Waddlia chondrophila induces systemic infection, organ pathology, and elicits Th1-associated humoral immunity in a murine model of genital infection

Waddlia chondrophila is a known bovine abortigenic Chlamydia-related bacterium that has been associated with adverse pregnancy outcomes in human. However, there is a lack of knowledge regarding how W. chondrophila infection spreads, its ability to elicit an immune response and induce pathology. A murine model of genital infection was developed to investigate the pathogenicity and immune response associated with a W. chondrophila infection. Genital inoculation of the bacterial agent resulted in a dose-dependent infection that spread to lumbar lymph nodes and successively to spleen and liver. Bacterial-induced pathology peaked on day 14, characterized by leukocyte infiltration (uterine horn, liver, and spleen), necrosis (liver) and extramedullary hematopoiesis (spleen). Immunohistochemistry demonstrated the presence of a large number of W. chondrophila in the spleen on day 14. Robust IgG titers were detected by day 14 and remained high until day 52. IgG isotypes consisted of high IgG2a, moderate IgG3 and no detectable IgG1, indicating a Th1-associated immune response. This study provides the first evidence that W. chondrophila genital infection is capable of inducing a systemic infection that spreads to major organs, induces uterus, spleen, and liver pathology and elicits a Th1-skewed humoral response. This new animal model will help our understanding of the mechanisms related to intracellular bacteria-induced miscarriages, the most frequent complication of pregnancy that affects one in four women.

The intracellular parasite Theileria parva protects infected T cells from apoptosis.

Parasites have evolved a plethora of strategies to ensure their survival. The intracellular parasite Theileria parva secures its propagation and spreads through the infected animal by infecting and transforming T cells, inducing their continuous proliferation and rendering them metastatic. In previous work, we have shown that the parasite induces constitutive activation of the transcription factor NF-kappaB, by inducing the constitutive degradation of its cytoplasmic inhibitors. The biological significance of NF-kappaB activation in T. parva-infected cells, however, has not yet been defined. Cells that have been transformed by viruses or oncogenes can persist only if they manage to avoid destruction by the apoptotic mechanisms that are activated on transformation and that contribute to maintain cellular homeostasis. We now demonstrate that parasite-induced NF-kappaB activation plays a crucial role in the survival of T. parva-transformed T cells by conveying protection against an apoptotic signal that accompanies parasite-mediated transformation. Consequently, inhibition of NF-kappaB nuclear translocation and the expression of dominant negative mutant forms of components of the NF-kappaB activation pathway, such as IkappaBalpha or p65, prompt rapid apoptosis of T. parva-transformed T cells. Our findings offer important insights into parasite survival strategies and demonstrate that parasite-induced constitutive NF-kappaB activation is an essential step in maintaining the transformed phenotype of the infected cells.

A Model Study of the Circulation in the Pearl River Estuary (PRE) and Its Adjacent Coastal Waters: 2. Sensitivity Experiments

The Princeton Ocean Model is used to study the circulation in the Pear River Estuary (PRE) and the adjacent coastal waters in the winter and summer seasons. Wong et al. [2003] compares the simulation results with the in situ measurements collected during the Pearl River Estuary Pollution Project (PREPP). In this paper, sensitivity experiments are carried out to examine the plume and the associated frontal dynamics in response to seasonal discharges and monsoon winds. During the winter, convergence between the seaward spreading plume water and the saline coastal water sets up a salinity front that aligns from the northeast to the southwest inside the PRE. During the summer the plume water fills the PRE at the surface and spreads eastward in the coastal waters in response to the prevailing southwesterly monsoon. The overall alignment of the plume is from the northwest to the southeast. The subsurface front is similar to that in the winter and summer except that the summer front is closer to the mouth and the winter front closer to the head of the estuary. Inside the PRE, bottom flows are always toward the head of the estuary, attributed to the density gradient associated with the plume front. In contrast, bottom flows in the shelf change from offshore in winter to onshore in summer, reflecting respectively the wintertime downwelling and summertime upwelling. Wind also plays an essential role in controlling the plume at the surface. An easterly wind drives the plume westward regardless winter or summer. The eastward spreading of the plume during the summer can be attributed to the southerly component of the wind. On the other hand, the surface area of the plume is positively proportional to the amount of discharge.

CYTOLOGICAL, ULTRASTRUCTURAL, AND BIOCHEMICAL STUDIES OF THE STRUCTURE OF PREMATURELY CONDENSED CHROMOSOMES

The phenomenon of premature chromosome condensation, resulting from fusion between mitotic and interphase cells, includes dissolution of the interphase nuclear framework, thus allowing a direct visualization of interphase chromosomes. Light microscope morphology of prematurely condensed chromosomes (PCC) from synchronized HeLa cells supports the model of an interphase "chromosome condensation cycle". PCC are increasingly attenuated as cells progress through G(,1). A maximum degree of decondensation is observed at active sites of DNA replication during S phase, and a condensed morphology is rapidly resumed following completion of replication of a chromosome segment.^ To permit ultrastructural and biochemical studies of PCC, a procedure was developed to induce premature chromosome condensation at high frequency. This was achieved by polyethylene glycol (PEG)-mediated fusion of a dense monolayer of mitotic and interphase cells induced by centrifugation onto lectin-coated culture dishes. Using this method, PCC induction frequencies of 60-90% are routinely obtained.^ Scanning electron microscope analysis of PCC spreads revealed that the extension of PCC during progression through G(,1) is accompanied by a transition of the basic 30 nm chromatin fiber from tightly packed looping fibers to extended longitudinal fibers. Sites of active DNA replication is S-PCC were indicated to be organized a single longitudinal fibers. Following replication of a chromosome segment, a rapid reorganization from the extended longitudinal fiber to packed looping fibers occurs. The postreplication maturation process appears to include the assembly of a chromosome core consisting of multiple longitudinal fibers.^ The role of histone H1 phosphorylation in PCC formation was investigated by acidurea polyacrylamide gel electrophoresis of total histone extracted from metaphase chromosomes and PCC following high frequency fusion. This investigation failed to demonstrate an extensive phosphorylation of H1 associated with PCC formation. However, significant dephosphorylation of superphosphorylated metaphase chromosome H1 was observed, indicating that interphase H1-phosphatase activity is dominant over metaphase H1 kinase activity. These observations provide evidence against models suggesting a role for H1 superphosphorylation in triggering mitotic condensation of chromosomes. ^

US Corporate Default Swap Valuation: The Market Liquidity Hypothesis and Autonomous Credit Risk

This paper develops a reduced form three-factor model which includes a liquidity proxy of market conditions which is then used to provide implicit prices. The model prices are then compared with observed market prices of credit default swaps to determine if swap rates adequately reflect market risks. The findings of the analysis illustrate the importance of liquidity in the valuation process. Moreover, market liquidity, a measure of investors. willingness to commit resources in the credit default swap (CDS) market, was also found to improve the valuation of investors. autonomous credit risk. Thus a failure to include a liquidity proxy could underestimate the implied autonomous credit risk. Autonomous credit risk is defined as the fractional credit risk which does not vary with changes in market risk and liquidity conditions.

(Table 1) Iceberg characteristics and start and end date and location of iceberg buoys in the Weddell Sea

The drift of 52 icebergs tagged with GPS buoys in the Weddell Sea since 1999 has been investigated with respect to prevalent drift tracks, sea ice/iceberg interaction, and freshwater fluxes. Buoys were deployed on small- to medium-sized icebergs (edge lengths ? 5 km) in the southwestern and eastern Weddell Sea. The basin-scale iceberg drift of this size class was established. In the western Weddell Sea, icebergs followed a northward course with little deviation and mean daily drift rates up to 9.5 ± 7.3 km/d. To the west of 40°W the drift of iceberg and sea ice was coherent. In the highly consolidated perennial sea ice cover of 95% the sea ice exerted a steering influence on the icebergs and was thus responsible for the coherence of the drift tracks. The northward drift of buoys to the east of 40°W was interrupted by large deviations due to the passage of low-pressure systems. Mean daily drift rates in this area were 11.5 ± 7.2 km/d. A lower threshold of 86% sea ice concentration for coherent sea ice/iceberg movement was determined by examining the sea ice concentration derived from Special Sensor Microwave Imager (SSM/I) and Advanced Microwave Scanning Radiometer for EOS (AMSR-E) satellite data. The length scale of coherent movement was estimated to be at least 200 km, about half the value found for the Arctic Ocean but twice as large as previously suggested. The freshwater fluxes estimated from three iceberg export scenarios deduced from the iceberg drift pattern were highly variable. Assuming a transit time in the Weddell Sea of 1 year, the iceberg meltwater input of 31 Gt which is about a third of the basal meltwater input from the Filchner Ronne Ice Shelf but spreads across the entire Weddell Sea. Iceberg meltwater export of 14.2 × 103 m3 s?1, if all icebergs are exported, is in the lower range of freshwater export by sea ice.

Walter Benjamin : a la búsqueda del tiempo perdido

El objeto de este trabajo es discutir algunas interpretaciones que, sobre la producción de Walter Benjamin, circulan en el espacio académico. Desde mi perspectiva las últimas lecturas han asignado a la obra benjaminiana una significación próxima a la de la teoría de la deconstrucción. Desde mi punto de vista estas interpretaciones se hallan bastante lejos de las preocupaciones que alientan en la producción del autor. La inocultable tensión entre una forma de escritura que puede ser leída sin dudas como poética y la crítica benjaminiana de la estetización fascista de la política, entre un lenguaje que asemeja en muchos casos el de los místicos judíos en el tiempo de la espera tensa del advenimiento del Mesías y el acontecimiento profano de cuya irrupción luminosa Benjamin aguarda la emancipación: la revolución social ha incitado intentos recurrentes de hacer jugar a Benjamin en el terreno de la moda. El modesto propósito de este escrito es el de esbozar apenas una aproximación a Benjamin, una suerte de lectura benjaminiana de Benjamin en una época que a la vez que rinde tributo a su producción (se han multiplicado las ediciones, traducciones, publicaciones, seminarios, cursos) tiende a obliterar en él la dimensión política.

La glosa de 1541 a los refranes que dizen las viejas tras el fuego

Los Refranes que dizen las viejas tras el fuego del Marqués de Santillana tuvieron una extendida difusión en el siglo XVI. La impresión que de ellos hizo Francisco Fernández de Córdoba en 1541 no sólo marca una particular forma de recepción, la de la colección ilustrada con breves glosas morales, sino que, además, fue una de las fuentes fundamentales de Juan de Mal Lara al componer su Philosophia vulgar (Sevilla, 1568). Se realiza aquí una transcripción de esta impresión de 1541 a partir del único impreso que la conserva, mejorando la edición que realizó Sbarbi (1874). Con esto se pretende acercar materiales para el estudio de la primitiva etapa impresa del Refranero hispánico.

Rendición o Resistencia? : El primer discurso latino

En la segunda mitad del siglo IV a. C. Roma ocupa la Italia central y se orienta al dominio de la región meridional en colisión posible con griegos y cartagineses; su influjo se extiende incluso al Jónico cuando varias ciudades de la Magna Grecia solicitan su protección, no así Tarento, que al anclar una escuadra romana en su puerto, reaccionó atacando las naves y una guarnición romana próxima. Tarento, ante una guerra inevitable, pidió apoyo al rey Pirro de Epiro, quien vio la oportunidad de extender hacia occidente las conquistas que Alejandro dejó inconclusas; su invasión de Italia generó fuerte resistencia, pero no le impidió victorias costosas ni su avance hacia el norte; propuso por intermedio de un embajador la rendición y condiciones gravosas para los romanos que estuvieron a punto de ceder. Allí surge Appio Claudia el Ciego, anciano senador ya retirado, que con un discurso breve, preciso y muy logrado produjo un giro en las decisiones de los patricios. Analizamos el discurso conservado por Plutarco en la Vida de Pirro y lo ubicamos dentro de su contexto histórico y político; gracias a él, Roma conservó sus fronteras itálicas y preparó su futura expansión.

La glosa de 1541 a los refranes que dizen las viejas tras el fuego

Los Refranes que dizen las viejas tras el fuego del Marqués de Santillana tuvieron una extendida difusión en el siglo XVI. La impresión que de ellos hizo Francisco Fernández de Córdoba en 1541 no sólo marca una particular forma de recepción, la de la colección ilustrada con breves glosas morales, sino que, además, fue una de las fuentes fundamentales de Juan de Mal Lara al componer su Philosophia vulgar (Sevilla, 1568). Se realiza aquí una transcripción de esta impresión de 1541 a partir del único impreso que la conserva, mejorando la edición que realizó Sbarbi (1874). Con esto se pretende acercar materiales para el estudio de la primitiva etapa impresa del Refranero hispánico.

Rendición o Resistencia? : El primer discurso latino

En la segunda mitad del siglo IV a. C. Roma ocupa la Italia central y se orienta al dominio de la región meridional en colisión posible con griegos y cartagineses; su influjo se extiende incluso al Jónico cuando varias ciudades de la Magna Grecia solicitan su protección, no así Tarento, que al anclar una escuadra romana en su puerto, reaccionó atacando las naves y una guarnición romana próxima. Tarento, ante una guerra inevitable, pidió apoyo al rey Pirro de Epiro, quien vio la oportunidad de extender hacia occidente las conquistas que Alejandro dejó inconclusas; su invasión de Italia generó fuerte resistencia, pero no le impidió victorias costosas ni su avance hacia el norte; propuso por intermedio de un embajador la rendición y condiciones gravosas para los romanos que estuvieron a punto de ceder. Allí surge Appio Claudia el Ciego, anciano senador ya retirado, que con un discurso breve, preciso y muy logrado produjo un giro en las decisiones de los patricios. Analizamos el discurso conservado por Plutarco en la Vida de Pirro y lo ubicamos dentro de su contexto histórico y político; gracias a él, Roma conservó sus fronteras itálicas y preparó su futura expansión.

Rendición o Resistencia? : El primer discurso latino

En la segunda mitad del siglo IV a. C. Roma ocupa la Italia central y se orienta al dominio de la región meridional en colisión posible con griegos y cartagineses; su influjo se extiende incluso al Jónico cuando varias ciudades de la Magna Grecia solicitan su protección, no así Tarento, que al anclar una escuadra romana en su puerto, reaccionó atacando las naves y una guarnición romana próxima. Tarento, ante una guerra inevitable, pidió apoyo al rey Pirro de Epiro, quien vio la oportunidad de extender hacia occidente las conquistas que Alejandro dejó inconclusas; su invasión de Italia generó fuerte resistencia, pero no le impidió victorias costosas ni su avance hacia el norte; propuso por intermedio de un embajador la rendición y condiciones gravosas para los romanos que estuvieron a punto de ceder. Allí surge Appio Claudia el Ciego, anciano senador ya retirado, que con un discurso breve, preciso y muy logrado produjo un giro en las decisiones de los patricios. Analizamos el discurso conservado por Plutarco en la Vida de Pirro y lo ubicamos dentro de su contexto histórico y político; gracias a él, Roma conservó sus fronteras itálicas y preparó su futura expansión.

Composition of Cape Leeuwin Manganese nodule deposit off Western Australia

In 1970 a large deposit of ferromanganese nodules was discovered on the floor of the Indian Ocean southwest of Cape Leeuwin by the research vessel USNS Eltanin. This discovery, which was based largely on bottom photographs from about 20 stations, was discussed by Frakes (1975) and Kennett and Watkins (1975, 1976). The photographs suggest that the deposit spreads, nearly continuously, over 900 000km^2, and cores showed that the nodules are essentially confined to the sediment surface. Kennett and Watkins (op. cit.) pointed to the abundance of ripple and scour marks and current-formed lineations on the present surface, and of extensive disconformities in the cores, as evidence of strong present and past bottom currents in the region. They suggested that the current action had resulted in very low sedimentation rates, which had allowed the nodule field, named by them (1976) the 'Southeast Indian Ocean Manganese Pavement', to develop. In early 1976 the authors used the research vessel HMAS Diamantina for a 10-day cruise in the region to sample the nodules in order to study their chemistry and mineralogy. During the cruise 9 stations were occupied, 8 of them successfully (Figure 1), and about 2000 nodules were recovered from the sea bed. The apparatus used was a light box dredge on the ships hydrowire, which had a breaking strain of about one tonne. Although an attempt was made to reoccupy Eltanin photographic stations, it should be noted that positioning was by celestial navigation, so errors of up to 10 km are possible.

(Table 3) Observations of Mediterranean water lenses in the Eastern North Atlantic

Spreading pattern and mesoscale structure of Mediterranean water outflow in the eastern North Atlantic are studied on the basis of historical hydrographical records. Effect of bottom topography on Mediterranean water distribution is revealed. It is shown that the Mediterranean water outflow is divided into two streams after leaving the Gulf of Cadiz. These are northwestern and southwestern ones; the former is more intensive and spreads in more regular and continuous way. West of the Tejo (Tagus) Plateau it splits into three branches; the most intense of them keeps continuity up to 14°W. The less intensive southwestern stream passes south of the Gettysburg Bank and splits into two branches immediately after the Gulf of Cadiz. From 11°W, this stream has lenticular, intermittent character. West of 14°-15°W all Mediterranean water branches are represented mainly by isolated salty patches. As a result of historical data analysis in the 32°-44°N, 8°-22°W area, 30 Mediterranean water lenses have been found; 12 of them had not been previously mentioned in publications. A table of main parameters of Mediterranean water lenses is presented. It includes data of 108 observations from 1911 to 1993.

Physiography of the Orca Seamount in the Bransfield Strait, Antarctic Peninsula

Extract from related chapter 5.5.2 in reference: The Orca Seamount was discovered in the central basin of the Bransfield Strait around the posit 62°26'S and 58°24'W on the west side of the Antarctic Peninsula, the most western area of the south polar continent. Through the discovery was made known in 1987, it was only during three bathymetric surveys with high resolution fan echosounders between 1993 and 1995 that the character and complete shape of a remarkable volcano seamount became evident. The data acquisition and processing revealed a spectacular crater of 350 m depth. The relative hight of this 3 km wide "caldera" rim is 550 m with a basal diameter of the seamount cone of 11 km. Its flanks are about 15° steep but in some places the slope reaches up to 36°. The nearly circular shape of the Orca edifice spreads outh with several pronounced spurs, trending parallel to the basin axis in a northeast-southwest direction. The Bransfield Strait is a trough-shaped basin of 400 km length and 2 km depth between the South Shetland Island Arc and the Antarctic Peninsula, formed by rifting behind the islands. The separation of the South Shetland island chain from the peninsula began possibly several million years ago. The active rifting is still going on however, and has caused recent earthquakes and volcanism along the Bransfield Strait. The Strait hosts a chain of submerged seamounts of volcanic origin with the presently inactive Ora Seamount as the most spectacular one. The South Shelfand Island owe their existence to a subduction related volcanism which is perhaps 5-10 times older than the age of Orca and the other seamounts along the central basin of the Bransfield Strait.