Systematics of african amphicyonidae, with descriptions of new material from Napak (Uganda) and Grillental (Namibia).
On the slopes of Akisim, Napak, Uganda (Fig. 1), extensive tree-cutting for the manufacture of charcoal has led to soil erosion in some sectors of the mountain, thereby exposing the underlying volcano-sedimentary deposits, which have long been known to yield abundant fossils (Musalizi et al., 2009).
One such erosion feature found in 2007 is the richly fossiliferous locality of Napak XV, not far from Napak V. Excavated over the next few years Napak XV yielded an astonishing variety of well preserved fossils including a complete skull of a gymnophionan (Rage and Pickford, 2011), articulated skeletons of rodents (Pickford et al., 2013, 2014), a skull and some postcranial remains of Ugandapithecus (Musalizi et al, 2009), a diversity of small apes (Pickford et al, 2010), and an assorted array of amphicyonid remains, which form the basis for the present revision.
Information about the geology of the volcanic setting of Napak is to be found in papers by King (1949), Trendall (1965), and Bishop and Trendall (1967), and other publications of a broad nature (Bishop et al, 1969; Pickford, 1986a; 1986b; 1986c). General works on the fauna, taphonomy and faunas are available (Bishop, 1958a; 1958b; 1962; 1963a; 1963b; 1964a; 1964b; 1967; 1968; 1971; 1972; Bishop and Trendall, 1967; Bishop and Whyte, 1962; Musalizi et al., 2009; Pickford and Senut, 1988; Pickford et al, 1986; Tricker et al., 1963).
Specialist studies of the fauna (Table 1) have been published. Pickford (1995, 2004) studied the fossil land snails from Napak. Rage and Pickford (2011) described a complete skull of a gymnophionan. Primates were dealt with by Allbrook and Bishop (1963) and other researchers (Bishop, 1964a; Fleagle, 1975; Fleagle and Simons, 1978; Gommery et al, 1998, 1999, 2002; Harrison, 1982, 1988; Leakey, 1967; Pickford et al., 2010; Pilbeam, 1969; Pilbeam and Walker, 1968; Rafferty et al., 1995; Senut et al., 2000; Simpson, 1967; Walker, 1969, 1974, 1978). Butler (1962, 1978a, 1978b, 1984) described the chalicotheres and insectivorans from the deposits. Hooijer (1966) and Guerin and Pickford (2003) dealt with the rhinocerotids from Napak, while Lavocat (1973) and Pickford et al. (2013, 2014) described the rodents. Morales et al. (2001, 2007) described new carnivorans from Napak following up on the pioneer work by Savage (1965) and the later studies by Schmidt-Kittler (1987) and Schmidt-Kittler and Heizmann (1991). The ruminants were studied by Pickford (2002) and Sanchez et al. (2015). Hyracoids were published by Tsujikawa and Pickford (2006) and Pickford (2013). Suids were studied by Wilkinson (1976) and Pickford (1986d).
The Napak deposits comprise predominantly sub-aerial volcanic ashes of carbonatitic and nephelinitic composition and palaeosols derived from these ashes. The base of the succession, called the Iriri Member, contains palaeosols and fluvio-palustral sediments, some of which are extremely rich in fossil remains. The higher levels of the succession, comprising the Napak Member, in which the sites of Napak I, IV, V, IX and XV occur, show few if any signs of aquatic deposition, being, in large measure, composed of subaerially deposited volcanic ash and immature palaeosols.
Seeds of Celtis are common in Napak XV, as are fragmentary leaves of dicotyledons, and stems of grasses or sedges and plant root traces. Fossil tree trunks are quite common in the agglomerates overlying the Napak Member, some layers of which contain abundant plant remains (wood, fruit, and leaves).
Fossils vertebrates in the Napak Member tend to occur as isolated fragments, but Napak XV is unusual in this respect, having yielded partial skeletons of a variety of vertebrates (crocodiles, rodents) and almost complete cranial remains (gymnophionan, Ugandapithecus, rodents, insectivores) and dentognathic fossils (relatively complete maxillae and mandibles of Limnopithecus, amphicyonids, tragulids, pecorans, suids).
The Napak deposits accumulated ca 20.5 Ma (Sawada et al., in progress) which correlates with the early Miocene (Aquitanian-Burdigalian of Europe). The palaeoenvironment on the slopes of the volcano was evidently forested with some open patches as shown by the fossil land snails (Pickford, 2004), and the domination of brachyodont and bunodont dentitions among the mammals. Open grassy areas did exist in the vicinity, as attested by the presence of hypsodont rodents (Diamantomys) (Lavocat, 1973), macroscelidids (Myohyrax) (Butler, 1962, 1978a) and rhinocerotids (Ougandatherium) (Guerin and Pickford, 2003).
This paper deals with the Napak amphicyonids Hecubides euryodon and Afrocyon sp. which are the largest fissiped carnivores known from the site, although they would have been dwarfed by the creodont Pterodon africanus. Hecubides euryodon and the slightly smaller barbourofelid Ginsburgsmilus napakensis would have had ample prey species at their disposal, concomitant with their body dimensions, including primates, hyracoids, suids and several ruminants (Table 1). Many of the fossil bones at Napak show bite marks and gnawing marks due to carnivore activity, as well as parallel gnawing traces made by rodents.
A note on an amphicyonid mandible from the Early Miocene of Grillental-VI, Sperrgebiet, Namibia (Fig.1) attributed to Hecubides euryodon, is included in order to contribute to the knowledge of this important species. Grillental-VI is located in the fossiliferous valley-fill sediments of the Northern Sperrgebiet, which are faunally similar to East African sites such as Songhor, Koru and Napak and to other Sperrgebiet sites such as Langental, Elisabethfeld and Grillental I-V, that are attributed to the Early Miocene, dated about 21-19 Ma (Pickford and Senut, 2008). The paper ends with a general discussion about African amphicyonids, including late Miocene forms.
The new material from Napak (NAP) described here is stored in the Uganda Museum (Kampala, Uganda). Fossils from the Speergebiet localities Arrisdrift (AD), Grillental (GT), Fiskus (FK) are curated in the Museum of the Geological Survey of Namibia (Windhoek, Namibia). Other specimens from Napak (NHM), Rusinga (NHM) and Gebel Zelten (NHM) are preserved in the Natural History Museun (London, UK). Specimens from Cynelos lemanensis from SaintGerand-le-Puy (SG) are curated in the Museum Nationale d'Histoire Naturelle (Paris, France).
2. Hecubides Systematic Description
ORDER Carnivora Bowdich, 1821
FAMILY Amphicyonidae Haeckel, 1866
SUBFAMILY Amphicyoninae Haeckel, 1866
GENUS Hecubides Savage, 1965
Included species: Hecubides euryodon Savage, 1965 (type species) and Hecubides minor Morales and Pickford, 2008.
Hecubides euryodon Savage, 1965
Type Locality: Napak I.
Age: Early Miocene (Faunal Set I, ca 20.5 Ma).
Holotype: NHM M-19805 (London), maxilla containing P3P4, M1-M2, and alveoli of P2 and M3 on both sides (Savage, 1965, Pl. 5-1).
Other localities: Uganda (Napak IV, Napak V, Napak XV); Kenya (Chamtwara, Koru, Mfwanganu, Rusinga, Songhor); Namibia (Grillental VI, Langental, Elisabethfeld).
Original Diagnosis: in Savage (1965, p. 289).
Emended Diagnosis: Amphicyoninae of medium size, similar in dimensions to European Cynelos lemanensis (SaintGerand-le-Puy, France). M3 and m3 not reduced, M1 and M2 similar to each other in size. M1 subtriangular, with well-developed metaconule united to the protocone, lingual part with a tendency to reduction. M2 subquadrate with broad lingual part. P4 with distinct protocone, and an incipient to well-developed parastyle. Mandible much elongated with diastemata between the premolars. The p4 has a strongly developed posterior cuspid, m1 with strong and voluminous metaconid, m2 big with reduced to absent paraconid, narrow talonid almost completely occupied by the hypoconid.
2.1. New material from Napak XV
NAP XV 97'07 + 150'07 + 91'08 right mandible comprised of three fragments found during different field seasons (Fig. 2-1). NAP XV 15'00, left mandible fragment, including part of the ascending ramus with the articular condyle. NAP XV 96'09, two fragments of left mandible, with part of the horizontal ramus, containing poorly preserved teeth. The state of preservation and wear of the teeth indicate that all these fragments, which were found close together, could comprise a single individual. NAP XV 162'08, moderately worn right m2 (Fig. 2-5); NAP XV 4'12, right m1; NAP XV 382'08, right M1 (Fig. 2-3); NAP XV 98'07, right M1 (Fig. 2-4); NAP XV 180'08, left M1 with damaged paracone-metacone; NAP XV 146'08, heavily worn left M2; NAP XV 127'07, deeply worn right M2; NAP XV 76'08, P4 (Fig. 2-2); NAP IX 14'02, right calcaneum (Fig. 3). Measurements in Table 2.
Mandible. NAP XV 97'07 + 150'07 + 91'08. The mandible is noticeably elongated (Fig. 2-1), very similar in dimensions and proportions to that of Cynelos lemanensis from Saint-Gerand-le-Puy (SG-490) figured by Ginsburg (1977). The dental series is damaged, only the canine, p3 and p4 being complete, although the last tooth is deeply worn, as is the canine. The p2 presents a small crack, and only the base of the m1 is preserved. The m3, m2 and p1 are missing, their alveoli filled with sediment. There are gaps between all the premolars and there is even a short diastema between the p4 and the m1 and a longer one between the canine and the p1. The p3, which is well preserved, is a small tooth with a low, elongated crown, with a main cusp showing long anterior and posterior crests. Posteriorly there is a small swelling, which interrupts the slope, forming a tiny, barely visible, cusplet. The p4 is also elongated but the crown is broken. The p2 was very reduced and, on the basis of its alveolus, the p1, which is missing, was uniradiculate. The jaw is broken distally in the region of the condyle. However, NAP XV 15'00, a left mandible fragment preserves the condyle in excellent condition, showing that it was short and lingually very broad. NAP XV 96'09, a fragment of left mandible, is heavily deformed (probably trampled) preserving the complete but deeply worn m2 and a damaged p4. NAP XV 162'08, a right m2 is quite worn lingually, missing the apex of the metaconid, but preserving a strong, globose protoconid (Fig. 2-5). The paraconid was probably absent, although the state of preservation of the tooth does not permit a firm conclusion to be reached, although close inspection reveals that the trigonid valley was very small, tall and closed anteriorly. The talonid is narrow, short, and has also lost its enamel, although it is possible to see that there is a swelling for the hypoconid, which would have occupied a large part of the surface of the talonid. NAP XV 4'12, is a well preserved right m1 with minor occlusal wear which affects the buccal wall and the apex of the protoconid and to a lesser extent, the anterior part of the paraconid and hypoconid. Lingually, the wear is heavier extending from the apex of the paraconid to the protoconid-metaconid and the hypoconid. The molar is gracile, with a relatively long paraconid, with an almost vertical anterior cristid and the metaconid is voluminous. The talonid is long, and broad, and is almost completely occupied by a globose, relatively low, hypoconid, which joins a peripherally positioned entocristid which extends to the base of the metaconid. The cingula are weak, almost non-existent except at the buccal base of the hypoconid.
NAP XV 76'08, a well preserved left P4 shows an incipient wear facet on its lingual wall, affecting part of the paracone and the metastyle (Fig. 2-2). The presence of a well-formed parastyle is notable. The protocone is slightly displaced posteriorly with a well-formed conical cuspid. The basal cingulum is continuous but weak buccally and strong lingually. NAP XV 382'08, a well-preserved right M1, is a subtriangular, quite long tooth (Fig. 2-3). The paracone is somewhat taller and larger than the metacone, and its apex shows a horizontal wear facet that extends onto the posterior crista. The lingual cingulum is weak. There is a well-defined parastyle which shows a contact facet with the P4. The trigone valley is shortened with respect to the lingual wall of the buccal cusps, and is delimited by the well-developed metaconule and a large, globose protocone, which continues lingually without separating from the lingual cingulum which is only well marked in the zone between the metaconule and protocone. Three clear wear facets affect 1) the metacone, especially at the junction with the base of the metacone and at its apex 2) the central valley of the trigone extending onto the inner wall of the protocone, and 3) the base of the junction between the protocone and paracone. NAP XV 180'08 is a left M1 in which the external part has split away almost vertically such that only the lingual parts of the paracone and metacone are preserved. There is a clear, well-developed, metaconule and a sharp separation between the protocone and the lingual cingulum. The wear facets are similar to the ones on the specimen described above. NAP XV 98'07, a right M1, is smaller than the molars described above, and has lost the enamel in the area of the parastyle and metastyle (Fig. 2-4). The buccal cingulum is quite well marked but remains weak. The rest of the morphology is similar to the teeth described above, although occlusal wear is more advanced in the zone of the metaconule and the trigone valley. The main difference from the molars described above concerns the lingual cingulum which is well-formed and clearly separated from the protocone. NAP XV 146'08 and NAP XV 127'07 are left and right M2s respectively, both of which are heavily worn. They differ from the M1 by their more rectangular occlusal outline without marked narrowing of the area of the trigone. The trigone cusps appear to be quite low, at least in comparison with those of the M1.
NAP IX 14'02, right calcaneum (Fig. 3). The size and morphology of the calcaneum indicate that it is close to that of Cynelos lemanensis, decribed and figured by Ginsburg (1977) from Saint Gerand-le-Puy, France. The fibular tuberosity is less well-developed than in this species, but this could be due to the state of preservation, which is slightly abraded as is the dorsal part of the tuber calcanei. The facet for the cuboid is short and ovoid in outline, differing from the sub-triangular outline seen in Amphicyon major (Ginsburg, 1961, Fig. 15, 2). This difference could be related to the lesser medial lateral extension of the sustentaculum tali. Overall, the articular zone for the talus in the Napak calcaneum indicates a lesser degree of plantigrady than was present in Amphicyon major (Fig. 4). Comparison with the calcaneum of Afrocyon ginsburgi (= Ysengrinia ginsburgi) from Arrisdrift (Morales et al., 2003. Pl.4, Fig. 3) show that the Napak specimen is quite a bit smaller, about 20% smaller in its maximum dimension (proximo-distal length) but morphologically close to it; both share the ovoid outline of the cuboid articulation, which is quite deep, and a small medio-lateral development of the sustentaculum tali. Indeed, apart from the size difference, the two specimens are closely similar (Fig. 4).
Comparison with Napak I
The new material from Napak XV adds to our knowledge of the species Hecubides euryodon, defined by Savage (1965) on the basis of fossils from Napak I, especially regarding the mandible and lower dentition which was less well known than the upper teeth. The mandible from Napak XV is the first known adult specimen of the species and allows us to obtain more precise information regarding the dentition of H. euryodon, which has four relatively small premolars, separated from each other by diastemata. The mandible is noticeably elongated and it suggests that the rostral part of the skull of H. euryodon was elongated. The lower molars, especially the m1, are close to the material from Napak I, in particular NHM M 19085 (paratype of the species), which shares the strong development of the metaconid, the barely distinguishable entoconid that is essentially a peripheral cristid, and the overall bunodont aspect of the tooth. The upper teeth from Napak XV are close in dimensions to those in the holotype maxilla (M 19084) and show no clear morphological differences, apart from those mentioned in the discussion concerning the M1, NAP XV 382'08, which has lingual morphology which is somewhat divergent from other specimens from the same locality, and different from the molars from Napak I, in that the separation between the protocone and lingual cingulum is clearly marked. Another interesting difference in our opinion, is the stronger development of the parastyle in the P4 from Napak XV compared with the fossils from Napak I. Morales et al. (2007) described additional material of this species from Napak I including upper and lower deciduous teeth and an unworn molar. In conclusion, the forms from Napak I and Napak XV can be classified in the same species without any difficulty. Schmidt-Kittler (1987) described various specimens from other localities in the Lower Miocene of East Africa and identified them as Cynelos euryodon. Among the fossils he studied were a m2 from Napak I (NAP-1), close in dimensions and morphology to NAP XV 162'08, the two molars lacking a paraconid, the trigonid valley being high and small, and the talonid narrower than the trigonid.
In addition, Schmidt-Kittler (1987) reported the presence of this species at several other lower Miocene localities in Kenya including Rusinga and Songhor, as already noted by Savage (1965) and at Chamtwara. Schmidt-Kittler (1987) commented on the homogeneity of the African fossils when compared to the greater morphological diversity which is evident in European species of Cynelos, and he noted that the observed differences in the teeth from the African localities are small and could be related to differences in geological age. In the present state of our knowledge this inference appears to be correct, and although there are differences in size, in particular the small m1 from Songhor (KNM SO-5668) or the greater dimensions of the m1 Napak IV (HMV-5830), most of the remains are remarkably homogeneous. The same is indicated by the morphology, the few differences observed in a single locality such as among the M1s at Napak XV, or the M2s at Chamtwara (Schmidt-Kittler, 1987) being of minor significance. Like the variation in dimensions, the morphological variation within a single locality could be extrapolated to different localities, including the presence of a relatively strong parastyle in the P4 from Napak XV, contrasting with the weaker or incipient parastyle in the P4 from Napak I. More material is required to demonstrate that the range of morphometric variation observed in the dentitions attributed to Hecubides euryodon might exceed species level variation.
Comparison with Cynelos lemanensis
Whilst the homogeneity of Hecubides euryodon appears to be clear at the species level and is now better documented, the validity of the genus Hecubides has been doubted on several occasions, with different authors synonymising it with Cynelos. Savage (1965) included Amphicyon lemanensis in his new genus, but the same year, Kuss (1965) revalidated (reutilised) the genus Cynelos Jourdan (1862) for the species A. lemanensis Pomel (1846). On this basis the combination Cynelos euryodon employed by Schmidt-Kittler (1987) for the African forms seemed to be beyond discussion. This was also the opinion supported by more recent authors such as Morlo et al. (2007) and Werdelin and Peigne (2010). In contrast Morales et al. (2007), Morales and Pickford (2008) and Morales et al. (2010) have used the Hecubides for these first African amphicyonids.
Hecubides euryodon is extraordinarily similar in dimensions to Cynelos lemanensis, at least as far as the dentition is concerned, and very few molars fall outside the range of variation known for the latter species in its type locality (SaintGerand-le-Puy, France), as can be observed in figures 5 and 6. The two species are longirostral with gracile and elongated mandibles. The anterior premolars (p1-p3) are reduced and separated from each other by diastemata. The large dimensions of the second molars (M2 and m2) with respect to the first ones (M1 and m1) is similar in the two forms (Fig. 6), and apart from other considerations is a solid indication of a close relationship between them, especially if we consider that the tendency to broaden the crushing molars is a derived character of the Amphicyonids, less common than the reduction of the post-carnassial molars. There are thus sufficient arguments to unite the two genera and to support the view that they are synonyms. Nevertheless some morphological characters indicate differences between these two species, in particular the incipient development in H. euryodon of a parastyle in the P4, starting from the union of the anterior crista of the paracone with the cingulum (NAP XV 76'08). In adddition the African species shows a clearly defined protocone. The M1 of H. euryodon shows a clear reduction of the protoconal zone, such that the protocone cingulum is almost central and very reduced, whereas in Cynelos lemanensis the protoconal area is less reduced and is more subquadrate. This fact is not evident in the figure published by Savage (1965, Pl. 5), probably due to an effect of light and shadow. In NAP XV 382'08 it is more than clear. However, it should be pointed out that Cynelos piveteaui Ginsburg (1966) shares with H. euryodon some of these features, in particular the narrowing of the protoconal area in the M1 and a better defined protocone in the P4. Nevertheless, it differs from H. euryodon by the greater development of the buccal cingula, and by the greater dimensions and robusticity of the P4, in which there is not a clearly defined parastyle. In the lower dentition, the differences are fainter, apparently in H. euryodon the hypoconid of the m1 seems to be somewhat more strongly developed, such that the lingual part of the talonid is narrower. Likewise the m2 of H. euryodon possesses a more reduced talonid, practically occupied by the hypoconid while in C. lemanensis the talonid is broader and possesses a relatively strong entoconid. Furthermore C. lemanensis presents a strong paraconid, equal to that of C. piveteaui, a cuspid that has been lost in H. euryodon. As has been pointed out, it is possible that the two genera were closely related, but the differences, although always difficult to evaluate in a family in which there is remarkable dental homogeneity (with some exceptions), tend to validate the independence of Hecubides. This is especially so when younger forms, some of which have also been included in Hecubides (or by some authors in Cynelos), the case with H. macrodon or Hecubides sp. from Wadi Moghara (Savage, 1965; Morlo et al., 2007), being more divergent from the standard morphology of Cynelos, as we discuss below, but showing closer affinities with Hecubides.
2.2. New material from Grillental VI
Locality: Grillental VI, Sperrgebiet, Namibia (Data about locality and fauna in Pickford and Senut (2008).
Age: Early Miocene (Faunal Set I, ca 20 Ma).
GT 35'15 is a left mandible containing p4-m2 and the alveoli of p3 and m3 (Fig. 7). The ascending ramus is broken off. The horizontal ramus is deep, and anteriorly shows a mental foramen, probably positioned beneath the p2 (which is not preserved) and the masseteric fossa is extensive and deep in its most posterior part. The specimen is close in dimensions and morphology to Hecubides from Napak V (Fig. 6, Table 2). The p3 has two roots and is separated from the p4 by a diastema. The p4 is damaged at is apex, posteriorly it is enlarged and possesses a well-developed posterior cusp and the main cusp would have been quite tall. The m1 is poorly preserved, retaining the antero-lingual part of the paraconid, the base of the protoconid and much of the talonid, in which a large hypoconid can be seen in a lingual position, and a crestiform entoconid. The m2 is broad with a short talonid. The protoconid is well-developed and is taller than the metaconid. There seems not to have been a metaconid. There also seems to be no paraconid, although the antero-lingual corner of the tooth is missing. The valley in front of the trigonid is small and is bordered anteriorly by a subtle cingulum. The talonid is dominated by a large hypoconid, and in the lingual margin, in the best preserved part, the beginning of a crest in the position of the entoconid can be observed. The posterior margin of the talonid is narrowed in its lingual part. There is a relatively big alveolus for the m3 in the jaw.
The new amphicyonid mandible from Grillental VI is the most complete specimen found in the early Miocene localities of the Sperrgebiet (excluding the site of Arrisdrift). In effect, in the sites of Langental, Elisabethfeld, Fiskus and Grillental amphicyonids were known, but only by post-cranial elements, save for an upper canine from Langental (LT 164'98). For this reason, the amphicyonids from the area were attributed to Ysengrinia sp. (Morales et al., 2008). Even though the preservation of the Grillental mandible is not excellent, it permits us to classify it as Hecubides euryodon for the following reasons; the dimensions of the jaw and of the teeth preserved in it, which are close to the smallest individuals of the species, represented by an m2 from Napak XV (Nap XV 162'08) and an ml from Songhor (KNM SO 5668); the p4 is close to a specimen described by Morales et al. (2007) from Napak I, sharing the posterior expansion and the posterior accessory cusplet; and the m2, without paraconid and with a short and postero-lingually narrowed talonid; all of which are charactersitic of the taxon. It is likely that most of the post-cranial bones from Langental, Elisabethfeld and Grillental can also be attributed to Hecubides euryodon on the basis of their dimensions which are compatible with the jaw. This species is smaller than Afrocyon ginsburgi from Arrisdrift (Morales et al., 2003).
3. Systematic approach to African Amphicyonidae not Hecubides
A classic problem with the palaeontology of carnivores is the relation between the upper and lower dentitions especially when there is scarce material, and/or which may belong to more than one species of the group, a situation which is quite common among the Amphicyonidae. The criterion of size on its own, with some exceptions, is difficult to apply on account of the presence of sexual dimorphism and bimodality, and because there is often overlap in dimensions of different species (Dehm, 1950). Additionally, as correctly one reviewer (L.W.) has pointed out "several of the type specimens of African Amphicyonidae are limited in scope or poorly preserved". For these reason the use of genera as Afrocyon and Myacyon poses serious problems. Conscious of this reality, however, we have preferred to use these existing names. The new material from Gebel Zelten described by Morales et al. (2010) in some ways compensates the poor preservation of the Afrocyon burolleti holotype. The case of Myacyon is completely different because it is not easy to find a holotype with quality to name a new genus, and restrict Myacyon domjabir to the type locality.
SUBFAMILY Amphicyoninae Haeckel, 1866
Genus: Afocyon Arambourg, 1961
Type species: Afrocyon burolleti Arambourg, 1961
Diagnosis: Werdelin and Peigne (2010).
Differential diagnosis: Apart from its smaller dimensions, Afrocyon differs from Amphicyon major and Megamphicyon giganteus by its clearly more hypercarnivorous dentition, which is more sectorial, the p4 is reduced, and the talonids of m1 and m2 are reduced although the hypoconid is more developed. Similarly, in the m2 of Afrocyon burolleti (NHM M 82374) the morphology is clearly more primitive than it is in Amphicyon major, as revealed by the retention of the paraconid, the taller and larger dimensions of the protoconid with respect to the metaconid, and its posterior position. Comparable differences apply to Megamphicyon giganteus, a species with larger premolars with barely any gaps between them. Afrocyon differs from Hecubides Savage (1965), not only by its greater dimensions, but mainly by its markedly more hypercarnivorous dentition. Finally, Afrocyon differs from Myacyon by the lesser developed carnassials (P4/m1), and the minor size of the parastyle in the P4.
Afrocyon burolleti Arambourg, 1961
Type locality: Gebel Zelten, Libya.
Age: Early/Middle Miocene, ca. 17-15 Ma.
Holotype: MNHN 1961-5-7, left mandible with abraded cheek teeth (p4-m3).
Remarks: New material was described by Morales et al. (2010) from Gebel Zelten. NHM M-82373, left mandible containing well preserved p4-m2, the alveoli for m3, p3 and p2 (Fig.8 and 9.1). NHM M-82374, left m2.
Afrocyon ginsburgi (Morales et al., 1998)
1978 Amphicyon cf. steinheimensis Hendey
1998 Ysengrinia ginsburgi Morales et al.
2003 Ysengrinia ginsburgi Morales et al.
2010 Ysengrinia ginsburgi Werdelin and Peigne
Type Locality: Arrisdrift, Namibia.
Age: Early Miocene, ca. 17.5-17 Ma.
Holotype: AD 133, left mandible.
Diagnosis: In Morales et al. (1998).
Remarks: The presence of a large M2 in this species excludes their classification as Ysengrinia. Even though the maxilla of Afrocyon ginsburgi AD 604'94 (Fig. 9.5) does not have an M2, the existence of an edentulous maxilla (Morales et al., 2003), which shows alveoli with appropriate dimensions, indicates that the M2 in the Namibian species was not reduced (Fig. 9.6), at least to the stage observed in the type species of the genus, Ysengrinia gerandiana (Viret, 1929; Ginsburg, 1966). Afrocyon ginsburgi differs from A. burolleti by its slightly smaller dimensions, and by the reduction of the m2. The only m2 preserved at Arrisdrift is somewhat smaller than the specimens from Gebel Zelten (Morales et al., 2010), and they differ in morphology, in particular by the strong elongation of the talonid. The differences between the material from Arrisdrift and Gebel Zelten are minor when compared with the m1s. However, this tooth is quite homogeneous among the African amphicyonids. Therefore, we are in the presence of a group of forms that are characterised by: significantly larger dimensions than Hecubides euryodon; lower carnassial relatively short with a vertical paraconid and strong hypoconid (Figs. 1, 3, 4), unreduced second molars, and a tendency to elongated the P4 which possesses an incipient parastyle.
Afrocyon macrodon (Savage, 1965)
1987 Cynelos macrodon Schmidt-Kittler
2010 Cynelos macrodon Werdelin and Peigne
Type Locality: Site 31, Rusinga, Kenya.
Age: Early Miocene, 18-17 Ma.
Holotype: NHM M-19086 left M1.
Diagnosis: In Savage (1965).
Measurements in Table 2.
Remarks: The greater dimensions of one M1 from Rusinga (Fig. 9.2), compared to the dentition classified as Hecubides euryodon from the same locality, prompted Savage (1965) to define a distinct species Hecubides macrodon, which Schmidt-Kittler (1987) considered to be ?Cynelos macrodon. This species was cited by Morales and Pickford (2008) at Kipsaraman, Kenya, on the basis of an isolated M2, now attributed to Myacyon kiptalami, a species also present in the site. A m1 found at Rusinga (NHM M-34303) not figured nor described by Savage (1965) is also attibuted to this species (Fig. 9.3). Afrocyon macrodon could be conspecific with Afrocyon burolleti, but the limited material does not permit precise comparisons.
Afrocyon nov. sp.
2007 Cynelos nov. sp. Morlo et al.
2010 Cynelos sp. Werdelin and Peigne.
Type Locality: Wadi Moghara.
Age: Early Miocene, 18-17 Ma.
Remarks: Morlo et al. (2007) classified four teeth collected at Wadi Moghara, Egypt, as Cynelos sp. nov., the dimensions of which are almost the same as those of Afrocyon macrodon from Rusinga, at least as concerns the m1 and M1 represented in both localities. There are no great differences in the morphology of these molars, in the m1 the hypoconid is voluminous and occupies the greater part of the talonid, but the m1 of Afrocyon buroleti and Afrocyon ginsburgi are in these respects similar. The M1 from Wadi Moghara is a bit more triangular and with a marked narrowing in the protoconal area, as occurs in Hecubides euryodon, but also as in the holotype of A. ginsburgi (Morales et al., 1998). Nevertheless, the lengthening of the P4 is notable, and by this feature and the presence of a clearly defined parastyle, it differs from the Arrisdrift species, the P4 of which is short with only an incipient parastyle. Finally, the presence at Wadi Moghara of a large M2 (Fig. 8), a feature which it shares with at least Hecubides euryodon, Afrocyon ginsburgi, and Myacyon kiptalami (= Agnotherium kiptalami). However, seen in the light of African Amphicyonidae, neither Ysengrinia nor Agnotherium appear to be sustainable as valid genera for these African species. Afrocyon nov. sp. from Wadi Moghara cannot be differentiated from A. macrodon, nor from A. burolleti, but its upper teeth show differences from those of Afrocyon ginsburgi in particular the lengthening of the P4, a tendency which is fully developed in more modern African amphicyonids classified as Myacyon (Fig. 8).
Locality: Fiskus, Namibia.
Age: Early Miocene (Faunal Set I, ca. 20 Ma).
FS 17'03 right calcaneum (Morales et al., 2008, Fig. 3, table 4) is clearly larger than the specimen from Napak XV described as Hecubides euryodon, and is close in dimensions to Afrocyon ginsburgi, and while its poor preservation does not permit precise comparisons, it does indicate the presence of a second species of Amphicyonidae in the Sperrgebiet localities, which can be named Afrocyon sp.
Locality: Napak 1.
Age: Early Miocene (Faunal Set I, ca. 20.5 Ma).
NAP-I 7'99 is a left M2 (Fig. 2.6) considerably larger than the homologous tooth of Hecubides euryodon (Table 2). It is a low-crowned tooth, almost completely surrounded by a cingulum, especially strong postero-lingually. The paracone is slightly taller than the metacone, the protocone is large and displaced mesially. Morphologically the tooth is very close to the M2 from Wadi Moghara identified by Morlo et al. (2007, Fig. 4-D). Nevertheless, with only one M2 available it is difficult to make an accurate identification and, as in the case of Grillental-VI we propose to attribute this tooth to Afrocyon sp., emphasizing the presence of two amphicyonid species in the Early Miocene deposits of Napak.
Genus: Myacyon Sudre and Hartenberger, 1992
Type species: Myacyon dojambir Sudre and Hartenberger, 1992
Diagnosis: In Sudre and Hartanberger (1992); modified by Werdelin and Peigne (2010).
Myacyon dojambir Sudre and Hartenberger, 1992
2010 Myacyon dojambir Werdelin and Peigne
Type Locality: Oued Mya, Algeria.
Age: Late Miocene, ca. 11.2-9 Ma.
Holotype: Right mandible with m1-m2, and m3 not yet erupted.
Diagnosis: In Sudre and Hartanberger (1992).
Remarks: Myacyon dojambir was described by Sudre and Hartenberger (1992) from the Late Miocene of Oued Mya 1, on the basis of a mandible containing m1-m2, poorly figured, approaches the dimensions of large Megamphicyon giganteus from Europe. It differs from them by the greater strength of the metaconid in the m1, a talonid narrower than the trigonid in the m2, as well as its smaller dimensions with respect to the m1.
Myacyon kiptalami (Morales and Pickford, 2005)
1997 Agnotherium sp. Pickford and Senut
2005 Agnotherium kiptalami Morales and Pickford
2008 Agnotherium cf. kiptalami Morales and Pickford
2010 Agnotherium kiptalami Werdelin and Peigne
Type Locality: 2/10, Kabarsero, Ngorora Formation, Kenya. Other localities: Kipsaraman, Kenya; Hondeklip Bay, South Africa.
Age: Middle Miocene, 16-12 Ma.
Holotype: KNM BN 488, snout broken off behind the second molars.
Diagnosis: In Morales and Pickford (2005).
Remarks: We mentioned above that the presence of a large M2 in several African forms as A. ginsburgi excludes their classification as Ysengrinia, and that the same criterion could apply to the forms classified as Agnotherium which retain large M2s, the case with Agnotherium kiptalami from the Ngorora Formation (Morales and Pickford, 2005). Agnotherium was, and is, a genus which is difficult to define, because it was erected on the basis of an isolated m1 (Kaup, 1832), and the reconstruction of the upper dentition by Kuss (1962) on the basis of specimens from Frohnstetten, was questioned by Kurten (1976) which caused much confusion by emphasizing that the reduction of the molars, in comparison to the size of the carnassial was not excessively marked. The problem is not solved transferring the Frohnstetten form to Tomocyon or Thaumastocyon as proposed by Kurten (1976), because the holotype of Agnotherium is indistinguishable of the m1 of Thaumastocyon bourgeoisi (Stehlin and Helbing, 1925) a genus which shows a reduction of the molars which is notable at least since the Middle Miocene, which also is present with Thaumastocyon dirus from the Upper Miocene of Los Valles de Fuentiduena (Ginsburg et al., 1981). However, ever since the Early Miocene, first with Ysengrinia and then with Thaumastocyon plus Agnotherium and Tomocyon, this group of hypercarnivorous amphicyonid shows a strong tendency for the reduction of the molars, which makes it incompatible that forms such as that described from Ngorora can be classified in Agnotherium. The presence of a large m2 in the Ngorora species (Morales et al., 2010) adds to the arguments in favour of a different generic identification for this form. Agnotherium has also been reported from Kipsaraman, on the basis of a mandible and a canine, as Agnotherium cf. kiptalami (Morales and Pickford, 2008). This material, in line with what was written above, could well be associated with the M2 identified as Hecubides macrodon from the same locality and included in this species. The P4 from Hondeklip Bay described by Pickford and Senut (1997) as Agnotherium sp. can also be attributed to this species (Morales and Pickford, 2005).
Myacyon cf. kiptalami (Morales and Pickford, 2005).
1976 Agnotherium cf. antiquum Kurten
2003 Amphicyonidae sp. A. Werdelin
2005 Amphicyonidae indet. Tsujikawa
2010 Agnotherium cf. antiquum Werdelin and Peigne
2010 Amphicyonidae sp. A Werdelin and Peigne
2010 Amphicyonidae indet. Werdelin and Peigne
Localities: Beglia Fm., Tunisia. Samburu and Lothagam, Kenya.
Age: Middle/Late Miocene, 13-6 Ma.
Remarks: Kurten (1976) included in Agnotherium antiquum a fragment of maxilla from the Beglia Formation, Tunisia, with a long P4 and alveoli of the M1 which shows that the tooth must have been quite big, in particular its length. The species from Beglia are among the largest in Africa, and morphologically is close to the species of Ngorora.
The mandible with m2 described by Tsujikawa (2005) from the Samburu Formation has slightly smaller dimensions but very similar morphology to the m2 described from Ngorora (Morales and Pickford, 2010). This m2 is also close to M. dojambir but somewhat more gracile, the cingulum of which is barely developed, a difference from M. dojambir. This determination should be extended to the M2 from Lothagam described by Werdelin (2003) as Amphicyonidae species A, wich size is close to M2 from Ngorora species,
Myacyon sp. I
2005 Agnotherium sp. Morales and Pickford
2009 Agnotherium sp. Werdelin and Simpson
2010 Agnotherium sp. Werdelin and Peigne
Locality: Fort Ternan, Kenya.
Age: Middle Miocene, ca. 14 Ma.
Remarks: Agnotherium has also been described from Fort Ternan (Morales and Pickford, 2005; Werdelin and Simpson, 2009). As in other sites the material is scarce, a damaged m1 the size of which could correspond to species of Afrocyon. It preserves a strong metaconid, already lost early in the Thaumastocyoninae, but the paraconid shows a strong anterior vertical cristid, a structure which is seen in m1s of Thaumastocyon. The M1 and P4 are relatively small, smaller than the measurements of species of Afrocyon. The presence of a parastyle in the P4 and the antero-posterior shortening of the protoconal area in the M1 are features present not only in Afrocyon, but also in the forms discussed in this section. Like the available material, the Fort Ternan amphicyonid could still be identified as Afrocyon sp., or could equally correspond to a small form of Myacyon.
Myacyon sp. II
1977 Agnotherium cf. antiquum Ginsburg
2010 Agnotherium cf. antiquum Werdelin and Peigne
Locality: Beni Mellal, Morocco.
Age: Middle Miocene, ca. 14 Ma
Remarks: The morphology of the m2 de Beni Mellal is apparently close to that of Myacyon dojambir (Sudre and Hartenberger, 1992) with a short talonid and a robust cingulum but it is considerably smaller.
Genus: Bonisicyon Werdelin and Simpson 2009
Type species: Bonisicyon illacabo Werdelin and Simpson 2009
Diagnosis: In Werdelin and Simpson 2009.
Bonisicyon illacabo Werdelin and Simpson 2009
2003 Amphicyonidae species B. Werdelin
2007 Simocyon sp. Howell and Garcia
2010 Bonisicyon illacabo Werdelin and Peigne
Type locality: Hamadi Das, Gona, Ethiopia Holotype: HMD1/P11, right m1.
Age: Late Miocene, 6.5-5.3 Ma.
Remarks: Bonisicyon illacabo was erected by Werdelin and Simpson (2009) for a group of fossils from various localities, characterised by their small dimensions and their more recent age (end Miocene) (Fig. 6). The holotype is an m1, from Gona (Ethiopia), similar in size to Hecubides euryodon, which however possesses a metaconid which is almost entirely reduced and quite a broad talonid and thereby differs from the latter taxon. From the same zone came a poorly preserved m2 which is markedly different in its squarer talonid from specimens of Hecubides euryodon. However, the M1 from Lemudong'o, Kenya, previously described as Simocyon sp., by Howell and Garcia (2007) and attributed to Bonisicyon by Werdelin and Simpson (2009) shows substantial differences from the Ml of Hecubides euryodon, in particular the strong reduction of the protoconal area, the almost perfectly semicircular morphology of the protocone in which the paraconule can barely be differentiated, and by the strong lingual cingulum.
With such scarce evidence it is difficult to determine the relationships to other African amphicyonids, and like Hecubides minor from Kipsaraman (Morales and Pickford, 2008), defined on the basis of an m2 which is smaller than that of Hecubides euryodon and Bonisicyon illacabo, these small forms need a better fossil record before a more plausible hypothesis about their phyologeneitc relationships can be proposed.
Caniformia indet. aff. amphicyonidae
Morales et al. (2005) referred a right P4 (KNM LU 227) from the Lukeino Formation (Kenya) to Plesiogulo praecocidens. Although the presence of the genus Plesiogulo in this formation is certain, this P4 must be excluded from the genus, which would be represented by a lingual part of an Ml (BAR 1893'00). Plesiogulo was recently described from Lemudong'o (Kenya) and Adu Dora (Ethiopia) aged 5, 5-6 Ma belonging to the new species P. botori Haile-Selassie et al. (2004). Morphologically the large mustelid from the Lukeino Formation accords better with this new species than with P. praecocidens.
The P4 from Lukeino (Fig. 10) presents an interesting association of morphological characters which clearly distinguishes it from Plesiogulo (and by extension from modern Mustelidae), such as the retention of a strong notch between the protocone and metastyle (loss of this notch is a derived feature of modern mustelids), as well as the reduction of the protocone, its relatively distal position and weak individualisation with respect to the paracone. The caniform morphology of this P4 seems beyond discussion, but its familial attribution is more problematic. The dimensions of the carnassial are close to those of Hecubides euryodon, although the tooth is more robust, in general it could correlate well with Bonisicyon illacabo (Fig. 6). However, the majority of the more modern Amphicyonidae, even though they present a strong reduction of the protocone of P4, it is rarely retracted. On the contrary in the Hemicyonidae the protocone of P4 is shifted distally, but not reduced, and soon increases in size. For this reason, the Lukeino form accords well with primitive species of the family Hemicyonidae, such as Hemicyon gargan or Hemicyon stehlini (Ginsburg and Morales, 1998). The Hemicyonidae are frankly rare in African faunas, but they occur in the Lower Miocene of Rusinga, where a P4 is known (Schmidt-Kittler, 1987), and near the Mio-Pliocene boundary, with the spread of Agriotherium (Morales et al, 2005), although the latter genus has a highly divergent P4 morphology compared to the Lukeino specimen. It is not reasonable to think of an alternative to Hemicyoninae, or by extension of Ursidae (which also possess highly derived P4). Similar morphology of the Lukeino P4 occurs in Simocyon, an Ailuridae which shows several dental convergences to Amphicyonidae, so much so that one of the molars (Ml) attributed to Bonisicyon illacabo was originally identified as Simocyon.
The P4 of Simocyon has a morpholoigcal pattern which is close to that of the Lukeino tooth, the parastyle is variable, depending on the species, in S. diaphorus from Rudabanya, Hungary, it is practically absent (Werdelin, 2005), whereas in S. batalleri from Batallones, Spain, and other more modern species such as S. primigenium is well-developed (Peigne et al, 2005). The position of the protocone in Simocyon appears to be related to the development of the parastyle, such that in S. diaphorus from Rudabanya the protocone occupies a very anterior position, in front of the the anterior border of the paracone, although it certainly extended distally. In contrast, in S. batalleri and S. primigenium in which the parastyle is well-developed, the protocone is positioned more distally, but also front of the paracone, or which is the same, it starts developing at the level of the separtion between the paracone and parastyle. As such, the Lukeino P4 does not correspond to any of these morphotypes, differing from that of S. diaphorus by the distal position of the protocone, and from S. batalleri and S. primigenium by the weak development of the parastyle. If we take into account the fact that until now there is no reliable record of Ailuridae in African faunas the hypothesis that the Lukeino P4 is related to this family seems improbable.
In summary, the Amphicyonidae hypothesis seems more plausible at the moment, two possibilities could give rise to this morphology; 1) from Afrocyon-Myacyon. In these forms the tendency for the P4 to develop parastyles could displace the protocone into a more distal position. Adaptation to a smaller size could be accompanied by regression of the parastyle, conserving the protocone in its distal position; 2) the Lukeino P4 could be related to Amphicyonidae in which the protocone of the P4 maintained its strong development, as in Pseudarctos and Ictiocyon (Ginsburg, 1999). It is evident that identification of the Lukeino P4 as an Amphicyonidae is likely, not only because of its morphology but also because of its dimensions and age, which are close to those of Bonisicyon illacabo.
4. Phylogenetic proximity
The available data about African amphicyonids are still insufficient for carrying out a rigorous analysis of their phylogenetic relationships. There are too many gaps and important questions without documentation. Nevertheless, the main aim of this contribution is to arrange the available information about this family in Africa (Fig. 11). The first conclusion that emerges is that there is a great deal of morphological homogeneity in the family in Africa, apparently confined to a single phylogenetic lineage, comprised of Hecubides-Afrocyon-Myacyon, with the exception of the large amphicyonid from Arrisdrift, identified as Megamphicyon giganteus (Morales et al., 1998) and the younger Bonisicyon illacabo Werdelin and Simpson (2009), the latter of which could be related to Hecubides, as discussed above.
It is clear that there is a strong resemblance between the first amphicyonids classified as Hecubides euryodon and the larger forms Afrocyon and Myacyon. The greater dimensions of Afrocyon can be related to morphological differences between the species of Afrocyon and Hecubides, in particular the stronger paracone in the M1 and the greater sectoriality of the m1 with a high and sharp trigonid. But above all, the great elongation of the P4 and to a lesser extent the m1, mark an important qualitative jump which allows us to separate Hecubides from Afrocyon. Relations within the genus Afrocyon are not resolved because of which we leave the specific status as it was. Myacyon is close to Afrocyon, but the tendency to elongate the carnassials, in the case of the P4 in addition developing a strong parastyle, led to some of these forms being previously related to Agnotherium (Kurten, 1976; Morales and Pickford, 2005) but the retention of relatively large post-carnassial molars renders this proposal unlikely. As in the case of Afrocyon, the relation between the species attributed to Myacyon is not resolved, and only a better fossil record will yield a solution. Forms such as those from Fort Ternan and Beni Mellal may be included in the genus Myacyon, in spite of their dimensions being closer to those of Afrocyon for the reasons pointed out above, the m1 from Fort Ternan is quite derived with respect to the species of Afrocyon (on the basis of this molar) and the m2 from Beni Mellal show undoubted morphological similarities to Myacyon dojambir, including the development of a strong buccal cingulum. Provisionally we call them Myacyon sp., in the hope of obtaining better documentation.
MP thanks the Sorbonne Universities for financial and administrative support. Thanks to the French Ministry of Foreign Affairs (Commision des Fouilles) and the Museum National d'Histoire Naturelle, Paris (B. Senut, S. Crasquin), and Namdeb (J. Jacob, Oranjemund) for funding field work in Uganda and Namibia. Thanks to the Uganda Museum (R. Mwanja, S. Musalizi) for providing access to fossil material and participating in field surveys, and the Geological Survey of Namibia (G. Schneider, G. Simabuli, H. Mocke) for local affiliation and assuring access to fossils. Research permits were issued by the Namibian National Heritage Council and the Uganda National Council for Science and Technology. We thank Philippa Brewer, NHM London, and Christine Argot, MNHN Paris, for access to the collections in their care. Project CGL2015-68333, MINECO (Spanish Government) and The Research Group BSCH-UCM 910607. A.V is Research student in the CSIC program JAE-PRE_CP2011 (CSIC program "Junta para la Ampliacion de Estudios"), co-funded by the European Social Fund. We thank the reviewers Humberto Astibia and Lars Werdelin for their useful comments and suggestions, which improved the original manu-script.
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J. Morales (1) *, M. Pickford (2), A. Valenciano (3,4)
(1) Departamento de Paleobiologia, Museo Nacional de Ciencias Naturales-CSIC, C/ Jose Gutierrez Abascal, 2, 28006 Madrid, Spain.
(2) Sorbonne Universites - CR2P, MNHN, CNRS, UPMC - Paris VI, 8, rue Buffon, 75005 Paris, France.
(3) Departamento de Geologia Sedimentaria y Cambio Medioambiental. Instituto de Geociencias (CSIC, UCM), c/Jose Antonio Novais, 12, 28040 Madrid, Spain.
(4) Departamento de Paleontologia, Facultad de Ciencias Geologicas Universidad Complutense de Madrid, 28040 Madrid, Spain.
e-mail addresses: email@example.com (JM, Corresponding author); firstname.lastname@example.org (MP); email@example.com (AV)
Received: 25 February 2016 / Accepted: 28 June 2016 / Available online: 10 August 2016
Caption: Fig. 1.- Geographic location of African Miocene localities that have yielded Amphicyonidae remains. 1.- North Africa. 2.- Ethiopia. 3.- Kenya. 4.Uganda, showing the location of the fossiliferous deposits of Napak in the north-east of the country, close to the western edge of the Gregory Rift Valley. 5.- Namibia, showing the location of fossil localities in Sperrgebiet. 6.- South Africa.
Caption: Fig. 2.- Hecubides euryodon from Napak-I. 1. NAP XV 97'07 + 150'07 + 91'08, right mandible. A) occlusal view. B) lingual view. C) buccal view. 2. NAP XV 76'08, left P4. A) lingual view. B) buccal view. C) occlusal view. 3. NAP XV 382'08, right M1. A) buccal view. B) occlusal view. 4. NAP XV 146'08, left M2, occlusal view. 5. NAP XV 162'08, right m2. A) buccal view. B) occlusal view. 6. Afrocyon sp. from Napak-I, NAP I 7'99, right M2 in occlusal view.
Caption: Fig. 3.- Hecubides euryodon from Napak. NAP IX right calcaneum. 1) lateral view. 2) plantar view. 3) medial view. 4) dorsal view. 5) distal view. 6) proximal view.
Caption: Fig. 4.- Comparison of the calcaneum of Amphicyonidae, dorsal view 1) Amphicyon sp. from Barajas 17 (Spain). 2. Hecubides euryodon from Napak NAP IX. 3) Afrocyon ginsburgi from Arrisdrift. The images are brought to the same size for ease of comparison.
Caption: Fig. 5.- Comparison of the mandibles of 1) Cynelos lemanensis (SG 490) from Saint-Gerand-lePuy (France). 2) Hecubides euryodon (NAP XV 97'07 + 150'07 + 91'08) from Napak XV (Uganda). 3) Hecubides euryodon (GT 35'15) from Grillental VI (Namibia).
Caption: Fig. 6.- Bivariate plots of the upper teeth (1) and lower teeth (2) of small Amphicyonidae from Napak and from other African localities.
Caption: Fig. 7.- Hecubides euryodon from Grillental VI. GT 35'15, left mandible with p4-m2. 1) buccal view. 2) lingual view. 3) stereo occlusal view.
Caption: Fig. 8.- Bivariate plots of the upper teeth (1) and lower teeth (2) of medium-large Amphicyonidae from African localities.
Caption: Fig. 9.- Afrocyon from African localities. 1. Afrocyon burolleti from Gebel Zelten. NHM M-82373, left mandible. A) buccal view. B) lingual view. C) occlusal view. 2) Afrocyon macrodon from Rusinga NHM M-19086, right M1 (holotype). A) occlusal view. B) buccal view. 3) Afrocyon macrodon from Rusinga NHM M-34303, right m1. A) occlusal view. B) lingual view. C) buccal view. 4. Afrocyon ginsburgi from Arrisdrift. AD 311'97, right m1. A) occlusal view. B) lingual view. C) buccal view. 5. Afrocyon ginsburgi from Arrisdrift. AD 604'94 right maxilla with M1-P3 in occlusal view. 6. Afrocyon ginsburgi from Arrisdrift. AD 606'94 edentulous maxilla in occlusal view.
Caption: Fig. 10.- Caniformia indet. aff Amphicyonidae. KNM LU 227, right P4. 1) stereo occlusal view. 2) stereo buccal view. 3) stereo lingual view.
Caption: Fig. 11.- Biostratigraphy of African Miocene localities, with the temporal ranges of the diverse species of amphicyonids found therein.
TABLE 1.- Updated Faunal List from Napak, Early Miocene (Uganda). GASTROPODA Perissodactyla Maizania lugubrioides Butleria rusingense Maizaniella sp. Aceratherium sp. Tholachatina leakeyi Brachypotherium sp. Burtoa nilotica Ougandatherium napakense Subulona sp. Oreohomorus sp. Carnivora Opeas sp. Edouardia sp. Hecubides euryodon Conulinus sp. ? Kichechia zamanae Krapfiella sp. Ugandictis napakensis Koruella magnifica Ginsburgsmilus napakensis Thapsia sp. Trochonanina sp. Chiroptera Trochozonites sp. Pupoides sp. Indet sp. Ptychotrema sp. ?Macrogonaxis sp. REPTILIA Gulella sp. 1 Gulella sp. 2 Ophidea Tayloria sp. Gymnophione Haplonepion naggsi Lacertidae Edentulina rusingensis Chamaeleonidae Varanidae INSECTA Chelonii Crocodylidae Millipedes Brochuchus pigotti Moth cocoons Termite bioconstructions MAMMALIA Insectivora Rodentia Amphechinus rusingensis Diamantomys luederitzi Erythrozootes chamerpes Paraphiomys pigotti Macroscelidea Paraphiomys stromeri Myohyrax sp. Epiphiomys coryndoni Miorhynchocyon sp. Simonimys genovefae Miophiomys arambourgi Artiodactyla Megapedetes pentadactylus Renefossor songhorensis Brachyodus aequatorialis Proheliophobius sp. Nguruwe kijivium Vulcanisciurus africanus Diamantohyus africanus Nonanomalurus soniae Afrotragulus parvus Paranomalurus bishopi Siamotragulus songhorensis Paranomalurus walkeri Dorcatherium iririensis Afrocricetodon songhorensis Walangania africanus Gomphotheriidae Creodonta Progomphotherium cf maraisi Metasinopa napaki Archaeobelodon sp. Pterodon africanus Isohyaenodon pilgrimi Deinotheriidae Isohyaenodon zadoki Leakitherium hiwegi Deinotherium hobleyi Teratodon spekei Orycteropodidae Primates Orycteropus africanus Mioeuoticus bishopi Progalago dorae Hyracoidea Komba robustus Komba minor Brachyhyrax aequatorialis Prohylobates sp. Meroehyrax bateae Micropithecus clarki Limnopithecus legetet Incertae sedis Kalepithecus songhorensis Lomorupithecus evansi Prionogale breviceps Iriripithecus alekileki Kelba quadeemae Karamojapithecus akisimia Dendropithecus ugandensis AVES Turkanapithecus rusingensis ? Proconsulnyanzae Large sp. Ugandapithecus major Hombill Medium sp. Small sp. TABLE 2.- Upper and lower teeth measurements (in mm) of Hecubides euryodon from Napak XV (Uganda) and Grillental VI (Namibia). Afrocyon sp. from Napak I (Uganda). Afrocyon macrodon from Rusinga (Kenya). * (c.a.) and ** (alveolus). Locality Species Specimen Tooth Length Width Napak XV Hecubides NAP XV-76'08 P4 18.3 10.1 euryodon NAP XV-98'07 M1 14.8 18.5 NAP XV-382'08 M1 15.4 19.9 NAP XV-180'08 M1 -- -- NAP XV-146'08 M2 11.5 15.5 NAP XV-127'07 M2 11.6 15.5 p4 11 4.9 * NAP XV-150'07 m1 20 * 9 m2 14 * 7 * m3 8 * 5.5 NAP XV-96'07 p4 12.1 5.7 m2 12.8 * 7.5 NAP XV 4'12 m1 21.1 10.2 p3 11.3 ** -- p4 12.4 6.5 Grillental GT 35'15 m1 18.7 8.6 VI m2 12.8 8.3 m3 6.9 ** 4 ** Napak I Afrocyon sp. NAP-I 7'99 M2 16.9 22.3 Rusinga Afrocyon NHM M-19086 M1 20 * 24.2 macrodon NHM M-34303 m1 25.8 11.6
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|Author:||Morales, J.; Pickford, M.; Valenciano, A.|
|Publication:||Journal of Iberian Geology|
|Date:||Jul 1, 2016|
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