Structures of ethylenediaminetetraacetato (3-) metal complexes. I complexes with Co, Mg and Cd metals

(I): Hexaaquacobalt(II) aqua[ethylenediaminetetraacetato(3-)]cobaltate(II) dihydrate, [Co(H2O)6][Co(C10H13N2O8)(H2O)]2.2H2O (Ibis): Hexaaquamagnesium(II) aqua[ethylenediaminetetraacetato(3-)]magnesiate(II) dihydrate, [Mg(H2O)6][Mg(C10H13N2O8)(H2O)]2.2H2O (II):Tetraaquabis{aqua[ethylenediaminetetraacetato(3-)]cadmium(II)-O-O'}Cadmium(II) tetrahydrate

Biochemical characterization of FANCD2 and FANCM in the Fanconi Anaemia pathway

Abstract : The maintenance of genome stability is a challenge for all living organisms. DNA is regularly subjected to chemical alterations by both endogenous and exogenous DNA damaging agents. If left unrepaired, these lesions will create mutations or lead to chromosomal instability. DNA crosslinking agents probably bring about the most toxic lesions. By linking covalently the two strands of DNA, crosslinking agents will impede essential cellular processes such as replication and transcription. Cells from Fanconi anaemia patients are extremely sensitive to these agents. Fanconi anaemia (FA) is a rare chromosomal instability disorder that leads to developmental defects, pancytopenia and cancer susceptibility. FA is a genetically heterogeneous disease with thirteen complementation groups identified. Proteins encoded by the FA genes work together in the FA pathway. Eight of these proteins form the FA core complex (FANC-A, B, C,E, F, G, L and -M), whose integrity is required to monoubiquitinate FANCD2 and FANCI in response to DNA damage. The hypersensitivity of FA cells to crosslinking agents, which perturb the progression of replication forks, has led to the hypothesis that FA proteins play a crucial role in the response to replication stress. However, at the molecular level, the functions of the FA pathway remain largely unknown. Our efforts were first focused on the characterization of FANCD2, "the key effector of the FA pathway". Using different substrates, we found that in vitro, purified hFANCD2 preferentially binds single strand DNA and double strand DNA extremities. Concomitantly, FANCM was identified as a new component of the FA core complex. Moreover FANCM was shown to have specific branch migration activities and probably a role as a "landing platform" on DNA for the other components of the core complex. By using FANCM mutants carrying deletions within the internal domain, we investigated the role of FANCM as a DNA anchor protein for the core complex. We observed that indeed, a specific part of the internal domain of FANCM interacts with components of the core complex. Finally, in collaboration with Weidong Wang's lab we characterized two new components of the FA pathway: FAAP10 and FAAP16. As a heterodimer these two proteins show affinity for dsDNA, and anneal complementary oligonucleotides in vitro. Moreover these proteins can associate with FANCM via a part of its internal domain. We find that FANCM, FAAP 10 and FAAP 16 can co-exist on the branch point of replication and recombination intermediates, and that FAAP10 and FAAP16 stimulate replication fork reversal by FANCM. These results suggest that FANCM may function as a landing platform for the core complex. After loading on DNA, the core complex can activate FANCD2 through monoubiquitination leading to its recruitment to the site of damage. Since ssDNA and double strand breaks are intermediates that are generated as a consequence of collapsed replication forks, FANCD2 by binding to ds DNA ends and ssDNA could protect such structures from the recombination repair machinery and prevent unscheduled recombination events. Alternatively, FANCD2 could avoid nucleases from gaining access to collapsed forks, preserving the DNA in state that can be used as a starting point for resumption of DNA synthesis. The overall comprehension of the FA pathway is far from been complete. Our results unravel new aspects of Fanconi Anaemia, which hopefully in the near future will address keys questions leading to a better understanding of the fascinating Fanconi Anaemia. Résumé : Le maintien de l'intégrité du génome est fondamentale chez tous les organismes vivants. L'ADN est constamment altéré par des composés aussi bien endogènes qu'exogènes. Si ces altérations ne sont pas réparées, elles peuvent conduire à l'apparition de mutations, ainsi qu'à une instabilité génomique accrue. Les lésions les plus sévères qui peuvent survenir sur l'ADN, sont les pontages inter caténaires. Des agents pontants en liant de façon covalente les deux brins d'ADN, vont empêcher le déroulement normal de processus cellulaires essentiels tels que la réplication ou la transcription. La compréhension des mécanismes permettant à la cellule de tolérer et réparer ces lésions est primordiale, notamment dans le cas des patients atteints de l'anémie de Fanconi qui présentent une très grande sensibilité à ces composés pontants. L'anémie de Fanconi est une maladie génétique rare appartenant à un groupe de pathologies associées à une grande instabilité chromosomique. Les patients atteints de l'anémie de Fanconi présentent des malformations du squelette, une pancytopénie et une forte propension à la survenue de cancer. L'anémie de Fanconi est génétiquement très hétérogène. À ce jour, 13 gènes codant pour 13 protéines FANC différentes ont été identifiés. Huit de ces protéines fonctionnent ensemble au sein d'un complexe (nommé le complexe FANC) ayant pour but de monoubiquitiner FANCD2 et FANCI en réponse à la formation de lésions sur l'ADN. L'extrême sensibilité des cellules de patients atteints de l'anémie de Fanconi à ces agents pontant l'ADN suggère l'implication des protéines FANC dans la réponse cellulaire suite à une stress réplicatif. Cependant, le rôle moléculaire exact de ces protéines demeure encore inconnu. Après purification, nous avons observé que FANCD2 était capable de lier l'ADN simple brin, ainsi que les extrémités d'ADN in vitro. Dans le même temps, FANCM fut identifié comme appartenant au complexe FANC. FANCM est décrit comme une translocase capable de promouvoir le déplacement de point de jonction dans des structures d'ADN spécifiques in vitro. De plus, en se liant à l'ADN, FANCM peut agir comme une plateforme pour les autres protéines FANC, leur permettant ainsi d'être adressées à l'ADN. En créant des protéines FANCM recombinantes ayant des délétions dans le domaine interne, nous avons pu observer que certaines protéines du complexe FANC se fixent à des sites spécifiques sur le domaine interne de FANCM. Enfin, au travers d'une collaboration, nous avons été amenés à caractériser deux nouvelles protéines appartenant au complexe FANC : FAAP 10 et FAAP16. Elles s'associent à FANCM par l'intermédiaire du domaine interne, et forment ainsi un hétérotrimére. La présence de FAAP10 et FAAP16 n'affecte pas la liaison de FANCM à l'ADN, mais semble potentialiser son activité de régression in vitro. FANCM semble donc fonctionner comme une plateforme pour les autres composants du complexe FANC. Ces derniers, une fois liés à l'ADN permettent la monoubiquitination de FANCD2 et son recrutement au site lésé de l'ADN. FANCD2 en se liant de façon préférentielle à l'ADN simple brin et aux extrémités d'ADN qui sont générés lors de l'arrêt et du démantèlement d'une fourche de réplication, pourrait protéger ces même fourches de réplication arrêtées, d'évènements de recombinaison aléatoires. Nos résultats apportent de nouveaux éléments concernant les mécanismes moléculaires de l'anémie de Fanconi. Enfin, l'étude de l'anémie de Fanconi permet aussi de mieux comprendre les mécanismes mis en place par la cellule pour tolérer des lésions survenant lors de la réplication.

Global DNA hypomethylation coupled to repressive chromatin domain formation and gene silencing in breast cancer.

While genetic mutation is a hallmark of cancer, many cancers also acquire epigenetic alterations during tumorigenesis including aberrant DNA hypermethylation of tumor suppressors, as well as changes in chromatin modifications as caused by genetic mutations of the chromatin-modifying machinery. However, the extent of epigenetic alterations in cancer cells has not been fully characterized. Here, we describe complete methylome maps at single nucleotide resolution of a low-passage breast cancer cell line and primary human mammary epithelial cells. We find widespread DNA hypomethylation in the cancer cell, primarily at partially methylated domains (PMDs) in normal breast cells. Unexpectedly, genes within these regions are largely silenced in cancer cells. The loss of DNA methylation in these regions is accompanied by formation of repressive chromatin, with a significant fraction displaying allelic DNA methylation where one allele is DNA methylated while the other allele is occupied by histone modifications H3K9me3 or H3K27me3. Our results show a mutually exclusive relationship between DNA methylation and H3K9me3 or H3K27me3. These results suggest that global DNA hypomethylation in breast cancer is tightly linked to the formation of repressive chromatin domains and gene silencing, thus identifying a potential epigenetic pathway for gene regulation in cancer cells.

Loss of Prestress, Camber, and Deflection of Non-Composite and Composite Structures Using Different Weight Concretes, HR-137, 1970

General equations are presented for predicting loss of prestress and camber of both composite and non- composite prestressed concrete structures. Continuous time functins of all parameters needed to solve the equations are given, and sample results included. Computed prestress loss and camber are compared with experimental data for normal weight and lightweight concrete. Methods are also presented for predicting the effect of non-prestressed tension steel in reducing time-dependent loss of prestress and camber, and for the determination of short-time deflections of uncracked and cracked prestressed members. Comparisons with experimental results are indicated for these partially prestressed methods.

Face Short-Term Memory-Related Electroencephalographic Patterns can Differentiate Multi- versus Single-Domain Amnestic Mild Cognitive Impairment.

Amnestic mild cognitive impairment (aMCI) is characterized by memory deficits alone (single-domain, sd-aMCI) or associated with other cognitive disabilities (multi-domain, md-aMCI). The present study assessed the patterns of electroencephalographic (EEG) activity during the encoding and retrieval phases of short-term memory in these two aMCI subtypes, to identify potential functional differences according to the neuropsychological profile. Continuous EEG was recorded in 43 aMCI patients, whose 16 sd-aMCI and 27 md-aMCI, and 36 age-matched controls (EC) during delayed match-to-sample tasks for face and letter stimuli. At encoding, attended stimuli elicited parietal alpha (8-12 Hz) power decrease (desynchronization), whereas distracting stimuli were associated with alpha power increase (synchronization) over right central sites. No difference was observed in parietal alpha desynchronization among the three groups. For attended faces, the alpha synchronization underlying suppression of distracting letters was reduced in both aMCI subgroups, but more severely in md-aMCI cases that differed significantly from EC. At retrieval, the early N250r recognition effect was significantly reduced for faces in md-aMCI as compared to both sd-aMCI and EC. The results suggest a differential alteration of working memory cerebral processes for faces in the two aMCI subtypes, face covert recognition processes being specifically altered in md-aMCI.

The histone-interacting domain of nuclear factor I activates simian virus 40 DNA replication in vivo.

Efficient initiation of SV40 DNA replication requires transcription factors that bind auxiliary sequences flanking the minimally required origin. To evaluate the possibility that transcription factors may activate SV40 replication by acting on the chromatin structure of the origin, we used an in vivo replication system in which we targeted GAL4 fusion proteins to the minimally required origin. We found that the proline-rich transcriptional activation domain of nuclear factor I (NF-I), which has been previously shown to interact with histone H3, specifically activates replication. Evaluation of a series of deletion and point mutants of NF-I indicates that the H3-binding domain and the replication activity coincide perfectly. Assays with other transcription factors, such as Sp1, confirmed the correlation between the interaction with H3 and the activation of replication. These findings imply that transcription factors such as NF-I can activate SV40 replication via direct interaction with chromatin components, thereby contributing to the relief of nucleosomal repression at the SV40 origin.

L'exploitation des ressources végétales dans les Pyrénées orientales durant l'holocène: analyse anthracologique des structures d'élevage, de four et de charbonnières dans l'Alt Urgell (Chaîne du Cadí) et la Vallée du Madriu (Andorre)

Dans ce travail, nous présentons le résultat des recherches anthracologiques réalisées sur des sites archéologiques de haute montagne dans les Pyrénées orientales. Cette recherche s’insère dans un projet d’archéologie du paysage. Les zones d’étude se situent dans les Pré-Pyrénées sur le versant méridional de la chaîne du Cadí (vallée de la Vansa, Alt Urgell), et dans la vallée du Madriu, située dans les Pyrénées axiales, en Andorre. Le but principal de l’analyse anthracologique a été de connaître et comprendre la dynamique et la relation qui unissent les populations qui ont occupé ces vallées avec le milieu forestier de haute montagne. Les échantillons ont été récupérés sur des structures archéologiques associés à l’exploitation forestière (charbonnières, fours pour la fabrication de résine), au pastoralisme (cabanes et enclos) et à l’exploitation minière-métallurgique (four de grillage), avec une chronologie qui débute au Néolithique Ancien et finit à l’époque moderne et contemporaine (XVIII-XIXe siècles). Les résultats indiquent une variabilité taxonomique pauvre avec la présence majoritaire du Pinus et la présence ponctuelle d’autres espèces arbustives (Ericaceae et Juniperus) et arborées, comme Betula alba ou Abies alba. Différentes formations végétales de haute montagne ont été identifiées, selon leur localisation en versant ensoleillé ou ombragé, ainsi que leur altitude. Les résultats montrent des traces d’exploitation forestière dès le Néolithique Ancien, une intensification des activités à l’Antiquité, même si l’impact anthropique majeur correspond à l’activité de charbonnage d’époque moderne.

The Dutung-Thaktote extensional fault zone and nappe structures documented by illite crystallinity and clay-mineral paragenesis in the Tethys Himalaya between Spiti river and Tso Morari, NW India

Numerous measurements by XRD of the Scherrer width at half-peak height (001 reflection of illite), coupled with analyses of clay-size assemblages, provide evidence for strong variations in the conditions of low temperature metamorphism in the Tethyan Himalaya metasediments between the Spiti river and the Tso Morari. Three sectors can be distinguished along the Spiti river-Tso Morari transect. In the SW, the Takling and Parang La area is characterised by a metamorphism around anchizone-epizone boundary conditions. Further north, in the Dutung area, the metamorphic grade abruptly decreases to weak diagenesis, with the presence of mixed-layered clay phases. At the end of the profile towards the NE, a progressive metamorphic increase up to greenschist facies is recorded, marked by the appearance of biotite and chloritoid. The combination of these data with the structural. observations permits to propose that a nappe stack has been crosscut by the younger Dutung-Thaktote extensional fault zone (DTFZ). The change in metamorphism across this zone helps to assess the displacements which occurred during synorogenic extension. In the SW and NE parts of the studied transect, a burial of 12 km has been estimated, assuming a geothermal gradient of 25 degrees C/km. In the SW part, this burial is due to the juxtaposition of the Shikar Beh and Mata nappes and in the NE part, solely to burial beneath the Mata nappe. In the central part of the profile, the effect of the DTFZ is to bring down diagenetic sediments in-between the two aforesaid metamorphic zones. The offset along the Dutung-Thaktote normal faults is estimated at 16 km.

Structural, metamorphic and geochronological relations between the Zanskar Shear Zone and the Miyar Shear Zone (NW Indian Himalaya): Evidence for two distinct tectonic structures and implications for the evolution of the High Himalayan Crystalline of Zanskar

The geologic structures and metamorphic zonation of the northwestern Indian Himalaya contrast significantly with those in the central and eastern parts of the range, where the high-grade metamorphic rocks of the High Himalayan Crystalline (HHC) thrust southward over the weakly metamorphosed sediments of the Lesser Himalaya along the Main Central Thrust (MCT). Indeed, the hanging wall of the MCT in the NW Himalaya mainly consists of the greenschist facies metasediments of the Chamba zone, whereas HHC high-grade rocks are exposed more internally in the range as a large-scale dome called the Gianbul dome. This Gianbul dome is bounded by two oppositely directed shear zones, the NE-dipping Zanskar Shear Zone (ZSZ) on the northern flank and the SW-dipping Miyar Shear Zone (MSZ) on the southern limb. Current models for the emplacement of the HHC in NW India as a dome structure differ mainly in terms of the roles played by both the ZSZ and the MSZ during the tectonothermal evolution of the HHC. In both the channel flow model and wedge extrusion model, the ZSZ acts as a backstop normal fault along which the high-grade metamorphic rocks of the HHC of Zanskar are exhumed. In contrast, the recently proposed tectonic wedging model argues that the ZSZ and the MSZ correspond to one single detachment system that operates as a subhorizontal backthrust off of the MCT. Thus, the kinematic evolution of the two shear zones, the ZSZ and the MSZ, and their structural, metamorphic and chronological relations appear to be diagnostic features for discriminating the different models. In this paper, structural, metamorphic and geochronological data demonstrate that the MSZ and the ZSZ experienced two distinct kinematic evolutions. As such, the data presented in this paper rule out the hypothesis that the MSZ and the ZSZ constitute one single detachment system, as postulated by the tectonic wedging model. Structural, metamorphic and geochronological data are used to present an alternative tectonic model for the large-scale doming in the NW Indian Himalaya involving early NE-directed tectonics, weakness in the upper crust, reduced erosion at the orogenic front and rapid exhumation along both the ZSZ and the MSZ.

Rift-related inheritance in orogens: a case study from the Austroalpine nappes in Central Alps (SE-Switzerland and N-Italy)

The Austroalpine nappe systems in SE-Switzerland and N-Italy preserve remnants of the Adriatic rifted margin. Based on new maps and cross-sections, we suggest that the complex structure of the Campo, Grosina/Languard, and Bernina nappes is inherited largely from Jurassic rifting. We propose a classification of the Austroalpine domain into Upper, Middle and Lower Austroalpine nappes that is new because it is based primarily on the rift-related Jurassic structure and paleogeography of these nappes. Based on the Alpine structures and pre-Alpine, rift-related geometry of the Lower (Bernina) and Middle (Campo, Grosina/Languard) Austroalpine nappes, we restore these nappes to their original positions along the former margin, as a means of understanding the formation and emplacement of the nappes during initial reactivation of the Alpine Tethyan margin. The Campo and Grosina/Languard nappes can be interpreted as remnants of a former necking zone that comprised pre-rift upper and middle crust. These nappes were juxtaposed with the Mesozoic cover of the Bernina nappe during Jurassic rifting. We find evidence for low-angle detachment faults and extensional allochthons in the Bernina nappe similar to those previously described in the Err nappe and explain their role during subsequent reactivation. Our observations reveal a strong control of rift-related structures during the subsequent Alpine reactivation on all scales of the former distal margin. Two zones of intense deformation, referred to as the Albula-Zebru and Lunghin-Mortirolo movement zones, have been reactivated during Alpine deformation and cannot be described as simple monophase faults or shear zones. We propose a tectonic model for the Austroalpine nappe systems that link inherited, rift-related structures with present-day Alpine structures. In conclusion, we believe that apart from the direct regional implications, the results of this paper are of general interest in understanding the control of rift structures during reactivation of distal-rifted margins.

Profile Following for Inspection of Underwater Structures

We present a seabed profile estimation and following method for close proximity inspection of 3D underwater structures using autonomous underwater vehicles (AUVs). The presented method is used to determine a path allowing the AUV to pass its sensors over all points of the target structure, which is known as coverage path planning. Our profile following method goes beyond traditional seabed following at a safe altitude and exploits hovering capabilities of recent AUV developments. A range sonar is used to incrementally construct a local probabilistic map representation of the environment and estimates of the local profile are obtained via linear regression. Two behavior-based controllers use these estimates to perform horizontal and vertical profile following. We build upon these tools to address coverage path planning for 3D underwater structures using a (potentially inaccurate) prior map and following cross-section profiles of the target structure. The feasibility of the proposed method is demonstrated using the GIRONA 500 AUV both in simulation using synthetic and real-world bathymetric data and in pool trials