A arqueologia urbana em Lisboa e a Praxis empresarial

O presente relatório resultou do estágio efectuado na Era-Arqueologia S.A., no âmbito da componente não lectiva do Mestrado em Arqueologia. O seu objectivo foi dar um contributo para a compreensão do estado actual da Arqueologia Urbana e Empresarial especificamente na cidade de Lisboa, através da experiencia e informação obtidas durante a realização do estágio na empresa.

Arqueologia, património e museus na Câmara Municipal de Almeida

Este relatório apresenta as atividades desenvolvidas ao longo do estágio curricular na Câmara Municipal de Almeida, como componente não letiva de formação no Mestrado de Arqueologia da Faculdade de Ciências Sociais e Humanas da Universidade Nova de Lisboa. O estágio teve como principal objetivo a elaboração da carta arqueológica do território das freguesias da Amoreira, Parada e Cabreira, uma parcela do concelho de Almeida. A carta foi elaborada a partir de evidências arqueológicas identificadas em prospeções, de análises da toponímia, da topografia, cartografia, fotografias aéreas e fontes orais do território almeidense. Paralelamente, e no quadro do Museu Histórico-Militar de Almeida, realizou-se um trabalho de organização da reserva arqueológica do município, através da inventariação de todo o espólio arqueológico existente e a elaboração de uma proposta preliminar de conservação preventiva do depósito museal, criando deste modo condições para a receção de novas coleções arqueológicas.

Povoamento e paisagens no Vale Superior do Rio Terva, Boticas: projecto de investigação plurianual em arqueologia (PoPaTERVA 2013-2016): trabalhos arqueológicos no povoado das Batocas: relatório 2013-2014

O relatório que se apresenta respeita aos trabalhos arqueológicos desenvolvidos entre 2013 e 2014, inscritos no Projeto de Investigação Plurianual de Arqueologia (adiante PIPA) “Povoamento e Paisagens no Vale Superior do Rio Terva, Boticas – PoPaTERVA 2013-2016”, oportunamente aprovado pela Direção Geral do Património Cultural (DGPC: ofício n.º 2013/1 (169) CS: 875795 informação n.º 1704/DBC/2013). O projeto Povoamento e Paisagens no Vale Superior do Rio Terva, Boticas/ PoPaTERVA surge na sequência da conclusão do projeto de Conservação, Estudo, Valorização e Divulgação do Complexo Mineiro Antigo do Vale Superior do Rio Terva, Boticas, concebido em 2006 pela UAUM e executado entre 2010 e 2012 no âmbito de protocolo estabelecido com a Câmara Municipal de Boticas. Desta primeira ação de investigação resultou a classificação do Complexo Mineiro Antigo do Vale Superior do Rio Terva como Sítio de Interesse Público, promulgado pela Portaria n.º 386/2013 (DR, 2.º Série, n.º 115 de 18 de Junho de 2013 – ver Apêndice 7.1.2).

Povoamento e paisagens no Vale Superior do Rio Terva, Boticas: projecto de investigação plurianual em arqueologia (PoPaTERVA 2013-2016): trabalhos arqueológicos no Castro de Sapelos: relatório 2014

O presente relatório enquadra-se na execução do Projeto PoPaTERVA 2013-2016, um projeto PIPA aprovado pela DGPC em 2013 (oficio nº 06922, de 04-07-13. Ref. 2013/1 (169) CS 875795). Para o corrente ano de 2014 pretendemos dar continuidade às investigações decorrentes da implementação do projeto referido anteriormente, iniciando assim o estudo em pormenor do Castro de Sapelos. Os trabalhos arqueológicos foram iniciados a 1 de Julho e terminaram no mês de Dezembro, contaram com a participação de 4 jovens voluntários do programa municipal Boticas Mexe.

Entrevista com Maria Manuela dos Reis Martins: reflexões sobre a Arqueologia Urbana, a paisagem e o território

"Entrevista concedida a Érica Cristhyane Morais da Silva"

Análise de fragmentos arqueológicos: um diálogo entre a Química, Biologia e Arqueologia

Dissertação de mestrado em Técnicas de Caracterização e Análise Química

Protistas "incerta sedis" de ofídios do Brasil: Toddia França, 1912 e Pirhemocyton Chatton & Blanc, 1914: estudo comparativo

Dentre 683 serpentes procedentes de diferentes pontos do Brasil, 16 (2,4%) apresentaram em seu sangue (em glóbulos vermelhos maturos e imaturos) Toddia ou Pirhemocyton. Denominamos provisoriamente Toddia os parasitos encontrados em Bothrops moojeni, B. pradoi, B. jararaca e Chironius flavolineatus e Pirhemocyton os encontrados em B. alternatus; fornecemos a primeira referência nestes hospedeiros. Estes parasitos foram estudados comparativamente com o objetivo de estabelecermos a extensão de suas afinidades. Com Toddia de B. moojeni realizamos técnica citoquímica para caracterização de ácidos nucleicos e encontramos positividade apenas para DNA. As maiores afinidades entre os parasitos estudados residiam nas características dos corpúsculos cromáticos e alterações celulares que determinam; observarmos quase total identidade nas maneiras como os parasitos da mesma espécie de serpente se apresentaram. Constatamos a coexistência de inclusões globóides, cristalóides e formas intermediárias associada aos parasitos de B. pradoi e B. alternatus; em C. flavolineatus encotnramos além dos cristais, raríssimas formas intermediárias entre estes e globóides. Afinidades entre Toddia e Pirhemocyton abrangendo o tipo de inclusão contrariam as descrições originais, tornando pouco válida esta separação genérica. Discutimos também os fundamentos da criação das espécies e a possível natureza virótica destes parasitos.

The viral nature of Toddia França, 1912

Toddia França, 1912 under the light microscope occurs as inclusion corpuscles in the cytoplasm of erythrocytes of cold-blooded vertebrates sometimes accompanied by crystalloid bodies. Its position among the protozoans or the viruses has been discussed by some authors, but remained unclear. To elucidate this problem we studied Toddia from a Brazilian frog (Leptodactylus ocellatus) by electron microscopy. In the cytoplasm of the infected cells we found no protozoan, but rather virus-like particles often hexagonal in outline, averaging 195 nm excluding their two involving membranes, and presenting a central area of variable electron density. Particles at different stages of development were generally found around or on area lighter density than the cytoplasm. which resembled a virus synthesis site. At high magnification, the nuclear or cytoplasmic crystals allied to Toddia resembled the crystalline lattice of the inclusion bodies associated with the polyhedrosis viruses and poxviruses from insects, of the capsules of granulosis viruses and of other protein crystals in ultrathin sections. Cytochemical tests in Toddia corpuscles displayed exclusively the presence of deoxyribonucleic acid. These findings indicate that Toddia is not a protozoan and demonstrate that it is in all probability a viral inclusion corpuscle. Taking into account the nucleic acid type found in its structure (DNA) and the hexagonal shape usually shown in ultrathin sections by its component particles, which have a cytoplasmic site of synthesis and assembly, we tentatively relate Toddia with the so-called "Icosahedral Cytoplasmic Deoxyriboviruses". We believe that the present paper gives the first report of virus-like particles in L. ocellatus.

The microps group of Lutzomyia França with descriptions of two new species from South America (Diptera: Psychodidae: Phlebotominae)

Six species of phlebotomine sand flies in the genus Lutzomyia França from South America are included in the newly-created species group microps. References and illustrations of the species are given, including descriptions of two new forms - L. nematoducta n.sp., male and female from northern Brazil, and l. preclara n.sp. male from Colombia and Peru. The males in the species group microps are keyed.

Recerca paleontològica als jaciments maastrichtians continentals de l'àrea de Fumanya (Alt Berguedà)

Memòria de la recerca realitzada a Vallcebre durant el 2006. S’ha estudiat el registre fòssil de l'àrea del sinclinal d’aquesta població de vertebrats i paleobotànic, concretament dels materials maastrichtians d'origen continental que hi afloren. S'han realitzat excavacions per recuperar restes òssies de vertebrats (per exemple dinosaures sauròpodes i cocodrils eosuquis) i cartografies d'icnites i rastres de titanosaure i de restes vegetals als megajaciments de Fumanya sud i Mina Esquirol. També s'ha avançat en l'estudi de postes de titanosaure excavades en campanyes d'anys anteriors. El treball realitzat està permeten acumular dades que seran de gran utilitat i rellevança científica per entendre com vivien els darrers dinosaures pirinencs.La recerca del projecte s'està realitzant en col•laboració amb l'Institut Català de Paleontologia, el Departament d'Estratigrafia de la Universitat Autònoma de Barcelona, el Departament d'Estratigrafia, Paleontologia i Geociències Marines de la Universitat de Barcelona i el Departament de Geociències de la Universitat de Rennes (França).

Cosa: arqueologia de un enclave comercial mediterráneo. Campaña de 2006

En el marco del proyecto “La ciutat romana de Cosa: arqueologia d’un enclau comercial mediterrani” , autorizado y apoyado por la Soprintendenza Archeologica por la Toscana, entre los dias 4 y 22 de septiembre de 2006 se ha realizado la segunda campaña de intervenciones arqueológicas en la ciudad romana de Cosa (Ansedonia, prov. Grosseto, Itàlia), colonia latina fundada en el 273 aC a unos 120 km. al norte de Roma. De acuerdo a los resultados obtenidos en la campanya del 2005 (localización/verificación de los límites precisos de la ínsula O-P/4-5 mediante la aplicación de técnicas de prospección geofísica completadas con la limpieza, registro y documentación arqueológica de las estructuras localizadas ) los trabajos del 2006 se han orientado hacia la identificación de la organización interna de la dicha ínsula tomando como referente el criptopórtico situado en el extremo N.E., el cual parece constituir el límite de una estructura singular (privada o pública ) estratégicamente ubicada en relación al fórum i a la Via Sacra. El trabajo de campo ha consistido en un intenso decapage con la finalidad de delimitar unidades de habitación complejas funcionalmente definidas y así la articulación existente entre ellas; en este sentido se ha podido documentar evidencias del espacio porticado superpuesto al criptopórtico así como, paralelamente a la calle 5 y en dirección a la Via Sacra, parte de habitaciones algunas de las cuales conservaban restos del pavimiento original, en un caso de mosaico. Paralelamente, se ha realizado el análisis en laboratorio de los materiales recuperados los cuales, aún procediendo de nivel superficial, empiezan a proporcionar datos sobre los diferentes momentos de ocupación de la zona, básicamente tardorepublicanos y augustales.

An 40Ar/39Ar, Rb/Sr, and stable isotope study of micas in low-grade fold-and-thrust belt: An example from the Swiss Helvetic Alps

White micas in carbonate-rich tectonites and a few other rock types of large thrusts in the Swiss Helvetic fold-and-thrust belt have been analyzed by Ar-40/Ar-39 and Rb/Sr techniques to better constrain the timing of Alpine deformation for this region. Incremental Ar-40/Ar-39 heating experiments of 25 weakly metamorphosed (anchizone to low greenschist) samples yield plateau and staircase spectra. We interpret most of the staircase release spectra result from variable mixtures of syntectonic (neoformed) and detrital micas. The range in dates obtained within individual spectra depends primarily on the duration of mica nucleation and growth, and relative proportions of neoformed and detrital mica. Rb/Sr analyses of 12 samples yield dates of ca. 10-39 Ma (excluding one anomalously young sample). These dates are slightly younger than the Ar-40/Ar-39 total gas dates obtained for the same samples. The Rb/ Sr dates were calculated using initial Sr-87/Sr-86 ratios obtained from the carbonate-dominated host rocks, which are higher than normal Mesozoic carbonate values due to exchange with fluids of higher Sr-87/Sr-86 ratios (and lower O-18/O-16 ratios). Model dates calculated using Sr-87/Sr-86 values typical of Mesozoic marine carbonates more closely approximate the Ar-40/Ar-39 total gas dates for most of the samples. The similarities of Rb/Sr and Ar-40/Ar-39 total gas dates are consistent with limited amounts of detrital mica in the samples. The delta(18)O values range from 24-15%. (VSMOW) for 2-6 mum micas and 27-16parts per thousand for the carbonate host rocks. The carbonate values are significantly lower than their protolith values due to localized fluid-rock interaction and fluid flow along most thrust surfaces. Although most calcite-mica pairs are not in oxygen isotope equilibrium at temperatures of ca. 200-400 degreesC, their isotopic fractionations are indicative of either 1) partial exchange between the minerals and a common external fluid, or 2) growth or isotopic exchange of the mica with the carbonate after the carbonate had isotopically exchanged with an external fluid. The geological significance of these results is not easily or uniquely determined, and exemplifies the difficulties inherent in dating very fine-grained micas of highly deformed tectonites in low-grade metamorphic terranes. Two generalizations can be made regarding the dates obtained from the Helvetic thrusts: 1) samples from the two highest thrusts (Mt. Gond and Sublage) have all of their Ar-40/Ar-39 steps above 20 Ma, and 2) most samples from the deepest Helvetic thrusts have steps (often accounting for more than 80% of Ar-39 release) between 15 and 25 Ma. These dates are consistent with the order of thrusting in the foreland-imbricating system and increase proportions of neoformed to detrital mica in the more metamorphosed hinterland and deeply buried portions of the nappe pile. Individual thrusts accommodated the majority of their displacement during their initial incorporation into the foreland-imbricating system, and some thrusts remained active or were reactivated down to 15 Ma.

The Teggiolo zone: a key to the Helvetic-Penninic connection (stratigraphy and tectonics in the Val Bavona, Ticino, Central Alps)

The Teggiolo zone is the sedimentary cover of the Antigorio nappe, one of the lowest tectonic units of the Penninic Central Alps. Detailed mapping, stratigraphic and structural analyses, and comparisons with less metamorphic series in several well-studied domains of the Alps, provide a new stratigraphic interpretation. The Teggiolo zone is comprised of several sedimentary cycles, separated by erosive surfaces and large stratigraphic gaps, which cover the time span from Triassic to Eocene. At Mid-Jurassic times it appears as an uplifted, partially emergent block, marking the southern limit of the main Helvetic basin (the Limiting South-Helvetic Rise LSHR). The main mass of the Teggiolo calcschists, whose base truncates the Triassic-Jurassic cycles and can erode the Antigorio basement, consists of fine-grained clastic sediments analogous to the deep-water flyschoid deposits of Late Cretaceous to Eocene age in the North-Penninic (or Valais s.l.) basins. Thus the Antigorio-Teggiolo domain occupies a crucial paleogeographic position, on the boundary between the Helvetic and Penninic realms: from Triassic to Early Cretaceous its affinity is with the Helvetic; at the end of Cretaceous it is incorporated into the North-Penninic basins. An unexpected result is the discovery of the important role played by complex formations of wildflysch type at the top of the Teggiolo zone. They contain blocks of various sizes. According to their nature, three different associations are distinguished that have specific vertical and lateral distributions. These blocks give clues to the existence of territories that have disappeared from the present-day level of observation and impose constraints on the kinematics of early folding and embryonic nappe emplacement. Tectonics produced several phases of superimposed folds and schistosities, more in the metasediments than in the gneissic basement. Older deformations that predate the amplification of the frontal hinge of the nappe generated the dominant schistosity and the km-wide Vanzèla isoclinal fold.

Modeling of in-situ crystallization processes in the Permian mafic layered intrusion of Mont Collon (Dent Blanche nappe, western Alps)

The Mont Collon mafic complex is one of the best preserved examples of the Early Permian magmatism in the Central Alps, related to the intra-continental collapse of the Variscan belt. It mostly consists (> 95 vol.%) of ol+hy-nonnative plagioclase-wehrlites, olivine- and cpx-gabbros with cumulitic structures, crosscut by acid dikes. Pegmatitic gabbros, troctolites and anorthosites outcrop locally. A well-preserved cumulative, sequence is exposed in the Dents de Bertol area (center of intrusion). PT-calculations indicate that this layered magma chamber emplaced at mid-crustal levels at about 0.5 GPa and 1100 degrees C. The Mont Collon cumulitic rocks record little magmatic differentiation, as illustrated by the restricted range of clinopyroxene mg-number (Mg#(cpx)=83-89). Whole-rock incompatible trace-element contents (e.g. Nb, Zr, Ba) vary largely and without correlation with major-element composition. These features are characteristic of an in-situ crystallization process with variable amounts of interstitial liquid L trapped between the cumulus mineral phases. LA-ICPMS measurements show that trace-element distribution in the latter is homogeneous, pointing to subsolidus re-equilibration between crystals and interstitial melts. A quantitative modeling based on Langmuir's in-situ crystallization equation successfully duplicated the REE concentrations in cumulitic minerals of all rock facies of the intrusion. The calculated amounts of interstitial liquid L vary between 0 and 35% for degrees of differentiation F of 0 to 20%, relative to the least evolved facies of the intrusion. L values are well correlated with the modal proportions of interstitial amphibole and whole-rock incompatible trace-element concentrations (e.g. Zr, Nb) of the tested samples. However, the in-situ crystallization model reaches its limitations with rock containing high modal content of REE-bearing minerals (i.e. zircon), such as pegmatitic gabbros. Dikes of anorthositic composition, locally crosscutting the layered lithologies, evidence that the Mont Collon rocks evolved in open system with mixing of intercumulus liquids of different origins and possibly contrasting compositions. The proposed model is not able to resolve these complex open systems, but migrating liquids could be partly responsible for the observed dispersion of points in some correlation diagrams. Absence of significant differentiation with recurrent lithologies in the cumulitic pile of Dents de Bertol points to an efficiently convective magma chamber, with possible periodic replenishment, (c) 2005 Elsevier B.V. All rights reserved.

Divergent and convergent margins in the north-western Alps - Confrontation to actualistic models

Divergent and convergent margins actualistic models are reviewed and applied to the history of the western Alps. Tethyan rifting history and geometry are analyzed: the northern European margin is considered as an upper plate whereas the southern Apulian margin is a lower plate; the Breche basin is regarded as the former break-away trough; the internal Brianconnais domain represents the northern rift shoulder whilst the more external domains are regarded as the infill of a complex rim basin locally affected by important extension (Valaisan and Vocontain trough). The Schistes lustres and ophiolites of the Tsate nappe are compared to an accretionary prism: the imbrication of this nappe elements is regarded as a direct consequence of the accretionary phenomena already active in early Cretaceous; the Gets/Simme complex could orginate from a more internal part of the accretionary prism. Some eclogitic basements represent the former Apulian margin substratum (Sesia) others (Mont-Rose) are interpreted as the former edge of the European margin. The history of the closing Tethyan domain is analyzed and the remaining problems concerning the cinematics, the presence/absence of a volcanic arc and the eoalpine metamorphism are discussed.