O contributo de uma estratégia de animação sociocultural na prevenção da depressão em idosos intitucionalizados

O envelhecimento faz parte do ciclo de vida de cada indivíduo e assume-se como um tema que preocupa a atualidade de Portugal e do mundo. Esta realidade provoca uma reflexão a respeito não só das infraestruturas e apoios existentes para a população idosa como ao próprio idoso, que pelas suas características, pela mudança de papéis e perdas que ocorrem nesta fase da vida, tornam-se pessoas mais vulneráveis, por vezes mais sós, sujeitos a depressões, isolamento e em situações extremas à exclusão social. Neste sentido, e com o objetivo de alterar mentalidades e comportamentos surge a ideia de desenvolver este trabalho que assenta essencialmente na perceção do impacto que as atividades de ASC (animação sociocultural) assumem na prevenção de quadros de sintomatologia depressiva em idosos institucionalizados. Assim sendo, este trabalho tem como objetivo primordial verificar se a realização de um conjunto diversificado de atividades de animação sociocultural contribuem efetivamente não só para o bem-estar, participação e aumento da qualidade de vida dos idosos, como contribuem essencialmente para a prevenção de quadros de sintomatologia depressiva. Assim, o presente projeto de intervenção tem como temática, “O Contributo de uma Estratégia de Animação Sociocultural na prevenção da Depressão em Idosos Institucionalizados”. O espaço eleito para o estudo e posteriormente para a intervenção é a Casa do Povo de Alagoa, uma IPSS de apoio a idosos que conta atualmente com um número aproximado de 65 clientes nas respetivas valências, Serviço de Apoio Domiciliário, Centro de Dia e ERPI (Estrutura Residencial para Pessoas Idosas) que se situa na Freguesia de Alagoa, Distrito de Portalegre. Trata-se portanto, de um estudo de caso de base mista (qualitativa e quantitativa), cingindo-se a uma amostra de 30 clientes institucionalizados, nas respetivas valências de Centro de Dia e ERPI. A metodologia selecionada para o estudo será o recurso a diversas técnicas tais como: o Questionário, MMS (Mini Mental State Examination) e a GDS (Escala de Depressão Geriátrica).

(Table 2) Species composition of agglutinated foraminifers from the abyssal zone of the Pacific Ocean

The quantitative study of distribution and taxonomic composition of recent living and dead (without plasma) benthic foraminifers revealed three foraminiferal assemblages in bottom sediments of the Pacific Ocean at depths of 3350 to 4981 m. The assemblage dominated by epibenthic Lagenammina difflugiformis, Reophax dentaliniformis, and Saccorhiza ramose occupies slopes of underwater hills. The assemblage with a high share of infaunal Cribrostomoides subglobosum, C. nitidum, and Ammobaculites agglutinans is registered on an abyssal plateau. The assemblage with a significant proportion of large Astrorhiza and Reophax species, which are characterized by active way of life, populates gentle slopes and narrow depressions with potentially strong bottom currents.

(Table 2) Radiocarbon contents of TOC and alkenone samples

Radiocarbon age relationships between co-occurring planktic foraminifera, alkenones, and total organic carbon in sediments from the continental margins of southern Chile, northwest Africa, and the South China Sea were compared with published results from the Namibian margin. Age relationships between the sediment components are site-specific and relatively constant over time. Similar to the Namibian slope, where alkenones have been reported to be 1000-4500 years older than co-occurring foraminifera, alkenones were significantly (~1000 years) older than co-occurring foraminifera in the Chilean margin sediments. In contrast, alkenones and foraminifera were of similar age (within 2 sigma error or better) in the NW African and South China Sea sediments. Total organic matter and alkenone ages were similar off Namibia (age difference TOC alkenones: 200-700 years), Chile (100-450 years), and NW Africa (360-770 years), suggesting minor contributions of preaged terrigenous material. In the South China Sea, total organic carbon is significantly (2000-3000 years) older owing to greater inputs of preaged terrigenous material. Age offsets between alkenones and planktic foraminifera are attributed to lateral advection of organic matter. Physical characteristics of the depositional setting, such as seafloor morphology, shelf width, and sediment composition, may control the age of co-occurring sediment components. In particular, offsets between alkenones and foraminifera appear to be greatest in deposition centers in morphologic depressions. Aging of organic matter is promoted by transport. Age offsets are correlated with organic richness, suggesting that formation of organic aggregates is a key process.

Pollen record and age determinations of a profile at Cape Mamontov Klyk, Siberia

Non-glaciated Arctic lowlands in north-east Siberia were subjected to extensive landscape and environmental changes during the Late Quaternary. Coastal cliffs along the Arctic shelf seas expose terrestrial archives containing numerous palaeoenvironmental indicators (e.g., pollen, plant macro-fossils and mammal fossils) preserved in the permafrost. The presented sedimentological (grain size, magnetic susceptibility and biogeochemical parameters), cryolithological, geochronological (radiocarbon, accelerator mass spectrometry and infrared-stimulated luminescence), heavy mineral and palaeoecological records from Cape Mamontov Klyk record the environmental dynamics of an Arctic shelf lowland east of the Taymyr Peninsula, and thus, near the eastern edge of the Eurasian ice sheet, over the last 60 Ky. This region is also considered to be the westernmost part of Beringia, the non-glaciated landmass that lay between the Eurasian and the Laurentian ice caps during the Late Pleistocene. Several units and subunits of sand deposits, peat-sand alternations, ice-rich palaeocryosol sequences (Ice Complex) and peaty fillings of thermokarst depressions and valleys were presented. The recorded proxy data sets reflect cold stadial climate conditions between 60 and 50 Kya, moderate inderstadial conditions between 50 and 25 Kya and cold stadial conditions from 25 to 15 Kya. The Late Pleistocene to Holocene transition, including the Allerød warm period, the early to middle Holocene thermal optimum and the late Holocene cooling, are also recorded. Three phases of landscape dynamic (fluvial/alluvial, irregular slope run-off and thermokarst) were presented in a schematic model, and were subsequently correlated with the supraregional environmental history between the Early Weichselian and the Holocene.

Reflecciones de actualidad : estudio del libro "Después de la crisis," escrito en Londres por el Sr. José Luis Tejada S. y algo sobre estadística bancaria /

Cover title.

Depression and recovery,

"Selected bibliography of recent literature": p. 289-292.

A History of modern banks of issue : with an account of the economic crises of the present century /

Includes index.

Monetary panics and their remedy ; with special reference to the panic of 11th May 1866 /

Mode of access: Internet.

The banks of New-York, their dealers, the clearinghouse, and the panic of 1857 ...

Mode of access: Internet.

Investigations in currency & finance,

Mode of access: Internet.

The panic of 1819: reactions and policies.

Mode of access: Internet.

Die wirtschaftliche krisis des jahres 1907 in den Vereinigten Staaten von Amerika.

Mode of access: Internet.

A digest of information on the relation of currency to the depression.

Mimeographed.

An examination of the report of the Joint Stock Bank Committee, &c. &c.

Goldsmiths'-Kress no. 29938.

Financial crises and periods of industrial and commercial depression,

Mode of access: Internet.