Burrowing in Marine Muds by Crack Propagation: Kinematics and Forces

The polychaete Nereis virens burrows through muddy sediments by exerting dorsoventral forces against the walls of its tongue-depressor- shaped burrow to extend an oblate hemispheroidal crack. Stress is concentrated at the crack tip, which extends when the stress intensity factor (K-I) exceeds the critical stress intensity factor (K-Ic). Relevant forces were measured in gelatin, an analog for elastic muds, by photoelastic stress analysis, and were 0.015 +/- 0.001 N (mean +/- s.d.;N= 5). Measured elastic moduli (E) for gelatin and sediment were used in finite element models to convert the forces in gelatin to those required in muds to maintain the same body shapes observed in gelatin. The force increases directly with increasing sediment stiffness, and is 0.16 N for measured sediment stiffness of E=2.7x10(4) Pa. This measurement of forces exerted by burrowers is the first that explicitly considers the mechanical behavior of the sediment. Calculated stress intensity factors fall within the range of critical values for gelatin and exceed those for sediment, showing that crack propagation is a mechanically feasible mechanism of burrowing. The pharynx extends anteriorly as it everts, extending the crack tip only as far as the anterior of the worm, consistent with wedge-driven fracture and drawing obvious parallels between soft-bodied burrowers and more rigid, wedge-shaped burrowers(i.e. clams). Our results raise questions about the reputed high energetic cost of burrowing and emphasize the need for better understanding of sediment mechanics to quantify external energy expenditure during burrowing.

Lessons learned from nationwide vaccine programs: Comparing human papillomavirus, poliomyelitis vaccine, and swine flu

This assessment compares the human papillomavirus (HPV) nationwide vaccine to the poliomyelitis vaccine and the swine flu vaccine with the purpose of finding parallels and lessons in the controversies faced by the development and use of the vaccines. There are a number of great barriers that are facing the HPV vaccine to date. These controversies lie in dealing with the risk involved in taking the vaccine, how much control the government should have in administering the vaccine, how to communicate the risk to the public, and the cost-effectiveness of the vaccine versus treatment for cervical cancer. The lessons for the HPV vaccine that were learned after comparison and assessment of the controversies were: (1) plan ahead of time on how to inform the public if a risk develops from taking the HPV vaccination and it may be better to provide some information while the event is occurring, always being as truthful as possible, and later dispensing more information once all of the facts are known, (2) the human papillomavirus is not something that will become a pandemic in a short amount of time because the virus takes a long time to develop into cervical cancer, so if a major risk begins to show after continuing to develop and administer the vaccine for an amount of time, it may be better to take it off the market for a while and possibly reconfigure it to help eliminate some of the risks, (3) if side reactions and risks do develop and the government assumes liability for these reactions, the cost-effectiveness can be greatly affected, so it is important to be constantly checking to see if all the monetary and health benefits of the vaccine are outweighing any of the negative costs of the vaccine, and lastly, (4) the public must feel that every aspect of the vaccine, both good and bad, has been thought over and the benefits of taking the vaccine prevail over the negatives and that politics and commercial interests have nothing to do with the production and administration of the vaccine. ^

MODULATION OF HOST INTESTINAL MYOELECTRIC ACTIVITY BY LOCAL ANAPHYLAXIS: A COMPONENT OF PROTECTIVE IMMUNITY TO AN ENTERIC PARASITE (TRICHINELLA SPIRALIS, EIMERIA NIESCHULZI, BOWEL MOTILITY)

The hypothesis tested was that rapid rejection of Trichinella spiralis infective larvae from immunized rats following a challenge infection is associated with a local anaphylactic reaction, and this response should be reflected in altered small intestinal motility. The objective was to determine if altered gut smooth muscle function accompanies worm rejection based on the assumption that anaphylaxis in vivo could be detected by changes in intestinal smooth muscle contractile activity (ie. an equivalent of the Schultz-Dale reaction or in vitro anaphylaxis). The aims were to (1) characterize motility changes by monitoring intestinal myoelectric activity in conscious rats during the enteric phase of T. spiralis infection in immunized hosts, (2) detect the onset and magnitude of myoelectric changes caused by challenge infection in immunized rats, (3) determine the parasite stimulus causing changes, and (4) determine the specificity of host response to stimulation. Electrical slow wave frequency, spiking activity, normal interdigestive migrating myoelectric complexes and abnormal migrating action potential complexes were measured. Changes in myoelectric parameters induced by larvae inoculated into the duodenum of immune hosts differed from those associated with primary infection with respect to time of onset, magnitude and duration. Myoelectric changes elicited by live larvae could not be reproduced by inoculation of hosts with dead larvae, larval excretory-secretory products, or by challenge with a heterologous parasite, Eimeria nieschulzi. These results indicate that (1) local anaphylaxis is a component of the initial response to T. spiralis in immune hosts, since the rapid onset of altered smooth muscle function parallels in time the expression of rapid rejection of infective larvae, and (2) an active mucosal penetration attempt by the worm is necessary to elicit this host response. These findings provide evidence that worm rejection is a consequence of, or sequel to, an immediate hypersensitivity reaction elicited when parasites attempt to invade the gut mucosa of immunized hosts. ^

Endemic tuberculosis, the homeless, and public transportation: A merging of geographical information systems surveillance and the Houston Tuberculosis Initiative Surveillance project

To reach the goals established by the Institute of Medicine (IOM) and the Centers for Disease Control's (CDC) STOP TB USA, measures must be taken to curtail a future peak in Tuberculosis (TB) incidence and speed the currently stagnant rate of TB elimination. Both efforts will require, at minimum, the consideration and understanding of the third dimension of TB transmission: the location-based spread of an airborne pathogen among persons known and unknown to each other. This consideration will require an elucidation of the areas within the U.S. that have endemic TB. The Houston Tuberculosis Initiative (HTI) was a population-based active surveillance of confirmed Houston/Harris County TB cases from 1995–2004. Strengths in this dataset include the molecular characterization of laboratory confirmed cases, the collection of geographic locations (including home addresses) frequented by cases, and the HTI time period that parallels a decline in TB incidence in the United States (U.S.). The HTI dataset was used in this secondary data analysis to implement a GIS analysis of TB cases, the locations frequented by cases, and their association with risk factors associated with TB transmission. ^ This study reports, for the first time, the incidence of TB among the homeless in Houston, Texas. The homeless are an at-risk population for TB disease, yet they are also a population whose TB incidence has been unknown and unreported due to their non-enumeration. The first section of this dissertation identifies local areas in Houston with endemic TB disease. Many Houston TB cases who reported living in these endemic areas also share the TB risk factor of current or recent homelessness. Merging the 2004–2005 Houston enumeration of the homeless with historical HTI surveillance data of TB cases in Houston enabled this first-time report of TB risk among the homeless in Houston. The homeless were more likely to be US-born, belong to a genotypic cluster, and belong to a cluster of a larger size. The calculated average incidence among homeless persons was 411/100,000, compared to 9.5/100,000 among housed. These alarming rates are not driven by a co-infection but by social determinants. The unsheltered persons were hospitalized more days and required more follow-up time by staff than those who reported a steady housing situation. The homeless are a specific example of the increased targeting of prevention dollars that could occur if TB rates were reported for specific areas with known health disparities rather than as a generalized rate normalized over a diverse population. ^ It has been estimated that 27% of Houstonians use public transportation. The city layout allows bus routes to run like veins connecting even the most diverse of populations within the metropolitan area. Secondary data analysis of frequent bus use (defined as riding a route weekly) among TB cases was assessed for its relationship with known TB risk factors. The spatial distribution of genotypic clusters associated with bus use was assessed, along with the reported routes and epidemiologic-links among cases belonging to the identified clusters. ^ TB cases who reported frequent bus use were more likely to have demographic and social risk factors associated with poverty, immune suppression and health disparities. An equal proportion of bus riders and non-bus riders were cultured for Mycobacterium tuberculosis, yet 75% of bus riders were genotypically clustered, indicating recent transmission, compared to 56% of non-bus riders (OR=2.4, 95%CI(2.0, 2.8), p<0.001). Bus riders had a mean cluster size of 50.14 vs. 28.9 (p<0.001). Second order spatial analysis of clustered fingerprint 2 (n=122), a Beijing family cluster, revealed geographic clustering among cases based on their report of bus use. Univariate and multivariate analysis of routes reported by cases belonging to these clusters found that 10 of the 14 clusters were associated with use. Individual Metro routes, including one route servicing the local hospitals, were found to be risk factors for belonging to a cluster shown to be endemic in Houston. The routes themselves geographically connect the census tracts previously identified as having endemic TB. 78% (15/23) of Houston Metro routes investigated had one or more print groups reporting frequent use for every HTI study year. We present data on three specific but clonally related print groups and show that bus-use is clustered in time by route and is the only known link between cases in one of the three prints: print 22. (Abstract shortened by UMI.)^

Late Miocene-early Pliocene stable isotope record of benthic foraminifera from ODP Site 177-1088 in the sub-Antarctic South Atlantic

Benthic foraminiferal stable isotope records for the past 11 Myr from a recently drilled site in the sub-Antarctic South Atlantic (Site 1088, Ocean Drilling Program Leg 177, 41°S, 15°E, 2082 m water depth) provide, for the first time, a continuous long-term perspective on deep water distribution patterns and Southern Ocean climate change from the late Miocene through the early Pliocene. I have compiled published late Miocene through Pliocene stable isotope records to place the new South Atlantic record in a global framework. Carbon isotope gradients between the North Atlantic, South Atlantic, and Pacific indicate that a nutrient-depleted watermass, probably of North Atlantic origin, reached the sub-Antarctic South Atlantic after 6.6 Ma. By 6.0 Ma the relative proportion of the northern-provenance watermass was similar to today and by the early Pliocene it had increased to greater than the modern proportion suggesting that thermohaline overturn in the Atlantic was relatively strong prior to the early Pliocene interval of inferred climatic warmth. Site 1088 oxygen isotope values display a two-step increase between ~7.4 Ma and 6.9 Ma, a trend that parallels a published delta18O record of a site on the Atlantic coast of Morocco. This is perhaps best explained by a gradual cooling of watermasses that were sinking in the Southern Ocean. I speculate that relatively strong thermohaline overturn at rates comparable to the present day interglacial interval during the latest Miocene may have provided the initial conditions for early Pliocene climatic warmth. The impact of an emerging Central American Seaway on Atlantic-Pacific Ocean upper water exchange may have been felt in the North Atlantic beginning in the latest Miocene between 6.6 and 6.0 Ma, which would be ~1.5 Myr earlier than previously thought.

Chemical element contents and accumulation rates in metalliferous sediments from DSDP Hole 34-319, Bauer Deep, Southeast Pacific

Marked variations in the chemical and mineralogical composition of sediments at Site 319 have occurred during the 15 My history of sedimentation at this site. The change in composition through time parallels the variability observed in surface sediments from various parts of the Nazca Plate and can be related to variations in the proportion of hydrothermal, hydrogenous, detrital and biogenous phases reaching this site at different times. Metal accumulation rates at Site 319 reach a maximum near the basement for most elements, suggesting a strong hydrothermal contribution during the early history of this site. The hydrothermal contribution decreased rapidly as Site 319 moved away from the spreading center, although a subtle increase in this source is detectable about the time spreading began on the East Pacific Rise. The most recent sedimentation exhibits a strong detritalhydrogenous influence. Post-depositional diagenesis of amorphous phases has converted them to ironrich smectite and well-crystallized goethite without significantly altering the bulk composition of the sediment.

(Table 1) GRACE-derived mass balance of the Greenland ice sheet 2002-2010

We re-evaluate the Greenland mass balance for the recent period using low-pass Independent Component Analysis (ICA) post-processing of the Level-2 GRACE data (2002-2010) from different official providers (UTCSR, JPL, GFZ) and confirm the present important ice mass loss in the range of -70 and -90 Gt/y of this ice sheet, due to negative contributions of the glaciers on the east coast. We highlight the high interannual variability of mass variations of the Greenland Ice Sheet (GrIS), especially the recent deceleration of ice loss in 2009-2010, once seasonal cycles are robustly removed by Seasonal Trend Loess (STL) decomposition. Interannual variability leads to varying trend estimates depending on the considered time span. Correction of post-glacial rebound effects on ice mass trend estimates represents no more than 8 Gt/y over the whole ice sheet. We also investigate possible climatic causes that can explain these ice mass interannual variations, as strong correlations between GRACE-based mass balance and atmosphere/ocean parallels are established: (1) changes in snow accumulation, and (2) the influence of inputs of warm ocean water that periodically accelerate the calving of glaciers in coastal regions and, feed-back effects of coastal water cooling by fresh currents from glaciers melting. These results suggest that the Greenland mass balance is driven by coastal sea surface temperature at time scales shorter than accumulation.

Chemical composition and sulfur-isotope ratios in DSDP Legs 69-and 70

As part of the geochemical-petrological study of basalts recovered from DSDP Hole 504B (Leg 70) on the southern flank of the Costa Rica Rift, we investigated specially the relationships between the distribution and isotopic composition of sulfur of scattered and vein sulfides on the one hand, and the observed pattern and processes of secondary alterations on the other. The following groups of observations are essential: (1) variations in the contents and isotopic composition of sulfur of different forms of sulfides are clearly interrelated and are observed solely in porous horizons established on the basis of detailed geophysical experiments; (2) the enrichment of sulfides in the light sulfur isotope decreases from the upper to the lower horizons, and within horizons in the direction of the less-altered rock; (3) the increase of d34S values of scattered sulfides in individual permeable zones parallels a decrease in the degree of iron oxidation in the contents of crystallization water, and in the concentrations of Mg, K, and Li in the rock.

El conflicto de los españoles ante el proceso de emancipación : Los casos del Río de La Plata y México en los albores del siglo XIX

Las guerras de independencia en Latinoamérica y el consecuente proceso de construcción de la nación, representaron para los españoles una inestabilidad manifestada, en diversos grados de intensidad, en los países emergentes. La intención de este trabajo es presentar, a manera de contraste, las medidas que los gobiernos de dos territorios disímbolos, más no extraños, como son México y el Río de la Plata, adoptaron en contra de los peninsulares para legitimarse. Las posturas de ambos gobiernos reflejan las relaciones y afrentas que cada país guardaba con sus otrora conquistadores y los niveles de dependencia hacia la comunidad ibérica que hacían inoperables, en muchos de los casos, la intención de agraviar sus privilegios. Por tanto se pretende mostrar las vicisitudes, los paralelismos y las discrepancias que estos países presentan en sus disposiciones frente a los españoles.

¿Hubo ritos de paso cruentos en el orfismo?

El modo de vida a que estaban sometidos los iniciados en el orfismo se caracterizaba por la abstención de alimento animado y el rechazo al sacrificio cruento. Pese a ello, dos textos considerados testimonios clave para el estudio y reconstrucción de los ritos y creencias órficos hacen mención explícita del sacrificio cruento y el consumo de carne. Para superar la aparente contradicción de ambos testimonios con las doctrinas órficas se ha propuesto que estas prácticas se adscriben a un primer ritual de iniciación que constituiría un rito de paso entre la condición de profano y la de iniciado. Sin embargo, es preciso examinar los paralelos literarios e iconográficos que ofrecen otros rituales griegos y orientales para determinar si los citados testimonios órficos constituyen casos aislados que no responden a un uso ritual común o si, por el contrario, estas prácticas pueden ser consideradas ritos de paso para alcanzar la condición de iniciado

¿Fue Ovidio un poeta latino de la Edad de Plata?

Este artículo busca establecer cómo las características más sobresalientes de las Metamorfosis de Ovidio, consideradas por muchos estudiosos como el modelo por excelencia de los poetas latinos del siglo I d.C. no resultan tan influyentes en la praxis poética de los autores neronianos y flavianos. Aun considerando los numerosos paralelismos formales y estilísticos existentes en estos autores, tal como el uso de la paradoja, la sobreexplicitación visual y la acumulación de detalles, resulta claro que el propósito y el uso de los diferentes topoi literarios que estos poetas hacen son completamente distintos. Un análisis de los motivos de la nekya y la tempestad en Ovidio, Lucano, Silio Itálico, Valerio Flaco y Estacio muestra cuánto más a menudo los poetas latinos del siglo I d.C. recurren a la obra de Virgilio que a la de Ovidio

Carbonate and Aluminium accumulation in the central equatorial Pacific Ocean

We examined the flux of Al to sediment accumulating beneath the zone of elevated productivity in the central equatorial Pacific Ocean, along a surface sediment transect at 135°W as well as downcore for a 650 kyr record at 1.3°N, 133.6°W. Across the surface transect, a pronounced, broadly equatorially symmetric increase in Al accumulation is observed, relative to Ti, with Al/Ti ratios reaching values 3-4 times that of potential detrital sources. The profile parallels biogenic accumulation and the modeled flux of particulate 234Th, suggesting rapid and preferential adsorptive removal of Al from seawater by settling biogenic particles. Normative calculations confirm that most Al is unsupported by the terrigenous fraction. The observed distributions are consistent with previous observations of the relative and absolute behavior of Al and Ti in seawater, and we can construct a reasonable mass balance between the amount of seawater-sourced Al retained in the sediment and the amount of seawater Al available in the overlying column. The close tie between Al/Ti and biogenic accumulation (as opposed to concentration) emphasizes that biogenic sedimentary Al/Ti responds to removal-transport phenomena and not bulk sediment composition. Thus, in these sediments dominated by the biogenic component, the bulk Al/Ti ratio reflects biogenic particle flux, and by extension, productivity of the overlying seawater. The downcore profile of Al/Ti at 1.3°N displays marked increases during glacial episodes, similar to that observed across the surface transect, from a background value near Al/Ti of average upper crust. The excursions in Al/Ti are stratigraphically coincident with maxima in both bulk and CaCO3 accumulation and the excess Al appears to not be preferentially affiliated with opaline or organic phases. Consistent with the similar behavioral removal of Al and 234Th, the latter of which responds to the total particle flux, the Al flux reflects carbonate accumulation only because carbonate comprises the dominant flux in these particular deposits. These results collectively indicate that (1) Al in biogenic sediment and settling biogenic particles is strongly affected by a component adsorbed from seawater. Therefore, the common tenet that Al is dominantly associated with terrestrial particulate matter, and the subsequent use of Al distributions to calculate the abundance and flux of terrestrial material in settling particles and sediment, needs to be reevaluated. (2) The Al/Ti ratio in biogenic sediment can be used to trace the productivity of the overlying water, providing a powerful new paleochemical tool to investigate oceanic response to climatic variation. (3) The close correlation between the Al/Ti productivity signal and carbonate maxima downcore at 1.3°N suggests that the sedimentary carbonate maxima in the central equatorial Pacific Ocean record increased productivity during glacial episodes.

El conflicto de los españoles ante el proceso de emancipación : Los casos del Río de La Plata y México en los albores del siglo XIX

Las guerras de independencia en Latinoamérica y el consecuente proceso de construcción de la nación, representaron para los españoles una inestabilidad manifestada, en diversos grados de intensidad, en los países emergentes. La intención de este trabajo es presentar, a manera de contraste, las medidas que los gobiernos de dos territorios disímbolos, más no extraños, como son México y el Río de la Plata, adoptaron en contra de los peninsulares para legitimarse. Las posturas de ambos gobiernos reflejan las relaciones y afrentas que cada país guardaba con sus otrora conquistadores y los niveles de dependencia hacia la comunidad ibérica que hacían inoperables, en muchos de los casos, la intención de agraviar sus privilegios. Por tanto se pretende mostrar las vicisitudes, los paralelismos y las discrepancias que estos países presentan en sus disposiciones frente a los españoles.

¿Hubo ritos de paso cruentos en el orfismo?

El modo de vida a que estaban sometidos los iniciados en el orfismo se caracterizaba por la abstención de alimento animado y el rechazo al sacrificio cruento. Pese a ello, dos textos considerados testimonios clave para el estudio y reconstrucción de los ritos y creencias órficos hacen mención explícita del sacrificio cruento y el consumo de carne. Para superar la aparente contradicción de ambos testimonios con las doctrinas órficas se ha propuesto que estas prácticas se adscriben a un primer ritual de iniciación que constituiría un rito de paso entre la condición de profano y la de iniciado. Sin embargo, es preciso examinar los paralelos literarios e iconográficos que ofrecen otros rituales griegos y orientales para determinar si los citados testimonios órficos constituyen casos aislados que no responden a un uso ritual común o si, por el contrario, estas prácticas pueden ser consideradas ritos de paso para alcanzar la condición de iniciado

¿Fue Ovidio un poeta latino de la Edad de Plata?

Este artículo busca establecer cómo las características más sobresalientes de las Metamorfosis de Ovidio, consideradas por muchos estudiosos como el modelo por excelencia de los poetas latinos del siglo I d.C. no resultan tan influyentes en la praxis poética de los autores neronianos y flavianos. Aun considerando los numerosos paralelismos formales y estilísticos existentes en estos autores, tal como el uso de la paradoja, la sobreexplicitación visual y la acumulación de detalles, resulta claro que el propósito y el uso de los diferentes topoi literarios que estos poetas hacen son completamente distintos. Un análisis de los motivos de la nekya y la tempestad en Ovidio, Lucano, Silio Itálico, Valerio Flaco y Estacio muestra cuánto más a menudo los poetas latinos del siglo I d.C. recurren a la obra de Virgilio que a la de Ovidio