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Chondrichthyans are one of the most threatened marine taxa worldwide. This is also the case in the Mediterranean Sea, which is considered an extinction hotspot for rays and sharks. The central position of the Italian peninsula makes it an ideal location for studying the status and changes of this sea. There is a lack of biological, ecological and historical data when assessing shark populations, which is also highlighted in the Red List of Threatened Species compiled by the International Union for the Conservation of Nature (IUCN). Historical data can provide important information to better understand how chondrichthyan populations have changed over time. This study aims to provide a clearer understanding of the changes in distribution and abundance of eight shark species in the Italian seas that are currently classified as at risk of extinction by the IUCN. In this respect, a bibliographic review was conducted on items from the 19th century to the first half of the 20th century, focusing on the selected species. The results show that all sharks were considered common until the beginning of the 20th century but have declined since, with a clear negative trend, mainly in the past 70 years. The strong local decline has been attributed to overexploitation, bycatch, habitat loss, depletion of prey items and environmental pollution. Furthermore, historical data also allow us to avoid the issue of a &lsquo, shifting baseline&rsquo, in which contemporary abundances are assumed to be &ldquo, normal&rdquo, Using historical data to further our knowledge of the marine environment is becoming increasingly common, and is fundamental in understanding human impact and evaluating mitigation measures to manage and conserve marine species and environments.

The locality of Pietraroia (Lower Albian, southern Apennines, Italy) has provided two fully articulated crocodylomorphs, exposed in ventral and in dorsal aspect, which are described here as representing a new species of a new genus, Pietraroiasuchus ormezzanoi gen. nov, sp. nov. The new taxon is found to be the sister taxon of Pachycheilosuchus trinquei from the Albian of the Glen Rose Formation, Texas. Pietraroiasuchus ormezzanoi resolves the phylogenetic position of the controversial P. trinquei, and is crucial in enabling an extensive understanding of the family Hylaeochampsidae. Phylogenetic analysis places Hylaeochampsa vectiana as a sister group of Iharkutosuchus makadii plus Pachycheilosuchus and Pietraroiasuchus. The phylogenetic result reveals the presence of an evolutionary mosaicism within non-crocodylian eusuchians. Mosaic features in Pietraroiasuchus are denoted by the combination of primitive character states, such as the position of the choana with its anterior margin formed by an inverted V-shaped palatine processeses, and the presumed presence of a tiny antorbital fossa, in conjunction with derived states involving the slight vertebral procoelia, the presence of tetraserial segmented dermal armour with an accessory lateral row, and isolated nuchal osteoderms. The disjoint occurrence between Pachycheilosuchus and Pietraroiasuchus species suggests that Pietraroia was a refuge island inhabited by endemic forms. © 2011 The Linnean Society of London, Zoological Journal of the Linnean Society, 2011, 163, S199–S227.

The Lower Cretaceous Pietraroia Plattenkalk is a fossiliferous, fine-grained cherty limestone from the Matese Mountains – Southern Apennines, Italy. The deposits are well known for the exceptional state of vertebrate fossil preservation. First considered as shallow lagoonal deposits or as intra-platform basin-fill, the Pietraroia Plattenkalk sequences are here interpreted as abandon deposits of a submarine channel (Pietraroia Channel) documenting a major transgressive event. Transgression was associated with the development of suboxic to anoxic conditions at the seafloor which favoured the preservation of fossils, as well as the deposition of coprolith-rich and bituminous layers. A peculiar paleogeographic and paleotopographic setting, which was strongly controlled by local tectonic, experienced the contiguity of wide emerged areas with a relatively deep-water channelised area where fossiliferous Plattenkalk sequences were deposited.

The Lower Cretaceous Pietraroia Plattenkalk (Benevento Province, southern Italy) has been known since the eighteenth century for its beautifully preserved fossil fishes. During Albian time (about 113 Myr ago1), deposition of fine marly limestone in a shallow lagoonal environment, affected by cyclic periods of low oxygen levels2, led to exceptional preservation of soft tissue in a juvenile theropod. The specimen, diagnosed here as Scipionyx samniticus gen. et sp. nov., is the first dinosaur ever to be found in Italy. The fossil has been mentioned previously in two brief notes3,4 and generally examined in a doctoral thesis5. Here we report the full preparation of the specimen which shows details of soft anatomy never seen previously in any dinosaur. The preservation is better than in other lagerstatten (conservative deposits)6 where theropod soft tissue has been reported, such as the Santana Formation of Brazil7 and the Yixian Formation of China8. Despite this, there is no evidence of feathers or any other integumentary remnants in the Italian specimen. Scipionyx represents a new maniraptoriform theropod. Its discovery is remarkable considering also the scarcity of juvenile theropod dinosaurs in the fossil record.

Ultraviolet light analysis of a fossil of the theropod dinosaurScipionyx samniticusrevealed that the liver subdivided the visceral cavity into distinct anterior pleuropericardial and posterior abdominal regions. In addition,Scipionyxapparently had diaphragmatic musculature and a dorsally attached posterior colon. These features provide evidence that diaphragm-assisted lung ventilation was present in theropods and that these dinosaurs may have used a pattern of exercise physiology unlike that in any group of living tetrapods.

This chapter presents an overview of evidence of predator-prey relationships in pterosaurs, with a focus on the Cretaceous (Santana Formation) pterosaurs from Chapado do Araripe, northeastern Brazil. The examples from the fossil record of pterosaurs as prey is scanty; the situation of pterosaurs as predators is not much better. However, especially for pterosaurs as predator, secondary evidence provides much insight in the life of these extinct predators. Here, we present a simple geometric model that proves the suggested way of predations of the toothed and crested taxa of the Anhangueridae.