Abstract Fishermen-hunter-gatherers of sambaquis (Brazilian shell mounds) had an intimate affinity with marine-coastal environments, where they exploited a great variety of fish and mollusks that comprise the best documented fauna from sambaquis. However, other groups of animals as mammals, birds, reptiles, and amphibians are also present in these sites, but are relatively less studied. This paper is the first one focused exclusively on the Tetrapoda biodiversity of sambaquis and aimed to identify tetrapods of ten sites from southern Brazil. We present a faunal inventory and data regarding animal capture and environmental exploitation. We identified the specimens anatomically and taxonomically, analyzed them concerning fragmentation, and quantified the data for the number of identified specimens (NISP) and minimum number of individuals (MNI). Despite the high degree of fragmentation of remains, we identified 46 taxa. As expected, most were from marine animals: cetaceans (total NISP = 2,568 and MNI = 27), otariids (total NISP = 248 and MNI = 32), and seabirds (total NISP = 65 and MNI = 23), indicating great relevance of marine tetrapod fauna as a resource for sambaqui builders (79.39% of NISP). We thus document the close bond between fishermen-hunter-gatherers of sambaquis and the marine tetrapods in southern Brazil. Fishermenhuntergatherers Fishermen hunter gatherers Brazilian mounds marinecoastal coastal environments However mammals birds reptiles studied Brazil exploitation taxonomically (NISP MNI. . (MNI) remains 4 taxa expected total 2568 2 568 2,56 27, 27 , 27) 24 32, 32 32) 6 23, 23 23) 79.39% 7939 79 39 (79.39 NISP. NISP) fishermenhuntergatherers fishermen (MNI 256 56 2,5 3 79.39 793 7 (79.3 25 5 2, 79.3 (79. 79. (79 (7 (

Abstract: Pterosaurs possess skeletal pneumatization, which can be assessed externally through the observation of pneumatic foramina. These foramina vary in position, shape, and number among taxa. Here we propose new characters referring to the position and number of pneumatic foramina present in cervical and dorsal vertebrae of pterosaurs. A cladistic analysis was performed after first-hand study of material in collections and using data from the literature in order to test these new characters for homology, and they were subsequently mapped in a strict consensus tree. The analysis resulted in nine equally parsimonious trees with 215 steps each. The strict consensus tree obtained does not present significant differences in relation to trees obtained in previous studies. The mapping performed identified that most pneumatic foramina evolved independently in several lineages, and only two of the eight added characters appeared once in the evolution of pterosaurs. In general, pneumatic foramina were more common in the Dsungaripteroidea, however, the flattened preservation of non-pterodactyloids and in the Archaeopterodactyloidea often precludes their visualization, and therefore the presence of vertebral pneumatization may be broaden with the discovery of new, better preserved specimens.

Abstract Fossil vertebrates from Antarctica are considerably rare, hampering our understanding of the evolutionary history of the biota from that continent. For several austral summers, the PALEOANTAR project has been carrying out fieldwork in the Antarctic Peninsula in search for fossils, particularly Cretaceous vertebrates. Among the specimens recovered so far are two bones referable to Pterosauria, more specifically to the Pterodacyloidea, the first volant reptiles from Antarctica to be fully described. MN 7800-V (part and counterpart) was recovered from a moraine at the Abernathy Flats (Santa Marta Formation, Lachman Crags Member, Santonian-Campanian) on James Ross Island. It is interpreted as the distal articulation of a first phalanx of the wing finger, representing an animal with an estimated wingspan between 3 and 4 m. The second specimen (MN 7801-V) comes from Vega Island (Snow Hill Island Formation, Maastrichtian) and is identified as a wing metacarpal IV of an animal with an estimated wingspan from 4 to 5 m. These occurrences show that pterodactyloids inhabited the Antarctic Peninsula at least during the Upper Cretaceous and demonstrate that large pterosaurs were widespread through all parts of the planet during that period.

A contraparte de um espécime anteriormente descrito, contendo uma fêmea de pterossauro não-pterodactiloide com um ovo, revela a existência de um segundo ovo, este situado dentro da cavidade corporal desta fêmea prenhe. O exemplar demonstra claramente que os pterossauros possuíam dois ovidutos funcionais, e evidencia que a redução de um oviduto não foi um pré-requisito para o desenvolvimento do voo ativo pelo menos neste grupo. A análise da composição de um dos ovos sugere a ausência de uma camada externa formada por carbonato de cálcio. Seções histológicas de um fêmur não registram osso medular e demonstram que este pterossauro atingiu maturidade reprodutiva antes da maturidade óssea. O presente estudo evidencia que os pterossauros punham ovos de tamanho ainda menor do que se supunha e que desenvolveram uma estratégia reprodutiva mais similar a dos répteis basais do que a das aves. Se pterossauros eram altamente precociais ou necessitavam de cuidado parental ainda está aberto à discussão.

The counterpart of a previously described non-pterodactyloid pterosaur with an egg revealed the presence of a second egg inside the body cavity of this gravid female. It clearly shows that pterosaurs had two functional oviducts and demonstrates that the reduction of one oviduct was not a prerequisite for developing powered flight, at least in this group. Compositional analysis of one egg suggests the lack of a hard external layer of calcium carbonate. Histological sections of one femur lack medullary bone and further demonstrate that this pterosaur reached reproductive maturity before skeletal maturity. This study shows that pterosaurs laid eggs even smaller than previously thought and had a reproductive strategy more similar to basal reptiles than to birds. Whether pterosaurs were highly precocial or needed parental care is still open to debate.

Um grande pterossauro (MN 6594-V) da Formação Romualdo (Aptiano/Albiano), Grupo Santana, Bacia do Araripe, é descrito. O espécime é referido a Tropeognathus cf. T. mesembrinus principalmente pela crista frontoparietal baixa e obtusa, por um número comparativamente baixo de dentes e pela inclinação da porção dorsal da região occipital. Duas distintas medidas de envergadura para pterossauros são introduzidas: a envergadura maximizada (maxws), que consiste essencialmente no dobro da soma de todos os elementos da asa e o comprimento da escápula ou do coracóide (o menor de ambos), e a envergadura normal (nws), que aplica um fator de redução (rdc) à envergadura maximizada para compensar as curvaturas naturais da asa. Para pteranodontóides o rfc sugerido é de 5%. No caso de MN 6594-V, maxws e nws correspondem a 8,70 m e 8,26 m, respectivamente, o que faz deste espécime o maior pterossauro coletado do Gondwana até hoje. A extremidade distal de um úmero de maior tamanho (MCT 1838-R) e uma asa parcial (MPSC R 1395) também são aqui descritos, mostrando que pterossauros grandes ou gigantescos formaram uma parcela significativa da fauna de pterossauros da Formação Romualdo. Finalmente, alguns comentários sobre a estabilidade nomenclatural para os depósitos de Santana são feitos.

A very large pterosaur (MN 6594-V) from the Romualdo Formation (Aptian/Albian), Santana Group, Araripe Basin, is described. The specimen is referred to Tropeognathus cf. T. mesembrinus mainly due to the presence of a low and blunt frontoparietal crest, the comparatively low number of teeth and the inclined dorsal part of the occipital region. Two distinct wingspan measurements for pterosaurs are introduced: the maximized wingspan (maxws), which essentially consists of doubling the addition of all wing elements and the length of the scapula or the coracoid (the smaller of the two), and the normal wingspan (nws), which applies a reducing factor (rfc) to the maximized wingspan to account for the natural flexures of the wing. The rfc suggested for pteranodontoids is 5%. In the case of MN 6594-V, the maxws and nws are 8.70 m and 8.26 m, respectively, making it the largest pterosaur recovered from Gondwana so far. The distal end of a larger humerus (MCT 1838-R) and a partial wing (MPSC R 1395) are also described showing that large to giant flying reptiles formed a significant part of the pterosaur fauna from the Romualdo Formation. Lastly, some comments on the nomenclatural stability of the Santana deposits are presented.

Répteis voadores da Austrália são muito raros e, na maioria dos casos, representados por ossos isolados procedentes da Formação Toolebuc (Cretáceo, Albiano), da região leste de Queensland. Entre os primeiros espécimes de pterossauros coletados nestes depósitos encontra-se uma sínfise mandibular que alguns autores acreditaram possuir afinidades com formas encontradas no Cambridge Greensand (Cenomaniano) da Inglaterra. O exemplar acabou sendo classificado como representando uma espécie pertencente ou proximamente relacionada aos gêneros Ornithocheirus, Lonchodectes ou Anhanguera. Neste trabalho nós redescrevemos este espécime e demonstramos que o mesmo não pode ser referido aos gêneros mencionados, mas representa uma nova espécie de Pteranodontóide (sensu Kellner 2003), aqui denominada de Aussiedraco molnari gen. et sp. nov. Este exemplar constitui a segunda espécie de pterossauro da Austrália a ser denominada e confirma a que os depósitos de Toolebuc são até o momento os mais importantes para a pesquisa de pterossauros desse país.

Flying reptiles from Australia are very rare, represented mostly by isolated bones coming from the Early Cretaceous (Albian) Toolebuc Formation, which crops out in western Queensland. Among the first pterosaur specimens discovered from this deposit is a mandibular symphysis that some authors thought to have a particular affinity to species found in the Cambridge Greensand (Cenomanian) of England. It was further referred as a member of or closely related to one of the genera Ornithocheirus, Lonchodectes or Anhanguera. Here we redescribe this specimen, showing that it cannot be referred to the aforementioned genera, but represents a new species of Pteranodontoid (sensu Kellner 2003), here named Aussiedraco molnari gen. et sp. nov. It is the second named pterosaur from Australia and confirms that the Toolebuc deposits are so far the most important for our understanding of the flying reptile fauna of this country.

Dois novos pterossauros de cauda longa procedentes de Linglongta, Jianchang County da região oeste de Liaoning, China, são descritos e referidos ao clado Wukongopteridae. Kunpengopterus sinensis gen. et sp. nov. difere dos demais integrantes desse clado basicamente pela região mais arredondada da parte posterior do crânio, pelo espesso processo lacrimal do jugal e pela ausência de uma crista óssea premaxilar. Esta espécie apresenta uma crista formada por tecido mole acima da região frontal e possui o dedo alar proporcionalmente maior do que nos demais wukongopterídeos. A segunda espécie é referida ao gênero Darwinopterus, D. linglongtaensis sp. nov., com base na região posterior do crânio. Difere dos deais pterossauros wukongopterídeos por possuir o processo lacrimal do jugal delgado, o forâmen no processo nasal arredondado e pela condição menos curvada da segunda falange do quinto dígito do pé. As principais diferenças entre os Wukongopteridae são encontradas na dentição e nos pés, o que sugere que estes ocupavam nichos ecológicos ligeiramente distintos. O pterossauro de cauda longa Changchen-gopterus pani também é tentativamente referido a esse clado. Novas diagnoses para os wukongopterídeos Wukongopterus lii e Darwinopterus modularis são apresentadas.

Two almost complete long-tailed pterosaurs from the Linglongta, Jianchang County, western Liaoning, China, are described and represent new taxa referred to the non-pterodactyloid clade Wukongopteridae. Kunpengopterus sinensis gen. et sp. nov. differs from other members of this clade mainly by the rounded posterior region of the skull, thick lacrimal process of the jugal and lack of a bony premaxillary crest. This species further shows a soft tissue crest above the frontal, a comparatively larger wing finger, and the proximal segment of the second pedal phalanx of the fifth toe shorter than in other wukongopterids. The second new species is referred to the genus Darwinopterus, D. linglongtaensis sp. nov. based on the posterior region of the skull. It further differs from other wukongopterid pterosaurs by the thin lacrimal process of the jugal, foramen on nasal process rounded, and by having the second pedal phalanx of the fifth toe less curved (115°). Several differences among the Wukongopteridae can be found in the dentition and the feet, suggesting that they might have occupied slightly different ecological niches. The long-tailed Changchengopterus pani is tentatively referred to this clade and new diagnosis for the wukongopterids Wukongopterus lii and Darwinopterus modularis is provided.