Langebaanweg’s sabertooth guild reveals an African Pliocene evolutionary hotspot for sabertooths (Carnivora; Felidae)

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•Langebaanweg’s (LBW) sabertooth cat’s guild includes two new species•Dinofelis from LBW is the potential ancestor of Plio-Pleistocene Dinofelis•We confirm a Pan-African distribution Adeilosmilus and Lokotunjailurus•Comparison with Eurasian felid implies open environment at Here, we describe revise craniodental material Langebaanweg ‘E’ Quarry (South Africa, early Pliocene, ∼5.2 Ma), which represents one largest best-preserved collections felids Mio-Pliocene deposits Africa. Four taxa, including species, are recognized: Lokotunjailurus chinsamyae sp. nov., aff. kabir, Yoshi obscura, Dinofelis werdelini nov. The composition analyzed herein suggests presence mosaic components in region, shows relationship that Yuanmou, suggesting similar and/or dispersal route/event. reassessment rich Pliocene step toward understanding transition evolution southern hemisphere during late Miocene to Pliocene. witnessed global climate change colder environment.1Zachos J. Pagani M. Sloan L. Thomas E. Billups K. Trends, rhythms, aberrations 65 Ma present.Science. 2001; 292: 686-693https://doi.org/10.1126/science.1059412Crossref PubMed Scopus (7758) Google Scholar,2Westerhold T. Marwan N. Drury A.J. Liebrand D. Agnini C. Anagnostou Barnet J.S.K. Bohaty S.M. De Vleeschouwer Florindo F. et al.An astronomically dated record Earth's its predictability over last 66 million years.Science. 2020; 369: 1383-1387https://doi.org/10.1126/science.aba6853Crossref Scholar Late fauna experienced significant Europe around boundary, documenting shift more savannah-like closed forest environment.3Koufos G.D. Vasileiadou Miocene/Pliocene mammal faunas Balkans: implications for biostratigraphy palaeoecology.Paleobiodivers. Paleoenviron. 2015; 95: 285-303https://doi.org/10.1007/s12549-015-0201-4Crossref (27) This contrasts eastern Africa where, Miocene, changed open, arid grassland or desert, continued into Pliocene.4Cerling T.E. Harris J.M. MacFadden B.J. Leakey M.G. Quade Eisenmann V. Ehleringer J.R. Global vegetation through boundary.Nature. 1997; 389: 153-158https://doi.org/10.1038/38229Crossref (1612) Scholar,5Hoetzel S. Dupont L.M. Wefer G. Miocene–Pliocene south-western (ODP Site 1081, offshore Namibia).Palaeogeogr. Palaeoclimatol. Palaeoecol. 423: 102-108Crossref (21) Scholar,6Feakins deMenocal P. african regional cenozoic.in: Werdelin Cenozoic Univ California Press, 2010: 45-55Crossref Scholar,7Dupont Rommerskirchen Mollenhauer Schefuß changes South African hydrology relation expansion C4 plants.Earth Planet Sci. Lett. 2013; 375: 408-417Crossref (53) Scholar,8Herbert T.D. Lawrence K.T. Tzanova A. Peterson L.C. Caballero-Gill R. Kelly C.S. cooling rise modern ecosystems.Nat. Geosci. 2016; 9: 843-847https://doi.org/10.1038/ngeo2813Crossref (473) Scholar,9Uno Polissar P.J. Jackson K.E. P.B. Neogene biomarker Africa.Proc. Natl. Acad. USA. 113: 6355-6363https://doi.org/10.1073/pnas.1521267113Crossref (93) Located on west coast (Figure 1), most important fossil communities document environmental animal Africa.10Roberts D.L. Matthews Herries A.I. Boulter Scott Dondo Mtembi Browning Smith R.M. Haarhoff Bateman M.D. Regional context cenozoic langebaanweg palaeontological site: Coast Africa.Earth Rev. 2011; 106: 191-214https://doi.org/10.1016/j.earscirev.2011.02.002Crossref (86) Scholar,11Hendey Q.B. Geological succession langebaanweg, Cape province, events tertiary.South Afr. 1981; 77: 33-38Google Baard’s comprise part locality located ∼13–15 km inland Saldanha Bay Africa’s 1).12Hendey Carnivora southwestern province Africa.Ann. Mus. 1974; 63: 1-369Google They were commercially exploited as open-cast phosphate mines 1943 1993. Singer Hooijer13Singer Hooijer D.A. A stegolophodon Africa.Nature. 1958; 182: 101-102https://doi.org/10.1038/182101a0Crossref (7) reported first occurrence Tertiary vertebrate fossils area, describing remains an elephant′s relative ‘Baard’s Quarry’ was later back-filled.14Hendey Q. age Baard's Quarry, Langebaanweg, 1978; 75: 1-24Google Fossils fragmentary show evidence rolling. thought originate river lag deposit reworked below level 2 may have been contemporaneous. In 1965, mining started Varswater mine, 2.5 producing diverse Langebaanweg.11Hendey Scholar,12Hendey Scholar,15Hendey Palaeoecology occurrences in" E" reinterpretation their geological context.Ann. 84: 1-104Google Fieldwork began 1965 continues until today. occur Formation spans middle (Langhian) (Zanclean).10Roberts Scholar,16Tankard langebaanweg–saldanha province.Trans. Geol. Soc. 263-283Google Scholar,17Hendey Langebaanweg: Record Past Life Museum).1989Google All terrestrial carnivoran Quarry,12Hendey Scholar,18Hendey ursid 1972; 59: 115-132Google Scholar,19Hendey Fossil bear south-africa.South 1977; 73: 112-116Google Scholar,20Hendey H. tertiary mustelidae (mammalia, Carnivora) 76: 329-357Google Scholar,21Hendey Hyaenidae relevance phylogeny family.Ann. 265-297Google Scholar,22Hendey Agriotherium ursidae) relationships genus.Ann. 1980; 81: 1-109Google Scholar,23Valenciano Govender New mellivora benfieldi Carnivora, mustelidae) langebaanweg,‘E’Quarry pliocene): Re-evaluation mellivorines.J. Vertebr. Paleontol. 40e1817754Crossref (11) Scholar,24Valenciano insights giant mustelids site (West Park, pliocene).PeerJ. 8e9221Crossref Scholar,25Valenciano Morales Eucyon khoikhoi nov.(carnivora: canidae) ‘E’Quarry (early pliocene, Africa): complete canini mio-pliocene.Zool. Linn. 2022; 194: 366-394Crossref (5) described herein, come Langeberg Quartz Sand Member (LQSM) Muishond Fontein Pelletal Phosphorite (MPPM). concentrated within ‘abbreviated’ stratigraphic interval ca 26–30 m above sea level10Roberts Scholar, p. 208 associated numerous transgressive-regressive episodes.10Roberts Scholar,26Roberts formation (including langeenheid clayey Sand, KoningVlei gravel, phosphatic member).in: Johnson Catalogue lithostratigraphic units. Committee Stratigraphy, 2006: 27-31Google LQSM deposited lagoonal estuarine setting protected wave action but sea.10Roberts Scholar,27Kensley B. marine invertebrates province.Ann. 60: 173-190Google Scholar,28Kensley second assemblage invertebrate Cape.Ann. 72: 189-210Google MPPM, Beds 3aN 3aS, shallow embayment sheltered ocean by granitic islands transgression.29Smith Sedimentology taphonomy pliocene sivathere bonebed western Africa.African Natural History. 2006; 2: 197-198Google Both beds inferred very close age, Bed 3aS being slightly older.11Hendey However, ages MPPM estimated palaeomagnetic data reconstructions ∼5.15 ± 0.1 Ma, accumulated stage Early transgression when 30m present level.10Roberts Quarry12Hendey Scholar,14Hendey interpreted much recent (late Pleistocene). well-suited because temporal position geographic location tip Africa.30Werdelin 201-202Google It extremely fossiliferous, than 230 documented species,15Hendey providing key information reconstruction animals this region. taxonomy, evolution, diversity therefore precise paleoenvironment. Following initial systematic study led Hendey,27Kensley Scholar,31Gentry A.W. bovidae (mammalia) 79: 213-337Google Scholar,32Hendey Further observations mammalian Langebaanweg.Cape Province. Paleoecology. 6: 172-175Google Scholar,33Hendey 1976; 69: 215-247Google Scholar,34Hooijer equidae Province, Africa.Zool. Verhandel. 148: 1-39Google Scholar,35Hooijer rhinoceros 151-191Google Scholar,36Pocock microfauna genus linking Otomyinae Murinae.South 58-60Google Scholar,37Simpson G.G. penguin 1979; 78: 1-9Google Scholar,38Harris giraffoidea artiodactyla) 325-353Google continuous taxonomic revision macro-mammal fossils, hyaenids,39Werdelin Turner Solounias Studies hyaenids: genera hyaenictis gaudry chasmaporthetes hay, reconsideration hyaenidae 1994; 111: 197-217https://doi.org/10.1111/j.1096-3642.1994.tb01483.xCrossref (47) viverrids,40Hunt R.J. Basicranial anatomy viverrid Africa.in: Stewart Seymour Churcher palaeoenvironments mammals: Tributes career CS Churcher. University Toronto 1996: 588-597Crossref mustelids,23Valenciano canids,25Valenciano equids,41Bernor R.L. Kaiser T.M. Systematics paleoecology earliest equid, Eurygnathohippus hooijeri n. Africa.Mitt. Hambg. Zool. Inst. 103: 149-186Google proboscideans42Sanders W.J. Taxonomic review proboscidea Africa.Trans. Roy. 2010; 62: 1-16https://doi.org/10.1080/00359190709519192Crossref (28) has undertaken. Sabertooth cats also group Langebaanweg. species sabertooth, cf. Homotherium sp., Machairodus diastemata, Felis Hendey.12Hendey Several studies discussed mentioned taxa fauna, e.g. Sardella,43Werdelin Sardella origin Homotherium.pala. 277: 123-130Crossref Peigné,44Werdelin Peigné Carnivora.in: Sanders Mammals 609-664Crossref obscura Turner,45Turner neogene/lower Pleistocene Felidae Africa: dispersal.Quartarpalaontologie. 1990; 8: 247-256Google diastemata Lewis,46Werdelin Lewis M.E. Felidae).Zool. 132: 147-258Crossref no comparison focused any these sabertoothed whole. Recently, knowledge Mio-Pleistocene greatly improved,46Werdelin Scholar,47Antón Salesa M.J. First known skulls scimitar-toothed cat aphanistus (Felidae, Spanish Batallones-1.J. 2004; 24: 957-969Crossref (89) Scholar,48Salesa Antón Alcalá Montoya Systematic sabre-toothed Paramachaerodus Spain.Palaeontology. 53: 1369-1391Crossref (48) Scholar,49Werdelin lothagam, Kenya.in: J.D. Lothagam: dawn humanity Columbia 2003: 261-328Crossref Scholar,50de Bonis Taisso Mackaye Likius Vignaud Brunet Toros Menalla (Chad).Comptes Rendus Palevol. 221-227https://doi.org/10.1016/j.crpv.2010.07.018Crossref Scholar,51Spassov Geraads balkans contents Metailurus Zdansky, 1924 (Carnivora, Felidae).J. Mamm. Evol. 22: 45-56Crossref (20) enabling current presents update dentognathic comprising classical material12Hendey previously unpublished (Table S1). Our main goal our composed genera, better understand paleobiology ecology guilds sabertooths Order Bowdich, 1821.Family Fischer, 1817.Subfamily Machairodontinae Gill, 1872.Tribe Machairodontini 1872.Lokotunjailurus Werdelin, 2003. Type species: emageritus Included fanonei al., 2010 Chronology distribution: Currently central, eastern, Amended diagnosis: medium large size. Very infraorbital foramen. Alisphenoid canal present. Glenoid fossa antero-posteriorly elongated, overhung. Mandibular flange absent weak, horizontal ramus slender, ascending relatively tall machairodont cat. Upper canine moderately laterally compressed, low-crowned. Serrations both anterior posterior edges. P2 often double rooted. carnassial long slender highly reduced protocone; p2 can be present; p3 small single root. Lower long, low. Metaconid-talonid complex absent.Lokotunjailurus nov.Machairodus p.149, Hendey, 1974.Machairodus p.248, Turner, 1990.Amphimachairodus B., 201, 2006.'Machairodus' p.73, 2007. Holotype: SAM-PQL20505, fragmented maxilla, mandible, basicranium same individual (Figures 2, 3, 4).Figure 3Basicranial LangebaanwegShow full caption(A–D) Braincase SAM-PQL41573, posterior, ventral, dorsal lateral views; (E F) glenoid basicranial fragment ventral views. Note elevated alisphenoid neither Scale bar equals 10 cm.View Large Image Figure ViewerDownload Hi-res image Download (PPT)Figure 4Mandibular fragments nov kabir QuarryShow captionLokotunjailurus (A–E). (A–C) SAM-PQL-12641, dorsal, (D E) SAM-PQL-20505, (F G) SAM-PQL-6386, 5 (PPT) (A–D) cm. Etymology: honor Prof. Anusuya Chinsamy, world renowned paleontologist her contributions paleontology. locality: LQSM, (5.2 Ma). Assigned material: SAM-PQL12641, right hemimandible i3-c, p2-3 alveoli, p4-m1. SAM-PQL-22193, six thoracic vertebrae, three lumbar femora, tibiae, left fibula, astragalus, calcaneum second, third fourth metatarsals; SAM-PQL-52061, Rabe al.52Rabe Chinsamy Valenciano palaeobiological large, pathological sabretooth Felidae, Machairodontinae) lower Africa.Papers Palaeontology. e1463https://doi.org/10.1002/spp2.1463Crossref (1) size, high femur greater trochanter indicate affinity. Moreover, morphology does not fit Amphimachairodus (and presumably Adeilosmilus), closer Lokotunjailurus, al.,52Rabe here assigned Known type (LQSM), Diagnosis: Medium-sized machairodontine jaguar. indistinct. Symphysis robust. robust low-crowned, clear serration. P3 less 1/2 length P4. P4 preparastyle. single-rooted. m1 slender. Differential Differs emageritus, having stronger mandibular flange, posteriorly extended angular process inclined coronoid process, retaining p2, p3; differs smaller longer C-P3 diastema, upper canine, process; especially rooted P2, proportionally p3/P3 (compared P4/m1), slenderer P4; larger weaker mandibula non-ventrally fossa, canal. Remarks: specimens SAM-PQL20505 SAM-PQL12641 Hendey (1974)12Hendey 4, 5; Tables 1 2). maxilla incomplete dentition well preserved. low crowned machairodontine. There strong serration keels canine. sides, side it whereas mesial accessory cusp medial cusp. distal cingulum cusp-like. elongated. preparastyle line axis tooth. protocone (more Amphimachairodus, state Homotherium), parastyle/paracone notch. mandible ramus, broken. symphysis thick. small. mental foramina. larger. poorly preserved, present, small.Table 1Measurements ratios studyTaxonDinofelis werdelini?Dinofelis werdeliniYoshi obscuraLokotunjailurus chinsamyaeCatalogL20284L47523 LL47523 RL20685 LL20685 RL50128L20702L2674L10100L20505 LL20505 RCL20.1718.6917.5517.8820.8418.6123.23CW13.2414.5310.5210.7313.259.0111.22CH50.0441.9642.5837.3049.40CW/L0.660.780.600.600.640.480.48CH/L2.482.392.381.792.13P3L19.8020.8319.3514.0015.55P3W11.6311.979.046.306.84P3W/L0.590.580.470.450.44P4L33.4533.2930.4923.8037.7137.19P4W17.8217.0314.3814.1812.2012.3713.25P4BW11.9212.339.849.7410.6910.85P4W/L0.530.510.470.510.330.36P4BW/L0.360.370.320.280.29M1L5.624.235.604.48M1W10.059.047.406.26M1W/L1.792.141.321.40CL/P4L0.560.550.63P3L/P4L0.590.630.590.41M1W/P4L0.300.310.17LT87.5259.6588.16LDP9.805.206.397.397.61LDP/LT0.110.110.09 Open table tab Table 2Measurements werdeliniLokotunjailurus chinsamyaecatalogL20995L20284L20284L51591L12237L20685L41054 LL41054 RL41726L12641L-20505cL15.2015.7916.4112.92cW9.9210.5612.0711.43cH23.7725.2520.5822.29cW/L0.650.670.740.89cH/L1.561.601.251.73p3L14.0314.5413.9915.2512.30p3W6.477.227.418.845.50p3W/L0.460.500.530.580.45p4L20.0922.3822.4522.6

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ژورنال

عنوان ژورنال: iScience

سال: 2023

ISSN: ['2589-0042']

DOI: https://doi.org/10.1016/j.isci.2023.107212