This is the accepted version of the article: Lavrov, A. V.; Gimranov, D. O.; Madurell Malapeira, Joan; [et al.]. «Megan- tereon adroveri from the Early Pleistocene of Taurida Cave, Crimea, and the European Lineage of Dirk-toothed Cats». Journal of Mammalian Evolution, (October 2021). DOI 10.1007/s10914-021-09578-1 This version is available at https://ddd.uab.cat/record/250708 under the terms of the license Megantereon adroveri from the Early Pleistocene of Taurida Cave, Crimea, and the European lineage of dirk-toothed cats A. V. Lavrov1, D. O. Gimranov2, J. Madurell-Malapeira3*, A.V. Lopatin1 1 Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, Russia 2 Institute of Plant and Animal Ecology, Ural Branch of the Russian Academy of Sciences, Yekaterinburg, Russia 3 Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona, Edifici ICTA-ICP, Barcelona, Spain Abstract Recent field surveys performed in the newly-discovered Taurida cave (Crimea, Russia, Late Villafranchian, 1.8–1.5 Ma) enabled us to unearth dentognathic remains of the dirk-toothed cat Megantereon. Here we describe in detail the recovered remains further comparing it anatomically and biometrically with coeval Eurasian and African sites. The performed analysis suggests the inclusion of the Taurida remains in the hypodigm of the Villafranchain European species Megantereon adroveri, a medium-sized saber-toothed cat poorly known in Europe as a consequence of the scarcity and fragmentary nature of the known remains. Our results and the putative transitional characters displayed by the Taurida specimen, support the idea put forward by previous authors of a continuous European lineage of dirk-toothed cats. Keywords: Megantereon, Machairodontinae, mandibular corpus, Pleistocene, Late Villafranchian, Crimea, Russia. *corresponding author: joan.madurell@icp.cat 1 Introduction The genus Megantereon includes several species of medium-sized saber-toothed cats scarcely recorded, mainly known only on the basis of fragmented and isolated dentognathic remains, in the Plio-Pleistocene of the Old World and North America (Antón 2013). Megantereon was an ambush predator with massive forelimbs that was the size of a jaguar and has been traditionally classified in the tribe Smilodontini (subfamily Machairodontinae), phylogenetically closely related to the American genus Smilodon (Antón 2013). Megantereon probably originated in North America according to the earliest records in the Bone Valley Formation of Florida (ca. 4.5 Ma; Berta and Galiano 1983; Wallace and Hulbert 2013). The earliest record in the Old World comes from the South Turkwel site in Kenya (ca. 3.5 Ma; Werdelin and Lewis 2000); however, unpublished African remains can be referred to 4.4 Ma (Werdelin and Peigné 2010), coeval with the first American records. In turn, the oldest European records can be related with the Early Villafranchian Perrier – Les Etouaires assemblage (ca. 2.8 Ma; Nomade et al. 2014). In Asia, the best sample of Megantereon comes from the Middle Villafranchian Longdan site (ca. 2.4-2.2 Ma, China; Qiu et al. 2004) and can be traced until the Middle Pleistocene of Zhoukoudian-1 (Pei 1934) In the latter case this represents the last record of this genus in the Old World. The taxonomy and phylogenetic relationships within the different formerly described species of Megantereon has been a matter of harsh debate in the last four decades; such a debate is probably consequence of their scarce and fragmentary record (Viret 1954; Ficcarelli 1979). Turner (1987) was the one of the first scholars who tried to organize the taxonomy of Old World Megantereon remains. According to the former author opinion all Eurasian and African remains can be accommodated in the species Megantereon cultridens (Cuvier, 1824) characterized by a high degree of intraspecific variability and sexual dimorphism. On the contrary, Pons-Moyà (1987) and Sardella (1998) included all the known Eurasian specimens in M. cultridens, which putatively display several evolutionary convergences with the African M. whitei. Then, Qiu et al. (2004), in a monograph of the Longdan fauna, reviewed the Eurasian record of the Megantereon genus and concluded that Megantereon nihowanensis Teilhard de Chardin and Piveteau, 1930 is the species recorded in the Middle Villafranchian of China (Longdan and Nihewan Loc. 18) and Megantereon lantianensis Hu and Qi, 1978 the species recorded in the Late Villafranchian. More 2 recently, Werdelin and Lewis (2000), in their description of the South Turkwel Kenyan carnivore sample, erected the species Megantereon ekidoit Werdelin and Lewis, 2000. This species differs from the youngest M. whitei in the absence of p3 and the morphology of the mandibular ramus. Taking into account the last morphological features, Werdelin and Lewis (2000) concluded that M. ekidoit is the earliest and the most primitive African species. Werdelin and Lewis (2000) also included all the European samples in a phylogenetic lineage composed of two forms, M. cultridens and M. adroveri (for further discussion see Lewis and Werdelin 2010; Werdelin and Flink 2018). Finally, in a series of publications, Martínez-Navarro and Palmqvist (1995, 1996) and Palmqvist et al. (2007) supported a new hypothesis on the origin and dispersal of Megantereon, including all Eurasian Early-Middle Villafranchian forms in M. cultridens and all the African ones in M. whitei. According to these authors, around ca. 2.0 Ma, M. whitei dispersed from Africa to Eurasia and replaced M. cultridens, thus remaining the only recorded species until its disappearance. In this paper, we favor the opinion of Pons-Moyà (1987), Turner (1987), Sardella (1998), Lewis and Werdelin (2000), and Werdelin and Flink (2018) and consider all European forms as members of a phylogenetic lineage composed of two chronospecies: M. cultridens and M. adroveri. We describe a well-preserved hemimandible of Megantereon recently unearthed from the Taurida cave in Crimea (Russia) and compare it morphologically and biometrically to remains from coeval Eurasian sites. Abbreviations. CFU – Vernadsky Crimean Federal University; H – height; L – length; PIN – Borissiak Paleontological Institute, Russian Academy of Sciences; W – width; ZMMU – Zoological Museum of the Lomonosov Moscow State University; ZIN – Zoological Institute, Russian Academy of Sciences Age and geological setting The Taurida cave and its large cave system were discovered in 2018 during the construction of the Taurida Highway from Simferopol to Kerch. The karstic system is located on the northern macroslope of the Crimean Mountains, in the interfluve of the Beshterek and Fundukla rivers (tributaries of the Zuya river, Salgir river basin). A large number of fossil terrestrial vertebrate bones were found in the southern corridor of the cave and in the small side hall of the Hyena Den (see Lopatin et al. 2019 for a synthesis and a complete faunal list). The preliminary results of the 3 first field surveys revealed a diverse faunal assemblage likely corresponding to the Late Villafranchian European biochron of Russia (Rook and Martínez-Navarro 2010; Madurell- Malapeira et al. 2014) and the Psekups faunal assemblage of Russia. The bone-bearing layers of the Taurida cave display a chronological range of 1.8–1.5 Ma according to the last published data (Lopatin et al. 2019; Lavrov et al. 2019; Vislobokova et al. 2019, 2020). Results Family Felidae Fischer, 1817 Subfamily Machairodontinae Gill, 1872 Megantereon Croizet and Jobert, 1828 Megantereon adroveri (Pons-Moyà, 1987) Referred specimen—A partial right mandibular corpus (coll. PIN No. 5644/95) with preserved i3, c1, p2 and m1 and alveoli of i2 and p3-p4. Measurements—Table 1. Description—The mandibular corpus is slender and narrow, the ventral edge has a straight ventral profile behind the symphysis. The symphysis is oriented practically vertically (Fig. 1a). The anterior surface of the symphysis is separated from the buccal corpus surface by a sharpened bone ridge. The mental flange is well defined and expanded ventrally. Three mental foramina are visible (Fig. 1A). The masseteric fossa is triangular, and its anterior margin is located on the line at the middle length of m1 protostylid. Concerning dentition, the i3 crown is slightly curved distally. There are pronounced lateral and medial ridges and a well-defined lateral basal tubercle. The c1 crown is also curved distally, but in a stronger way as compared to i3. A well-defined medial ridge is visible in c1, with a poorly defined basal tubercle. The c1-p3 diastema is mesiodistally long. In the corpus, an atavistic single-rooted p2 is erupting just buccally to the p3 mesial alveolus (Fig. 1d). The p2 is triangular in occlusal view, displaying a main cusp and two cuspulids: a mesial and a distal one. The labial and lingual cingulids are well expressed. The alveoli of a two-rooted p3 and p4 are visible in occlusal view (Fig. 1c). Finally, and concerning first lower molar, the paraconid is two times mesiodistally longer than the protoconid. The caudal surface of the protoconid forms the cutting ridge (the postprotocristid), at the base of which there is a tiny rudimentary talonid. The 4 parastylid and protostylid form an angle of about 90° in the parasagittal plane (in buccal view). The buccal surface of the tooth is convex, whereas the lingual surface is flat. Discussion Comparisons between the Taurida specimen and coeval European Megantereon remains. From our point of view, based only on anatomical characters, we favor the idea that the European records attest to the presence of two different forms that putatively can be included in a single phylogenetic lineage (sensu Lewis and Werdelin 2010). In this scenario, it seems that the earliest European records (e.g., Perrier – Les Etouaires and Saint Vallier; Early and Middle Villafranchian) apparently display more primitive characters, including: a less developed mental flange; two-rooted p3 with strong distal accessory cuspulid and distal cingulid; mesiodistally short c1-p3 diastema; few mesially and upright projected c1 and incisors; and a developed and high coronoid process (Fig. 2a-c; Croizet and Jobert 1828; Viret 1954; Ficcarelli 1979; Pons- Moyà 1987; Sardella 1998; Palmqvist et al. 2007; Sardella et al. 2008). Nevertheless, as usually happens, these characters are the most commonly displayed by M. cultridens, and several specimens display other features that can be interpreted as derived for the European Megantereon lineage or even transitional to the Late Villafranchian forms or simply intraspecific variability. For instance, a few specimens show an incipient diastema between p3 and p4, including specimens from Upper Valdarno, Fonelas P1, Senèze, and Les Etouaires; others display a small p3 without a distal cingulid and a less developed p3 distal accessory cuspulid, such as Fonelas, Upper Valdarno, and Senèze (Fig. 2a-c; Ficcarelli 1979; Christiansen and Adolfssen 2007; Palmqvist et al. 2007). The observed variability in the listed characters can be interpreted as a general trend of evolutionary changes, prompted by the effect of mosaic evolution and exacerbated by the scarce paleontological record. On the other side, Late Villafranchian and Epivillafranchian specimens putatively display more advanced features, such as: a more developed mental flange; mesiodistally long c1-p3 diastema; reduced p3 without accessory cuspulids; large p3-p4 diastema; small p4 compared to m1; and c1 and incisors more projected mesially and upright (Fig. 2h). The later features can be seen in the specimens from Dmanisi (Georgia; ca. 1.8 Ma), Venta Micena (Spain; ca. 1.5 Ma), and Apollonia-1 (Greece; 1.1 Ma) (Fig. 2g-h; Martínez-Navarro and Palmqvist 1995; Vekua 1995; Koufos 2018). 5 The Taurida specimen shares with the last forms strongly mesially projected c1 and incisors, a more developed and ventrally projected mental flange, a long c1-p3 diastema, and a small p4 alveolus compared with that of m1. However, the Taurida specimen also displays a two-rooted p3 and an only incipient diastema between p3-p4, characters traditionally considered as primitive in the Megantereon lineage but that we consider to be variable among samples, as explained by previous authors (Turner 1987; Sardella 1998). Comparisons of Taurida specimen with coeval Asian Megantereon remains. The Asian scenario is more complicated, with several species described that putatively represent a phylogenetic lineage: M. microta Zhu et al., 2015 > M. nihowanensis > M. inexpectatus Teilhard de Chardin, 1939 lantianensis (Zhu et al. 2020 and references therein). According to Zhu et al. (2020), an early form of small size included in M. microta displays a short diastema, two-rooted p3, poorly developed mental flange, and a moderately developed coronoid process. The later forms, exemplified by Longdan and Sabertooth Cave specimens, display a single-rooted p3, longer diastema, small coronoid process, and sometimes a tiny diastema between p3-p4 (Fig. 2d-e; Qiu et al. 2004; Zhu et al. 2020). The younger late Early Pleistocene and Middle Pleistocene forms are less common in Asia, only recorded by a single mandible from Lantian and a cranium of M. inexpectatus from Zhoukoudian-Loc.1 (Zhu et al. 2020). The Lantian mandible putatively displays more derived character states, with a small and single-rooted p3, a long diastema between c1-p3, and a well-developed p3-p4 diastema (Hu & Qi 1978). The Taurida specimen apparently displays a more developed and ventrally projected mental flange, more protruding c1 and incisors, and a straighter profile of the corpus than all Chinese specimens (Fig. 2d-e and g). Comparisons of Taurida specimen with coeval African Megantereon remains As compared with the Taurida specimen, the most complete Megantereon whitei Broom, 1937 specimens (i.e., Koobi Fora Okote Mb and Afar) display a less developed and ventrally projected mental flange and less protruding incisors, which are more primitive features (both ca. 1.8-1.5 Ma; Fig. 2f-h). On the other hand, the Koobi Fora mandible shows a very small p3 (not in the Afar one) and a large p3-p4 diastema compared to the Taurida specimen (Ficcarelli 1979; Lewis and Werdelin 2010). Additionally, M. whitei specimens display large lower incisors 6 compared to the Crimean specimen (Fig. 2). This may be related to mosaic (heterochronic) evolution and the specialization of the feeding apparatus (the incisors). Taxonomic attribution of Taurida Megantereon The studied specimen displays an atavistic p2, which is not rare in the Megantereon fossil record and is also noted in Monte Argentario (Megantereon adroveri) and Sabertooth Cave Megantereon nihowanensis (Iurino and Sardella 2014; Zhu et al. 2020). This feature is here interpreted as an atavistic tooth without taxonomical significance, as it is also present in rare occasions in extant Lynx lynx and Panthera pardus (J. M.-M. pers. observ.). Taking into account the single and fragmentary nature of the Taurida specimen, a few inferences can be made. The presence of a double-rooted p3 is here interpreted as a putatively primitive character state for the European Megantereon lineage, although it is necessary to make such an inference with caution considering the intraspecific variability observed in this lineage (sensu Turner 1987 and Sardella 1998). A well-developed and ventrally projected mental flange, mesiodistal elongated c1-p3 diastema, and the upright and mesially projected canine and incisors are clearly advanced character states in the Megantereon lineage that resemble the condition showed by Dmanisi, Argentario, and Apollonia-1 M. adroveri (Fig. 2g-h; Vekua 1995; Sardella 1998; Koufos 2008). It is also worth noting the smaller alveolar mesiodistal length of the Taurida p4 compared to m1, a putatively derived character state for European Megantereon, as already stated by Martínez-Navarro and Palmqvist (1996; Fig. 2). Finally, we compared the mandibular robustness (mesiodistal length of m1 / height of the corpus below m1) in all the analyzed specimens (Eurasian and African) with a boxplot (Fig. 3). The results show a quite homogeneous pattern in the Megantereon record. Nevertheless, the values of M. cultridens are generally higher than M. adroveri, with the Taurida specimen in the middle of the variability observed by the two European species. The values for Asian species appear too wide, from 55 to 98%. In turn, the African fossils have a range similar to but greater than M. adroveri, putatively explained by their adaptative convergences (Fig. 3). Therefore, and according to the reported evidence, we refer the Taurida specimen to Megantereon adroveri (sensu Lewis and Werdelin 2010); i.e., it is a European Megantereon with advanced character states different from coeval African M. whitei (Fig. 2f-h). We regard the maxillary fragment from Taurida previously described by Lavrov et al. (2020, fig. 2) as Megantereon sp., as already published. 7 Conclusions The taxonomy and phylogenetic relationships of Eurasian and African Pleistocene dirk- toothed cats have been a matter of intense debate in recent decades, probably because of their scanty record. Here we describe a fragment of the mandibular corpus of Megantereon from the newly discovered site of Taurida that displays more derived features as compared with chronologically older European and Asian specimens traditionally referred to M. cultridens and M. microta > M. nihowanensis, respectively. The studied specimen shares features in common with European and Asian sites from the latest Early Pleistocene (e.g., Apollonia-1, Monte Argentario, and Lantian) and clearly differs from coeval African specimens (e.g., Koobi Fora Okote Mb). According to the former characters, we refer the Taurida specimen to M. adroveri, i.e., a European Megantereon with advanced characters. Our results support the idea of other authors (e.g., Werdelin and Lewis 2000) of a continuous European lineage of dirk-toothed cats despite the claims of other recent authors of a putative African dispersion of M. whitei into Europe during the Late Villafranchian. Acknowledgments The authors thank L. Werdelin, B. Martínez-Navarro, Q. Jiangzuo and J. B. Fourvel for useful discussions and suggestions during the last months. We also thank Q. Jiangzuo, L. Werdelin, A. Arribas, L. Rook, S. Bartolini Lucenti and G. Koufos giving us permission for reproduce/figure specimens under their care. The authors express their gratitude to all participants in the excavations in the Taurida cave and especially to A.M. Berezkin. We also express our special gratitude to the organizers of the excavations, Dean of the Faculty of Geography of CFU B.A. Vakhrushev and G.V. Samokhin, employees of CFU D.B. Startsev and S.V. Tokarev. We sincerely thank the staff of ZMMU S.V. Volkov, S.V. Kruskop, V.S. Lebedev, A.A. Lisovsky, V.E. Lytvyn for advice and assistance in the work. The comments of two anonymous reviewers and the editor D. Croft significantly improved an early version of this work. Funding The work of J.M.-M. has been funded by the Agencia Estatal de Investigación-European Regional Development Fund of the European Union (CGL2017-82654-P, AEI/FEDER-UE) and 8 the Generalitat de Catalunya (CERCA Program). J.M.-M. is member of the consolidated research group 2017 SGR 116 (AGAUR, Generalitat de Catalunya). Availability of Data and Material The datasets generated during and/or analyzed during the current study are available from the corresponding author on reasonable request References Antón M (2013) Sabertooth. Indiana University Press. Berta A, Galiano H (1983) Megantereon hesperus from the Late Hemphillian of Florida with remarks on the phylogenetic relationships of machairodonts (Mammalia, Felidae, Machairodontinae). J Paleontol 57:892–899. Christiansen P, Adolfssen JS (2007) Osteology and ecology of Megantereon cultridens SE311 (Mammalia; Felidae; Machairodontinae), a sabrecat from the Late Pliocene – Early Pleistocene of Senéze, France. 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J Paleontol 74:1173–1180. Werdelin L, Peigné S (2010) Carnivora. In: Cenozoic Mammals of Africa. University of California Press, pp. 603–657. Werdelin L, Lewis ME (2001) A revision of the genus Dinofelis (Mammalia, Felidae). Zool J Linnean Soc 132:147–258. Werdelin L, Flink T (2018) The phylogenetic context of Smilodon. In: Werdelin L, McDonald G and Shaw CA (eds) Smilodon: the Iconic Saberthooth. Johns Hopkins University Press. Zhu, M, Jiangzuo Q, Qin D et al (2020). First discovery of Megantereon skull from southern China. Hist Biol 31:1–10. Figure Captions Figure 1. Megantereon adroveri mandibular corpus with i3-c1, p2 and m1 from Taurida cave (PIN No. 5644/95) in a, buccal view; b, lingual view and c, occlusal view, scale bar is 2cm. d, detail of p2 and alveolus of p3, scale bar is 1 cm. Figure 2. Pleistocene Megantereon mandibular remains from Old World. European Middle- Late Villafranchian: a, mandible of M. cultridens from Fonelas P-1 (Spain; FPI-2002-1391) in buccal view; b, mandible of M. cultridens from Fonelas P-1 (Spain; FPI-2002-5001) in buccal 11 view; c, mandible of M. cultridens from Upper Valdarno (Italy; IGF-827) in buccal view. Asian Middle-Late Villafranchian: d and e mandibles of M. nihowanensis from Longdan (China) in buccal view. African late Early Pleistocene: f, mandible of M. whitei from Koobi Fora Okote mb. (Kenia; ER793) in buccal view. European Epivillafranchian: g, corpus of M. adroveri from Taurida (Russia; PIN No. 5644/95) in buccal view; h; corpus of M. adroveri from Apollonia-1 (Greece; APL-12) in buccal view. Scale bar is 2 cm. Figure 3. Boxplots of mesiodistal length of m1 to height of corpus below m1 ratio (%) of Eurasian specimens of the genus Megantereon. 12 Table 1. The measurements of the lower jaw teeth of Megantereon adroveri from Tauridae cave (coll. PIN No. 5644/95). Teeth L W H i3 7.3 5.7 11.2 c1 10.9 7.2 15.3 p2 8.1 4.7 6.4 p3 13.01 5.31 - p4 14.81 7.61 - m1 20.1 9.8 14.5