Tertiary evolution of the São Vicente and Setúbal submarine canyons, Southwest Portugal: insights from seismic stratigraphy

The Setúbal and São Vicente canyons are two major modern submarine canyons located in the southwest Iberian margin of Portugal. Although recognised as Pliocene to Quaternary features, their development during the Tertiary has not been fully understood up to date. A grid of 2D seismic data has been used to characterise the sedimentary deposits of the adjacent flanks to the submarine canyons. The relationship between the geological structure of the margin and the canyon's present location has been investigated. The interpretation of the main seismic units allowed the recognition of three generations of ravinements probably originated after middle Oligocene. Six units grouped in two distinctive seismic sequences have been identified and correlated with offshore stratigraphic data. Seismic Sequence 2 (SS2), the oldest, overlies Mesozoic and upper Eocene deformed units. Seismic Sequence I (SS1) is composed of four different seismic packages separated from SS2 by an erosional surface. The base of the studied sediment ridges is marked by an extensive erosional surface derived from a early/middle Oligocene relative sea-level fall. Deposition in the adjacent area to the actual canyons was reinitiated in late Oligocene in the form of transgressive and channel-fill deposits. A new depositional hiatus is recorded onshore during the Burdigalian, coincident with the unconformity separating SS1 and SS2. This can be correlated with the Arrábida unconformity and with the paroxysmal Burdigalian phase of the Betic domain. Presently, the Setúbal and São Vicente submarine canyons locally cut SS1 and SS2, forming distinctive channels from those recognised on the seismic data. On the upper shelf both dissect highly deformed areas subject to important erosion.

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, São Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

Pliocene-quaternary upwelling in the SoutheasternAtlantic may reflect changes in water mass production

Proceedings of tile 1" R.C.A.N.S. Congress, Lisboa, October 1992

Earth mortars constructive use on Neolithic domestic structures. Some case studies in Alentejo.

HMC08 - 1st Historical Mortars Conference: Characterization, Diagnosis, Conservation, Repair and Compatibility, LNEC, Lisbon, 24-26 September 2008

Earth building materials in pre-historic domestic architectures on the south of Portugal

HERITAGE 2008 - World Heritage and Sustainable Development. Barcelos: Green Lines Institute for Sustainable Development, Vol. 2, p. 571-579

Suicide study : a psychological autopsy

RESUMO: O'suicídio'é'atualmente'um'problema'de'saúde'pública.'Estimarse'que'um'milhão'de'pessoas' morra'anualmente'devido'ao'suicídio.'De'acordo'com'diversas'agências'e'organizações'estimar 'que'ocorram'entre'20'a'40'tentativas'de'suicídio'por'cada'suicídio'consumado.'Os'custos'associados'ao'suicídio,'quer'humanos'quer'económicos'são'enormes'e'estendemrse'à'família,'emprego,'economia'e'finanças.'Os'números'oficiais'do'suicídio'em'Portugal'indicam'uma'taxa ligeiramente'acima'dos'10'por' cada'100'000'habitantes'mas' comportando' regiões'onde' são'observadas' taxas' muito' elevadas,' como' no' Sudoeste' de' Portugal' onde' se' observam particularmente taxas 3'vezes'acima'da'média'nacional.' Investigámos' o' fenómeno' com' os' objetivos' de' validar' a' técnica' de' autópsia' psicológica' em' contexto' comunitário' nunca' realizado' em' Portugal,' e' dar' um' contributo' para' uma' compreensão'mais'alargada'deste'problema'de'saúde'pública,'especialmente'nesta'região'de' Odemira.' A' autópsia' psicológica' consiste' em' reunir' detalhadamente' informação' sobre' a'personalidade' e' vida' de' alguém' que' morreu' em' circunstâncias' equívocas' (por' suicídio,' homicídio' ou' acidente)'recorrendo'ainda'a'registos'e'documentação,'bem'como'procedendo'a entrevistas' com' familiares,' colegas' ou' amigos.' Foi' feita' uma' adaptação' de' uma' entrevista' semirestruturada' para' o' efeito.' Foram' recrutados' 2' grupos' de' participantes:' um' grupo' de familiares de pessoas que cometeram'suicídio'(n=30)'e'um'grupo'de'familiares'de'pessoas'que morreram de causas' naturais' (n=24).' O' estudo' decorreu' em' 3' momentos' com' sessões' de' apresentação' (i),' sessões' de' preparação' (ii)' e' entrevistas' para' recolha' de' informação' e'monitorização.'' Os' principais' resultados'mostram' que' existiram' dificuldades' na' obtenção' da' informação' a'partir' dos' entrevistados,' a'maioria' dos' suicidas' eram'homens' acima' dos' 40' anos' de' idade,' afetados' por' lesões' graves' ou' doenças' graves' ' no' período' adulto' embora' apresentassem'condições' válidas' para' trabalhar,' reformados,' vivendo' em' família,' com' traços' de'personalidade' amargurados,' tristes' ou' pessimistas,' com' escassas' atividades' nos' tempos' de' lazer,' sem' problemas' somáticos' significativos' ou' perturbações'mentais' que' comunicaram' a intenção de morrer previamente'e'provenientes'de'famílias'sem'dificuldades'económicas'ou'relações'familiares'desadequadas.' Tendo'em'conta'a'literatura,'algumas'das'características'parecem'ser'muito'particulares'desta'população.'Aparentemente'o'suicídio'poderá'ter'implicações'genéticas'que'deveriam'ser'tidas'em'conta'em'futuras'investigações.' A'integração'da'saúde'mental'nos'cuidados'de'saúde'primários'afigurarse'urgente'tendo'em' conta' que' a' escassez' de' profissionais' de' saúde'mental' é' enorme' numa' parte' do' país' onde'ocorre' o'maior'número'de' suicídios.'Mudar'de'modelo'e'reorganizar'os' serviços'de' forma'a' poder' dar' uma' resposta' ao' défice' de' tratamento' de' saúde' mental' e' ter' em' conta' os' determinantes'sociais'da'saúde'para'fazer'face'ao'isolamento'é'fundamental.' ---------------ABSTRACT: Suicide' is,'nowadays,' a'public'health'problem.'A'million'dies' annually'by' suicide'worldwide.' According'to'several'agencies'and'organizations'an'estimation'of'20'to'40'suicide'attempts'is advanced for each complete' suicide. Associated'costs'to'suicide,'both'human'and'economic,'are' huge' and' spread' on' family,' jobs,' economy,' and' finances.' Official' available' figures' for' suicide' in' Portugal' indicate' a' rate' slightly' over' 10' for' each' 100' 000' inhabitants,' but' with'regions'where'one' can' actually' find'extremely'high' rates,' like' for' instance' in' the'Southwest' part' of' the' country,' where' are' regularly' found' rates' 3' times' higher,' when' compared' to'national'average.'' We' have' investigated' the' phenomenon' aiming' to' validate' the' technique' of' psychological'autopsy' in' a' community' context' never' explored' before' in' Portugal' and' to' contribute' for' a' wider' understanding' of' this' public' health' problem,' especially' in' this' region' of' Odemira.' Psychological'autopsy'consists'into'a'detailed'gathering'of'information'about'the'personality'and' life' of' someone' died' in' equivocal' circumstances' (suicide,' homicide,' accident),' registries and other'documentation'as'well'as'interviews'with'family'members,'corworkers'and'friends.' An' adaptation' of' a' semirstructured' interview' was' made.' Two' groups' of' participants' were'recruited: a'group of'relatives'of'people'committing'suicide'(n=30),'and'a'group'of'relatives'of'people' whose' death' was' after' natural' causes' (n=24).' Study' was'made' in' 3'moments' with'presentation'sessions;'(i)'preparation'sessions;'(ii)'interviewing'data'collection'and'monitoring' iii).'' Main'results'showed'difficulties'to'obtain'information'from'interviewees,'most'suicides'were' from males over 40 years old, affected'by'serious'illness'or'severe'injury'in'adulthood'but'valid'to'work,'retired,'living'in'family,'with'bitterness,'sad'or'pessimistic'as'personality'traits,'with'few' leisure' activities,' without' significant' health' somatic' problems' or' mental' disorders,'communicating'intention'to'die'previously,'coming'from'families'with'no'indication'of'financial'distress'or'inadequate'family'relationship.' Taking'into'account'the'literature'it'looks'like'some'features'seem'to'be'quiet'particular'from'this'population.'Apparently'one'might'say'that'suicide'could'have'genetic'implications'which'further'research'should'account'in'the'future.' Integration' of'mental' health' into' primary' care' is' urgent' once' the' scarcity' of'mental' health' professionals' is' enormous' in' a' part' of' the' country' where' most' suicides' occur.' Scaling' up services must go in order'to'address'to'treatment'gap'and'social'determinants'of'health'should'be'taken'into'account'to'face'isolation.' Results' show' that' the' profile' of' the' suicidal' in' the' region' of' Odemira' is' particular' and'implications' of' genetics' should' be' taken' into' account.' Moreover' much' can' be' done' in'organization' of' services' in' the' region' where' we' performed' the' present' study' in' order' to'address'to'treatment'gap'for'mental'disorders'and'to'the'social'determinants'of'health.

The role of qualitative data and systems thinking in addressing service decline in market towns

Retail services are a main contributor to municipal budget and are an activity that affects perceived quality-of-life, especially for those with mobility difficulties (e.g. the elderly, low income citizens). However, there is evidence of a decline in some of the services market towns provide to their citizens. In market towns, this decline has been reported all over the western world, from North America to Australia. The aim of this research was to understand retail decline and enlighten on some ways of addressing this decline, using a case study, Thornbury, a small town in the Southwest of England. Data collected came from two participatory approaches: photo-surveys and multicriteria mapping. The interpretation of data came from using participants as analysts, but also, using systems thinking (systems diagramming and social trap theory) for theory building. This research moves away from mainstream economic and town planning perspectives by making use of different methods and concepts used in anthropology and visual sociology (photo-surveys), decision-making and ecological economics (multicriteria mapping and social trap theory). In sum, this research has experimented with different methods, out of their context, to analyse retail decline in a small town. This research developed a conceptual model for retail decline and identified the existence of conflicting goals and interests and their implications for retail decline, as well as causes for these. Most of the potential causes have had little attention in the literature. This research also identified that some of the measures commonly used for dealing with retail decline may be contributing to the causes of retail decline itself. Additionally, this research reviewed some of the measures that can be used to deal with retail decline, implications for policy-making and reflected on the use of the data collection and analysis methods in the context of small to medium towns.

Assessment of NDVI, land surface temperature and precipitation anomalies for drought monitoring in Bayankhongor province, Mongolia

During the last decade Mongolia’s region was characterized by a rapid increase of both severity and frequency of drought events, leading to pasture reduction. Drought monitoring and assessment plays an important role in the region’s early warning systems as a way to mitigate the negative impacts in social, economic and environmental sectors. Nowadays it is possible to access information related to the hydrologic cycle through remote sensing, which provides a continuous monitoring of variables over very large areas where the weather stations are sparse. The present thesis aimed to explore the possibility of using NDVI as a potential drought indicator by studying anomaly patterns and correlations with other two climate variables, LST and precipitation. The study covered the growing season (March to September) of a fifteen year period, between 2000 and 2014, for Bayankhongor province in southwest Mongolia. The datasets used were MODIS NDVI, LST and TRMM Precipitation, which processing and analysis was supported by QGIS software and Python programming language. Monthly anomaly correlations between NDVI-LST and NDVI-Precipitation were generated as well as temporal correlations for the growing season for known drought years (2001, 2002 and 2009). The results show that the three variables follow a seasonal pattern expected for a northern hemisphere region, with occurrence of the rainy season in the summer months. The values of both NDVI and precipitation are remarkably low while LST values are high, which is explained by the region’s climate and ecosystems. The NDVI average, generally, reached higher values with high precipitation values and low LST values. The year of 2001 was the driest year of the time-series, while 2003 was the wet year with healthier vegetation. Monthly correlations registered weak results with low significance, with exception of NDVI-LST and NDVI-Precipitation correlations for June, July and August of 2002. The temporal correlations for the growing season also revealed weak results. The overall relationship between the variables anomalies showed weak correlation results with low significance, which suggests that an accurate answer for predicting drought using the relation between NDVI, LST and Precipitation cannot be given. Additional research should take place in order to achieve more conclusive results. However the NDVI anomaly images show that NDVI is a suitable drought index for Bayankhongor province.