Hydrogeophysical data integration at larger scales: Application of Bayesian sequential simulation for the characterization of heterogeneous alluvial aquifers

Knowledge of the spatial distribution of hydraulic conductivity (K) within an aquifer is critical for reliable predictions of solute transport and the development of effective groundwater management and/or remediation strategies. While core analyses and hydraulic logging can provide highly detailed information, such information is inherently localized around boreholes that tend to be sparsely distributed throughout the aquifer volume. Conversely, larger-scale hydraulic experiments like pumping and tracer tests provide relatively low-resolution estimates of K in the investigated subsurface region. As a result, traditional hydrogeological measurement techniques contain a gap in terms of spatial resolution and coverage, and they are often alone inadequate for characterizing heterogeneous aquifers. Geophysical methods have the potential to bridge this gap. The recent increased interest in the application of geophysical methods to hydrogeological problems is clearly evidenced by the formation and rapid growth of the domain of hydrogeophysics over the past decade (e.g., Rubin and Hubbard, 2005).

Anatomy of contaminated aquifers of an industrial site: insights from the stable isotope compositions of waters and dissolved inorganic carbon

The hydrogen and oxygen isotopes of water and the carbon isotope composition of dissolved inorganic carbon (DIC) from different aquifers at an industrial site, highly contaminated by organic pollutants representing residues of the former gas production, have been used as natural tracers to characterize the hydrologic system. On the basis of their stable isotope compositions as well as the seasonal variations, different groups of waters (precipitation, surface waters, groundwaters and mineral waters) as well as seasonably variable processes of mixing between these waters can clearly be distinguished. In addition, reservoir effects and infiltration rates can be estimated. In the northern part of the site an influence of uprising mineral waters within the Quaternary aquifers, presumably along a fault zone, can be recognized. Marginal infiltration from the Neckar River in the cast and surface water infiltration adjacent to a steep hill on the western edge of the site with an infiltration rate of about one month can also be resolved through the seasonal variation. Quaternary aquifers closer to the centre of the site show no seasonal variations, except for one borehole close to a former mill channel and another borehole adjacent to a rain water channel. Distinct carbon isotope compositions and concentrations of DIC for these different groups of waters reflect variable influence of different components of the natural carbon cycle: dissolution of marine carbonates in the mineral waters, biogenic, soil-derived CO2 in ground- and surface waters, as well as additional influence of atmospheric CO2 for the surface waters. Many Quaternary aquifer waters have, however, distinctly lower delta(13)C(DIC) values and higher DIC concentrations compared to those expected for natural waters. Given the location of contaminated groundwaters at this site but also in the industrially well-developed valley outside of this site, the most likely source for the low C-13(DIC) values is a biodegradation of anthropogenic organic substances, in particular the tar oils at the site.

Dirigent domain-containing protein is part of the machinery required for formation of the lignin-based Casparian strip in the root.

The endodermis acts as a "second skin" in plant roots by providing the cellular control necessary for the selective entry of water and solutes into the vascular system. To enable such control, Casparian strips span the cell wall of adjacent endodermal cells to form a tight junction that blocks extracellular diffusion across the endodermis. This junction is composed of lignin that is polymerized by oxidative coupling of monolignols through the action of a NADPH oxidase and peroxidases. Casparian strip domain proteins (CASPs) correctly position this biosynthetic machinery by forming a protein scaffold in the plasma membrane at the site where the Casparian strip forms. Here, we show that the dirigent-domain containing protein, enhanced suberin1 (ESB1), is part of this machinery, playing an essential role in the correct formation of Casparian strips. ESB1 is localized to Casparian strips in a CASP-dependent manner, and in the absence of ESB1, disordered and defective Casparian strips are formed. In addition, loss of ESB1 disrupts the localization of the CASP1 protein at the casparian strip domain, suggesting a reciprocal requirement for both ESB1 and CASPs in forming the casparian strip domain.

Landscape genetics of the Alpine newt (Mesotriton alpestris) inferred from a strip-based approach

Habitat destruction and fragmentation are known to strongly affect dispersal by altering the quality of the environment between populations. As a consequence, lower landscape connectivity is expected to enhance extinction risks through a decrease in gene flow and the resulting negative effects of genetic drift, accumulation of deleterious mutations and inbreeding depression. Such phenomena are particularly harmful for amphibian species, characterized by disjunct breeding habitats. The dispersal behaviour of amphibians being poorly understood, it is crucial to develop new tools, allowing us to determine the influence of landscape connectivity on the persistence of populations. In this study, we developed a new landscape genetics approach that aims at identifying land-uses affecting genetic differentiation, without a priori assumptions about associated ecological costs. We surveyed genetic variation at seven microsatellite loci for 19 Alpine newt (Mesotriton alpestris) populations in western Switzerland. Using strips of varying widths that define a dispersal corridor between pairs of populations, we were able to identify land-uses that act as dispersal barriers (i.e. urban areas) and corridors (i.e. forests). Our results suggest that habitat destruction and landscape fragmentation might in the near future affect common species such as M. alpestris. In addition, by identifying relevant landscape variables influencing population structure without unrealistic assumptions about dispersal, our method offers a simple and flexible tool of investigation as an alternative to least-cost models and other approaches.

Use of high-resolution geophysical data to characterize heterogeneous aquifers: influence of data integration method on hydrological predictions

The integration of geophysical data into the subsurface characterization problem has been shown in many cases to significantly improve hydrological knowledge by providing information at spatial scales and locations that is unattainable using conventional hydrological measurement techniques. The investigation of exactly how much benefit can be brought by geophysical data in terms of its effect on hydrological predictions, however, has received considerably less attention in the literature. Here, we examine the potential hydrological benefits brought by a recently introduced simulated annealing (SA) conditional stochastic simulation method designed for the assimilation of diverse hydrogeophysical data sets. We consider the specific case of integrating crosshole ground-penetrating radar (GPR) and borehole porosity log data to characterize the porosity distribution in saturated heterogeneous aquifers. In many cases, porosity is linked to hydraulic conductivity and thus to flow and transport behavior. To perform our evaluation, we first generate a number of synthetic porosity fields exhibiting varying degrees of spatial continuity and structural complexity. Next, we simulate the collection of crosshole GPR data between several boreholes in these fields, and the collection of porosity log data at the borehole locations. The inverted GPR data, together with the porosity logs, are then used to reconstruct the porosity field using the SA-based method, along with a number of other more elementary approaches. Assuming that the grid-cell-scale relationship between porosity and hydraulic conductivity is unique and known, the porosity realizations are then used in groundwater flow and contaminant transport simulations to assess the benefits and limitations of the different approaches.

Constraints on the permeability structure of alluvial aquifers from P-wave sonic logs

Modern sonic logging tools designed for shallow environmental and engineering applications allow for P-wave phase velocity measurements over a wide frequency band. Methodological considerations indicate that, for saturated unconsolidated sediments in the silt to sand range and source frequencies ranging from approximately 1 to 30 kHz, the observable poro-elastic P-wave velocity dispersion is sufficiently pronounced to allow for reliable first-order estimations of the underlying permeability structure. These predictions have been tested on and verified for a surficial alluvial aquifer. Our results indicate that, even without any further calibration, the thus obtained permeability estimates as well as their variabilities within the pertinent lithological units are remarkably close to those expected based on the corresponding granulometric characteristics.

A novel protein family mediates Casparian strip formation in the endodermis.

Polarized epithelia are fundamental to multicellular life. In animal epithelia, conserved junctional complexes establish membrane diffusion barriers, cellular adherence and sealing of the extracellular space. Plant cellular barriers are of independent evolutionary origin. The root endodermis strongly resembles a polarized epithelium and functions in nutrient uptake and stress resistance. Its defining features are the Casparian strips, belts of specialized cell wall material that generate an extracellular diffusion barrier. The mechanisms localizing Casparian strips are unknown. Here we identify and characterize a family of transmembrane proteins of previously unknown function. These 'CASPs' (Casparian strip membrane domain proteins) specifically mark a membrane domain that predicts the formation of Casparian strips. CASP1 displays numerous features required for a constituent of a plant junctional complex: it forms complexes with other CASPs; it becomes immobile upon localization; and it sediments like a large polymer. CASP double mutants display disorganized Casparian strips, demonstrating a role for CASPs in structuring and localizing this cell wall modification. To our knowledge, CASPs are the first molecular factors that are shown to establish a plasma membrane and extracellular diffusion barrier in plants, and represent a novel way of epithelial barrier formation in eukaryotes.

Integration of high-resolution geophysical data for the characterization of alluvial aquifers : new approaches and implications for hydrological predictions

Abstract Accurate characterization of the spatial distribution of hydrological properties in heterogeneous aquifers at a range of scales is a key prerequisite for reliable modeling of subsurface contaminant transport, and is essential for designing effective and cost-efficient groundwater management and remediation strategies. To this end, high-resolution geophysical methods have shown significant potential to bridge a critical gap in subsurface resolution and coverage between traditional hydrological measurement techniques such as borehole log/core analyses and tracer or pumping tests. An important and still largely unresolved issue, however, is how to best quantitatively integrate geophysical data into a characterization study in order to estimate the spatial distribution of one or more pertinent hydrological parameters, thus improving hydrological predictions. Recognizing the importance of this issue, the aim of the research presented in this thesis was to first develop a strategy for the assimilation of several types of hydrogeophysical data having varying degrees of resolution, subsurface coverage, and sensitivity to the hydrologic parameter of interest. In this regard a novel simulated annealing (SA)-based conditional simulation approach was developed and then tested in its ability to generate realizations of porosity given crosshole ground-penetrating radar (GPR) and neutron porosity log data. This was done successfully for both synthetic and field data sets. A subsequent issue that needed to be addressed involved assessing the potential benefits and implications of the resulting porosity realizations in terms of groundwater flow and contaminant transport. This was investigated synthetically assuming first that the relationship between porosity and hydraulic conductivity was well-defined. Then, the relationship was itself investigated in the context of a calibration procedure using hypothetical tracer test data. Essentially, the relationship best predicting the observed tracer test measurements was determined given the geophysically derived porosity structure. Both of these investigations showed that the SA-based approach, in general, allows much more reliable hydrological predictions than other more elementary techniques considered. Further, the developed calibration procedure was seen to be very effective, even at the scale of tomographic resolution, for predictions of transport. This also held true at locations within the aquifer where only geophysical data were available. This is significant because the acquisition of hydrological tracer test measurements is clearly more complicated and expensive than the acquisition of geophysical measurements. Although the above methodologies were tested using porosity logs and GPR data, the findings are expected to remain valid for a large number of pertinent combinations of geophysical and borehole log data of comparable resolution and sensitivity to the hydrological target parameter. Moreover, the obtained results allow us to have confidence for future developments in integration methodologies for geophysical and hydrological data to improve the 3-D estimation of hydrological properties.

Posterior auricular perichondrial cutaneous graft combined with cartilage strip in nostril reconstruction.

Objective: Reconstruction of alar structures of the nose remains difficult. The result has to be not only functional but also aesthetic. Different solutions to reconstruct alar defects are feasible. A good result that meets the specific demands on stability, aesthetics, and stable architecture without shrinkage of the area is not easily achieved. Method: A perichondrial cutaneous graft (PCCG), a graft consisting of a perichondral layer, fatty tissue, and skin that is harvested retroauriculary, is combined with an attached cartilage strip. Case Result: A 72-year-old patient suffering from basal cell carcinoma of the ala of the nose underwent the reconstructive procedure with a good result in 1 year in terms of stability, color match, and graft take. Conclusion: First, a strip of cartilage had been included in a PCCG where tumor resection required sacrifice of more than 50% of the alar rim. The case shows that one can consider a cartilage strip-enhanced PCCG graft to reconstruct alar defects.

Constraints on the permeability structure of alluvial aquifers from the poro-elastic inversion of multi-frequency P-wave velocity logs

We have explored the possibility of obtaining first-order permeability estimates for saturated alluvial sediments based on the poro-elastic interpretation of the P-wave velocity dispersion inferred from sonic logs. Modern sonic logging tools designed for environmental and engineering applications allow one for P-wave velocity measurements at multiple emitter frequencies over a bandwidth covering 5 to 10 octaves. Methodological considerations indicate that, for saturated unconsolidated sediments in the silt to sand range and typical emitter frequencies ranging from approximately 1 to 30 kHz, the observable velocity dispersion should be sufficiently pronounced to allow one for reliable first-order estimations of the permeability structure. The corresponding predictions have been tested on and verified for a borehole penetrating a typical surficial alluvial aquifer. In addition to multifrequency sonic logs, a comprehensive suite of nuclear and electrical logs, an S-wave log, a litholog, and a limited number laboratory measurements of the permeability from retrieved core material were also available. This complementary information was found to be essential for parameterizing the poro-elastic inversion procedure and for assessing the uncertainty and internal consistency of corresponding permeability estimates. Our results indicate that the thus obtained permeability estimates are largely consistent with those expected based on the corresponding granulometric characteristics, as well as with the available evidence form laboratory measurements. These findings are also consistent with evidence from ocean acoustics, which indicate that, over a frequency range of several orders-of-magnitude, the classical theory of poro-elasticity is generally capable of explaining the observed P-wave velocity dispersion in medium- to fine-grained seabed sediments

Casparian strip diffusion barrier in Arabidopsis is made of a lignin polymer without suberin.

Casparian strips are ring-like cell-wall modifications in the root endodermis of vascular plants. Their presence generates a paracellular barrier, analogous to animal tight junctions, that is thought to be crucial for selective nutrient uptake, exclusion of pathogens, and many other processes. Despite their importance, the chemical nature of Casparian strips has remained a matter of debate, confounding further molecular analysis. Suberin, lignin, lignin-like polymers, or both, have been claimed to make up Casparian strips. Here we show that, in Arabidopsis, suberin is produced much too late to take part in Casparian strip formation. In addition, we have generated plants devoid of any detectable suberin, which still establish functional Casparian strips. In contrast, manipulating lignin biosynthesis abrogates Casparian strip formation. Finally, monolignol feeding and lignin-specific chemical analysis indicates the presence of archetypal lignin in Casparian strips. Our findings establish the chemical nature of the primary root-diffusion barrier in Arabidopsis and enable a mechanistic dissection of the formation of Casparian strips, which are an independent way of generating tight junctions in eukaryotes.

Schwann cell strip for peripheral nerve repair.

Many strategies have been investigated to provide an ideal substitute to treat a nerve gap injury. Initially, silicone conduits were used and more recently conduits fabricated from natural materials such as poly-3-hydroxybutyrate (PHB) showed good results but still have their limitations. Surgically, a new concept optimising harvested autologous nerve graft has been introduced as the single fascicle method. It has been shown that a single fascicle repair of nerve grafting is successful. We investigated a new approach using a PHB strip seeded with Schwann cells to mimic a small nerve fascicle. Schwann cells were attached to the PHB strip using diluted fibrin glue and used to bridge a 10-mm sciatic nerve gap in rats. Comparison was made with a group using conventional PHB conduit tubes filled with Schwann cells and fibrin glue. After 2 weeks, the nerve samples were harvested and investigated for axonal and Schwann cell markers. PGP9.5 immunohistochemistry showed a superior nerve regeneration distance in the PHB strip group versus the PHB tube group (> 10 mm, crossed versus 3.17+/- 0.32 mm respectively, P<0.05) as well as superior Schwann cell intrusion (S100 staining) from proximal (> 10 mm, crossed versus 3.40+/- 0.36 mm, P<0.01) and distal (> 10 mm, crossed versus 2.91+/- 0.31 mm, P<0.001) ends. These findings suggest a significant advantage of a strip in rapidly connecting a nerve gap lesion and imply that single fascicle nerve grafting is advantageous for nerve repair in rats.

Simulated-annealing-based conditional simulation for the local-scale characterization of heterogeneous aquifers

Simulated-annealing-based conditional simulations provide a flexible means of quantitatively integrating diverse types of subsurface data. Although such techniques are being increasingly used in hydrocarbon reservoir characterization studies, their potential in environmental, engineering and hydrological investigations is still largely unexploited. Here, we introduce a novel simulated annealing (SA) algorithm geared towards the integration of high-resolution geophysical and hydrological data which, compared to more conventional approaches, provides significant advancements in the way that large-scale structural information in the geophysical data is accounted for. Model perturbations in the annealing procedure are made by drawing from a probability distribution for the target parameter conditioned to the geophysical data. This is the only place where geophysical information is utilized in our algorithm, which is in marked contrast to other approaches where model perturbations are made through the swapping of values in the simulation grid and agreement with soft data is enforced through a correlation coefficient constraint. Another major feature of our algorithm is the way in which available geostatistical information is utilized. Instead of constraining realizations to match a parametric target covariance model over a wide range of spatial lags, we constrain the realizations only at smaller lags where the available geophysical data cannot provide enough information. Thus we allow the larger-scale subsurface features resolved by the geophysical data to have much more due control on the output realizations. Further, since the only component of the SA objective function required in our approach is a covariance constraint at small lags, our method has improved convergence and computational efficiency over more traditional methods. Here, we present the results of applying our algorithm to the integration of porosity log and tomographic crosshole georadar data to generate stochastic realizations of the local-scale porosity structure. Our procedure is first tested on a synthetic data set, and then applied to data collected at the Boise Hydrogeophysical Research Site.

Identification of novel factors during the establishment of the Casparian strip in the endodermis

Multicellular organisms rely on specialized tissues that allow for the controlled exchange of matter with their surrounding. In order to function properly, these tissues need to establish a tight connection between the individual cells to prevent uncontrolled passive diffusion across the extracellular space. In animals, these connections are called tight and adherens junctions and are a critical feature of epithelia. These connections, however, rely on direct protein-protein interaction of plasma membrane proteins of adjacent cells. Such a mechanism is not possible in plants due to the cell wall, which encases the individual cells. In order to absorb nutrients, while simultaneously preventing uncontrolled diffusion between cells, land plants have evolved the root endodermis, which is functionally equivalent to animal epithelia. Its cells are surrounded by a precisely localized and aligned, ring-like lignin deposition, called the Casparian strip, and therefore tightly connected between each other. Very little was known about the development of the endodermis and the Casparian strip until recently. In the meantime, however, we have identified a family of endodermis- specific proteins, the CASPs, which recruits extracellular proteins the specific Casparian strip membrane domain (CSD) to locally synthesize lignin in the cell wall. Yet, we hardly knew any specifics on how the CSD is initially defined and how the critically important CASPs are being recruited to it. We therefore conducted a forward genetic screen on the localization of CASPI-GFP in order to identify novel mutants, which lack a defined CSD. We identified 48 mutants, which fell into 15 different complementation groups. While some of the isolated genes had previously been identified through different approaches, nine novel genes, which had never been implicated in CSD development and maintenance, were identified. One of them, LORD OF THE RINGS 2 (.LOTR2) is described to greater detail in this work. LOTR2 encodes for EX070A1, a protein of the evolutionary conserved exocyst complex. This complex has frequently been implicated in various secretory processes across kingdoms. In Arabidopsis, it transiently defines the positioning of CASPI-GFP. We have performed a detailed analysis of the dynamics of EX070A1 and CASPI-GFP, including studies with other markers and propose a mechanism, by which the cytosolic EX070A1 transiently defines a plasma membrane domain to recruit transmembrane proteins, which then recruit extracellular enzymes for localized cell wall modification. Considering the ubiquitous expression of EX070A1, we think that this mechanism is potentially of importance not only for the endodermis and the Casparian strip but also for many other tissues, in which the cell wall becomes locally modified. In fact, many other tissues with secondary cell wall modifications contain proteins very similar to the CASPs. It will be interesting to see to which degree this mechanism is employed in other tissues. As for the endodermis, we have now identified the first gene, which is not specific to the endodermis but shows endodermis-specific dynamics. This might give us a better insight on how the plant modulates this ubiquitously present factor in a cell- or tissue-type specific manner. Considering the knowledge, mutants and tools, which are available to us for investigating the endodermis, the Casparian strip, the exocyst complex and EX070A1 might be just the right experimental system to address these questions. -- Les organismes multicellulaires dépendent des tissues spécialisé pour l'échange contrôlé entre eux et leur environnement. Pour leur bon fonctionnement, les cellules de ces tissus ont besoin d'être très étroitement assemblés afin de prévenir la diffusion non-contrôlée à travers l'espace extracellulaire. Chez les animaux, ces connexions sont appelées jonctions serrées et jonctions adhérentes. Ces jonctions dépendent des interactions directes entre les protéines des cellules voisines. Ceci n'est pas possible chez les plantes à cause de la paroi cellulaire qui recouvre chaque cellule individuellement. Pour absorber les nutriments et en même temps empêcher la diffusion non-contrôlé entre cellules, les plantes ont évolué 1'endoderme dans la racine, qui est fonctionnellement équivalent aux épithéliums des animaux. Les cellules de l'endoderme sont ceinturées par une déposition de lignine très précisément localisées comme un anneau et alignées entre les cellules, et qui, donc, connecte étroitement les cellules avoisinante: Le cadre de Caspary. Peu était connu sur le développement de l'endoderme et le cadre de Caspaiy jusqu'à il y a quelques années. Récemment, pourtant, nous avons identifié une famille de protéines spécifiques à l'endoderme, les CASPs, qui définissent le domaine membranaire du cadre de Caspaiy (CSD). Les CASPs recrutent les protéines extracellulaires nécessaire à la synthèse du cadre de Caspary vers une région limité dans la paroi cellulaire. Pourtant, on connaît très peu les processus spécifiques concernant la définition initiale du CSD et comment les CASPs, qui ont une importance cruciale, sont recrutées vers ce domaine. Par conséquent nous avons mené un crible génétique sur la localisation du CASPI- GFP, qui sert comme marqueur pour le CSD. Notre but étant d'isoler de nouveaux mutants affectés dans l'établissement du CSD. Nous avons identifié 48 mutants, en 15 groupes de complémentation. Bien que certains des gènes isolés étaient déjà impliqué dans la formation du cadre de Caspary, neuf nouveaux gènes n'ayant jamais été impliqués dans le développement ou la maintenance du CSD ont pu être identifiés. Un de ces gènes, LORD OF THE RINGS2 (LOTR2) sera décrit plus en détail dans cette étude. LOTR2 code pour EX070A1, qui est une protéine, du complexe exocyste. Ce complexe de protéines a très bien été conservé au cours de l'évolution. Il était souvent impliqué dans plusieurs processus de sécrétion dans toutes les branches de la vie. Chez Arabidopsis, EX070A1 définit la position du CSD d'une façon transitoire et recrute CASP1- GFP. Nous avons mené une analyse détaillée des dynamiques d'EX070Al et CASPI-GFP ainsi que, des études avec des autres mutants. Nous proposons un mécanisme, d'après lequel EX070A1, recruté du cytosol, définit un domaine dans la membrane plasmique pour localiser des protéines transmembranaires, ces dernières ensuite recruteront des enzymes extracellulaires pour la modification locale de la paroi cellulaire. Vu qu'EX070A1 est exprimé dans toute dans la plante, nous pensons que ce mécanisme est potentiellement important non seulement pour l'endoderme et le cadre de Caspary, mais aussi pour les autres tissus où la paroi cellulaire doit être localement modifiée. En effet, plusieurs autres tissus contiennent des protéines très similaires aux CASPs. Il serait intéressant de voir à quelle dégrée ce mécanisme est également utilisé dans ces tissues. En ce qui concerne l'endoderme, nous avons maintenant identifié le premier gène qui n'est pas exprimé spécifiquement dans l'endoderme, mais qui montre tout de même une dynamique caractéristique dans ce tissu. Il serait intéressant de voir comment la plante peut moduler ce facteur omniprésent d'une façon spécifique. Vu les connaissances, les mutants et les outils qu'on a maintenant à notre disposition, l'endoderme et son cadre de Caspary, le complexe exocyste et EX070A1 sont probablement des bons systèmes expérimentaux pour étudier ces questions. -- Identification des nouveaux facteurs pendant l'établissement du cadre de Caspary dans l'endoderme. Lothar Kalmbach, Département de Biologie Moléculaire Végétale (DBMV), Université de Lausanne. Comme tous les autres organismes multicellulaires, les plantes terrestres dépendent de tissus spécialisés pour l'échange contrôlé avec leur environnement. Ces tissus sont importants pour l'absorption des nutriments mais également pour éviter l'influx de composés toxiques. Chez les plantes, ce tissu se trouve dans la racine. C'est l'endoderme. Grâce au cadre de Caspary, qui permet une forte connexion entre les cellules au niveau de leur paroi, l'endoderme empêche les éléments toxiques d'entrer dans le système vasculaire. Depuis quelques années, nous comprenons de plus en plus la nature et la biosynthèse, ainsi que les protéines impliquées dans l'ancrage des enzymes à la membrane plasmique. Nous n'avons eu, par contre, aucune idée sur le mécanisme qui d'abord définit cet endroit dans la membrane plasmique. Nous avons mené un crible génétique sur la localisation de CASPI-GFP, une protéine, qui recrute les enzymes extracellulaires pour la synthèse du cadre de Caspary. Nous avons identifié plusieurs nouveaux gènes qui sont impliqués dans l'intégrité du cadre de Caspary. L'un de ces gènes est EX070A1, qui est un facteur ayant un rôle important lors de la sécrétion des protéines dans tous les organismes eukaryotes. Ces mutants sont gravement affectés au niveau du cadre de Caspary, mais surtout ils ne sont plus capables de localiser CASPI-GFP. Nous avons suivi la dynamique d'EX070Al et de CASP1-GFP en combinaison avec d'autres marqueurs. Nous avons pu montrer que l'accumulation d'EX070Al est spécifique pour l'endoderme et essentielle pour bien localiser CASPI-GFP et donc, le cadre de Caspary. Ces résultats nous aident à mieux comprendre le développement de l'endoderme mais peuvent potentiellement aussi être utilisés pour étudier les modifications de la paroi cellulaire dans d'autres cellules de la plante.