Pedro Mocho

Estimating diversity patterns from the fossil record is essential for understanding the factors that shape biodiversity. The Jurassic/Cretaceous transition 143.1 million years (Ma) ago is a particular interval of pronounced ecological turnover accompanied by a global sharp diversity decline, disproportionately affecting larger and more specialised terrestrial taxa such as Sauropoda. Sauropods are a diverse group of large herbivorous dinosaurs, considered a good model for studying long-term biodiversity trends because of their prominent ecological roles and abundant fossil record. In this study, we analyse paleodiversity patterns for Diplodocoidea as a whole and for each of its subclades. Diplodocoidea is a subgroup of neosauropods that includes three main subclades: Dicraeosauridae, Diplodocidae, and Rebbachisauridae. The Flagellicaudata (= Dicraeosauridae + Diplodocidae) were notably affected by the Jurassic/Cretaceous faunal turnover, whereas Rebbachisauridae originated and persisted into the Early to mid-Cretaceous. Our key findings are: (1) high diversity during the Late Jurassic; (2) a sharp decline in diversity just before or during the Jurassic/Cretaceous transition; (3) a diversity peak in the Early Cretaceous Aptian stage; (4) overall higher Diplodocoidea diversity in the Early Cretaceous compared to the Late Jurassic; and (5) distinct geographic distributions, with Flagellicaudata restricted to high latitudes, while Rebbachisauridae occupied the full latitudinal range of Diplodocoidea. Our results suggest that the observed paleodiversity patterns were likely influenced by abiotic factors, and that Flagellicaudata and Rebbachisauridae may have been subject to distinct climatic constraints, potentially reflecting different ecological strategies. Additionally, this study underscores the impact of sampling biases on diversity estimates and challenges previous assumptions about sauropod diversity patterns, opening new directions for future research.

Para la conservación de los materiales paleontológicos es imprescindible disponer de forma ordenada toda la información que afecta a cada ejemplar y basándonos en la experiencia adquirida en la conservación de la colección de vertebrados del yacimiento del Cretácico Superior de Lo Hueco (Fuentes, Cuenca) se ha diseñado una base de datos orientada a la gestión. Para la toma de datos se ha considerado la información sobre la morfología y composición de los ejemplares y estado de conservación. Todos estos datos se han evaluado y baremado aunando en una misma herramienta la información valorada sobre el estado de conservación, la vulnerabilidad frente a agentes de deterioro y el valor científico, didáctico e histórico de los ejemplares, lo que facilita gestión de las colecciones. Esta información permite también establecer prioridades en las estrategias de conservación de la colección dirigidas a la jerarquización de sus necesidades.

A new lithostrotian titanosaur, Qunkasaura pintiquiniestra gen. et sp. nov., is described based on a single partial skeleton from the late Campanian-early Maastrichtian fossil-site of Lo Hueco (Cuenca, Spain). This new taxon is supported by an exclusive combination of characters that highlights strong convergences with members of the South American Aeolosaurini. Qunkasaura allows to reorganise the complex phylogenetic relationships of the increasingly diverse finicretaceous sauropods of Europe. Phylogenetic analyses places Qunkasaura within Saltasauridae and possibly Opisthocoelicaudiinae, together with Abditosaurus. A new clade is established, Lohuecosauria, including Saltasaurus, Lohuecotitan, their most recent common ancestor and all its descendants. Two distinct Ibero-Armorican Campanian-Maastrichtian saltasauroid lineages are recognised: (i) Lirainosaurinae that is exclusive from Europe, and (ii) a saltasaurid lineage with possible opisthocoelicaudiine affinities, with a Laurasian distribution. Lirainosaurinae was a relict lineage including possible dwarf forms that evolved in isolation after reaching Europe before the Late Cretaceous through the Apulian route. The occurrence of opisthocoelicaudiines in Europe may be the result of a Late Cretaceous interchange between Europe and Asia. No evidence of insular dwarfism is found in the Ibero-Armorican opisthocoelicaudiines suggesting that they may have been newcomers to the area that arrived before the ‘Maastrichtian Dinosaur Turnover’ in southwestern Europe.

The Upper Cretaceous sauropod record from Romania is abundant, but mainly composed by isolated and poorly preserved specimens. They were found in Maastrichtian units cropping out in both the western-southwestern margin of the Transylvanian Basin, and in the Hațeg and Rusca Montană basins. Two small-sized taxa, Magyorasaurus dacus and Paludititan nalatzensis, were considered as valid; however, the presence of other forms is not ruled out. An important sample of sauropod caudal vertebrae is described in detailed to provide new data about the diversity of the sauropods of the Hațeg Island during the Maastrichtian. Distinct morphologies are recognized for the caudal vertebrae, including four morphologies for the anterior-most elements; at least three for the anterior and middle ones, and at least two for the posterior caudals, including sauropods with opisthocoelous condition. The possibility of four different tail morphologies is suggested, which might belong to four different taxa, including Paludititan nalatzensis, Magyarosaurus dacus (the material previously referred to it seems to be composed by more than one taxon) and two other species. A new character for morphological datasets describing the position of the intraprezygapophyseal lamina in the middle and posterior caudals is proposed, which may be characteristic of some European taxa.

Sauropods were among the most diverse lineages of dinosaurs, with an ample geographic distribution throughout the Mesozoic. This evolutionary success is largely attributed to neck elongation and its impact on feeding efficiency. However, how neck elongation influenced exactly on feeding strategies is subject of debate. The process of mounting a nearly complete virtual skeleton of Spinophorosaurus nigerensis, from the Middle (?) Jurassic of Niger, has revealed several previously unknown osteological adaptations in this taxon. Wedged sacral and posterior dorsal vertebrae cause the presacral column to deflect antero-dorsally. This, together with elongated scapulae and humeri make the anterior region of the skeleton vertically lengthened. Also, elongated prezygapophyseal facets on the cervical vertebrae and a specialized first dorsal vertebra greatly increase the vertical range of motion of the neck. These characters support this early eusauropod as a more capable high browser than more basally branching sauropods. While limb proportions and zygapophyseal facets vary among Eusauropoda, the sacrum retained more than 10° of wedging in all Eusauropoda. This implied a functional constraint for sauropod species which evolved lower browsing feeding strategies: the antero-dorsal sloping caused by the sacrum had to be counteracted with further skeletal modifications, e.g. a ventrally curved mid to anterior presacral spine to hinder the dorsal slope of the whole presacral series caused by the wedged sacrum. This suggests that at least the last common ancestor of Eusauropoda developed high browsing capabilities, partially due to the modified wedged sacrum, likely a potential synapomorphy of the clade and key in the evolutionary history of the group.

The functional morphology of sauropod dinosaur long necks has been studied extensively, with virtual approaches yielding results that are difficult to obtain with actual fossils, due to their extreme fragility and size. However, analyses on virtual fossils have been questioned on several of their premises, such as the ability to accurately reconstruct intervertebral tissue with only skeletal data; or whether zygapophyseal overlap can be used to determine the limits of range of motion, since some extreme neck poses in extant giraffes have been claimed not to retain any zygapophyseal overlap. We compared articulation and range of motion in extant giraffes with the exceptionally well-preserved and complete basally branching eusauropod Spinophorosaurus nigerensis from the Middle (?) Jurassic of Niger, under the same virtual paleontology protocols. We examined the articulation and range of motion on grown and young specimens of both Spinophorosaurus and giraffes in order to record any potential changes during ontogeny. Also, the postures of virtual giraffes were compared with previously published data from living animals in the wild. Our analyses show that: (i) articulation of virtual bones in osteologically neutral pose (ONP) does enable accurate prediction of the amount of inter-vertebral space in giraffes and, roughly, in Spinophorosaurus; (ii) even the most extreme neck postures attained by living giraffes in the wild do not require to disarticulate cervical vertebrae; (iii) both living giraffes and Spinophorosaurus have large intervertebral spaces between their cervical centra in early ontogenetical stages, which decrease as ontogeny advances; and (iv) that grown specimens have a greater osteological range of motion in living giraffes and Spinophorosaurus.

Carcharodontosaurian allosauroids were temporally restricted to the Cretaceous, being known from all land masses with the exception of Antarctica. In addition to Veterupristisaurus from Tanzania, exceptions to this distribution have been reported recently, consisting on fragmentary materials from Upper Jurassic strata of China, Germany, and Portugal. Here, we propose a new Late Jurassic carcharodontosaurian taxon, Lusovenator santosi, gen. et sp. nov. based on the reevaluation of previously described specimens from the Lusitanian Basin, Portugal. The performed phylogenetic analysis recovered Lusovenator santosi as an early branching carcharodontosaurian allosauroid diagnosed by an exclusive combination of characters, including three autapomorphic features: (1) large recesses in neural arch of anterior dorsal vertebrae; (2) well-developed and continuous longitudinal laminae extending from the tip of the prezygapophyses to the distal end of the postzygapophyses in mid-caudal vertebrae; and (3) supraacetabular crest of ilium forming a prominent ventrolaterally projecting shelf. Lusovenator santosi is the oldest carcharodontosaurian allosauroid yet discovered from Laurasia and supports unequivocally the hypothesis of a pre-Cretaceous scenario for the radiation of the clade. The identification of this taxon highlights the high diversity of medium- to large-bodied theropods in the later part of the Late Jurassic of the Iberian Peninsula. Carcharodontosauria is not yet known in correlative levels of the North American Morrison Formation, and the existence of contacts after the late Tithonian between these landmasses could explain the distribution of this clade and other dinosaur groups present in the Iberian Jurassic and in the North American Lower Cretaceous.