Entrepreneurial structure of the mercantile company in pre-industrial Catalonia

The mercantile company was the basic form of enterprise in pre-industrial Catalonia. The aim of this paper is to study the formation and development of the mercantile companies in Barcelona whose end was the wholesale and retail sale of textiles in the botigues de teles (textile retail shops) throughout the eighteenth century. These firms were officially registered before a notary and their deeds reveal how these establishments were administered and managed.The study covers a sample of 121 mercantile companies, and the articles and documentation that were put into effect by 32 notaries who were active in Barcelona in the 18th century have been consulted in their entirety. From an initial selection of documentation, a total of 228 deeds registering companies have been found, 107 of which (47%) relate to the creation of companies whose various activities were centred in taverns, textile manufacturing, braiding.... While the 121 companies, which make up our sample and which account for 53% of the deeds registered with the notaries mentioned above, focused exclusively on the management of textile retail shops located in the commercial heart of the city. Thus one point of interest that the documentation reveals is that the majority of the mercantile companies registered by Barcelona notaries throughout the 18th century were establishments which traded in textiles. The first part of the article focuses on the structural characteristics of these enterprises, the number and socio-professional status of the partners and the extent of each partner s involvement in the administration and management. The second part of the article examines the capital investment made by each partner, their rights and obligations agreed on, the sharing out of profits and possible losses and the duration of the companies. The final aim of the paper is to highlight the evolution of these companies through one specific case.

Generation of the primary hair follicle pattern.

Hair follicles are spaced apart from one another at regular intervals through the skin. Although follicles are predominantly epidermal structures, classical tissue recombination experiments indicated that the underlying dermis defines their location during development. Although many molecules involved in hair follicle formation have been identified, the molecular interactions that determine the emergent property of pattern formation have remained elusive. We have used embryonic skin cultures to dissect signaling responses and patterning outcomes as the skin spatially organizes itself. We find that ectodysplasin receptor (Edar)-bone morphogenetic protein (BMP) signaling and transcriptional interactions are central to generation of the primary hair follicle pattern, with restriction of responsiveness, rather than localization of an inducing ligand, being the key driver in this process. The crux of this patterning mechanism is rapid Edar-positive feedback in the epidermis coupled with induction of dermal BMP4/7. The BMPs in turn repress epidermal Edar and hence follicle fate. Edar activation also induces connective tissue growth factor, an inhibitor of BMP signaling, allowing BMP action only at a distance from their site of synthesis. Consistent with this model, transgenic hyperactivation of Edar signaling leads to widespread overproduction of hair follicles. This Edar-BMP activation-inhibition mechanism appears to operate alongside a labile prepattern, suggesting that Edar-mediated stabilization of beta-catenin active foci is a key event in determining definitive follicle locations.

Tectonics of the Simplon massif and Lepontine gneiss dome: deformation structures due to collision between the underthrusting European plate and the Adriatic indenter

this study presents a review of published geological data, combined with original observations on the tectonics of the simplon massif and the Lepontine gneiss dome in the Western Alps. New observations concern the geometry of the Oligocene Vanzone back fold, formed under amphibolite facies conditions, and of its root between Domodossola and Locarno, which is cut at an acute angle by the Miocene, epi- to anchizonal, dextral centovalli strike-slip fault. the structures of the simplon massif result from collision over 50 Ma between two plate boundaries with a different geometry: the underthrusted European plate and the Adriatic indenter. Detailed mapping and analysis of a complex structural interference pattern, combined with observations on the metamorphic grade of the superimposed structures and radiometric data, allow a kinematic model to be developed for this zone of oblique continental collision. the following main Alpine tectonic phases and structures may be distinguished: 1. NW-directed nappe emplacement, starting in the Early Eocene (similar to 50 Ma); 2. W, SW and S- verging transverse folds; 3. transpressional movements on the dextral simplon ductile shear zone since similar to 32 Ma; 4. formation of the Bergell - Vanzone backfolds and of the southern steep belt during the Oligocene, emplacement of the mantle derived 31 - 29 Ma Bergell and Biella granodiorites and porphyritic andesites as well as intrusions of 29-25 Ma crustal aplites and pegmatites; 5. formation of the dextral discrete Rhone-Simplon line and the centovalli line during the Miocene, accompanied by the pull-apart development of the Lepontine gneiss dome - Dent blanche (Valpelline) depression. It is suggested that movements of shortening in fan shaped NW, W and sW directions accompanied the more regular NW- to WNW-directed displacement of the Adriatic indenter during continental collision.

Termite assemblages in five semideciduous Atlantic Forest fragments in the northern coastland limit of the biome

Termites are abundant organisms in tropical ecosystems and strongly influence the litter decomposition and soil formation. Despite their importance, few studies about their assemblage structures have been made in Brazilian Atlantic Forest fragments, especially in the area located north of the São Francisco River. This study aims to analyze the assemblage composition of five Atlantic Forest fragments located in the northern biome limit along the Brazilian coast. A standardized sampling protocol of termites was applied in each fragment. Thirty-three termite species belonging to twenty genera and three families were found in the forest fragments. The wood-feeder group was dominant both concerning to species richness and number of encounters in all areas. In sites northern to 7°S, there is an evident simplification of the termite assemblage composition regarding species richness and number of encounters by feeding group. This fact is apparently due to a higher sandy level in soils and to semideciduous character of the vegetation in the northern fragments. Thus, even on the north of São Francisco River, termite biodiversity is heterogeneously spread with highest density of species in the portion between 07°S and São Francisco River mouth (10°29'S).

Tertiary Himalayan structures and metamorphism in the Kulu Valley (Mandi-Khoksar transect of the Western Himalaya) - Shikar-Beh-nappe and crystalline nappe

The Crystalline Nappe of the High Himalayan Crystalline has been examined along the Kulu Valley and its vicinity (Mandi-Khoksar transect). This nappe was believed to have undergone deformation related only to its transport towards the SW essentially during the `'Main Central Thrust event''. New data has led to the conclusion that during the Himalayan orogeny, two distinctive phases, related to two opposite transport directions, characterize the evolution of this part of the chain, before the creation of the late NE-vergent backfolding. The first phase corresponds to an early NE-vergent folding and thrusting, creating the Tandi Syncline and the NE-oriented Shikar Beh Nappe stack, with a displacement amplitude of about 50 km. Two schistosities, together with a strong stretching lineation are developed at a deep tectonic level under amphibolite facies conditions (kyanite-staurolite-garnet-two mica schists). At a higher tectonic level and in the southern part of the section (Tandy Syncline and southern Kulu Valley between Kulu and Mandi) one or two schistosities are developed in the greenschist facies grade rocks (garnet-biotite and biotite schists). These structures and the associated Barrovian type metamorphism are all related to the NE-verging Shikar Beh Nappe. The creation of the NE-verging Shikar Beh Nappe may be explained by the reactivation of a SW dipping listric normal fault of the N Indian flexural passive margin, during the early stages of the Himalayan orogeny. In the second phase, the still hot metamorphic rocks of the Shikar Beh Nappe were folded and thrust towards the SW (mainly along the MBT and the MCT with a displacement in excess of 100 km) onto the cold, low-grade metamorphic rocks of the Larji-Kulu-Rampur Window or, near Mandi, on the non-metamorphic sandstones of the Ganges Molasse (Siwaliks). Sense of shear criteria and a strong NE-SW stretching-lineation indicate that the Crystalline Nappe has been overthrusted towards the SW. Thermometry on synkinematically crystallised garnet-biotite and garnet-hornblende pairs reveals the lower amphibolite facies temperature conditions related to the Crystalline Nappe formation. From the muscovite and biotite Rb-Sr cooling ages, the Shikar Beh Nappe emplacement occurred before 32 Ma and the southwestward thrusting of the Crystalline Nappe began before 21 Ma. Our model involving two opposite directions of thrusting goes against the conventional idea of only one main SW-oriented transport direction in the High Himalayan Crystalline Nappes.

Carbon and oxygen isotope study of hydrothermal carbonates in the zinc-lead deposits of the San Vicente district, central Peru: A quantitative modeling on mixing processes and CO2 degassing

Carbon and oxygen isotope studies of the host and gangue carbonates of Mississippi Valley-type zinc-lead deposits in the San Vicente District hosted in the Upper Triassic to Lower Jurassic dolostones of the Pucara basin (central Peru) were used to constrain models of the ore formation. A mixing model between an incoming hot saline slightly acidic radiogenic (Pb, Sr) fluid and the native formation water explains the overall isotopic variation (delta(13)C = - 11.5 to + 2.5 parts per thousand relative to PDB and delta(18)O = + 18.0 to + 24.3 parts per thousand relative to SMOW) of the carbonate generations. The dolomites formed during the main ore stage show a narrower range (delta(13)C = - 0.1 to + 1.7 parts per thousand and delta(18)O = + 18.7 to + 23.4 parts per thousand) which is explained by exchange between the mineralizing fluids and the host carbonates combined with changes in temperature and pressure. This model of fluid-rock interaction explains the pervasive alteration of the host dolomite I and precipitation of sphalerite I. The open-space filling hydrothermal white sparry dolomite and the coexisting sphalerite II formed by prolonged fluid-host dolomite interaction and limited CO2 degassing. Late void-filling dolomite III (or calcite) and the associated sphalerite III formed as the consequence of CO2 degassing and concomitant pH increase of a slightly acidic ore fluid. Widespread brecciation is associated to CO2 outgassing. Consequently, pressure variability plays a major role in the ore precipitation during the late hydrothermal events in San Vicente. The presence of native sulfur associated with extremely carbon-light calcites replacing evaporitic sulfates (e.g., delta(13)C = - 11.5 parts per thousand), altered native organic matter and heavier hydrothermal bitumen (from - 27.0 to - 23.0 parts per thousand delta(13)C) points to thermochemical reduction of sulfate and/or thiosulfate. The delta(13)C- and delta(18)O-values of the altered host dolostone and hydrothermal carbonates, and the carbon isotope composition of the associated organic matter show a strong regional homogeneity. These results coupled with the strong mineralogical and petrographic similarities of the different MVT occurrences perhaps reflects the fact that the mineralizing processes were similar in the whole San Vicente belt, suggesting the existence of a common regional mineralizing hydrothermal system with interconnected plumbing.

Transcriptional activation of the GLUT2 gene by the IPF-1/STF-1/IDX-1 homeobox factor.

The homeodomain protein PDX-1, referred as IPF-1/STF-1/IDX-1, is a transcriptional factor that plays a critical role in the control of several genes expressed in the pancreatic islet. PDX-1 gene expression has been previously shown to be reduced in cultured beta-cell lines chronically exposed to high glucose concentrations. As the glucose transporter type 2 (GLUT2) gene expression is selectively decreased in the beta-pancreatic cells of experimental models of diabetes, we postulated that the loss of GLUT2 gene expression in the pancreatic islets of diabetic animals may be due to the loss of PDX-1 transacting function on the GLUT2 gene. We, therefore, investigated the potential role of PDX-1 in the transcriptional control of GLUT2. We have identified a repeat of a TAAT motif (5'-TAATA-ATAACA-3') conserved in the sequence of the human and murine GLUT2 promoters. Recombinant PDX-1 binds to this GLUT2TAAT motif in electrophoretic mobility shift experiments. PDX-1 antiserum detects the formation of the complex of PDX-1 with the GLUT2TAAT motif in nuclear extracts from the pancreatic insulin-secreting cell line, beta TC3. The GLUT2TAAT motif was mutated in the murine GLUT2 promoter (-1308/+49 bp) linked to a luciferase reporter gene and transfected into beta TC3 cells. Compared with the transcriptional activity of the wild type promoter, that of the mutated promoter decreases by 41%. Multiple copies of the GLUT2TAAT motif were ligated 5' to a heterologous promoter and transfected into a PDX-1-expressing cell line (beta TC3) and into cell lines lacking the homeobox factor (InR1-G9 and JEG-3). The GLUT2TAAT motif mediates the activation of the heterologous promoter in the PDX-1-expressing cell line but not in InR1-G9 or JEG-3 cell lines. Furthermore, cotransfection in a PDX-1-deficient cell line with the expression vector encoding PDX-1 transactivates specifically the heterologous promoter containing the multimerized GLUT2TAAT motif. These data demonstrate that the murine GLUT2 promoter is controlled by the PDX-1 homeobox factor through the identified GLUT2TAAT motif.

Low-pressure environment and remodelling of the forearm vein in Brescia-Cimino haemodialysis access.

BACKGROUND: The aim of the study was to determine which, and to what extent, haemodynamic parameters contribute to the remodelling of the venous limb of the Brescia-Cimino haemodialysis access. METHODS: The dimensions of the radial artery and the venous limb of the haemodialysis access were measured by an echo-tracking technique. In six ESRD patients undergoing primary arteriovenous fistula (AVF) formation, vessel diameter, wall thickness, blood pressure and blood flow were measured after the operation, and at 1 and 3 months follow-up. The contralateral forearm vessels in their native position served as baseline values for comparison. RESULTS: The diameter of the proximal antecubital vein progressively increased over the study period without reaching significant differences (4430, 5041 and 6620 microm at weeks 1, 4 and 12 respectively), whereas the intima-media thickness remained unchanged. The venous dilatation was associated with a reduction of the mean shear stress that culminated after the operation and progressively returned to normal venous values at 3 months (24.5 vs 10.4 dyne/cm(2), P<0.043). Thus the venous limb of the AVF undergoes eccentric hypertrophy as demonstrated by the increase in wall cross-sectional area (4.42 vs 6.32 mm(2) at week 1 vs week 12, P<0.028). At the time of the operation, the blood pressure in the AVF was 151+/-14/92.4+/-11 mmHg vs 49+/-19/24.5+/-6 mmHg (means+/-SEM) for the radial artery and the venous limb of the vascular access, respectively. One year after the operation the blood pressure in the venous limb had not changed: 42+/-14/25.3+/-7 mmHg (means+/-SEM). Under these conditions, the systolo-diastolic diameter changes observed in the radial artery and the antecubital vein were within a similar range at all time points: 56+/-17 vs 90+/-26 microm (means+/-SEM) at week 12. CONCLUSIONS: The increased circumferential stress resulting from the flow-mediated dilatation rather than the elevation of blood pressure appears to represent the main contributing factor to the eccentric hypertrophy of the venous limb of Brescia-Cimino haemodialysis access.

NOTCH1 can initiate NF-κB activation via cytosolic interactions with components of the T cell Signalosome.

T cell stimulation requires the input and integration of external signals. Signaling through the T cell receptor (TCR) is known to induce formation of the membrane-tethered CBM complex, comprising CARMA1, BCL10, and MALT1, which is required for TCR-mediated NF-κB activation. TCR signaling has been shown to activate NOTCH proteins, transmembrane receptors also implicated in NF-κB activation. However, the link between TCR-mediated NOTCH signaling and early events leading to induction of NF-κB activity remains unclear. In this report, we demonstrate a novel cytosolic function for NOTCH1 and show that it is essential to CBM complex formation. Using a model of skin allograft rejection, we show in vivo that NOTCH1 acts in the same functional pathway as PKCθ, a T cell-specific kinase important for CBM assembly and classical NF-κB activation. We further demonstrate in vitro NOTCH1 associates physically with PKCθ and CARMA1 in the cytosol. Unexpectedly, when NOTCH1 expression was abrogated using RNAi approaches, interactions between CARMA1, BCL10, and MALT1 were lost. This failure in CBM assembly reduced inhibitor of kappa B alpha phosphorylation and diminished NF-κB-DNA binding. Finally, using a luciferase gene reporter assay, we show the intracellular domain of NOTCH1 can initiate robust NF-κB activity in stimulated T cells, even when NOTCH1 is excluded from the nucleus through modifications that restrict it to the cytoplasm or hold it tethered to the membrane. Collectively, these observations provide evidence that NOTCH1 may facilitate early events during T cell activation by nucleating the CBM complex and initiating NF-κB signaling.

Pseudomonas fluorescens CHA0 produces enantio-pyochelin, the optical antipode of the Pseudomonas aeruginosa siderophore pyochelin.

The siderophore pyochelin is made by a thiotemplate mechanism from salicylate and two molecules of cysteine. In Pseudomonas aeruginosa, the first cysteine residue is converted to its D-isoform during thiazoline ring formation whereas the second cysteine remains in its L-configuration, thus determining the stereochemistry of the two interconvertible pyochelin diastereoisomers as 4'R, 2''R, 4''R (pyochelin I) and 4'R, 2''S, 4''R (pyochelin II). Pseudomonas fluorescens CHA0 was found to make a different stereoisomeric mixture, which promoted growth under iron limitation in strain CHA0 and induced the expression of its biosynthetic genes, but was not recognized as a siderophore and signaling molecule by P. aeruginosa. Reciprocally, pyochelin promoted growth and induced pyochelin gene expression in P. aeruginosa, but was not functional in P. fluorescens. The structure of the CHA0 siderophore was determined by mass spectrometry, thin-layer chromatography, NMR, polarimetry, and chiral HPLC as enantio-pyochelin, the optical antipode of the P. aeruginosa siderophore pyochelin. Enantio-pyochelin was chemically synthesized and confirmed to be active in CHA0. Its potential biosynthetic pathway in CHA0 is discussed.

Persistence and cell culturability of biocontrol strain Pseudomonas fluorescens CHA0 under plough pan conditions in soil and influence of the anaerobic regulator gene anr.

Certain fluorescent pseudomonads can protect plants from soil-borne pathogens, and it is important to understand how these biocontrol agents survive in soil. The persistence of the biocontrol strain Pseudomonas fluorescens CHA0-Rif under plough pan conditions was assessed in non-sterile soil microcosms by counting total cells (immunofluorescence microscopy), intact cells (BacLight membrane permeability test), viable cells (Kogure's substrate-responsiveness test) and culturable cells (colony counts on selective plates) of the inoculant. Viable but non-culturable cells of CHA0-Rif (106 cells g-1 soil) were found in flooded microcosms amended with fermentable organic matter, in which the soil redox potential was low (plough pan conditions), in agreement with previous observations of plough pan samples from a field inoculated with CHA0-Rif. However, viable but non-culturable cells were not found in unamended flooded, amended unflooded or unamended unflooded (i.e. control) microcosms, suggesting that such cells resulted from exposure of CHA0-Rif to a combination of low redox potential and oxygen limitation in soil. CHA0-Rif is strictly aerobic. Its anaerobic regulator ANR is activated by low oxygen concentrations and it controls production of the biocontrol metabolite hydrogen cyanide under microaerophilic conditions. Under plough pan conditions, an anr-deficient mutant of CHA0-Rif and its complemented derivative displayed the same persistence pattern as CHA0-Rif, indicating that anr was not implicated in the formation of viable but non-culturable cells of this strain at the plough pan.

IRF6 is a mediator of the Notch pro-differentiation and tumour suppressive function in keratinocytes

I. Résumé large publicIRF6 est un médiateur de Notch dans la différenciation des kératinocytes et dans sa fonction de suppresseur de tumeursLa peau est l'organe le plus important du corps humain, elle représente chez l'adulte une surface d'environ 1,5 m2 et elle est composée de 2000 milliards de cellules. La peau est composée de plusieurs types cellulaires dont les kératinocvtes. Ces cellules, qui se trouvent dans la couche la plus externe de la peau (Pépiderme), nous protègent de la déshydratation et des agressions externes telles que les infections et rayons ultraviolets. Cette fonction de « barrière » est mise en place grâce à un processus appelé différenciation des kératinocvtes durant lequel les kératinocytes deviennent matures et finalement meurent pour former la couche cornée la plus externe difficilement pénétrable. L'homéostasie tissulaire est un mécanisme qui régule l'équilibre entre prolifération, différentiation et mort cellulaire. Une perturbation de cet équilibre peut mener à la formation d'une tumeur. Il existe différents types de tumeurs de la peau. Nous nous sommes intéressés aux «carcinomes spino-cellulaires» (SCC) qui se développent à partir des keratinocytes en différenciation. Notch est une molécule impliquée positivement dans la différenciation des kératinocytes et joue un rôle prépondérant dans la suppression des tumeurs kératinocytaires comme les SCC dans lesquelles Notch est faiblement exprimé. L'implication de Notch dans la différenciation et dans la carcinogenèse kératinocytaire n'est plus controversée, mais les mécanismes qui sont à la base de ces fonctions restent encore à élucider. IRfF6 est une protéine qui, d'après sa structure, a été classée parmi une famille de régulateurs de la défense de l'organisme (IRFs). Des études ultérieures ont montré qu'IRf 6 n'a pas de rôle dans la réponse immunitaire mais qu'il est plutôt impliqué dans le développement de l'épiderme. Dans ce travail, nous avons établi que, dans les kératinocytes, l'expression d'IPJF6 est contrôlé par Notch et que, comme pour ce dernier, elle est réduite dans les SCCs. De plus, nous avons observé qu'IRF6 régule les mêmes gènes que Notch, et qu'il est en effet un médiateur de la fonction de Notch dans la différenciation des kératinocytes. Parmi les gènes contrôlés par l'axe Notch-IRF6 il y en a trois qui sont sur-exprimés dans les SCCs et qui sont réprimés par cet axe. Il s'agit d'une part d'IRF3 et IRF7, deux autres membres de la famille IRF, et du récepteur EGFR (Epidermal growth factor receptor), un oncogène (un gène impliqué dans l'accélération de la formation de tumeurs). Dans leur ensemble, ces découvertes nous informent sur les mécanismes impliqués dans les fonctions pro-differentiatrice et tumeur suppressive de Notch. Plus encore, elles ouvrent des perspectives intéressantes quant au développement de nouvelles approches thérapeutiques dans le traitement des cancers.II. RésuméLa voie de signalisation de Notch joue un rôle très important dans la différenciation cellulaire et dans la carcinogenèse de nombreux tissus. Dans les kératinocytes, elle agit comme suppresseur de tumeurs, fonction altérée dans les cancers spino cellulaires SCC (tumeurs kératinocytaires) de part la perte d'expression de Notch.Bien que les fonctions pro-différenciatrice et tumeur-suppressive de la voie de signalisation de Notch soient aujourd'hui reconnues, les mécanismes sous-jacents restent à explorer.Dans ce travail, nous montrons qu'IRF6, un membre de la famille des régulateurs de la voie de l'interféron (IRF), ne possédant pas de rôles dans la réponse immunitaire mais essentiel dans le développement de l'épiderme, est d'autant plus exprimé que le kératinocytes sont différenciées alors que son expression est drastiquement diminuée dans les SCC. De façon intéressante, l'expression d'IRF6 durant la différenciation kératinocytaire est directement contrôlée par Notch.Dans les kératinocytes l'expression accrue d'IRP6 a les mêmes effets que 1'activation de la voie de Notch induisant les marqueurs de différentiation des couches supra-basales de l'épiderme et inhibant ceux de la couche basale impliqués dans la prolifération cellulaire. Cependant IRF6 n'est pas impliqué dans la régulation d'autres cibles de Notch, comme p21WAFI/CiP' et Hesl. Comme Notch, IRF6 contrôle négativement l'expression de EGFR et IRF3/7. De ce fait EGFR et IRF3 et IRF7 sont fortement exprimés dans les SCCs humaines où l'expression de Notch et IRF6 est fortement réduite.En conclusion, nous avons démontré qu'IRF6 est une cible directe de Notch/CSL dans les keratinocytes qui medie les effets "non-canonique" de cette voie de signalisation dans la différentiation et dans la suppression tumorale.III. SummaryThe Notch pathway is an important regulator of differentiation and carcinogenesis. In keratinocytes it acts as tumour suppressor and the Notch gene is markedly reduced in keratinocyte-derived squamous cell carcinoma (SCC). While the pro-differentiation and tumour suppressive functions of Notch signalling in keratinocytes are well established, the underlying mechanisms are still poorly understood, We report here that Interferon Regulatory Factor 6 (IRF6), an IRF family member with an essential role in epidermal development, is downmodulated in SCC and is induced in differentiating cells. We observed that the induction of IRF6 in differentiating keratinocytes is suppressed by Notch inhibition. IRF6 expression is also decreased in mice with keratinocyte-specific deletion of the Notch 1/2.Moreover we show that the expression of this gene is induced by Notch activation through a CSL-dependent mechanism even under conditions of protein synthesis inhibition, with endogenous Notch 1 binding to the IRF6 promoter.Increased IRJF6 expression is necessary for the impact of Notch activation on differentiation markers K1 and Involucrin, and proliferation markers integrins and p63, but not on other "canonical" Notch targets like p21WAF1/Cipl, Hes1 and Hey1. Like Notch 1, IRF6 down-modulates expression of epidermal growth factor receptor (EGFR) as well as two other IRF family members, IRF3 and 7, which we previously linked to positive control of p63 expression. Expression of IRF3, IRF7 and EGFR is enhanced in cutaneous squamous cell carcinomas, illustrating a strikingly opposite pattern compared to Notch and IRF6.Thus, IRF6 is a primary Notch target in keratinocytes, which mediates the effects of this pathway on differentiation and contributes to tumor suppression.

Stratigraphy, sedimentology and depositional environments of the Permian to uppermost Cretaceous Batain Group, eastern-Oman

Permian to Late Cretaceous allochthonous sedimentary and volcanic rocks exposed in the Batain area (eastern Oman Margin) have received comparably little attention in the past. They largely were considered as part of the Hamrat Duru Group (Hawasina Complex) of the northern Oman Mountains. Structural, kinematic and biostratigraphic results from our mapping campaign in the Batain area have now revealed, that emplacement of these units occurred in a WNW direction during latest Cretaceous/Early Paleogene time. This clearly contrasts with previous models that postulated a S-ward directed obduction in Campanian times such as recorded from the Hawasina Complex and Semail Ophiolite in the Oman Mountains. We herewith establish the `'Batain Group'' comprising all Permian to Late Cretaceous allochthonous units in the Batain Area. These are: 1.) the Permian Qarari Formation deposited in the toe of a slope setting; 2.) the Late Permian to late Liassic Al Jil Formation comprising periplatform detritus and very coarse breccias; 3.) the Scythian to Norian Matbat Formation formed by slope deposits; 4.) the Early Jurassic to early Oxfordian Guwayza Formation with high energy platform detritus; 5.) the Mid-Jurassic to earliest Cretaceous Ruwaydah Formation seamount; and 6.) the Oxfordian to Santonian Wahrah Formation, mainly radiolarites; and 7.) the Santonian to latest Maastrichtian Fayah Formation built by flysch-type sediments. These sedimentary and volcanic rocks represent deposits of the former ``Batain basin'' off eastern-Oman, destroyed by compressional tectonics at the Cretaceous/Paleogene transition. For tectono-stratigraphic reasons the Batain Group does not form part of the Hawasina Complex.

Lateral condyle fracture of the humerus in children treated with bioabsorbable materials

Les fractures du condyle externe de l'enfant sont un traumatisme relativement fréquent qui survient le plus souvent chez l'enfant entre 5 et 15 ans. Elles sont classées en 3 grades : le grade 1 sans déplacement qui peuvent être traitées conservativement et les grades 2 (déplacées) et 3 (disloquées) qui nécessitent une prise en charge chirurgicale par réduction ouverte et embrochage. Le traitement traditionnel de ces fractures consistent en la mise en place de broches/vis métalliques qui doivent être retirées quelques semaines plus tard lors d'une seconde intervention. Depuis les années 90, des matériaux bio-résorbables à base d'acide polyglycoliques sont apparus en chirurgie orthopédique et traumatologique. En raison de la survenue de complications telles que réactions inflammatoires, formation de séromes ou ostéolyse, l'utilisation du matériel conventionnel a été préférée. Cependant, depuis quelques années, de nouveaux matériaux en acide polylactique sont apparus sur le marché. La période de résorption étant beaucoup plus lente, ces matériaux induisent des réactions beaucoup plus faibles, sans conséquences cliniques relevées jusqu'à présent. Chez l'adulte, de récentes études ont prouvés l'efficacité et l'absence d'effets secondaires liés à ces matériaux. Par contre, chez l'enfant, peu d'études à moyen terme ont été réalisées et l'impact sur l'os en croissance est peu connu, même si pour l'heure aucune conséquence clinique n'a été relevée. Dans le cadre de notre étude, nous avons comparé 2 groupes d'enfants traités pour des fractures du condyle externe du coude. Le premier groupe traité par du matériel conventionnel et le second par matériel résorbable. Les enfants ont tous étés suivis de manière très étroite durant la première année et la récupération clinique est similaire pour les 2 groupes. A 4 ans du traumatisme, les résultats fonctionnels sont identiques pour les 2 groupes et aucune complication liée au matériel résorbable n'a été mise en évidence. Par ailleurs, à 1 et 4 ans, les clichés radiologiques montrent l'absence de lésions liées au matériel résorbable. En conclusion, dans le cadre de notre travail nous avons pu montrer l'efficacité des matériaux résorbables dans la prise en charge des fractures du condyle externe du coude chez l'enfant. Ces matériaux permettent d'optimiser la prise en charge de ce type de fracture en prévenant un risque opératoire et anesthésique liés à une seconde intervention nécessaire au retrait du matériel d'ostéosynthèse conventionnel. Par ailleurs le coût lié à la prise en charge globale de ce type de fracture est moindre lors de l'utilisation de matériel résorbable.

Radar analysis of the life cycle of mesoscale convective systems during the 10 June 2000 event

The 10 June 2000 event was the largest flash flood event that occurred in the Northeast of Spain in the late 20th century, both as regards its meteorological features and its considerable social impact. This paper focuses on analysis of the structures that produced the heavy rainfalls, especially from the point of view of meteorological radar. Due to the fact that this case is a good example of a Mediterranean flash flood event, a final objective of this paper is to undertake a description of the evolution of the rainfall structure that would be sufficiently clear to be understood at an interdisciplinary forum. Then, it could be useful not only to improve conceptual meteorological models, but also for application in downscaling models. The main precipitation structure was a Mesoscale Convective System (MCS) that crossed the region and that developed as a consequence of the merging of two previous squall lines. The paper analyses the main meteorological features that led to the development and triggering of the heavy rainfalls, with special emphasis on the features of this MCS, its life cycle and its dynamic features. To this end, 2-D and 3-D algorithms were applied to the imagery recorded over the complete life cycle of the structures, which lasted approximately 18 h. Mesoscale and synoptic information were also considered. Results show that it was an NS-MCS, quasi-stationary during its stage of maturity as a consequence of the formation of a convective train, the different displacement directions of the 2-D structures and the 3-D structures, including the propagation of new cells, and the slow movement of the convergence line associated with the Mediterranean mesoscale low.