Globally, non-hadrosauroid iguanodontians (‘basal iguanodontians’) reached their acme in terms of diversity during the Early Cretaceous. However, Gondwanan representatives of this clade are rare and are represented in Australia only by the enigmatic Muttaburrasaurus langdoni (upper Albian; Mackunda Formation). Here, we describe a new iguanodontian, Fostoria dhimbangunmal, gen. et sp. nov., from the Cenomanian Griman Creek Formation at Lightning Ridge, New South Wales, Australia. The holotype and referred specimens, preserved entirely in opal, pertain to at least four individuals from a monodominant bone bed excavated from an underground opal mine. This deposit constitutes the first ornithopod-dominated bone bed from Australia. Elements from most parts of the body are represented, including the first partial skull of a dinosaur recovered from New South Wales. The new taxon is identified by a number of autapomorphies that include, but are not restricted to, a stepped lateral margin of the frontal in dorsal view and a stout protuberance on the anterolateral corner of the frontal. Phylogenetic analysis based on a recently published data set recovers Fostoria as the sister taxon to a clade of Gondwanan iguanodontians that includes Anabisetia saldiviai, Talenkauen santacrucensis, and Muttaburrasaurus langdoni. The new taxon and M. langdoni represent the sole iguanodontians known from the eastern margin of the epeiric Eromanga Sea, whereas the group is conspicuously absent from the contemporaneous ornithopod-dominated ecosystems of the Australian-Antarctic rift valley in Victoria.

Kentriodontids are small- to medium-sized odontocetes with a wide geographic range that flourished during the Miocene. They are closely related to crown Delphinida. Seven fossil kentriodontid specimens have been recovered from the Haraichi Formation, Annaka Group (latest middle/earliest late Miocene, Serravallian/Tortonian), Gunma Prefecture, Japan. We describe and diagnose a new species of the genus Kentriodon. Kentriodon nakajimai, sp. nov., has a larger fossa for the hamular and preorbital lobes of the pterygoid sinuses, which suggests that the species was more highly adapted for diving than other Kentriodon species. Asymmetric development of left and right maxillary crests indicates asymmetric development of the facial muscles attached to the melon. If this is the case, it suggests that K. nakajimai possessed a more sophisticated echolocation system than other kentriodontids. Phylogenetic analysis suggests that K. nakajimai is most closely related to K. obscurus and the genus Kentriodon may have originated in the Pacific and then dispersed into the Atlantic several times.

We describe a new genus and species of Proterotheriinae from the Pleistocene of Uruguay. Several taxonomic, biostratigraphic, paleoecological, and paleoenvironmental analyses and interpretations have been performed in a detailed study of the Litopterna (Mammalia, ‘Meridiungulata’) of Uruguay. The Proterotheriidae is the most diverse family of the Litopterna. In Uruguay, the record of the Proterotheriidae, although in many cases fragmentary, includes interesting specimens in particular contexts and different ages in the late Oligocene–late Pleistocene. The aim of this work is to reassess the specimens primarily assigned four decades ago to ‘Licaphrium’ aff. floweri, redescribing them, evaluating their taxonomic status in the context of the Proterotheriidae, and establishing the characters that allow the determination of this taxon as a new genus and species of Proterotheriinae: Uruguayodon alius. We redescribe two specimens of this new taxon, which include dental and postcranial remains. The diagnostic element is the last lower molar, which shows, among other characters, paraconid and paralophid in a very lingual position, smoothed metaflexid, and absence of entoflexid. The individuals were excavated from a sandy level of the San José Member of the Raigón Formation, a unit that has an endemic fauna, a pattern discussed here in a paleogeographic framework. The provenance of the analyzed specimens from Pleistocene layers is indicated by mammalian content and absolute ages, which support the presence of another genus of Proterotheriidae surviving into the Quaternary, in addition to Neolicaphrium recens.

Animals with large differences in body size between adults and juveniles will often exhibit differences in behavior through ontogeny, and these behavioral differences can sometimes have direct effects on skeletal morphology. Scapula shape has been shown in several groups to be highly influenced by function and in some groups to be a good indicator of body size. Megalonyx and Paramylodon, two of the most common and widespread of the North American Plio-Pleistocene giant ground sloths, had overlapping temporal and geographic ranges. However, they have few co-occurrences in the fossil record. In this study, the scapulae of juvenile and adult Megalonyx jeffersonii and Paramylodon harlani were analyzed using geometric morphometrics and compared with those of the two genera of modern tree sloths, Bradypus and Choloepus. The ground sloths have significantly different scapula shapes from each other, as do the tree sloths. The scapula shapes between juveniles and adults of each genus are also significantly different from each other, with the scapulae of the juveniles of each species more circular in appearance than the more ovoid ones in adults. All four genera show significant allometry, but it is more apparent in adults than juveniles. However, there is no difference in nonallometric shape between adults and juveniles or between each pair of genera. The ground sloths exhibit similar changes in ontogeny to those observed in modern sloths, indicating that ground sloth juveniles may have engaged in similar behaviors to those of modern sloths, such as clinging to their mothers for transportation. Ground sloth juveniles also possess morphological traits that have been linked with semiarboreal behaviors.

Hyainailourine hyaenodonts are among the largest terrestrial carnivorous mammals known. The clade is widely dispersed, found in Eurasia, North America, and Afro-Arabia in the Paleogene and early Neogene. In this study, we describe dental and postcranial material from Simbakubwa kutokaafrika, gen. et sp. nov., the most complete hyainailourine known from sub-Saharan Africa. The material is from a relatively young adult from the early Miocene locality of Meswa Bridge, Kenya. Simbakubwa differs from Hyainailouros in exhibiting lingually oriented molar protocones, gracile metastyles, and buccolingually compressed, shearing canines. Like other large Miocene hyainailourines, Simbakubwa has deep carnassial notches on the molars and tall paracones fused to shorter metacones forming single piercing cusps. A Bayesian phylogenetic analysis recovers Simbakubwa as the sister taxon of a clade of large-bodied Miocene hyainailourines that includes Hyainailouros and Megistotherium. Bayesian ancestral state reconstruction supports an Afro-Arabian origin for Hyainailourinae with subsequent dispersal to Eurasia during the early Miocene. Regression analysis based on carnassial size is applied to Simbakubwa and closely related hyainailourines, recovering a body mass up to 1,500 kg for the new taxon. The evolution and extinction of Hyainailourinae offers important insights for interpreting ecological transitions from Paleogene to Neogene faunas in Afro-Arabia and Eurasia.

The near lack of vertebrate fossils from the Cenozoic of Madagascar has left many of the details regarding the origin and evolution of the island's extant faunas unknown. However, recent fossil discoveries from Madagascar's nearshore marine deposits have begun to elucidate this mystery. These finds include sharks, bony fish, turtles, crocodylians, a middle Eocene sirenian (Eotheroides lambondrano), and the island's first fossil dolphin. We report here at least three (possibly four) different early (or possibly later) Miocene dugongid sirenians recovered from the island of Nosy Makamby, Mahajanga Basin, northwestern Madagascar. These include (1) a fragmentary braincase originally attributed to the genus Halitherium but here reidentified as a previously named species known only from Libya (Rytiodus heali; Dugonginae); (2) a newly named genus and species (Norosiren zazavavindrano) interpreted as a primitive relative of Xenosiren (Dugonginae); (3) a probable dugongine not yet identified with any known species; and (4) a taxon reported here as Metaxytherium cf. krahuletzi (Halitheriinae), the first Neogene halitheriine credibly reported from the Indian Ocean basin. This pattern of shallow marine environments harboring multispecies sirenian paleofaunas is seen elsewhere in the world, and these three or four contemporaneous sirenians represent the first glimpse into Madagascar's sea cow diversity during the Miocene. This specific time period is a poorly known and critical interval for interpreting Madagascar's past, and these specimens are potentially highly significant for reconstructing sirenian evolutionary and biogeographic history. Surprisingly, this sirenian fauna, so far, shares no genera with the roughly contemporaneous and relatively nearby one from Kutch, western India.

A well-preserved braincase of the basal alligatoroid Diplocynodon tormis was found in the middle Eocene site of ‘Teso de la Flecha,’ Salamanca, Spain. The specimen was scanned using computed tomography (CT), and its inner cavities were digitally rendered in three dimensions. Most bones of the left side are missing, so the reconstruction was based mainly on the right half of the braincase. The endocast of the brain cavity, nerves, part of the inner ear, and blood vessel canals was reconstructed, as well as a complex network of air-filled cavities around the hindbrain formed by the median pharyngeal sinus and pharyngotympanic sinus systems. Inner cavities of the skull are considered to be conservative structures. The comparison of this specimen with several extant crocodilians (Alligatoroidea, Crocodyloidea, and Gavialoidea) allows us to identify a neuroanatomical evolutionary pattern that matches current phylogenetic hypotheses. All internal cavities of the braincase of Diplocynodon are similar to those of other studied eusuchians, with some noteworthy differences in shape and size, particularly regarding the cerebrum and the paratympanic sinus system. Diplocynodon tormis shows a combination of alligatoroid synapomorphies and crocodylian symplesiomorphies in its internal cavities, consistent with its phylogenetic placement as a basal alligatoroid.

Cretaceous fish fossils are reported from Malaysia for the first time. They were found with dinosaur and turtle remains in nonmarine sediments in the interior of Pahang State, Peninsular Malaysia. This fish assemblage consists mostly of isolated teeth, with minor amounts of noncranial remains, including vertebral centra, scales, coprolites, and hybodont fin spines. Over 100 fish teeth were examined. Nine taxa were confirmed from this fish assemblage: six (identified and unidentified) species of hybodont sharks, Heteroptychodus kokutensis, Isanodus paladeji, Lonchidion aff. khoratensis, Mukdahanodus aff. trisivakulii, Egertonodus sp., and Hybodontidae indet., and three species of actinopterygians (ray-finned fishes): ‘Lepidotes’ sp., Halecomorphi indet., and Ginglymodi indet. This fish assemblage has strong affinities with Early Cretaceous (Barremian–early Aptian) faunas of Thailand, because the four hybodont species, H. kokutensis, I. paladeji, L. khoratensis, and M. trisivakulii, were previously known only from the Sao Khua Formation (Khorat Group) and equivalent strata of Ko Kut (Kut Island). Egertonodus has been confirmed in Asia for the first time. Overall, this fish assemblage shows a close linkage to Early Cretaceous (Barremian–early Aptian) faunas of Thailand. Based on faunal composition and biostratigraphic correlation, we suggest a Barremian–early Aptian age for this new fauna from Malaysia.

The bristlebird family (Passeriformes, Dasyornithidae) constitutes one of the earliest branches in the oscine (songbird) tree. A new bristlebird, Dasyornis walterbolesi, sp. nov., is described from lower Miocene deposits of the Riversleigh World Heritage Area, Australia. This new species is based on a femur, a tibiotarsus, and a tarsometatarsus of one individual, the first known instance of associated passerine bones in the pre-Pleistocene record of Australia, as well as a distal part of a femur of a second individual. Dasyornis walterbolesi is smaller in size than the extant eastern bristlebird, D. brachypterus, and extends the known fossil record for Dasyornithidae by 18 million years. The new fossils considerably increase the geographic range of Dasyornithidae and indicate that the bristlebird family was once more widespread in Australia. A phylogenetic analysis of 91 morphological characters strongly supports the placement of the new fossil species in Dasyornithidae, although its intrafamilial relationships will only be better informed by discovery and study of additional material. Dasyornis walterbolesi meets five criteria for consideration as a well-justified fossil calibration and can be used to calibrate molecular estimates of the passerine evolutionary timescale.

Dugaldia emmilta is a teleostean fish found in the late Albian Toolebuc Formation in Queensland, Australia. In the original description, D. emmilta was attributed to the Neoteleostei because of the presence of a tripartite occipital condyle, and the species was postulated to have a basal position among neoteleosteans because of the presence of several plesiomorphic characters. A reexamination of the holotype, together with the description of two new specimens, indicates that D. emmilta is an ichthyodectiform fish. A phylogenetic analysis resolves this species as the sister to Ogunichthys + Ichthyodectoidei. This species shows unusual features for an ichthyodectiform, in particular the shape of the mandible and the arrangement of the teeth on the lower jaw. Jaw mechanics in ichthyodectiforms are peculiar because they allow a significant lateral enlargement. In Dugaldia, a similar disposition is present but is exaggerated by specific features of the maxilla and the mandible. Comparisons with the sarcastic fringehead (Neoclinus blanchardi), a living blenny that shows a ‘gaping display,’ reveal that Dugaldia was likely able to exhibit extreme lateral mouth enlargement.

Temnospondyls from the Middle–Late Triassic of Madagascar are problematic and scarce: ‘Metoposaurus hoffmani’ was erected on the basis of poor material, and this taxon has never been revised. Other remains were also reported and assigned to Temnospondyli indet., but they have never been described, nor figured. Here, we (re)describe in detail this historical material from the Folakara area of Madagascar (Isalo Group, Morondava Basin): the specimens include cranial and postcranial remains, most of them being referred to Metoposauridae indet. and a few to Stereospondyli indet. We also confirm that ‘M. hoffmani’ is a nomen dubium owing to the absence of any clear autapomorphy of the fragmentary type material. The material referred here to Metoposauridae indet. is incorporated in an updated paleobiogeographic analysis of the group: interestingly, it suggests a connection with Indian metoposaurids during the Late Triassic.

The presence of eagle rays of the genus Aetomylaeus in the Neogene of the Temperate Pacific coast of South America (TPSA) still is ambiguous, although the fossil record of elasmobranch fishes (sharks, rays, and skates) from this area is quite good. Here, we present the first unmistakable fossil remains of Aetomylaeus from the Neogene of the TPSA. The material comprises 13 dental plates from one site in Peru and six localities in Chile ranging in age from Miocene to Pliocene and was compared with dental plates of extant species. Our study reveals that the number of tooth rows and the shape of lateral teeth in extant species are seemingly very variable and need to be established before fossil specimens can be confidently identified. Consequently, we do not assign the fossil specimens from the Neogene of the TPSA to any species but leave them as Aetomylaeus. Moreover, we recognized that only the shape of medial teeth provides reliable diagnostic characters in our material, whereas the shape and number of lateral teeth are highly variable, similar to the condition seen in extant species.

The specimens described herein come from the Río Bote locality, Santa Cruz Formation (early Miocene), Santa Cruz Province, Argentina. They include the most complete cranial material of the ‘Notohippidae’ Notohippus toxodontoides and other remains that increase knowledge of the mandible and dentition. The new remains allow extension of the original description proposed by Ameghino in the 19th century and provide data on ontogenetic variation in the dental traits of this species. Notohippus differs from the Deseadan–Colhuehuapian genus Argyrohippus in the following features: discontinuous dentition; C and p1 absent; shorter P2–M3/p2–m3 series; crown of I1 highly curved; upper molars with less developed parastyle and paracone fold, less undulating ectoloph, deeper distolingual groove of M3 directed more lingually and presence of a very shallow distolabial groove; incisiform lower canine; and lower molars with posterolabial angle of talonid more rounded and narrower trigonid valley. As stated in previous works, our phylogenetic analysis indicates that the ‘Notohippidae’ do not constitute a monophyletic group, because Argyrohippus, Notohippus, and Toxodontidae are recovered as a clade. Internal relationships within this clade are not resolved in any of the phylogenetic analyses performed here. The presence of N. toxodontoides in the faunal assemblage found at the Río Bote locality adds to its previous records in Santa Cruz (Kar-Aiken and Cerro Centinela localities) Province, Argentina, and Sierra Baguales locality in Chile.

A new genus and species of plesiopedal mosasauroid, Portunatasaurus krambergeri, from the Cenomanian–Turonian (Late Cretaceous) of Croatia is described. An articulated skeleton, representing an animal roughly a meter long was found in 2008 on the island of Dugi Otok. The specimen is articulated, in approximate life position, and is well represented from the anterior cervical series to the pelvis. Preserved elements include cervical and dorsal vertebrae, rib fragments, pelvic fragments, and an exquisitely preserved right forelimb. The taxon possesses plesiomorphic characters such as terrestrial limbs and an elongate body similar to that of basal mosasauroids such as Aigialosaurus or Komensaurus, but also shares derived characteristics with mosasaurine mosasaurids such as Mosasaurus. The articulated hand exhibits a unique anatomy that appears to be transitional in form between the terrestrially capable aigialosaurs and fully aquatic mosasaurines, including 10 ossified carpal elements (as in aigialosaurs), intermediately reduced pro- and epipodials, and a broad, flattened first metacarpal (as in mosasaurines). The new and unique limb anatomy contributes to a revised scenario of mosasauroid paddle evolution, whereby the abbreviation of the forelimb and the hydrofoil shape of the paddle evolves either earlier in the mosasaur lineage than previously thought or more times than previously considered. The presence of this new genus, the third and geologically youngest species of aigialosaur from Croatia, suggests an unrealized diversity and ecological importance of this family within the shallow, Late Cretaceous Tethys Sea.

The Egerniinae (formerly the Egernia group) is a morphologically diverse clade of skinks comprising 61 extant species from eight genera, spread across Australia, New Guinea, and the Solomon Islands. The relatively large size and robustness of many egerniines has meant that they fossilize more readily than other Australian skinks and have been more frequently recorded from paleontological excavations. The Riversleigh World Heritage Area of northeastern Australia has yielded multiple egerniine fossils, but most are isolated jaw elements, and only one taxon (‘Tiliqua’ pusilla) has been formally described. Articulated remains recently recovered from the mid-Miocene AL90 site (14.8 Ma) at Riversleigh are here described as Egernia gillespieae and represent the first opportunity to describe the morphology of a significant portion of a single individual of a fossil member of the Egerniinae. We include this fossil and ‘T.’ pusilla in an integrated analysis of morphology and published molecular data to assess their relationships and to provide calibration points for the timing of the egerniine radiation. Our calibrated tree combining molecular and morphological data suggests that the modern Australian radiation dates to the end of the Eocene (34.1 Ma). Both fossils are within the Australian crown clade Egerniinae: Egernia gillespieae is placed close to species of the living genus Egernia, whereas ‘Tiliqua’ pusilla likely sits basal to the divergence of the clade inclusive of Tiliqua and Cyclodomorphus. The fossils thus provide direct evidence that the Australian radiation of the Egerniinae was well underway by the mid-Miocene.

A complete skull and well-preserved postcranium of a dvinosaurian temnospondyl from the Carboniferous-Permian boundary of Germany is referred to a new genus and species, Trypanognathus remigiusbergensis. The skull closely resembles that of the early Permian dvinosaurian genus Trimerorhachis in outline and suture topology, but the occiput and the palate differ substantially. Derived states are the penetration of vomerine tusks through the splenial and symphyseal tusks through the premaxilla. Trypanognathus shares with dvinosauroids the lack of a squamosal embayment, an elongated basipterygoid process, a foreshortened palatine ramus exclusively reaching the ectopterygoid, the absence of pterygoid denticles, and enlarged palatal tusks. The body is elongate with well-ossified, but small limbs, the presacral count is ca. 28, and the pleurocentra are large and reached ventrally almost as far as the intercentrum. The new taxon nests within Dvinosauria above the trimerorhachid clade and Erpetosaurus, at the base of the broad-skulled dvinosauroids. Trypanognathus occurs in a tetrapod fauna that closely resembles early Permian assemblages of western North America, with which it shares sphenacodontid and edaphosaurid synapsids, as well as eryopid temnospondyls.

Platypterygius sachicarum is one of the few Lower Cretaceous ichthyosaurian species described from the Hauterivian–Aptian-aged Paja Formation, the most complete Lower Cretaceous sedimentary sequence in northern South America. To date, P. sachicarum has been described only from a single skull, limiting morphological, stratigraphic, and phylogenetic comparisons. Here, we describe a new skull and associated postcranium of upper Barremian age from Villa de Leyva, Colombia, which represent the first documented postcranial remains of this species and enable detailed comparison with other Early Cretaceous ophthalmosaurid ichthyosaurs. Platypterygius sachicarum shares many morphological similarities with contemporaneous taxa from Europe but differs in both skull and tooth morphology from coeval South American species from northern South America and from the eastern Pacific. The additional data provide new diagnostic characters for this species and resolve the position of P. sachicarum as part of a polytomy of other species historically referred to Platypterygius. However, as with previous analyses, all recovered clades are poorly supported. The rich vertebrate fossil record of the Paja Formation provides an unparalleled opportunity to explore paleobiogeographic and paleoecological questions pertaining to Cretaceous marine reptiles; however, in most cases, a robust stratigraphic and phylogenetic framework remains elusive.

The Upper Jurassic of Portugal is relatively rich in sauropod remains. We describe a new sauropod specimen, which includes a partial tail, pectoral and pelvic girdle elements, and hind limb bones, from Praia de Valmitão (Praia da Amoreira-Porto Novo Formation, upper Kimmeridgian–lowermost Tithonian). This specimen constitutes the holotype of Oceanotitan dantasi, gen. et sp. nov., which shows a unique combination of characters, including the presence of anterior caudal vertebrae with a medial accessory articulation on the prezygapophysis; a circular, rough tuberosity on the medial surface of the scapula; an elliptical concavity on the ventral face of the scapula; an ischium that is shorter than the pubis; and a robust fourth trochanter located at the midline of the posterior face of the femur. Multiple phylogenetic analyses recover Oceanotitan dantasi within Titanosauriformes, with one resolving it at the base of Somphospondyli. This taxon shares several apomorphies with some Cretaceous somphospondylans and turiasaurs, such as the transverse furrow on the chevron articulations (shared with Tangvayosaurus and Phuwiangosaurus) and the ischium being shorter than the pubis (shared with Mierasaurus and somphospondylans). Oceanotitan might represent the oldest known somphospondylan, and its establishment increases the known diversity of the Late Jurassic–earliest Early Cretaceous sauropod fauna in the Iberian Peninsula, which also consists of turiasaurs, diplodocids and macronarians (non-camarasaurid, non-titanosauriform macronarians; camarasaurids; and brachiosaurids). This high diversity in sauropods suggests that this region might have played an important role during the Late Jurassic in the dispersal and diversification of several sauropod lineages between North America, Africa, and Europe, especially macronarians.