TL;DR: Sonorasaurus is taxonomically valid, represents one of the geologically youngest brachiosaurid sauropods, and inhabited a harsh inland evergreen-dominated woodland environment that limited its growth as mentioned in this paper.
Abstract: Sauropod dinosaurs are rare in the Cretaceous North American fossil record in general and are absent from that record for most of the Late Cretaceous. Sonorasaurus thompsoni from the Turney Ranch Formation of the Bisbee Group of Arizona, USA, potentially represents one of the youngest sauropods before their ca. 30-million-year-long hiatus from the record. The anatomy of Sonorasaurus has only been briefly described, its taxonomic validity has been questioned, several hypotheses have been proposed regarding its phylogenetic relationships, and its life history, geologic age, and reported paleoenvironment are ambiguous.Herein we assess the systematics, paleoenvironment, life history, and geologic age of Sonorasaurus based on firsthand observation, bone histology, and fieldwork in the holotypic quarry and environs. The validity of S. thompsoni is substantiated by autapomorphies. Cladistic analysis firmly places it within the Brachiosauridae, in contrast to results of some recent analyses. Bone histology suggests that the only known exemplar of Sonorasaurus grew slowly and sporadically compared to other sauropods and was approaching its adult size. In contrast with previous assessments of a coastal/estuarine paleoenvironment for the Turney Ranch Formation, our sedimentological and plant macrofossil data indicate that Sonorasaurus lived in a semiarid, low relief evergreen woodland that received highly variable (perhaps seasonal) precipitation. We obtained detrital zircons from the holotypic quarry for U-Pb dating, which only yielded Barremian-aged and older grains, whereas other radiometric and biostratigraphic data suggest that the sediments at the quarry were deposited near the Albian-Cenomanian boundary.Sonorasaurus is taxonomically valid, represents one of the geologically youngest brachiosaurid sauropods, and inhabited a harsh inland evergreen-dominated woodland environment that limited its growth. A review of other Bisbee Group dinosaurs suggests that its fauna, although poorly sampled, exhibits broad similarity to those from coeval North American horizons, reinforcing the apparent faunal homogeneity at the time.
TL;DR: The specimen described herein shows some clear brachiosaurid homologies that are both distinctly different from Pleurocoelus and from brachesaurids phylogenetically closer to the type Upper Jurassic Brachiosaurus, and a new taxonomic designation at the genus level is warranted.
Abstract: Remains of a brachiosaurid sauropod, Sonorasaurus thompsoni, gen. et sp. nov. , are reported from the Turaey Ranch Formation of southeastern Arizona, U.S.A. Brachiosaurids are represented in the earliest Cretaceous, the Barremian of England, by Pleurocoelus valdensis (Marsh 1888) and Pleurocoelus nanus (Marsh 1888) and P. altus (Marsh 1888) of the United States. The specimen described herein shows some clear brachiosaurid homologies that are both distinctly different from Pleurocoelus and from brachiosaurids phylogenetically closer to the type Upper Jurassic Brachiosaurus. Radioisotopic, stratigraphic and fossil pollen analysis are in progress to more precisely corroborate the tentative 97.6 Ma age of the Bisbee Group's Turaey Ranch Formation so that we can place this brachiosaur in the context of environmental settings of the middle range of the Cretaceous. Defining characteristics for this new taxon are the slender, splayed fibula; tibia with broad proximal end and very wide, shallow proximal end; long and slender metacarpals; reduced claws on the tarsal phalanx I-I and II-I; dorsal vertebra much like those of brachiosaurs with curled postzygaphphysis, deep lateral pleurocoels; caudal vertebrae having posterior angling transverse process, simple neural spines and lacking pleurocoels. Because of its temporal and geographical isolation, and because the specimen does not favorably conform wilh specific skeletal structures of other known members of the Brachiosaurinae, the new taxonomic designation at the genus level is warranted.
TL;DR: In the Black Mesa basin of northeastern Arizona, late Cenomanian-middle Turonian records of vertebrate fossils are mostly of selachian teeth but include a few records of marine turtles, crocodilians, plesiosaurs and mosasaurs as mentioned in this paper.
Abstract: Fossil vertebrates of Cretaceous age are known from two principal areas in Arizona—the
Lower and Upper Cretaceous strata of the Basin and Range of southeastern Arizona and the Upper
Cretaceous strata of the Black Mesa Basin on the Colorado Plateau in northeastern Arizona. Cretaceous fossil vertebrates, especially dinosaurs, from southeastern Arizona can be summarized as encompassing largely isolated records, mostly from Lower Cretaceous strata, and a single diverse assemblage from one Upper Cretaceous collecting area. These fossils can be assigned to two temporal intervals: (1) Albian records from the upper part of the Bisbee Group in the Empire, Whetstone and Mule Mountains, including the ornithopod “Tenontosaurus” and the sauropod Sonorasaurus thompsoni Ratkevich; and (2)
Campanian records, including titanosaurs, hadrosaurs, ceratopsians, dromaeosaurs, and tyrannosaurs from the Fort Crittenden Formation in the Santa Rita Mountains, and the “Tucson Mountains dinosaur,” a hadrosaur from the Tucson Mountains. In the Black Mesa basin of northeastern Arizona, late Cenomanian- middle Turonian records of vertebrate fossils are mostly of selachian teeth but include a few records of marine turtles, crocodilians, plesiosaurs and mosasaurs.
TL;DR: Vouivria is a basal brachiosaurid, confirming its status as the stratigraphically oldest known titanosauriform, and implementation of sensitivity analyses, in which these characters are excluded, has no effect on tree topology or resolution.
Abstract: Brachiosauridae is a clade of titanosauriform sauropod dinosaurs that includes the well-known Late Jurassic taxa Brachiosaurus and Giraffatitan. However, there is disagreement over the brachiosaurid affinities of most other taxa, and little consensus regarding the clade's composition or inter-relationships. An unnamed partial sauropod skeleton was collected from middle-late Oxfordian (early Late Jurassic) deposits in Damparis, in the Jura department of eastern France, in 1934. Since its brief description in 1943, this specimen has been informally known in the literature as the 'Damparis sauropod' and 'French Bothriospondylus', and has been considered a brachiosaurid by most authors. If correctly identified, this would make the specimen the earliest known titanosauriform. Coupled with its relatively complete nature and the rarity of Oxfordian sauropod remains in general, this is an important specimen for understanding the early evolution of Titanosauriformes. Full preparation and description of this specimen, known from teeth, vertebrae and most of the appendicular skeleton of a single individual, recognises it as a distinct taxon: Vouivria damparisensis gen. et sp. nov. Phylogenetic analysis of a data matrix comprising 77 taxa (including all putative brachiosaurids) scored for 416 characters recovers a fairly well resolved Brachiosauridae. Vouivria is a basal brachiosaurid, confirming its status as the stratigraphically oldest known titanosauriform. Brachiosauridae consists of a paraphyletic array of Late Jurassic forms, with Europasaurus, Vouivria and Brachiosaurus recovered as successively more nested genera that lie outside of a clade comprising (Giraffatitan + Sonorasaurus) + (Lusotitan + (Cedarosaurus + Venenosaurus)). Abydosaurus forms an unresolved polytomy with the latter five taxa. The Early Cretaceous South American sauropod Padillasaurus was previously regarded as a brachiosaurid, but is here placed within Somphospondyli. A recent study contended that a number of characters used in a previous iteration of this data matrix are 'biologically related', and thus should be excluded from phylogenetic analysis. We demonstrate that almost all of these characters show variation between taxa, and implementation of sensitivity analyses, in which these characters are excluded, has no effect on tree topology or resolution. We argue that where there is morphological variation, this should be captured, rather than ignored. Unambiguous brachiosaurid remains are known only from the USA, western Europe and Africa, and the clade spanned the Late Jurassic through to the late Albian/early Cenomanian, with the last known occurrences all from the USA. Regardless of whether their absence from the Cretaceous of Europe, as well as other regions entirely, reflects regional extinctions and genuine absences, or sampling artefacts, brachiosaurids appear to have become globally extinct by the earliest Late Cretaceous.