禄丰古猿地点中国兔猴一新种

本文记述的是在云南禄丰石灰坝古猿化石产地与古猿共生的一种中国兔猴化石。这类化石以下颌骨和牙齿较纤细,牙齿的颊侧齿带较发育,牙齿狭长,齿尖锐利和臼齿咬合面的三角凹较大,下次小尖向后延伸而使下内尖和下次小尖之间有较大间隔;上臼齿的颊舌径较小等特征区别于中国兔猴厚齿种(Sinoadapis carnosus Wu and Pan.)根据以上的形态特征,作者把它订为中国兔猴一新种:中国兔猴石灰坝种Sinoadapis shihuibaensis sp.nov.。     

NewProconsul (Xenopithecus) from the Miocene of Kenya

A maxillary fragment with M^2–3 from the middle Miocene of Lothidok Hill, northwestern Kenya represents a new species ofProconsul—the typical East African early and middle Miocene hominoid species group. M² inProconsul (Xenopithecus)hamiltoni sp. nov. is about 50% larger than in Kenyan lower MioceneP. (X.)koruensis. Xenopithecus is revived as a subgenus ofProconsul because its species are less derived than typical species of that genus in having small—unexpanded—trigons, in possessing an M² with a significantly lower relative length, and in lacking a hypocone and large metacone on M³; however, xenopithecines share with proconsulines welldefined trigon ridges on M^1–3, large hypocones on M^1–2, greater relative height of M^2–3, and crenulated cingula on M^1–3 four character complexes derived over those of plesiomorphous East African early and middle MioceneLimnopithecus. An upper canine from Lothidok Hill represents a second species ofProconsul, P. (Proconsul)major. This identification confirms earlier records of that species from Lothidok.     

云南禄丰晚中新世的长臂猿类化石

本文记述的是在禄丰腊玛古猿化石产地发现的长臂猿类化石,它是一种与上猿较为相似而又具有一些进步性质的长臂猿类。它的发现从根本上改变了晚中新世此类化石记录稀少的状况,使我们对这一时期的长臂猿类有了新的认识;同时,对现生长臂猿起源的研究提供了较为充分的化石依据。鉴于它的形态特征和地史分布,作者把它订为一新属新种Laccopithecusrobussus gen.et sp.nov.     

A new species of Pliopithecus Gervais, 1849 (Primates: Pliopithecidae) from the Middle Miocene (MN8) of Abocador de Can Mata (els Hostalets de Pierola,Catalonia, Spain)

Pliopithecus (Pliopithecus) canmatensis sp. nov. is described from several Late Aragonian localities from Abocador de Can Mata (ACM) in els Hostalets de Pierola (Vallès‐Penedès Basin, Catalonia, Spain), spanning from ～11.7 to 11.6 Ma (C5r.3r subchron), and being correlated to the MN8 (reference locality La Grive L3). The ACM remains display a pliopithecine dental morphology with well‐developed pliopithecine triangles on M/2 and M/3. This, together with other occlusal details, negates an attribution to the subgenus Epipliopithecus. Although slightly smaller, the ACM remains are most similar in size to comparable elements of P. piveteaui and P. antiquus. Several occlusal details (such as the greater development of the buccal cingulid in lower molars) and dental proportions (M/3 much longer than M/2), however, indicate greater similarities with P. antiquus from Sansan and La Grive. The ACM remains, however, differ from P. antiquus in dental proportions as well as occlusal morphology of the lower molars (including the less peripheral position of the protoconid and more medial position of the hypoconulid, the more mesial position of the buccal cuspids as compared to the lingual ones, the narrower but distinct mesial fovea, the higher trigonid, and the more extensive buccal cingulid, among others). These differences justify a taxonomic distinction at the species level of the ACM pliopithecid remains with respect to P. antiquus. Previous pliopithecid findings from the Vallès‐Penedès Basin, previously attributed to P. antiquus, are neither attributable to the latter species nor to the newly erected one. Am J Phys Anthropol, 2010. © 2009 Wiley‐Liss, Inc.     

New evidence for canine dietary function in Afropithecus turkanensis

Despite considerable post-cranial and cranial morphological overlap with Proconsul, Afropithecus turkanensis is distinguished from that taxon by a suite of anterior dental and gnathic characters shared in common with extant pitheciin monkeys (i.e. low crowned, robust and laterally splayed canines, procumbent incisors, prognathic premaxilla, powerful temporalis muscles, reduced or absent maxillary sinuses, and deep mandibular corpora). Pitheciins are unique among living anthropoids because their canines serve a habitual dietary function and are not strictly influenced by inter-male competition. Given the functional association between pitheciin canine morphological specializations and sclerocarp foraging, a feeding strategy where the hard pericarps of unripe fruit are mechanically deformed by the canines, it has been suggested that Afropithecus may also have used its canines in a dietary context. This is confirmed by quantitative morphometric analyses of Afropithecus canine curvature and basal dimensions demonstrating that Afropithecus and extant pitheciins (Chiropotes, Cacajao) are distinguished from all other anthropoids by pronounced and evenly distributed mesial canine crown contours as well as greater resistance to canine bending in both the mesiodistal and labiolingual axes. In addition, Afropithecus, Chiropotes and Cacajao are also shown to have significantly longer and more curved premaxillae with greater incisor procumbency that effectively isolates the incisor and canine functional complexes. These morphological similarities are a result of convergence and not a shared derived ancestry. Despite their considerable morphological overlap, it is unlikely that Afropithecus and extant pitheciin diets are identical given significant dissimilarities in their post-canine morphology, maximum angular gape and body size. Nevertheless, Afropithecus canine dietary function is unique among hominoids and may have been a key component for the expansion of hominoids into Eurasia at the end of the early Miocene.     

Premolar microwear and tooth use in Australopithecus afarensis

The mandibular third premolar (P₃) of Australopithecus afarensis is notable for extensive morphological variability (e.g., metaconid presence/absence, closure of the anterior fovea, root number) and temporal trends in crown length and shape change over its 700 Ka time range. Hominins preceding A. afarensis have unicuspid, mesiodistally elongated P₃s with smaller talonids, and subsequent australopiths have bicuspid, more symmetrically-shaped P₃ crowns with expanded talonids. For these features, A. afarensis is intermediate and, thus, evinces the incipient stages of P₃ molarization. Here, we examine A. afarensis P₃ Phase II microwear and compare it with that of Australopithecus africanus and Cercocebus atys, an extant hard-object specialist, to assess whether the role of the P₃ in food processing changed over time in A. afarensis. Premolar Phase II microwear textures are also compared with those of the molars to look for evidence of functional differentiation along the tooth row (i.e., that foods with different mechanical properties were processed by separate regions of the postcanine battery). Microwear textures were also examined along the mesial protoconid crest, the site of occlusion with the maxillary canine, of the A. afarensis P₃ and compared with the same region in Pan troglodytes to determine whether microwear can be useful for identifying changes in the occlusal relationship between the P₃ and maxillary canine in early Australopithecus. Finally, temporal trends in P₃ Phase II and mesial microwear are considered. Results indicate that 1) both the P₃ and molar Phase II facets of A. afarensis have less complex microwear textures than in A. africanus or C. atys; 2) A. afarensis P₃ and molar Phase II textures differ, though not to the extent seen in taxa that eat hard and tough items; 3) microwear along the A. afarensis mesial protoconid crest is clearly distinct from that of the P. troglodytes, indicating that there is no honing equivalent in A. afarensis; and 4) there is little evidence of change over time in A. afarensis P₃ microwear on either the mesial or Phase II facet. In sum, these results provide no evidence that A. afarensis routinely loaded either its premolars or molars to process hard objects or that A. afarensis P₃ function changed over time.     

Evolutionary and Biological Implications of Dental Mesial Drift in Rodents: The Case of the Ctenodactylidae (Rodentia,Mammalia)

Dental characters are importantly used for reconstructing the evolutionary history of mammals, because teeth represent the most abundant material available for the fossil species. However, the characteristics of dental renewal are presently poorly used, probably because dental formulae are frequently not properly established, whereas they could be of high interest for evolutionary and developmental issues. One of the oldest rodent families, the Ctenodactylidae, is intriguing in having longstanding disputed dental formulae. Here, we investigated 70 skulls among all extant ctenodactylid genera (Ctenodactylus, Felovia, Massoutiera and Pectinator) by using X-ray conventional and synchrotron microtomography in order to solve and discuss these dental issues. Our study clearly indicates that Massoutiera, Felovia and Ctenodactylus differ from Pectinator not only by a more derived dentition, but also by a more derived eruptive sequence. In addition to molars, their dentition only includes the fourth deciduous premolars, and no longer bears permanent premolars, conversely to Pectinator. Moreover, we found that these premolars are lost during adulthood, because of mesial drift of molars. Mesial drift is a striking mechanism involving migration of teeth allowed by both bone remodeling and dental resorption. This dental innovation is to date poorly known in rodents, since it is only the second report described. Interestingly, we noted that dental drift in rodents is always associated with high-crowned teeth favoring molar size enlargement. It can thus represent another adaptation to withstand high wear, inasmuch as these rodents inhabit desert environments where dust is abundant. A more accurate study of mesial drift in rodents would be very promising from evolutionary, biological and orthodontic points of view.     

The first female maxilla of the hominoid Ouranopithecus macedoniensis from the late Miocene of Macedonia,Greece

A maxilla with both toothrows C-M³ of a late Miocene hominoid is described. It was found at the locality Nikiti 1 (NKT) of Chalkidiki (Macedonia, Greece). The locality has been dated to late Vallesian-earliest Turolian. The morphological characters and the comparison of the new maxilla suggest that it is a female individual of Ouranopithecus macedoniensis. It is the first known female maxilla of the species. Comparison with the other two known male maxillae of Ouranopithecus macedoniensis indicates the following differences: smaller size of maxilla and teeth, smaller mesial groove in the canine, more lingually situated mesial groove in the canine, slightly smaller mesiobuccal projection in P³ and relatively shorter P⁴. There are no significant morphological differences in the molars. Various statistical parameters for the Ouranopithecus teeth have been calculated and compared with those of the extant hominoids. This comparison suggests the presence of a single species in the sample.     

First detailed description of Hispanomys bijugatus Mein and Freudenthal, 1971 (Rodentia, Cricetodontinae) from the Upper Aragonian of La Grive-Saint Alban (France): Biostratigraphical implications

The material of Hispanomys bijugatus (Rodentia, Cricetodontinae) from La Grive-Saint Alban (carrière Lechartier, fissure L3) is described for the first time and compared with all species of the genus known to date. As common in the Upper Aragonian populations of Hispanomys, this taxon evidences a low variability. H. bijugatus shows some progressive characters with respect to the remaining Aragonian congeneric species, such as the absence of labial and lingual cingula surrounding the upper and lower molar valleys respectively, the increase in the number of roots on the second lower molar, and the lost of mesolophs. This suggests that H. bijugatus, in spite of being one of the oldest species of the genus, is relatively derived with regard to the coeval congeneric species. Because H. bijugatus and H. decedens are believed to be closely related species within the same lineage, the fact that the former shows a more progressive dental morphology than the latter suggests that the unnamed fissure-fillings from La Grive and La Grive M (with H. decedens only) are older than La Grive L3 (with H. bijugatus only). The coexistence of both species at locality L5 suggests an intermediate age.     

Dental variation ofProconsulfrom the Tinderet region, Kenya

The morphology of mandibular molars of the twoProconsulspecies,Proconsul majorandProconsul africanus, from the Tinderet region, Kenya was analyzed. While the molar size variability within the TinderetP. majorwas slightly greater than those of local African ape subspecies, the shape variability was comparable. Because the twoProconsulspecies show some differences in cusp areal proportions,P. majoris not just a largerP. africanusin molar morphology. Napak specimens are generally similar to the TinderetP. major.     

内蒙古始新世梳趾鼠类化石

描述了４属１０种梳趾鼠类化石（Ｇｏｂｉｏｍｙｓ ｎｅｉｍｏｎｇｏｌｅｎｓｉｓ, Ｇ． ｅｘｉｇｕｕｓ（新种）, Ｇ． ｃｆ．Ｇ．ｅｘｉｇｕｕｓ,Ｇ．ａｓｉａｔｉｃｕｓ（新种）,Ｇｏｂｉｏｍｙｓ？ｓｐｐ．,Ａｄｖｅｎｉｍｕｓ　ｃｆ．Ａ．ｂｏｈｌｉｎｉ,Ａ．ｃｆ．Ａ．ｂｕｒｋｅｉ, Ｙｕｏｍｙｓ ｓｐ．和Ｐｒｏｔａｔａｒｏｍｙｓ　ｓｐ．）．以Ｍｅｒｇｅｎｏｍｙｓ　ｎｅｉｍｏｎｇｏｌｅｎｓｉｓ作属型种建了一新属,Ｇｏｂｉｏｍｙｓ。其特征是：门齿孔大;具Ｐ３;颊齿齿冠低,主尖明显,但不膨大,齿凹开阔;Ｐ４／ｐ４非臼齿化;上臼齿宽大于长,后脊较发育;Ｍ１和Ｍ２具内脊;下外脊和下次小尖位置偏外。Ｇ．ｅｘｉｇｕｕｓ的特点是：个体较小,上颌骨颧突根在Ｐ３之前,下臼齿缺下原失后臂舌部、下内尖臂和下前齿带．Ｇ．ａｓｉａｔｉｃｕｓ的上颌骨颧突后缘在Ｐ３的外方;臼齿具较发达的齿脊;上臼齿较宽短,后小尖较弱;下臼齿具较发达的内尖臂和前齿带。 Ｇｏｂｉｏｍｙｉｄａｅ新科包括Ｇｏｂｉｏｍｙｓ, Ｍｅｒｇｅｎｏｍｙｓ,Ｙｏｕｎｇｏｍｙｓ和哈萨克斯坦的未命名的新属等４属,组成与梳趾鼠科相对的姐妹群。其主要特征是,下颌骨缺咬肌窝上嵴。颊齿低冠,近于丘形     

安徽潜山新发现的假古猬类化石

记述了安徽省潜山盆地早～中古新世望虎墩组中发现的２属３种假古猬类化石,其中包括一个新种──望虎墩非猬（Ａｎｉｃｔｏｐｓ ｗａｎｇｈｕｄｕｎｅｎｓｉｓ ｓｐ． ｎｏｖ．）。新种不同于属型种大别非猬（Ａｎｉｃｔｏｐｓ ｔａｂｉｅｐｅｄｉｓ）在于下颊齿下前尖更衰退且更靠近下后尖,下次小尖不发育,ｍ３跟座呈圆形。上颊齿单面高冠现象较显著,相对横宽。     

A new spalacolestine mammal from the Early Cretaceous Jehol Biota and implications for the morphology,phylogeny, and palaeobiology of Laurasian ‘symmetrodontans’

‘Symmetrodontans’ are extinct mammals characterized by having a reversed‐triangle molar pattern in which three main cusps define a triangular molar crown. This dental morpholgy has been regarded as being intermediate between the ‘triconodont’ tooth and the tribosphenic pattern characterizing therians; it is a key feature in taxonomy of Mesozoic mammals and one to understand mammalian evolution and palaeobiology. Here we report a new genus and species of ‘symmetrodontan’ mammal, Lactodens sheni, from the Early Cretaceous Jehol Biota, represented by a partial skeleton with dentary and upper and lower teeth with dental morphologies well‐preserved. The new species has a dental formula of three upper incisors, one canine, three premolars, and six molars/three lower incisors, one canine, five premolars and six lower molars, double‐rooted canines, extremely low‐crowned and transversely thin premolars, and acute angled molars. The dental morphologies of molars and peculiar deciduous premolars are similar to those of Spalacolestes from North America. The associated upper and lower dentitions from one individual animal helped to clarify tooth identification of some spalacotheriids represented only by fragmentary material. Phylogenetic analyses indicate a close relationship of the new species to North American spalacolestines and faunal interchanges between Eurasia and North America, thus supporting the notion that small‐bodied spalacotheriids were diverse and had a pan‐Laurasian distribution during the Early Cretaceous. Absence of the Meckelian groove suggests acquisition of the definitive mammalian middle ear in spalacolestines, and deciduous canines and premolars in the slim and extremely long dentary imply a faunivorous diet.     

Trends in the evolution of the pongid dentition

The question investigated in this paper is whether long-range, parallel trends in evolution can be sustained in divergent though closely related lines. This study examines fossil and recent pongid dentitions, testing the hypothesis of the existence of certain trends in the pongid dental evolution. These are: reduction of the cingulum in both upper and lower molars; morphological and metrical reduction in third molars; mesial movement of the metaconid; buccal shifting of the hypoconulid; and alteration of the Dryopithecus groove pattern. More broadly the study tests conclusions of a previous study concerning parallelism of trends in the hominoid dentition. The results of reduction of the cingulum, reduction of the third molar, and alteration of the occlusal pattern on the lower molars support the theory that similar, long-term trends can operate in the evolution of divergent, though closely related lines. They also demonstrate that morphological resemblances between two forms are not certain proof of recent divergence.     

Draconematidae (Nematoda) from cold-water corals in the Porcupine Seabight: The genus Cygnonema Allen & Noffsinger, 1978

Two new and closely related species of the genus Cygnonema Allen & Noffsinger, 1978 are described from a cold-water coral degradation zone in the Porcupine Seabight (NE Atlantic). Both species differ from C. steineri Allen & Noffsinger, 1978 by more pronounced pharyngeal and posterior swellings, a smaller body, a shorter pharynx in relation to body length, a higher number of CAT, and by the absence of a dorsal tooth. Cygnonema verum sp. n. differs from C. belgicae sp. n. by its greater body length, the relatively larger head capsule, a higher number of CAT, a more anteriorly positioned anteriormost laterodorsal CAT, a higher number of PAT, by the external labial sensilla being setiform, a higher number of subcephalic setae, and by a more anterior position of the amphidial fovea on the head capsule. Males of C. verum sp. n. are easily recognised by the presence of two large subventral, precloacal corniform setae. They also differ from males of C. belgicae sp. n. in the smaller amount of cytoplasm in the sperm cells, a knob-like capitulum, and a relatively shorter tail tip. The diagnosis of Cygnonema is emended, a dichotomic identification key to the three species is provided, and their biogeography is discussed.     

Geographic Variation in Nonmetric Dental Traits of the Deciduous Molars of Pan and Gorilla

Physical anthropologists often use nonmetric dental traits to trace the movement of human populations, but similar analysis of the teeth of nonhuman primates or the deciduous teeth is rare. Because nonmetric dental characteristics are manifestations of genetic differences among groups, they vary among geographically distant members of the same species and subspecies. We use 28 nonmetric dental traits in the deciduous molars to compare genetically and geographically distinct groups of extant African apes (Gorilla and Pan). Previous researchers have studied these traits in the adult or juvenile teeth of great apes and humans, and we score our observations according to established standards for hominins. We observe marked differences in trait frequencies between Gorilla and Pan, Pan troglodytes and P. paniscus, and two P. troglodytes subspecies but we find no significant differences between geographically isolated groups within the subspecies. Trait frequencies differ from those found in previous studies that contained fewer individuals. We find that the deciduous molars show similar variation to adult premolars and molars within Pan and Gorilla. This suggests that the deciduous dentition of these and other apes may contain diagnostic traits that are not currently in use.     

Negative regulating factors of notch signaling may be a key factor for the teeth root formation

It is still an open question that how the teeth root development is initiated at the molecular level. But what we know is that the teeth root development begins after the crown part is completely formed, and then the terminal cervical loop structure faces two developmental fate options when the crown development is quite advanced: it can remain as a ‘crown’ pattern, and continue enamel production, or it can adopt the ‘root’ fate, and begins teeth root development. Epithelial notch and mesenchymal fgf10 signaling are thought to be the key switches of root or crown development pattern. But, for a rodent's molars and incisors, it is very interesting that after a similar teeth crown developmental process, the late development for the molars and incisors is quite different: the molar germ forms a multi-rooted pattern, while the incisor germ forms a single-rooted analogue and without a really root development process. In a recent study, one of the negative regulating factors for notch signaling, sel1l was found strongly related to the molar root development. So we hypotheses that the negative regulating factors of notch signaling, may be the key signals to determine the tooth root developmental onset, and the quantity or function's abnormal of that factors, may lead to hypoplasia of the teeth root.     

Similar variation in carbon storage between deciduous and evergreen treeline species across elevational gradients

Background and Aims

The most plausible explanation for treeline formation so far is provided by the growth limitation hypothesis (GLH), which proposes that carbon sinks are more restricted by low temperatures than by carbon sources. Evidence supporting the GLH has been strong in evergreen, but less and weaker in deciduous treeline species. Here a test is made of the GLH in deciduous–evergreen mixed species forests across elevational gradients, with the hypothesis that deciduous treeline species show a different carbon storage trend from that shown by evergreen species across elevations.

Methods

Tree growth and concentrations of non-structural carbohydrates (NSCs) in foliage, branch sapwood and stem sapwood tissues were measured at four elevations in six deciduous–evergreen treeline ecotones (including treeline) in the southern Andes of Chile (40°S, Nothofagus pumilio and Nothofagus betuloides; 46°S, Nothofagus pumilio and Pinus sylvestris) and in the Swiss Alps (46°N, Larix decidua and Pinus cembra).

Key Results

Tree growth (basal area increment) decreased with elevation for all species. Regardless of foliar habit, NSCs did not deplete across elevations, indicating no shortage of carbon storage in any of the investigated tissues. Rather, NSCs increased significantly with elevation in leaves (P < 0·001) and branch sapwood (P = 0·012) tissues. Deciduous species showed significantly higher NSCs than evergreens for all tissues; on average, the former had 11 % (leaves), 158 % (branch) and 103 % (sapwood) significantly (P < 0·001) higher NSCs than the latter. Finally, deciduous species had higher NSC (particularly starch) increases with elevation than evergreens for stem sapwood, but the opposite was true for leaves and branch sapwood.

Conclusions

Considering the observed decrease in tree growth and increase in NSCs with elevation, it is concluded that both deciduous and evergreen treeline species are sink limited when faced with decreasing temperatures. Despite the overall higher requirements of deciduous tree species for carbon storage, no indication was found of carbon limitation in deciduous species in the alpine treeline ecotone.     

New dental remains of Anoiapithecus and the first appearance datum of hominoids in the Iberian Peninsula

New dental remains of the fossil great ape Anoiapithecus brevirostris are described from the Middle Miocene local stratigraphic series of Abocador de Can Mata (ACM) in els Hostalets de Pierola (Vallès-Penedès Basin, NE Iberian Peninsula). These specimens correspond to maxillary fragments with upper teeth from two female individuals from two different localities: left P³–M¹ (IPS41712) from ACM/C3-Aj (type locality; 11.9 Ma [millions of years ago]); and right M¹–M² and left P⁴–M² (IPS35027) from ACM/C1-E* (12.3–12.2 Ma). Relative enamel thickness is also computed in the latter individual and re-evaluated in other Middle Miocene hominoids from ACM, in order to better assess their taxonomic affinities. With regard to maxillary sinus development, occlusal morphology, molar proportions and enamel thickness, the new specimens show greater resemblances with the (male) holotype specimen of A. brevirostris. They differ from Pierolapithecus catalaunicus in displaying less inflated crests, a more lingually-located hypocone, and relatively lower-crowned molars; from Dryopithecus fontani, in the relatively thicker enamel and lower-crowned molars; from Hispanopithecus spp., in the more inflated crown bases, less peripheral cusps and more restricted maxillary sinus; and from Hispanopithecus laietanus also in the thicker crests, more restricted occlusal foveae, and relatively lower-crowned molars. The new specimens of A. brevirostris show some slight differences compared with the holotype of this species: smaller size (presumably due to sexual size dimorphism), and less distally-tapering M² occlusal contour (which is highly variable in both extant and extinct hominoids). The reported remains provide valuable new evidence on dental intraspecific variation and sexual dimorphism in Anoiapithecus. From a taxonomic viewpoint, they support the distinction of this taxon from both Dryopithecus and Pierolapithecus. From a chronostratigraphic perspective, IPS35027 from ACM/C1-E* enlarges the known temporal distribution of Anoiapithecus, further representing the oldest record (first appearance datum) of hominoids in the Iberian Peninsula.     

New Early Eocene Basal tapiromorph from Southern China and Its Phylogenetic Implications

A new Early Eocene tapiromorph, Meridiolophus expansus gen. et sp. nov., from the Sanshui Basin, Guangdong Province, China, is described and discussed. It is the first reported Eocene mammal from the basin. The new taxon, represented by a left fragmentary mandible, is characterized by an expanded anterior symphyseal region, a long diastema between c1 and p1, a rather short diastema between p1 and p2, smaller premolars relative to molars, an incipient metaconid appressed to the protoconid on p3, a prominent entoconid on p4, molar metaconid not twinned, cristid obliqua extending mesially and slightly lingually from the hypoconid, inclined metalophid and hypolophid, and small hypoconulid on the lower preultimate molars. Meridiolophus is morphologically intermediate between basal Homogalax-like taxa and derived tapiromorphs (such as Heptodon). Phylogenetic analysis indicates Equidae is more closely related to Tapiromorpha than to Palaeotheriidae, although the latter is only represented by a single species Pachynolophus eulaliensis. ‘Isectolophidae’, with exception of Meridiolophus and Karagalax, has the closest affinity with Chalicotherioidea. Furthermore, the majority rule consensus tree shows that Meridiolophus is closer to Karagalax than to any other ‘isectolophid’, and both genera represent stem taxa to crown group Ceratomorpha.