(Table 2) Organic residue at DSDP Hole 76-534A

The kind, sedimentation rate, and diagenesis of organic particles delivered to the North Atlantic seafloor during the Middle Jurassic-Early Cretaceous were responsible for the presence of carbonaceous sediments in Hole 534A. Organic-rich black clays formed from the rapid supply of organic matter; this organic matter was composed of either abundant, well-preserved, and poorly sorted particles of land plants deposited in clays and silty clays within terrigenous turbiditic sequences (tracheal facies) or abundant amorphous debris (xenomorphic facies) generated through the digestive tracts of marine zooplankton and sedimented as fecal pellets. Evidence for the fecal-pellet origin of xenomorphic debris is illustrated. Black clays were also produced in sediments containing less organic matter as a result of the black color of carbonized particles composing all or most of the residues (micrinitic facies). Slowly sedimented hematitic Aptian clays contain very little carbonized, organic debris that survived diagenetic oxidation. In the red calcareous clay sequence of the Late Jurassic, larger amounts of this oxidized debris turned several clay layers black or blackish red. Carbonized debris also dominates the residues recovered in interbedded black and green Albian clays. Carbonization of organic matter in these sediments either turned them black or provided the diagenetic environment for reduced iron. Carbonized debris is also appreciable in burrow-mottled black-green Kimmeridgian clay. The study of Hole 534A organic matter indicates that during the middle Callovian there was a rapid supply of terrigenous organic matter, followed by a late Callovian episode of rapidly supplied xenomorphic debris deposited as fecal pellets. The Late Jurassic-Berriasian was a time of slower sedimentation of organic matter, primarily of a marine dinoflagellate flora in a poorly preserved xenomorphic facies variously affected by diagenetic oxidation. Several intervals of carbonized tracheal tissue in the Oxfordian and Kimmeridgian suggest episodes of oxidized terrigenous matter. The same sequence of Callovian organic events is evident in much of the Early Cretaceous

Cochinilla negra del olivo : control mediante insecticidas

El objetivo del presente trabajo fue comparar la eficiencia de 4 pesticidas: dimetoato, metidation, etion y clorpirifos, en el control de la cochinilla H [Saissetia oleae Bernard (Homoptera, Coccoidea, Lecaniidae)] también llamada cochinilla negra del olivo. Estos productos, conocidos en Mendoza (Argentina), se utilizan localmente. El ensayo se realizó en Vistalba (Luján de Cuyo). Para la evaluación se tuvo en cuenta el porcentaje de mortalidad. El análisis estadístico se efectuó transformando los datos según arcsen ( x / 1 0 0 ) .

Chert petrology and geochemistry at DSDP Leg 62 Holes

Sixty-five chert, porcellanite, and siliceous-chalk samples from Deep Sea Drilling Project Leg 62 were analyzed by petrography, scanning electron microscopy, analysis by energy-dispersive X-rays, X-ray diffraction, X-ray spectroscopy, and semiquantitative emission spectroscopy. Siliceous rocks occur mainly in chalks, but also in pelagic clay and marlstone at Site 464. Overall, chert probably constitutes less than 5% of the sections and occurs in deposits of Eocene to Barremian ages at sub-bottom depths of 10 to 820 meters. Chert nodules and beds are commonly rimmed by quartz porcellanite; opal-CT-rich rocks are minor in Leg 62 sediments 65 to 108 m.y. old and at sub-bottom depths of 65 to 520 meters. Chert ranges from white to black, shades of gray and brown being most common; yellow-brown and red-brown jaspers occur at Site 464. Seventy-eight percent of the studied cherts contain easily recognizable burrow structures. The youngest chert at Site 463 is a quartz cast of a burrow. Burrow silica maturation is always one step ahead of host-rock silicification. Burrows are commonly loci for initial silicification of the host carbonate. Silicification takes place by volume-f or-volume replacement of carbonate sediment, and more-clay-rich sediment at Site 464. Nannofossils are commonly pseudomorphically replaced by quartz near the edges of chert beds and nodules. Other microfossils, mostly radiolarians and foraminifers, whether in chalk or chert, can be either filled with or replaced by calcite, opal-CT, and (or) quartz. Chemical micro-environments ultimately control the removal, transport, and precipitation of calcite and silica. Two cherts from Site 465 contain sulfate minerals replaced by quartz. Site 465 was never subaerially exposed after sedimentation began, and the formation of the sulfate minerals and their subsequent replacement probably occurred in the marine environment. Several other cherts with odd textures are described in this paper, including (1) a chert breccia cemented by colloform opal-CT and chalcedony, (2) a transition zone between white porcellanite containing opal-CT and quartz and a burrowed brown chert, consisting of radial aggregates of opal-CT with hollow centers, and (3) a chert that consists of silica-replaced calcite pseudospherules interspersed with streaks and circular masses of dense quartz. X-ray-diffraction analyses show that when data from all sites are considered there are poorly defined trends indicating that older cherts have better quartz crystallinity than younger ones, and that opal-CT crystallite size increases and opal-CT cf-spacings decrease with depth of occurrence in the sections. In a general way, depth of burial and the presence of calcite promote the ordering in the opal-CT crystal structure which allows its eventual conversion to quartz. Opal-CT in porcellanites converts to quartz after reaching a minimum d-spacing of 4.07 Å. Quartz/opal-CT ratios and quartz crystallinity vary randomly on a fine scale across four chert beds, but quartz crystallinity increases from the edge to the center of a fifth chert bed; this may indicate maturation of the silica. Twenty-four rocks were analyzed for their major- and minor-element compositions. Many elements in cherts are closely related to major mineral components. The carbonate component is distinguished by high values of CaO, MgO, Mn, Ba, Sr, and (for unknown reasons) Zr. Tuffaceous cherts have high values of K and Al, and commonly Zn, Mo, and Cr. Pure cherts are characterized by high SiO2 and B. High B may be a good indicator of formation of chert in an open marine environment, isolated from volcanic and terrigenous materials.

(Table 3) Geochemistry at DSDP Leg 79 Holes

Detailed mineralogical and geochemical studies were performed on samples from selected time intervals recovered during Leg 79 on the Mazagan Plateau. The uppermost Albian and Cenomanian sediments of Sites 545 and 547 can be correlated on the basis of mineralogy and geochemistry; these sediments illustrate differential settling processes and the existence of hot climates with alternating humid and dry seasons in the African coastal zone. The upper Aptian to Albian black shales of Site 545 point to an irregular alternation of tectonic activity and relaxation stages, allowing different behaviors in the reworking of soils, crystalline rocks, and sediments born in peri-marine basins. The barren lower Mesozoic reddish sediments and evaporitic series of Sites 546 and 547 are characterized by a strong physical erosion of sialic landscapes, without clear evidence of post-depositional metamorphic events. At Site 546 strong early diagenetic processes in a confined evaporitic environment affect both the mineralogy and the geochemistry of pre-Miocene rocks.

Inorganic and organic geochemistry and sediment descriptions at DSDP Hole 93-603B

About one hundred samples of sediments and rocks recovered in Hole 603B were analyzed for type, abundance, and isotopic composition of organic matter, using a combination of Rock-Eval pyrolysis, C-H-N-S elemental analysis, and isotope-ratio mass spectrometry. Concentrations of major, minor, and trace inorganic elements were determined with a combination of X-ray fluorescence and induction-coupled plasma spectrometry. The oldest strata recovered in Hole 603B (lithologic Unit V) consist of interbedded light-colored limestones and marlstones, and black calcareous claystones of Neocomian age. The inorganic and organic geochemical results suggest a very terrigenous aspect to the black claystones. The organic geochemical results indicate that the limestones and marlstones contain a mixture of highly degraded marine and terrestrial organic matter. Comparison of the Neocomian carbonates at Site 603 with those on the other side of the North Atlantic, off Northwest Africa at Site 367, shows that the organic matter at Site 367 contains more marine organic matter, as indicated by higher pyrolysis hydrogen indices and lighter values of d13C. Comparison of inorganic geochemical results for the carbonate lithologies at Site 603 with those for carbonate lithologies at Site 367 suggests that the Site 603 carbonates may contain clastic material from both North American and African sources. The black claystones at Site 603, on the other hand, probably were derived almost entirely from North American clastic sources. Lithologic Unit IV overlying the Neocomian carbonates, consists of interbedded red, green, and black claystones. The black claystones at Site 603 contain more than ten times the organic carbon concentration of the interbedded green claystones. The average concentration of organic carbon in the black claystones (2.8%), however, is low relative to most mid-Cretaceous black claystones and shales in the Atlantic, particularly those found off Northwest Africa. The geochemical data all suggest that the organic matter in the black claystones is more abundant but generally more degraded than the organic matter in the green claystones, and that it was derived mainly from terrestrial sources and deposited in oxygenated bottom waters. The increased percentage of black claystone beds in the upper Cenomanian section, and the presence of more hydrogen-rich organic matter in this part of the section, probably resulted from the increased production and accumulation of marine organic matter that is represented worldwide near the Cenomanian/Turonian boundary in deep-sea and land sections. A few upper Cenomanian black claystone samples that have hydrogen indices > 150 also contain particularly high concentrations of V and Zn. Most samples of black claystone, however, are not particularly metal-rich compared with other black claystones and shales. Compared with red claystones from lithologic Unit IV, the green and black claystones are enriched in many trace transition elements, especially V, Zn, Cu, Co, and Pb. The main difference between the "carbonaceous" claystones of lithologic Unit IV and "variegated" or "multicolored" claystones of the overlying Upper Cretaceous to lower Tertiary Unit III is the absence of black claystone beds. As observed at several other sites (105 and 386), the multicolored claystones at Site 603 are somewhat enriched in several trace transition elements-especially Cu, Ni, and Cr-relative to most deep-sea clays. The multicolored claystones are not enriched in Fe and Mn, and therefore are not "metalliferous" sediments in the sense of those found at several locations in the eastern Pacific. The source of the slightly elevated concentrations of transition metals in the multicolored claystones probably is upward advection and diffusion of metals from the black claystones of the underlying Hatteras Formation. The red, orange, and green claystone beds of lithologic Unit II (Eocene), like those of Unit III, really represent a continuation of deposition of multicolored claystone that began after the deposition of the Neocomian carbonates. The color of the few black beds that occur within this unit results from high concentrations of manganese oxide rather than high concentrations of organic matter.

Podredumbre parda del melocotonero (Monilinia spp.) : detección, identificación de especies y contribución a la epidemiología de la enfermedad

Monilinia spp. (M. laxa, M. fructigena y M. fructicola) causa marchitez en brotes y flores, chancros en ramas y podredumbre de la fruta de hueso provocando pérdidas económicas importantes en años con climatología favorable para el desarrollo de la enfermedad, particularmente en variedades tardías de melocotonero y nectarino. En estos huéspedes en España, hasta el momento, la especie predominante es M. laxa y, en menor proporción, M. fructigena. La reciente introducción en Europa de la especie de cuarentena M. fructicola hace necesaria una detección e identificación rápida de cada una de las especies. Además, hay diversos aspectos de la etiología y epidemiología de la enfermedad que no se conocen en las condiciones de cultivo españolas. En un primer objetivo de esta Tesis se ha abordado la detección e identificación de las especies de Monilinia spp. causantes de podredumbre parda. El estudio de las bases epidemiológicas para el control de la enfermedad constituye el fin del segundo objetivo. Para la detección del género Monilinia en material vegetal por PCR, diferenciándolo de otros hongos presentes en la superficie del melocotonero, se diseñaron una pareja de cebadores siguiendo un análisis del ADN ribosomal. La discriminación entre especies de Monilinia se consiguió utilizando marcadores SCAR (región amplificada de secuencia caracterizada), obtenidos después de un estudio de marcadores polimórficos de ADN amplificados al azar (RAPDs). También fue diseñado un control interno de amplificación (CI) basado en la utilización de un plásmido con secuencias de los cebadores diferenciadores del género, para ser utilizado en el protocolo de diagnóstico de la podredumbre parda con el fin de reconocer falsos negativos debidos a la inhibición de PCR por componentes celulares del material vegetal. Se disponía de un kit comercial que permitía distinguir Monilinia de otros géneros y M. fructicola del resto de especies mediante anticuerpos monoclonales utilizando la técnica DAS-ELISA. En esta Tesis se probaron diferentes fuentes de material como micelio ó conidias procedentes de cultivos en APD, o el micelio de la superficie de frutas o de momias frescas, como formas de antígeno. Los resultados obtenidos con ELISA se compararon con la identificación por métodos morfológico-culturales y por PCR con los cebadores desarrollados en esta Tesis. Los resultados demostraron la posibilidad de una detección temprana en frutas frescas por este método, realzando las posibilidades de una diagnosis temprana para una prevención más eficaz de M. fructicola en fruta de hueso. El estudio epidemiológico de la enfermedad comenzó con la determinación de las principales fuentes de inóculo primario y su importancia relativa en melocotoneros y nectarinos del valle del Ebro. Para ello se muestrearon 9 huertos durante los años 2003 a 2005 recogiendo todas las momias, frutos abortados, gomas, chancros, y brotes necróticos en los árboles. También se recogieron brotes aparentemente sanos y muestras de material vegetal situados en el suelo. En estas muestras se determinó la presencia de Monilinia spp. Los resultados mostraron que la fuente principal de inóculo son las momias que se quedan en los árboles en las que la supervivencia del hongo tras el invierno es muy alta. También son fuentes de inóculo las momias del suelo y los brotes necróticos. De aquí se deriva que una recomendación importante para los agricultores es que deben eliminar este material de los huertos. Un aspecto no estudiado en melocotonero o nectarino en España es la posible relación que puede darse entre la incidencia de infecciones latentes en los frutos inmaduros a lo largo del cultivo y la incidencia de podredumbre en los frutos en el momento de la recolección y en postcosecha. Esta relación se había observado previamente en otros frutales de hueso infectados con M. fructicola en diversos países del mundo. Para estudiar esta relación se realizaron ensayos en cinco huertos comerciales de melocotonero y nectarino situados en el Valle del Ebro en cuatro estados fenológicos durante los años 2000-2002. No se observaron infecciones latentes en botón rosa, dándose la máxima incidencia en precosecha, aunque en algunos huertos se daba otro pico en el endurecimiento del embrión. La especie prevaleciente fue M. laxa. Se obtuvo una correlación positiva significativa entre la incidencia de infecciones latentes y la incidencia de podredumbre en postcosecha. Se desarrolló también un modelo de predicción de las infecciones latentes en función de la temperatura (T) y el periodo de humectación (W). Este modelo indicaba que T y W explicaban el 83% de la variación en la incidencia de infecciones latentes causadas por Monilinia spp. Por debajo de 8ºC no se predecían latentes, necesitándose más de 22h de W para predecir la ocurrencia de latentes con T = 8ºC, mientras que solo se necesitaban 5h de W a 25ºC. Se hicieron también ensayos en condiciones controladas para determinar la relación entre la incidencia de las infecciones latentes, las condiciones ambientales (T y W), la concentración de inóculo del patógeno (I) y el estado de desarrollo del huésped (S) y para validar el modelo de predicción desarrollado con los experimentos de campo. Estos ensayos se llevaron cabo con flores y frutos de nectarino procedentes de un huerto comercial en seis estados fenológicos en los años 2004 y 2005, demostrándose que la incidencia de podredumbre en postcosecha y de infecciones latentes estaba afectada por T, W, I y S. En los frutos se producían infecciones latentes cuando la T no era adecuada para el desarrollo de podredumbre. Una vez desarrollado el embrión eran necesarias más de 4-5h de W al día y un inóculo superior a 104 conidias ml-1 para que se desarrollase o podredumbre o infección latente. La ecuación del modelo obtenido con los datos de campo era capaz de predecir los datos observados en estos experimentos. Para evaluar el efecto del inóculo de Monilinia spp. en la incidencia de infecciones latentes y de podredumbre de frutos en postcosecha se hicieron 11 experimentos en huertos comerciales de melocotonero y nectarino del Valle del Ebro durante 2002 a 2005. Se observó una correlación positiva entre los números de conidias de Monilinia spp. en la superficie de los frutos y la incidencia de infecciones latentes De los estudios anteriores se deducen otras dos recomendaciones importantes para los agricultores: las estrategias de control deben tener en cuenta las infecciones latentes y estimar el riesgo potencial de las mismas basándose en la T y W. Deben tener también en cuenta la concentración de esporas de Monilinia spp. en la superficie de los frutos para disminuir el riesgo de podredumbre parda. El conocimiento de la estructura poblacional de los patógenos sienta las bases para establecer métodos más eficaces de manejo de las enfermedades. Por ello en esta Tesis se ha estudiado el grado de diversidad genética entre distintas poblaciones de M. laxa en diferentes localidades españolas utilizando 144 marcadores RAPDs (59 polimórficos y 85 monomórficos) y 21 aislados. El análisis de la estructura de la población reveló que la diversidad genética dentro de las subpoblaciones (huertos) (HS) representaba el 97% de la diversidad genética (HT), mientras que la diversidad genética entre subpoblaciones (DST) sólo representaba un 3% del total de esta diversidad. La magnitud relativa de la diferenciación génica entre subpoblaciones (GST) alcanzaba 0,032 y el número estimado de migrantes por generación (Nm) fue de 15,1. Los resultados obtenidos en los dendrogramas estaban de acuerdo con el análisis de diversidad génica. Las agrupaciones obtenidas eran independientes del huerto de procedencia, año o huésped. En la Tesis se discute la importancia relativa de las diferentes fuentes evolutivas en las poblaciones de M. laxa. Finalmente se realizó un muestreo en distintos huertos de melocotonero y nectarino del Valle del Ebro para determinar la existencia o no de aislados resistentes a los fungicidas del grupo de los benzimidazoles y las dicarboximidas, fungicidas utilizados habitualmente para el control de la podredumbre parda y con alto riesgo de desarrollar resistencia en las poblaciones patógenas. El análisis de 114 aislados de M. laxa con los fungicidas Benomilo (bencimidazol) (1Bg m.a ml-1), e Iprodiona (dicarboximida) (5Bg m.a ml-1), mostró que ninguno era resistente en las dosis ensayadas. Monilinia spp. (M. laxa, M. fructigena and M. fructicola) cause bud and flower wilt, canker in branches and stone fruit rot giving rise important economic losses in years with appropriate environmental conditions, it is particularly important in late varieties of peach and nectarine. Right now, M. laxa is the major species for peach and nectarine in Spain followed by M. fructigena, in a smaller proportion. The recent introduction of the quarantine organism M. fructicola in Europe makes detection and identification of each one of the species necessary. In addition, there are different aspects of disease etiology and epidemiology that are not well known in Spain conditions. The first goal of this Thesis was the detection and identification of Monilinia spp. causing brown rot. Study of the epidemiology basis for disease control was the second objective. A pair of primers for PCR detection was designed based on the ribosomal DNA sequence in order to detect Monilinia spp. in plant material and to discriminate it from other fungi colonizing peach tree surface. Discrimination among Monilinia spp. was successful by SCAR markers (Sequence Characterized Amplified Region), obtained after a random amplified polymorphic DNA markers (RAPDs) study. An internal control for the PCR (CI) based on the use of a mimic plasmid designed on the primers specific for Monilinia was constructed to be used in diagnosis protocol for brown rot in order to avoid false negatives due to the inhibition of PCR as consequence of remained plant material. A commercial kit based on DAS-ELISA and monoclonals antibodies was successfully tested to distinguish Monilinia from other fungus genera and M. fructicola from other Monilinia species. Different materials such as micelium or conidias from APD cultures, or micelium from fresh fruit surfaces or mummies were tested in this Thesis, as antigens. Results obtained by ELISA were compared to classical identification by morphologic methods and PCR with the primers developed in this Thesis. Results demonstrated the possibility of an early detection in fresh fruits by this method for a more effective prevention of M. fructicola in stone fruit. The epidemiology study of the disease started with the determination of the main sources of primary inoculum and its relative importance in peach trees and nectarines in the Ebro valley. Nine orchards were evaluated during years 2003 to 2005 collecting all mummies, aborted fruits, rubbers, cankers, and necrotic buds from the trees. Apparently healthy buds and plant material located in the ground were also collected. In these samples presence of Monilinia spp. was determined. Results showed that the main inoculum sources are mummies that stay in the trees and where fungus survival after the winter is very high. Mummies on the ground and the necrotics buds are also sources of inoculum. As consequence of this an important recommendation for the growers is the removal of this material of the orchards. An important issue not well studied in peach or nectarine in Spain is the possible relationship between the incidence of latent infections in the immature fruits and the incidence of fruit rot at harvesting and postharvesting. This relationship had been previously shown in other stone fruit trees infected with M. fructicola in different countries over the world. In order to study this relationship experiments were run in five commercial peach and nectarine orchards located in the Ebro Valley in four phenologic states from 2000 to 2002. Latent infections were not observed in pink button, the maxima incidence arise in preharvest, although in some orchards another increase occurred in the embryo hardening. The most prevalence species was M. laxa. A significant positive correlation between the incidence of latent infections and the incidence of rot in postharvest was obtained. A prediction model of the latent infections based on the temperature (T) and the wetness duration (W) was also developed. This model showed that T and W explained 83% of the variation in latent infection incidence caused by Monilinia spp. Below 8ºC latent infection was not predicted, more than 22h of W with T = 8ºC were needed to predict latent infection occurrence of, whereas at 25ºC just 5h of W were enough. Tests under controlled conditions were also made to determine the relationship among latent infections incidence, environmental conditions (T and W), inoculum concentration of the pathogen (I) and development state of the host (S) to validate the prediction model developed on the field experiments. These tests were made with flowers and fruits of nectarine coming from a commercial orchard, in six phenologic states in 2004 and 2005, showing that incidence of rot in postharvest and latent infections were affected by T, W, I and S. In fruits latent infections took place when the T was not suitable for rot development. Once developed the embryo, more than 4-5h of W per day and higher inoculums (104 conidia ml-1) were necessary for rot or latent infection development. The equation of the model obtained with the field data was able to predict the data observed in these experiments. In order to evaluate the effect of inoculum of Monilinia spp. in the incidence of latent infections and of rot of fruits in postharvest, 11 experiments in commercial orchards of peach and nectarine of the Ebro Valley were performed from 2002 to 2005. A positive correlation between the conidial numbers of Monilinia spp. in the surface of the fruits and the incidence of latent infections was observed. Based on those studies other two important recommendations for the agriculturists are deduced: control strategies must consider the latent infections and potential risk based on the T and W. Spores concentration of Monilinia spp. in the surface of fruits must be also taken in concern to reduce the brown rot risk. The knowledge of the population structure of the pathogens determines the bases to establish more effective methods of diseases handling. For that reason in this Thesis the degree of genetic diversity among different M. laxa populations has been studied in different Spanish locations using 144 RAPDs markers (59 polymorphic and 85 monomorphics) on 21 fungal isolates. The analysis of the structure of the population revealed that the genetic diversity within the subpopulations (orchards) (HS) represented 97% of the genetic diversity (HT), whereas the genetic diversity between subpopulations (DST) only represented a 3% of the total of this diversity. The relative magnitude of the genic differentiation between subpopulations (GST) reached 0.032 and the considered number of migrantes by generation (Nm) was of 15.1. The results obtained in dendrograms were in agreement with the analysis of genic diversity. The obtained groupings were independent of the orchard of origin, year or host. In the Thesis the relative importance of the different evolutionary sources in the populations from M. laxa is discussed. Finally a sampling of resistant isolates in different orchards from peach and nectarine of Ebro Valley was made to determine the existence of fungicide resistance of the group of benzimidazoles and the dicarboximidas, fungicides used habitually for the control of rot brown and with high risk of resistance developing in the pathogenic populations. The analysis of 114 isolated ones of M. laxa with the fungicides Benomilo (bencimidazol) (1Bg m.a ml-1), and Iprodiona (dicarboximida) (5Bg m.a ml-1), showed no resistant in the doses evaluated.

Carolyn Banner

Carolyn had a Bachelor of Science in Education degree from Langston University and a Master of Science degree in Early Childhood Development from the University of Minnesota. In 1959 Carolyn came to Lincoln as acting principal of the laboratory Elementary School and Supervisor of Elementary Student Teaching. She nurtured and taught hundreds of Lincoln’s students to be the finest, most qualified teachers in the country. Once retired she was able to enjoy the many awards that she received through out her years. The awards she received were citations, and honors: AAUW Woman of Achievement Award, and the MUATE Outstanding Teacher Educator Award. She was elected the first Black President of AAUW in 1965. She was appointed to the Mayor’s Census and Redistricting Committee in 1981. On June 21st, 1985 Mayor George Hartsfield declared that day as “Carolyn Banner Day” in Jefferson City. Carolyn Banner retired from Lincoln University in July 1985.

RELIGIÃO E IDENTIDADE: UM ESTUDO SOBRE NEGROS METODISTAS DA REGIÃO METROPOLITANA DE SÃO PAULO

Este estudo trata da dinâmica relacional das identidades religiosas e etno-raciais em torno de pessoas negras de igrejas metodistas da Região Metropolitana de São Paulo. Toma como referência empírica as Igrejas Metodistas em: Suzano, Itaquaquecetuba - Monte Belo - e Central em Santo André. Analisa as implicações identitárias do sujeito negro metodista e aponta contradições entre parâmetros socioculturais das identidades negras construídas ao longo da história e o modelo religioso metodista. Analisa a construção sociocultural das identidades religiosas, circunscritas às contingências materiais, econômicas e políticas da sociedade onde estão inseridos os sujeitos da pesquisa. Propõe que a identidade negra coletiva é uma mescla de associações, por um lado negativas resultantes tanto das condições socioeconômicas segregacionistas vinculadas ao racismo institucionalizado na sociedade e nos espaços religiosos, por outro, positivas, de um protagonismo cultural enriquecedor da cultura brasileira, além daquele marcado pela resistência, desenvolvido pelos movimentos negros. Demonstra o papel da instituição metodista que impõe uma padronização cultural de classe média branca e controle sobre as manifestações identitárias negras.(AU)

RELIGIÃO E IDENTIDADE: UM ESTUDO SOBRE NEGROS METODISTAS DA REGIÃO METROPOLITANA DE SÃO PAULO

Este estudo trata da dinâmica relacional das identidades religiosas e etno-raciais em torno de pessoas negras de igrejas metodistas da Região Metropolitana de São Paulo. Toma como referência empírica as Igrejas Metodistas em: Suzano, Itaquaquecetuba - Monte Belo - e Central em Santo André. Analisa as implicações identitárias do sujeito negro metodista e aponta contradições entre parâmetros socioculturais das identidades negras construídas ao longo da história e o modelo religioso metodista. Analisa a construção sociocultural das identidades religiosas, circunscritas às contingências materiais, econômicas e políticas da sociedade onde estão inseridos os sujeitos da pesquisa. Propõe que a identidade negra coletiva é uma mescla de associações, por um lado negativas resultantes tanto das condições socioeconômicas segregacionistas vinculadas ao racismo institucionalizado na sociedade e nos espaços religiosos, por outro, positivas, de um protagonismo cultural enriquecedor da cultura brasileira, além daquele marcado pela resistência, desenvolvido pelos movimentos negros. Demonstra o papel da instituição metodista que impõe uma padronização cultural de classe média branca e controle sobre as manifestações identitárias negras.(AU)

Kitâb-ı ahdnâme-yi hümâyûn-ı saâdet-makrûn : manuscript, 1740?

According to the colophon (f. 23r), copy of capitulations of 4 Rebīʻ I 1153 AH [May 31, 1740 AD], signed by the Grand Vezir el-Ḥācc Meḥmed Paşa and the French envoy Louis-Sauveur, Marquis de Villeneuve (mentionned f. 3r), granted to France. Contains renewal of the capitulations granted during the Reign of Sultan Meḥmed IV (r. 1058-99 [1648-87]) with some newly introduced articles.

Fī bayān mā dhakarahu Muḥammad Afandī al-Awaljī al-marsūl min ṭaraf al-dawlah al-ʻalīyah ilá Faransā wa-mā shāhadahu hunāk =: Traduction arabe de la relation de voyage en France de Mehmet Effendi, Ambassadeur de Turquie : manuscript, undated

بيان ما ذكره محمد افندي المرسول من طرف الدولة العلية إلى فرنسا وجميع ما شاهده هناك قال انه... :Incipit

Plasmodium pre-erythrocytic stages: what's new?

The pre-erythrocytic (PE) phase of malaria infection, which extends from injection of sporozoites into the skin to the release of the first generation of merozoites, has traditionally been the 'black box' of the Plasmodium life cycle. However, since the advent of parasite transfection technology 13 years ago, our understanding of the PE phase in cellular and molecular terms has dramatically improved. Here, we review and comment on the major developments in the field in the past five years. Progress has been made in many diverse areas, including identifying and characterizing new proteins of interest, imaging parasites in vivo, understanding better the cell biology of hepatocyte infection and developing new vaccines against PE stages of the parasite.

Calcium carbonate, organic carbon, sediment description and hydrogen and oxygen index at DSDP Sites 93-603, 93-605, 93-604 and 95-603

The organic matter contents of sediments and rocks sampled during DSDP Leg 93 have been characterized by CHN and Rock-Eval analyses. Most samples from Sites 604 and 605 on the New Jersey continental slope and from Site 603 on the Hatteras outer continental rise contained less than 0.5% organic carbon. Some Neogene samples from the slope contained 1 to 2% organic carbon, and Cretaceous samples from the outer rise were as rich as 13.6% organic carbon by weight. Thin layers of black claystones of Santonian, Cenomanian, and Albian age were found interbedded in organiccarbon- lean, bioturbated, turbiditic claystones. Similar layers of turbiditic black marlstones were interspersed among Neocomian limestones and sandstones. Although the organic matter in many of the samples appeared to be detrital continental material, according to Rock-Eval and C/N values, Cenomanian black shales, in particular, contained substantial proportions of marine-derived organic matter.

Las dos emparedadas, memorias de la inquisicíon.

Head and tail pieces; decorative initials.

Jean-Paul Marat; orné de son portrait; esprit politique accompagné de sa vie scientifique, politique et privée,

"Documents justificatifs": v. 2, p. [353]-519.