Selenogonus narinoensis Stirton, 1947 (Tayassuidae, Cetartiodactyla, Mammalia): taxonomic status and paleobiogeographic implications
The species Selenogonus narinoensis was described by Stirton (1947) based on a single specimen which comes from sediments cropping out in the Cocha Verde locality, Nariño Department (Colombia), tentatively referred to the late Pliocene–Pleistocene (MGN 931; IGM p002118, Museo Geológico Nacional, Servicio Geológico Colombiano, Bogotá). However, morphological studies and comparative morphometric observations of the specimen suggest that (1) no diagnostic character supports the validity of the species Selenogonus narinoensis (here considered species inquirenda); (2) a combination of features (e.g., the mandibular condyle located behind the posterior edge of the vertical mandibular ramus, the angular process which projects laterally outwards, a bunolophodont crown morphology, a mesodont crown height, and a simple crown morphology of the third lobe of m3) indicates it belongs to the genus Platygonus; (3) this specimen corresponds to one of the largest South American peccaries; (4) taking into account certain anatomical characters as well as its morphometric range, this specimen is assigned to Platygonus cf. marplatensis. Even though the stratigraphic provenance of the specimen is still doubtful, it can be proposed that (1) it could be one of the most ancient records of tayassuids in South America, as would be expected given its geographical position, and (2) considering the new taxonomic proposal, this specimen represents the first record of Platygonus cf. marplatensis in Colombia and represents one of the northernmost South American records of the genus. This new interpretation would be of great relevance in the Great American Biotic Interchange due to its strategic geographical proximity to the Isthmus of Panama.
The Tayassuidae (Mammalia, Cetartiodactyla) may have differentiated from their ancestor during the Eocene in Eurasia (Romer, 1966; Wright, 1998; Hulbert, 2001). Younger records suggest that the Tayassuidae expanded their range to North America from the late Eocene, where they reached their greatest diversity (Wright, 1998; Hulbert, 2001; Gasparini, 2007; Prothero, 2009; Prothero and Grenader, 2012; Prothero, 2015). From there they extended their distribution to South America during the Great American Biotic Interchange (GABI). They represent one of the first North American mammalian immigrants, after procyonids (Carnivora) and cricetid rodents (Woodburne, 2010; Cione et al., 2015; O'Dea et al., 2016).
The oldest unequivocal records of fossil tayassuids in South America date back to the late Pliocene (ca. 4–3.3 Ma; see Prevosti et al., 2006; Gasparini, 2013) and were found in sediments cropping out in southeastern Buenos Aires Province, Argentina. In contrast, Frailey and Campbell (2012), followed by Prothero and Pollen (2013), support the hypothesis of an early arrival of the Tayassuidae in South America, earlier than late Miocene and well before most of the Great American Biotic Interchange (GABI) that had occurred by the late Pliocene (Cione et al., 2015; O'Dea et al., 2016). This is based on the supposed record of peccaries, among other mammals of Nearctic origin (e.g., gomphotheres, tapirs, dromomerycine ruminants), coming from the Madre de Dios Formation (late Miocene) outcrops in southeastern Peru (Frailey and Campbell, 2012; Prothero and Pollen, 2013; Prothero et al., 2014) and on the divergence times suggested by molecular analyses (Theimer and Keim, 1998; Gongora and Moran, 2005; Perry et al., 2017). However, the chronological information about the sediments containing these remains and their taxonomic assignment is not accurate (Perini et al., 2016; Parisi Dutra et al., 2017a; Gasparini et al., 2021). According to these authors, the supposedly extinct Miocene species are indistinguishable from modern tayassuids (Tayassu pecari and Dicotyles tajacu), and the stratigraphic provenance of the specimens is highly dubious, and the fossils are likely Quaternary in age.
Tayassuids have been found in late-Cenozoic deposits mainly in Argentina and Brazil but also in Uruguay, Bolivia, Colombia, Peru, and Venezuela (Rincón et al., 2009; Gasparini, 2013; Montellano-Ballesteros et al., 2014; Parisi Dutra et al., 2017b), with 6 genera and 12 species (Gasparini, 2013; Parisi Dutra et al., 2017c). Platygonus Le Conte, 1848a (late Pliocene–Early to Middle Pleistocene; Argentina, Uruguay, Bolivia, and Colombia), is represented by 5 species: Platygonus kraglievichi Rusconi, 1930 (late Pliocene–earliest Pleistocene; Argentina); Platygonus scagliai Reig, 1952 (late Pliocene–earliest Pleistocene; Argentina); Platygonus marplatensis Reig, 1952 (late Pliocene–earliest Pleistocene; Argentina); Platygonus chapadmalensis (Ameghino, 1908) (late Pliocene? latest Pliocene–earliest Pleistocene; Argentina); and Platygonus cinctus (Ameghino, 1886) (Early to Middle Pleistocene; Argentina). Catagonus Ameghino, 1904 (late Pliocene? Early Pleistocene–Late Pleistocene/Early Holocene; Argentina and Uruguay), is represented by two species: Catagonus metropolitanus Ameghino, 1904 (Early to Middle Pleistocene; Argentina), and Catagonus bonaerensis (Ameghino, 1904) (Middle Pleistocene? Late Pleistocene/Early Holocene; Argentina and Uruguay). Brasiliochoerus Rusconi, 1930 (Middle Pleistocene–Late Pleistocene/Early Holocene; Argentina, Brazil, Bolivia, and Uruguay) is monospecific, Brasiliochoerus stenocephalus (Lund in Reinhardt, 1880). Parachoerus Rusconi, 1930 (Middle Pleistocene? Late Pleistocene–recent; with paleontological records in Argentina and Uruguay), is represented by two species: Parachoerus carlesi (Rusconi, 1930) (Middle Pleistocene? Late Pleistocene; Argentina), and Parachoerus wagneri (Rusconi, 1930) (Late Pleistocene/Early Holocene–recent; fossil records in Argentina and Uruguay and currently endemic to the Dry Chaco in Argentina, Bolivia, and Paraguay). Tayassu Fischer, 1814 (Middle Pleistocene–recent; fossil records in Argentina, Brazil, Uruguay, and Venezuela and currently inhabits southeastern Mexico to northern Argentina), has one extant species, Tayassu pecari (Link, 1795). Finally, Dicotyles Cuvier, 1816 (Middle Pleistocene–recent; fossil records in Argentina, Brazil, Peru, and Venezuela and currently from southwestern USA to north-central Argentina), has one extant species Dicotyles tajacu (Linnaeus, 1758).
In Colombia, very few remains of tayassuids have been registered (Stirton, 1947; Villarroel et al., 1989; Gasparini, 2013; Moreno Mancilla et al., 2019). One of them is the holotype and single specimen of Selenogonus narinoensis Stirton, 1947, which comes from sediments cropping out at the Cocha Verde locality, Nariño Department, tentatively referred to the late Pliocene–Pleistocene. However, the chronological information of the fossil-bearing sediments is not accurate. In turn, Menégaz and Ortiz Jaureguizar (1995), considering the hypotheses of Kraglievich (1959, pp. 233–234) and Reig (1981, p. 41), suggested a lower- to middle-Pliocene age for those fossil-bearing sediments. Fossil remains described as Platygonus sp. were found in sediments cropping out in the Villa de Leyva locality (Boyacá Department), but chronologic and stratigraphical information is still unknown (Gasparini et al., 2019). Other Tayassuidae remains were registered in Late Pleistocene sediments cropping out in the paleontological site named Los Hoyos located at the Tatacoa Desert (Huila Department) (Tayassu aff. tajacu sensu Villarroel et al., 1989).
The goals of this contribution are (1) to report the results of study of the fossil specimen from Nariño (Colombia); (2) to comment on the systematic validity of Selenogonus narinoensis Stirton, 1947; and (3) to discuss the paleobiogeographic and paleoecological significance of this peccary.
2.1 Repositories and institutional abbreviations
AMNH: American Museum of Natural History, New York, USA; ANSP: Academy of Natural Sciences of Drexel University, Philadelphia, USA; MACN: Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Ciudad Autónoma de Buenos Aires, Argentina; MLP: Museo de La Plata, Argentina; MGN: Museo Geológico Nacional, Bogotá, Colombia; MMP: Museo Municipal de Mar del Plata, Buenos Aires, Argentina; UF: Florida Museum of Natural History, University of Florida, Gainesville, FL, USA.
The studied specimen (MGN 931; IGM p002118) is housed at the Museo Geológico Nacional (MGN), Servicio Geológico Colombiano (Bogotá, Colombia). Taxonomic classification follows the proposal of Parisi Dutra et al. (2017c). For nomenclatural assignments of collared and white-lipped peccaries, we followed Acosta et al. (2020).
The material was compared with North American and South American extinct and extant tayassuids. The following materials were included in the morphometric comparisons: Platygonus sp. – UF 10422, UF 8922, UF 12942, UF 62700, UF 66679, UF 63904, UF 67178, MACN 10959, MACN 5337, MMP 1139, MMP 1212; P. vetus – UF 220478, UF 221010, UF 221174, UF 220479, UF 221766, UF 221767; P. cf. P. vetus – UF 67177; P. cumberlandensis – UF w/“no.” material, in exposition collection, AMNH 27871, AMNH 27872; P. compressus – AMNHFLA 6–90, AMNH Type 45724; P. kraglievichi – MACN Type 5341; P. scagliai – MMP-S 156, MMP-S 553, MMP-M 878; P. marplatensis – MMP-S Type 25, MACN 19726; P. chapadmalensis – MMP-M 246. Measurements were taken using Vernier calipers, with 0.01 mm accuracy; data are expressed in millimeters.
2.2 Measurements abbreviations
Hrmv: height of the vertical branch of the mandible, taken from the ventral part of the angular process to the depression between the coronoid process and the condyle; Hrmhm3: depth of horizontal ramus below m3; Lm3: maximum length of molar 3 in a parallel line to the sagittal plane; Am3: maximum width of molar 3 in a perpendicular line to the sagittal plane.
Class Mammalia Linnaeus, 1758
Order Cetartiodactyla Montgelard, Catzeflis,
and Douzery, 1997
Suborder Suiformes Jaeckel, 1911
Infraorder Suoidea Gray, 1821
Family Tayassuidae Palmer, 1897
Subfamily Tayassuinae Palmer, 1897
Tribe Platygonini Parisi Dutra et al., 2017c
Genus Platygonus Le Conte, 1848a
1848a Platigonus, Le Conte, p. 103 (lapsus calami).
1848b Platygonus, Le Conte, p. 258.
1848a Hyops, Le Conte, p. 104.
1848b Protochoerus, Le Conte, pp. 105–106
1852a Dicotyles, Le Conte (in part), p. 3.
1852b Dicotyles, Le Conte (in part), p. 5.
1853 Euchoerus, Leidy, p. 340.
1857 Dicotyles, Leidy (in part), p. 100.
1886 Antaodon, Ameghino, p. 149.
1887 Coyametla, Duges, p. 16.
1904 Listriodon, Ameghino, p. 76.
1930 Mylohyus, Rusconi, pp. 191–195
(nec Cope, 1889: p. 134).
1947 Selenogonus, Stirton, p. 322.
1959 Argyrohyus, Kraglievich, p. 230.
Platygonus compressus Le Conte, 1848a (ANSP 11512, ANSP 11515, ANSP 11522, ANSP 11524, ANSP 11533, ANSP 11534, ANSP 11539), Pleistocene sediments from a fissure fill near Galena, Jo Daviess County, Illinois, USA.
Late Miocene–Late Pleistocene (North America); late Pliocene–Early to Middle Pleistocene (South America). In South America there are paleontological records in Argentina (Buenos Aires and Jujuy provinces), Bolivia (Tarija valley), Uruguay (Canelones Department), and Colombia (Boyacá and Nariño departments) (Gasparini et al., 2010; Gasparini and Ubilla, 2011; Gasparini, 2013; Gasparini et al., 2019; Moreno Mancilla et al., 2019).
The original spelling was actually “Platigonus”, but there is sufficient indication that this was a misprint. The name is differently misprinted (Platydonus) in another paper by Le Conte, published almost simultaneously. “Platygonus is now universally used and may be retained” (Simpson, 1945, p. 146) (see McKenna and Bell, 1997). See also the International Code of Zoological Nomenclature (1999), articles 32 and 33.
Platygonus marplatensis Reig, 1952
1927 Homo chapadmalensis, Castellanos, pp. 1–15.
1941 Homo neogaeus (not Lehmann Nitsche, 1907),
Vignati, pp. 274–358 (misidentification)
1952 Platygonus marplatensis, Reig, pp. 121–122.
1959 Argyrohyus chapadmalensis, Kraglievich, p. 230.
1977 Platygonus marplatensis, Wetzel, pp. 1–36.
1995 Platygonus marplatensis, Menégaz and
Ortiz Jaureguizar, pp. 314–315.
2002 Platygonus marplatensis, Quintana, pp. 263–275.
2007 Platygonus marplatensis, Gasparini, pp. 178–183.
2013 Platygonus marplatensis, Gasparini, p. 58.
2017b Platygonus marplatensis, Parisi Dutra et al., p. 355.
MMP-S Type 25. Partial mandible. Layer 3, Chapadmalal Formation, Barranca de los Lobos, General Pueyrredón county, Buenos Aires Province, Argentina; late Pliocene (Fig. 1c).
Late Pliocene–earliest Pleistocene (Chapadmalalan Stage/Age, Marplatan Stage/Age (Sanandresian Substage/Subage sensu Cione et al., 2015); coastal cliff in Chapadmalal region and Miramar (General Pueyrredón and General Alvarado counties), in southeastern Buenos Aires Province, Argentina (Kraglievich, 1952; Reig, 1952; Quintana, 2002; Gasparini, 2004; Gasparini and Ubilla, 2011; Gasparini, 2013) (Fig. 2).
Castellanos (1927) referred some teeth exhumed from the southeastern coast of Buenos Aires Province to Homo chapadmalensis. Vignati (1941) included these remains in the species Homo neogaeus Lehmann Nitsche, 1907, a species based on a fossil found in the Monte Hermoso cliff. Reig (1952) established the species Platygonus marplatensis based on a partial mandible found in the Chapadmalal Formation, Barranca de los Lobos, General Pueyrredón county, Buenos Aires Province. Kraglievich (1959) created the genus Argyrohyus with the species Argyrohyus chapadmalensis and included in the synonym Homo chapadmalensis Castellanos, 1927; Homo neogaeus sensu Vignati, 1941; and Platygonus marplatensis Reig, 1952. Menégaz and Ortiz Jaureguizar (1995) suggested that A. chapadmalensis could be a synonym of Platygonus marplatensis.
Concerning the specific reassignment, it is worth mentioning that Rusconi (1930) included the species Listriodon chapadmalensis Ameghino, 1908, in the genus Platygonus. This generates a case of secondary homonymy (they are homonyms as a consequence of a new combination and not as a consequence of origin), and it must be solved by priority. Thus, the species of Ameghino, 1908, may continue to be called Platygonus chapadmalensis, while for that of Castellanos, 1927, a replacement must be considered. Therefore, the oldest name is Platygonus marplatensis Reig, 1952 (see Wetzel, 1977; Gasparini, 2007, 2013; Parisi Dutra et al., 2017c).
Platygonus cf. marplatensis Reig, 1952
Portion of vertical ramus of a left hemimandible with m3 partially preserved (Selenogonus narinoensis Stirton, 1947, holotype MGN 931 (IGM p002118)) (Fig. 1a, b).
Dark-green fine-grained sandstone exposed in Cocha Verde, Túquerres highway, Tangua Municipality, Nariño Department, Colombia. Late Pliocene or Pleistocene (sic Stirton, 1947, p. 322) (Fig. 2).
This mandible corresponds to a large specimen. It has a shallow but sharply outlined masseteric fossa and a deep internal temporal fossa. The angular process projects forward to the middle part of m3, and its lower edge is slightly projecting laterally outwards. The lower border of the horizontal ramus is sharply hooked (accentuated) distally. The mandibular condyle is located behind the posterior edge of the vertical mandibular ramus. The coronoid process ascends behind m3.
The lower molar 3 only preserves the distal pair of main cusps (hypoconid and entoconid) and the third lobe, which has a well-developed single cusp, and a pair of smaller accessory cusps both located labially and lingually. Despite its incompleteness, a mesodont and bunolophodont dental morphology is observed.
4.1 Taxonomic comments and comparisons
Stirton (1947) erected the genus and species Selenogonus narinoensis for this specimen based on some features that basically coincide with those of the Platygonus genus. Mainly these features are
Large, evidently about equal in size to Platygonus uquiensis Rusconi; masseteric fossa shallow but sharply outlined; internal temporal fossa deep; […] ascending ramus relatively and actually higher than in other peccaries; angle below lower border of horizontal ramus, sharply hooked anteriorly; […] m3 hypso-brachyodont; evidently more lophiodont than in Platygonus. (Stirton, 1947, p. 322)
However, these features do not differ from those described for Platygonus, given the diversity observed within the genus (Gasparini, 2007; Gasparini and Ubilla, 2011; De los Reyes et al., 2014). In addition, the following morphological features support the inclusion of this specimen within the genus Platygonus: mandibular condyle located behind the posterior edge of the vertical mandibular ramus, angular process projected laterally outwards, bunolophodont crown morphology, mesodont crown height, and simple crown morphology of the third lobe of m3.
The development of mesodont and bunolophodont cheek teeth in Platygonus differs from the brachyodont and bunodont morphology observed in Tayassu pecari, Dicotyles tajacu, Parachoerus carlesi, and Brasiliochoerus stenocephalus; from the mesodont and bunodont cheek teeth typical of Catagonus metropolitanus and Catagonus bonaerensis; and from the mesodont crown height and bunodont with high crowns (referred to as “zygodont” by some authors (Gasparini, 2007; Prothero and Grenader, 2012; Gasparini et al., 2013)) observed in Parachoerus wagneri.
The sharp outline of the masseteric fossa is remarkable in the specimen studied. A similar condition was observed in Platygonus marplatensis, Platygonus chapadmalensis, Platygonus sp. (MMP 1212), Brasiliochoerus stenocephalus among South American species, and Platygonus compressus among North American species.
The lower margin of the horizontal ramus in the specimen studied is also singular. A sharply hooked (accentuated) distal condition was observed only in the holotype of Platygonus marplatensis (MMP-S Type 25; see Fig. 1c). However, this character is not present in the other specimens assigned to this species (MACN 5420 type synonym, MMP-S 200, MMP-S 188, MMP-S 199, MMP-S 674, MACN 19725, MACN 19726) due to their partial preservation.
The incomplete state of preservation of the material prevents us from obtaining absolute measurements. However, taking into account its relative size, this specimen is within the proportions observed in species of the genus Platygonus (see Table 1). It is worth mentioning that the vertical mandibular ramus of this specimen is one of the largest among South American species, only comparable to P. marplatensis, P. chapadmalensis, and P. scagliai and to the largest specimens of North American Platygonus (e.g., Platygonus cumberlandensis Gidley, 1920).
The specimen under study has no diagnostic characters that support the species Selenogonus narinoensis as valid and identifiable (species inquirenda). The combination of features suggests it pertains to the genus Platygonus. As a consequence, based on the reflected taxonomic problems and taking into account certain anatomical characters (e.g., the position of the mandibular condyle, the outline and laterally outward projection of the angular process, the crown height and morphology of the tooth, and the distal condition of the lower margin of the horizontal ramus) as well as its morphometric range, this specimen is considered Platygonus cf. marplatensis.
4.2 Paleobiogeographical aspects
The Tayassuidae represent one of the first North American immigrant mammals as well as the first ungulates that entered South America during the GABI (Gasparini, 2013; Cione et al., 2015; O'Dea et al., 2016).
According to phylogenetic analyses as well as chronological and geographical evidence, Platygonus represents a Tayassuidae lineage that originated in North America and corresponds to the first group of peccaries that entered South America during the late Pliocene (Prevosti et al., 2006; Gasparini and Ubilla, 2011; Gasparini, 2013; De los Reyes et al., 2014; Parisi Dutra et al., 2017c). The greatest specific diversity of Platygonus is recorded during the late Pliocene–earliest Pleistocene in South America, mainly in Argentina (represented by P. marplatensis, P. chapadmalensis, P. scagliai, P. kraglievichi, and Platygonus sp.) and Uruguay (Platygonus sp.) (Gasparini and Ubilla, 2011; Gasparini, 2013, and bibliographies cited therein). If the stratigraphic provenance of the fossil specimen found in Nariño (Colombia) is confirmed, it could be one of the most ancient records of tayassuids on this continent, as would be expected given its geographical position. In addition, considering the new taxonomic proposal, this specimen represents the first record of Platygonus cf. marplatensis in Colombia. At the same time, it is remarkable that this Colombian record, together with the one registered in Villa de Leyva, represents the northernmost South American records of the genus Platygonus. This could have had great relevance in the Great American Biotic Interchange due to its strategic geographical proximity to the Isthmus of Panama.
In the Early to Middle Pleistocene, the taxonomic diversity and abundance of records of Platygonus are notably reduced (P. cinctus) and the genus Catagonus (C. metropolitanus) appears reliably for the first time in the paleontological record and only in Argentina (Gasparini, 2013).
The greatest specific diversity and abundance of tayassuids is documented during the Middle Pleistocene to Late Pleistocene–Early Holocene in South America (e.g., Argentina, Brazil, Uruguay, Bolivia, Peru, Colombia, and Venezuela) represented by Catagonus, Parachoerus, Brasiliochoerus, Tayassu, and Dicotyles (Gasparini, 2013; Parisi Dutra et al., 2017b). In the Middle Pleistocene the genera Brasiliochoerus, Tayassu, and Dicotyles and probably the species Parachoerus carlesi and C. bonaerensis appear for the first time in the South American fossil record (Gasparini, 2013). In the Late Pleistocene–Early Holocene, P. wagneri is registered for the first time (e.g., Uruguay) and P. carlesi and C. bonaerensis are reliably recorded (e.g., Argentina and Uruguay) on this continent. At the Pleistocene–Holocene boundary (about 10 000 years ago) all megamammals and most of the large mammals became extinct in South America in a remarkable extinction event. The tayassuids were affected by this extinction, and only 25 % of their taxonomic diversity has survived. Currently, peccaries are represented by only three species (Tayassu pecari, Dicotyles tajacu, and Parachoerus wagneri) (Gasparini, 2013; Parisi Dutra et al., 2017c; Acosta et al., 2020).
4.3 Ecological and anatomical considerations
The peccaries of the genus Platygonus have certain morphological features that allow some inferences about their habits: a great development of nasal sinuses and chambers, orbits located in a superior–posterior position and behind upper molar 3 due to elongation of the rostrum, a possession of a distinct basicranial flexure, a laterally outward projection of the angular process of the jaw (providing a greater surface for insertion of the lateral deep masseter muscle), a reduction of the lateral digits in the limbs, a mesodont crown height, and a bunolophodont crown morphology, among others. Therefore, this set of anatomical characters indicates that these large-sized peccaries have diurnal habits, a herbivorous diet, and probably a foraging habit and lived in dry and relatively open environments (Guilday et al., 1971; Wetzel, 1977; Menégaz and Ortiz Jaureguizar, 1995; Gasparini, 2007; Gasparini and Ubilla, 2011). Paleoecological studies (e.g., dental microwear and isotopic analysis) on North American Platygonus have shown a C3-browser to mixed-feeder diet and probably a C4-grass diet, under special conditions (Feranec and MacFadden, 2000; Feranec, 2007; Schmidt, 2008).
The faunal changes that have occurred since the late Pliocene could have been strongly influenced by climate (Cione et al., 2015, and references cited therein). The open and arid environments of great latitudinal extent developed during glacial cycles allowed the dispersion of Platygonus, Catagonus, Brasiliochoerus, and Parachoerus.
Based on paleontological records, as well as certain anatomical features (e.g., crown teeth morphology, limb development) linked to diet and life habits, together with body mass, it can be inferred that the species of Catagonus, Brasiliochoerus, and Parachoerus have replaced those of Platygonus since the Middle Pleistocene, probably as a consequence of the reduction of the open environments for which Platygonus species would be more specialized. This predominantly arid or semi-arid and cold period alternating with brief more humid and warmer pulses would have allowed the late expansion of the species of Tayassu and Dicotyles.
5.1 Taxonomic final remarks
Morphological studies and comparative morphometric observations of the Colombian specimen suggest that (1) no diagnostic character supports the validity of the species Selenogonus narinoensis (here considered species inquirenda); (2) a combination of features (e.g., the mandibular condyle located behind the posterior edge of the vertical mandibular ramus, the angular process that projects laterally outwards, a bunolophodont crown morphology, a mesodont crown height, and a simple crown morphology of the third lobe of m3) indicates it belongs to the genus Platygonus; (3) this specimen corresponds to one of the largest South American peccaries; and (4) taking into account certain anatomical characters as well as its morphometric range, this specimen is assigned to Platygonus cf. marplatensis.
5.2 Paleobiogeographical remarks
Even though the stratigraphic provenance of the specimen found in Nariño (Colombia) is still doubtful (late Pliocene or Pleistocene?), it can be proposed that (1) it could be one of the most ancient records of tayassuids in South America, as would be expected given its geographical position, and (2) considering the new taxonomic proposal, this specimen represents the first record of Platygonus cf. marplatensis in Colombia and, together with the one registered in Villa de Leyva, establishes the northernmost South American records of the genus. This new interpretation would be of great relevance in the Great American Biotic Interchange due to its strategic geographical proximity to the Isthmus of Panama.
The studied specimen (MGN 931, IGM p002118) is housed at the Museo Geológico Nacional (MGN), Servicio Geológico Colombiano (Bogotá, Colombia). The holotype and referred materials for Platygonus marplatensis are housed at Museo Municipal de Mar del Plata and Museo Argentino de Ciencias Naturales “Bernardino Rivadavia” (Buenos Aires, Argentina).
GMG conducted the analysis and wrote the manuscript with contributions from all co-authors. OFMM prepared the figures. OFMM and JLC were in charge of the logistics to study the specimen (MGN 931, IGM p002118) housed at the Museo Geológico Nacional (MGN), Servicio Geológico Colombiano (Bogotá, Colombia).
The authors declare that they have no conflict of interest.
The authors are grateful to Cecilia Deschamps, Darin Croft, Spencer G. Lucas and to the anonymous reviewer of a previous version and the final version of the manuscript for their valuable comments and suggestions and for improving the English version; to the Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) for permanent financial support; and to the authorities of paleontological collections (AMNH, MACN, MGN, MLP, MMP, UF) for providing material for analysis. This work was partially funded by 11/N864 UNLP, PICT-2017-0765, PICT-2016-2698, PIP 0496, and the Evolutionary and Epistemological Biology Investigation Group (BIEVEP).
This work was partially funded by 11/N864 UNLP, PICT-2017-0765, PICT-2016-2698, PIP 0496, and the Evolutionary and Epistemological Biology Investigation Group (BIEVEP).
This paper was edited by Torsten Scheyer and reviewed by Spencer G. Lucas and one anonymous referee.
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