Patagorhynchus pascuali Chimento &amp; Agnolín &amp; Manabe &amp; Tsuihiji &amp; Rich &amp; Vickers-Rich &amp; Novas 2023, sp. nov.
Creators: name: Chimento, Nicolás R.
name: Agnolín, Federico L.
name: Manabe, Makoto
name: Tsuihiji, Takanobu
name: Rich, Thomas H.
name: Vickers-Rich, Patricia
name: Novas, Fernando E.
Publisher: name: Zenodo
Year: 2023
Subjects: Biodiversity
Taxonomy
Animalia
Monotremata
Patagorhynchus
Patagorhynchus pascuali

description: <i>Patagorhynchus pascuali</i> sp. nov. (2023) 6:146 | https://doi.org/10.1038/s42003-023-04498-7 | www.nature.com/commsbio <b>Etymology</b>. Species name honors the Argentine paleomammalogist Rosendo Pascual (1923–2012), who described the first Cenozoic monotreme remains from Patagonia, thus demonstrating the presence of this clade outside Australia. <b>Holotype</b>. MPM-PV-23087, Museo Padre Molina (Rio Gallegos, Santa Cruz, Argentina), a right lower m2 attached to a fragment of dentary. Collected by N. R. Chimento during a joint ArgentineJapanese field trip in March 2022. <b>Diagnosis</b>. The same as for genus by monotypy. <b>Type locality and age</b>. La Anita farm, Santa Cruz Province, Patagonia, Argentina. The tooth was collected from the “Puma Cave” fossil site (S 50 30.639 W 72 33.617), Chorrillo Formation, early Maastrichtian7,8. This new discovery expands the list of Late Cretaceous mammaliaforms recorded in the Chorrillo Formation and equivalent Dorotea Formation in southern Chile, previously known to include gondwanatherians (<i>Magallanodon</i>) and dryolestoids (<i>Orretherium</i>)9–11,13. <b>Description</b>. Despite the occlusal surface being somewhat damaged, the morphology of the main cusps and anatomical details can be clearly discerned. The tooth is identified as a second lower molar based on the similarities with the m2 of <i>Obdurodon</i>, including a subrectangular-shaped outline in occlusal view, the presence of two lobes each bearing three cusps, a mid-valley lacking cusps, and prominent anterior and posterior cingulids (Fig. 1). Immediately anterior to m2, the fragmentary mandible shows a partially preserved and relatively small alveolus on the labial margin, which presumably corresponds to one of the roots of m1. The <i>Patagorhynchus</i> m2 exhibits a distinct morphology that easily identifies it as a monotreme. This includes a unique lophid and cusp structure resulting in the presence of two mesiodistally compressed lobes that are sub-equally in shaped and size each consisting of three cusps, twinned paraconid and metaconid, wrapping cingulid, hypsodont lobes, and un-basined talonid12,14,15. The m2 is 5.8 mm in mesiodistal length (see Supplementary Results 3), indicating that this tooth of <i>Patagorhynchus</i> was possibly intermediate in size between <i>Monotrematum</i> and some species of <i>Obdurodon</i>. The m2 is mesiodistally longer than transversely wide, and narrows mesially. Six large cusps are present: protoconid, paraconid, metaconid, hypoconid, hypoconulid, and NC1 (neomorphic cuspid 1)16. These cusps are relatively low and mound-like and connected by lophids, which form two main lobes or triakididrepanids (Fig. 1, Supplementary Fig. 2). The anterior lobe (equivalent to trigonid) is labiolingually narrower and apicobasally taller than the posterior lobe (equivalent to a talonid), a condition shared with <i>Obdurodon</i> 12. In <i>Patagorhynchus</i>, the anterior lobe is heart-shaped, with the anterior and posterior lophids being slightly convex posteriorly. This results in the paraconids being located anteriorly at the same level as the protoconid. In <i>Obdurodon</i>, by contrast, the anterior lophid is anteriorly convex and the posterior one is straight, resulting in metaconid and protoconid being located at the same level. In <i>Patagorhynchus</i>, the paraconid is larger than the metaconid, and its base is ventrally positioned relative to the base of both the metaconid and protoconid, suggesting that the paraconid was more ventrally located than the other cusps. The posterior (talonid) lobe is similar in shape to the anterior (trigonid) lobe, but much wider labiolingually. The lingual cusps are notably taller than the labial one (hypoconid). The preserved bases of the NC1 and hypoconulid are subequal in size and position. The hypoconid is mesiodistally narrower than the protoconid. Between the lingual cusps of paired lobes there is a narrow, eye-shaped enamel invagination, reminiscent of a flexid. Such a condition is also present in <i>Monotrematum</i> 17 and some specimens of <i>Obdurodon</i> 18. <i>Patagorhynchus</i> resembles <i>Monotrematum</i> in that the invaginations are delimited by a narrow enamel layer (Fig. 2, Supplementary Fig. 2), in contrast to <i>Obdurodon</i> in which the invaginations are labiolingually extended19. Both lobes are separated by a wide, deep mid-valley, which extends from the labial through the lingual edges of the tooth. The margins of the valley widen slightly towards the labial edge of the tooth. The valley lacks well-defined cusps or fossettes, and becomes deeper towards its labial margin. Posterior and anterior cingulids are prominent, being wider than those in <i>Teinolophos</i> but narrower than those in <i>Obdurodon</i> 16,20. The posterior cingulum is eroded on its lingual end, but the preserved segment maintains a constant width along its length, being similar in this morphology to that in <i>Obdurodon</i>. In contrast, the cingulids become lingually wider in <i>Teinolophos</i> 20. The anterior cingulid hosts a small cusp on its lingual end, whereas in the posterior cingulid the labial end shows a cusp (the lingual end of this cingulid is eroded, precluding the recognition of cusps), similar to the morphology in <i>Monotrematum</i>, but differing from that in <i>Obdurodon</i> (Fig. 2, Supplementary Fig. 2). The tooth bears two roots that are broad labiolingually and constricted at mid-height; they are obliquely oriented with respect to the main axis of the tooth. Regarding the root number, <i>Patagorhynchus</i> retains the ancestral condition in m2 shared with <i>Teinolophos</i> (and probably <i>Monotrematum</i>), differing from the multiple roots present in <i>Obdurodon</i> and <i>Ornithorhynchus</i> 16,20. Discussion As indicated above, the crown shape of <i>Patagorhynchus</i> unambiguously indicates that this taxon belongs to monotremes. With the aim to test the phylogenetic position of <i>Patagorhynchus</i>, we scored this tooth into a previously published data matrix composed by 558 characters and 128 taxa21 (see Supplementary Methods 1 and 2). We concentrated on the characters available in this new tooth, a total of 54 characters can be scored for <i>Patagorhynchus</i> (Supplementary Results 1 and 2). The results of the phylogenetic analysis consistently place <i>Patagorhynchus</i> as nested within monotremes, together with the genera <i>Ornithorhynchus, Tachyglossus, Monotrematum</i> and <i>Obdurodon</i> (Fig. 3, Supplementary Fig. 1). Australia has yielded the most complete fossil record of monotremes2, including an array of Barremian through Cenomanian taxa, as well as several species of the Oligocene-Pliocene monotreme <i>Obdurodon</i>. In this context, the presence of the toothed monotreme <i>Monotrematum</i> in the early Paleocene of Patagonia1,22 was interpreted as the result of a single dispersal of monotremes from Australia to South America, before or during the Late Cretaceous or early Paleocene2–6. Discovery of <i>Patagorhynchus</i> clearly demonstrates that the monotremes had already attained a wide paleogeographic distribution, stretching across southern South America, Australia, and Antarctica, the later one as a connecting pathway (but fossil monotremes are still unknown from this landmass), constituting a clade characteristic of the Weddelian Paleobiogeographical Province23–28. The new discovery expands the list of mammals documented in the Chorrillo and equivalent Dorotea formations of southern South America, adding the Monotremata to the assemblage of non-therian mammals (i.e., gondwanatherians and meridiolestidan dryolestoids9–11,13). Remarkably, monotremes are absent from the extensively sampled Late Cretaceous localities of northern and central Patagonia2,29,30. Such a difference among mammalian assemblages characteristic of Patagonia is consistent with the uneven distribution of non-avian dinosaurs in this region. For example, megaraptorid theropods, colossosaurian titanosaurs, and elasmarian iguanodontians are numerically dominant in the Chorrillo Formation8,31 whereas abelisaurid theropods and saltasaurine titanosaurs are prevalent in coeval units in northern Patagonia. Similar differences are documented in terrestrial and marine biotas between southern and northern Patagonia32–34. Thus, evidence at hand suggests that the Maastrichtian vertebrate fauna in southern Patagonia was different from that in northern Patagonia. It is noteworthy that the former had, instead, several taxa in common with Australia (<i>e.g</i>., Monotremata, Megaraptoridae). It is likely that a latitudinal zonation of environmental conditions (i.e., dry and warm in northern Patagonia versus humid and cold in southern Patagonia) controlled the distribution and partial abundance of the above-mentioned vertebrate clades. (2023) 6:146 | https://doi.org/10.1038/s42003-023-04498-7 | www.nature.com/commsbio The presence of monotremes in the southern La Anita fossil site (which occupied a paleolatitude of approximately 60° S during the Maastrichtian, roughly the same as that of southern Australia35) is congruent with the interpretation by Flannery et al.2 that monotremes evolved under humid, cool and densely forested environments in circumpolar Gondwana. Some authors already proposed that certain anatomical and physiological characteristics of living monotremes (e.g., low metabolism, a mechanoreceptive and electroreceptive beak for probe feeding, and relatively large body size) may have evolved in the context of polar environments2,18,36. The crown morphology of the only available molar of <i>Patagorhynchus</i> is closely similar to that of the Paleogene <i>Monotrematum</i> and the Neogene <i>Obdurodon</i>, revealing a highly conservative dental morphology for toothed monotremes15. Remarkably, this molar pattern underwent only minor changes for approximately 60 million years from the Late Cretaceous through to Miocene times. This duration of stasis in dental morphology considerably exceeds that seen in other mammalian groups (<i>e.g</i>., therians and dryolestoids37–40). The labiolingually broad segment of the molar of <i>Patagorhynchus</i> and the reduction in the number of teeth (eventually restricted to only two upper molars inferred for <i>Monotrematum</i> 2) may be congruent with the duck-billed morphology of the snout documented in more derived ornithorhynchids. In addition, the presence of a hypertrophied mandibular canal in <i>Teinolophos</i> suggests the development of electroreception occurred early in the evolutionary history of Monotremata and that the acquisition of a specialized duckbill for high-resolution aquatic electroreception is unique to the clade39. Based on such evidence, we hypothesize that a highly sensitive duck-billed snout is likely to have already been present in Late Cretaceous monotremes, such as <i>Patagorhynchus</i>. Apparently, a similar anatomical inference could be made for the rest of the body, as suggested by the morphology of the distal femur of <i>Monotrematum</i> 41 being almost identical to that of the living platypus. As in <i>Ornithorhynchus</i>, extinct monotremes may have had a sprawling posture of their hind limbs, and eventually adapted for swimming42. The possibility that <i>Patagorhynchus</i> had already acquired ecological and behavioral characteristics similar to those of the living platypus, which inhabits ponds and lakes, is congruent with sedimentological evidence suggesting that such environments were prevalent during deposition of the Chorrillo Formation7, as well as with occurrences of Nymphaeaceae aquatic plants, freshwater snails and abundant larvae of chironomid insects, with the latter two invertebrates constituting part of the food for the living platypuses8,36,43. Discovery of <i>Patagorhynchus</i> gives an insight into the degree of continuity between the terrestrial vertebrate faunas of western and eastern Gondwana during the Late Cretaceous, suggesting the lack of paleobiogeographic barriers to their dispersal prior to the deep-water opening of the Drake Passage and the Tasman Gateway. The diversification of monotremes towards the end of the Mesozoic suggested by the present discovery implies that an extensive and still unknown history of this clade of peculiar mammals awaits to be documented in Mesozoic beds in southern South America.
description: Published as part of <i>Chimento, Nicolás R., Agnolín, Federico L., Manabe, Makoto, Tsuihiji, Takanobu, Rich, Thomas H., Vickers-Rich, Patricia &amp; Novas, Fernando E., 2023, First monotreme from the Late Cretaceous of South America, pp. 1-6 in Communications Biology (146) (146) 6</i> on pages 2-4, DOI: 10.1038/s42003-023-04498-7, http://zenodo.org/record/7664992