Essential oils from medicinal and aromatic plants: A review of the gastroprotective and ulcer-healing activities

Gastric ulcer is an excoriated area of the gastric mucosa. It is among the predominant gastrointestinal chronic diseases. The essential oils represent an important part of the traditional pharmacopoeia in many countries and have been successfully used for gastroprotection and ulcer healing. Thus, this review presents the experimental activity of essential oils traditionally used in the gastric ulcer prevention and treatment, considering their families, part of the plant studied, bioassays, and their mechanisms of gastroprotection and ulcer healing, with the aim of stimulating novel studies in the search for a new phytomedicine to treat gastric diseases. © 2012 The Authors Fundamental and Clinical Pharmacology © 2012 Société Française de Pharmacologie et de Thérapeutique.

Libros de texto y aprendizaje en la escuela.

Con el interés de conocer a fondo el lenguaje presente en los libros de texto de Ciencias Naturales y Ciencias Sociales y de determinar su incidencia en los procesos de aprendizaje, se han observado varios grupos de estudiantes de secundaria de Barranquilla (Colombia), empleando el método de investigación etnográfica. Se analizan las reacciones observadas en los estudiantes ante el libro de texto y qué características del mismo suscitan esas reacciones, aspectos que pueden influir en el nivel de aprendizaje. En la obra se presentan algunas orientaciones para analizar el libro de texto y establecer la relación entre éste y el aprendizaje de los alumnos, proponiendo unas pautas para elaborar un cuestionario que permita evaluar el libro de texto.

Sobre la identitat dels Matiners a les comarques del N.E. de Catalunya

This study attempts to throw some light on the identity of the Matiners of the regions of north-eastern Catalonia by analizing a notebook which was a register of rebels. This notebook gives the age, geographical origin and profession of the rebels. The War of the matiners (1846-49) was a Catalan rebellion framed within the context of popular opposition to the regime of the moderates, and in the midst of a general crisis. Themen who formed the groups of ((trabucaires)) were particulary young (the problem of recriting must not be forgotten), and came from the country, the crafts, and industry, and were militarized above all in the interior regions

Estudo aerobiológico da cidade do Funchal: detecção bioquímica dos principais aeroalergénios polínicos

A abordagem da doença alérgica, nomeadamente da alergia respiratória, surge reforçada com o contributo da Aerobiologia no conhecimento, evolução e controlo da doença. Por seu turno, a caracterização bioquímica dos aeroalergénios de uma região pemite avaliar a sua composição e potencial alergénico, com particular interesse para espécies vegetais cuja introdução e/ou proximidade a áreas populacionais, potenciam o aparecimento ou o aumento de sensibilização a aeroalergénios. O trabalho apresentado nesta dissertação incidiu em duas vertentes de investigação distintas, porém complementares e interdependentes: numa primeira parte, no estudo da composição aerobiológica da atmosfera da cidade do Funchal no período 2002-2004 (Capítulo I), e numa segunda parte, na caracterização bioquímica dos alergénios polínicos mais frequentes detectados no referido período (Capítulo II). Assim, numa primeira parte, a monitorização aerobiológica (incluindo pólenes, esporos de fungos e demais partículas de origem biológica), foi realizada com um polinómetro do tipo volumétrico, tipo Hirst (Burkard). Os dados obtidos foram correlacionados com os parâmetros meteorológicos e avaliado o seu significado estatístico, permitindo antever a influência das variáveis ambientais em cada tipo particular de pólen e de fungo. Constataram-se algumas diferenças no conteúdo aerobiológico comparativamente ao restante território nacional. No espectro polínico dominaram as Poaceae e Urticaceae, plantas ornamentais (Asteraceae, Boraginaceae, Cupressaceae) e as representativas da faixa norte da cidade (Ericaceae, Myrtaceae e Pinaceae). Comparativamente a outras regiões do País, o espectro polínico foi no cômputo geral semelhante, embora se destaque para esta região, a expressividade do tipo Corylus no total polínico anual. A Primavera e o início de Verão, corresponderam às épocas de maior diversidade e concentração de pólenes. As diferenças encontradas no espectro polínico da cidade do Funchal são explicadas por variáveis intrínsecas desta região, tais como a composição vegetal, a localização da cidade, condições geo-climáticas inerentes, e a influência dos parâmetros meteorológicos, nomeadamente a temperatura e humidade relativa. Verificou-se a ocorrência de um maior número de pólenes quando a humidade se situa entre os 50 e 60 %, com a precipitação e a velocidade do vento a atingir valores mais baixos. A análise da variação intra-diurna observada revelou que há uma maior representação de pólenes entre as 11 e as 16 horas. Este estudo aerobiológico confere dados para o estabelecimento do primeiro calendário polínico da região e a definição de padrões de sazonalidade. Por seu turno, a fenologia dos principais tipos polínicos observados no Funchal permite definir um padrão anual de ocorrências polínicas. Relativamente à aeromicologia, verifica-se que, durante o período de estudo foram observados esporos de fungos sobretudo na Primavera (particularmente em Abril e Maio), início do Verão e no Outono. Os Deuteromicetes representaram a classe predominante, sendo Cladosporium o fungo mais abundante na atmosfera do Funchal, cujas concentrações mais elevadas ocorrem a humidades relativas de 40 a 70%. Tal como os pólenes, os esporos apresentam um dinâmica de variação intra-diurna particular: ocorreram em maior concentração entre as 13 e as 15 horas, surgindo igualmente nas primeiras horas da madrugada e da noite. O coberto vegetal do Funchal poderá afectar a aeromicologia local, na medida em que constitui um substrato importante para o crescimento de fungos, tal como as gramíneas que proliferam em quantidade e variedade ao longo de todo o ano. Constatou-se a existência de correlação entre a ocorrência de alguns esporos de fungos e taxa polínicos mais frequentes na atmosfera do Funchal. A análise de Spearman sugere a existência de correlação entre a ocorrência de Parietaria com a de Alternaria e Drechslera. Os esporos de fungos, incluindo esporos de fetos constituem uma fracção significativa das partículas na atmosfera do Funchal, sendo cerca de 11 vezes superior à dos pólenes. Na segunda parte do trabalho, o estudo bioquímico dos aeroalergénios polínicos implicou a optimização dos procedimentos de extracção, apurando-se três técnicas para a obtenção dos perfis proteicos de extractos de pólen desde a sua fonte natural. Esta análise permitiu detectar e identificar através das técnicas de SDS-PAGE-Imunoblotting, proteínas IgE específicas do pólen de plantas possivelmente relacionadas com a sensibilização alérgica. Em consonância com a monitorização aerobiológica, foram preparados extractos de pólen de 10 espécies de plantas. Os resultados em SDS-PAGE revelaram um elevado polimorfismo proteico em todos os extractos. Obtiveram-se extractos de pólen de 7 plantas acerca das quais não se conheciam estudos desta natureza: Acacia mearnsii, Avena barbata, Carduus squarrosus, Carlina salicifolia, Datura candida, Echium nervosum e Urtica membranosa. Por imunoblotting detectou-se no soro de dois pacientes IgE específica a proteínas de D. candida, com pesos moleculares entre 150,71 ± 0,05 e 58,92 ± 5,67 KDa. O soro de um deles reagiu igualmente com 5 alergénios de P. pinaster com 42,02 ± 0,05; 38,61 ± 0,46 ; 35,70 ± 7,78 ; 31,82 ± 2,11 e 27,45 ± 0,46 KDa. No soro de outro indivíduo foi detectada IgE específica para uma proteína de A. mearnsii com 66,66 ± 0,13 KDa, e outra de C. squarrosus,de 67,53 ± 0,29 KDa. É de destacar a sensibilidade e fiabilidade da técnica de Imunoblotting, e o interesse em incluila na metodologia de diagnóstico complementar da alergia respiratória. A ampla difusão de espécies como Ricinus communis, Urtica spp. ou A. mearnsii e sua proximidade à presença humana, reforçam, por um lado, a importância da vigilância aerobiológica, e por outro lado, requer uma definição do seu carácter alergénico para a população desta região.

Search for a W ' or Techni-rho Decaying into WZ in pp Collisions at root s=7 TeV

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Pollen records and lithology of profiles from Lobsigensee, Switzerland

Lobsigensee is a small kettle hole lake 15 km north-west of Bern on the Swiss Plateau, at an altitude of 514 m asl. Its surface is 2ha today, its maximum depth 2.7 m; it has no inlet and the overflow functions mainly during snow melting. The area was covered by Rhone ice during the Last Glaciation (map in Fig.2). Local geology, climate and vegetation are summarized in Figure 3A-C, the history of settlement in Figures 5-7. In order to reconstruct the vegetational and environmental history of the lake and its surroundings pollen analysis and other bio- and isotope stratigraphies were applied to twelve profiles cored across the basin with modified Livingstone corers (Fig.3 D). (1) The standard diagram: The central core LQ-90 is described as the standard pollen diagram (Chapter 3) with 10 local pollen assemblage zones of the Late-Glacial (local PAZ Ll to Ll0, from about 16'000(7) to 10'000 years BP) and 20 PAZ of the Holocene (local PAZ L11 to L30), see Figs. 8-10 and 20-24. Local PAZ L 1 to L3 are in the Late-Glacial clay and record the vegetational development after the ice retreat: L1 shows very low pollen concentration and high Pinus percentages due to long-distance transport and reworking; the latter mechanism is corroborated by the findings of thermophilous and pre-Quaternary taxa. Local PAZ L2 has a high di versi ty of non-arboreal pollen (NAP) and reflects the Late-Glacial steppe rich in heliophilous species. Local PAZ L3 is similar but additionally rich in Betula nana and Sal1x, thus reflecting a "shrub tundra". The PAZ L1 to L3 belong to the Oldest Dryas biozone. Local PAZ L4 to L 10 are found in the gyttja of the profundal or in the lake marl of the littoral and record the Late-Glacial forests. L4 is the shrub phase of reforestation with very high Junlperus and rapidly increasing Betula percentages. L5 is the PAZ with a first, L7 with a second dominance of tree-birches, separated by L6 showing a depression in the Betula curve. L4 to L7 can be assigned to the Balling biozone. Possible correlation of the Betula depression to the Older Dryas biozone is discussed. In local PAZ L8 Plnus immigrates and expands. L9 shows a facies difference in that Plnus dominates over Betula in littoral but not in profundal spectra. L8 and L9 belong to the Allerod biozone. In its youngest part the volcanic ash from Laach/Eifel is regularly found (11,000 BP). The local PAZ Ll0 corresponds to the Younger Dryas blozone. The merely slight increase of the NAP indicates that the pine forests of the lowland were not strongly affected by a cooler climate. In order to evaluate the significance of the littoral accumulation of coniferous pollen the littoral profile LQ-150 is compared to the profundal. Radiocarbon stratigraphies derived from different materials are presented in Figures 13 and 14 and in Tables 2 and 3. The hard-water errors in the gyttja samples and the carbonate samples are similar. The samples of terrestrial plant macrofossils are not affected by hard-water errors. Two plateaux of constant age appear in the age-depth relationship; their consequence for biostratigraphy as well as pollen concentration and influx diagrams are discussed. Radiocarbon ages of the Late-Glacial pollen zones are shown in Table 10. The Holocene vegetational history is recorded in the local PAZ L 11 to L30. After a Preboreal (PAZ L11) dominated by pine and birch the expansions of Corylus, Ulmus and Quercus are very rapid. Among these taxa Corylus dominates dur ing the Boreal (PAZ L 12 and L 1 3), whereas the components of the mixed oak forest dominate in the Older Atlantic (PAZ L14 to L16). In the Younger Atlantic (PAZ L 17 to L 19) Fagus and Alnus play an increasing, the mixed oak forest a decreasing role. During the period of local PAZ L19 Neolithic settlers lived on the shore of Lobsigensee. During the Subboreal (PAZ L20 and L21) and the Older Subatlantic (L22 to L25) strong fluctuations of Fagus and often antagonistic peaks of NAP, Alnus, Betula and Corylus can be interpreted as signs of human impact on vegetation. L23 is characterized not only by high values of NAP (especially apophytes and anthropochorous species) but also by the appearance of Juglans, Castanea and Secale which point to the Roman colonization of the area. For a certain period during the Younger Subatlantic (PAZ L26 to L30) the lake was used for retting hemp (Cannabis). Later the dominance of Quercus pollen indicates the importance of wood pastures. The youngest sediments reflect the wide-spread agricultural grass lands and the plantation of Pinus and Picea. Radiocarbon dates for the Holocene are given in Figure 23 and Table 4, the extrapolated ages of the Holocene pollen zones in Table 15. (2) The cross sections: Figures 25 and 26 give a summary of the litho- and palynostratigraphy of the two cross sections. Based on 11 Late-Glacial and 9 Holocene pollen diagrams (in addition to the standard ones), the consistency of the criteria for the definition of the pollen zones is examined in Tables 7 and 8 for the Late-Glacial and in Tables 11 to 14 for the Holocene. Sediment thicknesses across the basin for each pollen zone are presented in these tables as well as in Figures 43 to 45 for the Late-Glacial and in Figures 59 to 65 for the Holocene. Sediment focusing can explain differences between the gyttja cores of the profundal. Focusing is more than compensated for through "stretching" by carbonate precipitation on the littoral terrace. Pollen influx to the cross section are discussed (Chapters 4.1.5. and 4.2.3.). (3) The regional pollen zones: Based on some selected sites between Lake Geneva and Lake Constance regional pollen zones are proposed (Table 16, 17 and 19). (4) Paleoecology: Climatic change in the Late-Glacial can be inferred from Coleoptera, Trichoptera, Chironomidae and d18O of carbonates: a distinct warming is recorded around 12' 600 BP and around 10' 000 BP. The Younger Dryas biozone (10'700-10'000 BP) was the only cooling found in the Late-Glacial. The Betula depression often correlated wi th the Older Dryas biozone was possibl not colder but dryer than the previous period. During the Holocene the lowland site is not very sensitive to the minor climatic changes. Table 22 summarizes climatic and trophic changes before 8'000 BP as deduced from various biostratigraphies studied by a number of authors. Ostracods, Chironomids and fossil pigments indicate that anoxic conditions prevailed during the BoIling (possibly meromixis). Changes in the lake level are illustrated in Figure 74. A first lake-level lowering occurred in the early Holocene (10'000 to 9'000 BP), a second during the Atlantic (about 6'800 to 5'200 BP). The first "shrinking" of the lake volume resulted in a eutrophication recorded by laminations in the profundal and by pigments of Cyanophyceae. The second fall in water level corresponds to an increase of Nymphaeaceae. Human impact can be inferred in three ways: eutrophication of the lake (since the Neolithic), changes of terrestrial vegetation by deforestations (cyclicity of Fagus, see Figures 78 to 80), and enhanced erosion (increasing sedimentation rates by inwashed clay, particularly since the Roman Colonization, see Figures 49 and 81). Summary: This paper was planned as the final report on Lobsigensee. However, a number of issues are not answered but can only be asked more precisely, for example: (1) For the two periods with the highest rates of change, Le. the Bolling and the Preboreal biozones, pollen influx may reflect vegetation dynamics. Detailed investigations of these periods in annually laminated sediments are planned. (2) Biostratigraphies other than palynostratigraphy are needed to estimate the degree of linkage or independence in the development of terrestrial and lacustrine ecosystems. Often our sampling intervals were not identical, thus influencing our temporal resolution. (3) 6180- and 14C-stratigraPhies with high resolution will elucidate the leads and lags of these dynamic periods. Plateaux of constant age in the age-depth relationship have a strong bearing on both biological and geophysical understanding of Late-Glacial and early Holocene developments. (4) Numerical methods applied to the pollen diagrams of the cross section will help to quantify the significance of similari ties and dissimilarities across a single basin (with Prof. Birks). (5) Numerical methods applied to different sites on the Swiss Plateau and on the transect across the Alps will be helpful in evaluating the influence of different environmental factors (with Prof. Birks). (6) A new map 1: 1000 with 50cm-contour lines prov ided by Prof. Zurbuchen will be combined with a grid of cores sampling the transition from lake marl to peat enabling us to calculate paleo-volumes of the lake. This is interesting for the two "shrinking periods" (in Fig. 74A numbers 2-6 and 7-10), both accompanied by eutrophication. The pal eo-volume during the Neoli thic set tlement of the Cortaillod culture linked wi th an est l.mate of trophic change derived from diatoms (Prof. Smol in prep.) could possibly give an indication of the size of the human population of this period. (7) For the period with the antagonism between Fagus peaks and ABC-peaks close collaboration between palynologists, geochemists and archeologists should enable us to determine the influence of prehistoric and historic people on vegetation (collaboration with Prof. Stockli and Prof. Herzig). (8) The core LL-75 taken with a "cold letter box" will be analysed for major and trace elements by Dr. Sturm for 210pb and 137Cs by Prof.von Gunten and for pollen. We will see if our local PAZ L30 really corresponds to the surface sediment and if the small seepage lake reflects modern pollution.