Carnivora
OrdreRègne AnimaliaBowdich, 1821Diversité décrite (Catalogue of Life)
655
genres
29
familles
570
espèces
1
variety
2
suborder
20
subfamily
778
sous-espèces
Statut de conservation IUCN (parmi les espèces évaluées)
- LC207 (57.2%)
- VU53 (14.6%)
- NT39 (10.8%)
- EN30 (8.3%)
- NA10 (2.8%)
- CR10 (2.8%)
- EX6 (1.7%)
- DD5 (1.4%)
- RE2 (0.6%)
Distribution biogéographique
- Southern Asia114 esp.
- Africa93 esp.
- Europe & Northern Asia (excluding China)68 esp.
- South America63 esp.
- North America60 esp.
- Middle America43 esp.
- East Pacific16 esp.
- Indo-West Pacific14 esp.
- Australia12 esp.
- Western Atlantic Ocean9 esp.
- Caribbean9 esp.
- Eastern Atlantic Ocean8 esp.
- Antarctica/Southern Ocean8 esp.
- Oceania3 esp.
- DISTRIBUTION: Latest Oligocene, late midArikareean, John Day Formation, Wheeler County, Oregon.1 esp.
- DISTRIBUTION: Mid- or late Arikareean, John Day Formation, John Day valley, Oregon.1 esp.
- DISTRIBUTION:? Mid-Arikareean, Arikaree Group, near head of Warbonnet Creek, Sioux County, Nebraska.1 esp.
- Distribution. Circumpolar in the Southern Ocean.1 esp.
- Distribution. Mainly in NW Hawaiian Is (Kure Atoll, Midway Atoll, Pearl and Hermes Reef, Lisianski I, Laysan I, and French Frigate Shoals) but increasingly seen at the main Hawaiian Is.1 esp.
- DISTRIBUTION: Late Arikareean, Harrison Formation and basal Anderson Ranch Formation, Agate Fossil Beds National Monument, Sioux County, Nebraska.1 esp.
- Elle est rare, et nous ne Favons trouvée qu`au sein des forêts clıaudes et humides du pied oriental des Andes boliviennes au pays des Yuracares.1 esp.
- DISTRIBUTION: Iriomote Isl. (Ryukyu Isis.)1 esp.
- DISTRIBUTION: Late Arikareean, upper Arikaree Group, Sioux County, Nebraska.1 esp.
- Habitat in America.1 esp.
- Habitat in Europa, Asia.1 esp.
- DISTRIBUTION: Early or mid-Arikareean, John Day Formation, Grant County, Oregon.1 esp.
- LOCALITY. — China, Songlinzhuang, Sihong area, Jiangsu Province. Sihong Fauna, Xiacaowan Formation (Qiu Z. - D. & Qiu 2013), late Early Miocene Shanwangian (Qiu Z. - X. et al. 2013).1 esp.
- DISTRIBUTION: Early Oligocene of northcentral Mongolian People’s Republic. Dashzeveg (1996: fig. 1) reported that Amphicynodon teilhardi occurs in both the lower Tatal Member and upper Shand Member of the Hsanda Gol Formation. An undescribed record was reported in the early Oligocene KhatanKhayrkhan locality of Altai Province of Mongolia by Russell and Zhai (1987: 324). EMENDED DIAGNOSIS: As the only known species from Asia, Amphicynodon teilhardi differs from all European species of the genus, except A. velaunus, in its shortened m 2, along with a correspondingly reduced M 2, in contrast to a primitively long m 2 and large M 2 in most European species. A. teilhardi primitively retains a distinct posterior accessory cusp on p 4, which is lost or extremely reduced in the European A. gracilis, A. speciosus, and A. velaunus. A. teilhardi further differs from European A. typicus, A. gracilis, and A. crassirostris in its relatively low hypoconid of m 1 with wrinkled enamel, in contrast to a trenchant talonid in the latter three species.1 esp.
- DISTRIBUTION: Early Oligocene of northcentral Mongolia. An undescribed record was mentioned in the early Oligocene Khatan Khayrkhan locality of Altai Province of Mongolia by Russell and Zhai (1987: 324). GEOLOGY AND AGE: The above referred specimens of Amphicticeps shackelfordi come from three localities (some specimens lack a detailed locality record): (1) general vicinity of Loh for AMNH 19017 and 19127; (2) 2 mi southwest of Loh for AMNH 19010, AMNH 19128, MAE BU. 91.9187 – 90, and MAE M 217; (3) general vicinity or 2 mi west of the Ulaan Khongil (‘‘ Grand Canyon’ ’ or Tatal Gol) for AMNH 21695 and 83610. While field studies are currently pursued by the ongoing joint expeditions of the MAE and formal stratigraphic revisions will have to wait for that result (see Höck et al., 1999, for a recent summary), it is relevant to note here that the above three Amphicticeps producing localities fall within a more restricted concept of the Hsanda Gol Formation close to the level of a discontinuous but approximately contemporary basaltic lava (Basalt I of Höck et al., 1999). Historic collections are largely concentrated in the Ulaan Khongil fauna in the lower part of the Hsanda Gol Formation below the prominent basaltic lava and immediately above. Amphicticeps specimens from near the Loh campsite and 2 mi southwest of Loh (including the holotype) are darkly stained due to the percolation of ground water, and they all belong to the Ulaan Khongil fauna. AMNH 21695 and 83610 from near the ‘‘ Grand Canyon’ ’ area, on the other hand, are lightcolored and may belong to the Zavlia fauna in the upper part of the Hsanda Gol Formation above the lava. This presumed younger age of AMNH 21695 and 83610 relative to the rest of the A. shackelfordi hypodigm is also consistent with the former’s wider m 1 and more prominent lingual cingulum on the m 1 trigonid, tendencies that indicate a slightly more advanced stage of evolution for the species. EMENDED DIAGNOSIS: Amphicticeps shackelfordi is distinguishable from the more derived A. makhchinus and A. dorog by its smaller size, smaller angle between the labial borders of P 4 and M 1, more enlarged M 1 parastyle, larger M 1 metaconule, more reduced anterior cingulum of M 1, and more lingually located M 2. In addition, the P 4 protocone of A. shackelfordi is larger than in A. dorog, but is less well developed than in A. makhchinus.1 esp.
- DISTRIBUTION: Early Arikareean, John Day Formation, Oregon.1 esp.
Régions biogéographiques agrégées depuis Catalogue of Life Cross-References (distribution par espèce déclarative).
Profil de traits agrégé
- wikidata_iucn_status288 esp.Least Concern173Vulnerable44Near Threatened31
- max_longevity_y279 esp.-83.25à56.00yearsmoy -10.71
- diet_plant_other_pct278 esp.0.00à90.00%moy 3.53
- diet_fruit_pct278 esp.0.00à80.00%moy 8.42
- diet_nectar_pct278 esp.0.00à20.00%moy 0.07
- binomial_msw05278 esp.Ailuropoda melanoleuca1Ailurus fulgens1Acinonyx jubatus1
- body_mass_g278 esp.57.00à1600000.00gmoy 40364.61
- aet_mean_mm278 esp.-999.00à1840.00mmmoy 557.79
- adult_forearm_length_mm278 esp.-999.00à246.00mmmoy -994.52
- body_mass_source278 esp.Ref_117227Ref_5826"Ref_2, Ref_3"19
- adult_body_mass_kg278 esp.-1.00à1600.00kgmoy 42.11
- diet_breadth278 esp.-999.00à7.00moy -176.79
Traits agrégés sur les espèces du taxon (matview taxon_traits_best : WoRMS, FishBase, EBird, GBIF, EOL, TRY…).
Taxons enfants directs (52)
- Genre Acheronictis1
- Famille Adapisoriculidae7
- Genre Adracon1
- Genre Aeluropsis
- Famille Amphicynodontidae6
- Famille Amphicyonidae55
- Genre Arikarictis1
- unranked BOLD:AAE9178
- unranked BOLD:AAF6571
- unranked BOLD:AAH2944
- unranked BOLD:AAJ1863
- unranked BOLD:AAJ7206
- unranked BOLD:AAJ7207
- unranked BOLD:AAN3846
- unranked BOLD:AAU5960
- unranked BOLD:ABW9198
- Famille Barbourofelidae9
- Genre Bestiopeda
- Sous-ordre Caniformia11
- Genre Carnivoripeda
- Genre Chaprongictis
- Genre Creodontipus
- Cuon
- Genre Cynelos1
+ 28 taxons enfants supplémentaires
- Famille Desmatophocidae4
- Famille Didymictidae
- Genre Dormaalocyon
- Genre Elmensius
- Famille Enaliarctidae1
- Genre Eodesmatodon
- Sous-ordre Feliformia8
- Genre Lonchocyon
- Famille Lophocyonidae4
- Genre Lycophocyon1
- Genre Mellivorodon
- Genre Mustelipeda
- Famille Nimravidae12
- Genre Notoamphicyon
- Genre Pacificotaria
- Famille Palaeogalidae2
- Genre Paruusipeda
- Genre Pinnarctidion
- Genre Plesiocyon
- Proteles
- Genre Pteronarctos
- Genre Puijila
- Genre Ravenictis
- Genre Shandgolictis
- Famille Stenoplesictidae2
- Famille Subparictidae3
- Genre Viretictis
- Famille Viverravidae15
Source : Catalogue of Life (Cross-References) — données live sur les taxons enfants. Comparaison avec estimations externes (sources bibliographiques) quand disponibles.
Espèces représentatives (570)
1–50 sur 570Tri :
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Source : Catalogue of Life (espèces acceptées) · Photos Commons/Wikidata · Statut IUCN Red List · Connectivité : matview species_connectivity_rank (GloBI agrégé).
Liens externesWikipedia · EOL · Wikidata · IUCN · GBIFExpert
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