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Book
Coelho,(ed)C., & et al (2013).  Arrábida - al-rábita. , Lisboa, 229 pp.: Associação de Município da Região de Setúbal
Pais, {J. J. C. }, Kullberg {J. C. R. }, de} Melo {J. M. D. J., Mateus O., & de} Almeida {J. A. (2013).  Arrábida - al-rábita. , 1: Associação de Municípos da Região de Lisboa Abstract

The publication of the present work - rightly designated as the book of Arrabida's nomination file for inscription on the World Heritage list - has for all of us a special significance as it represents, in a sense, the culmination of a complex, challenging and rewarding process. As is widely known, the Arrábida is included since 2004 in UNESCO's Portuguese tentative list, with AMRS being one of this process' promoters. It wouldn't be appropriate to describe here all the details, but it is fair to say that since 2004 to the present day, we've come a long way in recovering and valuing the Arrábida. It is with sincere satisfaction that we can say: our knowledge of the Property is now deeper, up to date and much more accurate, doing justice to the exceptional values contained within the Arrábida - which is well expressed in the work now published, based on researches and works of the highest scientific value. This is also a regional development project, to value our lands, people and the natural and cultural heritage. The Setúbal's Peninsula is a region that contains within its territory a vast natural and cultural heritage, being the Arrábida one of the most beautiful and significant natural areas in the Mediterranean. The Arrábida Mountain is a place with its own identity, being the result of a long history of Man's adaptation to Nature. It is a place of unmistakable aesthetic beauty, a unique place where nature and culture intertwine; it is a place of contrasts, of land and sea, sky and mountains, a place of combined actions by Man and Nature. Place of vibrant social practices, of rituals and festivals, of knowledge, of representations and expressions, of instruments, objects and artifacts. Place with a history that must be preserved and bequeathed to future generations. Place with monuments of vanished civilizations, but also of living traditions. These are some of the values supporting the Arrábida's nomination for the World's Heritage list. It is a complex and demanding nomination file, which this work is an illustrative sample of. A mixed application - as it includes both the natural and cultural heritage - which, given the richness and uniqueness of the Property in question, is fully justified. It is our profound conviction that this Nomination streamlines the potential of our region, bringing benefits not only to the local population, but also to the whole country. To that extent, it is also a sign of hope and confidence showing that it is possible to build a different future; that by investing in our people, in their abilities, knowledge and traditions, it is possible to create a sustainable development; that is possible to leave for future generations a legacy of which we are proud of having worked on. To be able enjoy this magnificent edition is a step in that direction.

Mateus, O. (2010).  Colecções e museus de Geologia: missão e gestão. , 1: Ed. Universidade de Coimbra e Centro de Estudos de História e Filosofia da Ciência Abstract
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Moreno-Azanza, M., Gasca J. M., Canudo J. I., Lázaro B. B., & Mateus O. (2016).  The evolution of the ornithischian eggshell: State of the art and perspectives. : Palaeontological Society of Japan Abstract
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Mateus, O., Jacobs L. L., Polcyn {M. J. }, Myers T. S., & Schulp A. S. (2015).  The fossil record of testudines from Angola from the Turonian to Oligocene. : Journal of Vertebrate Paleontology Abstract
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Marzola, M., Mateus O., Wings O., Klein N., Milan J., & [Unknown] L. B. C. (2016).  The herpetofauna from the Late Triassic of the Jameson Land Basin (East Greenland): review and updates. : XIV EAVP Meeting, Programme and Abstract Book Abstract
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Myers, T. S., Mateus O., Polcyn {M. J. }, Vineyard D., & Jacobs L. L. (2016).  A new chelonioid turtle from the Paleocene of Cabinda, Angola. Abstract

We report a new chelonioid turtle on the basis of a nearly complete skull collected in lower Paleocene, shallow marine deposits, equivalent to the offshore Landana Formation, near the town of Landana in Cabinda Province, Angola. Chelonioid material previously reported from this locality is likely referable to this new taxon. The well-preserved skull is missing the left quadrate, squamosal, and prootic, both opisthotics, and the mandible. The skull possesses a rod-like basisphenoid rostrum, which is a synapomorphy of Chelonioidea, but it differs from other chelonioid skulls in that the contact between the parietal and squamosal is absent, and the posterior palatine foramen is present. Phylogenetic analysis recovers the new taxon as a basal chelonioid. The Paleocenetextendash Eocene strata near Landana have produced a wealth of turtle fossils, including the holotype of the pleurodire Taphrosphys congolensis. A turtle humerus collected from the Landana locality differs morphologically from the humeri of chelonioids and Taphrosphys, indicating the presence of a third taxon. Chelonioid fossil material in the Landana assemblage is rare compared to the abundant fragmentary remains of Taphrosphys that are found throughout the stratigraphic section. This disparity in abundance suggests the new chelonioid taxon preferred open marine habitats, whereas Taphrosphys frequented nearshore environments.

Muchagata, J., & Mateus O. (2016).  Sexual display and rostral variation in extinct beaked whale, Globicetus hiberus. : XIV EAVP Meeting, Programme and Abstract Book Abstract
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Polcyn, {M. J. }, Jacobs L. L., Schulp A. S., & Mateus O. (2015).  Tethyan and Weddellian biogeographic mixing in the Maastrichtian of Angola. : Journal of Vertebrate Paleontology Abstract
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Polcyn, {M. J. }, Jacobs {L. L. }, Schulp {A. S. }, & Mateus O. (2015).  Trolling the Cretaceous Seas: Marine Amniotes of Two West Coast Margins. : Geological Society of America Abstracts with Programs. Vol. 47, No. 4, p.55 Abstract

In this session we review the Upper Cretaceous marine amniote records from the west coasts of North America and Africa. Recent work by our group in Angola, on the west coast of Africa, has opened up new fossiliferous localities, producing well-preserved turtles, plesiosaurs, and mosasaurs, ranging in age from Late Turonian to Late Maastrichtian. These African localities were deposited in arid latitudes and highly productive upwelling zones along the passive margin of a growing South Atlantic Ocean. The fossil record of Cretaceous marine amniotes from the West Coast of North America is relatively meager when compared to the African record and the prolific fossil beds laid down in the epicontinental seas of the Western Interior Seaway and northern Europe. Nonetheless, these localities provide an important glimpse of a marine ecosystem that developed on the active margins of a deep ocean basin. Historically considered to be depauperate and endemic, the west coast fauna was characterized by unusual forms such as Plotosaurus, arguably one of the most derived mosasaurs; however, in recent years, additional taxa have been described, revealing species diversity and ecological partitioning within these communities and in some cases, faunal interchange with other regions. The large quantity of well-preserved fossils from the west coast of Africa is influenced in part by its paleogeographic position, deposited within highly productive areas of Hadley Cell controlled upwelling zones. By contrast, the North American west coast localities have been deposited in temperate and higher latitudes since the Late Cretaceous. Nonetheless, the North American and African faunas share some common characteristics in a possessing a mix of endemic and more cosmopolitan forms. Habitat partitioning reflected in tooth form and body size is comparable between the Angolan and the North American west coast, and there is remarkable convergence in taxa which appear to exploit certain like-niches.

Silva, T., Costa F., Fernandes J., Calvo R., & Mateus O. (2016).  The use of a portable X-ray fluorescence analyzer in the reconstitution of dinosaur fossils. , 7: European Conference on X-Ray Spectrometry (EXRS) Abstract

Portable X-ray fluorescence spectrometers (p-XRF) have been used in many fields of application/studies like art, archaeology, heavy metals in soil, rocks and ores characterization, and have been a powerful tool for a rapid non-destructive in-situ analysis, without any sample preparation required. This approach was applied in the present case, to distinguish the origin of the fossil bones of two dinosaur specimens from different localities that were accidentally put together in the museum a few years ago. Fossil bones with sedimentary matrix associated were stored together until today in the collection of Geological Museum (Lisbon) and regarded as one single specimen. One set of bones is part of the holotype MG 5787 of the ankylosaur Dracopelta zbyszweskii, which was discovered at Praia do Sul, and described in 1980, while the other, is an undescribed half skeleton of dacentrurine stegosaur, unearthed in the 1960’s at Atouguia da Baleia, near Peniche (both in the coast of central Portugal, distanced about 100 km from each other). Since both specimens are highly valuable for paleontology, a study was developed with the aim of separating and reconstituting the two specimens. The handheld p-XRF (Genius 9000+7000 from Skyray Instrument) was directly used in the sedimentary matrix when it was separated from the bone, and the measure of the chemical content was performed in the intermediate layer between the surface and the bone, to avoid contaminations. Although the light elements could not be attained, because the analyzer is not equipped with the option of gas charging system, the spectra obtained showed differences mainly in the ratio K/Ca, allowing distinguishing the provenance of the bones (Atouguia or Praia do Sul). These results were compared with chemical analysis obtained with XRF laboratorial equipment and complemented by the mineralogical study through X-ray diffraction (XRD) of the sediments where the bones fossilized. The difference observed in the mineralogical constitution of the sedimentary matrix from the two localities (mainly quartz, calcite, feldspars and micas with variable content) explains the variation in the values found for the ratio K/Ca (<0.5 for Atouguia and >>1 for Praia do Sul). The data obtained will be presented and discussed focusing on the importance of using a portable X-ray fluorescence analyzer applied to the reconstitution of dinosaur fossils that proved to be very useful in the present case.

Book Chapter
Kullberg, J. C., Rocha R. B., Soares A. F., Rey J., Terrinha P., Azerêdo A. C., Callapez P., Duarte, L.V., Kullberg M. C., Martins L., Miranda J. R., Alves C., Mata J., Madeira J., Mateus O., Moreira M., & Nogueira C. R. (2013).  A Bacia Lusitaniana: Estratigrafia, Paleogeografia e Tectónica. (Dias, R. Araújo, A, Terrinha, P. and Kullberg, J. C., Ed.).Geologia de Portugal no contexto da Ibéria. Volume II. 195-350., Lisboa: Escolar Editorakullberg_et_al_2013_a_bacia_lusitaniana.pdf
da} Rocha, {R. E. B., Kullberg {J. C. R. }, & Mateus O. (2013).  A Bacia Lusitaniana: Estratigrafia, Paleogeografia e Tectónica. (Dias, Araújo, R., A, Terrinha, P., Kullberg, {J. C.}, Ed.).Geologia de Portugal no contexto da Ibéria. 195–347., 1: Escolar Editora Abstract
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Gaspar, A., Avelar T., & Mateus O. (2007).  Criacionismo e Sociedade no Séc. XX. (Avelar, T., O. Mateus, Almada, F., Gaspar, A., Ed.).Evolução e Criacionismo: Uma Relação Impossível. 133-160., Lisboa: Quasi ed. gasparavelarmateus2007evoluoecriacio.pdf
Gaspar, A., Avelar T., & Mateus O. (2007).  Criacionismo e Sociedade no Séc. XX.  Evolução e Criacionismo: Uma Relação Impossível. 133-160., Lisboa Abstract
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Mateus, O. (2006).  The European Enigmatic Dinosaur Evolution [in Japanese]. The Gigantic dinosaur Expo 2006 (catalogue). 69-71.mateus_2006_european.pdf
Araújo, R., Castanhinha R., & Mateus O. (2011).  Evolutionary major trends of ornithopod dinosaurs teeth. (J.Calvo, J. Porfiri, B. Gonzalez Riga y D. Dos Santos (scientific editors), Ed.).Dinosaurios y paleontología desde América Latina. 25-31., Jan: EDIUNC, Editorial de la Universidad Nacional de Cuyo Abstractaraujo_et_al_2011_evolutionary_major_trends_of_ornithopod_dinosaurs_teeth.pdf

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Mateus, O. (2011).  Evolutionary major trends of ornithopod dinosaurs teeth. (Unknown Unknown, Ed.).Dinosaurios y paleontología desde América Latina. 25–31., 1: EDIUNC, Editorial de la Universidad Nacional de Cuyo Abstract
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Mateus, O. (2010).  Evolutionary major trends of ornithopod dinosaurs teeth.. (J Calvo, J Porfiri, Y, {D Dos Santos BGR}, Ed.).Dinosaurios y paleontología desde América Latina,. 25–31 pp.., 1: EDIUNC Abstract
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Mateus, O. (2016).  Exemplos bizarros de evolução em dinossauros e alguns casos portugueses. Do Big Bang ao Homem. 81-95., Porto: U.Porto Ediçõesmateus_2016_capitulo_livro_dinosaurs.pdf
Mateus, O. (2016).  Exemplos bizarros de evolucão em dinossauros e alguns casos portugueses. Do Big Bang ao Homem. 81–95.: U.Porto Edicões Abstract
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Mateus, O. (2016).  Exemplos bizarros de evolução em dinossauros e alguns casos portugueses. Do Big Bang ao Homem. 81-95., Porto: U.Porto Edi{\c c}ões Abstract
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Mateus, O. (2016).  Exemplos bizarros de evolução em dinossauros e alguns casos portugueses. Do Big Bang ao Homem. 81-95., Porto Abstract
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Mateus, O. (2008).  Fósseis de transição, elos perdidos, fósseis vivos e espécies estáveis. (Levy, et al, Ed.).Evolução: História e Argumentos. 77-96., Lisboa: Esfera do Caosmateus_2008_evolucao_fosseis_de_transicao.pdf
Mateus, O., Callapez P. M., Polcyn M. J., Schulp A. S., Gonçalves A. O., & Jacobs L. L. (2019).  The Fossil Record of Biodiversity in Angola Through Time: A Paleontological Perspective. (Huntley, Brian J., Russo, Vladimir, Lages, Fernanda, Ferrand, Nuno, Ed.).Biodiversity of Angola: Science & Conservation: A Modern Synthesis. 53–76.: Springer International Publishing Abstractmateus2019_chapter_thefossilrecordofbiodiversityi.pdf

This chapter provides an overview of the alpha paleobiodiversity of Angola based on the available fossil record that is limited to the sedimentary rocks, ranging in age from Precambrian to the present. The geological period with the highest paleobiodiversity in the Angolan fossil record is the Cretaceous, with more than 80{%} of the total known fossil taxa, especially marine molluscs, including ammonites as a majority among them. The vertebrates represent about 15{%} of the known fauna and about one tenth of them are species firstly described based on specimens from Angola.

Mateus, O., Callapez P. M., Polcyn M. J., Schulp A. S., Gonçalves A. O., & Jacobs L. L. (2019).  The Fossil Record of Biodiversity in Angola Through Time: A Paleontological Perspective. (Huntley, Brian J., Russo, Vladimir, Lages, Fernanda, Ferrand, Nuno, Ed.).Biodiversity of Angola: Science {&} Conservation: A Modern Synthesis. 53–76., Cham: Springer International Publishing Abstract

This chapter provides an overview of the alpha paleobiodiversity of Angola based on the available fossil record that is limited to the sedimentary rocks, ranging in age from Precambrian to the present. The geological period with the highest paleobiodiversity in the Angolan fossil record is the Cretaceous, with more than 80{%} of the total known fossil taxa, especially marine molluscs, including ammonites as a majority among them. The vertebrates represent about 15{%} of the known fauna and about one tenth of them are species firstly described based on specimens from Angola.

Mateus, O. (2014).  Gigantic Jurassic predators. 52 Things You Should Know About Palaeontology. 56-57.: Agile Libremateus_2014_gigantic_jurassic_predators.pdf
Mateus, O. (2014).  Gigantic jurassic predators. (Agile Libre, Ed.).52 Things You Should Know About Palaeontology. 56–57.: Agile Libre Abstract
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Mateus, O., & Jacinto J. (2008).  Hemidactylus turcicus. Atlas dos Anfíbios e Répteis de Portugal. 130-131., Lisboa: A. Loureiro, N. Ferrand de Almeida, M.A. Carretero, O.S. Paulo. Instituto da Conservação da Natureza e da Biodiversidademateus__jacinto_2008_hemidactylus_turcicus_in_atlas_dos_anfibios_e_repteis_de_portugal.pdf
Mateus, O., & Jacinto J. J. (2008).  Hemidactylus turcicus. (A Loureiro, N F de Almeida, M.A Carretero, O S Paulo, Ed.).Atlas dos Anfíbio e Répteis de Portugal. 134-135. Abstract
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Puértolas-Pascual, E., Mateus O., & Callapez P. M. (2018).  Implicaciones de la fenestra mandibular externa en el origen de Crocodylia. EJIP Life finds a way. 14-144., Gasteiz, Spainpuertolas-pascual_et_al_2018_ejip.pdf
authors listed, N. (2009).  International Conference on the Geological Collections and Museums: mission and management.. (Brandao J, Callapez P, Mateus O, Castro P, Ed.). , Jan: Journal of Paleontological Techniques 5 (special volume) Abstract
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Rotatori, F. M., Moreno-Azanza M., & Mateus O. (2018).  Isolated dryosaurid (Dinosauria: Ornithopoda) cranial remains from the Late Jurassic of Portugal. EJIP Life finds a way. 95-98., Gasteiz, Spainrotatori_et_al_2018_ejip.pdf
Mateus, O., & Campos H. (2018).  Loulé há mais de 220 Milhões de anos: os vertebrados fósseis do Algarve triásico. Loulé: Territórios. Memórias. Identidades. 651-659.: Museu Nacional de Arqueologia | Imprensa Nacionalmateus_campos2018_algarve_triasico.pdf
Mateus, O., Callapez P. M., Polcyn M. J., Schulp A. S., Gonçalves A. O., & Jacobs L. L. (2019).  O registo fóssil da biodiversidade em Angola ao longo do tempo: uma perspectiva paleontológica. (Huntley B.J., Russo V., Lages F., Ferrand N., Ed.).Biodiversidade de Angola: Ciência e Conservação - Uma Síntese Moderna. 89-116., Porto: Arte & Ciência Abstractmateus_et_al_2019_paleobiodiversidade_angola.pdf

Este capítulo apresenta uma visão geral da paleobiodiversidade alfa de Angola com base no registo fóssil disponível, o qual se limita às rochas sedimentares, a sua idade variando entre o Pré‑Câmbrico e o pre‑
sente. O período geológico com a maior paleobiodiversidade no registo fóssil angolano é o Cretácico, com mais de 80% do total dos táxones fósseis conhecidos, especialmente moluscos marinhos, sendo estes na sua maioria
amonites. Os vertebrados representam cerca de 15% da fauna conhecida e cerca de um décimo destes são espécies descritas pela primeira vez com base em espécimes de Angola.

Gaspar, A., Mateus O., & Almada F. (2007).  Os argumentos criacionistas em face da evidência científica. Evolução e Criacionismo: Uma Relação Impossível. 197-237., Lisboa: Quasi ed.gasparmateusealmada2007argumentosevo.pdf
Gaspar, A., Mateus O., & Almada F. (2007).  Os argumentos criacionistas em face da evidência científica. Evolução e Criacionismo: Uma Relação Impossível. 197-237., Lisboa Abstract
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Mateus, O. (2010).  Paleontological collections of the Museum of Lourinhã (Portugal). (Brandao, JM, Callapez, PM, O. Mateus, Castro, P, Ed.).Colecções e museus de Geologia: missão e gestão. 121-126., Jan: Ed. Universidade de Coimbra e Centro de Estudos e Filosofia da História da Ciência Coimbra Abstractmateus_2010_paleontological_collections_of_the_museum_of_lourinha__geocoleccoes_omateus.pdf

Abstract: The paleontological collections of the Museum of Lourinhã, in Portugal, has a rich paleontological collection, particularly of Late Jurassic dinosaurs of the Lourinhã Formation (Kimmeridgian-Tithonian). Most salient highlights comprehend the following dinosaur holotype specimens: stegosaur Miragaia longicollum, theropod Lourinhanosaurus antunesi, sauropod Dinheirosaurus lourinhanensis, ornithopod Draconyx loureiroi, theropod Allosaurus europaeus, and, a mammal, Kuehneodon hahni. Other dinosaur specimens are referred including the nest and eggs and embryos of Lourinhanosaurus. Portugal is very productive in Late Jurassic vertebrates, being the seventh country bearing more dinosaur taxa.

Mateus, O. (2010).  Paleontological collections of the Museum of Lourinhã (Portugal). (Brandao, JM, Callapez, PM, O. Mateus, Castro, P, Ed.).Colecções e museus de Geologia: missão e gestão. 121–126., 1: Ed. Universidade de Coimbra e Centro de Estudos e Filosofia da História da Ciência Coimbra Abstract
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Mateus, O. (2010).  Paleontological collections of the Museum of Lourinhã (Portugal). (JM Brandão, Callapez, PM, O. Mateus, Castro, P, Ed.).Colecções e museus de Geologia: missão e gestão. 121–126., 1: Ed. Universidade de Coimbra e Centro de Estudos de História e Filosofia da Ciência Abstract
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Salminen, J., Dinis J., & Mateus O. (2014).  Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal. (Rogério Rocha, João Pais, José Carlos Kullberg, Stanley Finney, Ed.).STRATI 2013 First International Congress on Stratigraphy At the Cutting Edge of Stratigraphy. 873-877., Heidelberg New York Dordrecht London: Springer Abstractsalminen_et_al_2014_porto_da_calada_stratigraphy_jk_boundary_in_rocha_et_al_strati_.pdf

We present a stratigraphic log supporting a preliminary magnetostratigraphy of a Tithonian–Berriasian section in Porto da Calada (Portugal). Based on biostratigraphy and reversed and normal magnetostratigraphy, the location of the Tithonian–Berriasian boundary is tentatively located at ca. 52 m, not in disagreement
with former proposals. Due to the occurrence of later remagnetization (diagenesis), the magnetostratigraphic definition of the Tithonian–Berriasian section at the Cabo Espichel (Portugal) location was not able to be established.

Mateus, O. (2014).  Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal. (Rogério Rocha, João Pais, Kullberg, {José Carlos}, Stanley Finney, Ed.).STRATI 2013:First International Congress on Stratigraphy At the Cutting Edge of Stratigraphy. 873–877., 1: Springer International Publishing Switzerland Abstract

We present a stratigraphic log supporting a preliminary magnetostratigraphy of a Tithonian–Berriasian section in Porto da Calada (Portugal). Based on biostratigraphy and reversed and normal magnetostratigraphy, the location of the Tithonian–Berriasian boundary is tentatively located at ca. 52 m, not in disagreement with former proposals. Due to the occurrence of later remagnetization (diagenesis), the magnetostratigraphic definition of the Tithonian–Berriasian section at the Cabo Espichel (Portugal) location was not able to be established

Salminen, J., Dinis J., & Mateus O. (2014).  Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal. {STRATI} 2013. 873–877.: Springer Science $\mathplus$ Business Media Abstract
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Mateus, O. (2008).   Fósseis de transição, elos perdidos, fósseis vivos e espécies estáveis . Evolução: História e Argumentos. 77-96., Lisboa Abstract
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Chart
Mateus, O. (2017).  Que Dinossauros Existiram em Portugal?. : Poster 80x59 cm, as a supplement of newspaper “Correio da Manhã” of 16 September 2017poster_correio_da_manha.jpg
Conference Paper
Marzola, M., Mateus O., Milàn J., & Clemmensen L. B. (2017).  The 2016 Dinosaur Expedition to the Late Triassic of the Jameson Land Basin, East Greenland. Abstract book of the XV Encuentro de Jóvenes Investigadores en Paleontolog{\'ıa/XV Encontro de Jovenes Investigadores em Paleontologia, Pombal, 428 pp.. 249–253. Abstract
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Marzola, M., Mateus O., Milàn J., & Clemmensen {L. B. } (2017).  The 2016 Dinosaur Expedition to the Late Triassic of the Jameson Land Basin, East Greenland. 249–253. Abstract
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Mateus, O. (2012).  Age and paleoecology of mosasaurs and plesiosaurs from the Late Cretaceous South Atlantic margin at Bentiaba, Angola. Journal of Vertebrate Paleontology, Program and Abstracts, 2012. 180.. 180–181., 1 Abstract
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