@article {ValerianJPJsus2025, title = {Late Triassic small and medium-sized vertebrates from the Fleming Fjord Group of the Jameson Land Basin, central East Greenland}, journal = {Palaentologia Electronica}, volume = {28}, year = {2025}, note = {

n/a

}, pages = {1}, abstract = {

The Late Triassic deposits in the Jameson Land Basin, central East Greenland, stand as a crucial fossil area, yielding a diverse Norian vertebrate fauna. This basin, situated at a palaeolatitude of 41{\textdegree} N on the northern rim of Pangea and bordered in the North by the Boreal Sea, was a hub of activity during the Late Triassic. A large ephemeral to perennial lake system developed in the central and eastern parts of the basin, with rivers transporting sediment from the uplands northwest of the basin. Our research focused on the microvertebrate remains recovered from an expedition to Jameson Land in 1991 which yielded significant findings. These specimens, meticulously photographed and listed in a catalogue, comprise 950 vertebrate remains. Notably, we have identified new taxa never described from the Late Triassic sediments of Greenland, including sharks (Lissodus, Rhomphaiodon), bony fish (Gyrolepis), and reptiles (Doswelliidae and Rhynchocephalia). The revision of two sphenodontians jaw fragments as Clevosauridae, in association with Lissodus lepagei, Lissodus cf. Lissodus minimus, Rhomphaiodon sp., Saurichthys sp., and Gyrolepis sp., which are taxa that are highly documented in Europe and Asia, confirms a relationship between faunas of Greenland and Eurasia during the Late Triassic, a statement previously based on macro vertebrate studies.

}, url = {https://doi.org/10.26879/1423}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/jesus_et_al_2025_greenland_triassic_1423.pdf}, author = {Valerian J. P. J{\'e}sus and Mateus,Oct{\'a}vio and Mil{\`a}n, Jesper and Clemmensen, Lars B.} } @article {martino_late_2023, title = {The Late Miocene hippopotamid, Archaeopotamus pantanellii nov. comb., from the Casino Basin (Tuscany, Italy): paleobiogeographic implications}, journal = {Historical Biology}, volume = {36}, year = {2024}, note = {

Publisher: Taylor \& Francis

}, pages = {891-904}, abstract = {

n/a

}, issn = {0891-2963}, doi = {10.1080/08912963.2023.2194912}, url = {https://www.tandfonline.com/doi/citedby/10.1080/08912963.2023.2194912}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/martino_et_al_2024_the_late_miocene_hippopotamid__archaeopotamus_pantanellii.pdf}, author = {Martino, R. and Rook, L. and O. Mateus and Pandolfi, L.} } @article {16611, title = {Luis Nabais Conde (1937-2023) in memoriam}, journal = {Tylostoma}, volume = {2}, year = {2023}, pages = {134-136}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_2023_paleo-obituarios_tylostoma_0.pdf}, author = {Mateus,Oct{\'a}vio} } @article {BELVEDERE2019103547, title = {Late Jurassic globetrotters compared: A closer look at large and giant theropod tracks of North Africa and Europe}, journal = {Journal of African Earth Sciences}, volume = {158}, year = {2019}, note = {

n/a

}, pages = {103547}, abstract = {

Late Jurassic theropod tracks are very common both in North Africa and Europe. Two recently described ichnotaxa Megalosauripus transjuranicus and Jurabrontes curtedulensis from the Kimmeridgian of Switzerland show the coexistence of two apex predators in the same palaeoenvironment. Similar tracks can be found in tracksites from the Iberian Peninsula and from Morocco. Here, we further explore the similarities among the Swiss ichnotaxa and the other tracks from Germany (Kimmeridgian), Spain (Tithonian-Berriasian), Portugal (Oxfordian-Tithonian) and Morocco (Kimmeridgian) through novel three-dimensional data comparisons. Specimens were grouped in two morphotypes: 1) large and gracile (30 \< Foot Length\<50 cm) and 2) giant and robust (FL \> 50 cm). The analyses show a great morphological overlap among these two morphotypes and the Swiss ichnotaxa (Megalosauripus transjuranicus and Jurabrontes curtedulensis, respectively), even despite the differences in sedimentary environment and age. This suggests a widespread occurrence of similar ichnotaxa along the western margin of Tethys during the Late Jurassic. The new data support the hypothesis of a Gondwana-Laurasia faunal exchange during the Middle or early Late Jurassic, and the presence of migratory routes around the Tethys.

}, keywords = {Digital ichnology, Ichnotaxonomy, Late Jurassic, Palaeobiogeography, theropod, Vertebrate tracks}, issn = {1464-343X}, doi = {https://doi.org/10.1016/j.jafrearsci.2019.103547}, url = {http://www.sciencedirect.com/science/article/pii/S1464343X19302006}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/belvedere_et_al_2019_jurassic_globetrotters_compared.pdf}, author = {Belvedere, Matteo and Diego Castanera and Christian A. Meyer and Marty, Daniel and Octavio Mateus and Bruno Camilo Silva and Vanda F. Santos and Alberto Cobos} } @inbook {11927, title = {Loul{\'e} h{\'a} mais de 220 Milh{\~o}es de anos: os vertebrados f{\'o}sseis do Algarve tri{\'a}sico}, booktitle = {Loul{\'e}: Territ{\'o}rios. Mem{\'o}rias. Identidades}, year = {2018}, pages = {651-659}, publisher = {Museu Nacional de Arqueologia | Imprensa Nacional}, organization = {Museu Nacional de Arqueologia | Imprensa Nacional}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_campos2018_algarve_triasico.pdf}, author = {O. Mateus and Campos, H.} } @article {Mateus_2017, title = {The Lourinh{\~a} Formation: the Upper Jurassic to lower most Cretaceous of the Lusitanian Basin, Portugal {\textendash} landscapes where dinosaurs walked}, journal = {Ci{\^e}ncias da Terra - Earth Sciences Journal}, volume = {19}, number = {1}, year = {2017}, note = {n/a}, month = {sep}, pages = {75{\textendash}97}, publisher = {{NOVA}.{ID}.{FCT}}, abstract = {n/a}, doi = {10.21695/cterra/esj.v19i1.355}, url = {https://doi.org/10.21695\%2Fcterra\%2Fesj.v19i1.355}, author = {O. Mateus and and J. Dinis and P P Cunha and and} } @article {11926, title = {Lourinh{\~a} Formation: Upper Jurassic to Lowermost Cretaceous of the Lusitanian Basin, Portugal - landscapes where dinosaurs walked}, journal = {Ci{\^e}ncias da Terra / Earth Sciences Journal}, volume = {19}, year = {2017}, pages = {75-97}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_et_al_2017_lourinha_formation.pdf}, author = {O. Mateus and Dinis, J. and P P Cunha} } @proceedings {9266, title = {Late Jurassic of Morrison Formation and Portugal tetrapods compared: a model to explain faunal exchange and similarity}, journal = {Annual Meeting of the Society of Vertebrate Paleontology}, year = {2016}, pages = {185}, publisher = {Journal of Vertebrate Paleontology, Program and Abstracts, 2016}, address = {Salt Late City}, abstract = {

The precursor of the North Atlantic existed between the North American and Iberian blocks from the earliest Jurassic Hettangian and has been ever expanding since. By the Kimmeridgian and Tithonian, when much of the Morrison Fm rocks were deposited, the proto-Atlantic was more than 300 km wide at 27{\textdegree} paleolatitude between North America and Iberia. Macrovertebrate paleontology reveals a unique story to the isolation of Iberia and instead suggest a paleogeographic land connection between North American and Iberia. Torvosaurus, Allosaurus, Ceratosaurus, Stegosaurus, Supersaurus and others have a distribution restricted to Morrison Formation in North America and Lourinh{\~a} Formation in Portugal. A novel paleogeographic model is here suggested: (1) around the Middle{\textendash}Late Jurassic transition there is a major palaeoceanographic and palaeoclimatic reorganization, coincidental to a major eustatic sea-level drop and uplift associated with the Callovian{\textendash} Oxfordian Atlantic Regressive Event; (2) creating an ephemeral land bridge presenting a temporary opportunity for terrestrial gateways likely across the Flemish Cap and Galician Bank land masses, allowing large dinosaurian taxa to cross the northern proto-Atlantic in both directions; (3) finally, a Callovian{\textendash}Oxfordian faunal exchange around the 163 Ma, through latest Kimmeridgian at 152 Ma (the age of equivalent genera in both Morrison and Portugal), is was an interval that allowed speciation, but retaining generic similarity of vertebrates. This model is consistent with the chronology and taxonomy required for speciation of the Iberian and American forms, exemplified by the coeval sister-taxa pairs Torvosaurus tanneri and T. gurneyi, Allosaurus fragilis and A. europaeus, or Supersaurus vivianae and S. lourinhanensis. While some of the smaller animals in the fauna show Morrison/Portugal affinities, most from Iberia have European or even Asian affinities. The larger-bodied fauna are more closely related to Morrison than to mainland Europe (except for dacentrurine stegosaurs). The body size differences and affinities of taxa across paleogeography is comparable to what is observed today across the Wallace Line. Migration may have also occurred in both directions. The closest relative of Torvosaurus is likely the European Bathonian Megalosaurus, thus the presence of the genus in North America represents a European migration. On other hand, Allosaurus and Supersaurus origins are consistent with a North American origin, representing an westto-east migration.

}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_2016_late_jurassic_morrison_svp_abstract.pdf}, author = {O. Mateus} } @article {9115, title = {The long term preservation of Late Jurassic sandstone dinosaur footprints in a museum environment}, journal = {International Journal of Conservation Science}, volume = {7}, year = {2016}, pages = {627-646}, abstract = {

This study focuses on the assessment of the degradation processes occurring in three sandstone infills of fossilized Late Jurassic ornithopod tridactyl footprints, found in 2001 in a coastline cliff in Porto das Barcas (Lourinh{\~a}, Portugal) and exhibited in a museum display since 2004. These dinosaur footprints present nowadays severe decay phenomena compromising their physical integrity and are leading gradually to their loss of value. The deterioration patterns were recorded, a map of their distribution was prepared and several samples were collected both in the dinosaur footprints and in the coastline cliff. Different analytical procedures were applied such as XRD, FTIR, FESEM and Ion Chromatography. A microclimatic survey was also performed and air temperature and relative humidity was measured during eight months both indoor and also outdoor. The decay patterns observed are a combination intrinsic and extrinsic factors the stone material, namely swelling of clay minerals in the rock matrix (smectite and chlorite-smectite mixed-layer), presence of salts (mainly chlorides), application of past conservation treatments (poly(vinyl) acetate and epoxy resins) and with the museum{\textquoteright}s indoor thermohygrometric conditions (mainly non-stable hygrometric conditions). This scientific knowledge is therefore essential to the sustainable preservation of this paleontological heritage.

}, url = {http://www.ijcs.uaic.ro/public/IJCS-16-36_Leal.pdf}, author = {Leal, A.A. and Dion{\'\i}sio, A. and Braga, M.A.S. and O. Mateus} } @conference {a6f2c1f51b1c445a9582e8c09b80376e, title = {Late Jurassic of Morrison Formation and Portugal tetrapods compared: a model to explain faunal exchange and similarity}, year = {2016}, note = {

Sem PDF.

}, pages = {185}, abstract = {n/a}, author = {O. Mateus} } @proceedings {9266, title = {Late Jurassic of Morrison Formation and Portugal tetrapods compared: a model to explain faunal exchange and similarity}, journal = {Annual Meeting of the Society of Vertebrate Paleontology}, year = {2016}, note = {n/a}, pages = {185}, publisher = {Journal of Vertebrate Paleontology, Program and Abstracts, 2016}, address = {Salt Late City}, abstract = {

The precursor of the North Atlantic existed between the North American and Iberian blocks from the earliest Jurassic Hettangian and has been ever expanding since. By the Kimmeridgian and Tithonian, when much of the Morrison Fm rocks were deposited, the proto-Atlantic was more than 300 km wide at 27{\textdegree} paleolatitude between North America and Iberia. Macrovertebrate paleontology reveals a unique story to the isolation of Iberia and instead suggest a paleogeographic land connection between North American and Iberia. Torvosaurus, Allosaurus, Ceratosaurus, Stegosaurus, Supersaurus and others have a distribution restricted to Morrison Formation in North America and Lourinh{\~a} Formation in Portugal. A novel paleogeographic model is here suggested: (1) around the Middle{\textendash}Late Jurassic transition there is a major palaeoceanographic and palaeoclimatic reorganization, coincidental to a major eustatic sea-level drop and uplift associated with the Callovian{\textendash} Oxfordian Atlantic Regressive Event; (2) creating an ephemeral land bridge presenting a temporary opportunity for terrestrial gateways likely across the Flemish Cap and Galician Bank land masses, allowing large dinosaurian taxa to cross the northern proto-Atlantic in both directions; (3) finally, a Callovian{\textendash}Oxfordian faunal exchange around the 163 Ma, through latest Kimmeridgian at 152 Ma (the age of equivalent genera in both Morrison and Portugal), is was an interval that allowed speciation, but retaining generic similarity of vertebrates. This model is consistent with the chronology and taxonomy required for speciation of the Iberian and American forms, exemplified by the coeval sister-taxa pairs Torvosaurus tanneri and T. gurneyi, Allosaurus fragilis and A. europaeus, or Supersaurus vivianae and S. lourinhanensis. While some of the smaller animals in the fauna show Morrison/Portugal affinities, most from Iberia have European or even Asian affinities. The larger-bodied fauna are more closely related to Morrison than to mainland Europe (except for dacentrurine stegosaurs). The body size differences and affinities of taxa across paleogeography is comparable to what is observed today across the Wallace Line. Migration may have also occurred in both directions. The closest relative of Torvosaurus is likely the European Bathonian Megalosaurus, thus the presence of the genus in North America represents a European migration. On other hand, Allosaurus and Supersaurus origins are consistent with a North American origin, representing an westto-east migration.

}, author = {O. Mateus} } @conference {RID:0209191141994-410, title = {Late Jurassic of Morrison Formation and Portugal tetrapods compared: a model to explain faunal exchange and similarity}, booktitle = {Annual Meeting of the Society of Vertebrate Paleontology}, year = {2016}, note = {n/a}, pages = {185}, address = {Salt Late City}, abstract = {n/a}, author = {O. Mateus} } @article {9115, title = {The long term preservation of Late Jurassic sandstone dinosaur footprints in a museum environment}, journal = {International Journal of Conservation Science}, volume = {7}, year = {2016}, note = {n/a}, pages = {627-646}, abstract = {

This study focuses on the assessment of the degradation processes occurring in three sandstone infills of fossilized Late Jurassic ornithopod tridactyl footprints, found in 2001 in a coastline cliff in Porto das Barcas (Lourinh{\~a}, Portugal) and exhibited in a museum display since 2004. These dinosaur footprints present nowadays severe decay phenomena compromising their physical integrity and are leading gradually to their loss of value. The deterioration patterns were recorded, a map of their distribution was prepared and several samples were collected both in the dinosaur footprints and in the coastline cliff. Different analytical procedures were applied such as XRD, FTIR, FESEM and Ion Chromatography. A microclimatic survey was also performed and air temperature and relative humidity was measured during eight months both indoor and also outdoor. The decay patterns observed are a combination intrinsic and extrinsic factors the stone material, namely swelling of clay minerals in the rock matrix (smectite and chlorite-smectite mixed-layer), presence of salts (mainly chlorides), application of past conservation treatments (poly(vinyl) acetate and epoxy resins) and with the museum{\textquoteright}s indoor thermohygrometric conditions (mainly non-stable hygrometric conditions). This scientific knowledge is therefore essential to the sustainable preservation of this paleontological heritage.

}, url = {http://www.ijcs.uaic.ro/public/IJCS-16-36_Leal.pdf}, author = {Leal, A.A. and Dion{\'{\i}sio, A. and Braga, M.A.S. and O. Mateus} } @article {RID:0209191141995-416, title = {The long term preservation of Late Jurassic sandstone dinosaur footprints in a museum environment}, journal = {International Journal of Conservation Science}, volume = {7}, year = {2016}, note = {n/a}, pages = {627-646}, abstract = {n/a}, author = {Leal, A.A. and Dion\{\'{\i}\}sio, A. and Braga, M.A.S. and O. Mateus} } @article {Mateus2016, title = {The long term preservation of late jurassic sandstone dinossaur footprints in a museum environment}, journal = {International Journal of Conservation Science}, volume = {7}, number = {3}, year = {2016}, note = {n/a}, pages = {627-646}, abstract = {n/a}, author = {Leal, AS and Dion{\'\i}sio, A. and Sequeira Braga, M.A. and O. Mateus} } @conference {3aacfb8d8e7d47ad8990d6da5b5e437e, title = {The Late Triassic of Jameson Land revisited: new vertebrate findings and the first phytosaur from Greenland}, year = {2014}, note = {

Annual Meeting of teh Society of Vertebrate Paleontology ; Conference date: 01-01-2014

}, month = {11}, pages = {182}, abstract = {n/a}, author = {Mateus,Oct{\'a}vio} } @article {6164, title = {The Late Triassic of Jameson Land revisited: new vertebrate findings and the first phytosaur from Greenland}, journal = {Journal of Vertebrate Paleontology}, volume = {Program and Abstracts, 2014}, year = {2014}, pages = {182}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_et_al2014-_jameson_land_revisited_-_svp_2014.pdf}, author = {O. Mateus and Clemmensen, L. and N. Klein and O. Wings and N. Frob{\o}se and Mil{\`a}n, J. and Adolfssen, J. and Estrup, E.} } @proceedings {4531, title = {Late Cretaceous marine reptiles and cooling at the South Atlantic coast inferred through stable oxygen isotopes of Inoceramus from the Namibe Basin, Angola}, journal = {Geological Society of America Abstracts with Programs. Vol. 45, No. 7, p.0}, year = {2013}, url = {https://gsa.confex.com/gsa/2013AM/webprogram/Paper223295.html}, author = {Christopher Strganac and Jacobs,Louis L. and Kurt M. Ferguson and Michael J. Polcyn and Mateus,Oct{\'a}vio and Anne S. Schulp and Maria Lu{\'\i}sa Morais} } @proceedings {2788, title = {Late Jurassic theropod embryos from Porto das Barcas, Lourinh{\~a} formation, Portugal}, journal = {Journal of Vertebrate Paleontology, Program and Abstracts, 2012, ISSN 1937-2809 }, year = {2012}, pages = {57}, abstract = {

A clutch of several crushed eggs and embryos from the Late Jurassic (near the Kimmeridgian-Tithonian
boundary), Lourinh{\~a} Formation, Portugal contains a complete maxilla, erupted and scattered teeth,
and presacral vertebrae. The maxilla bears four teeth separated by individualized interdental plates,
the dorsal process of the maxilla is confluent with the maxillary body, the ventral rim of the antorbital
fossa is parallel to the tooth row, and the anterior border of the maxilla forms a right angle with the
ventral margin. The teeth are conical and recurved distally with carinae on mesial and distal sides. The
vertebrae are amphiplatyan, with a ventral pair of neurovascular foramina and heavily pitted articular
facets. These fossils allow unambiguous association of basal theropod osteology (Megalosauroidea) with
a new eggshell morphotype. Synchrotron micro-computed tomographic scanning (SRμCT), scanning
electron microscopy, and thin-sections under polarized and normal light revealed that the outer
ornamentation of the eggshell is composed of anastomosing ridges and islets, the pores communicate
near the outer region of the eggshells, and in radial section they are irregular canals that ramify towards
the surface. Micro-proto induced x-ray emission (micro-PIXE) analysis of the eggshell (excluding pores)
revealed the presence of Mg, Fe, Mn (0.33\%, 0.27\% and 0.18\%, respectively) and several trace elements,
with a corresponding loss of Ca (39.4\% detected but 40.0\% expected for calcite), which suggests minimal
eggshell diagenesis. The eggshells do not luminesce, which could imply that no diagenetic alteration
took effect. However, the quenching effect of Fe2+ has to be taken into consideration. Conversely,
luminescence is observed in the pores since they are filled with sediment, composed of phyllosilicates,
as revealed by SRμCT, micro-PIXE and x-ray diffraction analyses.

}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/araujo_et_al_mateus_2012_dinosaur_eggs_portugal_svp_2012_abstract_book_meeting_abstracts.pdf.pdf}, author = {Ara{\'u}jo, R. and Castanhinha, R and O. Mateus and Martins, R.} } @conference { ref100, title = {Landmarks in the history of dinosaur paleontology in Portugal, focusing on skeletal remains}, booktitle = {Abstract volume, Dinosaurs - A Historical Perspective, 6-7 may 2008}, year = {2008}, note = {n/a}, address = {London}, abstract = {

Portugal has been providing dinosaur remains since, at least, 1863. The 18th century tiles depicting the legend of Our Lady in Cabo Espichel are probably the oldest known dinosaur track illustration. To our knowledge, the first remains found in Portugal were theropod teeth collected near Porto das Barcas (Late Jurassic of Lourinh\&$\#$227;) in June 20th, 1863 by the geologist Carlos Ribeiro (1813-1882). The first dinosaur paper was written by Henri Sauvage (1842-1917) published in 1896. All remains collected since 19th century were gathered in a work signed by Albert de Lapparent (1905-1975) and Georges Zbyszewski (1909-1999 ) titled Les Dinosauriens du Portugal (1957) that was a significant milestone in the Portuguese dinosaur paleontology and gives the state-of-the-art by the time. Several dinosaurs are named, described, depicted and mapped in that monograph. The first track record is given by Jacinto Pedro Gomes (1844-1916) in 1916. Concerning the non-scientific literature referring to dinosaurs, in 1884 the newspaper Occidente reports the Bernissart findings in Belgium. In the 1959 occurs the first visit to Portugal of Walter K\&$\#$252;hne (1911-1991) from the Free University of Berlin. Further visits and work granted the access to the Guimarota Mine and other Late Jurassic deposits in the 1960\’s, 70\’s and 80\’s with a high number of publications. In the 1980\’s and early 1990\’s starts a progressive era for dinosaur paleontology in Portugal with the works of Peter Galton, Miguel Telles Antunes, the Natural History Museum, the Museum of Lourinh\&$\#$227; and the New University of Lisbon, Oliver Rauhut, and others.

}, url = {http://omateus.googlepages.com/Mateus_Antunes2008Landmarksinthehist.pdf}, author = {O. Mateus and Antunes, MT} } @conference {RID:1218131049171-298, title = {Landmarks in the history of dinosaur paleontology in Portugal, focusing on skeletal remains}, booktitle = {Abstract volume, Dinosaurs - A Historical Perspective, 6-7 may 2008}, year = {2008}, note = {n/a}, address = {London}, abstract = {n/a}, author = {O. Mateus and Antunes, MT} } @conference {14282, title = {Landmarks in the history of dinosaur paleontology in Portugal, focusing on skeletal remains}, booktitle = {Abstract volume, Dinosaurs - A Historical Perspective, 6-7 may 2008}, year = {2008}, note = {n/a}, address = {London}, abstract = {n/a}, author = {O. Mateus and Antunes, MT} } @article {1617, title = {The large theropod fauna of the Lourinh{\~a} Formation (Portugal) and its similarity to the Morrison Formation, with a description of a new species of Allosaurus}, journal = {New Mexico Museum of Natural History and Science Bulletin}, volume = {36}, year = {2006}, pages = {123-129}, abstract = {

Late Jurassic theropod dinosaurs have been known in Portugal since 1863 but only now are they being fully understood, with the recognition of genera such as Allosaurus, Aviatyrannis, Ceratosaurus, Lourinhanosaurus, and Torvosaurus from the Lourinh{\~a} and Alcoba{\c c}a Formations (Kimmeridgian/Tithonian). Ceratosaurus dentisulcatus can now be reported from Portugal. It represents the only occurrence of this species outside the Morrison Formation.
New cranial elements confirm the presence of Torvosaurus tanneri, in Portugal. Torvosaurus was the largest Late Jurassic land carnivore. New postcranial and cranial elements allow the erection of a new species from Portugal, Allosaurus europaeus n.sp. The theropod assemblage of Portugal is similar to that of the Morrison Formation.

}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_walen_antunes_-_2006_-_the_large_theropod_fauna_of_the_lourinha_formation__portugal__and_its_similarity_to_the_morrison_formation__with_a_description_of_a_new_species_of_allosaurus.pdf}, author = {O. Mateus and Walen, A and Antunes, MT} } @article {1618, title = {Late Jurassic dinosaurs from the Morrison Formation, the Lourinh{\~a} and Alcoba{\c c}a Formations (Portugal), and the Tendaguru Beds (Tanzania): a comparison}, journal = {New Mexico Museum of Natural History and Science Bulletin}, volume = {36}, year = {2006}, pages = {223-231}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_-_2006_-_late_jurassic_dinosaurs_from_the_morrison_formation_usa_the_lourinha_and_alcobaca_formations_portugal_and_the_tendaguru_beds_tanzania_a_comparison.pdf}, author = {O. Mateus} } @article {RID:1218131049459-1, title = {The large theropod fauna of the Lourinh{\~a} Formation (Portugal) and its similarity to that of the Morrison Formation, with a description of new species of Allosaurus}, journal = {New Mexico Museum of Natural History and Science Bulletin}, volume = {36}, number = {123-129}, year = {2006}, note = {n/a}, abstract = {n/a}, author = {O. Mateus and Walen, A and Antunes, MT} } @article {RID:1218131051564-3, title = {Late Jurassic dinosaurs from the Morrison formation (USA), the Lourinh{\~a} and Alcoba{\c c}a Formations (Portugal), and the Tendaguru Beds (Tanzania): A Comparison}, journal = {New Mexico Museum of Natural History and Science Bulletin}, volume = {36}, year = {2006}, note = {n/a}, pages = {223-231}, abstract = {n/a}, author = {O. Mateus} } @conference { ref113, title = {Late Jurassic dinosaurs of Portugal.}, booktitle = {Abstracts of the 1st Symposium of European Dinosaurs, p.18}, year = {2000}, note = {

n/a

}, address = {Dusseldorf, Germany.}, abstract = {

n/a

}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus__antunes_2000_late_jurassic_dinosaurs_of_portugal_dusseldorf_2000.pdf}, author = {O. Mateus and Antunes, MT} } @conference {RID:1218131049461-311, title = {Late Jurassic dinosaurs of Portugal}, booktitle = {Abstracts of the 1st Symposium of European Dinosaurs}, year = {2000}, note = {n/a}, address = {Dusseldorf, Germany.}, abstract = {n/a}, author = {O. Mateus and Antunes, MT} } @conference {14348, title = {Late Jurassic dinosaurs of Portugal}, booktitle = {Abstracts of the 1st Symposium of European Dinosaurs}, year = {2000}, note = {n/a}, address = {Dusseldorf, Germany.}, abstract = {n/a}, author = {O. Mateus and Antunes, MT} } @article { ref27, title = {Lourinhanosaurus antunesi, a new Upper Jurassic allosauroid (Dinosauria : Theropoda) from Lourinha, Portugal}, journal = {Mem{\'o}rias da Academia de Ci{\^e}ncias de Lisboa}, volume = {37}, year = {1998}, note = {

n/a

}, pages = {111-124}, abstract = {

n/a

}, url = {http://www.museulourinha.org/pt/Omateus/Papers/Mateus\%201998\%20Lourinhanosaurus.pdf}, attachments = {https://docentes.fct.unl.pt/sites/default/files/omateus/files/mateus_1998_lourinhanosaurus_antunesi.pdf}, author = {O. Mateus} } @article {RID:1218131049462-259, title = {Lourinhanosaurus antunesi, a new Upper Jurassic allosauroid (Dinosauria : Theropoda) from Lourinha, Portugal}, journal = {Mem{\'o}rias da Academia de Ci{\^e}ncias de Lisboa}, volume = {37}, year = {1998}, note = {n/a}, pages = {111-124}, abstract = {n/a}, author = {O. Mateus} }