Hippopotamodon erymanthius (Pickford, 2015)

Pickford, M., 2016, Hippopotamodon erymanthius (Suidae, Mammalia) from Mahmutgazi, Denizli-Çal basin, Turkey, Fossil Imprint 72, pp. 183-201 : 186-191

publication ID

https://doi.org/ 10.5281/zenodo.1432664

DOI

https://doi.org/10.5281/zenodo.4415824

persistent identifier

https://treatment.plazi.org/id/03B7D02C-FFFE-FFD6-FF1F-A080FD121A0E

treatment provided by

Yanell

scientific name

Hippopotamodon erymanthius
status

 

Species Hippopotamodon erymanthius (ROTH et WAGNER, 1854)

Holotype. Lower jaw GoogleMaps illustrated by Roth and Wagner (1854: pl. 5, fig. 1). The whereabouts of the fossil are not known, although a cast is reported to be preserved in the NHMUK, London (Van der Made et al. 2013).

Type locality. Pikermi, Greece.

Diagnosis. Large species of Hippopotamodon in which the length of m/3 ranges between 40.5 and 51.6 mm, and M3/ from 38 to 44 mm. Tendency for P1/ and p/1 to be suppressed. Adult males have a prominent supra-canine flange with rugose lateral and dorsal surfaces.

Description

Skull

In the Karlsruhe collection of Hippopotamodon erymanthius from Mahmutgazi, there is a partial skull, and several mandible fragments, including parts of a juvenile maxilla and mandibles.

The most complete skull fragment in the sample is a right maxilla ( Text-figs 2 View Text-fig. 2 , 3 View Text-fig. 3 ) of a fully adult individual (M1/ deeply worn, M3/ in moderate wear) (SMNK Ma1 MP 8 GoogleMaps ). Almost none of the zygomatic or frontal bones is preserved. There is a large supra-canine flange above and behind the level of the canine, which has highly rugose lateral and dorsal surfaces, which indicate that the specimen is likely to represent a male individual. Dorsally, the rugose part of the canine flange is separated from the facial part of the maxilla by a deep, smooth, groove via which passed the tendons of the snout musculature. The area of the origins of the snout musculature are large, that for the levator rostri occupying a large area of the zygomatic process of the maxilla above the facial crest, beneath which is an extensive zone for the depressor rostri and dilatator nasalis lateralis musculature.

In ventral view, the front of the canine flange ends above the canine, and the rear edge terminates opposite the level of the P2/, forming a right angle with the facial process of the maxilla. There is an alveolar ridge in front of the P2/, which curves slightly laterally as it courses anteriorly, and in the preserved part there is no sign of a P1/ alveolus. The leading edge of the zygomatic arch flares laterally at an angle of about 45°, its anterior root being opposite the front of M2/ and the maxillary recess lying opposite the rear loph of the M3/. A small part of the anterior edge of the orbit is preserved above and well behind the level of the M3/.

Mandible

The lower jaw of Hippopotamodon erymanthius from Mahmutgazi (SMNK Ma1 Gips 6 GoogleMaps ) shows a long diastema between the canine and the p/2 occupied by a sharp alveolar ridge ( Text-fig. 4 View Text-fig. 4 ). There is no sign of the p/1 or of an alveolus for this tooth. There is a short gap between the i/3 and the canine. The rear of the symphysis extends as far back as the level of the front of p/2. The incisor battery is proclive and lies well beneath the occlusal surface of the cheek teeth. The lower canine is short and stubby, and projects laterally and anteriorly only slightly. The left mandible and symphysis from the site (SMNK Ma1 Gips 17 GoogleMaps ) shows essentially the same morphology as the previous specimen ( Text-fig. 5 View Text-fig. 5 ).

Deciduous teeth

There are two juvenile mandibles and a maxilla in the collection at Karlsruhe. Ma1 MP 5 GoogleMaps is a left maxilla containing D3/–D4/ and M1/ ( Text-fig. 6a View Text-fig. 6 ), and Ma1 Nr 196 GoogleMaps is a right mandible containing d/2–d/4, m/1 and a left mandible with d/4–m/1 ( Text-fig. 6b View Text-fig. 6 ).

In occlusal view, the outline of the D3/ is triangular with rounded corners, with a large mesial cusp and a pair of distal cusps forming the rear loph. There are weak mesial distal cingula, as well as small cingular tubercles on the inner face of the mesial cusp. The main cusps are indented by Fürchen.

The D4/ is tetracuspid, like the permanent molars, but the mesial pair of cusps is slightly narrower than the distal pair, which imparts a trapezoidal occlusal outline to the tooth. In the centre-line of the tooth there are small, low, anterior, median and posterior accessory cusplets. The mesial and distal cingula are well formed but do not extend onto the buccal or lingual surface. There is a low tubercle in the lingual end of the median transverse valley. The Fürchen pattern is like that in the permanent molars.

The d/2 is triangular in buccal view with the mesial and distal cusplets about half the height of the main cusp, and it is sectorial in occlusal view. It is narrower mesially than distally. The two roots are splayed apart anteriorly and posteriorly.

The d/3 is a larger version of the d/2.

The d/ 4 in contrast is molariform, with six cusplets arranged in three lophids, as is usual in artiodactyls. The root arrangement is the usual one found in suids, with splayed mesial and distal roots supporting the anterior and posterior lophids, and a single buccal root under the protoconid of the second lophid.

Permanent teeth

The upper right central incisor from Mahmutgazi (SMNK Ma1 Nr 176 GoogleMaps ) is unworn and shows a prominent cusplet on the lingual part of the tooth ( Text-fig. 7a View Text-fig. 7 ). This tubercle is an enlarged bead of the lingual cingulum. The cusplet is confluent with the rest of the lingual cingulum and walls off a capacious lingual fossa. The labial side of the crown is bulbous. There is a shallow slit apically, and the distal edge of the crown is beaded, markedly so near the cervix.

SMNK Ma1 MP 6, GoogleMaps is a worn right I3 / with a swollen lingual cingulum interrupted distally by a slit ( Text-fig. 7b View Text-fig. 7 ).

The upper premolars and molars of Hippopotamodon erymanthius were described by Pickford (2015). The Mahmutgazi specimens are typical of the species ( Text-fig. 8 View Text-fig. 8 ). Although the evidence is weak, the only available maxilla suggests that the P1/ was suppressed, which indicates a derived species of the genus. The P2/ has a diminutive disto-lingual tubercle, as in material from Pikermi. The P3/ GoogleMaps possesses a thick lingual cingulum, closing off a small mesial fovea, and a capacious distal lingual basin. The rear of the tooth is broad, due to the well-developed disto-lingual cusp. The P4/ GoogleMaps is tricuspid, with a pair of sagittal cusplets in the valley between the protocone on the one hand and the paracone-metacone on the other. The incision between the paracone and metacone is relatively shallow, and becomes obsolete in medium wear.

The upper third molars GoogleMaps from Mahmutgazi have a short lingually positioned talon ( Text-fig. 9a, b View Text-fig. 9 ), while the lower third molars GoogleMaps have a double-cusped talonid, with the lingual cuspid usually smaller and lower than the buccal one ( Text-fig. 9c, d, e View Text-fig. 9 ).

The central and second lower incisors GoogleMaps are extremely tall, and even the i/3 is elongated and barely separated from the canine ( Text-figs 10 View Text-fig. 10 , 11 View Text-fig. 11 ). The incisors GoogleMaps are arranged such that they comprise a continuous occlusal surface which wears almost flat. The canine GoogleMaps extends only slightly above this occlusal surface, and is functionally linked to the same dental battery.

The anterior lower premolars GoogleMaps are sectorial with the mesial and distal tubercles about half the height of the main cusp. The p/4 has a clear inner cusp and a large posterior cusplet ( Text-figs 12 View Text-fig. 12 , 13 View Text-fig. 13 ). The p/1 is absent in all three mandibles that preserve the requisite part of the jaw, which indicates a derived species of the genus ( Text-figs 4 View Text-fig. 4 , 5 View Text-fig. 5 ).

Post-cranial bones

The only suid post-cranial element in the Mahmutgazi collection in Karlsruhe is a proximal left radio-ulna ( Ma1 Gips 12 GoogleMaps ) ( Text-fig. 14 View Text-fig. 14 ). The radius is solidly fused to the ulna, even though the sutures between the bones are clearly visible.

The olecranon process is relatively short and medio-laterally robust (broken caudally). In the radius, the articular surface for the distal epiphysis of the humerus shows a broad medial basin, a relatively prominent central groove and a deep but small lateral basin. The articular part of the medial edge of the sigmoid notch in the ulna is expansive. The corresponding part on the lateral side is less expansive. The sigmoid notch extends over more than a semi-circle, all of which indicates an elbow in which joint movements were constrained to the para-sagittal plane.

Metric analysis of the teeth of Hippopotamodon erymanthius from Mahmutgazi, Turkey

The dimensions of the dental sample of Hippopotamodon from Mahmutgazi ( Tab. 2) are smaller than any of the specimens from Luberon, France, the type locality of Hippopotamodon major (basal MN 13), and are smaller on average than the mean of the Pikermi (MN 12) and Samos (MN 11 + MN 12 or MN 13) samples of Hippopotamodon erymanthius ( Text-fig. 15 View Text-fig. 15 ). They are similar to the collection from Akkaşdağı, Turkey, ( Text-fig. 16 View Text-fig. 16 ) correlated to MN 12 by Liu et al. (2005), and to the large sample from Maragheh (= Maragha) (Iran) correlated to MN 11 by Pickford (2015). Overall the Mahmutgazi specimens are similar in dimensions to the comprehensive sample from Dorn-Dürkheim 1, Germany (Van der Made 1997), which is correlated to MN 11, but are on average smaller than the material from Kalimantsi (Kotopoulos et al. 2001), although there is overlap in the ranges of variation of the fossils from the two localities.

Concerning Turkish samples of Microstonyx major (which according to Liu et al. (2005), includes Microstonyx erymanthius), the authors wrote that “we usually deal with faunal lists or fragmentary and isolated specimens which preclude a direct comparison with the Akkaşdağı form”. This concern can now be partly addressed (see measurements and descriptions of Turkish suids from many localities published by Pickford (2015)), and it is clear that the cranial and dental suid specimens from Akkaşdağı and Mahmutgazi are metrically closely similar to each other, suggesting similar chronological and/or palaeoecological contexts. The fact that both of these localities have yielded material that is on average smaller than the samples from Pikermi and Samos (Greece) suggests either that the latter two localities are not the same age as Mahmutgazi and Akkaşdağı, or that their palaeoenvironments may have differed, or that they comprise multiple levels (the case for Samos).

Specimens of Hippopotamodon erymanthius from Pikermi, Greece, in the SMNK

The SMNK possesses two dentognathic specimens (containing 12 teeth) of Hippopotamodon erymanthius from Pikermi, Greece ( Tab. 3 View Table 3 ). This sample augments the large amount of material that has been described from Pikermi (now standing at 358 teeth) ( Pickford 2015).

The snout ( SMNK MP3) is interesting, as it probably represents a young adult female individual, with no sign of a supra-canine flange, only a bowing out of the maxilla behind the level of the canine ( Text-fig. 17 View Text-fig. 17 ). The left and right I2 /s are in their crypts, but show the serrated postcrista typical of the genus, and the right P2/–M2/ are fully erupted. The only teeth showing light wear at the apices of the cusps are the M1/ and the P3/.

The P4/ shows well-formed sagittal cusplets attached to the buccal cusps and strong mesial and distal cingula ( Text-fig. 17b View Text-fig. 17 ).

The second specimen of Hippopotamodon erymanthius in the Karlsruhe collection is a left mandible fragment with moderately worn m/1–m/2 and the front lophid of m/3. Measurements of the teeth are provided below ( Tab. 3 View Table 3 ).

Sexual dimorphism in Hippopotamodon erymanthius

The fossil record of Hippopotamodon erymanthius is now comprehensive enough to indicate that the species was sexually dimorphic in the area of the upper canine. There seems to be no bimodality in dental dimensions, save for the fact that males seem to have a slightly larger upper canines than females. The incisors and cheek teeth appear to be metrically unimodal. This finding agrees with the discussion by Liu et al. (2005).

The most obvious sexual character is the supra-canine flange, which is large in males and is adorned with rugose lateral and dorsal surfaces, almost like the rugose surface of cauliflowers. Females show a bowing out of the maxilla behind the upper canine, but there is little or no development of a flange ( Liu et al. (2005) thought that females also have supra-canine flanges). In males, the supra-canine flange extends from above the canine backwards to the level of the P2/, corresponding to the diastema between the canine and P2/. In the Mahmutgazi specimen, the flange is 7 cm long and adds ca. 3 cm to the breadth of the snout on each side. The contrast between males and females is well shown in the Karlsruhe collection by a male specimen from Mahmutgazi and a female individual from Pikermi. The presence of a large supra-canine flange in males suggests that it served as a weapon during male-on-male combat, or perhaps for protection during such encounters. The canines in Hippopotamodon erymanthius are reduced in dimensions and probably played little if any role in intraspecific combat. The canine flanges in contrast are strong in males, and were probably covered in thick skin, perhaps with bristles emerging from them, in which case pushing, shoving and butting the opponent with the side of the snout was probably the main form of combat between males during the rutting period.

NHMUK

NHMUK

SMNK

Germany, Karlsruhe, Staatliches Museum fuer Naturkunde Karlsruhe

Kingdom

Animalia

Phylum

Chordata

Class

Mammalia

Order

Artiodactyla

Family

Suidae

Genus

Hippopotamodon

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF