A new symmetrodont mammal (Trechnotheria: Zhangheotheriidae) from the Early Cretaceous of China and trechnotherian character evolution

We report the discovery of Anebodon luoi, a new genus and species of zhangheotheriid symmetrodont mammal from the Lujiatun site of the Lower Cretaceous Yixian Formation, China. The fossil is represented by an associated partial skull and dentaries with a nearly complete dentition, and with a dental formula of I4/3 C1/1 P5/4 M3/4. This new taxon lacks the high molar count typical of derived symmetrodonts, differing from the well-represented zhangheotheriids Zhangheotherium and Maotherium in having a postcanine dental formula that resembles more primitive tinodontid symmetrodonts on the one hand, and sister taxa to therians such as Peramus on the other. Upper and lower distal premolars are strongly molariform and are captured undergoing replacement, clarifying positional homology among related taxa. We also describe the rostrum and, for the first time in a symmetrodont, much of the orbital mosaic. Importantly, our new taxon occupies a basal position within the Zhangheotheriidae and permits discussion of trechnotherian character evolution, ultimately shedding additional light on the evolution of therians.

Mesozoic mammals with molariform teeth bearing a simple, triangular arrangement of principal cusps were traditionally assigned to the Order Symmetrodonta 1 . Based originally on taxa from the Upper Jurassic-Lower Cretaceous Morrison and Purbeck formations (e.g., Spalacotherium 2 and Tinodon 3 ), this classification stood for well over a half century and incorporated subsequently described forms ranging from Kuehneotherium (Early Jurassic of Britain 4 ) to the pseudotribosphenic Shuotherium (Middle Jurassic of China and Britain [5][6][7][8]. Phylogenetic analyses imply that this grouping is artificial, with the symmetrodont molar pattern representing a structural grade that evolved multiple times [9][10][11] . In fact, weakly-triangulated molariforms, as represented by tinodontids, are present near the base of Mammalia in recent analyses [12][13][14] , suggesting that this pattern was shared by the ancestors of dentally specialised but structurally disparate groups such as eutriconodontans, multituberculates, dryolestoids, and therians. Classic studies of molar evolution have proposed homologies of cusps between therians (the group containing marsupials and placentals) and non-therians [15][16][17] , and there has been broad agreement when it comes to transformations from a symmetrodont pattern (though notable exceptions include the fate of upper molar cusp C with regards to the metacone, and the homology of the distal lower molar cusp d with the cusps of the therian talonid); see recent review by Davis 18 . Therefore, discoveries of well-preserved symmetrodont specimens have the potential to illuminate the morphological transitions that gave rise to therians.
Scientific RepoRts | 6:26668 | DOI: 10.1038/srep26668 Symmetrodont taxa with acutely-triangulated molar cusps ("acute-angled symmetrodonts") form a monophyletic group in recent analyses [19][20][21] , positioned at the base of the Trechnotheria, a clade which also contains dryolestoids and therians. These symmetrodonts are known principally from the Early Cretaceous and became extinct prior to the Campanian 22 . They segregate into two lineages: the Spalacotheriidae, a diverse group which contain some dentally specialised taxa bearing a high number of mesiodistally compressed molars, and the Zhangheotheriidae, a group restricted to Asia and bearing a more plesiomorphic dentition. Of this latter group, only three genera have been previously described. Zhangheotherium quinquecuspidens 23 is known by a nearly complete skeleton and a second, badly crushed but ontogenetically younger specimen 24 , showing evidence of tooth replacement. A second genus, Maotherium, is known by two specimens from the Lower Cretaceous Yixian Formation of Liaoning Province, China (the same unit that yielded Zhangheotherium). The type species, M. sinensis 25 , is represented by a flattened but fully articulated skeleton with associated soft tissue impressions. A second species, M. asiaticus 26 , is represented by a beautifully preserved but only partially described skeleton. Only one zhangheotheriid is known from outside China-Kiyatherium cardiodens 27 , from the Lower Cretaceous Ilek Formation of western Siberia. The holotype is an isolated maxilla fragment bearing the canine and most of the postcanine dentition. Additional material was described by Lopatin et al. 28 , including a second maxilla and several dentary fragments, permitting description of the complete lower dentition.
We describe a new zhangheotheriid, also from the Yixian Formation, represented by a partial skull and associated dentaries. Upon analysis, this taxon is positioned at the base of the Zhangheotheriidae. The rostrum and much of the orbital mosaic are well preserved. Despite the lack of preservation of the basicranium and postcranial skeleton, this specimen is the first symmetrodont in which the crown morphology for the complete dental series is fully exposed, showing a formula of I4/3 C1/1 P5/4 M3/4; as most of the record of trechnotherian diversity consists of isolated teeth and fragmentary jaws, our new specimen provides an opportunity to explore postcanine positional homology across symmetrodonts. A postcanine count of five premolars and three molars is generally regarded as primitive for therians 29 , suggesting that this tooth count may be primitive for Trechnotheria as a whole. Diagnosis: Zhangheotheriid differing from Maotherium and Zhangheotherium in having a postcanine dental formula of P5/4 M3/4, and in more obtuse triangulation of distal molars. Further differs from Zhangheotherium in having upper molars with deeper ectoflexus, subequal cusp B and metacone, and well-developed lingual cingulum, and lower molars with paraconid taller than metaconid. Differs from Maotherium and Kiyatherium in the absence of upper molar parastyle and less reduction of ultimate molar. Most closely resembles Kiyatherium but differs in having double-rooted upper canine, molariform P3/p3, and weaker upper molar ectocingulum and lingual cingulum. Description and Comparisons. Skull. A detailed description and additional images of the skull, dentary, and dentition of Anebodon can be found in the Supplementary Information. Anebodon is now the third zhangheotheriid known by cranial material. Unfortunately, most of the descriptions of Maotherium and Zhangheotherium are focused on the character-rich petrosal, which is not preserved in our new taxon. However, some comparisons with these taxa can be made from the limited overlapping described skull regions and from gleaning morphological information from the character dataset of Ji et al. 26 . The skull of Anebodon is relatively low-vaulted and generally primitive in construction ( Fig. 1), as in other zhangheotheriids. While generally well preserved in three dimensions, the skull is distorted such that the right side is sheared anteriorly relative to the left side (most apparent along the posterior margin of the palate, Fig. 1b,f). This distortion affects to some degree the appearance and relative sizes of the bones in the orbitotemporal region and what remains of the sidewall of the braincase, and the associated crushing has made some sutural boundaries difficult to interpret. The slender appearance of the snout (in dorsal and ventral views) is due to the collapse of most of the right half of the palate. In general proportions, the skull of Anebodon would likely have resembled that reconstructed for Maotherium sinensis 25 . The lateral margin of the nasal cavity is formed by a relatively large septomaxilla (Fig. 1d,g), a primitive condition shared with other zhangheotheriids. This bone bears a medially-directed horizontal process, though it is unclear if a septomaxillary foramen is present due to matrix infill. The vertical portion of the bone tapers posterodorsally but is damaged, making it impossible to determine if it contacted the maxilla (as in Vincelestes 30 ) or if the facial process of the premaxilla separated it from the maxilla (as in docodonts 31 ). The premaxilla is similarly damaged, so contact between it and the nasals cannot be determined. A moderate-sized infraorbital foramen is present on the facial portion of the maxilla above the ultimate premolar, but this region is damaged and no additional foramina are visible. The nasals are anteriorly narrow in dorsal view and broaden considerably posteriorly towards their relatively straight contact with the frontals (Fig. 1a,e), as in Maotherium sinensis 25 . It should be noted that the nasals are scored as posteriorly narrow by Ji et al. 26 in both Maotherium and Zhangheotherium. No nasal foramina are visible.
Scientific RepoRts | 6:26668 | DOI: 10.1038/srep26668 The frontal and lacrimal have limited orbital exposure, with most of the anteromedial wall of the orbit formed by a large perpendicular process of the palatine (Figs 1 and S1), the condition in mammaliaforms such as Morganucodon and Haldanodon 31,32 , and differing from that in multituberculates which have large orbital contributions from the frontal and maxilla 33 . While not described, the zhangheotheriids Maotherium and Zhangheotherium were scored as having expansive orbital exposure of the maxilla 26 . The ethmoidal foramen is positioned at the suture between frontal and palatine, and the frontal forms the entire anterior opening of the orbitotemporal canal (Fig. S1). A well-defined, anterodorsally-directed foramen is present at the presumed posterior extent of the palatine where this bone would have met the sphenoid complex. A possible identification for this foramen is the transverse canal, a feature common among extant metatherians and in some eutherians 34,35 , but so far limited among non-therians to the multituberculate Kryptobaatar 33 . The orbitosphenoid is comparable in development to Morganucodon 31 and Kryptobaatar. The alisphenoid is interpreted as a relatively large and broad element, contacting the frontal at its anterodorsal margin. Much of the inferior portion of the alisphenoid is missing; accordingly, other major openings in the sidewall of the braincase cannot be identified. A thickened vertical ridge is interpreted as the suture between alisphenoid and anterior lamina of the petrosal. The posterior extent of the latter element is missing, but it appears likely that the relative proportions of these two bones were similar to the condition in the zatherian Vincelestes 36 .
The alveolar portions of both dentaries are well preserved, but each is missing most or all of the posteroventral portion behind the tooth row. From available evidence, the dentary of Anebodon differs little from other zhangheotheriids; the coronoid process ascends at a low angle (~150°), and a well-defined Meckel's groove is present on the medial side of the dentary (Fig. 2).
Dentition. The dental formula of Anebodon is interpreted as I4/3 C1/1 P5/4 M3/4, with the left side of the specimen preserving evidence of the entire upper and lower dentition (Figs 1,2 and S2). Anebodon is referred to the Zhangheotheriidae based primarily on features of the dentition. Anebodon can be distinguished from tinodontids in that the upper and lower molars are better triangulated (Fig. 3). It differs from spalacotheriids in the strong development of cusp B and retention of a large metacone, as well as the presence of a strong lingual cingulum and the lack of mesiodistal compression of the molars. Both upper and lower canines are small in Anebodon, a feature shared among tinodontids and zhangheotheriids. The upper canine crown is premolariform and double-rooted, while the lower crown is incisiform and single-rooted. The first two upper and lower premolars in Anebodon are premolariform. The P2 is very small and has a single, heavy root though it is grooved buccally and may divide deeper in the alveolus (Fig. 3b,d). Due to its small size, it is possible that this tooth could be interpreted as a retained DP1, but based on the very limited evidence for replacement at this position in Mesozoic mammals we prefer a conservative approach. The lower p2 bears a distinct but damaged metaconid. The remaining premolars are strongly molariform, with the upper premolars having a progressively better-developed lingual cingulum (complete on the P5). The P4 is the tallest tooth in the postcanine series, even accounting for the incomplete eruption of the P5. The crowns of the P5/p4 lack wear and are not fully erupted, as the distal base of the crowns has yet to clear the alveolar margin (Fig. 3b,e); evidence of replacement at these tooth positions establishes a minimum upper and lower premolar count which we interpret to be the full adult condition (see Discussion below). Among zhangheotheriids, Anebodon differs most strikingly from the well-represented Zhangheotherium and Maotherium in postcanine dental formula. These two genera, known by multiple nearly complete skeletons, have postcanine counts of P2/3 M5/5-6 and P1-2/1-3 M4-5/6, respectively [23][24][25][26] . These differ considerably from the count of P5/4 M3/4 in Anebodon. We consider the increase in number of molars in some zhangheotheriids to be derived (but see discussion below), with our new taxon more closely resembling tinodontids in this regard.
The mesial molars in Anebodon are more acutely triangulated than the ultimate premolars (M1 = 95°, m1 = 85°). The main accessory cusps are well developed, though the metacone/metaconid and metastylar region decrease in size distally (Figs 3 and S2). The upper molars have a complete and rather crenulated lingual cingulum. Molars of Anebodon differ from Zhangheotherium and Maotherium in lacking progressively more acute triangulation of the three main cusps distally through the molar series, a feature which these other taxa share with more derived spalacotheriids 22 . Instead, the cusp angle in Anebodon increases slightly distally, and by the ultimate lower molar (m4) the main cusps are nearly in-line (Figs 3h and S2k). Anebodon further differs from Zhangheotherium in the strong development of the upper molar lingual cingulid and greater depth of the ectoflexus; upper molars of the new taxon differ from those of Maotherium in lacking a parastyle and development of a mesially-projecting parastylar hook.
Among known zhangheotheriids, comparisons to Kiyatherium cardiodens 28 are most favourable. The two partial maxillae referred to Kiyatherium preserve evidence of the entire postcanine dentition, originally interpreted as P1-4 and M1-4 with the first upper molar undergoing replacement (designated as RM1 28 ). However, molars are by definition never replaced 37 , and this fifth postcanine should be identified as the P5. Contrary to the original interpretation, it is likely that both maxillae referred to Kiyatherium bear the entire molar series, with the M3 more reduced in size in the holotype specimen 28 . Though damaged, it is clear that the P5 of the referred specimen is less worn than the M1 and belongs to a different tooth generation. Under our interpretation, Anebodon and Kiyatherium share a postcanine dental formula of P5/4 M3/4. These two taxa are also broadly similar in molar morphology, and differ only in that Anebodon possesses a relative more molariform the third premolar, double-rooted upper canine, weaker development of upper molar cingula, and less reduction of the ultimate upper and lower molars.

Discussion
Zhangheotheriids are trechnotherian mammals forming the sister group to the Spalacotheriidae in most recent analyses 13,19,38 . Despite limited taxonomic diversity, zhangheotheriids are known by relatively well-preserved material including partial skulls and nearly complete skeletons [23][24][25][26]28 . The known record of this group is restricted to the Early Cretaceous of China and Siberia. Zhangheotheriids share a peculiar morphology of the posterior part of the dentary, namely a deep notch separating the slender, reclined coronoid process from the stout, upturned condylar process. As in spalacotheriids, an angular process is absent but a medially-directed pterygoid flange is generally developed along the ventral and posterior margin of the postdentary region. The molariforms in zhangheotheriids are somewhat intermediate in morphology between tinodontids and spalacotheriids; the primary cusps are somewhat more acutely triangulated than in tinodontids and further decrease in angle posteriorly through the molar series, especially with regards to the upper molars (though the angle actually increases distally in Anebodon and Kiyatherium, Fig. 3). The upper molars are further derived (with respect to tinodontids) in the tall height of cusp B as well as the possession of a strong lingual cingulum. However, the molar cusps are conical and lack tight, preformed occlusal fit with the opposing teeth, which develops only after wear (a primitive condition). The apices of the stylocone and metastyle only participate in shearing once the pre-and postvallum crests have worn considerably.
Most of these dental and mandibular features uniting zhangheotheriids are either plesiomorphic or can be viewed as transitional between tinodontids and more derived spalacotheriids. Not surprisingly, our result suggests that Zhangheotheridae represent a paraphyletic group, with Anebodon and Kiyatherium occupying a basal position (Fig. 4). These two taxa are least derived among zhangheotheriids with respect to distal molar triangulation and number of upper molars. However, it is worth noting that Anebodon and Kiyatherium have a postcanine dental formula of P5/4 M3/4, a condition shared (at least in part) with basal therians (the aegialodontid Kielantherium likely has a lower postcanine count of p4/m4 39 ). In contrast, spalacotheriids increase the number of molariforms up to seven. This suggests that there were two evolutionary trends among acute-angled symmetrodonts: one retaining a relatively low molar count leading to therians, and the other increasing molar count to specialised spalacotheriids (and occurring in parallel among dryolestoids 22 ).
An additional feature which appears to characterise zhangheotheriids is the strong molarization of the posterior premolars. Moreover, based on evidence from Anebodon, the ultimate premolar is replaced at a relatively advanced ontogenetic stage; instead of occurring in concert with eruption of the last molar, as is characteristic of therians 40 , the ultimate premolar was replaced after the last molar had accumulated substantial wear (Figs 3 and S2a). The lack of a clear morphological break in the postcanine series has led to differences in nomenclature with regards to the premolar-molar boundary in this and similar groups, with related inconsistencies in tooth formulae. For instance, specimens of the zhangheotheriid Kiyatherium from the Early Cretaceous of Siberia record clear replacement of the fifth postcanine upper tooth (a molariform), yet this position is identified as the M1 with the successional tooth given the awkward moniker of 'RM1' for 'replacement M1' 41 . Our specimen has the same number of postcanine teeth and shows evidence of replacement at the same locus (Fig. 3). Molars, as defined by Owen 37 , are a posterior extension of the primary dental series (derived from the primary dental lamina) and are not replaced. Premolars, on the other hand, are defined as postcanines which exhibit replacement; as such, deciduous premolars belong to the primary dental series and adult premolars to the secondary series. In some instances, anterior postcanines are not replaced (e.g., P1 in eutherians); the definition can simply be amended such that a molar is any tooth posterior to the last postcanine showing evidence of replacement. Accordingly, we regard the tooth in question in Anebodon and Kiyatherium as the ultimate premolar (P5). Along these lines, it is possible that the postcanine formula in other zhangheotheriids should be reinterpreted. In the juvenile specimen of Zhangheotherium 26 , the tooth identified as the m1 may instead be the dp4. The p3 position is undergoing replacement-if premolar replacement was alternating, as in Dryolestes and basal therians 42,43 and as appears to be the case in Zhangheotherium, the presence of an unshed dp2 implies that the fourth postcanine is the dp4 and that this tooth will likely be replaced at a later ontogenetic stage. This interpretation matches the relatively early ontogenetic age of this individual (relative to the holotype of Zhangheotherium quinquecuspidens), and reduces the disparity in lower dental formula among zhangheotheriids.
Far from an issue of semantics, identification of postcanine tooth positions affects interpretation of homology across Mesozoic lineages (particularly those at the base of the therian line) and reconstruction of ontogenetic processes such as the timing and pattern of tooth replacement. We interpret our specimen to have an upper postcanine formula of P5/M3, which is generally thought to be the primitive count for therians 29,44 . Additionally, the penultimate upper premolar (P4) in Anebodon is the tallest tooth in the postcanine series, a feature also characteristic of therians 29 . Some degree of molarization of the posterior premolars also occurs in various spalacotheriids [45][46][47] , but evidence of replacement of strongly molariform teeth is currently lacking in this derived group. Retention of molariform premolars in the adult dentition is also a characteristic of the endemic South American meridiolestidan dryolestoids 48 ; the distribution of this feature suggests that it is basal to the Trechnotheria and possibly represents the primitive condition for the therian line 25 . Ultimately, the craniodental morphology of Anebodon and the implications raised by its placement at the base of a paraphyletic Zhangheotheriidae highlight the need for a more expansive analysis to explore the interrelationships of basal trechnotherians and, more pointedly, the role these symmetrodont taxa play in an improved understanding of therian evolution.

Methods
Terminology and conventions. Dental measurements are shown in Table 1. We follow the measurement conventions and terminologies of Cifelli and Madsen 49 and Rougier et al. 25,50 . However, we employ traditional therian terminology for tooth structures that have been proposed as homologous in symmetrodonts (e.g., cusp C = metacone, cusp d = hypoconid); see recent review in Davis 18 . Phylogenetic analysis. The data matrix was based on that of Sweetman 51 with an additional character (molarization of the ultimate premolar; see the Supplementary Information for complete character list). Our new taxon and Kiyatherium were added to the matrix. In addition, we updated some scores for Maotherium for characters 3, 24, and 28 based on our observations (BD). The data matrix consisting of 17 taxa and 30 characters was analyzed using a traditional search of TNT 52 . All characters are equally-weighted and non-additive. The TNT analysis produced 10 most parsimonious trees with a tree length of 65 steps, a consistency index of 0.53, and a retention index of 0.72; a strict consensus of these is presented in Fig. 4.  51 . Colours represent global distribution of taxa. Taxa in grey box represent the Zhangheotheriidae, a paraphyletic group in this analysis. Time scale modified from Gradstein et al. 53