Os custos das fracturas de etiologia osteoporótica em mulheres : institucionalização na Rede Nacional de Cuidados Continuados (RNCCI) e lares de 3ª idade

RESUMO - Contexto: A osteoporose é uma doença sistémica associada à diminuição da resistência óssea que condiciona o aparecimento de fracturas por traumatismos de baixa energia as quais reduzem em muitos casos a esperança e a qualidade de vida, implicando um elevado número de horas de dedicação dos cuidadores e conduzindo, em muitos casos, à necessidade de institucionalização dos doentes. Em Portugal, ocorrem cerca de 40.000 fracturas anualmente, das quais 8.500 do fémur proximal, que se estima consumirem mais de 50 milhões de euros só em cuidados hospitalares1. Objectivo: Avaliar o impacto económico da institucionalização na Rede Nacional de Cuidados Continuados Integrados e Lares da 3ª idade por fractura de etiologia osteoporótica em mulheres no ano 2009, em Portugal. Métodos: O estudo começa por analisar sucintamente os aspectos clínicos, sociais e epidemiológicos da osteoporose, focando a perda de autonomia e qualidade de vida dos doentes vítimas deste episódio e a subsequente necessidade de institucionalização. Descrevem-se os custos associados à institucionalização na RNCCI, em Portugal, ano 2009, utilizando como fonte principal a base de dados da instituição “Gestcare CCI”, complementada com dados da literatura. Apuram-se os custos totais associados ao encaminhamento dos doentes para Lares de 3ª Idade em Portugal no ano 2009, utilizando-se informação proveniente de um painel de Delphi modificado e dados da literatura. A valorização dos recursos tem por base os preços em vigor no território nacional, expressos nos decretos-lei devidamente referenciados. Resultados: No ano 2009 em Portugal foram empregues cerca de 2,5 milhões de euros no internamento das mulheres na RNCCI, na perspectiva da sociedade, sendo cerca de 2,2 milhões atribuíveis à osteoporose (90%). Cerca de 91% dos custos totais são alocados à fractura osteoporótica da anca (2 milhões €). Para a fractura vertebral, úmero e punho os custos foram mais baixos - 7,1%, 1,3% e 1% dos custos totais da osteoporose, respectivamente. Nos Lares de 3ª idade, estimou-se a admissão de aproximadamente 14.372 doentes com fractura osteoporótica em diferentes localizações, em 2009, Portugal, com um custo que oscilou entre os 19 e os 21,6 milhões de euros. A fractura osteoporótica da anca foi a mais incidente e a que representou custos mais elevados para a Segurança Social – entre 17,5 e 19,7 milhões de euros. Considerando como referência os 52 milhões de euros gastos em 2006 no tratamento hospitalar da fractura da anca (DGS, 2006), o encaminhamento das mulheres para a RNCCI e Lares da 3ª Idade corresponde a 42% do bolo total. Assim, os resultados nacionais enquadram-se no que se encontra descrito na literatura internacional - os custos atribuíveis à hospitalização oscilaram entre 17%50 e 63%29 da despesa total da doença e das institucionalizações entre os 16%58 e os 59%51. Conclusões: Em Portugal o impacto económico da institucionalização por fractura osteoporótica, sobretudo por fractura da anca, não é desprezável e mostra que existiriam poupanças significativas se fosse possível reduzir a prevalência da doença em Portugal. Face às alterações demográficas associadas ao envelhecimento da população, é expectável que a incidência e custos com o tratamento das fracturas do colo do fémur, mais associadas à osteoporose, venham a subir nos próximos anos, pelo que o combate à doença deve ser considerada uma prioridade nacional. A decisão pela opção por determinados programas de prevenção da doença ou da comparticipação ou não de determinada terapêutica necessita contudo de ser complementada com a medição da dimensão dos benefícios terapêuticos. --- ABSTRACT - Background: Osteoporosis is a systemic disease associated with the loss off the bone strength and it is one of the major causes of low energy fractures, which in many cases reduce life hope and quality. This happens because it has associated extensive treatments and it usually carries loss of independence, implying many hours of caregivers dedication and leading, in many cases, to the institutionalization of the patients. In Portugal, about 40,000 fractures occur annually, which 8,500 are proximal femur, and that are estimated to consume over 50 million euros only in hospital care. Objective: Evaluate the economic impact of institutionalization on the Integrated Continued Care National Network (RNCCI) and Care Homes associated to osteoporotic fractures in women, in the year 2009 in Portugal. Methods: The study begins by reviewing briefly the clinical, social, and epidemiological studies of osteoporosis and osteoporotic fractures, focusing on the patient autonomy loss and life quality. The total and average costs per episode associated with the institutionalization in RNCCI are described, in Portugal, year 2009, using as main data source the application "Gestcare CCI", complemented with literature data. The total costs associated with the patients referral for the Care Homes in Portugal in 2009 is also calculated, using information from a modified Delphi panel and some literature data. The resources valuation is based on prices prevailing in Portugal. Results: In 2009, women relocation in RNCCI consumed approximately 2.5 million euros, which 2.2 million are attributable to osteoporosis (90%). About 91% of the total costs are allocated to osteoporotic hip fracture (€ 2 million). For vertebral, humerus, and wrist fracture, the associated costs were lower, 7.1%, 1.3%, and 1% of total costs of osteoporosis treatment, respectively. In Care Homes, an intake of approximately 14 372 patients with osteoporotic fracture was estimated, at a cost that is between 19 and 21.6 million euros. The osteoporotic hip fracture was the most frequent and represented higher costs for Social Security - between 17.5 and 19.7 million euros. Taking as reference the 52 million spent in 2006 with hospital treatment of hip fracture (DGS, 2006), referring women to RNCCI and Care Homes represents 42% of the total costs. The results are in accordance with the international literature - costs attributable to hospitalization ranged between 17% and 63% of total expenditure of illness and institutionalization between 16% and 59%. Conclusions: In Portugal, the economic impact of institutionalization for osteoporotic fracture, particularly for hip fracture, is not negligible. It was shown that there would be significant savings if it were possible to reduce the prevalence of the disease in Portugal. Femoral fractures were the second most frequent diagnosis in RNCCI in 2008 and 2009 (16% of all episodes recorded). The execution of RNCCI in 2008 was 75 million euros, and 2.7% consumed by hip fracture and 0.3% by wrist, humerus, and spine fractures. The average cost per episode in 2009, from the perspective of society, for hip fracture, vertebral, humerus, and wrist (or non-osteoporotic) was € 5,195, € 5,160, € 5,030, and € 4,854 respectively. Thus, considering an average cost per episode in RNCCI from January to March of 3230€, the expense related to the treatment of these patients in RNCCI in 2009 was higher. For the Care Homes, an intake of approximately 14 372 patients with osteoporotic fracture in 2009 was estimated, at a cost to Social Security that ranged from 19 to 21.6 million €. The osteoporotic hip fracture was the most frequent and it was shown to absorve higher resources from Social Security - between 17.5 and 19.7 million €. This was followed by the analysis of vertebral and humerus fracture and the results showed that these fractures have a low incidence and low proportion of institutionalization, with a significantly lower cost - only about 4.7% and 3.3% of total expenditure, respectively. With demographic changes associated to ageing, it is expected that the incidence and treatment cost of the femoral neck fractures, more commonly associated with osteoporosis, will climb in coming years, so the fight against the disease should be considered a national priority. The decision to choose a certain disease prevention program or to reimburse a certain drug not should only account about the costs, but also the benefits of it. In fact, the size and impact of this problem, makes it necessary to focus all interventions in the prevention of these episodes either by using an appropriate therapy, either through real programs for disease prevention. Once the problem is installed, we must measure the health gains associated with the patient institutionalization by conducting additional research.

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.

Notes sur la géologie et la paléontologie du Miocène de Lisbonne. XXI Primeira caracterização de dinoflagelados dos níveis mais baixos da série miocénica de Lisboa

This is the first report on Dinoflagellata from lowermost Miocene beds in Portugal (Tagus basin, Lisbon region, exposure at Benfica). Some general data about Dinoflagellata are presented. Descriptions are provided for some forms: Gonyaulacysta tenuitabulata, Spiniferites ramosus, Achomosphaera sp., Hystrichokolpoma rigaudae, Homotriblium cf. pallidum, Cordosphaeridium sp, and Lingulodinium machaerophorum. Lithostratigraphical study of an important section along Circular highway at Benfica has shown that there is a hitherto unknown sedimentary cycle in Lisbon's lowermost Miocene (upper Oligocene?). Pollen and Ostracoda point out to an Lower Aquitanian or even Upper Chattian age for the first Neogene marine transgression in Portugal, previously considered as Upper Aquitanian or Lower Burdigalian.

Notes sur la géologie et la paleontology du Miocène de Lisbonne. XXII - Une Espèce nouvelle Pokornyella Lusitanica (Ostrocoda), dans le Miocène Inférieur du bassin du Tage

A new species, Pokornyella lusitanica (Ostracoda), from the Lower Miocene (Aquitanian) of the Lisbon area, is described. Some palaeoecological data are presented.

Contributions à la paleontology du Miocène moyen continental du basin du tage

This study on middle Miocene Charophytes from the Tagus'basin indicates the presence of two species. hitherto undescribed from these strata in Portugal, Correlation diagrams of height and width of gyrogonite demonstrate that the populations of Nitellopsis (Tectochara) etrusca from the localities Póvoa de Santarém and Pêro Filho are identical to that from La Grenatière (Hérault, France), The population of Lychnothamnus duplicicarinatus from Tremês is identical to that already known from Anwill (Switzerland). The age of this flora is therefore suggested as being the upper part of the middle Miocene. The results of Charophyte studies are in accordance with stratigraphical conclusions from previously conducted mammalian studies (Antunes and Mein), A table showing the distribution of species in the three portuguese localities is given.

Contributions à la paleontology du Miocène moyen continental du basin du tage

The lignite-clays of Póvoa de Santarém dated as Upper «Vindobonian» (mammalian zone MN6), fielded abundant remains of animals and plants (spores, pollens, seeds, etc.). The forms identified are indicative of several environments. Plants, either aquatic or belonging to swampy areas are predominant (Nuphar sp., Sparganium sp., Stratiotes kaltennordheimensis, cf. Ranunculus sp.). There are also remains of plants characteristiques of a humid rather than a swampy soil such as Polypodiaceae, Myrica ceriferiformis, Toddalia maii, Spirematospermum wetzeleri. The genera Vitis and Ephedra, although rare, point fowards the existence of drier regions in the neighbourhood. The presence of polens such as Picea indicate the presence at some distance less warm upland forest areas.

Notes sur la géologie et la paleontology du Miocène de Lisbonne

This note deals with the stratigraphical and paleontological study of the Palença section on the southern bank of the river Tagus, Portugal, and specially with its coccolithophorids. Three main lithostratigraphical units may be recognized: the lowest one does correspond to the upper part of COTTER's division II, the intermediate one to divisions III and IV-a, the third corresponding to pratically the whole division IV-b, However other and higher levels are also represented. Higher beds are also represented in the same sections; they are less well exposed and were not studied in detail. Caracterisation of biozones on the basis of Coccoliths so far found at Palença section is difficultsince MARTINI's zones have been defined mainly by forms of Discoaster and other genera that are wanting. However we can recognize that the richest assemblage (from beds 17-18, the uppermost layers of blue clays IV-a) may correspond to NN4. This is not in opposition to the results of the study of planctonic foraminifera, that are characteristic of BLOW's N7. Coccoliths from lower beds do not allow at present any valid comparisons.

Contributions à la Paléontologie du Miocène moyen continental du Bassin du Tage. I - Quelques mollusques - Pero Filho, Póvoa de Santarém, Sítio do Mirante

Some land and freshwater mollusks (Gastropoda, Pelecypoda) from three middle Miocene localities: Pêro Filho, Póvoa de Santarém, Sítio do Mirante, all in Ribatejo province, Portugal, are summarily studied. On a systematical viewpoint it has been shown (see also Tableau): - the presence of the genus Janulus, whose species only survive now at Madeira and Canary's islands; - the presence of "Helix" cotteri that may indeed belong in the genus Megalotachea, common in western Europe since "Helvetian" to Messinian times; - Limax, Testacella, Acroloxus and Pseudamnicola are quoted for the first time in portuguese tertiary formations; Ferrisia has been identified for the first time in Iberian Peninsule; - the presence of other forms previously quoted by ANTUNES & ZBYSZEWSKI (1973), is confirmed: Bithynia, Theodoxus, Pisidium. Such faunules are compatible with a middle Miocene age. On a paleobiogeographical viewpoint, some forms suggest mediterranean affinities. Fossil associations do correspond ecologically to either palustrine or stagnant, calm and shallow water conditions (Sítio do Mirante, and essentially also Póvoa de Santarém), or to fluviatile conditions (Pêro Filho).

Contributions à la Paléontologie du Miocène moyen continental du Bassin du Tage. II - Observations sur les dents pharyngiennes de poissons cyprinidés - Póvoa de Santarém.

The study of Cyprinid fish pharyngeal teeth, collected by M. Telles Antunes in continental "Helvetian" sediments from Póvoa de Santarém, makes possible to demonstrate the occurrence of two distinct species. One remains undetermined. The other belongs to the recent genus Leuciscus CUV. Several dental types of this genus are described and figured as Leuciscus antunesi nov. sp. Palaeoclimatical and palaeoecological interpretations are proposed.

Contributions à la Paléontologie du Miocène moyen continental du Bassin du Tage. III - Mammifères - Póvoa de Santarém, Pêro Filho et Chões (Secorio). Conclusions générales

This study on middle Miocene mammalian faunas from Tagus'basin deals particularly with some small mammals hitherto undescribed from Portugal, including a new Glirid (Paraglirulus scalabicensis nov. sp.); it allows an accurate datation by biostratigraphical standards, Megacricetodon crusafonti, Fahlbuschia darocensis, Cricetodon jotae being characteristic of mammalian MN6 unit, thus their age is nearly that of Sansan and Manchones (however the presence of Peridyromys hamadryas and Lagopsis verus do suggest, amidst this biozone, a somewhat later age than Sansan's); it contributes with indirect correlation data with marine formations, as underlying oyster-bearing beds most probably are in correspondance to the apogee of the same transgression that deposed near Lisbon ”schlier" facies from VI-a division (Serravalian, Blow's zones 10-13, Globorotalia meyeri zone); the diversity of mammalian assemblages is surely related to an environement with varied biotopes, whose characterisation becomes easier if account is taken of the preceding papers on mollusks (G. Truc) and Cyprinid fishes (J. Gaudant), and also according to some unpublished paleobotanical data (J. Pais). A table with a synthesis of all paleontological data so far known is presented.

Le monument de “Pedras da Granja” ou de “Pedras Altas” dans la “Várzea de Sintra"

In the present work, the authors describe the excavation of the monument of "Pedras da Granja" or "Pedras Altas", in the Várzea de Sintra. The first part consists of the diary of the excavations, a description of the stratigraphy encountered and of the position of the finds. An inventory of all the material found in this monument is given in the second part. The conclusions show that the monument was built on the surface of a lapiás whose crevices were used for the insertion of the standing stones, and for the deposition of the dead. Three archaeological levels were shown to exist: - upper level: Bell Beaker level; - intermediate level containing some artifacts of the Bell Beaker culture; - lower, older level with human remains more or less in situ, belonging to a local Neolithic-culture influenced by cultural imports of foreign origin. The three levels are separated, at the southern edge of the site, by layers of fallen stones. The human remains belong to some old people, but mostly to young men, women and children.

Connaissances stratigraphiques sur la base du Mésozoique portugais

In Portugal, the Mesozoic lower part is principally composed of conglomeratic, arenitic and pelitic deposits, which are here and there associated with carbonates rocks and evaporites. The Germanic Triassic succession is not observed. The Muschelkalk facies do not exist. Carbonates formation, and some thick evaporites deposits (Keuper facies) are of early Jurassic in age. The thick red beds accumulations deposited in a continental environment are Triassic. In Coimbra area the oldest palynomorphs found are Camian-Norian. In South Portugal (Algarve), the triassic serie must be more complete with a lower Triassic rich in Stegocephales bone-beds.

Le Crétacé inférieur de la marge atlantique portugaise: biostratigraphie, organization séquentielle, evolution paléogéographique

This paper gives a short description of main stratigraphic unities from the early Cretaceous in Estremadura and Algarve, with their lithological, sedimentological and paleontological characteristics. The distribution of facies enable to propose a paleogeographic frame including eroded high areas and sedimentary low areas roughly parallel to the present coast. The early Cretaceous from Estremadura is splited up into three megasequences each one with regressive then transgressive tendencies: this fact must be connected with the leading action of distensive, slow or sudden, movements. Beyond the hercynian fault of Messejana, Algarve presents a different sedimentary evolution during the early Cretaceous.

Évolution géologique de la marge ouest-ibérique

This paper is a summary of the results of the authors recent researches about the Western Iberian continental margin. During the Mesozoic, the margin is affected by two consecutive extensional phases interpreted as the result from two episodes of rifting in the Atlantic. Then during Cenozoic, subsidence was interrupted by compression and related deformation, specially during Eocene time. Ante-mesozoic basement controls the structural and sedimentary evolution of the margin.

La marge continentale sud-portugaise: évolution structurale et sédimentaire

The structural and sedimentary evolution of the portuguese continental margin South of Setúbal Canyon is outlined from the study of many seismic reflection profiles and rocks samples. During Triassic and Early Liassic time, a distension affects the Algarve margin that belongs to the Mesogean area. Off Baixo Alentejo rifting phases at Late Jurassic and Early Cretaceous times induced opening or widening of the adjacent part of the Atlantic ocean. Alpine orogeny is inferred to explain the Eocene and Miocene deformation of the margin specially along the main NE-SW fractures.