Candela et al.—Paleobiology of the basal hydrochoerine Cardiomys
to that of Hydrochoerus, being wider and relatively shorter than that of caviines, dolichotines, and Dasyprocta (Figs. 3.4, 3.6, 4.1). The preserved portion of the cuboid indicates that, as in
other cavioids, the dorsal face of this bone is smaller than the ectocuneiform (Fig. 3.2). The calcaneo-cuboid facet of the cuboid is also similar to that of other cavioids. The plantar process of this bone is robust (Fig. 3.5), similar to that of Hydrochoerus (Fig. 3.4) and caviines but somewhat more robust than that of Dolichotis (Fig. 3.6). The ectocuneiform shows the typical plantar extension
observed in other cavioids. Its dorsal surface has a subrectan- gular outline, being relatively proximodistally longer than that of Hydrochoerus but shorter than that of Dolichotis (Fig. 3.1–3.3). The third metatarsal (Fig. 3.2) is relatively more gracile and
elongated than that of Hydrochoerus (Fig. 3.1) and Cuniculus but more robust than that of Dolichotis (Fig. 3.3), Cavia Pallas, 1766, and Galea Meyen, 1833 (Fig. 4.2). The preserved proximal portions of the second and fourth
metatarsals (Fig. 3.2) are morphologically similar but slenderer than those of Hydrochoerus (Fig. 3.1). The proximal and middle phalanges of the third digit and the middle phalanx of the forth digit are slenderer than those of Hydrochoerus and morpholo- gically similar to those of Caviodon.
Materials.—MLP 29-IX-3-19, right M3, distal ends of both humeri, proximal portions of both ulnae, right radius without its distal end, proximal portion of the left radius, left pisiform, proximal end of the left fourth metacarpal, portion of the left ischium, distal end of the right fibula, right calcaneus and partially preserved right navicular, right ectocuneiform, poorly preserved right cuboid, right Mt III, proximal portions of right Mt II and Mt IV, right proximal and middle phalanges of the third digit and middle phalanx of the fourth digit of the pes.
Remarks.—Specimen MLP 29-IX-3-19 is referred to Cardi- omys because its M3 has four prisms, which are relatively anteroposteriorly wider and present relatively more superficial labial flexi (= sulci) than those of Caviodon and Xenocardia species (Pascual et al., 1966; Vucetich et al., 2010; Vucetich et al., 2011). Therefore, we excluded assignment to Caviodon australis Ameghino, 1888 (Montehermosan, early Pliocene; Rovereto, 1914) and Caviodon pozzi Kraglievich, 1927 (Cha- padmalalan, late Pliocene) as both species have M3 with more prisms and much more penetrating fissures. Xenocardia (Chas-
icoan?) was also eliminated as it also has more penetrating labial flexi and more delicate prisms (Vucetich et al., 2010). Specimen MLP 29-IX-3-19 also differs from the type of Procardiomys martinoi Pascual, 1961 because the latter has an M3 with three lobes and a well-developed posterior projection (Pérez et al., 2014). The M3 of the type of Cardiomys ameghinorum Rover- eto, 1914 has four prims and one posterior projection (a fifth
Figure 2.
915
small lobe) that is well differentiated from the last prism by a lingual flexus. Specimen MLP 29-IX-3-19 differs from the type of this species because the fourth prism of M3 is narrower than the third and the posterior projection is continuous with the fourth prism. The M3 of the specimen MLP 29-IX-3-19 is very similar in size and general morphology (number and relative size of prisms, depth of labial flexi) to that of the type of Cardiomys leufuensis, but differs from it in the morphology of the second prism, which has two labial flexi in MLP 29-IX-3-19 and a straight labial side in C. leufuensis (Pérez et al., 2017a, fig. 6F). Besides this difference, all other shared features support the specific assignment of the MLP 29-IX-3-19 to C. leufuensis.
Discussion
Systematic considerations on the postcranial features.—The phylogeny of Cavioidea has been based on molecular, cranial, and dental data while postcranial features have not been analyzed from a systematic point of view. Our study indicates that many postcranial features of Cardiomys are shared with other analyzed cavioids (proximal portion of radius cranially located with respect to the ulna, olecranon fossa perforated, distal articular humeral surface relatively high, radial head lateromedially extended and posteriorly flattened, distal portion of calcaneus extended, dorsal face of cuboid smaller than that of ectocuneiform). Character mapping (Fig. 5) indicates that the extreme reduction of the lateral coronoid process of the ulna (character state 31), presence of a greatly differentiated capitular tail of the humerus (character state 52), shortening of the Mt III (character 1), and shortening of the plantar process of the navicular (character 2) would be potential synapomorphies of Hydrochoerinae, in the context of Cavioidea. Thus, these characters support Cardiomys as within Hydrochoerinae, in agreement with phylogenetic hypothesis based on other morphological characters. Optimization of robustness of Mt III (character 1) shows that dolichotines have a more slender Mt III than the remaining cavioids, whereas the Hydrochoerinae dis- play the most robust Mt III in the context of this group. Within the Hydrochoerinae, Mt III of Cardiomys is less robust than that of Hydrochoerus, closer to the ancestral condition of this clade. In the phylogenetic context of cavioids, the well-differentiated and craniodistally narrow capitular tail facet of the radius (character state 62) is a feature only present in Cardiomys and Hydrochoerus. However, ambiguous optimization of this feature at the node of the clade that contains Dolichotinae and Hydrochoerinae precludes us from inferring whether this feature could be a potential synapomorphy of Hydrochoerinae. Chasicoan hydrochoerines have been recognized as critical to understanding the early evolution of the group because they display dental features that anticipate the derived dentition of modern capybaras (Pérez et al., 2014). In agreement with this, some postcranial features of Cardiomys seem to be more generalized than those of modern capybaras (relatively more
(1–3) Cranial view of right humeri. (4–6) Proximal and cranial views of right radii. (7–9) Cranial and lateral views of left ulnae. (1, 4, 7)
Hydrochoerus hydrochaeris (MPS-Z 142); (2, 5, 8) Cardiomys leufuensis (MLP 29-IX-3-19); (3, 6, 9) Dolichotis patagonum (MLP 249). Views 1, 3, and 4 are mirrored. c=capitulum; ce=capitular eminence; ct=capitular tail; ctf=capitular tail facet; en=entepicondyle; f=fovea; lcp=lateral coronoid process; mcp=medial coronoid process; o=olecranon; rn=radial notch; t=trochlea; tf=trochlear facet; tn=trochlear notch. Scale bars=10mm.
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