Les Plus Anciens Mastodontes Tetralophodontes (Langhien inférieur Vb), évolution et remarques sur la Tetralophodontie

This study deals with mastodont teeth found near Lisbon in Lower Langhian (lower Middle Miocene) fluviatile, feldspathic sands (Vb division). Conclusions are as follows: 1. Tetralophodont molars (even if at a still primitive stade of the tetralophodont condition) do exist at least since lower Langhian times, and not only since late Middle Miocene as was previously known. 2. Tri- and tetralophodont structures may (and indeed do) coexist in the same individual: such examples do not correspond to transitional forms, but instead to a mosaic of juxtaposed characters (however this does not mean there are no transitional forms in other instances). 3. So these structures coexisted in a population not yet genetically separated beyond fertile cross-breeding, i.e. beyond species' level. 4. Origin of the tetralophodont molar was due to some mutation (s). but without crossing species, limits and even more genus'ones. 5. At this times probably soon after the first appearance of tetralophodont mutants, animals with such characters were a small but significant minority among the population (17% if account is taken on D4's: only 2% after M2's). 6. There was not then any direct and clear correlation between number of lophs (transversal crests) and tooth size, even if the increase of such number goes along with length's increase. 7. Dimensions (length in special) in tetralophodont teeth tend to exceed those in «normal» trilophodont teeth, this being particularly clear in D4, even if there is no clear distinction: the situation is quite the same, maybe less marked, with the M2. 8. According to the preceding conclusions there are no reasons to segregate different taxa among such mastodont population on the grounds of the presence in D4, M1 and M2 of 3 or 4 crests (this character being regarded as diagnostic of the genus Tetralophodon). 9. On the contrary, if any natural (in biological sense) classification is disregarded and a morphological parataxonomy is adopted there should be considered both Gomphotherium angustidens and Tetralophodon sp.: however this is absolutely not our opinion.

Notas sobre depósitos de Taveiro estratigrafia, paleontologia, idade, paleoecologia

This paper reports some research work that has been done to support Geological Survey's field work for the 1:50.000 Carta Geológica de Portugal, (sheets 19-C Figueira da Foz and 19-D Coimbra-Lousã). Its main purpose was to establish the age of some continental formations. At Cerâmica do Mondego, Ld.ª near Taveiro, two series were observed. The lower one is mainly pelitic, montmorillonite being predominant. It also includes some sandy beds and channel deposits with high energy sediments (conglomerate with limestone pebbles). The upper series lies unconformably upon the former, and there is a neat discontinuity surface between the two. It mainly consists of sands, kaolinite being the most abundant of the clay minerals. This seems to indicate an intensive weathering, an acid, well drained environment and transportation by quite high energy running waters. No fossils were recorded. Preliminary paleontological results are presented, along with some data concerning other localities (Aveiro, etc.). Fossils found in the lower series are: gastropoda (Bulimus gaudryi, TV. 15 bed), several vertebrates (TV. 18), fishes (TV. 19?) and plants (TV. 19-TV. 24). Vertebrata belong to the same fauna as that from Vizo, Aveiro, etc. The presence of mammals is most important as only a single tooth was previously Know in Europe (Southern France) in Late Cretaceous formations. Elsewhere there are some mammalian remains in Peru besides the rich assemblages found in the USA and Mongolia. Plants are representative of the «Debeya flora» well known at several localities in Beira Litoral province, in «Buçaco sandstones», and in Lisbon's «Basaltic Complex». The most important stratigraphical conclusion is that the lower series is Upper Campanian and/or Maastrichtian in age, and not Tertiary as sometimes it has been considered. As at Aveiro, «Bebeya flora» occurs in-beds somewhat higher than those with the Aveiro-Vizo-Taveiro vertebrate fauna. Correlation with other «Debeya flora» localities are now more clear. Data concerning Taveiro lower series, in the whole, point out to a rather warm (and moist?) environment in an occasionally (seasonally?) flooded region.

Notes sur la géologie et la paleontology du Miocène de Lisbonne; (XX) les plus anciens mastodontes tetralophodontes (Langhien inférieur Vb), évolution et remarques sur la tetralophodontie

This study deals with mastodont teeth found near Lisbon in Lower Langhian (lower Middle Miocene) fluviatile, feldspathic sands (Vb division). Conclusions are as follows: 1. Tetralophodont molars (even if at a still primitive stade of the tetralophodont condition) do exist at least since lower Langhian times, and not only since late Middle Miocene as was previously known. 2. Tri- and tetralophodont structures may (and indeed do) coexist in the same individual: such examples do not correspond to transitional forms, but instead to a mosaic of juxtaposed characters (however this does not mean there are no transitional forms in other instances). 3. So these structures coexisted in a population not yet geneticaliy separated beyond fertile cross-breeding, i.e. beyond species'level. 4. Origin of the tetralophodont molar was due to some mutation (s). but without crossing species, limits and even more genus' ones. 5. At this times probably soon after the first appearance of tetralophodont mutants, animals with such characters were a small but signifiant minority among the population (17% if account is taken on D4's: only 2% after M2's). 6. There was not then any direct and clear correlation between number of lophs (transversal crests) and tooth size, even if the increase of such number goes along with length's increase. 7. Dimensions (length in special) in tetralophodont teeth tend to exceed those in «normal» trilophodont teeth, this being particularly clear in D4, even if there is no clear distinction: the situation is quite the same, maybe less marked, with the M2. 8. According to the preceding conclusions there are no reasons to segregate different taxa among such mastodont population on the grounds of the presence in D4, M1 and M2 of 3 or 4 crests (this character being regarded as diagnostic of the genus Tetralophodon). 9. On the contrary, if any natural (in biological sense) classification is disregarded and a morphological parataxonomy is adopted there should be considered both Gomphotherium angustidens and Tetralophodon sp.: however this is absolutely not our opinion.

Notas sobre depósitos de Taveiro estratigrafia, paleontologia, idade, paleoecologia

This paper reports some research work that has been done to support Geological Survey's field work for the 1:50.000 Carta Geológica de Portugal, (sheets 19-C Figueira da Foz and 19-D Coimbra-Lousã). Its main purpose was to establish the age of some continental formations. At Cerâmica do Mondego, Lda. near Taveiro, two series were observed. The lower one is mainly pelitic, montmorillonite being predominant. It also includes some sandy beds and channel deposits with high energy sediments (conglomerate with limestone pebbles). The upper series lies unconformably upon the former, and there is a neat discontinuity surface between the two. It mainly consists of sands, kaolinite being the most abundant of the clay minerals. This seems to indicate an intensive weathering, an acid, well drained environment and transportation by quite high energy running waters. No fossils were recorded. Preliminary paleontological results are presented, along with some data concerning other localities (Aveiro, etc). Fossils found in the lower series are: gastropoda (Bulimus gaudryi, TV. 15 bed), several vertebrates (TV. 18), fishes (TV. 19?) and plants (TV. 19-TV. 24). Vertebrata belong to the same fauna as that from Vizo, Aveiro, etc. The presence of mammals is most important as only a single tooth was previously know in Europe (Southern France) in Late Cretaceous formations. Elsewhere there are some mammalian remains in Peru besides the rich assemblages found in the USA and Mongolia. Plants are representative of the «Debeya flora» well known at several localities in Beira Litoral province, in «Buçaco sandstones», and in Lisbon's «Basaltic Complex». The most important stratigraphical conclusion is that the lower series is Upper Campanian and/or Maastrichtian in age, and not Tertiary as sometimes it has been considered. As at Aveiro, «Bebeya flora» occurs in-beds somewhat higher than those with the Aveiro-Vizo-Taveiro vertebrate fauna. Correlation with other «Debeya flora» localities are now more clear. Data concerning Taveiro lower series, in the whole, point out to a rather warm (and moist?) environment in an occasionally (seasonally?) flooded region.

Paralophiodon cf. leptorhynchum (tapiroidea, mammalia) à Vale Furado: contribution à la connaissance de l’éocène au Portugal

A canine tooth from Vale Furado is classified as Paralophiodon cf. leptorhynchum. The genus Paralophiodon indicates an age from Lower Lutetian to Auversian, Middle Eocene. As it belongs in the lineage of P. leptorhynchum, possible age span is furth~L~uced from Middle Lutetian to Auversian. This conclusion remains valid or nearly so even in the less probable case of confusion with some form included in P. isselensis lineage. Our previous (1975) datation for sandstones and pelites from Vale Furado is thus confirmed, and more accurately recognized. Paralophiodon and the crocodilian Iberosuchus are a rather sound basis for correlation with stratigraphical units near Zamora and Salamanca in Spain.

The bovid from the Carriça clay-pit (Côja): a discussion

A Bovid tooth referred to in the litterature as from the same locality that yielded upper Eocene mammals belongs to a modem or probably contemporary Bos taurus (domestic cattle); it is not a fossil and certainly was not found in situ. As it may induce in confusion, it must not anymore be taken into account in future paleontological and stratigraphic work.

Patologia óssea do insuficiente renal crónico: desafio clínico-biológico ; Caracterização da osteodistrofia renal e efeitos da biocompatibilidade de membranas de hemodiálise, na remodelação óssea

Resumo: Os resultados das nossas investigações, apresentadas ao longo desta dissertação,contribuíram para a otimização do diagnóstico invasivo e não invasivo da osteodistrofia renal e permitiram evidenciar a relevância, para a expressão clínica e histológica da ODR, de algumas articularidades específicas da população hemodialisada, nomeadamente: a utilização de membranas de hemodiálise mais biocompatíveis e com elevada permeabilidade, o recurso a técnicas de hemodiafiltração com otimização da capacidade convectiva, as limitações dos marcadores bioquímicos de remodelação óssea ou a insuficiência / deficiência em vitamina D nativa (bem como os resultados da suplementação com esta vitamina). Testámos, pela primeira vez em doentes hemodialisados, novos marcadores da formação e reabsorção óssea, que validámos mediante a comparação com os resultados da histomorfometria óssea. No seu conjunto, e de forma integrada, as nossas investigações permitiram-nos: - Evidenciar a diminuição da expressão do recetor da PTH/PTHrP na cartilagem de crescimento, num modelo animal de IRC, o que explica, pelo menos em parte, o atraso de crescimento observado nesta patologia, bem como a diminuição da resposta à ação da PTH; - Demonstrar as vantagens da determinação da isoforma óssea da fosfatase alcalina, em relação à fosfatase alcalina total, no diagnóstico diferencial entre baixa e elevada remodelação óssea; - Utilizar, pela primeira vez em hemodialisados, a piridinolina e a desoxipiridinolina no diagnóstico da reabsorção óssea. Este foi o primeiro marcador sérico específico da atividade osteoclástica, utilizado com sucesso em doentes anúricos em hemodiálise. Evidenciámos uma excelente correlação destes dois marcadores bioquímicos com a superfície osteoclástica e com o número de osteoclastos/mm2;- Demonstrar as acentuadas limitações de outros marcadores da formação e reabsorção óssea (nomeadamente a osteocalcina, o propeptido carboxiterminal do procolagénio tipo I-PICP, e o Telopeptido do colagénio tipo I – ICTP) com base nas correlações entre os doseamentos séricos ou plasmáticos destes marcadores e a biópsia óssea com avaliação histomorfométrica; -Evidenciar as limitações induzidas pela sobrecarga alumínica na interpretação dos níveis séricos dos marcadores não invasivos da remodelação óssea;-Testar a eficácia e segurança da utilização de “microdoses” de desferroxamina na terapêutica da intoxicação alumínica, em doentes com acentuada exposição a este metal;-Demonstrar que os doentes hemodialisados cronicamente com dialisadores de poliacrilonitrilo (membranas de alta permeabilidade),apresentavam menor ativação osteoblástica e osteoclástica, que os doentes dialisados com membranas de cuprofano(baixa permeabilidade), sendo os níveis de iPTH semelhantes em ambos os grupos estudados. Estes resultados apontam para uma menor ativação da remodelação óssea quando se utilizam membranas de hemodiálise mais biocompatíveis e/ou de maior permeabilidade, o que se poderá relacionar com a ultrafiltração de mediadores da ativação celular ou com a menor ativação dos mecanismos estimuladores da remodelação óssea, por parte destas membranas. Entre os mediadores da remodelação óssea que demonstrámos serem relevantes e estarem aumentados no soro de hemodialisados com membranas de baixo fluxo, contam-se a beta-2-microglobulina (2-M) e algumas citoquinas, com ação estimuladora das linhagens celulares envolvidas na remodelação óssea. Demonstrámos igualmente uma correlação positiva dos níveis séricos de 2-M com os níveis séricos da osteocalcina, da isoenzima óssea da fosfatase alcalina (marcadores da formação óssea) e com os níveis séricos da piridinolina (marcador da reabsorção óssea). Os níveis séricos de 2-M correlacionaram-se ainda, de forma negativa, com o volume osteoide (matriz óssea não calcificada). Nestes doentes hemodialisados, demonstrámos a presença de níveis séricos aumentados da interleucina-1, do antagonista do recetor da interleucina-1, da interleucina-6 e do recetor solúvel da interleucina-6. Salientamos as relações inversas que observámos, por um lado entre os níveis de antagonista do recetor da interleucina-1 e a superfície osteoblástica, e por outro lado entre o rácio do recetor da interleucina-6 / interleucina-6 (IL6-r/IL6) e a superfície osteoclástica. De acordo com estes nossos resultados originais, entendemos que a interferência nos níveis circulantes e na ativação local destes mediadores poderá justificar, em grande parte, o aumento da prevalência de doença óssea adinâmica, descrita por nós e por outros grupos. Evidenciámos uma elevadíssima prevalência de doença adinâmica (>50% dos doentes), numa população de hemodialisados sem exposição prévia ao alumínio, tratados de acordo com os K/DOQI “guidelines” e que ao longo de um ano mantiveram níveis séricos de cálcio e de fósforo controlados. Consequentemente, os doentes tratados de forma otimizada apresentaram uma prevalência surpreendentemente elevada de doença adinâmica. Os nossos resultados (classificados com o grau de evidência máxima pelos peritos KDIGO) contribuíram para dar suporte à grande diferença nos guidelines K/DOQI (2003) e KDIGO (2009) no que respeita aos valores alvo da PTH. Estamos conscientes que de que o facto de termos uma percentagem tão elevada de doença óssea adinâmica nas nossas populações de hemodialisados, bem como a demonstração de que alguns doentes com valores de PTH intacta (2ª geração) de cerca de 600 pg/ml tinham doença óssea adinâmica, condicionaram os novos objetivos KDIGO para a PTH. Os nossos resultados suportam, em nossa opinião, a adequação e vantagem da utilização dos critérios da KDIGO em vez dos KDOQI. Tendo em conta que os primeiros definem objetivos para a PTH entre 2 e 9 vezes o limite superior do normal e não se comprometem com valores alvo absolutos e rígidos (definidos previamente nos KDOQI entre 150 e 300 pg/mL), esta nova abordagem parece-nos mais correta.Na nossa investigação clínica, caracterizámos ainda a população hemodialisada portuguesa no que respeita aos níveis séricos de calcidiol, identificando a população com suficiência, insuficiência ou deficiência em vitamina D3. Documentámos uma acentuada prevalência de insuficiência e mesmo de deficiência nesta vitamina, numa vasta população de hemodialisados, a qual, muito provavelmente, reflete de forma fidedigna, o que se pode observar na restante população de doentes portugueses IRC em estádio 5d (em diálise). Descrevemos, pela primeira vez em doentes hemodialisados, uma associação entre deficiência em calcidiol e a presença de fatores de risco cardiovascular (que têm sido identificados nos doentes urémicos). A nossa investigação conduziu-nos a resultados originais, ao identificar os níveis baixos de 25(OH)vitamina D3 como um provável fator de risco cardiovascular em hemodialisados, visto que a deficiência nesta vitamina se associou, de forma muito significativa, ao aumento da prevalência de calcificações vasculares, a inflamação, a pressão de pulso mais elevada, a hipertrofia ventricular esquerda, a insuficiência cardíaca e a níveis séricos aumentados de “BNP-Brain natriuretic peptide”. Finalmente, numa avaliação prospetiva, de intervenção terapêutica, corrigimos a insuficiência ou deficiência em 25(OH)vitamina D3 e demonstrámos que essa correção se associou a uma redução dos fatores de risco cardiovascular. Esta última intervenção foi totalmente inovadora, visto ser a primeira avaliação prospetiva da evolução dos fatores de risco cardiovasculares, em função da suplementação com vitamina D nativa, em doentes hemodialisados. Em resumo, pensamos que os resultados das nossas investigações, acima sumarizadas e apresentadas ao longo dos diversos capítulos desta dissertação,contribuiram para uma nova perspetiva da osteodistrofia renal e para recolocar o foco da atenção dos nefrologistas no tecido ósseo e no eixo paratormona – vitamina D – remodelação óssea. Este eixo surje claramente envolvido em múltiplos processos fisiopatológicos, que suportam a elevada morbilidade e mortalidade (nomeadamente de causa cardiovascular) observada nos doentes urémicos.---------ABSTRACT: The results of our research, presented throughout this thesis, contributed towards the optimisation of the invasive and non-invasive diagnosis of renal osteodystrophy. They have also highlighted the importance, to the clinical and histological expression of the ODR, of some specific characteristics of the haemodialysis population, including: the use of biocompatible high permeability haemodialysis membranes, the use of haemodiafiltration techniques with convection enhancement, as well as the limitations of biochemical markers of bone turnover or native vitamin D insufficiency/deficiency (along with the supplementation results of this vitamin). New bone formation and resorption markers, which were validated by comparison with the results of bone histomorphometry, have been tested for the first time on haemodialysis patients.As a whole, and in an integrated approach, our research enabled us to: - Show the decrease of the PTH/PTHrP receptor expression in cartilage growth, used on an IRC animal model, which explains, to some extent, not only the delayed growth observed in this pathology, but also the slow response to PTH. - Point out the advantages of the determination of bone isoform of alkaline phosphatase, in relation to the total alkaline phosphatase, in the differential diagnosis between low and high-bone turnover.- Use pyridinoline and deoxypyridinoline in the diagnosis of bone resorption for the first time on haemodialysis patients. This was the first specific serum market of the osteoclastic activity, which was successfully used on anuric patients undergoing haemodialysis treatment. We also observed an excellent correlation of these biochemical markers with the osteoclastic surface and the number of osteoclasts/mm2. - Demonstrate the sharp limitations of other markers of bone formation and resorption (namely osteocalcin, carboxyterminal propeptide of type I-PICP procollagen and telopeptide of type I-ICTP collagen) based on correlations between these markers’ serum or plasma assays and bone biopsy with histomorphometric assessment.-Show the limitations induced by aluminium overload in the interpretation of serum levels of bone remodelling non-invasive markers.-Test the efficacy and the safety of the use of deferoxamine “microdoses” for treatment of aluminium overload among patients with high levels of serum aluminium. - Demonstrate that patients with chronic haemodialysis dialysers of polyacrylonitrile (high permeability membranes) show a lower osteoblastic and osteoclastic activation than those undergoing dialysis with cuprofan membranes (low permeability), being the iPTH levels similar in both groups of patients. These findings point towards a lower activation of bone remodelling when using more biocompatible dialysis membranes and/or of higher permeability, which may relate to the ultrafiltration of cell activation mediators or to the lower activation of the stimulating mechanisms of bone remodelling, regarding the membranes. Beta-2-microglobulin (2-M) and some cytokines that play a role/participate in bone remodelling are among the bone remodelling mediators, which we demonstrated to be relevant and to be increased in the serum of haemodialysis with low flow membranes. We also proved that there is a positive correlation of serum 2-M levels not only with serum osteocalcin levels, of the bone isoenzyme of alkaline phosphatase (bone forming markers), but also with levels of serum pyridinoline (bone resorption marker).Serum 2-M levels correlate negatively with the volume of osteoid (uncalcified bone matrix). We also demonstrated the presence of elevated serum levels of interleukin-1,interleukin-1 receptor antagonist, interleukin-6 and soluble interleukin-6 receptor in haemodialysis patients. We stress the inverse relationship which we observed on one hand between the interleukin-1 receptor antagonist levels and the osteoblastic surface and on the other between the ratio of interleukin-6 receptor / interleukin-6 (IL6-r/IL6) and the osteoblastic surface. According to these unique findings, we believe that the interference in the circulating levels and in the local activation of these mediators may partly explain the rising prevalence of adynamic bone disease. A high prevalence of adynamic disease has also been observed in a haemodialysis population (>50% of patients) with no previous exposure to aluminium. The patients were treated according to K/DOQI guidelines and maintained controlled serum calcium and phosphorus levels over one year. As a result, the patients who received optimised treatment showed a surprisingly high prevalence of adynamic disease. Our results, which were ranked with the highest degree of evidence by KDIGO experts, contributed to the great difference regarding the target values of PTH in the K/DOQI (2003) and KDIGO (2009) guidelines. We are aware that the finding of such a high percentage of adynamic bone disease in our haemodialysis population, as well as the evidence that some patients with intact PTH values (2nd generation) of 600 pg/ml suffered from adynamic bone disease, have hindered, the new KDIGO objectives to PTH.In our opinion, our results support the suitability and the advantage of using KDIGO criteria instead of KDOQI. This seems to be the right approach when taking into consideration that KDIGO sets objectives to PTH between 2 and 9 times the normal upper limit and does not compromise with the rigid and absolute target values (between 150 and 300 pg/mL) previously defined by KDOQI. In our clinical research, the Portuguese haemodialysis population was characterised in terms of serum clacidiol levels and identified as having vitamin D3 sufficiency, insufficiency or deficiency. It was also recorded the prevalence of severe vitamin D3 insufficiency and even deficiency in a large haemodialysis population, which most likely provides a reliable picture of the rest of the population in IRC Portuguese patients with 5d stage (undergoing dialysis). We described for the first time in aemosialysis patients an association between calcidiol deficiency and the presence of ardiovascular risk factors, (which have been identified on uraemic patients).Our research led us to unique findings by having identified the low levels of 25(OH) vitamin D3 as a likely cardiovascular risk factor in patients undergoing haemodialysis treatment, given that deficiency in this vitamin has been significantly associated not only with a rise in the prevalence of vascular calcifications, but also inflammation, left ventricular hypertrophy, high pulse pressure and high serum BNPBrain natriuretic peptide levels. Finally, based on a prospective assessment of therapeutic intervention, 25(OH)vitamin D3 insufficiency or deficiency was corrected and we were able to demonstrate that this same correction was associated with a reduction in cardiovascular risk factors. This was a forward-looking intervention regarding the supplementation of native vitamin D in haemodialysis patients, since it was the first prospective assessment of the evolution of cardiovascular risk factors. In short, the results of our research, summarised above and presented throughout the various chapters of this thesis, contributed towards a new perspective of the renal osteodystrophy and also to draw the nephrologists’ attention to the bone tissue and to the axis PTH – vitamin D – bone remodelling. This axis appears clearly involved in multiple physiopathological processes, which support the high morbidity and mortality rate, (particularly of cardiovascular causes), observed in uraemic patients.

Empirical models for quantification of machining damage in composite materials

Dissertação para obtenção do Grau de Doutor em Engenharia Mecânica

Mastodonte em depósitos marinhos da Praia do Penedo (Portugal)

O achado de um dente de mastodonte, cf. Tetralophodon longirostris, em depósitos marinhos expostos na praia de Penedo Norte, na Península de Setúbal, permitiu datação rigorosa. Provém da camada 8 do corte, parte basal da sequência deposicional T1; data do início do Tortoniano, ca. de 11.6 Ma, com base em foraminíferos planctónicos (zona N14) e em 87Sr/86Sr e K/Ar. O dente de mastodonte parece pertencer a Tetralophodon longirostris, espécie conhecida em Portugal em depósitos continentais da primeira parte do Miocénico superior.

Osteoclast activity in ankylosing spondylitis patients before and after TNF-blocking therapy

Ankylosing spondylitis (AS) is a chronic inflammatory rheumatic disease of the axial skeleton. The major outcome of this disease is defined by new bone formation, commonly observed in the ligaments of the intervertebral joints, that can lead to the formation of bony spurs, known as syndesmophytes. Previous studies have shown that serum levels of TNF, IL-6 and IL-17 are increased in AS patients and may be implicated in the development of secondary osteoporosis, since these cytokines are able to induce osteoclast (OC) differentiation and, therefore, bone resorption. In this work we aimed to assess the effects of TNF-blocking therapy in the systemic inflammatory environment of AS patients with active disease as well as in OC differentiation and activity. To accomplish this objective, we cultured circulating monocytes from AS patients, before and after therapy, under osteoclastogenic conditions and we performed two functional assays (TRAP staining and resorption pit assay) and analyzed the expression of osteoclast specific genes. We have shown that AS patients with active disease have increased levels of pro-inflammatory cytokines when compared with healthy subjects. We also found that IL-17, TGF-β and osteoprotegerin are decreased after TNF-blocking therapy. Interestingly, we also observed that after TNF-blocking therapy the expression of some genes is favoring osteoclastogenesis and that differentiated OCs have increased resorption activity. These results suggest that in active AS there may be an uncoupling between inflammation and OC activity that is reset by TNF-blocking therapy.

Evolution of Teeth and Quadrate in Non-avian Theropoda (Dinosauria: Saurischia), with the Description of Torvosaurus Remains from Portugal

Theropods form a highly successful and morphologically diversified group of dinosaurs that gave rise to birds. They include most, if not all, carnivorous dinosaurs, yet many theropod clades were secondarily adapted to piscivory, omnivory and herbivory, and theropods show a large array of skull and dentition morphologies. This work aims to investigate aspects of the evolution of theropod dinosaurs by analyzing in detail both the anatomy and ontogeny of teeth and quadrates in non-avian theropods, and by studying embryonic and adult material of a new species of theropod. A standardized list of terms and notations for each anatomical entity of the tooth, quadrate, and maxilla is here proposed with the goal of facilitating descriptions of these important cranial and dental elements. The distribution of thirty dental characters among 113 theropod taxa is investigated, and a list of diagnostic dental characters is proposed. As an example, four isolated theropod teeth from the Lourinhã Formation (Kimmeridgian‒Tithonian) of Portugal are described and identified based on a cladistic analysis performed on a data matrix of 141 dentition-based characters coded in 60 taxa. Two shed teeth are referred to an abelisaurid, providing the first record of Abelisauridae in the Jurassic of Laurasia and the one of the oldest records of this clade in the world, suggesting a possible radiation of Abelisauridae in Europe well before the Upper Cretaceous. The consensus tree resulting from this phylogenetic analysis, the most extensive on theropod teeth, indicates that theropod teeth provide reliable data for identification at approximately family level, and this method will help identifying theropod teeth with more confidence. A detailed description of the dentition of Megalosauridae is also provided, and a discriminant analysis performed on a dataset of numerical data collected on the teeth of 62 theropod taxa reveals that megalosaurid teeth are hardly distinguishable from other theropod clades with ziphodont dentition. This study highlights the importance of detailing anatomical descriptions and providing additional morphometric data on teeth with the purpose of helping to identify isolated theropod teeth. In order to evaluate the phylogenetic potential and investigate the evolutionary transformations of the quadrate, a phylogenetic morphometric analysis as well as a cladistic analysis using 98 discrete quadrate related characters were conducted. The quadrate morphology by its own provides a wealth of data with strong phylogenetic signal, and the phylogenetic morphometric analysis reveals two main morphotypes of the mandibular articulation of the quadrate linked to function. As an example, six isolated quadrates from the Kem Kem beds (Cenomanian) of Morocco are determined to be from juvenile and adult individuals of Spinosaurinae based on phylogenetic, morphometric, and phylogenetic morphometric analyses. Morphofunctional analysis of the spinosaurid mandibular articulation has shown that the posterior parts of the two mandibular rami displaced laterally when the jaw was depressed due to a mediolaterally oriented intercondylar sulcus of the quadrate. Such lateral movement of the mandibular ramus was possible due to a movable mandibular symphysis in spinosaurids, allowing the pharynx to be widened. A new species of theropod from the Lourinhã Formation of Portugal, Torvosaurus gurneyi, is erected based on a right maxilla and an incomplete caudal centrum. This taxon supports the mechanism of vicariance that occurred in the Iberian Meseta during the Late Jurassic when the proto-Atlantic was already well formed. A theropod clutch containing several crushed eggs and embryonic material is also assigned to this new species of Torvosaurus. Investigation on the maxilla ontogeny in basal tetanurans reveals that crown denticles, elongation of the anterior ramus, and fusion of interdental plates appear at a posthatchling stage. On the other hand, maxillary pneumaticity is already present at an embryonic stage in non-avian theropods.

Osteoclastogenesis, inflammatory cytokines and biomarkers of bone metabolism in psoriatic arthritis

RESUMO:A artrite psoriática (AP) é uma doença inflamatória crónica caracterizada por várias manifestações nas articulações, nas enteses e na pele. A formação de novo osso após inflamação nas enteses é um dos aspetos mais intrigantes desta doença. Os mecanismos celulares e moleculares deste processo ainda não são completamente conhecidos. Este estudo tem como objetivo compreender melhor os mecanismos subjacentes à formação e reabsorção óssea, bem como o efeito de anti-inflamatórios não esteroides (AINEs) nestes processos. Para atingir este objetivo foram quantificados biomarcadores do metabolismo ósseo e citocinas inflamatórias em doentes AP, antes e após terapêutica com AINEs. Os biomarcadores selecionados foram marcadores de remodelação óssea como CTX-I e P1NP, fatores de diferenciação e ativação de osteoclastos como o RANKL e a OPG, inibidores da via de sinalização Wnt, nomeadamente o DKK-1 e a SOST e ainda citocinas pro-inflamatórias como a IL-22 e a IL-23 e a prostaglandina PGE2. Neste contexto foram também estabelecidas culturas celulares de monócitos, isoladas de doentes AP e de controlos saudáveis. Os monócitos foram cultivados in vitro em condições não estimuladas e estimuladas e realizados dois ensaios funcionais: coloração com TRAP e ensaio de reabsorção. Foi observada uma diminuição nos níveis séricos de CTX-I e OPG em doentes AP em relação aos controlos. De igual forma os níveis séricos de SOST encontram-se significativamente mais baixos, em comparação com os controlos saudáveis. Estes valores de SOST são semelhantes aos dos doentes com espondilite anquilosante (EA), documentados anteriormente. Os ensaios com osteoclastos confirmaram a necessidade da presença de RANKL para estimulação da osteoclastogénese e que o celecoxib parece ter um papel inibitório neste processo. Os resultados obtidos sugerem que a população de doentes com AP analisados têm baixos níveis de reabsorção óssea e alguma atividade na formação óssea. --------------------------- ABSTRACT: Psoriatic arthritis (PsA) is a chronic inflammatory disease characterized by several manifestations involving the joints, enthesis and the skin. New bone formation after inflammation at enthesis site has been one of the most intriguing aspects of the disease. Cellular and molecular mechanisms in this process are still not completely understood. This study aims to understand better the mechanisms underlying bone formation and resorption and the effect of non-steroid anti-inflammatory drugs (NSAIDs) in these processes. To access that, biomarkers of bone metabolism and inflammatory cytokines were measured in PsA patients’ serum before and after NSAID therapy. These selected biomarkers were bone turnover markers such as CTX-I and P1NP, osteoclast differentiation and activation factors RANKL and OPG, Wnt pathway inhibitors DKK-1 and SOST and pro-inflammatory cytokines IL-22, IL-23 and prostaglandin PGE2. In this context monocyte cell culture was also established after PBMC isolation from PsA patients and healthy controls. Monocytes were cultured in vitro under unstimulated and stimulated conditions and two functional assays were performed: TRAP staining and resorption pit assay. It was demonstrated that CTX-I and OPG serum levels in PsA patients were lower than controls. SOST levels were extremely decreased in comparison with controls, resembling the ankylosing spondylitis patients results already documented. Osteoclast assays confirmed the need of RANKL in stimulating osteoclastogenesis and that celecoxib seems to have an inhibitor role in this process. The results obtained suggest that PsA patient population analyzed in this study have low bone resorption levels and some bone formation activity.