Pebanista is an extinct genus of platanistid "river dolphin" that lived during the Early to Middle Miocene in Peru. As a member of the Platanistidae, Pebanista is most closely related to the extant Ganges and Indus river dolphins (Platanista) of South Asia and shares no close relation to the modern Amazon river dolphin (Inia geoffrensis) that inhabits the same region today. Like its close relatives, Pebanista possesses enlarged crests that would have covered the melon in life, possibly helping to focus their biosonar while hunting in murky waters. Pebanista further stands out as being the largest "river dolphin" yet discovered, reaching lengths between 2.8–3.47 m (9 ft 2 in – 11 ft 5 in) at minimum, much larger than the biggest recorded freshwater cetaceans of today. Given its relatively robust if elongated snout, it is thought that Pebanista was an active predator, profiting from the rich prey selection available to it in the enormous Pebas wetlands that covered South America during the early parts of the Miocene. Only a single species of Pebanista is known so far: P. yacuruna.
History and naming Pebanista was described based on MUSM 4017, a nearly complete skull recovered from the early to middle Miocene strata of the Pebas Formation in Peru. More specifically, the fossil was discovered in 2018 in the banks of the Rio Napo in the province of Loreto in sediments that indicate that it dates to the latest Early Miocene. The specimen is currently housed at the Museo de Historia Natural de la Universidad Nacional Mayor de San Marcos. The team that described Pebanista, headed by Aldo Benites-Palomino, also highlight two additional fossils that may be referrable to this genus or a related form. Namely MUSM 3593, a fragment of a snout tentatively referred to as cf. Pebanista, and MUSM 4759, a tympanic bulla only identified as Platanistidae indet. While the latter also stems from the Pebas Formation, the former was discovered in strata of the Ipururo Formation. The name Pebanista is composed of Pebas, in reference to the name of the formation and ancient wetland system that this animal once inhabited, and the genus name of the modern South Asian river dolphins Platanista. The name was specifically chosen to reflect both the close relationship between Pebanista and Platanista as well as its specific geographic origin, highlighting the great distance between the two taxa. The species name meanwhile derives from the yacuruna, mythical water beings of the Quechua people of the Peruvian Amazon.
Description
The snout or rostrum of Pebanista; formed chiefly by the bones of the premaxillae, maxillae and vomers; is elongated (longirostrine) and flattened top to bottom (dorsoventrally). In this regard the taxon bears close resemblance to other extinct platanistid dolphins like Prepomatodelphis, Pomatodelphis and Zarhachis, whereas the rostrum of extant Platanista has flattened sides (transverse compression). Additionally, the rostrum of Pebanista doesn't simply lack transverse compression, but actually shows a much greater transverse robustness than any other platanistid. Several tooth sockets are preserved in the holotype specimen, indicating that the animal had proportionally larger teeth than its relatives. Possibly the most distinct trait of the two extant Platanista species are the enlarged supraorbital crests, thin and pneumatic structures that encase large parts of the melon, a key organ used by toothed whales to echolocate. A similar crest can be found in Pebanista, showing the same transverse flattening of the bony plates that sets them apart from more basal forms such as Pomatodelphis and Zarhachis. At the same time, the crests of Pebanista are more robust than what is seen in Platanista, somewhat like an intermediate between it and the marine forms. Another major difference lies in the structural origins of the crests. In Pebanista the supraorbital crests are formed by the frontal bones, while in Platanista it is the maxillae that form these structures. Pomatodelphis and Zarhachis meanwhile show a mix between the two conditions, with both the frontals and the maxillae participating in forming the crests. The dorsomedial margin of the crests, the upper edges that faces inward towards the midline of the skull, show several prominent open spaces referred to as vacuities or cavities. Benites-Palomino and colleagues hypothesize that these cavities may have been an early stage in the development of fully excavated supraorbital crests as seen in today's Platanista species. The supraorbital crests arch over the medial part of the skull and form the lateral border to the circumnarial basin, with the back of said basin being restricted by the nuchal crest. This gives the back of the skull a more rectangular appearance. The circumnarial basin is a large depression in the upper surface of the skull that surrounds the bony nares, which in Pebanista are shifted towards the left side, contributing to the asymmetry among the facial bones. This is regarded a notable feature that helps identify Pebanista as a platanistid. This asymmetry is not simply limited to the nares either. The highest point of the skull, the vertex is shifted towards the left as well, as are the premaxillae and several facial bones. Only a single orbit is preserved in the holotype, however, based on this it appears to have been proportionally shorter, which is only shared by species of Platanista and not seen in other members of the family. The ventral surface of the skull prominently displays the pterygoid bones, which obscure the vast majority of the palatines sans narrow regions exposed towards the side of the skull. The temporal fossae, which stretch across the lateral surface of the skull on either side, are noted to be longer than they are high and extend so far back that they enter the occipital region. Vice versa, the occipital shield might project slightly forward into the anterior parts of the skull, however, it is likewise possible that this condition was simply caused by the skull being distorted during preservation.
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