Compositional and structural variabilities of Mg-rich iron oxide spinels from tuffite

Maghemite (γFe2O3) from tuffite is exceptionally rich in Mg, relatively to most of those reportedly found in other mafic lithosystems. To investigate in detail the compositional and structural variabilities of this natural magnetic iron oxide, sets of crystals were isolated from samples collected at different positions in a tuffite weathering mantle. These sets of crystal were individually powdered and studied by X-ray diffractometry, Mössbauer spectroscopy, magnetization measurements and chemical analysis. Lattice parameter of the cubic cell (a0) was found to vary from 0.834(1) to 0.8412(1) nm. Lower a0-values are characteristic of maghemite whereas higher ones are related to a magnetite precursor. FeO content ranges up to 17 mass % and spontaneous magnetization ranges from 8 to 32 J T-1 kg-1. Zero-field room temperature Mössbauer spectra are rather complex, indicating that the hyperfine field distributions due to Fe3+ and mixed valence Fe3+/2+ overlap. The structural variabilities of the (Mg, Ti)-rich iron oxide spinels is essentially related to the range of chemical composition of its precursor (Mg, Ti)-rich magnetite, and probably to the extent to which it has been oxidized during transformation in soil.

Biología y pesquería del perico o dorado Coryphaena hippurus, febrero 2010

La prospección para evaluar la biología y pesquería de Coryphaena hippurus perico o dorado, se efectuó del 10 de febrero al 1 de marzo 2010, a bordo del BIC Imarpe V. El área de extracción fue de 4°59’32,8’’ a 10°15’20,1’’S y de 79°55’16,2’’ a 84°35’04,2’’W; la captura total fue 1.500,5 kg. La CPUE varió de 0,9 a 18,2 kg/Nº Anzuelos/1000*hora efectiva de pesca. Se encontró alta selección interespecífi ca del espinel superfi cial, al capturar 87,8% de perico y 8 especies de peces, tortugas y cefalópodos. El rango de tallas para hembras fue 79 - 141 cm de LT, en machos fue 100 - 157 cm LT. El factor de condición de Fulton en machos varió de 0,30 a 0,46 y en hembras de 0,32 a 0,40. Se determinó para hembras: L∞=148,92 cm, tasa de crecimiento anual (K) 1,081, se estimó t0 = -0,076 años, el Índice de performance Ǿ= 4,38; para machos, estos parámetros fueron L∞=169,75 cm, tasa de crecimiento anual (K) de 0,893, t0 = -0,115, índice de performance Ǿ= 4,40. La curva de crecimiento en talla para hembras, indica que a un año de edad la LT es 102,4 cm y en machos 107 cm. El máximo crecimiento en peso para hembras y machos fue a 1,5 años de vida. El Índice gonadosomático (IGS) fl uctuó de 3,2 a 4,6 mostrando comportamiento heterogéneo. La proporción sexual fue de 2:1 favorable a las hembras. La fecundidad parcial fue de 324.416 ovocitos por tanda de desove. La fecundidad relativa fue 56 ovocitos/ gramo de peso corporal. El tipo de alimento fue peces, cefalópodos y crustáceos con dominancia de Exocoetus volitans (%IRI = 31,6), Argonauta spp. (%IRI = 26,4) mostrando variaciones según zonas y tallas. El consumo de alimento fue 472,7 g/ind./día correspondiente a 7,4% de su peso corporal, presentando fl uctuaciones con respecto a la talla; alimentándose en horas de la mañana, con un máximo entre las 8:00 y 9:59 horas. Se encontraron 5.762 parásitos, identifi cándose 8 especies en cuatro taxas. La prevalencia parasitaria indica que Tentacularia coryphaenae y Bathycotyle coryphaenae alcanzan el 100%, seguido por Hysterothylacium sp. 62% y Caligus coryphaenae 46%. El mayor número de parásitos se encontró en el estómago. Los peces entre 96–100 cm de LT son los más parasitados. La mayor incidencia parasitaria se encontró en la zona norte, en el tramo Paita-Salaverry. Los registros de temperatura en la columna de agua fueron de 12,7 a 27,3 °C y las ATSM de 0,2 a 4,1 °C. Por el frente oceánico se observaron comportamientos térmicos cálidos asociados a las masas de Aguas Ecuatoriales Superfi ciales y Aguas Subtropicales Superfi ciales y por la zona costera se localizaron Aguas Costeras Frías tanto en Chimbote como en Chicama con temperaturas próximas a 22,0 °C. La concentración de oxígeno disuelto superfi cial se presentó favorable para el perico.

New reference tables and user-friendly Internet application for predicted heart weights.

BACKGROUND: Knowledge of normal heart weight ranges is important information for pathologists. Comparing the measured heart weight to reference values is one of the key elements used to determine if the heart is pathological, as heart weight increases in many cardiac pathologies. The current reference tables are old and in need of an update. AIMS: The purposes of this study are to establish new reference tables for normal heart weights in the local population and to determine the best predictive factor for normal heart weight. We also aim to provide technical support to calculate the predictive normal heart weight. METHODS: The reference values are based on retrospective analysis of adult Caucasian autopsy cases without any obvious pathology that were collected at the University Centre of Legal Medicine in Lausanne from 2007 to 2011. We selected 288 cases. The mean age was 39.2 years. There were 118 men and 170 women. Regression analyses were performed to assess the relationship of heart weight to body weight, body height, body mass index (BMI) and body surface area (BSA). RESULTS: The heart weight increased along with an increase in all the parameters studied. The mean heart weight was greater in men than in women at a similar body weight. BSA was determined to be the best predictor for normal heart weight. New reference tables for predicted heart weights are presented as a web application that enable the comparison of heart weights observed at autopsy with the reference values. CONCLUSIONS: The reference tables for heart weight and other organs should be systematically updated and adapted for the local population. Web access and smartphone applications for the predicted heart weight represent important investigational tools.

Correspondance de MARCA avec F. BOSQUET. — Pièces diverses relatives à MARCA et à sa famille.

Contient : Lettres de Marca à François Bosquet (1er janvier 1654-28 avril 1662) ; en majeure partie autographes, rangées par ordre chronologique ; Lettre de Bosquet à Mazarin, 1er décembre 1643, — de Cl. de Rébé, archevêque de Narbonne, au même, du 17 novembre 1643 (copies de la main de Baluze) ; Lettres de Bosquet à Marca, en majeure partie autographes, rangées par ordre chronologique (13 mars 1640-30 juin 1654), parmi lesquelles (f. 90) deux lettres de Marca à Bosquet (14 mars et 28 avril 1662) ; Pièces concernant la famille de P. de Marca et sa biographie, parmi lesquelles on remarque : ; Deux lettres adressées à Marca par Marguerite d'Espenan (15 janvier 1660 et 13 décembre 1659 ; originaux.) ; Contrats de mariage de Jérome de Marca (12 février 1341-1342 n. st.) et de son fils Pierre (7 juin 1398) ; copies de la main de Baluze ; Notice sommaire sur Marca, par le même ; Note sur la famille de Marca, depuis 1118, et sur la vie de P. de Marca jusqu'en 1652 ; Généalogies des maisons de Lavedan et de Marca, de la main de P. de Marca ; Mémoires sur les maisons de la Marque en Gascogne et de Rivière en Bigorre ; placards imprimés, extraits du Dictionnaire de Moreri, éd. Vaultier (2 exemplaires) ; Donation d'une somme de 2.000 écus faite par Henri III à Arnauld d'Ossat, 18 juillet 1586 (original) ; Lettres écrites par M. d'Ossat à Thomas de Marca (10 mai 1559-mai 1562) ; Lettre du même à M. de Castille, receveur du clergé, 18 mai 1587 (original) ; Procurations données par le même pour la perception des 2.000 écus à lui attribués (11 février 1588-19 mai 1587) ; originaux, dont le second est accompagné d'un sceau de cire rouge sur cordelettes ; Notice sur la vie de Marca depuis 1652 [cf. supra, f. 117] ; Note sur les dates principales de la vie de Marca (en espagnol) ; Copie des certificats de tonsure, etc. de Marca (1608) ; Billet de La Reynie, 8 janvier 1703 (original) ; Nomination de Marca comme conseiller d'Etat, 15 novembre 1658 ; Note sur la nomination du même à l'évêché de Conserans ; Mémoire sur la censure faite à Rome du De concordia Sacerdotii et Imperii (imprimé de 2 pages in-fol. ; 2 exemplaires) ; Note sur les affaires d'Espagne ; « Commission à MM. les archevesque de Toulouse et evesque d'Orange pour convenir avec les commissaires du roy d'Espagne des limites des deux royaumes du costé de Catalogne. » ; Notes de Baluze sur le projet d'une nouvelle édition du De concordia, et mémoires envoyés par lui sur ce sujet à Le Tellier (21 juin et 18 décembre 1663) ; Arrêt du Conseil d'état condamnant les Lettres de l'autheur des reigles très importantes au sieur de Marca (imprimé de 7 pages in-4° ; Paris, 1659) ; Bref de N. S. P. le pape Alexandre VII escrit à Monseigneur de Marca, du 5 juin 1662 (imprimé de 4 pages in-4° ; Paris, 1662) ; Mémoire pour servir au jugement de l'instance générale de la régale (imprimé de 14 pages in-4° ; s. l. n. d.) ; Mémoire sur la censure du De concordia ; Profession de foi de Marca, renonçant aux opinions contraires à la doctrine de l'Église romaine émises dans le De concordia ; Note sur les derniers moments de Marca ; Note relative à l'affaire du De concordia ; imprimé, 2 p. in-4°, s. l. n. d ; Petrus de Marca lectori ; Barcelone, 14 août 1646 ; imprimé de 4 pages in-4° (3 exemplaires)

Características geológicas y geotécnicas de los lodos de flotación de la Sierra Minera de Cartagena-La Unión (SE España)

We present the results of a geological and geotechnical characterization of the metallurgic waste from the Sierra Minera de Cartagena-La Union. We have studied eight tailings dams from which we collected and analysed 42 samples of metallurgic waste. We measured grainsize distribution, the specific gravity of solid particles, plasticity index, permeability, both in situ and in the laboratory, direct shear characteristicsand moisture content. According to size distribution the tailings can be classified as sandy silt. Their plasticity index ranges from medium to nil. The internal friction angle varies between 28 and 42 degrees. Cohesion is between 0 and 2.2 t/m2. The specific gravity of the solid particles ranges widely from 1.8 to 4 g/cm3. The saturated hydraulic conductivity values vary between 1.3x 10-5 and 3.2x 10-9 m/s.The water content measured in situ shows that the degree of saturation remains relatively high despite low rainfall and high evaporation rates. Several tailings dams have failed. The leading causes of tailings-dam failure are: 1) slope instability; 2) overflow; 3) erosion; and 4) subsidence or collapse. The main factor leading to dam failure is that the tailings stored in the ponds are highly saturated

Determinación de sistemas de flujo regionales y locales en las depresiones tectónicas del Baix Empordà y La Selva (NE de España) en base a datos hidroquímicos e isotópicos

The Baix Empordà-Selva-Gavarres aquifer system is related to the fault set that created the tectonic basins of Empordà and Selva areas (NE Spain) during the Neogene. In this work, we describe groundwater hydrogeological, hydrochemical and isotopical (3H, δD, δ18O, and the 87Sr/86Sr ratio) characteristics of this system in order to illustrate the relevance of fault zones in groundwater flow-paths and the recharge. In that way, we identify two flow systems, with distinct hydrochemistry and isotopes. A local flow system originates at the Gavarres Range, and it flows towards the basins of the Baix Empordà and Selva, with an approximate residence time of 20 years. Additionally, a regional flow system has only been identified in the Selva basin. This one is related to the main fault zones, as preferential flow paths. Its recharge is located in mountain ranges with higher altitudes, namely the Transversal and Guilleries Ranges, with residence times larger than 50 years. Isotopical data has also shown mixing processes between both flow systems and rainfall recharge while multivariate statistical analysis of principal components has shown the main processes that control hydrochemistry of each flow systems

Complex interplay between LPS and IL-10 in dendritic cells: uncoupling of inflammatory chemokine receptors and positive effects on B cell chemokines

Abstract: Protective immune responses against pathogen invasion and transformed cells requires the coordinated action of distinct leukocyte subsets and soluble factors, overall termed immunological network. Among antigen-presenting cells (APC), a crucial role is played by dendritic cells (DC), which initiate, amplify and determine the outcome of the immune response. Micro-environmental conditions profoundly influence DC in such ways that the resulting immune response ranges from successful immune stimulation to abortive response or immune suppression. For instance, the presence in the milieu of anti-inflammatory cytokine interleukin-10 (IL-10) reverts most of the effects mediated on DC by even strong pro-inflammatory agents such as bacterial Lipopolysaccharide (LPS), in terms of differentiation, activation and functions. In an environment containing both LPS and IL-10, uncoupling of receptors for inflammatory chemokines already occurs after a few hours and in a reversible manner on DC, allowing scavenging of chemokines and, consequently, attenuation of the inflammatory process which could be deleterious to the organism. By studying the effects on DC of concomitant stimulation by LPS and IL-10 from the gene expression point of view, we were able to define four distinct transcriptional programs: A. the inhibition of inflammation and immunity, B. the regulation of tissue remodeling, C. the tuning of cytokine/growth factor receptors and G protein-coupled receptors, D. the stimulation of B cell function and lymphoid tissue neogenesis. Among the latter genes, we further demonstrated that IL-10 synergizes with Toll-like receptor ligands for the production of functionally active B cell attracting chemokine CXCL13. Our data provide evidence that the combined exposure of APC to LPS and IL-10, via the production of CXCL13, involves humoral immunity by attracting antibody-producing cells. It is well known that the persistent release of CXCL13 leads to the development of ectopic lymphoid tissue aggregates and production of high levels of antibodies, thus favoring the induction of auto-immunity. Our findings suggest that the IL-10 produced in chronic inflammatory conditions may promote lymphoid tissue neogenesis through increased release of CXCL13. IL-10 is an anti-inflammatory cytokine inhibiting cellular-mediated TH 1-polarized immune responses. In this study we demonstrate that IL- 10 strongly supports the development of humoral immunity. IL-10 and CXCL13 can thus be targets for specific therapies in auto-immune diseases.

Microvascular burden and Alzheimer-type lesions across the age spectrum.

The occurrence of microvascular and small macrovascular lesions and Alzheimer's disease (AD)-related pathology in the aging human brain is a well-described phenomenon. Although there is a wide consensus about the relationship between macroscopic vascular lesions and incident dementia, the cognitive consequences of the progressive accumulation of these small vascular lesions in the human brain are still a matter of debate. Among the vast group of small vessel-related forms of ischemic brain injuries, the present review discusses the cognitive impact of cortical microinfarcts, subcortical gray matter and deep white matter lacunes, periventricular and diffuse white matter demyelinations, and focal or diffuse gliosis in old age. A special focus will be on the sub-types of microvascular lesions not detected by currently available neuroimaging studies in routine clinical settings. After providing a critical overview of in vivo data on white matter demyelinations and lacunes, we summarize the clinicopathological studies performed by our center in large cohorts of individuals with microvascular lesions and concomitant AD-related pathology across two age ranges (the younger old, 65-85 years old, versus the oldest old, nonagenarians and centenarians). In conjunction with other autopsy datasets, these observations fully support the idea that cortical microinfarcts are the only consistent determinant of cognitive decline across the entire spectrum from pure vascular cases to cases with combined vascular and AD lesion burden.

Application of K-feldspar-jadeite-quartz barometry to eclogite facies metagranites and metapelites in the Sesia Lanzo Zone (Western Alps, Italy)

The eclogite facies assemblage K-feldspar-jadeite-quartz in metagranites and metapelites from the Sesia-Lanzo Zone (Western Alps, Italy) records the equilibration pressure by dilution of the reaction jadeite + quartz = albite. The metapelites show partial transformation from a pre-Alpine assemblage of garnet (Alm(63)Prp(26)Grs(10))-K-feldspar-plagioclase-biotite +/- sillimanite to the Eo-Alpine high-pressure assemblage garnet (Alm(50)Prp(14)Grs(35))-jadeite (Jd(80-97)Di(0-4)Hd(0-8)Acm(0-7))=zoisite-phengite. Plagioclase is replaced by jadeite-zoisite-kyanite-K-feldspar-quartz and biotite is replaced by garnet-phengite or omphacite-kyanite-phengite. Equilibrium was attained only in local domains in the metapelites and therefore the K-feldspar-jadeite-quartz (KJQ) barometer was applied only to the plagioclase pseudomorphs and K-feldspar domains. The albite content of K-feldspar ranges from 4 to 11 mol% in less equilibrated assemblages from Val Savenca and from 4 to 7 mol% in the partially equilibrated samples from Monte Mucrone and the equilibrated samples from Montestrutto and Tavagnasco. Thermodynamic calculations on the stability of the assemblage K-feldspar-jadeite-quartz using available mixing data for K-feldspar and pyroxene indicate pressures of 15-21 kbar (+/- 1.6-1.9 kbar) at 550 +/- 50 degrees C. This barometer yields direct pressure estimates in high-pressure rocks where pressures are seldom otherwise fixed, although it is sensitive to analytical precision and the choice of thermodynamic mixing model for K-feldspar. Moreover, the KJQ barometer is independent of the ratio P-H2O/P-T. The inferred limiting a(H2O) for the assemblage jadeite-kyanite in the metapelites from Val Savenca is low and varies from 0.2 to 0.6.

Das römische Theater von Avenches/Aventicum : Architektur, Baugeschichte, kulturhistorische Aspekte

Résumée Le théâtre romain d'Aventicum s'inscrit entre la petite ville moderne d'Avenches et le village de Donatyre, au pied d'une colline en pente douce délimitant au sud-est la plaine de la Broye. Il se situe à l'ouest des quartiers urbains antiques, construits selon un plan orthogonal, et s'intègre à une zone comptant divers temples et édifices publics. Dès l'hiver 1889/1890, l'Association Pro Aventico nouvellement fondée lança les premières fouilles archéologiques. Jusqu'en 1914, on dégagea les parties originales de la maçonnerie tout en assurant la restauration de l'édifice. En 1926/1927 et de 1939 à 1942 auront lieu d'autres fouilles de grande envergure, accompagnées de mesures de conservation. En 2001, la Fondation Pro Aventico lança un projet visant à étudier l'histoire de la construction ainsi que l'architecture du monument, alors connues en partie seulement. Sur la base de vestiges attestant la présence d'édifices antérieurs au théâtre, on définira pour la construction de ce dernier un terminus post quem entre 100 et 120 ap. J.-C. Comme l'indique l'étude du plan au sol, ce projet nécessita une importante planification. L'édifice lui-même se constitue d'une zone en demi-cercle réservée au public, dont les substructions indiquent qu'elle était partiellement isolée des autres. La cavea, subdivisée en trois secteurs concentriques, se termine par le bâtiment des halles et par les aditus; on relèvera que les rangées supérieures réservées aux spectateurs s'étendaient sans doute au-delà des halles et jusqu'à la façade. Les aditus permettaient d'accéder à la zone de l'orchestra et de la scène, dominée par une plate-forme de plan rectangulaire et bordée d'une proédrie. On disposait de deux voies d'accès différentes: l'une à l'avant, par les arcades des halles, et l'une à l'arrière, pratiquée dans le mur en demi-cercle; apparemment, on ne pouvait pénétrer que dans la partie centrale de ce dernier. On ne parvient à restituer que partiellement les voies de circulation dans les substructions de la cavea, en raison de leur piètre état de conservation. On a par contre pu repérer le deambulatorium, à la périphérie, ainsi que cinq vomitoria sur la première praecinctio et six vomitoria sur la seconde praecinctio. On peut admettre, sans toutefois disposer d'arguments à toute épreuve, que la troisième rangée, en haut, était accessible par des cages d'escaliers conduisant à la summa cavea. Ces hypothèses, fondées essentiellement sur le plan au sol de l'édifice et touchant aux voies de circulation, sont corroborées par une restitution des gradins des parties en élévation, aujourd'hui disparus. Quelques éléments architecturaux fournissent des arguments décisifs pour cette restitution, comme par exemple un bloc de gradin qui permet de conclure à un pendage de la cavea de 26.5°. On peut par ailleurs démontrer que le module architectural défini sur la base du plan au sol fut également appliqué lors de la planification de l'élévation. Grâce à des fragments de corniche, à deux chapiteaux de pilastre ornés de feuilles d'acanthe, à une base de pilastre engagée in situ dans la maçonnerie restaurée, et en tenant compte du module architectural, on peut proposer une reconstitution approximative de la composition de la façade de l'enceinte en demi-cercle. Si les structures architecturales révèlent que le théâtre fut planifié et édifié selon un seul et unique concept, on observe cependant quelques transformations et modifications au cours du temps. D'une part, on décèle en divers endroits des traces de réparation et de consolidation, visant sans doute à stabiliser un bâtiment ayant visiblement subi des dégâts. Par ailleurs, on a également entrepris des modifications structurelles ou fonctionnelles, comme l'édification ultérieure du postscaenium le long du mur de scène extérieur. Dans un contexte identique, on relèvera également deux murs flanquant les basiliques, qu'on suppose être en relation avec l'agrandissement du complexe architectural du temple du Cigognier et du théâtre, augmenté des deux temples édifiés au milieu du 2e s. ap. J.-C. au lieu-dit Au Lavoëx. L'excavation, au cours du dernier tiers du IIIe siècle ap. J.-C., d'un fossé de près de 6 m de large pour 1.5 m de profondeur tout autour de l'édifice fit du théâtre un véritable lieu fortifié. Au-dessus du fossé, on a pu relever une séquence stratigraphique témoignant d'une activité d'habitation à proximité du théâtre pour la période allant du IVe au VIIe siècle ap. J.-C. Il s'agit de l'un des rares cas où l'on peut, à Avenches, évoquer la présence d'un habitat de la période du Haut Moyen Age.

Development of targeted therapies in advanced gastric cancer: promising exploratory steps in a new era.

PURPOSE OF REVIEW: Many chemotherapeutic drugs, including fluoropyrimidines, platinums, CPT-11, taxanes and adriamycin have single-agent activity in advanced gastric cancer. Although combination chemotherapy has been shown to be more effective than single agents, response rates between 30 and 50% have not fulfilled their promise as progression-free survival from the best combinations ranges between 3 and 7 months and overall survival between 8 and 11 months. The development of targeted therapies in gastric cancer clearly stays behind the integration of these novel agents into new treatment concepts for patients with colorectal cancer. This review summarizes the experience and major recent advances in the development of targeted therapies in advanced gastric cancer. RECENT FINDINGS: Recent publications on targeted therapies in gastric cancer are limited to nonrandomized phase I or II trials. The majority of agents tested were angiogenesis inhibitors or agents targeting the epidermal growth factor receptors epidermal growth factor receptor 1 and HER2. SUMMARY: Adequately powered, randomized phase III trials are necessary to define the clinical role of targeted therapies in advanced gastric cancer. Biomarker studies to correlate with treatment outcomes will be critical to identify patients who benefit most from chemotherapy and targeted therapy.

Adaptation to marginal habitats

The ability to adapt to marginal habitats, in which survival and reproduction are initially poor, plays a crucial role in the evolution of ecological niches and species ranges. Adaptation to marginal habitats may be limited by genetic, developmental, and functional constraints, but also by consequences of demographic characteristics of marginal populations. Marginal populations are often sparse, fragmented, prone to local extinctions, or are demographic sinks subject to high immigration from high-quality core habitats. This makes them demographically and genetically dependent on core habitats and prone to gene flow counteracting local selection. Theoretical and empirical research in the past decade has advanced our understanding of conditions that favor adaptation to marginal habitats despite those limitations. This review is an attempt at synthesis of those developments and of the emerging conceptual framework.

Secondary UBVRI-CCD standard stars in the neighbourhood of Landolt standard stars

A list of 681 UBVRI secondary standard stars for CCD photometry is presented. Visual magnitude ranges from 9.7 to 19.4, and the B-V colour index varies from 1.15 to 1.97. The stars are grouped into 11 different fields, each of them is generally observable in a single CCD frame. The stars are located near Landolt UBVRI equatorial standards, accessible to telescopes in both hemispheres, and mainly within the 5 - 8 hours range of right ascension. Photometry, equatorial coordinates and finding charts are provided.

Expression of E-Selectin and Vascular Cell Adhesion Molecule-1 in So-Called 'Negative' Appendices: First Results to Support the Pathological Diagnosis in Borderline Cases.

Background: Since the rate of histologically 'negative' appendices still ranges between 15 and 20%, appendicitis in 'borderline' cases remains a challenging disease. As previously described, cell adhesion molecule expression correlates with different stages of appendicitis. Therefore, it was of interest to determine whether the 'negative' appendix correlated with the absence of E-selectin or vascular cell adhesion molecule-1 (VCAM-1). Methods: Nineteen grossly normal appendices from a series of 120 appendectomy specimens from patients with suspected appendicitis were analysed in frozen sections for the expression of E-selectin and VCAM-1. As control, 5 normal appendices were stained. Results: This study showed a coexpression of E-selectin and VCAM-1 in endothelial cells in early and recurrent appendicitis. In patients with symptoms for less than 6 h, only E-selectin was detected. Cases with fibrosis and luminal obliteration were only positive for VCAM-1. In cases of early appendicitis with symptoms of less than 6 h duration, a discordance between histological and immunohistochemical results was found. Conclusions: This report indicates that E-selectin and VCAM-1 expression could be useful parameters in the diagnosis of appendicitis in borderline cases.

Rate and processes of river network rearrangement during incipient faulting: The case of the Cahabon river, Guatemala

Deeply incised river networks are generally regarded as robust features that are not easily modified by erosion or tectonics. Although the reorganization of deeply incised drainage systems has been documented, the corresponding importance with regard to the overall landscape evolution of mountain ranges and the factors that permit such reorganizations are poorly understood. To address this problem, we have explored the rapid drainage reorganization that affected the Cahabon River in Guatemala during the Quaternary. Sediment-provenance analysis, field mapping, and electrical resistivity tomography (ERT) imaging are used to reconstruct the geometry of the valley before the river was captured. Dating of the abandoned valley sediments by the Be-10-Al-26 burial method and geomagnetic polarity analysis allow us to determine the age of the capture events and then to quantify several processes, such as the rate of tectonic deformation of the paleovalley, the rate of propagation of post-capture drainage reversal, and the rate at which canyons that formed at the capture sites have propagated along the paleovalley. Transtensional faulting started 1 to 3 million years ago, produced ground tilting and ground faulting along the Cahabon River, and thus generated differential uplift rate of 0.3 +/- 0.1 up to 0.7 +/- 0.4 mm . y(-1) along the river's course. The river responded to faulting by incising the areas of relative uplift and depositing a few tens of meters of sediment above the areas of relative subsidence. Then, the river experienced two captures and one avulsion between 700 ky and 100 ky. The captures breached high-standing ridges that separate the Cahabon River from its captors. Captures occurred at specific points where ridges are made permeable by fault damage zones and/or soluble rocks. Groundwater flow from the Cahabon River down to its captors likely increased the erosive power of the captors thus promoting focused erosion of the ridges. Valley-fill formation and capture occurred in close temporal succession, suggesting a genetic link between the two. We suggest that the aquifers accumulated within the valley-fills, increased the head along the subterraneous system connecting the Cahabon River to its captors, and promoted their development. Upon capture, the breached valley experienced widespread drainage reversal toward the capture sites. We attribute the generalized reversal to combined effects of groundwater sapping in the valley-fill, axial drainage obstruction by lateral fans, and tectonic tilting. Drainage reversal increased the size of the captured areas by a factor of 4 to 6. At the capture sites, 500 m deep canyons have been incised into the bedrock and are propagating upstream at a rate of 3 to 11 mm . y(-1) deepening at a rate of 0.7 to 1 5 mm . y(-1). At this rate, 1 to 2 million years will be necessary for headward erosion to completely erase the topographic expression of the paleovalley. It is concluded that the rapid reorganization of this drainage system was made possible by the way the river adjusted to the new tectonic strain field, which involved transient sedimentation along the river's course. If the river had escaped its early reorganization and had been given the time necessary to reach a new dynamic equilibrium, then the transient conditions that promoted capture would have vanished and its vulnerability to capture would have been strongly reduced.