Non-technical Summary
The new fossil dissorophid amphibian Buxierophus pouilloni represents the only known skeleton to date of the family Dissorophidae in Europe. Dissorophids are common in the Lower Permian Red Beds of the USA. Buxierophus pouilloni new genus new species is based on well-preserved cranial and postcranial material from ca. 295-million-year-old lake deposit of the Lower Permian (Asselian–Sakmarian) in the Bourbon-l’Archambault Basin of Allier in France. This new dissorophid, with a skull length of about 12 cm, is characterized by a unique combination of characters: a new type of dorsal shield to protect the vertebral column, and the shape of the neural arches of vertebrae. A phylogenetic analysis places Buxierophus n. gen. at the base of the Dissorophidae. This new dissorophid shows aquatic characters such as an ossified ceratobranchial skeleton but a relatively robust body, therefore t may have been semi-aquatic. Buxierophus n. gen. was among the large predators of the Bourbon-l’Archambault Basin.
Introduction
Dissorophoid temnospondyls form an interesting amphibian group with about a hundred species ranging from the Moscovian (upper Carboniferous) to the Induan (Lower Triassic) (Schoch, Reference Schoch2019). Most authors consider that dissorophoid temnospondyls represent the stem-group of Lissamphibia, the clade that comprises all modern amphibians (e.g., Ruta et al., Reference Ruta, Coates and Quicke2003; Ruta and Coates, Reference Ruta and Coates2007; Schoch, Reference Schoch2019; Kligman et al., Reference Kligman, Gee, Marsh, Nesbitt, Smith, Parker and Stocker2023). The body-size reduction, shortening of the trunk, and cranial bone pattern shared by both amphibamiform dissorophoids and lissamphibians support the temnospondyl origin of the latter group (e.g., Fröbisch and Schoch, Reference Fröbisch and Schoch2009). However, this hypothesis of a monophyletic Lissamphibia derived from temnospondyls is still debated and other authors suggest a “lepospondyl” origin of all lissamphibians (Laurin and Reisz, Reference Laurin, Reisz, Sumida and Martin1997; Marjanović and Laurin, Reference Marjanović and Laurin2019). A polyphyletic origin of lissamphibians also has been proposed by some authors (e.g., Anderson et al., Reference Anderson, Reisz, Scott, Fröbisch and Sumida2008a; Pardo et al., Reference Pardo, Small and Huttenlocker2017).
Dissorophoids are small to middle-sized temnospondyls. The smallest known dissorophoids are the branchiosaurids, reaching a maximum skull length of only 35–40 mm in Melanerpeton eisfeldi Werneburg, Reference Werneburg1988, and Leptorophus tener (Schönfeld, Reference Schönfeld1911) (Werneburg, Reference Werneburg1988; RW, personal observation). In contrast, the largest dissorophoids are the trematopids with skull lengths up to 18 cm in Acheloma cumminsi (Olson, Reference Olson1941), and the dissorophids with skull lengths normally up to 19–20 cm in Dissorophus multicinctus Cope, Reference Cope1895, Cacops aspidephorus Williston, Reference Williston1910a, 35 cm in Kamacops acervalis Gubin, Reference Gubin1980 (Schoch and Milner, Reference Schoch and Milner2014), and exceptionally around 40 cm in Anakamacops petrolicus Li and Cheng, Reference Li and Cheng1999 (Schoch and Milner, Reference Schoch and Milner2014; Liu, Reference Liu2018).
Even if their anatomy is relatively well known, the origin of dissorophoids remains enigmatic due to the scarcity of Carboniferous specimens in the fossil record. This contrasts with the abundance of specimens in Lower Permian deposits, which suggests a much earlier diversification of the group (Schoch, Reference Schoch2019; Schoch et al., Reference Schoch, Henrici and Hook2021). Within dissorophoids, recent phylogenetic studies suggest that Amphibamiformes is the sister taxon to the heavily ossified terrestrial Trematopidae and Dissorophidae (both forming Olsoniformes). The monophyly of the dissorophoids has been confirmed (Milner, Reference Milner1993; Anderson et al., Reference Anderson, Henrici, Sumida, Martens and Berman2008b; Reisz et al., Reference Reisz, Schoch and Anderson2009; Schoch, Reference Schoch2012, Reference Schoch2019; Maddin et al., Reference Maddin, Fröbisch, Evans and Milner2013). Among the Olsoniformes, the Dissorophidae are mostly known in the Cisuralian (Lower Permian) of North America (Carroll, Reference Carroll1964; Schoch, Reference Schoch2012) and the Guadalupian (Middle Permian) of Russia and China (Eichwald, Reference Eichwald1848; Gubin, Reference Gubin1980, Reference Gubin1983; Li and Cheng, Reference Li and Cheng1999; Liu, Reference Liu2018).
Here, we describe in detail Buxierophus pouilloni n. gen. n. sp., a relatively large-sized dissorophid temnospondyl from the Lower Permian of Buxières-les-Mines (Allier, France), a rich fossiliferous locality (Steyer et al., Reference Steyer, Escuillié, Pouillon, Broutin and Debriette2000a; Štamberg and Steyer, Reference Štamberg and Steyer2021). Historically, the first fossils from this locality (plants, amphibians and fishes) were mentioned as early as the nineteenth century (de Launay, Reference de Launay1888). However, the first descriptions were made much later (e.g., Letourneur, Reference Letourneur1953; Bougnères, Reference Bougnères1961; Heyler, Reference Heyler1969; Doubinger et al., Reference Doubinger, Vetter, Langiaux, Galtier and Broutin1995).
More recently, between 1992 and 2007, systematic excavations have been conducted by the paleontological Rhinopolis Association under a convention with the HBCM (Houillières des Bassins Centre et Midi). Thanks to its mining activity (the last coal mine closed in 2001), Buxières-les-Mines yielded an important vertebrate fauna composed of large temnospondyls including Onchiodon Geinitz, Reference Geinitz1862 (“Actinodon Gaudry, Reference Gaudry1866”) and Cheliderpeton Fritsch, Reference Fritsch1877 (Werneburg and Steyer, Reference Werneburg and Steyer1999; Steyer et al., Reference Steyer, Escuillié, Pouillon, Broutin and Debriette2000a) as well as the smaller branchiosaurid Xerodromeus gracilis (Credner, Reference Credner1881) (in Werneburg, Reference Werneburg2003, compare Schoch and Werneburg, Reference Schoch and Werneburg2023), the actinopterygians Progyrolepis heyleri Poplin, Reference Poplin1999, Aeduella blainvillei Heyler, Reference Heyler1969, and Paramblypterus cf. P. duvernoyi (Agassiz, Reference Agassiz1833) (Štamberg, Reference Štamberg2018), the acanthodian Acanthodes, and the xenacanth sharks Orthacanthus kounoviensis Fritsch, Reference Fritsch1889 (Schultze and Soler-Gijon, Reference Schultze and Soler-Gijon2004; Luccisano et al., Reference Luccisano, Pradel, Amiot, Pouillon, Kindlimann, Steyer and Cuny2022), Bohemiacanthus sp. and cf. Lissodus (Steyer et al., Reference Steyer, Escuillié, Pouillon, Broutin and Debriette2000a).
The paleoenvironment of Buxières-les-Mines, interpreted as lacustrine, belongs to the Carboniferous–Permian basin of Bourbon-l’Archambault (also called “Aumance Basin”), which is also known from other important localities such as Souvigny (Steyer et al., Reference Steyer, Heyler and Guillot2000b) and Franchesse (Steyer et al., Reference Steyer, Sanchez, Debriette, Valli, Escuillié, Pohl, Dechambre, Vacant, Spence and de Ploeg2012). The new dissorophid of Buxières-les-Mines adds to our knowledge on the amphibian faunas from the Paleozoic of France (e.g., Steyer et al., Reference Steyer, Gand and Pouillon1998).
The objectives of the present study are to: (1) name and describe the new genus and new species with a special emphasis on its peculiar osteoderms, (2) elucidate its phylogenetic position, and (3) evaluate its lifestyle.
Material and methods
Material examined
Buxierophus pouilloni n. gen. n. sp. is represented by an anterior skeleton, RH-D 20-03-99 (21), described here. This specimen was discovered March 20, 1999, by Jacques Rival, technician responsible of the excavations of Buxières-les-Mines (Fig. 1) and preparator in paleontology. These excavations have been conducted by the paleontological Rhinopolis Association since the 1990s. Following the international working convention of Buxières-les-Mines (Pouillon and Steyer, Reference Pouillon and Steyer2001), the specimen described here belongs to the Rhinopolis collection under the number RH-D 20-03-99 (21). The Rhinopolis Association is a public and permanent institution with a large collection and a permanent exhibition in Gannat, Allier, France.
Simplified geology of the Bourbon-l’Archambault Basin near Moulins, France, with the Buxières-les-Mines locality.

The specimen was prepared by Jacques Rival (Rhinopolis Association, France) and Georg Sommer (NaturHistorisches Museum Schloss Bertholdsburg Schleusingen, Germany) with pneumatic tools and needles under a binocular microscope. It is relatively well preserved (Figs. 2, 3) in a “bituminous shale” slab (10 × 20 cm), which corresponds to a thin and laminated dark claystone that is very rich in organic matter. As the slab is very thin and fragile, wax has been used to consolidate the claystone and G. Sommer carefully prepared the specimen on the ventral side too. Photographs were taken using Nikon D5100 and D200 cameras as well as a Zeiss STEREO Discovery V8 stereomicroscope with camera. Interpretative drawings were prepared with a camera lucida on a Motic binocular microscope.
Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (1, 2) Photo in dorsal and ventral views.

Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (1, 2) Interpretative drawing in dorsal and ventral views. a = angular; ap = anterior palatal depression; ar = articular; atl = atlas; ax = axis; beo = basi-exoccipital; c1–3 = coronoids 1–3; cb = ceratobranchials; ch = choane; chy = ceratohyal; cl = clavicle; cth = cleithrum; d = dentary; ec = ectopterygoid; ex.os = external osteoderm; f = frontal; fsgl = supraglenoid foramen; ic = intercentrum; icl = interclavicle; in.os = internal osteoderm; j = jugal; j.e = jugal eminence; la = lacrimal; lee = lateral exposed ectopterygoid; lep = lateral exposed palatine; lsr = lateral supraglenoid ridge; m = maxilla; mf = Meckelian fenestra; n = nasal; na4–8 = neural arch 4–8; n.o = narial opening; op = opisthotic plate; p = parietal; pa = prearticular; p.c = cultriform process of parasphenoid; pc = pleurocentrum; pcl = clavicular process; pl = palatine; pm = premaxilla; po = postorbital; pop = prootic-opisthotic plate; pp = postparietal; ppc = palpebral cup; ppl = palatal plates; prf = prefrontal; ps = parasphenoid; psp = postsplenial; pt = pterygoid; ptf = postfrontal; q = quadrate; qj = quadratojugal; r = rib; sa = surangular; scl = element of sclerotic ring; sc.l = left scapulocoracoid; sc.r = right scapulocoracoid; sm = septomaxilla; sphet = sphenethmoid; sq = squamosal; st = supratemporal; stp = stapes; sy = symphysis region; t = tabular; v = vomer; vs = ventral scales.

Phylogenetical methods
We used a modified version of the character–taxon matrix of Gee (Reference Gee2021) to test the phylogenetic position of Buxierophus n. gen. within dissorophoid temnospondyls. This matrix integrates data from Schoch (Reference Schoch2019), Dilkes (Reference Dilkes2020) and Schoch et al. (Reference Schoch, Henrici and Hook2021) on dissorophoid relationships, and was selected over the Schoch and Sues (Reference Schoch and Sues2022) matrix, which is a down-stream version of the Schoch (Reference Schoch2019) matrix. The matrix of Gee (Reference Gee2021) was chosen because it focuses on dissorophids and includes a more exhaustive sample of dissorophid taxa than other matrices, making it more relevant for our study. This matrix (Gee, Reference Gee2021) is actually derived from Gee (Reference Gee2020), which is mostly a combination of Schoch (Reference Schoch2012) and a suite of trematopid analyses (mostly Polley and Reisz, Reference Polley and Reisz2011, but also Berman et al., Reference Berman, Henrici, Brezinski and Kollar2010, Reference Berman, Henrici, Martens, Sumida and Anderson2011).
All analyses were performed with PAUP* 4.0a169 using a heuristic algorithm with 1000 random additional sequence replicates, a tree bisection reconnection branch swapping algorithm (reconnection limit = 8). Branches were collapsed if they lacked transformations under all optimizations (i.e., if maximum length of branch is zero). Multistate taxa were treated as polymorphic following Gee (Reference Gee2021), including polymorphism coded for Buxierophus n. gen. (character 4). Dendrysekos Steen, Reference Steen1934 (but actually Dendrysekos was synonymized with Dendrerpeton by Arbez et al., Reference Arbez, Atkins and Maddin2022) and Eryops Cope, Reference Cope1878 were used as outgroups for analyses 1–3. Because our focus is here on dissorophid interrelationships, we constrained the monophyly of Dissorophoidea Bolt, Reference Bolt1969, for all analyses in PAUP*.
Character sample
We slightly modified the character sample of Gee (Reference Gee2021) as follows. We added three new characters: (90) osteoderm reticulated ornamentation present (0), absent (1); (92) internal osteoderm with dorsal bi- or multilobed articulation surfaces absent (0), present (1); and (103) clavicle dorsal process overall plain (0), with anterior elbow-like postclavicular process (1). We also slightly modified the character state (1) of character (59) ornamentation (dorsal eminences): “skull table with elevated eminences on the nasal, frontal, parietal, postfrontal and postparietal” into “skull table with elevated eminences on the nasal, frontal, parietal, postfrontal, postparietal and jugal”. The character definitions, the new scorings of Buxierophus n. gen., and the revised matrix are provided in Supplementary Material.
Taxon sample
We conducted several analyses based on subsets of the original taxon sample of Gee (Reference Gee2021) and with the addition of Buxierophus n. gen. Our various analyses are intended to mimic a subset of those of Gee (Reference Gee2021) (e.g., with or without wildcards, with or without non-Dissorophoidea, etc.).
Analyses 1a and 1b
Analyses 1a and 1b employ a reduced dataset compared to Gee (Reference Gee2021). All taxa with less than 25% of scored characters were removed from the matrix of Gee (Reference Gee2021), as well as specimen level-OTUs and several non-dissorophids. We found this pertinent given that our aim here is to study the systematic position of Buxierophus n. gen. among dissorophoids and not to reassess dissorophoid interrelationships. Dendryskeos and Eryops were retained to serve as outgroups to Dissorophoidea Bolt, Reference Bolt1969. In addition, we also retained the putative non-Xerodrome dissorophoid Micromelerpeton Bulman and Whittard, Reference Bulman and Whittard1926, the putative non-Olsoniform Doleserpeton Bolt, Reference Bolt1969, as well as Palodromeus in order to test the monophyly of Dissorophoidea, Xerodromes Schoch and Milner, Reference Schoch and Milner2014, and Olsoniformes Anderson et al., Reference Anderson, Henrici, Sumida, Martens and Berman2008b. Analysis 1a does not include Buxierophus n. gen. in order to assess the topology recovered by this reduced-taxon sampling before inclusion of the new taxon in analysis 1b. The total number of OTUs is thus 29 (analysis 1a) and 30 (analysis 1b).
Analysis 2
Analysis 2 employs a similar taxon sample to Analysis 1b with the exclusion of the wildcard taxa Brevidorsum Carroll, Reference Carroll1964, and Reiszerpeton Maddin et al., Reference Maddin, Fröbisch, Evans and Milner2013, identified by Dilkes (Reference Dilkes2020) and Gee (Reference Gee2021) but not Conjunctio Carroll, Reference Carroll1964, and Scapanops Schoch and Sues, Reference Schoch and Sues2013, also identified as wildcards by Dilkes (Reference Dilkes2020) and Gee (Reference Gee2021), but which share many anatomical similarities with Buxierophus n. gen. (see description above). The total number of OTUs is thus 28.
Analysis 3
Analysis 3 employs a similar taxon sample to Analysis 2, but with the exclusion of the wildcard taxa Conjunctio and Scapanops. The total number of OTUs is thus 26 (see Appendix 2).
Repositories and institutional abbreviations
AMNH FARB, American Museum of Natural History, Fossil Amphibians, Reptiles, and Birds, New York, NY American Museum of Natural History, New York, USA; FMNH, Field Museum of Natural History, Chicago, USA; MCZ, Museum of Comparative Zoology, Cambridge/Boston, USA; RH, Rhinopolis Associative Museum, Gannat, France.
Systematic paleontology
Temnospondyli Zittel, Reference Zittel1888
Rhachitomi Watson, Reference Watson1919, sensu Schoch, Reference Schoch2013
Dissorophoidea Bolt, Reference Bolt1969
Olsoniformes Anderson et al., Reference Anderson, Henrici, Sumida, Martens and Berman2008b
Dissorophidae Boulenger, Reference Boulenger, Wallace, Hadley and Chisolm1902
Buxierophus new genus
Types species
Buxierophus pouilloni n. gen. n. sp.
Diagnosis
As for type species by monotypy.
Etymology
After the type locality of Buxières-les-Mines in France, and the ancient Greek orophe (roof) in reference to its armored appearance.
Holotype
RH-D 20-03-99 (21), right half of the skull and its articulated anterior skeleton.
Diagnosis
Buxierophus pouilloni n. gen. n. sp. differs from all other dissorophids in the following diagnostic combination of characters.
Autapomorphies
(1) external osteoderms in dorsal view smooth except for few conspicuous peaks; (2) external osteoderms thin (thickness about 1 mm); (3) internal osteoderms with dorsal bi- or multilobed articulation surfaces; (4) anterior neural arches of the same sagittal length than that of the osteoderms; (5) anterior trunk ribs with widened distal ends.
Synapomorphic characters shared with some of the dissorophids
(1) narrow parabolic tip of snout laterally convex (also in Conjunctio multidens Carroll, Reference Carroll1964, sensu Schoch and Sues, Reference Schoch and Sues2013; Cacops morrisi Reisz, Schoch, and Anderson, Reference Reisz, Schoch and Anderson2009; Broiliellus texensis Williston, Reference Williston1914; or Aspidosaurus Broili, Reference Broili1904; but in contrast to more pointed snout of Dissorophus multicinctus Cope, Reference Cope1895, and others); (2) relatively flat relief of roofing elements (in contrast to Broiliellus arroyoensis DeMar, Reference DeMar1967; Fig. 4.3) and Broiellus olsoni DeMar, Reference DeMar1967; (3) cranial ornamentation varies greatly in intensity (also in Cacops Williston, Reference Williston1910a); (4) nasal extends beyond anterior margins of external nares (also in Cacops aspidephorus Williston, Reference Williston1910a); (5) postorbital narrowing posteriorly, resulting in a more triangular dorsal contour (also in Broiellus brevis Carroll, Reference Carroll1964, Cacops woehri Fröbisch and Reisz, Reference Fröbisch and Reisz2012, Conjunctio multidens, see Schoch and Sues, Reference Schoch and Sues2013, Dissorophus Cope, Reference Cope1895, Platyhystrix rugosa Berman, Reisz, and Fracasso, Reference Berman, Reisz and Fracasso1981, and Scapanops Schoch and Sues, Reference Schoch and Sues2013); (6) jugal with large eminence bearing knobby ornament (also in Dissorophus, Scapanops, Broiellus reiszi Holmes et al., Reference Holmes, Berman and Anderson2013, Broiellus brevis, and Broiellus texensis); (7) elevated ridge on jugal (only in Cacops morrisi); (8) interorbital region very narrow (IOw/Sl lower than 0.20; in contrast to nearly all other dissorophids; only similar in Cacops morrisi); (9) dorsal exposure of suture between squamosal and supratemporal more than half as long as supratemporal itself (also in Cacops woehri and Conjunctio multidens); (10) supratemporal without ventral projection into squamosal embayment (semilunar flange sensu Bolt, Reference Bolt1974b) (also in Broiellus reiszi); (11) lacrimal as part of orbital margin (in contrast to Cacops morrisi); (12) dorsolateral exposure of ectopterygoid (also in Broiliellus reiszi Holmes et al., Reference Holmes, Berman and Anderson2013, Cacops morrisi, Cacops aspidephorus; see Anderson et al., Reference Anderson, Scott and Reisz2020); (13) basal plate of parasphenoid 1.7 times wider than long (only shared with Broiellus brevis); (14) carotid foramina clearly spaced in wide distance on basal plate (in contrast to cacopines); (15) mid-trunk neural arches with large expansion of spines along sagittal axis (shared with Cacops; see Dilkes and Brown, Reference Dilkes and Brown2007; Gee et al., Reference Gee, Bevitt and Reisz2019b; Diploseira, Dilkes, Reference Dilkes2020), but in contrast to other ones (Schoch, Reference Schoch2012). (16) narrow external osteoderms only 1.4 times wider than long (in Aspidosaurus/syn. Alegeinosaurus and Dissorophus 2.2–6.5 times wider than long); (17) internal osteoderm unfused with neural arch (also in Dissorophinae, see Schoch, Reference Schoch2012); (18) clavicle ornamented with pitting or grooves similar to the skull (also in Dissorophus); (19) clavicular dorsal process with anterior elbow-like postclavicular process (also in Dissorophus and in amphibamiform Eoscopus Daly, Reference Daly1994).
Occurrence
Ancient open coal mine («Découverte») N°IV of the HBCM (Houillières des Bassins Centre et Midi, Charbonnages de France) located 1 km northeast from the village of Buxières-les-Mines, Bourbon-l’Archambault Basin (sometimes called Aumance Basin), Allier, France. The coal mine closed in 2001 and is now completely filled. Type horizon is a laminated claystone of the bituminous shale sequence of the Supra Buxières Member of the Buxières-les-Mines Formation (Debriette, Reference Debriette1992), Asselian and/or Sakmarian, Lower Permian (Werneburg, Reference Werneburg2003; Steyer, Reference Steyer2004; Schneider et al., Reference Schneider, Lucas, Scholze, Voigt and Marchetti2020).
Comparative description
The specimen is well preserved in a thin-bedded and laminated claystone slab (Figs. 2, 3). It consists of the right half of a skull and its associated anterior postcranial skeleton. The frontals, parietals and postparietals are not well-preserved and the forelimbs are missing. Details of the skeleton are shown in Figures 4–10, partly in comparison with related dissorophids.
Comparison of pronounced nasal and jugal sharp ridges (white arrows) between (1, 4, 5) Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21); (2) Broiliellus texensis, MCZ 1747; and (3) Broiliellus arroyoensis, FMNH – UR 431.

The vertebral centra and parts of the endocranium are well ossified, and the dermal bones show a relatively well-developed ornamentation (see below). These suggest that the specimen is an adult or sub-adult individual in age (e.g., Steyer, Reference Steyer2000).
Skull roof
The right half of the skull is nearly complete and allows us to reconstruct the skull in dorsal and ventral views (Fig. 10.1–10.3). The midline skull length is 11.8 cm. The tip of the snout is parabolic, as in Conjunctio multidens (see Schoch and Sues, Reference Schoch and Sues2013) or Cacops morrisi (see Reisz, Schoch, and Anderson, Reference Reisz, Schoch and Anderson2009). The preorbital length of the skull is greater than the postorbital length (by more than 10%), as in Aspidosaurus binasser Berman and Lucas, Reference Berman and Lucas2003, and Cacops morrisi (compare Table 1). The orbital openings are relatively large (Ol/Sl = 0.29), in contrast to A. binasser. The otic notch is very deep. The minimum distance between the otic notch and the posterior orbital margin is distinctly short, only about 11% of the total midline length. The interorbital region is especially narrow (IOw/Sl = 0.18), in contrast to all other dissorophids (Table 1). The external narial opening is elongated oval in shape. The angle between the length axis of the naris and the midline suture of the skull is close to 45°, as in Dissorophus and Broiliellus. This angle is very variable within dissorophids; it is more than 45° in Cacops morrisi and Conjunctio multidens, but close to 0° in A. binasser and Scapanops neglectus Schoch and Sues, Reference Schoch and Sues2013. The well-preserved anteromedial margin of the right premaxilla is incised to frame a small broad-oval-shaped ‘internarial’ fenestra (Fig. 3.1), which is similar to those known in Cacops morrisi, Conjunctio multidens, A. binasser and S. neglectus, but not in Broiliellus and probably not in Dissorophus (Schoch, Reference Schoch2012; contra Dilkes, Reference Dilkes2020, p. 22). However, this small ‘internarial’ fenestra is contained entirely within the premaxillae as is known from a few trematopids (e.g., Acheloma; Polley and Reisz, Reference Polley and Reisz2011) but not from dissorophids.
Biometric characters in dissorophids; largest and smallest quotients in bold (compare with Fig. 10.5). aSw = anterior skull width at level of maxilla-premaxilla sutures; Hl = postorbital midline skull length from level of posterior margins of orbits; Hw = postorbital skull width between lateral margins of supratemporals; INw = minimum internarial width; IOw = minimum interorbital width; mSw = midlength skull width at midlength level of orbits; Occ-Q = length between levels of occipital midline margin and posterior quadrate margin; ON-O = length between levels of anterior otic notch margin and posterior orbital margin; Ol = maximum length of orbit; POl = preorbital midline skull length from level of anterior margins of orbits; Pol = maximum posterior length of postorbital from posteriormost extent of orbit; pSw = maximum posterior skull width at level of posterolateral margins of cheeks; Sl = midline skull length; Thl = length of tabular horn between levels of posterior tabular corner and occipital midline margin

The dermal sculpturing of the dorsal skull roof is very characteristic of this new species. It is a reticulated pattern of mostly low, coarse ornament: small-scale elongated ridges surround rounded pits to form polygons, or they surround more elongated pits and valleys. Buxierophus n. gen. also has a peculiar system of cranial ridges probably to stabilize the skull roof (Figs. 2.1, 3.1, 4.1, 4.4, 4.5, 10.1, 10.3); a pronounced sharp ridge runs on the nasal from the posterior tip of the alary process of the premaxilla to the most anterior part of the prefrontal. This sharp ridge merges on the prefrontal in a large strut-like ridge formed by more knobby ornament, then it curves on the posterior tip of the prefrontal. The next pronounced ridge, which runs on the jugal beside the posteroventral margin of the orbit, is a wall-like sharp ridge of more heavy ornament. A similar ridge is also known in Cacops morrisi (see Reisz et al., Reference Reisz, Schoch and Anderson2009). This sharp ridge continues with a gap on the postorbital where it is Y-shaped and swollen; it indeed runs anteroposteriorly from the posterior end of the postorbital (or from the supratemporal) in two directions towards the anterolateral suture with the jugal and towards the anteromedial part of the postorbital. A relatively large strut-like ridge, formed by the knobby ornamentation of the skull roof bones, runs from the tabular horn anteriorly to the posterior half of the supratemporal. These ridges are not preserved on the frontal, postfrontal, or anterior supratemporal. The nearly orthogonal curved ridge system on the nasal and prefrontal is well known in Broiliellus and Dissorophus. It is similar in Broiellus texensis Williston, Reference Williston1914 (Fig. 4.2), D. multicinctus (see Schoch, Reference Schoch2012), and Broiellus arroyoensis (Fig. 4.3). Other dissorophids also have these ridges, but they are always shallower (Schoch, Reference Schoch2012). The ridges on the postorbital are reported in Broiellus brevis, D. multicinctus, and Conjunctio multidens. In Buxierophus n. gen., the dorsal surface of the jugal surprisingly bears a large eminence located on its posterior part and formed by a rounded triangular knobby ornament. This ornamental element is similarly developed in D. multicinctus (see Schoch, Reference Schoch2012), Broiellus brevis (see Carroll, Reference Carroll1964), Broiellus texensis, Broiellus reiszi, and Scapanops.
The skull roof bones of Buxierophus n. gen. are relatively thin, compared with similar-sized skulls of Cacops morrisi (Reisz et al., Reference Reisz, Schoch and Anderson2009; Schoch Reference Schoch2012) or D. multicinctus (Williston, Reference Williston1910b; DeMar, Reference DeMar1968; Milner, Reference Milner2003). The position of the jaw articulation is slightly posterior to the posterior facets of the basisphenoid-exoccipital.
Most of the proportions discussed here are presented in Table 1, where measurements of related dissorophids are compared. Figure 10.5 illustrates the position of the measurements.
The premaxilla is relatively narrow and has a very elongated distinct alary process overlapping the nasal and reaches the middle or the posterior part of the naris. The existence of a small ‘internarial’ fenestra between both premaxillae is discussed above. The maxilla, an elongated and narrow bone, probably terminates posteriorly into the quadratojugal, up to the level of the anterior margin of the otic notch. Its anterodorsal portion is relatively low. The septomaxilla is rarely recorded in dissorophids. The midlateral corner of the right nasal margin accounts for articulation with a small rectangular bony plate, as does the septomaxilla at the posterior rim of the naris and above the lacrimal. The nasal is the most elongated median skull-roof bone. Its anterior third is narrower because of the curved margin of the narial opening. The pronounced sharp ridge runs on the nasal from the posterior tip of the overlapping premaxilla up to the most anterior part of the prefrontal. On the prefrontal, this ridge is swollen by more knobby ornament and curved to the posterior tip of the prefrontal. The prefrontal contacts neither the postfrontal nor the jugal. It is ventrolaterally expanded, stabilizes the anterior orbital rim and is overlapped by the posterodorsal part of the lacrimal. This ventrolateral prefrontal process is in contact with both lateral exposed palatine (LEP) and ectopterygoid (LEE; Fig. 10.3). The laterally visible palatine is small and triangular. The laterally exposed ectopterygoid has a very narrow but elongated lateral expansion. The lacrimal contacts the septomaxilla anteriorly and the orbital margin posteriorly. The nasolacrimal canal is represented by a narrow distinct furrow which runs from the posteromedian edge of the lacrimal to nearly the middle of this bone. In Buxierophus n. gen., the lacerated and lobed posterior margin of the lacrimal is similar, as in Cacops woehri (Fröbisch and Reisz, Reference Fröbisch and Reisz2012), which has yet shorter furrows.
The jugal, relatively narrow and triangular, is reaching anteriorly to the level of the anterior quarter of the orbit. It is in contact anterolaterally with the lateral exposed ectopterygoid and ventrolaterally with the maxilla, but not with the lacrimal. A pronounced sharp ridge runs beside the posteroventral orbital margin, which in dissorophids is known only in Cacops (e.g., Cacops morrisi, see Reisz et al., Reference Reisz, Schoch and Anderson2009). The jugal bears an additional sculpture pattern element on its posterior part: a large rounded triangular eminence with a knobby ornament, which is known in few dissorophoids (see above).
The quadratojugal is very elongated anteriorly, up to the mid-level of the lateral orbital margin. Its lateroventral margin is convex, as in D. multicinctus (Schoch, Reference Schoch2012, fig. 4C). The posterolateral end of the quadratojugal forms a boss-like process and contacts the prominent posterodorsal outgrowth of the quadrate (i.e., quadrate boss). The anterior part of the quadratojugal probably receives the posterior peaks of the maxilla and jugal. The most posterior part of the quadratojugal is strongly concave and forms the posterolateral margin of the otic notch. The dorsal quadrate shows a small crescent-shaped process. The squamosal surrounds nearly completely the otic notch. It shows a dorsally to laterally exposed ornamented area (= supratympanic flange of Bolt, Reference Bolt1974b; = semilunar flange of Schoch and Rubidge, Reference Schoch and Rubidge2005), which continues ventrally into poorly ornamented or smooth portions of the squamosal (compare Schoch, Reference Schoch2012). The curvature along the ventral border of the supratympanic flange is semilunar in shape. The dorsal suture between the squamosal and supratemporal is long, equal to half the length of the supratemporal, like in Conjunctio, and more elongated than in all other dissorophids (Schoch, Reference Schoch2012). The squamosal and tabular are separated by the supratemporal in dorsolateral view (Fig. 10.3), but their contact may be more ventrolaterally located (compare Schoch, Reference Schoch2012, fig. 4A–C). The supratemporal, which is longer than wide, has no ventral projection into the otic notch (semilunar flange sensu Bolt, Reference Bolt1974b) (i.e., it has neither a semilunar flange nor a supratemporal flange, sensu Schoch and Rubidge, Reference Schoch and Rubidge2005). This absence of a semilunar flange is shared with Broiellus reiszi (Holmes et al., Reference Holmes, Berman and Anderson2013) and Broiellus olsoni (Schoch, Reference Schoch2012) but not with the other dissorophids. The tabular is wider than long and presents posterolaterally some knobby tubercles. The tabular horn is rounded and short, without a distinct tabular process. This absence of a tabular process is shared with few other dissorophids (e.g., Aspidosaurus or Scapanops, see Schoch, Reference Schoch2012). The postorbital is broad, but bears a short, rapidly tapering posterior process, which reaches posteriorly the level of the anterior margin of the otic notch. The postorbital has a relatively wide suture with the supratemporal, therefore precluding contact between the squamosal and postfrontal, as in Cacops morrisi (Reisz et al., Reference Reisz, Schoch and Anderson2009). The postparietal, parietal, frontal, and postfrontal are poorly preserved. The frontal enters the orbital margin. It is slightly shorter than the nasal and especially very narrow in its posterior half (IOw/Sl = 0.18). The frontal is more elongated than the lateral part of the orbit. The parietal is relatively short, and about twice as long as wide.
The sclerotic ring, which lies in the orbital opening, is composed of relatively small rectangular bony plates (Figs. 2, 3.2). Numerous and relatively large palpebral ossicles are situated at the medial margin of this sclerotic ring. Beside these ossicles, a very large palpebral cup is also visible in the orbital opening: it is much longer than the basal plate of the parasphenoid. The palpebral ossicles show a reticulated dorsal ornamentation, as seen on the skull roof bones, but their ornamentation pattern here is thinner and smaller in size. They have a smooth ventral surface. A large palpebral cup is also visible in Broiellus brevis, Broiellus texensis, and Brevidorsum profundum Carroll, Reference Carroll1964.
Palate
The palate of the right half-skull and the endocranium are nearly complete and well exposed in ventral view. The ventral surface of the palatal bones is flat and does not show any strutting pattern of larger ridges, as it is the case in eryopids (Werneburg and Berman, Reference Werneburg and Berman2012). Yet the vomer of Buxierophus n. gen. has a slightly striated posterior margin. The palatal bones are covered by denticle shagreens or patches. The interpterygoid vacuities are relatively large and semi-circular (i.e., with a maximum width at the level of their midlength) as in D. multicinctus and Broiellus brevis. In contrast, Cacops has narrower interpterygoid vacuities (Fröbisch and Reisz, Reference Fröbisch and Reisz2012; Schoch, Reference Schoch2012), and Kamacops and Parioxys have shorter ones (Schoch and Sues, Reference Schoch and Sues2022). Each palatine borders the interpterygoid vacuity along its entire medial margin. These interpterygoid vacuities are partially filled by numerous bony plates of various size, which are also covered by a shagreen of small teeth in ventral view. These bony plates form a series running along the posterior margin of the vomer and the medial palatine, but they covered the complete interpterygoid vacuities in life. This is also the case in Cacops morrisi (Reisz et al., Reference Reisz, Schoch and Anderson2009).
The vomer is relatively wide; therefore, the snout is not markedly pointed. Its posteromedian margin is straight horizontally, as in Broiellus reiszi (Holmes et al., Reference Holmes, Berman and Anderson2013) but not in the other dissorophids (Schoch, Reference Schoch2012, fig. 2). The vomer of Buxierophus n. gen. has probably two dorsal depressed areas in its anteromedian region, namely the paired anterior palatal fossae. Although these fossae are known in various temnospondyls (e.g., eryopids, plagiosaurids, or cochleosaurids), they are here probably unique among dissorophids. The vomer is covered with a dense shagreen of small teeth. It has a pair of relatively small fangs between the choana and anteropalatal fossa. These fangs are similar in size to those of the ectopterygoid, but smaller than those of the palatine. The fangs of the vomer in Cacops morrisi are much larger and as large as those on its palatine (Schoch, Reference Schoch2012). The vomer of Buxierophus n. gen. has no denticles along the medial edge of the choana. That is an additional difference from Cacops morrisi (Reisz et al., Reference Reisz, Schoch and Anderson2009; Schoch, Reference Schoch2012).
The palatine bears a large fang pair and has an elongated suture with the vomer and ectopterygoid. It enters the interpterygoid vacuity. The lateral exposed palatine is discussed above. The palatine and ectopterygoid are much wider than the maxilla. Both are covered by a shagreen of teeth and are relatively short, so that the ectopterygoid terminates anterior to the posterior margin of the orbit. This ectopterygoid bears a small pair of fangs (see above), which is known in other dissorophids (e.g., Cacops woehri, Fröbisch and Reisz, Reference Fröbisch and Reisz2012; Broiellus reiszi, Holmes et al., Reference Holmes, Berman and Anderson2013).
The pterygoid contacts the palatine but not the vomer. A shagreen of small teeth covers most of the pterygoid. The basipterygoid branch of the pterygoid is firmly sutured with the parasphenoid at mid-level of its widened basipterygoid process. Its palatine ramus is broadening abruptly and forms a pronounced transverse flange, giving its lateral margin a rectangular shape. Schoch (Reference Schoch2012) defined this feature as synapomorphic for the dissorophids. The transverse flange is completely covered by a shagreen of teeth in Buxierophus n. gen. in contrast to D. multicinctus (compare Schoch, Reference Schoch2012, figs. 3D, 4H). The quadrate condyle is relative narrow and intercalated between the pterygoid and quadratojugal.
The parasphenoid has a smooth ventral surface lacking denticles, which is characteristic for dissorophids, most branchiosaurids, and Phonerpeton Dilkes, Reference Dilkes1990 (Schoch, Reference Schoch2012). The carotid artery foramen pierces the anteromedian portion of the parasphenoid basal plate, as in most dissorophids. However, in Cacops, this foramen is situated on the posterior part of the cultriform process (Reisz et al., Reference Reisz, Schoch and Anderson2009; Fröbisch and Reisz, Reference Fröbisch and Reisz2012). In Buxierophus n. gen., the parasphenoid basal plate is much shorter than wide, as in Broiellus brevis (Schoch, Reference Schoch2012), but it differs from the narrower basal plate of all other dissorophids. The cultriform process is narrow and relatively thin. It is clearly narrower and slightly swollen in most of its anterior part. This feature is only shared with Kamacops (Schoch, Reference Schoch1999, Reference Schoch2012). The posterolateral wing of the parasphenoid plate is located well beyond the level of the basipterygoid suture. The posterior margin of the basal plate is crenulated with several narrow lobes and one pair of these lobes is more elongated (Fig. 5.5; compare the trematopid Acheloma Cope, 1882, cited in Maddin et al., Reference Maddin, Reisz and Anderson2010, fig. 4C).
Endocranium
The basioccipital and exoccipital are fused in a basioccipital-exoccipital complex. The width of this complex is slightly superior to the distance between the carotid foramina. The posterior part of the basioccipital-exoccipital complex is bilobed, forming the double cotyloform facet of the occipital condyle which contacts the atlas (Figs. 5.5, 10.2). The ventromedian part of the basioccipital-exoccipital complex is composed of two posterolateral facets and a pair of ventrally directed processes or facets (Fig. 5.5). The narrow opisthotic and the poorly preserved prootic-opisthotic complex are visible laterally to the basioccipital-exoccipital complex. These complexes together have the same width as the basal plate of the parasphenoid. The occipital condyle lies slightly anterior to the level of the jaw articulation, in contrast to D. multicinctus (Schoch, Reference Schoch2012, figs. 2, 3D). The configuration of the basioccipital and exoccipital is very variable in dissorophids (Schoch, Reference Schoch2012). The shape of the basioccipital-exoccipital complex in Buxierophus n. gen. is very similar than that of Broiellus brevis (Carroll, Reference Carroll1964). A small part of the sphenethmoid may be preserved dorsal to the cultriform process (Fig. 3.2).
Visceral skeleton
The right stapes is preserved nearly in its anatomical position. The stapedial footplate is widened and clearly pierced by the stapedial foramen which is combined with an elongated furrow. A small expansion, visible on the midshaft of the bone, may be the dorsal process. The stapes of dissorophids is rarely preserved. The stapes of Buxierophus n. gen. has the same shape as that of Broiellus reiszi but the later shows no stapedial foramen (Holmes et al., Reference Holmes, Berman and Anderson2013). Beyond Buxierophus n. gen., a stapedial foramen also has been reported in the stapes of Cacops morrisi (Schoch, Reference Schoch2012), D. cf. D. multicinctus (Gee et al., Reference Gee, Bevitt and Reisz2019b, fig. 14), and Aspidosaurus binasser (Berman and Lucas, Reference Berman and Lucas2003, p. 251).
Interestingly, Buxierophus n. gen. also shows ossified ceratobranchial elements. This is the first time a preserved ossified ceratobranchial skeleton has been reported in dissorophids. The right ceratohyal and one ceratobranchial (probably cb1) can be confidently recognized (Fig. 5). The ceratohyal is distinctly narrow in ventral view and greatly expanded dorsoventrally. It is very similar in shape to that of the eryopid Glaukerpeton avinoffi Romer, Reference Romer1952 (Werneburg and Berman, Reference Werneburg and Berman2012, figs. 9, 11, 12B). The probable ceratobranchial 1 has an only slightly expanded anterior end and a much more widened posterior end. Its anterior part clearly exhibits a median keel in ventral view. The extremities of the possible ceratobranchials 2 and 3 are preserved on the posterior end of the ceratobranchial 1. Its narrower extremity may be the anterior end of the bone, and the much more widened extremity may be the posterior end of the ceratobranchials. Additionally, two widened posterior ends of possible ceratobranchials are situated in the otic notch in dorsal view (Figs. 2.1, 3.1, 5.4). The ceratohyal and the probable original four ceratobranchials are used in the reconstruction of the visceral skeleton (Fig. 10.2).
Detailed view of the palate, endocranium, and visceral skeleton of Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). Ceratobranchial with deep groove: (1, 2) photo and interpretative drawing. (3) Ceratohyal in lateral and ventral views, interpretative drawing; compare with Figure 5.5. (4) Photo of ceratobranchials in dorsal view presented in otic notch, compare with Figures 2.1 and 3.1. (5) Interpretative drawing of the palate, visceral skeleton, endocranium, and first vertebrae. atl = atlas; ax = axis; beo = basi-exoccipital; c1–3 = coronoids 1-3; cb = ceratobranchials; chy = ceratohyal; cg = groove for carotid artery; cl = clavicle; op = opisthotic plate; p.c = cultriform process of parasphenoid; pop = prootic-opisthotic plate; ppl = palatal plates; ps = parasphenoid (basal plate); ps.p = basipterygoid process of parasphenoid; pt = pterygoid; sa = surangular; sq = squamosal; stp = stapes.

Mandible and dentition
Both rami of the lower jaw are partly visible in medial view. The right one and the coronoid-surangular process of the left one are used in the reconstruction of Figure 10.4. The mandible of Buxierophus n. gen. is relatively flat in comparison with the high posterior region of the lower jaw in Broiellus reiszi (Holmes et al., Reference Holmes, Berman and Anderson2013). The posterior part of the mandible in D. multicinctus (DeMar, Reference DeMar1968) is similarly flat as that of Buxierophus n. gen.
A coarse dermal sculpturing pattern extends onto the ventromedial surface of the angular and on the ventral side of the postsplenial. The anteriorly curved rim of the Meckelian fenestra may be preserved on the prearticular. This sculptured part of the postsplenial is rarely preserved in other dissorophids (Cacops morrisi, Gee and Reisz, Reference Gee and Reisz2018, fig. 10; Gee et al., Reference Gee, Bevitt and Reisz2019b, fig. 5; Cacops aspidephorus, Anderson et al., Reference Anderson, Scott and Reisz2020). An inflection of the prearticular along the medial rim of the adductor fossa (Dilkes, Reference Dilkes1990; Schoch, Reference Schoch2012) is absent. The posterior coronoid (c3) appears on the dorsal rim of the hemimandible as a process-like, rounded crest (Figs. 3.2, 10.4). Small denticles are preserved on the middle coronoid. A symphyseal depression is visible between the anterior coronoid and the dentary, but no details are preserved. A separated small bone fragment lies on the posterior end of the prearticular and belongs to the surangular. Two other small bony pieces in this region represent the articular.
The dentary teeth are relatively short, about 3 mm in height. One tooth is well preserved in labiolingual view (Fig. 3.1). Its base is rounded, and the tip of the crown has lateral blades. There is no evidence of labyrinthine infolding or pedicellate structure. The preserved teeth of the dentary show little recurvature. The typical, gradual decrease in tooth height in the posterior direction is not clearly visible.
Vertebrae and ribs
Remains of the first nine presacral vertebrae are visible, but without the dorsal portion of their neural spines (Fig. 6). The vertebrae are of rhachitomous type, which is common in dissorophids. The lateral shape of the intercentrum is triangular and that of the pleurocentrum is bean-like. Remains of the neural arches of the atlas and axis, with crest-like ridges, are preserved posteriorly to the basioccipital (Fig. 5.5). The mid-trunk neural arches have a large expansion of the spines along the sagittal axis (Fig. 6), as known from a few dissorophids (e.g., Cacops, see Dilkes and Brown, Reference Dilkes and Brown2007, fig. 2; Gee et al., Reference Gee, Bevitt and Reisz2019b, fig. 2; Diploseira, see Dilkes, Reference Dilkes2020, p. 15), but in contrast to other ones (Schoch, Reference Schoch2012, fig. 7). The postzygapophyses are very elongated posteriorly compared to those of the other dissorophids.
Vertebral column with ribs of Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21): (1) interpretative drawing and (3) photo; (2) vertebral reconstruction with osteoderms in lateral view. az = anterior zygapophysis; cl = clavicle; cth = cleithrum; ex.os = external osteoderm; ic = intercentrum; in.os = internal osteoderm; na4–8 = neural arch 4–8; pc = pleurocentrum; pz = posterior zygapophysis; r = rib; rf = rib facet; sc.l = left scapulocoracoid.

Osteoderms of Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (1, 2) Reconstruction of external and internal osteoderms in dorsal view and lateral views; (3, 4) interpretative drawing and photo. ex.os = external osteoderm; in.os = internal osteoderm.

Three anterior ribs are visible (Figs. 2, 3, 6.1, 7.4, 9.3). One of the most anterior ribs has a widened proximal and distal head and may be relatively short. There is no apparent uncinate process as well.
Osteoderms
Two series of osteoderms, comprising an internal and an external osteoderm for each vertebra, are recorded in the region of the 9th and 10th vertebrae (Fig. 7). They are covering the vertebral column dorsally and are transversely short. The osteoderms of the internal series are intersegmental in position and each of the external series may be arranged above the neural spine of the vertebrae. A ventrally projecting flange of the internal osteroderm inserts between successive neural spines but is not fused with the adjacent vertebrae (Fig. 6.2). This osteoderm pattern is well known in most representatives of the Dissorophinae (Carroll, Reference Carroll1964; DeMar Reference DeMar1968; Bolt, Reference Bolt1974a; Schoch, Reference Schoch2012), particularly in Dissorophus and most species of Broiliellus.
The osteoderms of the internal series have a step-like facet on the anterior margin and a pair of lobed facets on the posterior margin to articulate dorsally with the external osteoderms. The external osteoderms are very narrow, only 1.4 times wider than long (Fig. 8). They are as wide as the tabular of the skull roof. Such osteoderms are far narrower than those of the typical dissorophine, the external osteoderms of Dissorophus are 6 times wider than long and reach at least the width of two postparietals (Schoch, Reference Schoch2012).
Comparison of the ornamentation pattern on osteoderms. (1) Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (2) “Alegeinosaurus aphthitos” Case, Reference Case1911, AMNH FARB 4756, which may be a junior synonym of Aspidosaurus sensu Gee, Reference Gee2018. (3) Aspidosaurus glascocki Case, Reference Case1910, AMNH 4864. (4–6) Aspidosaurus sp., MCZ 1477. (7) Dissorophus sp., MCZ 4188. ex.os = external osteoderm; in.os = internal osteoderm.

In Buxierophus n. gen., the external osteoderms are thin, about 1 mm thick. The dorsal surface of the external osteoderms is smooth but bears two lateral peaks and one median conspicuous peak. In nearly all other dissorophids, the dorsal surface of the osteoderms shows a characteristic reticulated ornamentation, as is the case on the skull roof and ventral pectoral girdle bones (Fig. 8.2–8.7). The osteoderms of the dissorophid ‘Aspidosaurus apicalis’ (Cope, Reference Cope1881) do not show this typical ornamentation of the skull either—they seemingly appear to be relatively flat but bear few robust tubercles (see Gee, Reference Gee2021, fig. 24). However, these thick osteoderms with sparse ornamentation are not comparable with the thin and smooth osteoderms of Buxierophus n. gen.
Pectoral girdle
The clavicle is completely preserved and shows a relatively short ventral blade with a striated dermal sculpture (Fig. 9). Its postclavicular process at the end of the ventral blade is pronounced anteriorly and similar to that of Dissorophus (DeMar, Reference DeMar1968) and of the amphibamiform Eoscopus (Daly, Reference Daly1994). The cleithrum is recorded with its relatively thick ventrally directed process, its dorsal end is not preserved. The small, preserved part of the interclavicle suggests that it had a short plate without a posterior process, like in Dissorophus (DeMar, Reference DeMar1968). The central parts of the scapulocoracoids indicate relatively narrow bony scapular blades. The dorsal margin of the glenoid foramen is preserved in lateral view. The pectoral girdle of Buxierophus n. gen. in lateral view is very similar to that of Dissorophus (Carroll, Reference Carroll1964; DeMar, Reference DeMar1968).
Pectoral girdle of Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (1, 2) Reconstruction in ventral and lateral views. (3) Photo. cl = clavicle; cth = cleithrum; fsgl = supraglenoid foramen; gl = glenoid fossa; icl = interclavicle; lsr = lateral supraglenoid ridge; pcl = clavicular process; sc.r = right scapulocoracoid.

Skull of Buxierophus pouilloni n. gen. n. sp., holotype RH-D 20-03-99 (21). (1–3) reconstructions in dorsal, ventral, and lateral views; (4) reconstruction of the mandible in medial view; (5) measurements on dorsal skull. Abbreviations (1–4): a = angular; adf = adductor mandibular fossa; ap = anterior palatal depression; ar = articular; beo = basi-exoccipital; c1–3 = coronoids 1–3; cb1–4 = ceratobranchials 1–4; ch = choana; chy = ceratohyal; ec = ectopterygoid; f = frontal; ipf = interpremaxillar fontanel; ipv = interpterygoid vacuity; j = jugal; j.e = jugal eminence; la = lacrimal; LEE = lateral exposed ectopterygoid; LEP = lateral exposed palatine; m = maxilla; md = mandible; mf = Meckelian fenestra; n = nasal; n.o = narial opening; op = opisthotic plate; ot.n = otic notch; p = parietal; pa = prearticular; p.c = cultriform process of parasphenoid; pl = palatine; pm = premaxilla; po = postorbital; pop = prootic-opisthotic plate; pp = postparietal; ppc = palpebral cup; ppl = palatal plates; prf = prefrontal; prsp = presplenial; ps = parasphenoid; psp = postsplenial; pt = pterygoid; ptf = postfrontal; q = quadrate; qj = quadratojugal; sa = surangular; sm = septomaxilla; sq = squamosal; st = supratemporal; stf = subtemporal fenestra; stp = stapes; sy = symphyseal region; t = tabular; v = vomer. Abbreviations (5): aSw = anterior skull width at level of maxilla-premaxilla sutures; Hl = postorbital midline skull length from level of posterior margins of orbits; Hw = postorbital skull width between lateral margins of supratemporals; INw = minimum internarial width; IOw = minimum interorbital width; mSw = midlength skull width at midlength level of orbits; Occ-Q = length between levels of occipital midline margin and posterior quadrate margin; ON-O = length between levels of anterior otic notch margin and posterior orbital margin; Ol = maximum length of orbit; POl = preorbital midline skull length from level of anterior margins of orbits; Pol = maximum posterior length of postorbital from posteriormost extent of orbit; pSw = maximum posterior skull width at level of posterolateral margins of cheeks; Sl = midline skull length; Thl = length of tabular horn between levels of posterior tabular corner and occipital midline margin; Ww = maximum transverse width of cheek from lateral margin of supratemporal anterior to otic notch.

Etymology
Dedicated to Jean-Marc Pouillon, ex-COGEMA (COmpagnie GEnérale des MAtières Nucléaires) geologist, for his great contribution to the knowledge of the Carboniferous and Permian of France.
Remarks
None.
Discussion
Phylogenetic analyses
Whereas analysis 1b recovered Buxierophus n. gen. as an olsoniform (Fig. 11.2), the much better-resolved topologies recovered by analyses 2 and 3 both recovered Buxierophus n. gen. as a dissorophid (Fig. 12). The outgroup consists of Dendrysekos and Eryops megacephalus Cope, Reference Cope1878. Most analyses recovered only relatively resolved topologies, similar to Gee’s (Reference Gee2021) results. This may be due to in part to the high degree of polymorphism included in this character–taxon matrix. Only analyses 2 and 3 are discussed here as they provide the most useful information to assess the position of Buxierophus n. gen. in relation to the Dissorophidae sub-families Dissorophinae and Cacopinae Schoch and Sues, Reference Schoch and Sues2013. Further comments on analyses 1a and 1b (Fig. 11) can be found in the Supplementary Information.
Phylogenetic position of Buxierophus n. gen. in comparison to a reduced dataset compared to Gee (Reference Gee2021). All taxa with less than 25% of scored characters were removed from the matrix of Gee (Reference Gee2021), as well as specimen level-OTUs and several non-dissorophids. (1) Analysis 1a with the exclusion of Buxierophus n. gen. in order to assess the topology recovered by this reduced taxon sampling. (2) Analysis 1b with the inclusion of Buxierophus n. gen. See Appendix 3 for discussion on both analyses. Node labels: Bremer value (when > 1), with ‘X’ showing constrained node.

Phylogenetic position of Buxierophus n. gen. in two different variants. (1) Analysis 2 with the exclusion of the wildcard taxa Brevidorsum and Reiszerpeton, but not Conjunctio and Scapanops. (2) Analysis 3 employs a similar taxon sample to Analysis 2, but with the exclusion of the wildcard taxa Conjunctio and Scapanops. Node labels: Bremer value (when > 1), with ‘X’ showing constrained node.

Analysis 2 (Fig. 12.1) keeps the wildcards Conjunctio and Scapanops because they are often compared with Buxierophus n. gen. in our description. Analysis 2 recovered 194 most parsimonious trees (MPT) of 362 steps. The strict consensus tree of this analysis is characterized by: [TL] = 381, [CI] = 0.4619, and [RI] = 0.5255. Analysis 2 recovered the clades Dissorophoidea (with its basal Micromelerpeton credneri Bulman and Whittard, Reference Bulman and Whittard1926), Xerodromes, and Olsoniformes Anderson et al., Reference Anderson, Reisz, Scott, Fröbisch and Sumida2008a, with the inclusion of Palodromeus Schoch et al., Reference Schoch, Henrici and Hook2021, as in Schoch and Sues (Reference Schoch and Sues2022). Among Olsoniformes, Trematopidae Williston, Reference Williston1910a, Cacopinae, and Dissorophinae are recovered. Cacopinae + Dissorophinae form a polytomy with the two wild cards Scapanops and Conjunctio, and with Aspidosaurus and Buxierophus n. gen. We did not recover a monophyletic Dissorophidae because Platyhystrix, Palodromeus, and Trematopidae were recovered in polytomy with other dissorphids.
The position of Buxierophus n. gen. among Olsoniformes (sensu Schoch and Milner, Reference Schoch and Milner2014) is supported by seven unambiguous synapomorphies in Analysis 2 (listed in Appendix 2). The position among Dissorophidae (sensu Schoch and Milner, Reference Schoch and Milner2014) is supported by five unambiguous synapomorphies, including two previously proposed by Schoch and Milner (Reference Schoch and Milner2014; see characters 66 and 72, Supplement for more characters): parasphenoid plate without denticles; basipterygoid region sutured. Buxierophus n. gen. is recovered in a polytomy with Dissorophinae, Cacopinae, as well as Scapanops, Conjunctio, and Aspidosaurus binasser. Scapanops and Conjunctio are here recovered outside Eucacopinae (sensu Schoch and Milner, Reference Schoch and Milner2014) as well, in agreement with Dilkes (Reference Dilkes2020), but contrary to the results of Schoch and Sues (Reference Schoch and Sues2013) and most analyses of Gee (Reference Gee2021). Buxierophus n. gen. shares few unambiguous synapomorphies with Dissorophinae (only 3, see Appendix 3, including a skull roof with elevated eminences on the nasal, frontal, parietal, postfrontal, and jugal, previously proposed by Schoch and Milner, Reference Schoch and Milner2014) and none with Cacopinae (see Appendix 3, however most of the characters recovered as unambiguous synapomorphies for Cacopinae were non-coded for Buxierophus n. gen.).
Analysis 3 (Fig. 12.2), which excluded the wildcard taxa Conjunctio and Scapanops, recovered eight most parsimonious trees (MPT) of 341 steps. The strict consensus tree of this analysis is characterized by: [TL] = 359, [CI] = 0.4763, and [RI] = 0.5358. This analysis recovered Buxierophus n. gen. as the first-diverging dissorophid. The position of Buxierophus n. gen. among Dissorophidae is here supported by seven unambiguous synapomorphies, while its basal position is supported by eight unambiguous synapomorphies (listed in Appendix 2). However, the Bremer support values are low, indicating some degree of lability. Interestingly, Analysis 3 recovered a parasphenoid plate without denticles (character 66: state 1) and a sutured basipterygoid region (72:1) as synapomorphies of Dissorophidae, as proposed by Schoch and Milner (Reference Schoch and Milner2014), but a short postorbital narrowing posteriorly (66:1) is here recovered as a synapomorphy of all dissorophids except Buxierophus n. gen.
To sum up, our phylogenetic analyses indicate Buxierophus n. gen. is a non-cacopine and non-dissorophine dissorophid. The mosaic of plesiomorphic and apomorphic characters recovered for Buxierophus n. gen. (see diagnosis) makes this new genus unique within Dissorophidae.
European occurrences
Until now, the Dissorophidae have been represented in Western and Central Europe by only few questionable vertebrae. According to Schoch and Milner (Reference Schoch and Milner2014, p. 79) “Gaudry (Reference Gaudry1879, Reference Gaudry1883) described aspidosaurine vertebrae from the Autunian of France.” A bibliographic search in Gaudry’s literature (e.g., Gaudry, Reference Gaudry1883) suggests that Schoch and Milner probably confused ‘aspidosaurine’ vertebrae with those of the eryopoid “Euchirosaurus” (i.e., adult Onchiodon/Actinodon frossardi Gaudry, Reference Gaudry1866, Werneburg and Steyer, Reference Werneburg and Steyer1999), which also shows long and vertical extensions of the neurapophyses.
Another vertebra with a wide, expanded dorsal part of the neural spine was found in the marine Kupferschiefer (Lopingian, Upper Permian) of the Richelsdorf Mountains in Hesse, Germany (Witzmann, Reference Witzmann2005). Recently, similar neural spines were described in the stereospondylomorphs Korkonterpeton kalnense Werneburg et al., Reference Werneburg, Štamberg and Steyer2020 (fig. 11) and Memonomenos amelangi Werneburg and Schoch, Reference Werneburg and Schoch2024 (fig. 3b), suggesting that the vertebra from Richelsdorf does not necessarily have to belong to a dissorophid, it can also belong to a stereospondylomorph.
The large skulls of Kamacops acervalis, Iratusaurus vorax Gubin, Reference Gubin1980, and Zygosaurus lucius Eichwald, Reference Eichwald1848, as well as a single osteoderm of ‘Alegeinosaurus’ sp. (Gubin, Reference Gubin1993) represent the dissorophids of Eastern Europe. However, Buxierophus pouilloni n. gen. n. sp. represents the only Lower Permian dissorophid from Europe.
Paleoecology
The lifestyle of Buxierophus n. gen. is difficult to interpret. Its relatively large and heavy skull, its pectoral girdle like in Dissorophus and dorsal shield, and its well-ossified skeletal elements suggest a terrestrial mode of life according to previous experience, as interpreted for most of the dissorophids (e.g., DeMar, Reference DeMar1968). But this well-ossified skeleton would certainly also be advantageous for locomotion in shallow nearshore waters.
However, Buxierophus n. gen. retains a complete, ossified ceratobranchial skeleton (Fig. 10.2). One very interesting fact here is that the ceratobranchials possess a deep groove according to Figure 5. This indicates that Buxierophus n. gen. had fish-like internal gills in the adult stage (sensu Schoch and Witzmann, Reference Schoch and Witzmann2011, “Bystrow’s paradox”). Ventrally grooved ceratobranchials occur in most dvinosaurs, plagiosaurids, and at least some brachyopids, in the stem-metoposaurid Callistomordax (Witzmann, Reference Witzmann2013). A complete, ossified ceratobranchial skeleton has been found in the aquatic eryopid Glaukerpeton (Werneburg and Berman, Reference Werneburg and Berman2012). For a long time, eryopids were only considered to be terrestrially adapted. Now we have a similar case with the dissorophids. The mixture of clear aquatic and possible terrestrial adaptations of Buxierophus pouilloni n. gen. n. sp. attest to its semi-aquatic lifestyle.
Unfortunately, the paleoenvironment of Buxières-les-Mines, which is supposed to have been a relatively deep paleolake (e.g., Steyer et al., Reference Steyer, Escuillié, Pouillon, Broutin and Debriette2000a), cannot help to better understand the paleoecology of Buxierophus n. gen. because this locality yielded various taxa, whether aquatic (e.g., actinopterygians), amphibious (e.g., erypoids), or terrestrial (e.g., blattoid insect).
Conclusions
The new dissorophid specimen Buxierophus pouilloni n. gen. n. sp. found in the Lower Permian bituminous claystone of Buxières-les-Mines, a fossiliferous locality of the Bourbon-l’Archambault Basin (Allier) in France, allowed for the following conclusions regarding its phylogeny, evolution, and paleoecology. (1) Buxierophus pouilloni n. gen. n. sp. clearly belongs to the family Dissorophidae with the synapomorphic dorsal osteoderms and several characters unambiguous to the Dissorophoidea (e.g., the narrow anterior jugal). (2) Five autapomorphies distinguish Buxierophus pouilloni n. gen. n. sp. from all other dissorophids: dorsal osteoderms composed of two series of thin and smooth osteoderms, some bearing conspicuous peaks dorsally; internal osteoderms with bi- or multi-lobed dorsal articulation surfaces; anterior neural arches of the same sagittal length than that of the osteoderms; anterior trunk ribs with widened distal ends. Nineteen synapomorphies complete the diagnosis of the new species. (3) A phylogenetic analysis places the non-cacopine and non-dissorophine Buxierophus pouilloni n. gen. n. sp. at the base of the Dissorophidae. (4) The paleoecological placement of Buxierophus pouilloni n. gen. n. sp. in the Lower Permian landscape of the Bourbon-l’Archambault Basin is surprising. It may have been terrestrial as in all other dissorophids, for example according to its lightly built pectoral girdle, like in Dissorophus. Otherwise, it retained an ossified ceratobranchial skeleton with grooved ceratobranchials, which indicate that Buxierophus n. gen. had fish-like internal gills in adult stage. These semi-aquatic adaptations speak for a truly amphibious way of life for Buxierophus pouilloni n. gen. n. sp., living around and in the relatively deep and large Buxières paleolake. This would be an almost unique characteristic among the otherwise terrestrially adapted members of the family Dissorophidae. (5) Buxierophus pouilloni n. gen. n. sp. represents the only Lower Permian dissorophid from Europe.
Acknowledgments
The authors thank J. Rival (ex. RH) and G. Sommer (NHMS) for the fine preparation of the studied specimen, and J.-M. Pouillon (RH) who allowed us to study it. We would especially like to thank V. Buffa (Paris) for his help in editing the manuscript. We also acknowledge all the members of the Rhinopolis systematic excavations of Buxières-les-Mines who worked hard splitting the bituminous shale slabs permanently from 1995 to 2001. We also thank the Municipality of Buxières-les-Mines and Pierre Debriette (HBCM, Charbonnages de France) who also allow work on these rocks. RW was supported by grants We 2833/2-1 and We 2883/3-1 from the Deutsche Forschungsgemeinschaft (DFG). AL was supported by the Humboldt Research Track Scholarship predoctoral grant from the Humboldt Universität Berlin and the IPV (Interface pour le Vivant) doctoral grant from Sorbonne Université Paris. JSS was supported by regular annual credits attributed to the MESR to his lab. We thank Florian Witzmann and Bryan Gee for their helpfully constructive reviews.
Competing interests
The authors declare that they have no competing interests.
Data availability statement
Data available from the Dryad Digital Repository: https://doi.org/10.5061/dryad.z612jm6pf.