Le Paléolithique de la République Tchèque

Bohemia and Moravia, the two parts constituting together the Czech Republic, do not only represent historical countries, but they also display distinct geographies. As Bohemia is surrounded by mountains, its territory is often called the Bohemian Basin. In Moravia, the mountains in the north of the country are interrupted by the Moravian Gate, giving access to the Great Northern Plain of Europe with its rich sources of Northern flints, the best raw material for chipped stone industries available in Central Europe. The southern part opens directly towards the Danubian region with its more temperate environment, and connecting the south of Germany with the Balkans. The morphology of the territory had obviously influenced the Palaeolithic occupation. In the Lower and Middle Palaeolithic when communication did not play any major role, the two countries were settled relatively regularly, although not too densely. The Early Upper Palaeolithic brought a substantial change: In Moravia hundreds of sites proliferate, while there are only few of them in Bohemia. The Pavlovian phase of the Gravettian seems to be completely missing in Bohemia, while in Moravia it is concentrated in several megasites on the banks of the main rivers. This is certainly caused by the presence of the South-North artery of animal migrations and human communication. Since the Epigravettian, the density of occupation became balanced again. The local evolution of the Upper Palaeolithic was interrupted by the invasion of the Magdalenians coming from the West, on the one side along the Danube River, on the other by the northern route through Poland. The Late Palaeolithic, subject to influences coming from the North, gradually transformed into the Mesolithic.     

Découverte de Foraminifères planctoniques paléocènes dans les brèches,précédemment tenues pour aptiennes et d'origine diapirique,des Pyrénées basco-béarnaises

After the dating, by means of planktonic Foraminifera, of post-metamorphic marine breccias, Upper Danian–Lower Selandian in age, associated to hemipelagites and unconformably overlying the Cretaceous tectogenic axis of the Pyrenees from Roussillon to Bigorre, was it possible to extend westwards the breccia-filled Palaeocene ‘trough’ as far as the ‘Zone des Chaı̂nons béarnais’? This later unit, which belonged to the North-Iberian palaeomargin during Lower Cretaceous, was previously considered by several authors as characterized by an important halokinesis generating, during Aptian/?Albian, collapses of the Jurassic–Lower Cretaceous carbonate cover above dissolved salt domes and spectacular accumulations of breccias. In fact, we have everywhere identified Palaeocene planktonic microfauna within the matrix of these breccias (and within the associated hemipelagites), particularly of the reference ‘diapiric’ breccias of Etchebar, Lauriolle, Layens and Bosmendiette/Beloscare. Deposited into intra- ‘trough’ sub-marine canyons, after karstification and erosion of intermediate mountains with a steep topography previously induced by Uppermost Cretaceous compressions, the herein studied Palaeocene marine breccias should not be hereafter regarded as linked to any Lower Cretaceous diapirism on the North-Iberian palaeomargin. To cite this article: B. Peybernès et al., C. R. Palevol 1 (2002) 3–10.     

Effect of discothèque environment on epileptic children.

A free-field study of 22 epileptic children, selected on the basis of past electroencephalographic abnormality, identified a group who exhibited a significant increase in epileptiform discharge rate on electroencephalography in a discothèque environment (p less than 0.05). Laboratory investigations showed that these children were activated by a wide range of stimuli, including intermittent photic stimulation and exercise. The response to exercise was a good predictor of a child''s electroencephalographic response in a discothèque. The findings suggest that most epileptic children are not particularly vulnerable in a discothèque environment.     

L'évolution des gastéropodes lacustres et la paléoéologie des diatomées dans le Néogène de Kos (Dodécanèse,Grèce)

Evolutionary lineages of several limnic gastropod genera (Viviparus, Melanopsis, Theodoxus) from the Neogene of Kos island (Dodecanese, Greece) are described and interpreted. The attempt is made to analyse the paleoecological development of a limnic sedimentary basin in the eastern portion of Kos by means of Diatoms. Obviously, there is no relation between the chemical parameters of the water of the former lake and the morphological development of the gastropods. The lineages of Viviparus brevis, Theodoxus doricus and Melanopsis gorceixi are suggested to be caused by phyletic transformations and not by changing environmental conditions. It is, thus, possible to establish a local biostratigraphy based on subspecies, and moreover, a more regional one based on longer ranging species.     

Une syringocèle révélée par un abcès périntéal

Purpose

The authors present a clinical report of a perforate syringocele diagnosed in a male patient and they review the clinical, radiological and therapeutic aspects of this disease.

Case report

A 50-year-old man attended the emergency room with perineal abscess. Computerized Tomography (CT) scan was used to establish the diagnosis. This patient also underwent urethrocystoscopy, sonography and retrograde urethrography.

Results

Treatment consisted of open surgical evacuation of the perineal abscess with bladder catheter. Urethrocystoscopy showed a large perforate syringocele in the urethra with no need for endoscopy marsupialization. No recurrence was observed at follow-up at 3 months.

Conclusion

Syringocele is a rare malformation which usually is asymptomatic. It can be congenital or acquired and can be classified into four morphological types. The most frequent treatment is endoscopic marsupialization of the syringocèle. Open surgical excision is recommended for complicated syringocèle with abscess or perineal pain.     

Première biozonation du Pléistocène Européen,principal résultat biostratigraphique de l'étude des Rhinocerotidae (Mammalia,Perissodactyla) du Miocène terminal au Pléistocène supérieur d'Europe Occidentale

For the Uppermost Miocene the already known zones MN 9 to MN 13 are used without any change; they prove to be particularly useful for the study of fossil rhinocerotids. The Plio-Villafranchian age corresponds to the zones 14 to 19, the definition of the first five being completed and the last being new. Middle to Upper Pleistocene age deals with the zones 20 to 26, all being new and defined following the same principles.     

Las ganas de vivir como expresión del bienestar de las personas mayores

IntroductionWill-to-live, a central concept in well-being theories, represents a positive attitudinal component towards one's own life. It has been identified as a mediator between the self-perception of aging and longevity and health. The objective of this study is to characterise elderly people with high levels of will-to-live in the main dimensions of positive psychology.MethodThe study included the voluntary participation of 165 adults, aged between 54-89 years, users of senior centres in the Community of Madrid. Will-to-live and other dimensions of well-being and health were evaluated. The correlations between the different evaluated dimensions were analysed, and comparisons made in terms of different levels of will-to-live, as well as an analysis of the dimensions that contribute most to the will-to-live.ResultsCorrelations among the majority of variables were statistically significant, with a decrease in the coefficients being observed when controlling the effect of the will-to-live. When groups with different levels of will-to-live are compared with well-being and health, there are statistically significant differences in practically all of the dimensions. Gratitude, positive affect, and depression are the dimensions that best predict will-to-live.ConclusionOlder adults that make up the group with high will-to-live are characterised by higher levels of optimism, gratitude, positive affect, sense of life, psychological prosperity, resilience, happiness, and satisfaction with life, as well as lower levels of depression and negative self-perception of aging. The implications of these results point towards the relevance of will-to-live in successful aging.