Organic matter composition and sulfate reduction intensity in Oman Margin sediments

Petrographical and geochemical studies of Neogene marine sediments from the Oman Sea (Leg 117, Sites 720, 724, 726 and 730), show a close relationship between the nature and amount of the organic matter, and the degree of degradation of organic matter by sulfate reduction, i.e. pyritization. Petrographically, three major pyritization types were observed: (1) Finely dispersed pyrite framboids in sediments from Oman Margin and Indus Fan, enriched in autochthonous marine organic matter. (2) Infilling of pores by massive pyrite crystals in Oman Margin sediments with a low TOC and a high microfossil content. (3) Pyrite mineralization of lignaceous fragments in organic-depleted sediments from the Indus Fan leading to more massive pyrite. Geochemically, we can define a sulfate reduction index (SRI) as the percentage of initial organic carbon versus that of residual organic carbon. Finely laminated Pliocene-Pleistocene sediments from the Oman Margin exclusively contain organic matter deriving from organic phytoplankton, for which the quantity (TOC) positively correlates with the geochemical quality (Hydrogen Index). We think that the occurrence of this residual organic matter is linked mainly to a high primary paleo-productivity. The intensity of sulfate reduction is constant for sediments with TOC up to 2% and becomes more important when organic input decreases. This degradation process can destroy up to 50% of the initial organic matter, but is not sufficient to explain some of the encountered very low TOC values. It can be seen that sharp increases of certain plankton species (with mineral skeletons) are responsible for a pronounced degradation of organic matter, due to increased sulfate reduction. In that case, the organic matter may be strongly degraded (high SRI), although deposited in an oxygen-depleted environment. Conversely, Miocene-Pliocene sediments contain an autochthonous organic matter that is typical of both low productivity and oxic processes; their very low sulfate reduction index indicates that very little metabolizable organic matter was initially present.

Geochemistry of phosphate and glauconites of ODP Leg 128 samples

Glauconites and phosphates have been detected in almost all investigated samples at Sites 798 (uppermost Miocene or lower Pliocene to Pleistocene) and 799 (early middle Miocene to Pleistocene). Autochthonous occurrences appear in very minor quantities (generally below 0.2%) throughout the drilled sequences, whereas allochthonous accumulations are limited to the lower Pliocene or uppermost Miocene sequence at Site 798 (glauconites) and to the upper and middle Miocene sequence at Site 799 (upper and middle Miocene: glauconites; middle Miocene: phosphates). X-ray fluorescence, microprobe, and bulk chemical analyses indicate high variabilities in cations and anions and generally low oxide totals. This is probably related to the substitution of phosphate and fluoride aniors by hydroxide and carbonate anions in phosphates and to the depletion of iron, aluminum, and potassium cations and the enrichment in hydroxide and crystal water in glauconites. Gradients in pore-water contents of dissolved phosphate and fluoride at Sites 798 and 799 suggest a depth of phosphate precipitation between 30 and 50 mbsf, with fluoride as the limiting element for phosphate precipitation at Site 798. Phosphate and fluoride appear to be balanced at Site 799. Crude extrapolations indicate that the Japan-Sea sediments may have taken up approximately 7.2*10**10 g P total/yr during the Neogene and Pleistocene. This amount corresponds to approximately 0.3% of the estimated present-day global transfer of phosphorus into the sediments and suggests that the Japan Sea constitutes an average sink for this element. The two main carriers of phosphorus into the present Japan Sea are the Tshushima and the Liman currents, importing approximately 6.6*10**10 g P and 5.7*10**10 g P per year, respectively. Bulk chemical analyses suggest that at least 36% of P total in the sediments is organically bound phosphorus. This rather high value, which corresponds to the measured Japan-Sea deep-water P organic/P total ratios, probably reflects rapid transport of organic phosphorus into the depth of the Japan Sea.

Sediments in arctic sea ice - entrainment, characterization and quantification

Sediments in Arctic sea ice are important for erosion and redistribution and consequently a factor for the sediment budget of the Arctic Ocean. The processes leading to the incorporation of sediments into the ice are not understood in detail yet. In the present study, experiments on the incorporation of sediments were therefore conducted in ice tanks of The Hamburg Ship Model Basin (HSVA) in winter 1996/1997, These experiments showed that on average 75 % of the artificial sea-ice sediments were located in the brine-channel system. The sediments were scavenged from the water column by frazil ice. Sediments functioning as a nucleus for the formation of frazil ice were less important for the incorporation. Filtration in grease ice during relatively calm hydrodynamic conditions was probably an effective process to enrich sediments in the ice. Wave fields did not play an important role for the incorporation of sediments into the artificial sea ice. During the expedition TRANSDRIFT III (TDIII, October 1995), different types of natural, newly-formed sea ice (grease ice, nilas and young ice) were sampled in the inner Laptev Sea at the time of freeze-up. The incorporation of sediments took place during calm meteorological conditions then. The characteristics of the clay mineral assemblages of these sedirnents served as references for sea-ice sediments which were sampled from first-year drift ice in the outer Laptev Sea and the adjacent Arctic Ocean during the POLARSTERN expedition ARK-XI/1 (July-September 1995). Based on the clay mineral assemblages, probable incorporation areas for the sedirnents in first-year drift ice could be statistically reconstructed in the inner Laptev Sea (eastern, central, and Western Laptev Sea) as well as in adjacent regions. Comparing the amounts of particulate organic carbon (POC) in sea-ice sediments and in surface sediments from the shelves of potential incorporation areas often reveals higher values in sea-ice sediments (TDIII: 3.6 %DM; ARK-XI/1: 2.3 %DM). This enrichment of POC is probably due to the incorporation process into the sea ice, as could be deducted from maceral analysis and Rock-Eval pyrolysis. Both methods were applied in the present study to particulate organic material (POM) from sea-ice sediments for the first time. It was shown that the POM of the sea-ice sediments from the Laptev Sea and the adjacent Arctic Ocean was dominated by reworked, strongly fragmented, allochthonous (terrigenous) material. This terrigenous component accounted for more than 75 % of all counted macerals. The autochthonous (marine) component was also strongly fragmented, and higher in the sediments from newly-formed sea ice (24 % of all counted macerals) as compared to first-year drift ice (17 % of all counted macerals). Average hydroge indices confirmed this pattern and were in the transition zone between kerogen types II and III (TDIII: 275 mg KW/g POC; ARK-XI/1: 200 mg KW/g POC). The sediment loads quantified in natural sea ice (TDIII: 33.6 mg/l, ARK-XI/1: 49.0 mg/l) indicated that sea-ice sediments are an important factor for the sediment budget in the Laptev Sea. In particular during the incorporation phase in autumn and early winter, about 12 % of the sediment load imported annually by rivers into the Laptev Sea can be incorporated into sea ice and redistributed during calm meteorological conditions. Single entrainment events can incorporate about 35 % of the river input into the sea ice (ca. 9 x 10**6 t) and export it via the Transpolar Drift from the Eurasian shelf to the Fram Strait.

Physical oceanography and current meter measurements on the Gulf of Lion continental margin between June 1993 and July 1996

Nine hydrographic cruises were performed on the Gulf of Lion continental margin between June 1993 and July 1996. These observations are analysed to quantify the fluxes of particulate matter and organic carbon transported along the slope by the Northern Current and to characterise their seasonal variability. Concentration of particulate matter and organic carbon are derived from light-transmission data and water sample analyses. The circulation is estimated from the geostrophic current field. The uncertainty on the transport estimate, related to the error on the prediction of particle concentrations from light-transmission data and the error on velocities, is assessed. The particulate matter inflow entering the Gulf of Lion off Marseille is comparable to the Rhône River input and varies seasonally with a maximum transport between autumn and spring. These modifications result from variations of the water flux rather than variations of the particulate matter concentration. Residual transports of particulate matter and organic carbon across the entire Gulf of Lion are calculated for two cruises enclosing the domain that were performed in February 1995 and July 1996. The particulate matter budgets indicate a larger export from the shelf to deep ocean in February 1995 (110 ± 20 kg/s) than in July 1996 (25 ± 18 kg/s). Likewise, the mean particulate organic carbon export is 12.8 ± 0.5 kg/s in February 1995 and 0.8 ± 0.2 kg/s in July 1996. This winter increase is due to larger allochthonous and autochthonous inputs and also to enhanced shelf-slope exchange processes, in particular the cascading of cold water from the shelf. The export of particulate matter by the horizontal currents is moreover two orders of magnitude larger than the vertical particulate fluxes measured at the same time with sediment traps on the continental slope.

Mesozooplankton of the northern Barents Sea in October 1998

Qualitative and quantitative mesozooplankton composition was examined on materials collected during an expedition carried out in October 1998 onboard the research icebreaker Akademik Fedorov. At different stations number of species varied from 25 to 33; wet biomass - from 20 to 109 g/m**2. Flux of autochthonous organic matter through plankton communities calculated from data on structural and functional analysis was from 2 to 40 mg C/m**2/day.

Pollen analysis of a peat profile from the Rieseberger Moor, Lower Saxony, Germany

The Rieseberger Moor is a fen, 145 hectares in size, situated about 20 km east of Brunswick (Braunschweig), Lower Saxony, Germany. Peat was dug in the fen - with changing intensity - since the mid-18th century until around AD 1955. According to Schneekloth & Schneider (1971) the remaining peat (fen and wood peat) is predominantly 1.5 to 2 m thick (maximum 2.7 m). Part of the fen - now a nature reserve (NSG BR 005) - is wooded (Betula, Salix, Alnus). For more information on the Rieseberger Moor see http://de.wikipedia.org/wiki/Rieseberger_Moor. Willi Selle was the first to publish pollen diagrams from this site (Selle 1935, profiles Rieseberger Torfmoor I and II). This report deals with a 2.2 m long profile from the wooded south-eastern part of the fen consisting of strongly decomposed fen peat taken A.D. 1965 and studied by pollen analysis in the same year. The peat below 1.45 m contained silt and clay, samples 1.48 and 1.58 m even fine sand. These samples had to be treated with HF (hydrofluoric acid) in addition to the treatment with hot caustic potash solution. The coring ended in sandy material. The new pollen data reflect the early part of the known postglacial development of the vegetation of this area: the change from a birch dominated forest to a pine forest and the later spreading of Corylus and of the thermophilous deciduous tree genera Quercus, Ulmus, Tilia and Fraxinus followed by the expansion of Alnus. The new data are in agreement with Selle's results, except for Alnus, which in Selle's pollen diagram II shows high values (up to 42% of the arboreal pollen sum) even in samples deposited before Corylus and Quercus started to spread. On contrary the new pollen diagram shows that alder pollen - although present in all samples - is frequent in the three youngest pollen spectra only. A period with dominating Alnus as seen in the uppermost part of Selle's pollen diagrams is missing. The latter is most likely the result of peat cutting at the later coring site, whereas the early, unusually high alder values of Selle's pollen study are probably caused by contamination of the pollen samples with younger peat. Selle took peat samples usually with a "Torfbohrer" (= Hiller sampler). This side-filling type of sampler with an inner chamber and an outer loose jacket offers - if not handled with appropriate care - ample opportunities to contaminate older peat with carried off younger material. Pollen grains of Fagus (2 % of the arboreal pollen sum) were found in two samples only, namely in the uppermost samples of the new profile (0.18 m) and of Selle's profile I (0.25 m). If this pollen is autochthonous, with other words: if this surface-near peat was not disturbed by human activities, the Fagus pollen indicates an Early Subboreal age of this part of the profile. The accumulation of the Rieseberg peat started during the Preboreal. Increased values of Corylus, Quercus and Ulmus indicate that sample 0.78 m of the new profile is the oldest Boreal sample. The high Alnus values prove the Atlantic age of the younger peat. Whether Early Subboreal peat exists at the site is questionable, but evidently none of the three profiles reaches to Late Subboreal time, when Fagus spread in the region. Did peat-growth end during the Subboreal? Did younger peat exist, but got lost by peat cutting or has younger peat simply not yet been found in the Rieseberg fen? These questions cannot be answered with this study. The temporary decline of the curve of Pinus for the benefit of Betula during the Preboreal, unusual for this period, is contemporaneous with the deposition of sand (Rieseberger Moor II, 1.33 - 1,41 m; samples 1.48 and 1.58 m of the new profile) and must be considered a local phenomenon. Literature: Schneekloth, Heinrich & Schneider, Siegfried (1971). Die Moore in Niedersachsen. 2. Teil. Bereich des Blattes Braunschweig der Geologischen Karte der Bundesrepublik Deutschland (1:200000). - Schriften der wirtschaftswissenschaftlichen Gesellschaft zum Studium Niedersachsens e.V. Reihe A I., Band 96, Heft 2, 83 Seiten, Göttingen. Selle, Willi (1935) Das Torfmoor bei Rieseberg. - Jahresbericht des Vereins für Naturwissenschaft zu Braunschweig, 23, 46-58, Braunschweig.

Domes of adobe and stone on the rural architecture of centre of Castilla y León (Spain)

In the centre of Castilla y León (extensive zone of Spain) still there are some examples of the old rural buildings linked to the economic activities that have been developed in the agrarian field. These are called chozos and casetas, and they have been erected with domed solutions using the autochthonous materi-als: the mud in the region of Tierra de Campos and the stone in the region of Montes Torozos. The influence of traditional construction techniques of both elements has generated a singular typological range rarely seen in the rest of the Península Ibérica. All different types of domes found in this place will be explained from its construction process, adding its structural capacity and energy bioclimatic qualities. -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- En el centro de Castilla y León todavía se mantienen algunos ejemplos de antiguas construcciones rurales vinculadas a las actividades económicas que se han desarrollado en el ámbito agrario. Éstas, conocidas como chozos y casetas, han sido ejecutadas con soluciones cupuliformes empleándose los materiales que más a mano se disponen, siendo el barro más característico en la región de Tierra de Campos y la piedra en la comarca de Montes Torozos. La influencia de las técnicas constructivas tradicionales de ambos elementos ha generado un abanico tipológico singular poco visto en el resto de la península. Los diferentes tipos de cúpulas encontrados se explicarán desde su proceso constructivo, añadiendo su capacidad estructural y sus cualidades bioclimáticas.

Caracterización de poblaciones de vid silvestre de la Península Ibérica

La vid silvestre se considera como el ancestro autóctono de las vides cultivadas y una enorme reserva genética en peligro de extinción. La prospección llevada a cabo entre 2003 y 2004 permitió catalogar 51 localizaciones de vides silvestres españolas, la mayoría de ellas ubicadas en riberas de ríos. Estos ejemplares se incluyeron en el Banco de Germoplasma de la Finca "El Encín" (BGVCAM - Alcalá de Henares, Madrid, España). En primer lugar, se caracterizó la cantidad y la distribución de su diversidad genética utilizando 25 loci empleando microsatélites nucleares (SSR). Hemos analizado también la posible coexistencia en el hábitat natural de vides silvestres con vides cultivadas naturalizadas y portainjertos. De este modo, los análisis fenotípicos y genéticos identificaron el 19% de las muestras recogidas como derivadas de genotipos cultivados, siendo, o bien vides cultivadas naturalizadas o genotipos híbridos derivados de cruces espontáneos entre vides silvestres y cultivadas. La diversidad genética de las poblaciones de vides silvestres fue similar a la observada en el grupo de las cultivadas. El análisis molecular mostró que el germoplasma de cultivadas y silvestres es genéticamente divergente con bajo nivel de introgresión. Se ha identificado cuatro grupos genéticos, con dos de ellos fundamentalmente representados por los genotipos de vides cultivadas y dos por las accesiones silvestres. El análisis de los vínculos genéticos entre las vides silvestres y cultivadas podría sugerir una contribución genética de las accesiones silvestres españolas a las actuales variedades occidentales. En segundo lugar, se realizó un profundo estudio morfológico "ex situ " y se contrastaron con los resultados de la caracterización realizada en 182 variedades comerciales españolas de la misma colección. Todos los individuos silvestres mostraron diferencias morfológicas con Vitis vinifera L subsp. vinifera, pero no se encontraron diferencias significativas dentro Vitis vinifera L. subsp. sylvestris, ni por localización geográfica ni por sexo. Los resultados de este estudio describen las principales características morfológicas de las vides silvestres españolas y sus rasgos diferenciales con su pariente cultivada. Por último, se analizó la composición antociánica presente en 21 accesiones de vides silvestres de la Península Ibérica conservadas en el BGVCAM de la Finca "El Encín" y seleccionadas basándose en diferencias ampelográficas y caracterización molecular. La concentración de antocianinas es similar la encontrad en vides cultivadas con destino a la vinificación. Las accesiones estudiadas mostraron una variabilidad considerable en su perfil antociánico y fue posible distinguir varios grupos. Sin embargo, la presencia de material silvestre con perfiles antociánicos poco comunes o inexistentes en variedades españolas, sugiere que la variabilidad genética relacionada con antocianinas en poblaciones españolas de vides silvestres podría ser más alta que la de variedades cultivadas comúnmente consideradas de origen español. ABSTRACT The wild grapevine is considered an autochthonous relative of cultivated vines and a huge gene pool endangered in Europe. Prospecting carried out between 2003 and 2004 enabled to inventory 51 Spanish sites with wild grapevines, most of them located near rivers. These individuals were grafted in the collection of "El Encín" (BGVCAM - Alcalá de Henares, Madrid, Spain). Firstly, werw characterized the amount and distribution of their genetic diversity using 25 nuclear SSR loci. We have also analysed the possible coexistence in the natural habitat of wild grapevines with naturalized grapevine cultivars and rootstocks. In this way, phenotypic and genetic analyses identified 19% of the collected samples as derived from cultivated genotypes, being either naturalized cultivars or hybrid genotypes derived from spontaneous crosses between wild and cultivated grapevines. The genetic diversity of wild grapevine populations was similar than that observed in the cultivated group. The molecular analysis showed that cultivated germplasm and wild germplasm are genetically divergent with low level of introgression. We identified four genetic groups, with two of them fundamentally represented among cultivated genotypes and two among wild accessions. The analyses of genetic relationships between wild and cultivated grapevines could suggest a genetic contribution of wild accessions from Spain to current Western cultivars. Secondly, a morphological study was done "ex situ" and were compared with data from 182 Spanish commercial cultivars grown in the same collection. All wild individuals showed morphological differences with Vitis vinifera L. ssp. vinifera but no significant differences were found within Vitis vinifera L subsp. sylvestris neither by geographic origin nor by sex. A pattern with the main characteristics of Spanish wild grapevines is suggested. Ultimately, were investigated the anthocyanin composition of 21 mostly Spanish wild grapevine accessions preserved at BGVCAM "El Encín" and selected in consideration of observed ampelographic differences and molecular characterization. Total anthocyanin concentration was similar to that found in winegrape cultivars. The accessions studied showed considerable variability in their anthocyanin fingerprints and it was possible to distinguish several groups, similar to previous reports on the anthocyanin fingerprint of winegrapes. The anthocyanin composition of wild grapevine accessions was similar to that of cultivated grapes. Nevertheless, the presence of wild accessions with anthocyanin fingerprints uncommon or nonexistent in Spanish cultivated varieties suggests that the genetic variability related to anthocyanins in Spanish wild grapevine populations may be higher than that of cultivated varieties commonly considered of Spanish origin.

Proyecto y lugar en la arquitectura doméstica de Jørn Utzon

En medio de un bosque danés, de altos arboles que se mueven al fuerte viento nórdico bajo el débil sol de las latitudes altas, y cargado de unos cuantos tableros de madera que consiguió de una exposición ya terminada, realizó Utzon su maqueta a escala real de su primera casa familiar en Hellebæk (1950-52) a la edad de treinta y dos años. De la misma manera que el pintor William Turner necesitó atarse a lo alto de un mástil de un barco, para vivir en directo una de las muchas tormentas que tantas y tantas veces había pintado en sus cuadros, el joven Utzon consideró indispensable introducirse dentro de la maqueta de su propia casa antes de construirla, para valorar in situ las potencialidades de aquel proyecto en relación al lugar. La obra de Jørn Utzon (1918-2008) es una arquitectura expectante y atenta del lugar donde se ubica. Jørn Utzon es un arquitecto de origen nórdico, que descubre su verdadera idiosincrasia en la cultura mediterránea, cultura en la que reside durante casi la mitad de toda su vida. Esta tesis se ha centrado en analizar exhaustivamente la relación de su arquitectura doméstica con el lugar donde se halla. Aspecto tan citado en la bibliografía existente de su obra, aunque nunca desarrollado de manera exhaustiva. El objetivo del análisis ha sido intentar encontrar invariantes o patrones que pudieran subyacer en su obra residencial en relación a ese tema. Para dicho análisis, se ha tomado una muestra suficientemente amplia de veinte viviendas o conjuntos residenciales (entre ellas sus cuatro viviendas familiares proyectadas), repartidas por cinco países (Suecia, Dinamarca, Reino Unido, España y Nueva Gales del Sur), que constituyen la tercera parte de su obra doméstica y la mitad de su obra construida residencial, así como las citas explícitas del autor sobre este tema en su obra escrita, y los planos o croquis de su obra gráfica. Como metodología de trabajo se ha recurrido a la consulta de las fuentes primarias: viajando y conociendo in-situ las casas seleccionadas en Dinamarca, Suecia, España y Australia; viviendo un mes en una de las casas (Can Lis) gracias a una beca del Gobierno danés y la Utzon Foundation; y realizando entrevistas a las personas que más cerca estuvieron del arquitecto en su entorno familiar y profesional. Asimismo, también se ha publicado parte de su contenido en medios internacionales: 4th International Utzon Symposium (7/3/2013-9/3/2014) y la página web oficial de Can Lis dependiente de la Utzon Foundation (www.canlis.dk). Las doce invariantes encontradas en relación al proyecto y lugar en los proyectos seleccionados, han sido agrupadas en torno a tres grandes elementos sobre los que Utzon constantemente reflexiona en sus escritos propios: horizonte, sol y material autóctono. Elementos que tienen su origen en la influencia que la navegación tuvo en su vida, y en su carácter espiritual y austero en lo material. La historia de Utzon es la de un nórdico, de vocación navegante, que encuentra su lugar en la cultura mediterránea, rodeado entre piedras de Marés, mientras divisa en silencio el horizonte marino en el umbral entre luz y sombra. ABSTRACT In the middle of a Danish forest, with high trees which move with the Nordic wind under the weak sun of high latitudes, and with the help of some wooden canvases acquired from an already completed exhibition, Jørn Utzon built a real-scale model of his first family house in Hellebæk (1950-52) at the age of thirty-two. In the same way that William Turner needed to be tied up on the top of a boat flagpole in order to have a first-hand experience of one of the many storms that he had depicted in his paintings so many times before, the young Utzon thought it was crucial to go into the model of his own house before building it, to evaluate in situ the potential of that project in relation to the place. Utzon’s work is architecture interested in and attentive of the place where it is situated. Jørn Utzon (1918-2008) is an architect of Nordic origin who discovered his own idiosyncrasy in the Mediterranean culture, in which he resided for half of his live. This thesis has focused on an exhaustive analysis of the relation between his domestic architecture and the place where it is located. This issue has been often cited in the existing bibliography, although it has never been exhaustively developed. The analysis objective has been to attempt to find invariants and patterns that could exist in his domestic work in relation to this subject. For this analysis, a sufficiently large sample has been selected: twenty houses or housing complexes (among others his own four family houses), distributed in five countries (Sweden, Denmark, United Kingdom, Spain and New South Wales), which constitute the third part of his domestic work, and half of his residential constructed projects, as well as Utzon’s written texts about this theme, and the drawings and sketches of his graphic work. The methodology used was based on consultation of primary sources: travelling and examining in situ the selected houses in Denmark, Sweden, Spain and Australia; living for a month in one of the houses (Can Lis) thanks to a research grant from the Danish Government and the Utzon Foundation; and interviewing people from his closest family and professional circles. Furthermore, part of the thesis has been published in international media: 4th International Utzon Symposium (7/3/2013-9/3/2014) and on the official web site of Can Lis, an Utzon Foundation subsidiary(www.canlis.dk). The twelve invariants discovered in relation to the project and the location of the selected projects, have been grouped according to three elements which Utzon continuously reflects upon in his own writings: the horizon, the sun and autochthonous material. Elements which originate from the influence that navigation had in his life, and from his spiritual and austere character. The story of Utzon is that of a Nordic person, with the vocation of a navigator, who found his place in the Mediterranean culture, surrounded with Marés stones, while silently making out the sea horizon on the threshold between light and shadow.

ORLANDO COSTAS: ENSAIOS NO CAMINHO PARA UMA PASTORAL EVANGÉLICA LATINO-AMERICANA

Nesta pesquisa se propõe analisar a pastoral evangélica latino-americana elaborada por Orlando Costas. Teólogo pastoralista, missiólogo e de origem porto-riquenha, Costas elaborou método e metodologia de pastoral a partir de sua confissão religiosa evangelical em diálogo ecumênico e em consonância crítica com a situação política, econômica, social e religiosa de Porto Rico e da América Latina. Costas, juntamente com Emilio Castro, foi um dos primeiros a lançar as bases para uma pastoral evangélica visando ao homem latino-americano. Criticou o modelo da teologia pastoral norte-atlântica centrada no pastor com sujeito da ação pastoral da igreja alegando ser; repetitiva, profissional e eclesiocêntrica. A pesquisa foi realizada em três passos, que se realizam nos capítulos um, dois e três, respectivamente, compreender o contexto político, econômico, social e religioso da vida de Orlando Costas a partir de Porto Rico, suas experiências de conversão-ruptura dentro da sua tradição religiosa e a nova percepção pastoral; analisar o desenvolvimento histórico teológico da pastoral evangélica, ou seja, os movimentos, conferências, instituições e teólogos que influenciaram o pensamento de Costas; e, apresentar os fundamentos missiológicos e teológicos da pastoral evangélica, em que se demonstra que a pastoral de Costas é missiológico-pastoral, pois assume a missio Dei como princípio arquitetônico e a pastoral como princípio hermenêutico para a ação missional e pastoral. Conclui-se que a proposta de Costas é de uma pastoral evangélica e ecumênica, contextual e autóctone, dentro e fora da igreja.(AU)

ORLANDO COSTAS: ENSAIOS NO CAMINHO PARA UMA PASTORAL EVANGÉLICA LATINO-AMERICANA

Nesta pesquisa se propõe analisar a pastoral evangélica latino-americana elaborada por Orlando Costas. Teólogo pastoralista, missiólogo e de origem porto-riquenha, Costas elaborou método e metodologia de pastoral a partir de sua confissão religiosa evangelical em diálogo ecumênico e em consonância crítica com a situação política, econômica, social e religiosa de Porto Rico e da América Latina. Costas, juntamente com Emilio Castro, foi um dos primeiros a lançar as bases para uma pastoral evangélica visando ao homem latino-americano. Criticou o modelo da teologia pastoral norte-atlântica centrada no pastor com sujeito da ação pastoral da igreja alegando ser; repetitiva, profissional e eclesiocêntrica. A pesquisa foi realizada em três passos, que se realizam nos capítulos um, dois e três, respectivamente, compreender o contexto político, econômico, social e religioso da vida de Orlando Costas a partir de Porto Rico, suas experiências de conversão-ruptura dentro da sua tradição religiosa e a nova percepção pastoral; analisar o desenvolvimento histórico teológico da pastoral evangélica, ou seja, os movimentos, conferências, instituições e teólogos que influenciaram o pensamento de Costas; e, apresentar os fundamentos missiológicos e teológicos da pastoral evangélica, em que se demonstra que a pastoral de Costas é missiológico-pastoral, pois assume a missio Dei como princípio arquitetônico e a pastoral como princípio hermenêutico para a ação missional e pastoral. Conclui-se que a proposta de Costas é de uma pastoral evangélica e ecumênica, contextual e autóctone, dentro e fora da igreja.(AU)

Climate and infectious disease: Use of remote sensing for detection of Vibrio cholerae by indirect measurement

It has long been known that cholera outbreaks can be initiated when Vibrio cholerae, the bacterium that causes cholera, is present in drinking water in sufficient numbers to constitute an infective dose, if ingested by humans. Outbreaks associated with drinking or bathing in unpurified river or brackish water may directly or indirectly depend on such conditions as water temperature, nutrient concentration, and plankton production that may be favorable for growth and reproduction of the bacterium. Although these environmental parameters have routinely been measured by using water samples collected aboard research ships, the available data sets are sparse and infrequent. Furthermore, shipboard data acquisition is both expensive and time-consuming. Interpolation to regional scales can also be problematic. Although the bacterium, V. cholerae, cannot be sensed directly, remotely sensed data can be used to infer its presence. In the study reported here, satellite data were used to monitor the timing and spread of cholera. Public domain remote sensing data for the Bay of Bengal were compared directly with cholera case data collected in Bangladesh from 1992–1995. The remote sensing data included sea surface temperature and sea surface height. It was discovered that sea surface temperature shows an annual cycle similar to the cholera case data. Sea surface height may be an indicator of incursion of plankton-laden water inland, e.g., tidal rivers, because it was also found to be correlated with cholera outbreaks. The extensive studies accomplished during the past 25 years, confirming the hypothesis that V. cholerae is autochthonous to the aquatic environment and is a commensal of zooplankton, i.e., copepods, when combined with the findings of the satellite data analyses, provide strong evidence that cholera epidemics are climate-linked.

Estudo da expansão da Leishmaniose Visceral no estado de São Paulo e de fatores intervenientes

INTRODUÇÃO: Leishmaniose visceral (LV) é uma doença negligenciada que afeta milhões de pessoas no mundo e que constitui um grave problema de saúde pública. OBJETIVOS: Descrever no tempo e no espaço, a dispersão de Lutzomyia longipalpis e a expansão da LV no estado de São Paulo (SP); identificar fatores associados a estes processos. MÉTODOS: Foram realizados estudos descritivos, ecológicos e de análise de sobrevida. Informações sobre o vetor e os casos foram obtidas na Superintendência de Controle de Endemias e no Sistema de Informações de Agravos de Notificação para o período de 1997 a 2014. A área de estudo foi composta pelos 645 municípios de SP. Foram produzidos mapas temáticos e de fluxo e calcularam-se incidência, mortalidade e letalidade por LV em humanos (LVH). Utilizou-se a técnica de análise de sobrevida (Curvas de Kaplan-Meier e Regressão de Cox) para a identificação de fatores associados à dispersão do vetor e expansão da LV. RESULTADOS: A partir da detecção de Lu. longipalpis em Araçatuba em 1997, deram-se a ocorrência do primeiro caso canino (LVC) (1998) e o primeiro caso humano (LVH) autóctones (1999) em SP. Até 2014, foi detectada a presença do vetor em 173 (26,8 por cento ) municípios, LVC em 108 (16,7 por cento ) e LVH em 84 (13 por cento ). A expansão dos três fenômenos ocorreu no sentido noroeste para sudeste e se deram a velocidades constantes. Na região de São José do Rio Preto, a dispersão do vetor deu-se por vizinhança com municípios anteriormente infestados, a expansão da LV relacionou-se com os municípios sede das microrregiões e a doença ocorreu com maior intensidade nas áreas periféricas dos municípios. A presença da Rodovia Marechal Rondon e a divisa com o Mato Grosso do Sul foram fatores associados à ocorrência dos três eventos, assim como a presença da Rodovia Euclides da Cunha para presença do vetor e casos caninos, e, presença de presídios para casos humanos. CONCLUSÕES: A dispersão do vetor e da LV em SP iniciou-se, a partir de 1997, próximo à divisa com o estado do Mato Grosso do Sul, avançou no sentido noroeste para sudeste, na trajetória da rodovia Marechal Rondon, e ocorreu em progressão aritmética, com as sedes das microrregiões de SP tendo papel preponderante neste processo. A ocorrência autóctone de LVC e LVH iniciou-se na sequência da detecção de Lu. longipalpis em Araçatuba e de seu espalhamento por SP e não a partir dos locais onde anteriormente ele já estava presente. O uso da análise de sobrevida permitiu identificar fatores associados à dispersão do vetor e a expansão da LV. Os resultados deste estudo podem ser úteis para aprimorar as atividades de vigilância e controle da LV, no sentido de retardar sua expansão e/ou de mitigar seus efeitos, quando de sua ocorrência.

New data on the Vrancea Nappe (Moldavidian Basin, Outer Carpathian Domain, Romania): paleogeographic and geodynamic reconstructions

A study has been performed on the Cretaceous to Early Miocene succession of the Vrancea Nappe (Outer Carpathians, Romania), based on field reconstruction of the stratigraphic record, mineralogical-petrographic and geochemical analyses. Extra-basinal clastic supply and intra-basinal autochthonous deposits have been differentiated, appearing laterally inter-fingered and/or interbedded. The main clastic petrofacies consist of calcarenites, sub-litharenites, quartzarenites, sub-arkoses, and polygenic conglomerates derived from extra-basinal margins. An alternate internal and external provenance of the different supplies is the result of the paleogeographic re-organization of the basin/margins system due to tectonic activation and exhumation of rising areas. The intra-basinal deposits consist of black shales and siliceous sediments (silexites and cherty beds), evidencing major environmental changes in the Moldavidian Basin. Organic-matter-rich black shales were deposited during anoxic episodes related to sediment starvation and high nutrient influx due to paleogeographic isolation of the basin caused by plate drifting. The black shales display relatively high contents in sub-mature to mature, Type II lipidic organic matter (good oil and gas-prone source rocks) constituting a potentially active petroleum system. The intra-basinal siliceous sediments are related to oxic pelagic or hemipelagic environments under tectonic quiescence conditions although its increase in the Oligocene part of the succession can be correlated with volcanic supplies. The integration of all the data in the “progressive reorientation of convergence direction” Carpathian model, and their consideration in the framework of a foreland basin, led to propose some constrains on the paleogeographic-geodynamic evolutionary model of the Moldavidian Basin from the Late Cretaceous to the Burdigalian.

Stable oxygen and carbon isotope ratios of Globigerinoides obliquus of quantitative range chart of the ostracodes in the Pliocene-Pleistocene interval of ODP Hole 107-654A

Deep-water benthic ostracodes from the Pliocene-Pleistocene interval of ODP Leg 107, Hole 654A (Tyrrhenian Sea) were studied. From a total of 106 samples, 40 species considered autochthonous were identified. Detailed investigations have established the biostratigraphic distribution of the most frequent ostracode taxa. The extinction levels of Agrenocythere pliocenica (a psychrospheric ostracode) in Hole 654A and in some Italian land sections lead to the conclusion that the removal of psychrospheric conditions took place in the Mediterranean Sea during or after the time interval corresponding to the Small Gephyrocapsa Zone (upper part of early Pleistocene), and not at the beginning of the Quaternary, as previously stated. Based on a reduced matrix of quantitative data of 63 samples and 20 variables of ostracodes, four varimax assemblages were extracted by a Q-mode factor analysis. Six factors and eight varimax assemblages were recognized from the Q-mode factor analysis of the quantitative data of 162 samples and 47 variables of the benthic foraminifers. The stratigraphic distributions of the varimax assemblages of the two faunistic groups were plotted against the calcareous plankton biostratigraphic scheme and compared in order to trace the relationship between the benthic foraminifers and ostracodes varimax assemblages. General results show that the two populations, belonging to quite different taxa, display almost coeval changes along the Pliocene-Pleistocene sequence of Hole 654A, essentially induced by paleoenvironmental modifications. Mainly on the base of the benthic foraminifer assemblages (which are quantitatively better represented than the ostracode assemblages), it is possible to identify such modifications as variations in sedimentation depth and in bottom oxygen content.