384 resultados para seashore meadows


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A published formula containing minimal aortic cross-sectional area and the flow deceleration pattern in the descending aorta obtained by cardiovascular magnetic resonance predicts significant coarctation of the aorta (CoA). However, the existing formula is complicated to use in clinical practice and has not been externally validated. Consequently, its clinical utility has been limited. The aim of this study was to derive a simple and clinically practical algorithm to predict severe CoA from data obtained by cardiovascular magnetic resonance. Seventy-nine consecutive patients who underwent cardiovascular magnetic resonance and cardiac catheterization for the evaluation of native or recurrent CoA at Children's Hospital Boston (n = 30) and the University of California, San Francisco (n = 49), were retrospectively reviewed. The published formula derived from data obtained at Children's Hospital Boston was first validated from data obtained at the University of California, San Francisco. Next, pooled data from the 2 institutions were analyzed, and a refined model was created using logistic regression methods. Finally, recursive partitioning was used to develop a clinically practical prediction tree to predict transcatheter systolic pressure gradient ≥ 20 mm Hg. Severe CoA was present in 48 patients (61%). Indexed minimal aortic cross-sectional area and heart rate-corrected flow deceleration time in the descending aorta were independent predictors of CoA gradient ≥ 20 mm Hg (p <0.01 for both). A prediction tree combining these variables reached a sensitivity and specificity of 90% and 76%, respectively. In conclusion, the presented prediction tree on the basis of cutoff values is easy to use and may help guide the management of patients investigated for CoA.

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This thesis examines the local and regional scale determinants of biodiversity patterns using existing species and environmental data. The research focuses on agricultural environments that have experienced rapid declines of biodiversity during past decades. Existing digital databases provide vast opportunities for habitat mapping, predictive mapping of species occurrences and richness and understanding the speciesenvironment relationships. The applicability of these databases depends on the required accuracy and quality of the data needed to answer the landscape ecological and biogeographical questions in hand. Patterns of biodiversity arise from confounded effects of different factors, such as climate, land cover and geographical location. Complementary statistical approaches that can show the relative effects of different factors are needed in biodiversity analyses in addition to classical multivariate models. Better understanding of the key factors underlying the variation in diversity requires the analyses of multiple taxonomic groups from different perspectives, such as richness, occurrence, threat status and population trends. The geographical coincidence of species richness of different taxonomic groups can be rather limited. This implies that multiple geographical regions should be taken into account in order to preserve various groups of species. Boreal agricultural biodiversity and in particular, distribution and richness of threatened species is strongly associated with various grasslands. Further, heterogeneous agricultural landscapes characterized by moderate field size, forest patches and non-crop agricultural habitats enhance the biodiversity of rural environments. From the landscape ecological perspective, the major threats to Finnish agricultural biodiversity are the decline of connected grassland habitat networks, and general homogenization of landscape structure resulting from both intensification and marginalization of agriculture. The maintenance of key habitats, such as meadows and pastures is an essential task in conservation of agricultural biodiversity. Furthermore, a larger landscape context should be incorporated in conservation planning and decision making processes in order to respond to the needs of different species and to maintain heterogeneous rural landscapes and viable agricultural diversity in the future.

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BACKGROUND: Although intra-retinal tumor has long been staged presurgically according to the Reese-Ellsworth (R-E) system, retinoblastoma differs from other pediatric neoplasms in never having had a widely accepted classification system that encompasses the entire spectrum of the disease. Comparisons among studies that consider disease extension, risk factors for extra-ocular relapse, and response to therapy require a universally accepted staging system for extra-ocular disease. PROCEDURE: A committee of retinoblastoma experts from large centers worldwide has developed a consensus classification that can encompass all retinoblastoma cases and is presented herein. Patients are classified according to extent of disease and the presence of overt extra-ocular extension. In addition, a proposal for substaging considering histopathological features of enucleated specimens is presented to further discriminate between Stage I and II patients. RESULTS: The following is a summary of the classification system developed-Stage 0: Patients treated conservatively (subject to presurgical ophthalmologic classifications); Stage I: Eye enucleated, completely resected histologically; Stage II: Eye enucleated, microscopic residual tumor; Stage III: Regional extension [(a) overt orbital disease, (b) preauricular or cervical lymph node extension]; Stage IV: Metastatic disease [(a) hematogenous metastasis: (1) single lesion, (2) multiple lesions; (b) CNS extension: (1) prechiasmatic lesion, (2) CNS mass, (3) leptomeningeal disease]. A proposal is also presented for substaging of enucleated Stages I and II eyes. CONCLUSIONS: The proposed staging system is the product of an international effort to adopt a uniform staging system for patients with retinoblastoma to cover the whole spectrum of the disease.

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Alpine flora and climate change: monitoring of three summits in Valais (Switzerland) during the 20th century Climate change might trigger an upward shift of the flora in the Swiss Alps, especially since these experienced higher change in average than observed on a global scale. Previous investigations in the canton des Grisons (Switzerland) and Austria have revealed an increase of floristic diversity on alpine summits since the beginning of the 20th century. Three summits in Valais were revisited in this study: the Gornergrat (first inventory in 1919), the Torrenthorn (about in 1885) and the Beaufort (about in 1920). Every summit was newly inventoried in 2003 in the framework of the PERMANENT.PLOT.CH project. All showed a strong increase in species richness. On the Gornergrat (3135 m), 16 species were not found anymore, but 35 new ones were observed. The number of species on this exceptionally rich summit rose from 102 to 121. In comparison, the floristic richness increased from 24 to 63 species on the Torrenthorn (2924 m) and from 16 to 48 species on the Beaufort (3048 m). As in previous studies, this increase seems likely to be associated with climate change: the new species prefer, in average, higher temperature conditions than those previously prevailing on the summits. On the Gornergrat and Beaufort, our observations reveal a development of alpine meadows, whereas species typical of rocks and raw soils are predominantly colonising the Torrenthorn. This difference might be related to the important damage caused by wanderers on the vegetation of the Torrenthorn.

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A causa de la ràpida evolució de la tecnologia, una gran quantitat de publicacions sobre pastures i farratges fetes a Catalunya han quedat oblidades. S'aprofita l'oportunitat de participar en el projecte «Tipificación, cartografía y evolución de los pastos españoles (1800-2004)» per posar al dia la revisió bibliogràfica. Amb la nostra recerca s'han trobat 316 articles o llibres sobre cultius farratgers i 159 sobre prats i pastures que en aquest treball es presenten ordenats per cultius.

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Durante estos últimos 50 años ha tenido lugar un abandono de las masías y de los cultivos tradicionales en los Prepirineos catalanes. En este trabajo se han estudiado los cambios de usos del suelo desde los años 50 hasta la actualidad en una cuenca de 6577 ha situada en la cabecera de la Ribera Salada (El Solsonès). Para ello se han utilizado fotografías aéreas del año 1957 y del año 1992. Como base cartográfica sirvieron los ortofotomapas del año 1993. El análisis de los cambios de usos según diferentes variables (pendiente y orientación) y según diferentes enfoques (intensidad del cambio y uso final), se ha llevado a cabo mediante el programa de SIG ARC/INFO®. Se han establecido tendencias en la evolución de los usos según la pendiente y la orientación. Los resultados obtenidos muestran que los campos de cultivo son los que han disminuido más en superficie, dando lugar a pastos. Por otro lado, el bosque denso ha aumentado considerablemente su extensión (845 ha).

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A causa de la ràpida evolució de la tecnologia, una gran quantitat de publicacions sobre pastures i farratges fetes a Catalunya han quedat oblidades. S’aprofita l’oportunitat de participar en el projecte «Tipificación, cartogra- fía y evolución de los pastos españoles (1800-2004)» per posar al dia la revisió bibliogràfica.Amb la nostra recerca s’han trobat 316 articles o llibres sobre cultius farratgers i 159 sobre prats i pastures que en aquest treball es presenten ordenats per cultius.

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[cat]Els treballs arqueològics duts a terme al solar localitzat entre la plaça de Pau Vila i els carrers del Dr. Aiguader i de la Marquesa, al peu del baluard del Migdia, han permès descriure l'evolució geoarqueològica d'un tram del front marítim de Barcelona i generar dades fiables de la configuració de la façana litoral. Sota una potent capa de sorres, s'identificà un paquet de llims i argiles orgàniques característiques d'un medi de baixa energia; és a dir, protegit de l'onatge marí probablement per barres sorrenques. Aquesta seqüència presenta una cronologia entre finals del segle IX i ca. 1440, moment en què es realitzaren els primers intents de construcció d'estructures portuàries. En aquest nivell llimoargilós s'han dut a terme analítiques paleoambientals consistents en l'estudi pol·línic, sedimentològic i geoquímic dels sediments que han posat en evidència els canvis ambientals del front marítim barceloní, del paisatge vegetal del pla, com també de les activitats agrícoles i productives urbanes en època medieval i inicis de l'edat moderna. La informació així obtinguda ha estat contrastada amb la informació històrica. [eng]The archaeological work conducted at the site located at the foot of the Baluard del Migdia bastion between Plaça Pau Vila and Carrer Dr. Aiguader and Carrer Marquesa has provided the opportunity to describe the geoarchaeological evolution of a stretch of the seafront of Barcelona and to generate reliable data on the configuration of the coastline. A layer of silt and organic clays typical of a low-energy environment was found below a thick layer of sands. In other words, this packet was protected from the swell of the sea, probably by sandbars. This sequence presents a chronology spanning from the late 9th century BC to around 1440, the time when the first attempts were made to build port structures. This layer of silt and clay has been subjected to palaeoenvironmental analyses consisting of the study of the pollen, sediment and the geochemistry of the sediments. The results of this analysis provide evidence of the environmental changes in the seafront of Barcelona and the landscape in the plain, as well as the urban agricultural and production activities in medieval times and the early modern age. The information obtained has been compared with historical information.

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A Catalunya, la protecció i gestió de zones d’especial interès natural ha estat majoritàriament realitzada pel conjunt de les administracions públiques. Tot i així, en els últims anys han sorgit un conjunt d’iniciatives privades que a través d’acords de custòdia han passat a tenir un paper actiu en la protecció i gestió d’algunes finques amb un alt valor natural. És el cas de la finca els Cingles de l’Avenc, on s’ha dut a terme aquest treball, en la qual es pretén desenvolupar una activitat ramadera compatible amb la conservació dels valors naturals de la finca. L’objectiu principal d’aquest treball és conèixer la producció i qualitat farratgera dels diferents tipus de pastures que hi ha a la finca, i establir la càrrega ramadera que poden admetre. Aquest estudi ha tingut una durada de 3 anys i en aquest treball es presenten els resultats del 2011 i es fa l’anàlisi dels resultats dels 3 anys (2009, 2010, i 2011). L’estudi s’ha portat a terme en els 4 tipus principals de pastures que hi ha a la finca: joncedes, pastures mesòfiles, prats de dall i pastures sembrades. S’han utilitzat 11 parcel·les permanents excloses de la pastura, establertes l’any 2009, que inclouen la diversitat de tipus i zones de pastura. S’ha realitzat un mostreig de la biomassa mensual, d’abril a novembre, que ha consistit en dallar 4 quadrats de 50 x 50 cm, i s’ha calculat la producció anual. S’ha determinat la qualitat farratgera de l’herba de 4 moments de l’any: maig, juny, juliol i octubre. Després dels tres anys d’estudi hem obtingut que les pastures sembrades i els prats de dall són els més productius (1.067 g/m2.any i 1.005 g/m2.any, respectivament). La producció de les pastures mesòfiles i de les joncedes són més baixes (554 g/m2.any i 291 g/m2.any, respectivament). La qualitat farratgera de les pastures és bona a totes les comunitats, amb valors mitjans de proteïna digerible de 6,63%, de fibra bruta de 29,13%, de lignina de 7,29% i de 0,69 (ENL/1,700) unitats farratgeres. La producció anual global obtinguda a la finca durant aquests tres anys permet suportar una càrrega ramadera admissible d’unes 208 UBG (Unitats de Bestiar Gros. 1 U.B.G equival a 1 vaca a partir de 2 anys).

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[spa] En los últimos años ha aumentado el interés arqueológico por los cambios territoriales de época histórica. Asimismo, el número de registros polínicos ha aumentado sensiblemente. A pesar de que la falta de marcos cronológicos fiables impone límites a las interpretaciones sobre antropización, el presente artículo pretende realizar una síntesis de los cambios paleoambientales documentados entre los siglos VIII aC y XII dC, haciendo especial referencia a las transformaciones humanas del entorno. Este conjunto de datos polínicos hace evidente una intervención humana al inicio del periodo ibérico, presión que se intensifica durante el iberismo Pleno con la expansión de actividades agrícolas. El mundo romano significa una explotación del espacio menos extensiva, si bien el el siglo VII dC se produce una extensión de los pastos tanto en sectores elevados del Pirineo como de litoral catalán que modifica profundamente el paisaje. [eng] The archaeological interest on the environmental changes during historical times has increased during the last decades. In accordance, a number of palynological from NE Spain records has been recently published. Despite chronological frame works are not yet enough reliable, this paper proposes a synthesis of landscape changes from VIIIth century BC to XIIth century AD. Palynological data suggest the presence of human impacts at ghe beginning of iberic times. Humans pressure, mainly farmning activities, intensified during iberian times. Roman times record a less extensive land use but at the IVth century AD, grazing expanded at regional scale. Pastures expanded again at VIIth century AD, reaching high altitudes in the Pyrenees while at littoral plains, meadows were used for grazing. This period resulted in a deep change of the Catalan lansacapes.

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A detailed analysis of the morphology and the Holocene seismic and sequence stratigraphy and architecture of the infralittoral sedimentary environment of the El Masnou coast (Catalonia, NW Mediterranean Sea) was carried out using multibeam bathymetry and GeoPulse seismic data. This environment extends down to 26-30 m water depth, and is defined morphologically by two depositional wedges whose seafloor is affected by erosive furrows, slides, fields of large- and small-scale wavy bedforms, and dredging trenches and pits. Erosive terraces are also identified in the transition domain toward the inner continental shelf. The Holocene stratigraphy of the infralittoral environment is defined by two major seismic sequences (lower and upper), each one formed by internal seismic units. The sequences and units are characterised by downlapping surfaces made up of deposits formed by progradation of coastal lithosomes. The stratigraphy and stratal architecture, displaying a retrogradational arrangement with progradational patterns of minor order, were controlled by different sea-level positions. The stratigraphic division represents the coastal response to the last fourth-order transgressive and highstand conditions, modulated by small-scale sea-level oscillations (≈1-2 m) of fith to sixth order. This study also highlights the advantage of an integrated analysis using acoustic/seismic methods for practical assessment of the anthropogenic effects on infralittoral domains based on the association of marine geological observations.

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Soil properties on the Cap de Creus Peninsula, NE Spain depend primarily on scarce agricultural practices and early abandonment. In the study area, 90% of which is mainly covered by Cistus shrubs, 8 environments representing variations in land use/land cover and soil properties at different depths were identified. In each environment variously vegetated areas were selected and sampled. The soils, collected at different depths, were classified as Lithic Xerorthents according to the United States Department of Agriculture system of soil classification (USDA-NRCS 1975). Differences in soil properties were largely found according to the evolution of the plant canopy and the land use history. To identify underlying patterns in soil properties related to environmental evolution, factor analysis was performed and factor scores were used to determine how the factor patterns varied between soil variables, soil depths and selected environments. The three-factor model always accounted for 80% of the total variation in the data at the different soil depths. Organic matter was the more relevant soil property at 0–2 cm depth, whereas active minerals (silt and clay) were found to be the most relevant soil parameters controlling soil dynamics at the other depths investigated. Results showed that vineyards and olive tree soils are poorly developed and present worse conditions for mineral and organic compounds. Analysis of factor scores allowed independent assessment of soils, depth and plant cover and demonstrated that soils present the best physico-chemical characteristics under Erica arborea and meadows. In contrast, soils under Cistus monspeliensis were less nutrient rich and less well structured