of South Asia |url=https://www.sciencedirect.com/science/article/pii/S136791201730603X |journal=Journal of Asian Earth Sciences |series=Emergence and Evolution of Himalayan Foreland Basin |language=en |volume=162 |pages=54–68 |doi=10.1016/j.jseaes.2017.10.035 |bibcode=2018JAESc.162...54N |s2cid=134929306 |issn=1367-9120}}</ref> It has been suggested that none of the Siwalik species truly belong to ''Amphicyon'',<ref>{{Cite journal |last1=Raza |first1=S. Mahmood |last2=Barry |first2=John C. |last3=Meyer |first3=Grant E. |last4=Martin |first4=Lawrence |date=1984-12-01 |title=Preliminary report on the geology and vertebrate fauna of the Miocene Manchar Formation, Sind, Pakistan |url=https://doi.org/10.1080/02724634.1984.10012034 |journal=Journal of Vertebrate Paleontology |volume=4 |issue=4 |pages=584–599 |doi=10.1080/02724634.1984.10012034 |bibcode=1984JVPal...4..584R |issn=0272-4634}}</ref> although others suggests that ''A. palaeindicus'' should be referred to this genus.<ref name=":03">{{Cite journal |last=Hunt |first=Robert M. |date=2003 |title=Intercontinental Migration of Large Mammalian Carnivores: Earliest Occurrence of the Old World Beardog Amphicyon (Carnivora, Amphicyonidae) in North America |url=https://digitalcommons.unl.edu/geosciencefacpub/545 |journal=Bulletin of the American Museum of Natural History |volume=279 |page=77 |doi=10.1206/0003-0090(2003)279<0077:C>2.0.CO;2}}</ref>
*'''''Amphicyon pithecophilus'''''
:Pilgrim erected this species in 1932 on basis of an isolated m2 from Chinji. He furthermore assigned two fragmentary mandibles, from Chinji and Nurpur, previously referred to ''A. palaeindicus'' to this species.<ref name=":22" /> Colbert considered it a synonym of that species, although later authors considered it distinct due to its larger metacone and stronger buccal cingulum on the M2.<ref name=":42"/><ref name=":14" /><ref name=":32" />
*'''''Amphicyon sindiensis'''''
:''A. sindiensis'' is one of the most poorly known species assigned to the genus, being only known from a fragmentary right mandible and an isolated molar from the basal beds of the Manchar Formation in Pakistan, dating to the early Middle Miocene. The dimensions of its m2 are similar to those of ''[[Maemohcyon]]''.<ref name=":14" />
*'''''Amphicyon shahbazi'''''
:''A. shahbazi'' was described by Pilgrim in 1910 on the basis of two poorly preserved mandibular fragments from the Bugti Hills. the exact age of these fossils is not known, but other fragmentary remains assigned to this species, discovered in the upper Chitarwata Formation and lower Vihowa Formation, which correlate with MN2-3, suggests they date to the Early Miocene.<ref name=":21" /><ref name=":14" />
*'''''Amphicyon confucianus'''''
:It is only known from a single, fragmentary right hemimandible, which includes p3 and m1. ''A. confucianus'' is part of the Shanwang Local Fauna, which dates to ca. 16 Ma. It is a large species, comparable to ''A. ulungurensis'' in size.<ref name=":14" /><ref name=":03" /> The attribution of this species to ''Amphicyon'' remains unclear, although it probably does not belong to this genus.<ref name=":32" />
*'''''Amphicyon tairumensis'''''
:''"Amphicyon" tairumensis'' was described by [[Edwin H. Colbert|Edwin Harris Colbert]] in 1939, on the basis of a left hemimandible with heavily worn teeth discovered in the Inner Mongolian Tunggur Formation.<ref>{{Cite web |last1=Expeditions |first1=Central Asiatic |last2=Colbert |first2=Edwin H. |others=American Museum of Natural History Library |title=Carnivora of the Tung Gur Formation of Mongolia. Bulletin of the AMNH ; v. 76, article 2 |url=https://www.biodiversitylibrary.org/bibliography/88570 |access-date=2023-03-27 |website=Biodiversity Heritage Library}}</ref> It is a wolf-sized predator, considerably smaller than ''A. major''.<ref>{{Cite journal |last1=Wang |last2=Ye |last3=Meng |last4=Wu |last5=Liu |last6=Bi |date=1998 |title=Carnivora from middle Miocene of northern Junggar Basin, Xinjiang Autonomous Region, China |journal=Vertebrata PalAsiatica |volume=36 |issue=3 |pages=218–243}}</ref><ref name=":14" /> The m1 is swollen at the lingual point between the talonid and the trigonid, a feature not seen in European members of the genus. A similar, but currently unpublished, form from Laogou has upper dental characteristics quite unlike ''Amphicyon'', and it has been proposed that it is more closely related to ''Pseudocyon'' because of its size and the lingual convexity of its m1.<ref name=":32" /><ref>{{Cite journal |last1=Jiangzuo |first1=Qigao |last2=Sun |first2=Danhui |last3=Flynn |first3=John J. |date=2021-09-02 |title=Paleobiogeographic implications of additional Felidae (Carnivora, Mammalia) specimens from the Siwaliks |url=https://doi.org/10.1080/08912963.2020.1737683 |journal=Historical Biology |volume=33 |issue=9 |pages=1767–1780 |doi=10.1080/08912963.2020.1737683 |s2cid=216279658 |issn=0891-2963}}</ref>
=== North American species ===
*'''''Amphicyon galushai'''''
:[[File:Amphicyon-ingens reconstruction.jpg|thumb|Restoration of ''A. ingens''|300x300px]]''A. galushai'' represents the first occurrence of ''Amphicyon'' in North America, approximately 18.8&ndash;17.5 Mya during the early [[Hemingfordian]]. Described by Robert M. Hunt Jr. in 2003, it is mostly known from fossils found in the Runningwater Formation of western [[Nebraska]] and includes a complete adult skull, a partial juvenile skull, 3 mandibles and teeth and postcranial elemenents representing least 15 individuals. There is an additional skull fragment from the Troublesome Formation of Colorado. ''A. galushai'' is considered ancestral to the late Hemingfordian species, ''Amphicyon frendens''.<ref name=":03"/>
*'''''Amphicyon frendens'''''
:''A. frendens'' lived during the late Hemingfordian, 17.5&ndash;15.9 Mya. The species was originally described by W. Matthew in 1924 from specimens found in the middle member of the Sheep Creek Formation, [[Sioux County, Nebraska]].<ref name="Matthew1924">W. D. Matthew. 1924. Third contribution to the Snake Creek Fauna. Bulletin of the American Museum of Natural History 50:59-210</ref> ''A. frendens'' specimens have since been found at sites in [[Harney County, Oregon|Harney]] and [[Malheur County, Oregon|Malheur Counties, Oregon]]. It was considerably bigger than the earlier ''A. galushai'', and possessed a larger M2.<ref name="Hunt1998">{{cite book |last=Hunt |first=Robert M. |title=Evolution of tertiary mammals of North America, volume 1: Terrestrial carnivores, ungulates and ungulatelike mammals |publisher=Cambridge University Press. |year=1998 |isbn=978-0521355193 |editor=Janis, C. M. |location=Cambridge, UK |pages=196–227 |chapter=Amphicyonidae |editor2=Scott, K.M. |editor3=Jacobs, L. L. |chapter-url=https://books.google.com/books?id=I-RgojcDyWYC&q=Amphicyonidae}}</ref>
*'''''Amphicyon ingens'''''
:This huge species lived during the early to middle [[Barstovian]], 15.8&ndash;14.0 Mya.<ref name=Sorkin2>{{cite journal|last=Sorkin|first=B.|title=Ecomorphology of the giant bear-dogs ''Amphicyon'' and ''Ischyrocyon''|journal=Historical Biology|year=2006|volume=18|issue=4|pages=375–388|doi=10.1080/08912960600618073|s2cid=85341612|url=http://doc.rero.ch/record/13473/files/PAL_E154.pdf }}</ref> It was originally described by W. Matthew in 1924 from specimens found in the Olcott Formation, [[Sioux County, Nebraska]].<ref name="Matthew1924"/> Specimens attributed to this species have since been found in [[California]], [[Colorado]] and [[New Mexico]].<ref name=Hunt1998/> ''A. ingens'' possessed the largest canines of any amphicyonine.<ref name=":03" />
*'''''Amphicyon longiramus'''''
:"''Amphicyon intermedius''" is a name used to refer to a dubious species found at Thomas Farm of the Hawthorne Formation in Florida, which was described by White in 1940. However, the name was preoccupied by a different species described by von Meyer in 1849, which is a synonym of ''[[Crassidia|Crassidia intermedia]]'', a [[Thaumastocyoninae|thaumastocyonine]] found in the localities of Germany and France that is not closely related to the taxon found in Florida.<ref name="crassidia">{{Cite journal |last1=Heizmann |last2=Kordikova |date=2000 |title=Zur systematischen Stellung von "Amphicyon" intermedius H. v. Meyer, 1849 (Carnivora, Amphicyonidae) |url=https://www.zobodat.at/pdf/Carolinea_58_0069-0082.pdf |journal=Carolinea}}</ref><ref>{{cite journal|last1=Morales|first1=Jorge|last2=Fejfar|first2=Oldřich|last3=Heizmann|first3=Elmar|last4=Wagner|first4=Jan|last5=Vaquero|first5=Alberto Valenciano|last6=Abella|first6=Juan|year=2019|title=A New Thaumastocyoninae (Amphicyonidae, Carnivora) from the Early Miocene of Tuchořice, the Czech Republic|journal=Fossil Imprint|volume=75|issue=3–4|pages=397–411|doi=10.2478/if-2019-0025|s2cid=210921722 |doi-access=free}}</ref> The species as referred to White were attributed additionally to ''Amphicyon'' remains found in 1992 in the lower part of the Calvert Formation at the Pollack Farm Site in [[Delaware]] dating to the early [[Hemingfordian]] (or early Miocene) based on the past referral of the Hawthorne Formation fossils to ''A. intermedius''.<ref name=":27">{{Cite journal|last1=Emry|first1=Robert J.|last2=Eshelman|first2=Ralph E.|year=1998|title=The Early Hemingfordian (Early Miocene) Pollack Farm Local Fauna: First Tertiary Land Mammals Described From Delaware|journal=Delaware Geological Society, Special Publication|pages=153–174}}</ref> However, a 1960 source by Olsen refers to ''A. intermedius'' as a synonym to ''A. longiramus'', which Heizmann and Kordikova acknowledged in 2000 as making ''A. longiramus'' the valid name over White's ''A. intermedius'' name.<ref>{{cite journal|last=Olsen|first=Stanley J.|year=1960|title=The fossil carnivore Amphicyon longiramus from the Thomas farm Miocene. Part II: postcranial skeleton.|journal=Bulletin of the Museum of Comparative Zoology at Harvard College in Cambridge|volume=123|issue=1|pages=1–45}}</ref><ref name="crassidia"/> Additionally, a 2012 article on ''Amphicyon'' by the [[Florida Museum of Natural History]] also refers to ''A. intermedius'' as a synonym to ''A. longiramus'' based on the similarities of the two in the localities of Florida and Delaware. The species ''A. longiramus'' is said to have coexisted with the smaller amphicyonine ''[[Cynelos]] caroniavorus'' (White, 1942), which was also found in the Thomas Farm locality.<ref name=":28">{{cite web|url=https://www.floridamuseum.ufl.edu/florida-vertebrate-fossils/species/amphicyon-longiramus/|last=Morse|first=Paul E.|date=October 5, 2012|title=Amphicyon longiramus|publisher=Florida Museum of Natural History|access-date=9 April 2023|language=en}}</ref>
==Description==
[[File:Africa - the evolution of a continent and its large mammal fauna (2006) fig. 7.png|thumb|Size comparison of ''[[Hyainailouros|Hyainailouros sulzeri]]'', ''Amphicyon giganteus'' and ''[[Spotted hyena|Crocuta crocuta]]''|300x300px]]
''Amphicyon'' was a large to very large predator, although the various species differ considerably in size, ranging from moderately sized species such as ''A. astrei'' to the huge ''A. ingens'', which was one of the biggest carnivorans of all time. The estimated weight of male ''A. major'' is 212&nbsp;kg, while females are smaller, at only 122&nbsp;kg, indicating significant sexual dimorphism. The shoulder height of a young female, which has been estimated to have weighed 125&nbsp;kg, has been reconstructed as 65&nbsp;cm.<ref name=":29">{{Cite journal |last=Argot |first=Christine |date=2010 |title=Morphofunctional analysis of the postcranium of Amphicyon major (Mammalia, Carnivora, Amphicyonidae) from the Miocene of Sansan (Gers, France) compared to three extant carnivores: Ursus arctos, Panthera leo, and Canis lupus |url=https://sciencepress.mnhn.fr/en/periodiques/geodiversitas/32/1/analyse-morphofonctionnelle-du-squelette-postcranien-d-amphicyon-major-mammalia-carnivora-amphicyonidae-du-miocene-de-sansan-gers-france-compare-trois-carnivores-actuels-ursus-arctos-panthera-leo-et-canis-lupus |journal=Geodiversitas |volume=32 |issue=1 |pages=65–106|doi=10.5252/g2010n1a2 |s2cid=129286228 }}</ref> As the largest Old World species of the genus, ''A. giganteus'' was considerably larger, with females weighing 157&nbsp;kg and males 317&nbsp;kg, although they may have grown considerably larger.<ref name=":6">{{Cite journal |last=Viranta |first=Suvi |date=1996 |title=European Miocene Amphicyonidae –taxonomy, systematics and ecology. |journal=Acta Zoologica Fennica |volume=204 |pages=1–61}}</ref><ref name=":10">{{Cite journal |last1=Siliceo |first1=Gema |last2=Morales |first2=Jorge |last3=Antón |first3=Mauricio |last4=Salesa |first4=Manuel J. |date=2020-06-18 |title=New fossils of Amphicyonidae (Carnivora) from the middle Miocene (MN6) site of Carpetana (Madrid, Spain) |url=https://digital.csic.es/handle/10261/230330 |journal=Geodiversitas |doi=10.13039/501100002911 |hdl=10261/230330 |issn=1638-9395}}</ref> The mass of several other European species has been estimated craniodental measurements, which generally falls into the range of estimations derived from postcranial remains, although it may slightly overestimate their weight.<ref name=":8">{{Cite journal |last1=Figueirido |last2=Pérez-Claros |last3=Hunt |last4=Palmqvist |date=2011 |title=Body Mass Estimation in Amphicyonid Carnivoran Mammals: A Multiple Regression Approach from the Skull and Skeleton |url=https://bioone.org/journals/acta-palaeontologica-polonica/volume-56/issue-2/app.2010.0005/Body-Mass-Estimation-in-Amphicyonid-Carnivoran-Mammals--A-Multiple/10.4202/app.2010.0005.full |journal=Acta Palaeontologica Polonica|volume=56 |issue=2 |pages=225–246 |doi=10.4202/app.2010.0005 |s2cid=56051166 |doi-access=free }}</ref> ''A. astrei'' is the smallest species, estimated at 112&nbsp;kg, while ''A. laugnacensis'' and ''A.'' ''lactorensis'' were somewhat larger, at ~130&nbsp;kg and 132&nbsp;kg, respectively. ''A. olisiponensis'' is estimated at 147&nbsp;kg and ''A. carnutense'' as 182&nbsp;kg, while ''A. eppelsheimensis'' and ''A. gutmanni'' are among the biggest members of the genus, with estimated weights of 225 and 246&nbsp;kg.<ref name=":9" /> The North American species of the genus show a considerable size increase over the course of their evolution, with the earliest one, ''A. galushai'', being estimated at 187&nbsp;kg, whereas ''A. frendens'' was considerably larger, at 432&nbsp;kg. Finally, the terminal North American species, ''A. ingens'', was among the largest of all amphicyonids, with an estimated body mass of 550&nbsp;kg.<ref name=":8" /><ref>{{Cite journal |last=Sorkin |first=B. |date=2006-12-01 |title=Ecomorphology of the giant bear-dogs Amphicyon and Ischyrocyon |url=https://doi.org/10.1080/08912960600618073 |journal=Historical Biology |volume=18 |issue=4 |pages=375–388 |doi=10.1080/08912960600618073 |s2cid=85341612 |issn=0891-2963}}</ref>
Its skeleton showcases a variety of features resembling canids, ursids and felids. ''Amphicyon'' possessed a powerful skull, with a long snout and high sagittal crests. The canines are robust, and the posterior molars are enlarged, whereas the anterior premolars are reduced. Its neck is wide, similar to that of a bear.<ref>{{Cite journal |last1=Siliceo |first1=Gema |last2=Salesa |first2=Manuel J. |last3=Antón |first3=Mauricio |last4=Pastor |first4=Juan F. |last5=Morales |first5=Jorge |date=2015-06-01 |title=Comparative Anatomy of the Shoulder Region in the Late Miocene Amphicyonid Magericyon anceps (Carnivora): Functional and Paleoecological Inferences |url=https://doi.org/10.1007/s10914-014-9270-9 |journal=Journal of Mammalian Evolution |language=en |volume=22 |issue=2 |pages=243–258 |doi=10.1007/s10914-014-9270-9 |hdl=10261/121791 |s2cid=254699569 |issn=1573-7055|hdl-access=free }}</ref> Its postcranial skeleton is stout and robust, with massive, powerful limbs, and mobile shoulder joints as well as flexible wrists. The upper limb bones are comparatively long in comparison to the lower ones, and it did not possess any adaption towards cursoriality. Its posture was more similar to plantigrade taxa such as ursids than to digitgrade ones like felids, and their claws were not retractable. ''Amphicyon'' also had a rather flexible back, and a heavy tail, which has been estimated to have possessed as many as 28 caudal vertebrae, and may have been as long as the rest of the spine.<ref name=":03" /><ref name=":29" />
==Palaeobiology==
=== Diet and predatory behaviour ===
The diet of ''Amphicyon'' has proven difficult to reconstruct, as its dentition possesses both crushing and shearing functions. It has been proposed, on the basis of dental wear patterns and morphology, that European species of this genus were bone-crushing [[mesocarnivore]]s.<ref name=":6" /> One study argued that ''A. longiramus'' was [[Hypercarnivore|hypercarnivorous]], as the relative grinding area of its lower molars is similar to that of carnivorous canids, whereas another suggested that the North American species of the genus were omnivores.<ref name="sorkin">{{cite journal |last1=Sorkin |first1=B. |year=2006 |title=Ecomorphology of the giant bear-dogs ''Amphicyon'' and ''Ischyrocyon'' |url=https://www.researchgate.net/publication/40661208 |journal=Historical Biology |volume=18 |issue=4 |pages=375–388 |doi=10.1080/08912960600618073 |s2cid=85341612}}</ref><ref name=":03" /> A dental microwear analysis of ''A. major'' recovers the diet of this species as mesocarnivorous, similar to [[red fox]]es, consuming meat as well as plants and hard items, which presumably included bone.<ref>{{Cite journal |last1=Goillot |first1=Cyrielle |last2=Blondel |first2=Cécile |last3=Peigné |first3=Stéphane |date=2009-01-01 |title=Relationships between dental microwear and diet in Carnivora (Mammalia) — Implications for the reconstruction of the diet of extinct taxa |url=https://www.sciencedirect.com/science/article/pii/S0031018208005245 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=271 |issue=1 |pages=13–23 |doi=10.1016/j.palaeo.2008.09.004 |bibcode=2009PPP...271...13G |issn=0031-0182}}</ref> Another dental microwear analysis also supports an omnivorous diet for ''A. giganteus'', whose dentition possesses a high number of large pits and several small pits, and notes that it clearly differs from bone-crushing taxa such as hyaenas.<ref>{{Cite journal |last1=Xafis |first1=Alexandros |last2=Saarinen |first2=Juha |last3=Bastl |first3=Katharina |last4=Nagel |first4=Doris |last5=Grímsson |first5=Friðgeir |date=2020-06-01 |title=Palaeodietary traits of large mammals from the middle Miocene of Gračanica (Bugojno Basin, Bosnia-Herzegovina) |url=https://doi.org/10.1007/s12549-020-00435-2 |journal=Palaeobiodiversity and Palaeoenvironments |language=en |volume=100 |issue=2 |pages=457–477 |doi=10.1007/s12549-020-00435-2 |issn=1867-1608 |pmc=7320953 |pmid=32647552}}</ref> As both its anterior premolars and posterior molars are reduced, ''A. olisiponensis'' may have been more hypercarnivorous than other European species.<ref name=":32" />
[[File:Mascall-Mural-Amphicyon & Miolabis.jpg|thumb|300x300px|''Amphicyon'' attacking ''Miolabis'']]
As it lacked the adaptations for rapid acceleration, ''Amphicyon'' seems to have hunted quite unlike lions and tigers, which approach their prey very closely, before overtaking it after a quick burst of speed. However, as even modern pursuit predators such as wolves stalk and ambush their prey, it is likely that ''Amphicyon'' did the same. It has been proposed that it pursued its prey for longer distances, and at a speed notably slower than modern wolves. After catching up to its victim, it was likely able to immobilize it with its powerful forelimbs. Its postscapular fossa indicates a well-developed subscapularis minor muscle, which fixes the shoulder joint, and prevents the head of the humerus from being dislocated by the struggles of a prey animal trying to break free. The anatomy of its humerus also supports this, as it showcases the presence of a strong pronator teres muscle, and thereby pronation of the forearm, and powerful flexors of digits and wrists, which are integral to the prey-grasping ability of both extant bears and big cats. Indeed, the trochlea of its humeral condyle is shallower than that of a tiger, suggesting that the  pronation/supination of its forearms might have been even greater than in large felids, although it likely lacked the ability of cats to retract their claws. Its small infraorbital foramina indicates that it lacked the well-developed vibrissae of cats, which provides them with the sensory information needed to place a precise killing bite. Therefore, it may have killed its prey by tearing open the preys ribcage, as thylacines did, or by biting into its neck to sever major blood vessels. Just like modern predators, it likely did not target its preys abdomen, as wounds in that area do not kill quickly. As the elongation of its distal limb segments was more similar to that of the solitary tiger than to the social lion, ''Amphicyon'' was likely solitary as well. Due to its comparatively slow maximum speed and lack of rapid acceleration, it is unlikely that ''Amphicyon'' preyed on cursorial ungulates. However, it has been proposed that its pursuit capabilities were suited to chase mediportal ungulates, such as merycoidodontids and rhinoceroses.<ref name="sorkin" /> A specimen of the rhinoceros ''[[Prosantorhinus|Prosantorhinus douvillei]]'' was discovered with bitemarks corresponding to those of ''A. giganteus'', although it remains unclear if this was the result of active predation or merely scavenging of remains.<ref name="Antunesa2006">{{cite journal |author=M. T. Antunes |display-authors=etal |year=2006 |title=Ichnological evidence of a Miocene rhinoceros bitten by a bear-dog (Amphicyon giganteus) |journal=Annales de Paléontologie |volume=92 |issue=1 |pages=31–39 |doi=10.1016/j.annpal.2005.10.002|bibcode=2006AnPal..92...31A }}</ref><ref>{{Cite journal |last=Heissig |first=Kurt |date=2017-12-31 |title=Revision Of The European Species Of Prosantorhinus Heissig, 1974 (Mammalia, Perissodactyla, Rhinocerotidae) |url=http://fi.nm.cz/wp-content/uploads/2017/12/02_Heissig_2017.pdf |journal=Fossil Imprint |volume=73 |issue=3–4 |pages=236–274 |doi=10.2478/iF-2017-0014|s2cid=134330581 }}</ref> Other bitemarks referred to the species ''A. olisiponensis'' were found on a metapodial belonging to the large anthracothere ''[[Brachyodus|Brachyodus onoideus]]''.<ref name=":19">{{Cite journal |last1=Antunes |first1=M. Telles |last2=Ginsburg |first2=L. |date=2010-12-30 |title=The last Anthracothere Brachyodus onoideus (Mammalia, Artiodactyla) from westernmost Europe and its extinction |url=https://run.unl.pt/handle/10362/4741 |journal=Ciências da Terra}}</ref> Bite traces on various mammalian long bones from the Early Miocene of Czechia have also been attributed to Amphicyon. As patterned bones have no immediate benefit for feeding, they likely represent evidence of active predation.<ref>{{Cite journal |last1=Mikuláš |first1=Radek |last2=Kadlecová |first2=Eva |last3=Fejfar |first3=Oldřich |last4=Dvořák |first4=Zdeněk |date=2006-09-01 |title=Three New Ichnogenera of Biting and Gnawing Traces on Reptilian and Mammalian Bones: A Case Study from the Miocene of the Czech Republic |url=https://doi.org/10.1080/10420940600850729 |journal=Ichnos |volume=13 |issue=3 |pages=113–127 |doi=10.1080/10420940600850729 |s2cid=128644469 |issn=1042-0940}}</ref>
=== Sexual dimorphism ===
Strong sexual dimorphism is present in a variety of species, known from both Europe and North America, with the males being considerably larger than the females. Although this size difference is present in many amphicyonids, it is more strongly developed in ''Amphicyon'' than in ''Cynelos lemanensis''.<ref>{{Cite book |last=Peigné |first=Stéphane |url=https://katalog.ub.tu-freiberg.de/Record/0-1183785186 |title=The Amphicyonidae (Mammalia: Carnivora) from Ulm-Westtangente (MN 2, Early Miocene), Baden-Württemberg, Germany: systematics and ecomorphology; with 14 tables |date=2003 |publisher=Staatliches Museum für Naturkunde |series=Stuttgarter Beiträge zur Naturkunde / B, 343}}</ref> The males furthermore possess slightly longer and more robust snouts, larger canines and immense sagittal crests. Comparison with other strongly sexually dimorphic carnivorans suggests that ''Amphicyon'' was [[Polygyny in animals|polygynous]], with territorial males competing with each other for females during the mating season. This may have contributed to the size increase observed within the genus.<ref name=":03" />
=== Possible footprints ===
Footprints assigned to the [[ichnotaxon]] ''Hirpexipes alfi'' were discovered in the Californian Barstow Formation, and match the feet of ''A. ingens''. They showcase that the animal was semidigitigrade to semiplantigrade, and possessed long and sharp claws. Hiripex means "rake", and references the long, flexible digits of the foot, which reminded the authors of the prongs of leaf rakes.<ref>{{Cite journal |last1=Sarjeant |last2=Reynolds |last3=Kissell-Jones |date=2002 |editor-last=Reynolds |title=Fossil Creodont and Carnivore Footprints from California, Nevada, and Wyoming |url=http://www.desertsymposium.org/DS_2002_Between_the_Basins.pdf#page=37 |journal=Between the Basins: Exploring the Western Mojave and Southern Basin and Range Province|archive-url=https://web.archive.org/web/20230721104541/http://www.desertsymposium.org/DS_2002_Between_the_Basins.pdf#page=37|archive-date=21 July 2023}}</ref>
Another ichnotaxon associated with ''Amphicyon'' is ''Platykopus maxima'' from the Hungarian Early Miocene locality Ipolytarnóc. The footprints were attributed to ''A. major'' on the basis of their size and short phalanges.<ref>{{Cite journal |last1=Botfalvai |first1=Gábor |last2=Magyar |first2=János |last3=Watah |first3=Veronika |last4=Szarvas |first4=Imre |last5=Szolyák |first5=Péter |date=2022-08-16 |title=Large-sized pentadactyl carnivore footprints from the early Miocene fossil track site at Ipolytarnóc (Hungary): 3D data presentation and ichnotaxonomical revision |url=https://doi.org/10.1080/08912963.2022.2109967 |journal=Historical Biology |volume=35 |issue=9 |pages=1709–1725 |doi=10.1080/08912963.2022.2109967 |s2cid=251633910 |issn=0891-2963}}</ref>
==Fossil distribution==
Fossil remains of ''Amphicyon'' are most common in Western and Central Europe, where they were discovered in various countries, including France, Germany, Spain and Hungary, but were also found in Bosnia-Herzegovina and Turkey. ''A. astrei'' is the oldest known species, and may have been the ancestor of the later members of the genus, and is known from the earliest Miocene of France.<ref name=":32" /> Species belonging to the ''A. giganteus'' lineage appeared shortly afterwards, and are common in Europe until MN6, which corresponds to 13.7 to 12.75 Ma. However, this species is also known from Turkey, where it was found in the Karacalar locality, which dates to 11.6 ± 0.25 Ma, indicating that it survived in Anatolia after it had already disappeared in Europe.<ref name=":12" /> Throughout the Middle Miocene of Europe, it was sympatric with the considerably smaller ''A. major'', although the two species were likely ecologically or environmentally separated.<ref name=":10" /> While common throughout the continent during the Middle Miocene, amphicyonid diversity decreased following the Vallesian Turnover, with the last known European species of the genus surviving in Central Europe until MN11, which dates from 8.7 to 7.75 Ma.<ref name=":9" /><ref name=":6" /><ref name=":15" />
While various remains and species of ''Amphicyon'' have been reported from South and East Asia, their referral is often problematic, as they're usually known from fragmentary material and all large sized amphicyonids found on the continent are generally placed in this genus.<ref name=":03" /> The only species definitely belonging to this genus is ''A. zhanxiangi'' from the middle Miocene of China.<ref name=":32" /> Other, tentatively assigned, species of this genus are known from China throughout the early Middle Miocene, but disappear by the late Miocene.<ref name=":26" /><ref>{{Cite journal |last1=Jiangzuo |first1=Qigao |last2=Wang |first2=Shiqi |last3=Deng |first3=Tao |date=2023-04-01 |title=Chronological framework and palaeoecology of Carnivora from the Linxia Basin, China |url=https://www.sciencedirect.com/science/article/pii/S0031018223000810 |journal=Palaeogeography, Palaeoclimatology, Palaeoecology |language=en |volume=615 |pages=111463 |doi=10.1016/j.palaeo.2023.111463 |bibcode=2023PPP...615k1463J |s2cid=257061069 |issn=0031-0182}}</ref> It has been suggested that there were at least three dispersal events from European Amphicyon into Eastern Asia, with the first one being the ancestors of the North American species, the second one dating to the Early Miocene or earliest Middle Miocene, leading to ''A. zhanxiangi,'' and the last one, that of the ''A. ulungurensis'' lineage, which occurred slightly later. There was generally no closer affinity between the Chinese amphicyonids and those of the Indian Subcontinent during the middle Miocene.<ref name=":32" /> However, it has been proposed that the late Miocene ''A. lydekkeri'' from Pakistan, which is sometimes attributed to the separate genus ''Arctamphicyon'', is a descendant of ''A. zhanxiangi'', with the lineage immigrating from Northern China to Southern Asia. Further remains showcasing affinities with these species are also known from Yunnan, and their dispersal might be linked to the uplifting of the Tibetan Plateau and the strengthening of the Asian Monsoon.<ref name=":5" /> The attribution of the various ''Amphicyon'' species described from the South Asian Siwaliks is similarly questionable.<ref name=":14" /> They are found throughout the whole Miocene epoch, with ''A. shahbazi'' being known from the earliest Miocene, whereas remains of ''A. lydekkeri'' date to the latest Miocene (~7-5 Ma), making it one of the youngest amphicyonids known.<ref name=":21" /><ref name=":022">{{Cite journal |last1=Werdelin |first1=Lars |last2=Simpson |first2=Scott W. |date=2009 |title=The last amphicyonid (Mammalia, Carnivora) in Africa |url=http://www.bioone.org/doi/abs/10.5252/g2009n4a775 |journal=Geodiversitas |language=en |volume=31 |issue=4 |pages=775–787 |doi=10.5252/g2009n4a775 |issn=1280-9659 |s2cid=73677723}}</ref> A very large humerus from the Manchar formation indicates that a gigantic species was present in the Siwaliks during the early parts of the Middle Miocene.<ref>{{Cite journal |last1=Viranta |first1=S. |last2=Hussein |first2=S. T. |last3=Bernor |first3=R. L. |date=2004 |title=The Anatomical Characteristics of a Giant Miocene Amphicyonid (Carnivora) Humerus from Pakistan |url=https://www.academia.edu/25187305 |journal=Pakistan Journal of Zoology |volume=36 |issue=1 |pages=1–6}}</ref> South East Asian reports include a large incisor from the Aquitanian (~23-21 Ma) of Vietnam, and a species from the Lower Irrawaddy Formation of Myanmar, which is likely closely related to ''Arctamphicyon''.<ref>{{Cite journal |last1=Prieto |first1=Jerome |last2=Antoine |first2=Pierre-Olivier |last3=Made |first3=Jan van der |last4=Metais |first4=Gregoire |last5=Phuc |first5=Laq The |last6=Quan |first6=Quy Truong |last7=Schneider |first7=Simon |last8=Tran |first8=Dang Ngoc |last9=Vasilyan |first9=Davit |last10=Viet |first10=Luong The |last11=Böhme |first11=Madelaine |date=2018 |title=Biochronological and palaeobiogeographical significance of the earliest Miocene mammal fauna from Northern Vietnam |url=https://epub.ub.uni-muenchen.de/67976/ |journal=Palaeobiodiversity and Palaeoenvironments |volume=98 |issue=2 |pages=287–313 |doi=10.1007/s12549-017-0295-y |s2cid=134056591 |issn=1867-1594}}</ref><ref name=":5" /> Scarce dental remains have also been reported from the Saudi Arabian Dam Formation, which dates to ca 17-15 Ma, in 1982. These remains show morphological differences to ''A. major'', and several of the species to which it had been compared, mostly because of their similar, small size, including ''A. bohemicus'', ''A. styriacus'' and ''A. steinheimensis'' (which also shares the apomorphic features present in the Arabian taxon), have since been moved to other genera.<ref name=":20" /><ref>{{Cite journal |last=H |first=Thomas |date=1982 |title=The lower Miocene fauna of Al-Sarrar (Eastern Province, Saudi Arabia) |url=https://cir.nii.ac.jp/crid/1571417125838654720 |journal=ATLAL, Journal of Saudi Arabian Archaeology |volume=5 |pages=109–136}}</ref><ref>{{Cite journal |last1=Peigne |first1=Stephane |last2=Salesa |first2=Manuel J. |last3=Anton |first3=Mauricio |last4=Morales |first4=Jorge |title=A New Amphicyonine (Carnivora: Amphicyonidae) from the Upper Miocene of Batallones-1, Madrid, Spain |date=2008 |journal=Palaeontology |language=en |volume=51 |issue=4 |pages=943–965 |doi=10.1111/j.1475-4983.2008.00788.x|bibcode=2008Palgy..51..943P |s2cid=55334897 |doi-access=free }}</ref>
The only definitive African remains of ''Amphicyon'' are from Arrisdrift in Namibia, which has variously been dated to 17.5 Ma or 16 Ma, and belong to the species ''A. giganteus''.<ref>{{Cite journal |last=Pickford |first=Martin |date=1995 |title=Suidae from the Middle Miocene of Arrisdrift, Namibia |url=https://www.researchgate.net/publication/288592776 |journal=Comptes Rendus de l'Académie des Sciences}}</ref><ref>{{Cite journal |last1=Van Couvering |first1=John A. |last2=Delson |first2=Eric |date=2020-12-01 |title=African Land Mammal Ages |url=https://doi.org/10.1080/02724634.2020.1803340 |journal=Journal of Vertebrate Paleontology |volume=40 |issue=5 |pages=e1803340 |doi=10.1080/02724634.2020.1803340 |bibcode=2020JVPal..40E3340V |s2cid=229372221 |issn=0272-4634}}</ref><ref name=":0" /> Further remains from this species have also been reported from the slightly older locality Moghra in Egypt, and it has been suggested that a mandible from Gebel Zelten, which is of similar age, in Libya indicates the presence of another, smaller species of the genus in the early Miocene of Africa.<ref name=":24" /> However, other authors assign these fossils to ''[[Afrocyon]]'' and ''[[Mogharacyon]]'', respectively.<ref name=":2" /> Much younger remains of large, African amphicyonids have previously been referred to ''Amphicyon''.<ref name=":022"/> Most notable among these are a molar and fragmentary postcranial remains from the [[Lothagam|Lower Nawatwa Formation]], dating to 7.4 ± 0.1 – 6.5 ± 0.1 Ma, which represents one of the youngest amphicyonids known.<ref name="S03">{{Cite book |last1=Leakey |first1=Meave G. |url=https://books.google.com/books?id=7qerAgAAQBAJ&q=Lothagam |title=Lothagam: The Dawn of Humanity in Eastern Africa |last2=Harris |first2=John Michael |date=2003 |publisher=Columbia University Press |isbn=978-0-231-11870-5 |language=en}}</ref> Others tentatively refer this taxon to the genus ''[[Myacyon]]''.<ref name=":23">{{Cite journal |last1=Morales |first1=Jorge |last2=Pickford |first2=M. |last3=Valenciano |first3=Alberto |date=2016 |title=Systematics of African Amphicyonidae, with descriptions of new material from Napak (Uganda) and Grillental (Namibia) |journal=Journal of Iberian Geology|url=https://digital.csic.es/handle/10261/137042 |doi=10.13039/501100003329 |issn=1698-6180 |hdl=10261/137042}}</ref>
The migration of ''Amphicyon'' from Eurasia to North America was part of a trans-[[Beringia]]n faunal exchange between the two continents during the Early Miocene. The oldest North American member of the genus is ''A. galushai'', which first appeared between 18.8 and 18.2 Ma. It likely gave rise to the larger ''A. frendens'', which itself was ancestral to the huge ''A. ingens'', which was also the last North American member of the genus, disappearing around 14.2 Ma. This lineage was probably endemic to North America, and is mostly known from the Great Plains, although remains of ''A. ingens'' were also discovered in California and New Mexico.<ref name=":03" /> Another species, ''A. longiramus'', is known from the Thomas Farm Site of Florida, which dates to ca. 18 Ma, and possibly the Pollack Farm Local Fauna of Delaware, as well as the Texan Garvin Gully fauna, which are of similar age. The relationship of this species to the Great Plains lineage is unclear.<ref name=":27" /><ref name=":28" /><ref>{{Cite journal |last=Wilson |first=John Andrew |date=1960 |title=Miocene Carnivores, Texas Coastal Plain |url=https://www.jstor.org/stable/1301024 |journal=Journal of Paleontology |volume=34 |issue=5 |pages=983–1000 |jstor=1301024 |issn=0022-3360}}</ref><ref>{{Cite journal |last=Albright |first=L. Barry |date=1998-01-01 |title=The Arikareean Land Mammal Age in Texas and Florida: Southern extension of Great Plains faunas and Gulf Coastal Plain endemism |url=https://www.researchgate.net/publication/235984524 |journal=Geological Society of America |language=en |doi=10.1130/0-8137-2325-6.167|isbn=9780813723259 }}</ref>
==References==
{{Reflist|2}}
{{Commons category|Amphicyon}}
{{Amphicyonidae|A.|state=collapsed}}
{{Taxonbar|from=Q139110}}
{{Portal|Paleontology}}
[[Category:Miocene mammals of Europe]]
[[Category:Amphicyonidae]]
[[Category:Oligocene caniforms]]
[[Category:Miocene Amphicyonidae]]
[[Category:Miocene mammals of Asia]]
[[Category:Miocene mammals of North America]]
[[Category:Aquitanian genus first appearances]]
[[Category:Tortonian extinctions]]
[[Category:Fossil taxa described in 1836]]
[[Category:Prehistoric carnivoran genera]]