Gain-of-function haplotype in the epithelial calcium channel TRPV6 is a risk factor for renal calcium stone formation.

The rate-limiting step of dietary calcium absorption in the intestine requires the brush border calcium entry channel TRPV6. The TRPV6 gene was completely sequenced in 170 renal calcium stone patients. The frequency of an ancestral TRPV6 haplotype consisting of three non-synonymous polymorphisms (C157R, M378V, M681T) was significantly higher (P = 0.039) in calcium stone formers (8.4%; derived = 502, ancestral = 46) compared to non-stone-forming individuals (5.4%; derived = 645, ancestral = 37). Mineral metabolism was investigated on four different calcium regimens: (i) free-choice diet, (ii) low calcium diet, (iii) fasting and (iv) after a 1 g oral calcium load. When patients homozygous for the derived haplotype were compared with heterozygous patients, no differences were found with respect to the plasma concentrations of 1,25-vitamin D, PTH and calcium, and the urinary excretion of calcium. In one stone-forming patient, the ancestral haplotype was found to be homozygous. This patient had absorptive hypercalciuria. We therefore expressed the ancestral protein (157R+378V+681T) in Xenopus oocytes and found a significantly enhanced calcium permeability when tested by a (45)Ca(2+) uptake assay (7.11 +/- 1.93 versus 3.61 +/- 1.01 pmol/min/oocyte for ancestral versus derived haplotype, P < 0.01). These results suggest that the ancestral gain-of-function haplotype in TRPV6 plays a role in calcium stone formation in certain forms of absorptive hypercalciuria.

GATA3-driven Th2 responses inhibit TGF-beta1-induced FOXP3 expression and the formation of regulatory T cells.

Transcription factors act in concert to induce lineage commitment towards Th1, Th2, or T regulatory (Treg) cells, and their counter-regulatory mechanisms were shown to be critical for polarization between Th1 and Th2 phenotypes. FOXP3 is an essential transcription factor for natural, thymus-derived (nTreg) and inducible Treg (iTreg) commitment; however, the mechanisms regulating its expression are as yet unknown. We describe a mechanism controlling iTreg polarization, which is overruled by the Th2 differentiation pathway. We demonstrated that interleukin 4 (IL-4) present at the time of T cell priming inhibits FOXP3. This inhibitory mechanism was also confirmed in Th2 cells and in T cells of transgenic mice overexpressing GATA-3 in T cells, which are shown to be deficient in transforming growth factor (TGF)-beta-mediated FOXP3 induction. This inhibition is mediated by direct binding of GATA3 to the FOXP3 promoter, which represses its transactivation process. Therefore, this study provides a new understanding of tolerance development, controlled by a type 2 immune response. IL-4 treatment in mice reduces iTreg cell frequency, highlighting that therapeutic approaches that target IL-4 or GATA3 might provide new preventive strategies facilitating tolerance induction particularly in Th2-mediated diseases, such as allergy.

Formation of chlorite during thrust fault reactivation. Record of fluid origin and P-T conditions in the Monte Perdido thrust fault (southern Pyrenees)

The chemical and isotopic compositions of clay minerals such as illite and chlorite are commonly used to quantify diagenetic and low-grade metamorphic conditions, an approach that is also used in the present study of the Monte Perdido thrust fault from the South Pyrenean fold-and-thrust belt. The Monte Perdido thrust fault is a shallow thrust juxtaposing upper Cretaceous-Paleocene platform carbonates and Lower Eocene marls and turbidites from the Jaca basin. The core zone of the fault, about 6 m thick, consists of intensely deformed clay-bearing rocks bounded by major shear surfaces. Illite and chlorite are the main hydrous minerals in the fault zone. Illite is oriented along cleavage planes while chlorite formed along shear veins (< 50 mu m in thickness). Authigenic chlorite provides essential information about the origin of fluids and their temperature. delta O-18 and delta D values of newly formed chlorite support equilibration with sedimentary interstitial water, directly derived from the local hanging wall and footwall during deformation. Given the absence of large-scale fluid flow, the mineralization observed in the thrust faults records the P-T conditions of thrust activity. Temperatures of chlorite formation of about 240A degrees C are obtained via two independent methods: chlorite compositional thermometers and oxygen isotope fractionation between cogenetic chlorite and quartz. Burial depth conditions of 7 km are determined for the Monte Perdido thrust reactivation, coupling calculated temperature and fluid inclusion isochores. The present study demonstrates that both isotopic and thermodynamic methods applied to clay minerals formed in thrust fault are useful to help constrain diagenetic and low-grade metamorphic conditions.

New gene functions in megakaryopoiesis and platelet formation.

Platelets are the second most abundant cell type in blood and are essential for maintaining haemostasis. Their count and volume are tightly controlled within narrow physiological ranges, but there is only limited understanding of the molecular processes controlling both traits. Here we carried out a high-powered meta-analysis of genome-wide association studies (GWAS) in up to 66,867 individuals of European ancestry, followed by extensive biological and functional assessment. We identified 68 genomic loci reliably associated with platelet count and volume mapping to established and putative novel regulators of megakaryopoiesis and platelet formation. These genes show megakaryocyte-specific gene expression patterns and extensive network connectivity. Using gene silencing in Danio rerio and Drosophila melanogaster, we identified 11 of the genes as novel regulators of blood cell formation. Taken together, our findings advance understanding of novel gene functions controlling fate-determining events during megakaryopoiesis and platelet formation, providing a new example of successful translation of GWAS to function.

Régulation du processus métastatique tumoral par l'oxyde nitrique (NO), le TGF-β el les cellules de l'hôte

RESUME Nous avons étudié le rôle de deux molécules, le Transfon-ning Growth Factor (TGF-β) et l'oxyde nitrique (NO), dans le processus métastatique. Deux clones tumoraux ont été sélectionnés à partir d'un carcinome du côlon pour leur différence de potentiel tumorigénique dans des rats syngéniques. La croissance tumorale du clone progressif PROb a été corrélée à sa capacité à sécréter le TGF-β actif Cependant, la transfection du clone régressif REGb, sécrétant du TGF-β latent, par une vecteur codant pour le TGF-β bio-actif n'a pas permis d'induire le développement tumoral. Les deux clones tumoraux présentent des activités des protéases MMP-2, APN et DPPIV identiques et qui ne semblent pas modifiées par le TGF-β. L'interaction des cellules tumorales avec l'endothélium et l'activité de la NO synthase (iNOS) responsable de la synthèse de NO sont impliqués dans la progression de nombreux cancers. Le clone PROb, mais pas le clone REGb, inhibe l'activation de la iNOS des cellules endothéliales par sa sécrétion de TGF-β actif Les deux clones montrent cependant des propriétés d'adhésion identiques aux cellules endothéliales et sont capables d'inhiber par contact cellulaire direct l'activation de la iNOS endothéliale. Ceci suggère que ces contacts directs pourraient créer un micro-environnement favorable à la conversion du TGF-β latent en TGF-β actif ou à d'autres interactions moléculaires pouvant réguler l'activation endothéliale. Par ailleurs, les deux clones activent des macrophages du système nerveux central, organe où ils ne forment pas de métastases, mais pas les macrophages circulants, illustrant des mécanismes différentiels et spécifiques dans l'activation de différents types de cellules immunitaires. Afin de mieux comprendre le rôle du NO dans la dissémination métastatique, deux clones cellulaires différant par le taux d'activité de la iNOS ont été sélectionnés à partir de la lignée murine parentale de carcinome du sein EMT-6. Bien que le NO soit un inhibiteur potentiel de la prolifération cellulaire, les deux clones montrent des propriétés prolifératives identiques in vitro. Les cellules EMT-6H qui produisent peu de NO in vitro forment de nombreux nodules tumoraux pulmonaires in vivo corrélés à une mortalité significative des souris syngéniques injectées. Les cellules EMT-6J qui présentent une expression élevée de iNOS et de NO induisent de rares nodules tumoraux pulmonaires et peu de mortalité. Dans ce modèle, l'expression tumorale de NO semble donc défavoriser la croissance tumorale. Les deux clones cellulaires ont des propriétés identiques d'adhésion et de prolifération mesurées in vitro sur des cellules endothéliales primaires isolées de différents organes et in vivo par une colocalisation identique dans les poumons de souris syngéniques 48h après leur injection. Les cellules EMT-6H présentent une activité MMP-2 plus élevée alors que les activités des protéases APN et DPPIV sont identiques dans les deux clones cellulaires. Le TGF-β soluble ainsi que les fibroblastes primaires bloquent la prolifération des deux clones cellulaires. Cependant, l'activation préalable des fibroblastes par du TGF-β restaure partiellement la prolifération du clone EMT-6H mais pas celle du clone EMT-6J. Ces résultats montrent que le rôle de molécules telles que le TGF-β et le NO tumoral dans la progression tumorale doit être considéré dans un contexte d'interactions des cellules tumorales avec les différentes types cellulaires de l'hôte: en particulier, notre travail souligne que les macrophages et les fibroblastes sont déterminants dans la progression métastatique des carcinomes du côlon ou du sein. RESUME DESTINE A UN LARGE PUBLIC Les métastases tumorales, disséminées et intraitables par chirurgie, représentent un problème majeur dans le traitement clinique du cancer. Elles sont dues à des cellules tumorales qui ont migré de leur site tumoral primaire, circulé et survécu dans le système vasculaire de l'hôte, échappé au système immunitaire, adhéré à et survécu sur l'endothélium des vaisseaux, et envahi le tissu sous-jacent où elles ont proliféré. Cette capacité à former des métastases implique de nombreux facteurs dont certains ont été identifiés mais dont le rôle reste controversé dans les différentes études. Nous nous sommes intéressés au rôle de l'oxyde nitrique (NO) et du facteur de croissance et de transformation cellulaire TGF-β. Dans les carcinomes du sein, l'expression des enzymes responsables de la synthèse de NO a été corrélée avec l'invasion tumorale mais aussi avec un pronostic favorable selon les études. Deux clones cellulaires ont été isolés à partir de la tumeur mammaire EMT-6 chez la souris. Le clone EMT-6H sécrète peu de NO et forme de nombreuses tumeurs dans les poumons des souris *entraînant leur décès. Le clone EMT-6J sécrète beaucoup de NO et ne se développe que peu dans les poumons. Dans ce modèle expérimental, le NO semble donc défavoriser la croissance tumorale. L'analyse des interactions avec les cellules de l'hôte rencontrées lors de la formation de métastases pulmonaires a montré que les deux clones cellulaires adhérent et prolifèrent de manière similaire sur les cellules endothéliales tapissant l'intérieur des vaisseaux sanguins. L'arrêt des cellules tumorales dans les poumons ne permet donc pas d'expliquer la différence de croissance tumorale. Cependant, le clone agressif EMT-6H présente une activité élevée d'une protéase (MMP-2) qui lui permettrait par la suite d'envahir le tissu pulmonaire. Par ailleurs, l'activation des fibroblastes du tissu pulmonaire par le TGF-β, une molécule observée dans des conditions inflammatoires, permet au clone agressif EMT-6H de proliférer mais inhibe la croissance du clone EMT-6J. Dans un modèle expérimental de carcinome du côlon, le TGF-β est considéré favorable à la croissance tumorale. Isolées à partir de la même tumeur initiale, deux lignées de cellules ont des comportements opposés lorsqu'elles sont injectées sous la peau des rats. La capacité de la lignée PROb à former des tumeurs a été corrélée à la sécrétion de TGF-β actif L'introduction du gène codant pour le TGF-β actif dans la lignée REGb, qui ne sécrète pas de TGF-β actif et ne forme pas de tumeurs chez le rat, ne restaure pas leur potentiel tumorigénique. Dans ce modèle, l'expression de TGF-β actif ne semble donc pas suffisante à la croissance tumorale. Les interactions avec différents types cellulaires de l'hôte ont été étudiées. Les deux lignées tumorales adhérent de manière similaire sur les cellules endothéliales et sont capables d'inhiber leur activation, un mécanisme qui pourrait participer à la destruction. Les deux lignées activent les cellules immunitaires du système nerveux central, un organe où elles ne forment pas de métastase. Ces résultats suggèrent que la sélection des cellules métastatiques ne s'effectue pas sur l'endothélium des vaisseaux sanguins mais à des étapes ultérieures dans le micro- environnement cellulaire du nouvel organe colonisé. SUMMARY Metastasis results from the migration of tumor cells from their primary tumor, circulation through the bloodstream, attachment to the endothelium, and invasion of the surrounding tissue where they create a microenvironnement favoring their growth. This multistep process implies various cellular interactions and molecules. Among those, we were interested in the role of the Transforming Growth Factor beta (TGF-β) and the nitric oxide (NO). Two cell lines were isolated from a rat colon tumor and assessed for their metastatic potential in vivo. The PROb cell line that expresses active TGF-β formed subcutaneous tumors in rats while the REGb cell line that expresses only latent TGF-β did not. Transfection of REGb cells with a plasmid encoding for the active form of TGF-β failed to restore their metastatic ability. Thus TGF-β secretion is not sufficient to induce colon carcinoma progression. Activities of various proteases such as APN, DPPIV and MMP were similar in both cell lines and were not regulated by TGF-β. Interactions with the endothelium as well as NO synthase activity (iNOS) and local NO concentrations are believed to be crucial steps in cancer metastasis. Coculture of the two clones with endothelial cells inhibited the cytokine-triggered activation of the iNOS enzyme in primary rat endothelial cells but only PROb cells were capable of increasing the expression of IL-6, a protumoral interleukin that may participate in the impairment of the anti-tumoral immune response of the host. Both cell lines exhibited potential to activate microglial cells but not bone marrow-derived macrophages, pointing to a differential regulation of specialized immune cells. To better understand the conflicting role of NO in breast cancer progression, two cell clones were selected from the murine tumorigenic cell line EMT-6 based on their iNOS activity and NO secretion. Although NO has been shown to inhibit cell proliferation, the two cell clones exhibited similar proliferation rates in vitro. The EMT-6H cells expressed little NO and grew actively in the lungs of syngenic mice, leading to their death. Opposite results were observed with the EMT-6J cells. In these in vivo conditions, NO seems to impair tumor growth. Both clones exhibited similar in vitro adhesive properties to primary endothelial cells isolated from various mouse organs and similar localization in the lungs of mice 48 hours after injection. Sustained metalloproteinase MMP-2 activity was detected in the tumorigenic EMT-6H clone, but not in the EMT-6J cells while other proteases such as APN and DPPIV showed no difference. These results suggested that the two clones differed in invasion steps following adhesion to the endothelium and that NO did not participate in previous steps. Consistent with this, both soluble TGF-β and supernatants of cultures of mouse primary lung fibroblasts inhibited the growth of the two clones. However, previous activation of these fibroblasts with TGF-β restored the growth of the tumorigenic EMT-6H cells, but not of EMT-6J cells. Altogether, these results indicate that the role of a given molecule, such as NO or TGF-β, must be considered in a context of interaction of tumor cells with host cells. They further imply that interaction of tumor cells with specialized immune cells and with stromal cells of the colonized organ, rather than with the endothelium, are critical in regulating metastasis.

Anachronistic facies from a drowned Lower Triassic carbonate platform: Lower member of the Alwa Formation (Ba'id Exotic), Oman Mountains

- The lower member of the Alwa Formation (Lower Olenekian), found within the Ba'id Exotic in the Oman Mountains (Sultanate of Oman), consists of ammonoid-bearing, pelagic limestones that were deposited on an isolated, drowned carbonate platform on the Neotethyan Gondwana margin. The strata contain a variety of unusual carbonate textures and features, including thrombolites, Frutexites-bearing microbialites that contain synsedimentary cements, matrix-free breccias surrounded by isopachous calcite cement, and fissures and cavities filled with large botryoidal cements. Thrombolites are found throughout the study interval, and occur as 0.5-1.0 m thick lenses or beds that contain laterally laterally-linked stromatactis cavities. The Frutexites-bearing microbialites occur less frequently, and also form lenses or beds, up to 30 cm thick; the microbialites may be laminated, and often developed on hardgrounds. In addition, the Frutexites-bearing microbialites also contain synsedimentary calcite cement crusts and botryoids (typically <1 cm thick) that harbour layers or pockets of what appear to be bacterial sheaths and coccoids, and are indicative of biologically mediated precipitation of the cement bodies. Slumping following lithification led to fracturing of the limestone and the precipitation of large, botryoidal aragonite cements in fissures that cut across the primary fabric. Environmental conditions, specifically palaeoxygenation and the degree of calcium carbonate supersaturation, likely controlled whether the thrombolites (high level of calcium carbonate supersaturation associated with vertical mixing of water masses and dysoxic conditions) or Frutexites-bearing microbialites (low level of calcium carbonate supersaturation associated with anoxic conditions and deposition below a stable chemocline) formed. The results of this study point to continued environmental stress in the region during the Early Triassic that likely contributed to the uneven recovery from the Permian-Triassic mass extinction.

Repression of flagellar genes in exponential phase by CsgD and CpxR, two crucial modulators of Escherichia coli biofilm formation.

Escherichia coli adapts its lifestyle to the variations of environmental growth conditions, swapping between swimming motility or biofilm formation. The stationary-phase sigma factor RpoS is an important regulator of this switch, since it stimulates adhesion and represses flagellar biosynthesis. By measuring the dynamics of gene expression, we show that RpoS inhibits the transcription of the flagellar sigma factor, FliA, in exponential growth phase. RpoS also partially controls the expression of CsgD and CpxR, two transcription factors important for bacterial adhesion. We demonstrate that these two regulators repress the transcription of fliA, flgM, and tar and that this regulation is dependent on the growth medium. CsgD binds to the flgM and fliA promoters around their -10 promoter element, strongly suggesting direct repression. We show that CsgD and CpxR also affect the expression of other known modulators of cell motility. We propose an updated structure of the regulatory network controlling the choice between adhesion and motility.

Biogeochemical evolution of a marine shore tailings deposit during bioremediation

Summary : Mining activities produce enormous amounts of waste material known as tailings which are composed of fine to medium size particles. These tailings often contain sulfides, which oxidation can lead to acid and metal contamination of water; therefore they need to be remediated. In this work a tailings bioremediation approach was investigated by an interdisciplinary study including geochemistry, mineralogy and microbiology. The aim of the work was to study the effect of the implementation of wetland above oxidizing tailings on the hydrogeology and the biogeochemical element cycles, and to assess the system evolution over time. To reach these goals, biogeochemical processes occurring in a marine shore tailings deposit were investigated. The studied tailings deposit is located at the Bahìa de Ite, Pacific Ocean, southern Peru, where between 1940 and 1996 the tailings were discharged from the two porphyry copper mines Cuajone and Toquepala. After the end of deposition, a remediation approach was initiated in 1997 with a wetland implementation above the oxidizing tailings. Around 90% of the tailings deposits (total 16 km2) were thus remediated, except the central delta area and some areas close to the shoreline. The multi-stable isotope study showed that the tailings were saturated with fresh water in spite of the marine setting, due to the high hydraulic gradient resulting from the wetland implementation. Submarine groundwater discharge (SGD) was the major source of SO4 2-, C1-, Na+, Fe2+, and Mn2+ input into the tailings at the original shelf-seawater interface. The geochemical study (aquatic geochemistry and X-Ray diffraction (XRD) and sequential extractions from the solid fraction) showed that iron and sulfur oxidation were the main processes in the non-remediated tailings, which showed a top a low-pH oxidation zone with strong accumulation of efflorescent salts at the surface due to capillary upward transport of heavy metals (Fe, Cu, Zn, Mn, Cd, Co, and Ni) in the arid climate. The study showed also that the implementation of the wetland resulted in very low concentrations of heavy metals in solution (mainly under the detection limit) due to the near neutral pH and more reducing conditions (100-150 mV). The heavy metals, which were taken from solution, precipitated as hydroxides and sulfides or were bound to organic matter. The bacterial community composition analysis by Terminal Restriction Fragment Length Polymorphism (T-RFLP) and cloning and sequencing of 16S rRNA genes combined with a detailed statistical analysis revealed a high correlation between the bacterial distribution and the geochemical variables. Acidophilic autotrophic oxidizing bacteria were dominating the oxidizing tailings, whereas neutrophilic and heterotrophic reducing bacteria were driving the biogeochemical processes in the remediated tailings below the wetland. At the subsurface of the remediated tailings, an iron cycling was highlighted with oxidation and reduction processes due to micro-aerophilic niches provided by the plant rhizosphere in this overall reducing environment. The in situ bioremediation experiment showed that the main parameter to take into account for the effectiveness was the water table and chemistry which controls the system. The constructed remediation cells were more efficient and rapid in metal removal when saturation conditions were available. This study showed that the bioremediation by wetland implementation could be an effective and rapid treatment for some sulfidic mine tailings deposits. However, the water saturation of the tailings has to be managed on a long-term basis in order to guarantee stability. Résumé : L'activité minière produit d'énormes quantités de déchets géologiques connus sous le nom de « tailings » composées de particules de taille fine à moyenne. Ces déchets contiennent souvent des sulfures dont l'oxydation conduit à la formation d'effluents acides contaminés en métaux, d'où la nécessité d'effectuer une remédiation des sites de stockage concernés. Le but de ce travail est dans un premier temps d'étudier l'effet de la bio-remédiation d'un dépôt de tailings oxydés sur l'hydrogéologie du système et les cycles biogéochimiques des éléments et en second lieu, d'évaluer l'évolution du processus de remédiation dans le temps. Le site étudié dans ce travail est situé dans la Bahía de Ite, au sud du Pérou, au bord de l'Océan Pacifique. Les déchets miniers en question sont déposés dans un environnement marin. De 1940 à 1996, les déchets de deux mines de porphyre cuprifère - Cuajone et Toquepala - ont été acheminés sur le site via la rivière Locumba. En 1997, une première remédiation a été initiée avec la construction d'une zone humide sur les tailings. Depuis, environ 90% de la surface du dépôt (16 km2) a été traité, les parties restantes étant la zone centrale du delta du Locumba et certaines zones proches de la plage. Malgré la proximité de l'océan, les études isotopiques menées dans le cadre de ce travail ont montré que les tailings étaient saturés en eau douce. Cette saturation est due à la pression hydraulique résultant de la mise en place des zones humides. Un écoulement d'eau souterrain sous-marin a été à détecté à l'interface entre les résidus et l'ancien fond marin. En raison de la géologie locale, il constitue une source d'entrée de SO4 2-, Cl-, Na+, FeZ+, et Mn2+ dans le système. L'analyse de la géochimie aquatique, la Diffraction aux Rayons X (XRD) et l'extraction séquentielle ont montré que l'oxydation du fer et .des sulfures est le principal processus se produisant dans les déchets non remédiés. Ceci a entraîné le développement d'une zone d'oxydation à pH bas induisant une forte accumulation des sels efflorescents, conséquence de la migration capillaire des métaux lourds (Fe, Cu, Zn, Mn, Cd, Co et Ni) de la solution vers la surface dans ce climat aride. Cette étude a montré également que la construction de la zone humide a eu comme résultats une précipitation des métaux dans des phases minérales en raison du pH neutre et des conditions réductrices (100-150mV). Les métaux lourds ont précipité sous la forme d'hydroxydes et de sulfures ou sont adsorbés à la matière organique. L'analyse de la composition de la communauté bactérienne à l'aide la technique T-RFLP (Terminal Restriction Fragment Length Polymorphism) et par le clonage/séquençage des gènes de l'ARNr 16S a été combinée à une statistique détaillée. Cette dernière a révélé une forte corrélation entre la distribution de bactéries spécifiques et la géochimie : Les bactéries autotrophes acidophiles dominent dans les déchets oxydés non remédiés, tandis que des bactéries hétérotrophes neutrophiles ont mené les processus microbiens dans les déchets remédiés sous la zone humide. Sous la surface de la zone humide, nos analyses ont également mis en évidence un cycle du fer par des processus d'oxydoréduction rendus possibles par la présence de niches micro-aérées par la rhizosphère dans cet environnement réducteur. L'expérience de bio-remédiation in situ a montré que les paramètres clés qui contrôlent l'efficacité du traitement sont le niveau de la nappe aquifère et la chimie de l'eau. Les cellules de remédiation se sont montrées plus efficaces et plus rapides lorsque le système a pu être saturé en eau. Finalement, cette étude a montré que la bio-remédiation de déchets miniers par la construction de zones humides est un moyen de traitement efficace, rapide et peu coûteux. Cependant, la saturation en eau du système doit être gérée sur le long terme afin de garantir la stabilité de l'ensemble du système.

Fibronectin distribution in the chick embryo during formation of the blastula.

The distribution of the fibronectin-rich extracellular matrix (ECM) in the chick embryo during formation of the blastula has been evaluated semiquantitatively using an electron microscopical immunogold staining technique. During the first 10 h of postlaying development, fibronectin was found in both embryonic area pellucida and extra-embryonic area opaca of the blastoderm. In the area pellucida, the fibronectin was (1) associated with the basal lamina of the epiblast, (2) present between epiblastic and hypoblastic cells and (3) occasionally internalized in hypoblastic cells. Along the embryonic axis, a transient and high density of ECM was associated with the front of the anteriorly and rapidly expanding hypoblast. Very high density of fibronectin was observed in the marginal zone of the area pellucida, where the epiblastic and deeper cell layers show contacts and intense re-arrangements. In the area opaca, fibronectin was at first found only sporadically between contacting cells, but its density increased steadily and markedly during the first day of development. These rapid and significant changes in the regional distribution of fibronectin-rich ECM are discussed with respect to the early morphogenesis of the chick embryo.

Influence of physico-chemical material characteristics on staphylococcal biofilm formation--a qualitative and quantitative in vitro analysis of five different calcium phosphate bone grafts.

Various compositions of synthetic calcium phosphates (CaP) have been proposed and their use has considerably increased over the past decades. Besides differences in physico-chemical properties, resorption and osseointegration, artificial CaP bone graft might differ in their resistance against biofilm formation. We investigated standardised cylinders of 5 different CaP bone grafts (cyclOS, chronOS (both β-TCP (tricalcium phosphate)), dicalcium phosphate (DCP), calcium-deficient hydroxyapatite (CDHA) and α-TCP). Various physico-chemical characterisations e.g., geometrical density, porosity, and specific surface area were investigated. Biofilm formation was carried out in tryptic soy broth (TSB) and human serum (SE) using Staphylococcus aureus (ATCC 29213) and S. epidermidis RP62A (ATCC 35984). The amount of biofilm was analysed by an established protocol using sonication and microcalorimetry. Physico-chemical characterisation showed marked differences concerning macro- and micropore size, specific surface area and porosity accessible to bacteria between the 5 scaffolds. Biofilm formation was found on all scaffolds and was comparable for α-TCP, chronOS, CDHA and DCP at corresponding time points when the scaffolds were incubated with the same germ and/or growth media, but much lower for cyclOS. This is peculiar because cyclOS had an intermediate porosity, mean pore size, specific surface area, and porosity accessible to bacteria. Our results suggest that biofilm formation is not influenced by a single physico-chemical parameter alone but is a multi-step process influenced by several factors in parallel. Transfer from in vitro data to clinical situations is difficult; thus, advocating the use of cyclOS scaffolds over the four other CaP bone grafts in clinical situations with a high risk of infection cannot be clearly supported based on our data.