Myacyon
| Myacyon | |
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Научная классификация 
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| Домен: | Эукариота |
| Королевство: | Животное |
| Филум: | Chordata |
| Сорт: | Млекопитающие |
| Заказ: | Хищник |
| Семья: | † amphicyonidae |
| Род: | † MyAcyon Sudre and Hartenberger, 1992 |
| Тип видов | |
| †Myacyon dojambir Sudre and Hartenberger, 1992
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| Other species | |
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| Synonyms | |
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Myacyon - это вымерший род карниворских млекопитающих большого размера, принадлежащих к семейству Amphicyonidae («Bear Dogs»), которые жили в Африке во время миоценовой эпохи. Из -за ограниченного объема и фрагментарного характера сильно поврежденного голотипа, а также иллюстраций в его описаниях, которые были названы неадекватными, использование этого рода создает серьезные проблемы. [ 1 ] [ 2 ] Тем не менее, это примечательно быть одним из последних выживших членов своей семьи и ее адаптации к гиперкарноделии . [ 3 ] Его отношения с другими амфичинидами неясны, и они не тесно связаны с Bonisicicyon , другим поздним выжившим африканским родом, хотя было предложено, чтобы он спускался от вида Cynelos [ 4 ] или намибиоцион . [ 5 ]
История и виды
[ редактировать ]Род был построен в 1992 году на основе сильно поврежденной и фрагментированной дистальной половины правой нижней челюсти , содержащей М1-М2, и еще не развернутый М3, обнаруженный в местности MYA в Алжире . [ 6 ] В 2005 году был описан видовый agnotherium kiptalami на основе морды, разбитой за вторым моляром (кНМ BN 488). [ 7 ] A revision of African amphicyonids by Morales et al. in 2016 moved this species, as well as all African material referred to Agnotherium to the genus Myacyon.[2] However, a redescription of Agnotherium in 2020 tentatively included material from Tunisia in this genus instead of Myacyon, although they note that the lack of definitive upper teeth belonging to Agnotherium does not allow them to confidently assign these remains. This material consists of a right maxilla fragment (NOM T-370), a proximal left radius fragment (NOM T-179) and a metatarsal V (NOM T-2269).[8] Morales et al. further referred teeth (KNM-LT 23049, KNM-LT 23073 and KNM-LT 23051) of a large amphicyonid from Lothagam, which represents one of the youngest occurrences of the family worldwide,[9] to Myacyon cf. kiptalami. Additionally, they proposed that a m2 from Beni Mellal, Morocco represents a new species.[2] In 2022 an isolated m2 from Napudet, Kenya was described, likely belong to another, enormous but currently undescribed species.[5]
The species ?Myacyon peignei was described in 2019 based on remains found in Kenya and tentatively assigned to the genus. It is only known from teeth—the holotype is a P4 (KNM-FT 3611), while the other remains are a left m1 (KNM-FT 3379) and right m1 (KNM-FT 3399).[1]
The genus name references the Wadi Mya, which is located close to the site where the remains were found. The species name dojambir is the Arabic word for “December”, the month in which the remains were discovered,[6] whereas the names of the other two species honor Kiptalam Cheboi[7] and Stéphane Peigné,[1] respectively.
Fossil distribution
[edit]M. dojambir -
- Oued Mya 1, Algeria, ca. 11.2-9 Ma[6]
M. kiptalami -
- Member D, Ngorora Formation, Kenya, ca. 12 Ma[7]
- Kipsaraman, Muruyur Formation, Kenya, ca. 14.5 Ma[10]
- Hondeklip Bay, South Africa, ca. 12 Ma[11]
M. cf. kiptalami -
- Bled Douarah, Beglia Formation, Tunisia, 13-11 Ma[12]
- Samburu Hills, Kenya, 9.5 Ma[13]
- Lower Nawata Formation, Lothagam, Kenya, 7.4 ± 0.1 – 6.5 ± 0.1 Ma[14]
?M. peignei -
- Fort Ternan, Kenya, early Serravallian, 13.8-13.7 Ma[1]
Myacyon sp. -
Description
[edit]Most material belonging to this genus suggests that Myacyon included large to very large amphicyonids. The dimensions of Myacyon dojambir and the m2 from Napudet approach those of the largest Amphicyon giganteus and the enormous Cynelos jitu, which have been estimated to weigh over 300 kg,[5][15] although the material from the Samburu Hills[13] and Beni Mellal is considerably smaller.[6] M. kiptalami is as large or slightly larger than a lion,[7] and the remains from Kipsaraman, Bled Douarah and Lothagam suggest a similar size,[2][10] ?M. peignei is not nearly as large, being smaller than most Early Miocene species of Cynelos, except for C. euryodon,[4] itself comparable in size to the 42 kg[16] heavy C. lemanensis.[2]
It is characterized by its sectorial molars, showing adaptions towards hypercarnivory.[17] The large m1 is unlike that of any other amphicyonid, possessing a shallow carnassial notch.[18] It has an elongated trigonid, a strong protoconid, which possesses a strong and tall trenchant anterior crest and a short talonid, with a robust, crested hypoconid and a far distally located entoconid which is small, poorly developed and lacks a crest. The paraconid is indistinct and separated from the protoconid by a very weak notch, which is visible on the buccal margin of the anterior crest, while the metaconid is reduced and situated slightly posteriorly. The short and oblong m2 lacks a paraconid and only possesses a poorly developed metaconid, which is situated at the level of the trenchant protoconid. Its talonid is short and narrower than the trigonid, possessing a strong hypoconid but lacking an entoconid. The trigonids of both teeth have a strong buccal cingulum. The m3 is present, but probably reduced.[6][12]
The cranial remains of M. kiptalami superficially resembles those of large felids and nimravids, with a short snout, enlarged canines and long diastemata. As in lions, the anterior extremities of its nasals flare outwards and slightly downwards, thereby shifting the nasal notches laterally and widening the nostrils. Its maxillo-premaxillary does not touch the nasals until it has reached the orbital line, which is much further back than in canids. Furthermore, the upper border of the stout premaxilla is lower than in dogs, but similarly projects anteriorly, even if it is less pointed, resulting in the incisors lying in an almost straight line, curved incisor battery of dogs. The incisors have steep roots and long axes and occlusal apices, which point sharply towards the rear. As a result of the outbowing of the maxilla in the region of the carnassial and molar, the maxilla is antero-posteriorly shortened. A further adaption towards shortening the snout is the 90° rotation of the P3 along the part of the maxilla in which it is located. It is tucked behind the parastyle of the carnassial, a position usually be filled by a protocone among other amphicyonids. Above it, a large infraorbital foramen is located. It furthermore possesses a large facial fossa, which lies anterior to the orbit and extends anteriorly and ventrally as a curved furrow immediately behind the canine jugum. As a result of these adaptions, Myacyon had a considerable gape, with canine tips extending 40 mm beneath the occlusal surface of the carnassial and incisors.[7]
M. peignei is only known from a handful teeth, although the development of the protoconid shelf on its P4 is a distinct feature of this taxon.[1]
Paleoecology
[edit]At Oued Mya, Myacyon coexisted with the equid Hipparion and the rhinoceros Aceratherium, as well as the giraffid Palaeotragus and proboscideans.[6]
The discoveries at Member D of the Ngorora Formation suggests that it was once covered by open woodland, with fluvial conditions being present.[19] Here Myacyon was found alongside the immense hyaenodont Megistotherium and its smaller relative Dissopsalis, the lioness-sized hyaena Percrocuta as well as a variety of smaller carnivorans.[7] A large variety of herbivores are known from this site, among them the proboscidean Deinotherium,[19] bovids, suids[20] and the early hippopotamus Kenyapotamus.[21] Fossils of crocodylians, freshwater turtles and fish have also been found.[21]
As indicated by palaeosol carbon isotope studies and tooth microwear patterns, Fort Ternan, where ?M. peignei has been found, was covered by open woodland and located adjacent to highlands.[22] The locality shares many taxons with the Ngorora Formation, among them Afrochoerodon, Climacoceras, Chilotheridium, Gentrytragus, Kipsigicerus, Dorcatherium and Kenyapotamus.[23] The carnivoran assemblage is also similar, including Percrocuta, Dissopsalis and Tugenictis, with a gigantic hyainailourine as the largest predator.[1] The hominoid Kenyapithecus is among the few genera unique to this site.[24]
References
[edit]- ^ Jump up to: a b c d e f Werdelin, Lars (2019). "Middle Miocene Carnivora and Hyaenodonta from Fort Ternan, western Kenya". Geodiversitas. 41 (6): 267–283. doi:10.5252/geodiversitas2019v41a6. S2CID 146620949.
- ^ Jump up to: a b c d e f Morales, Jorge; Pickford, M.; Valenciano, Alberto (2016). "Systematics of African Amphicyonidae, with descriptions of new material from Napak (Uganda) and Grillental (Namibia)". Journal of Iberian Geology. doi:10.13039/501100003329. hdl:10261/137042. ISSN 1698-6180.
- ^ Morlo, Michael; Miller, Ellen R.; Bastl, Katharina; Abdelgawad, Mohamed K.; Hamdan, Mohammed; El-Barkooky, Ahmed N.; Nagel, Doris (2019). "New Amphicyonids (Mammalia, Carnivora) from Moghra, Early Miocene, Egypt". Geodiversitas. 41 (1): 731–745. doi:10.5252/geodiversitas2019v41a21. ISSN 1280-9659. S2CID 208284245.
- ^ Jump up to: a b Morlo, M.; Friscia, A.; Miller, E.; Locke, Ellis M.; Nengo, I.; Morlo (2021). "Systematics and paleobiology of Carnivora and Hyaenodonta from the lower Miocene of Buluk, Kenya". S2CID 237336425.
- ^ Jump up to: a b c d Morlo, M.; Nengo, I. O.; Friscia, A.; Mbogo, W.; Miller, E. R.; Russo, G. A. (2023). "Presence of a giant amphicyonid and other carnivores (Mammalia) from the Middle Miocene of Napudet, Kenya". Journal of Vertebrate Paleontology. 42 (2). e2160643. doi:10.1080/02724634.2022.2160643. S2CID 256354136.
- ^ Jump up to: a b c d e f Sudre, Jean; Hartenberger, Jean-Louis (1992-01-01). "Oued Mya 1, nouveau gisement demammifères du Miocène supérieur dans le sud Algérien". Geobios (in French). 25 (4): 553–565. doi:10.1016/S0016-6995(92)80083-P. ISSN 0016-6995.
- ^ Jump up to: a b c d e f Morales, J.; Pickford, M.H.L. (2005). "Carnivores from the Middle Miocene Ngorora Formation (13-12 Ma), Kenya". Estudios Geológicos. 61 (3). doi:10.3989/egeol.05613-668.
- ^ Morlo M, Bastl K, Habersetzer J, Engel T, Lischewsky B, Lutz H, von Berg A, Rabenstein R, Nagel D. 2020. The apex of amphicyonid hypercarnivory: solving the riddle of Agnotherium antiquum Kaup, 1833 (Mammalia, Carnivora). Journal of Vertebrate Paleontology 39(5):e1705848 DOI 10.1080/02724634.2019.1705848.
- ^ Werdelin, Lars (2003). Mio-Pliocene Carnivora from Lothagam, Kenya. In: Lothagam: The Dawn of Humanity in Eastern Africa pp. 261–328. New York. Columbia University Press. ISBN 0-231-11870-8.
- ^ Jump up to: a b Morales, Jorge; Pickford, Martin (2008-12-01). "Creodonts and carnivores from the Middle Miocene Muruyur Formation at Kipsaraman and Cheparawa, Baringo District, Kenya". Comptes Rendus Palevol. Les Carnivora d'Afrique du Miocène moyen au Pléistocène : Nouvelles données, systématique, évolution, biogéographie/African Carnivora from the Middle Miocene to the Pleistocene: New data, systematics, evolution, biogeography. 7 (8): 487–497. doi:10.1016/j.crpv.2008.09.011. ISSN 1631-0683.
- ^ Pickford, Martin; Senut, Brigitte (1997). "Cainozoic mammals from coastal Namaqualand, South Africa" (PDF). Palaeontologia Africana. 34.
- ^ Jump up to: a b Werdelin, Lars (2010). Cenozoic Mammals of Africa. University of California Press. ISBN 978-0520257214.
- ^ Jump up to: а беременный Цудзикава, Хироши (2005). «Обновленная фауна в позднем миоцене из Самбуру Хиллз, Северная Кения» . Африканские учебные монографии. Дополнительная проблема . 32 : 1–50. doi : 10.14989/68471 . ISSN 0286-9667 .
- ^ Storrs, GW (2003). Числовой контроль возраста для миоценовой плиоценовой последовательности в Лотагаме, гоминоид-несущая последовательность в северной Кении. В: Лотагам: Рассвет человечества в Восточной Африке, стр. 43–6 Нью-Йорк. Издательство Колумбийского университета. ISBN 0-231-11870-8 .
- ^ Мигающий, Пекка; Линнавуори, Рауно; Virranta, Suvi (1996). Европейская миоцена Amphicyonidae: таксономия, систематика и экология . Финский зоологический и ботанический паб. Доска. ISBN 978-951-9481-47-0 .
- ^ Солнце, цветочный; Спорт, Жан-Франсуа; Хейц, Антуан; Mennecart, Bassion (2022-06-15). "Плотно, плотоядное животное, плотоядное животное, плотоядное животное , ПЕРЕЙ 10 : E13457. два 10.7717/peerj.13457: ISSN 2167-8 9206431PMC 35726261PMID
- ^ Моралес, Хорхе; Пивовар, PIP; Мартин, Пикфорд (2010). «Плотоядные (креодонта и плотоядные) из базального среднего миоцена Гебель Зелтен, Ливия, с нотой на большом амфичиониде из среднего миоцена Ngorora, Кения» . Бюллетень геологического общества Тетиса . 5 : 43–54.
- ^ Верделин, Ларс; Симпсон, Скотт В. (2009). «Последний амфионид (млекопитающие, плотова) в Африке » GeoDiversitass 31 (4): 775–7 Doi : 10.5252/ g2009n4a7 ISSN 1280-9 S2CID 73677723
- ^ Jump up to: а беременный Епископ, WW; Чепмен, Гр (1970). «Ранние плиоценовые отложения и окаменелости из северной Кении рифтовой долины» . Природа . 226 (5249): 914–918. doi : 10.1038/226914A0 . ISSN 1476-4687 . PMID 16057593 . S2CID 4289662 .
- ^ Пикфорд, Мартин (2001). «Новые виды Listroidon (Suidae, Mammalia) из Bartule, член A, Ngorora Formation (около 13 мА), Туген -Хиллз, Кения» . Анналес де палеонтологии . 87 (3): 207–221. doi : 10.1016/s0753-3969 (01) 80010-0 .
- ^ Jump up to: а беременный Пикфорд, М. (2011-12-30). «Уганда Morotocchoerus (17,5 млн лет) и Кеньяпотамус де Кениа (13-11 млн лет): последствия для происхождения гипопотамид » . Геологические исследования (на испанском). 67 (2): 523–540. Doi : 10.3989/egeol.40393.205 . ISSN 1988-3250 .
- ^ Пеннингтон, Pt; Cronk, QCB; Ричардсон, JA; Джейкобс, Бонни Ф. (2004-10-29). «Палеоботанические исследования по тропической Африке: отношение к эволюции биомов леса, леса и саванны» . Философские транзакции Королевского общества Лондона. Серия B: Биологические науки . 359 (1450): 1573–1583. doi : 10.1098/rstb.2004.1533 . PMC 1693443 . PMID 15519973 .
- ^ Пикфорд, Мартин; Савада, Йоширо; Таяма, Рёчи; Мацуда, Ю-Ко; Итая, Тецумару; Hyodo, Hironobu; Senut, Brigitte (2006-06-01). «Уточнение эпохи средних миоценовых кроватей Форт -Тернан, Западная Кения и его последствия для биохронологии Старого Света » Comptes rendus Geoscience 338 (8): 545–555. Doi : 10.1016/ j.crte.2006.02.0 ISSN 1631-0
- ^ Каппельман, Джон (1991-02-01). «Палеоокружение Ofkenyapithecus в форте Тернан» . Журнал человеческой эволюции . 20 (2): 95–129. doi : 10.1016/0047-2484 (91) 90053-x . ISSN 0047-2484 .
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