Effect of deletion of 5'HS3 or 5'HS2 of the human beta-globin locus control region on the developmental regulation of globin gene expression in beta-globin locus yeast artificial chromosome transgenic mice.

To analyze the function of the 5' DNase I hypersensitive sites (HSs) of the locus control region (LCR) on beta-like globin gene expression, a 2.3-kb deletion of 5'HS3 or a 1.9-kb deletion of 5'HS2 was recombined into a beta-globin locus yeast artificial chromosome, and transgenic mice were produced. Deletion of 5'HS3 resulted in a significant decrease of epsilon-globin gene expression and an increase of gamma-globin gene expression in embryonic cells. Deletion of 5'HS2 resulted in only a small decrease in expression of epsilon-, gamma-, and beta-globin mRNA at all stages of development. Neither deletion affected the temporal pattern of globin gene switching. These results suggest that the LCR contains functionally redundant elements and that LCR complex formation does not require the presence of all DNase I hypersensitive sites. The phenotype of the 5'HS3 deletion suggests that individual HSs may influence the interaction of the LCR with specific globin gene promoters during the course of ontogeny.

Étude de la collaboration entre les facteurs de transcription hématopoïétiques lors du développement et de la différenciation des cellules érythroïdes

La régulation transcriptionnelle des gènes est cruciale pour permettre le bon fonctionnement des cellules. Afin que les cellules puissent accomplir leurs fonctions, les gènes doivent être exprimés adéquatement dans le bon type cellulaire et au stade de développement et de différenciation approprié. Un dérèglement dans l’expression de un ou plusieurs gènes peut entraîner de graves conséquences sur le destin de la cellule. Divers éléments en cis (ex : promoteurs et enhancers) et en trans (machinerie transcriptionnelle et facteurs de transcription) sont impliqués dans la régulation de la transcription. Les gènes du locus humain beta-globine (hub) sont exprimés dans les cellules érythroïdes et sont finenement régulés lors du développement et de la différenciation. Des mutations dans différentes régions du locus causent entre autres les beta-thalassémies. Nous avons utilisé ce modèle bien caractérisé afin d’étudier différents mécanismes de régulation favorisés par les facteurs de transcription qui sont exprimés dans les cellules érythroïdes. Nous nous sommes intéressés à l’importance de l’élément en cis HS2 du Locus control region. Cet élément possède plusieurs sites de liaison pour des facteurs de transcription impliqués dans la régulation des gènes du locus hub. Nos résultats montrent que HS2 possède un rôle dans l’organisation de la chromatine du locus qui peut être dissocié de son rôle d’enhancer. De plus, HS2 n’est pas essentiel pour l’expression à haut niveau du gène beta alors qu’il est important pour l’expression des gènes gamma. Ceci suggère que le recrutement des différents facteurs au site HS2 lors du développement influence différement les gènes du locus. Dans un deuxième temps, nous avons investigué l’importance de HS2 lors de la différenciation des cellules érythroïdes. Il avait été rapporté que l’absence de HS2 influence grandement la potentialisation de la chromatine du gène beta. La potentialisation dans les cellules progénitrices favorise l’activation transcriptionnelle du gène dans les cellules matures. Nous avons caractérisé le recrutement de différents facteurs de transcription au site HS2 et au promoteur beta dans les cellules progénitrices hématopoïétiques (CPH) ainsi que dans les cellules érythroïdes matures. Nos résultats montrent que le facteur EKLF est impliqué dans la potentialisation de la chromatine et favorise le recrutement des facteurs BRG1, p45 et CBP dans les CPH. L’expression de GATA-1 dans les cellules érythroïdes matures permet le recrutement de GATA-1 au locus hub dans ces cellules. Ces données suggèrent que la combinaison de EKLF et GATA-1 est requise pour permettre une activation maximale du gène beta dans les cellules érythroïdes matures. Un autre facteur impliqué dans la régulation du locus hub est Ikaros. Nous avons étudié son recrutement au locus hub et avons observé que Ikaros est impliqué dans la répression des gènes gamma. Nos résultats montrent aussi que GATA-1 est impliqué dans la répression de ces gènes et qu’il interagit avec Ikaros. Ensemble, Ikaros et GATA-1 favorisent la formation d’un complexe de répression aux promoteurs gamma. Cette étude nous a aussi permis d’observer que Ikaros et GATA-1 sont impliqués dans la répression du gène Gata2. De façon intéressante, nous avons caractérisé le mécanisme de répression du gène Hes1 (un gène cible de la voie Notch) lors de la différenciation érythroïde. Similairement à ce qui a été observé pour les gènes gamma, Hes1 est aussi réprimé par Ikaros et GATA-1. Ces résultats suggèrent donc que la combinaison de Ikaros et GATA-1 est associée à la répression de plusieurs de gènes dans les cellules érythroïdes. Globalement cette thèse rapporte de nouveaux mécanismes d’action de différents facteurs de transcription dans les cellules érythroïdes. Particulièrement, nos travaux ont permis de proposer un modèle pour la régulation des gènes du locus hub lors du développement et de la différenciation. De plus, nous rapportons pour la première fois l’importance de la collaboration entre les facteurs Ikaros et GATA-1 dans la régulation transcriptionnelle de gènes dans les cellules érythroïdes. Des mutations associées à certains des facteurs étudiés ont été rapportées dans des cas de beta-thalassémies ainsi que de leucémies. Nos travaux serviront donc à avoir une meilleure compréhension des mécanismes d’action de ces facteurs afin de potentiellement pouvoir les utiliser comme cibles thérapeutiques.

Incorporation of a sodium ion guest in the host of copper(II)-Schiff-base complexes: Structural characterization and magnetic study

Three copper(II) complexes, [CuL1], [CuL2] and [CuL3] where L-1, L-2 and L-3 are the tetradentate di-Schiff-base ligands prepared by the condensation of acetylacetone and appropriate diamines (e.g. 1,2-diaminoethane, 1,2-diaminopropane and 1,3-diaminopropane, respectively) in 2:1 ratios, have been prepared. These complexes act as host molecules and include a guest sodium ion by coordinating through the oxygen atoms to result in corresponding new trinuclear complexes, [(CuL1)(2)Na(ClO4)(H2O)][CuL1], [(CuL2)(2)Na(ClO4)(H2O)] (2) and [(CuL3)(2)Na(ClO4)(H2O)] (3) when crystallized from methanol solution containing sodium perchlorate. All three complexes have been characterized by single crystal X-ray crystallography. In all the complexes, the sodium cation has a six-coordinate distorted octahedral environment being bonded to four oxygen atoms from two Schiff-base complexes of Cu(II) in addition to a perchlorate anion and a water molecule. The copper atoms are four coordinate in a square planar environment being bonded to two oxygen atoms and two nitrogen atoms of the Schiff-base ligand. The variable temperature susceptibilities for complexes 1-3 were measured over the range 2-300 K. The isotropic Hamiltonian, H = g(1)beta HS1 + g(2)beta HS2 + J(12)S(1)S(2) + g(3)beta HS3 for complex 1 and H = g(1)beta HS1 + g2 beta HS2 +J(12)S(1)S(2) for complexes 2 and 3 has been used to interpret the magnetic data. The best fit parameters obtained are: g(1) = g(2) = 2.07(0), J = - 1.09(1) cm(-1) for complex 1, g(1) = g(2) = 2.06(0), J = -0.55(1) cm(-1) for complex 2 and g1 = g2 = 2.07(0).J = -0.80(1) cm(-1) for 3. Electrochemical studies displayed an irreversible Cu(II)/Cu(I) one-electron reduction process. (C) 2008 Elsevier Ltd. All rights reserved.

Magnetic properties of two cores from the Iberian Margin

Magnetic properties of late Quaternary sediments on the SW Iberian Margin are dominated by bacterial magnetite, observed by transmission electron microscopy (TEM), with contributions from detrital titanomagnetite and hematite. Reactive hematite from eolian dust, together with low organic matter concentrations and the lack of sulfate reduction, lead to dissimilatory iron reduction and availability of Fe(II) for abundant magnetotactic bacteria. Magnetite grain-size proxies (kARM/k and ARM/IRM) and S-ratios (sensitive to hematite) vary on stadial/interstadial timescales, contain orbital power, and mimic planktic d18O. The detrital/biogenic magnetite ratio and hematite concentration are greater during stadials and glacial isotopic stages, reflecting increased detrital (magnetite) input during times of lowered sea level, coinciding with atmospheric conditions favoring hematitic dust supply. Magnetic susceptibility, on the other hand, has a very different response being sensitive to coarse detrital multidomain (MD) magnetite associated with ice-rafted debris (IRD). High susceptibility and/or magnetic grain size coarsening, mark Heinrich stadials (HS), particularly HS2, HS3, HS4, HS5, HS6 and HS7, as well as older Heinrich-like detrital layers, indicating the sensitivity of this region to fluctuations in the position of the polar front. Relative paleointensity (RPI) records have well-constrained age models based on planktic d18O correlation to ice-core chronologies, however, they differ from reference records (e.g. PISO) particularly in the vicinity of glacial maxima, mainly due to inefficient normalization of RPI records in intervals of enhanced detrital/eolian hematite input.

Generation of a high-titer retroviral vector capable of expressing high levels of the human beta-globin gene.

Retrovirus-mediated gene transfer into hematopoietic cells may provide a means of treating both inherited and acquired diseases involving hematopoietic cells. Implementation of this approach for disorders resulting from mutations affecting the beta-globin gene (e.g., beta-thalassemia and sickle cell anemia), however, has been hampered by the inability to generate recombinant viruses able to efficiently and faithfully transmit the necessary sequences for appropriate gene expression. We have addressed this problem by carefully examining the interactions between retroviral and beta-globin gene sequences which affect vector transmission, stability, and expression. First, we examined the transmission properties of a large number of different recombinant proviral genomes which vary both in the precise nature of vector, beta-globin structural gene, and locus control region (LCR) core sequences incorporated and in the placement and orientation of those sequences. Through this analysis, we identified one specific vector, termed M beta 6L, which carries both the human beta-globin gene and core elements HS2, HS3, and HS4 from the LCR and faithfully transmits recombinant proviral sequences to cells with titers greater than 10(6) per ml. Populations of murine erythroleukemia (MEL) cells transduced by this virus expressed levels of human beta-globin transcript which, on a per gene copy basis, were 78% of the levels detected in an MEL-derived cell line, Hu11, which carries human chromosome 11, the site of the beta-globin locus. Analysis of individual transduced MEL cell clones, however, indicated that, while expression was detected in every clone tested (n = 17), the levels of human beta-globin treatment varied between 4% and 146% of the levels in Hu11. This clonal variation in expression levels suggests that small beta-globin LCR sequences may not provide for as strict chromosomal position-independent expression of beta-globin as previously suspected, at least in the context of retrovirus-mediated gene transfer.

Factors important to the secretion and matrix deposition of tissue transglutaminase

Data suggest that for TG2 to be secreted, an intact N-terminal FN binding site (for which TG2 has high affinity) is required, however interaction of TG2 with its high affinity binding partners presents both in the intracellular and extracellular space as well as with specific cell surface receptors may also be involved in this process. Using a site-directed mutagenesis approach, the effects of specific mutations of TG2 on its translocation to the cell surface and secretion into the ECM have been investigated. Mutations include those affecting FN binding (FN1), HSPGs binding (HS1, HS2) GTP/GDP binding site (GTP1, 2) as well as N-terminal and C-terminal domains (TG2 deletion mutants N, and C). By performing transglutaminase activity assays, cell surface protein biotinylation and verifying distribution of TG2 mutants in the ECM we demonstrated that one of the potential heparan sulfate binding site mutants (HS2 mutant) is secreted at the cell surface in a much reduced manner and is less deposited into the ECM than the HS1 mutant. The HS2 mutant showed a low affinity for binding to a heparin sepharose column demonstrating this mutation site may be a potential heparan binding site of TG2. Analogous peptides to this site were shown to have some efficiency in the inhibition of the binding of the FN-TG2 complex to cell surface heparan sulfates in a cell adhesion assay indicating the peptide to be representative of the novel heparin binding site within TG2. The GTP binding site mutants GTP1 and GTP2 exhibited low specific activity however, GTP2 showed more secretion to the cell surface in comparison to GTP1. The FN1 binding mutant did not greatly affect TG2 activity nor did it alter TG2 secretion at the cell surface and deposition into the ECM indicating that fibronectin binding at this site on the enzyme is not an important factor. Interestingly an intact N-terminus (?1-15) appeared to be essential for enzyme externalisation. Removal of the first 15 amino acids (N-terminal mutant) abolished TG2 secretion to the cell surface as well as deposition into the ECM. In addition it reduced the enzymes affinity for binding to heparin. In contrast, deletion of the C-terminal TG2 domain (?594-687) increased enzyme secretion to the cell surface. Consistent with the data presented in this thesis we speculate that TG2 must fulfill two requirements to be successfully secreted from cells. The findings indicate that the closed conformation of the enzyme as well as intact N-terminal tail and a novel HS binding site within the TG2 molecule are key elements for the enzyme’s localisation at the cell surface and its deposition into the extracellular matrix. The importance of understanding the interactions between TG2, heparan sulfates and other TG2 binding partners at the cell surface could have an impact on the design of novel strategies for enzyme inhibition which could be important in the control of extracellular TG2 related diseases.

Régulation épigénétique au locus humain de la [bêta]-globine lors de la différenciation de cellules ES

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Régulation épigénétique au locus humain de la [bêta]-globine lors de la différenciation de cellules ES

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Grain-size, lithic grains, foraminifera-derived and dinocyst-derived data of sediment core MD99-2281

The last glacial period was punctuated by abrupt climatic events with extrema known as Heinrich and Dansgaard-Oeschger events. These millennial events have been the subject of many paleoreconstructions and model experiments in the past decades, but yet the hydrological processes involved remain elusive. In the present work, high-resolution analyses were conducted on the 12-42 ka BP section of core MD99-2281 retrieved southwest of the Faeroe Islands, and combined with analyses conducted in two previous studies (Zumaque et al., 2012; Caulle et al., 2013). Such a multiproxy approach, coupling micropaleontological, geochemical and sedimentological analyses, allows us to track surface, subsurface, and deep hydrological processes occurring during these rapid climatic changes. Records indicate that the coldest episodes of the studied period (Greenland stadials and Heinrich stadials) were characterized by a strong stratification of surface waters. This surface stratification seems to have played a key role in the dynamics of subsurface and deep-water masses. Indeed, periods of high surface stratification are marked by a coupling of subsurface and deep circulations which sharply weaken at the beginning of stadials, while surface conditions progressively deteriorate throughout these cold episodes; conversely, periods of decreasing surface stratification (Greenland interstadials) are characterized by a coupling of surface and deep hydrological processes, with progressively milder surface conditions and gradual intensification of the deep circulation, while the vigor of the subsurface northward Atlantic flow remains constantly high. Our results also reveal different and atypical hydrological signatures during Heinrich stadials (HSs): while HS1 and HS4 exhibit a "usual" scheme with reduced overturning circulation, a relatively active North Atlantic circulation seems to have prevailed during HS2, and HS3 seems to have experienced a re-intensification of this circulation during the middle of the event. Our findings thus bring valuable information to better understand hydrological processes occurring in a key area during the abrupt climatic shifts of the last glacial period.

Millennial-scale fluctuations of the European Ice Sheet at the end of the last glacial, and their potential impact on global climate

Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing to the ocean is important to better understand the mechanisms behind abrupt climate changes. To date, research efforts have mainly focused on the North American (Laurentide) ice-sheets (LIS), leaving the potential role of the European Ice Sheet (EIS), and of the Scandinavian ice-sheet (SIS) in particular, largely unexplored. Using neodymium isotopes in detrital sediments deposited off the Channel River, we provide a continuous and well-dated record for the evolution of the EIS southern margin through the end of the last glacial period and during the deglaciation. Our results reveal that the evolution of EIS margins was accompanied with substantial ice recession (especially of the SIS) and simultaneous release of meltwater to the North Atlantic. These events occurred both in the course of the EIS to its LGM position (i.e., during Heinrich Stadial –HS– 3 and HS2; ∼31–29 ka and ∼26–23 ka, respectively) and during the deglaciation (i.e., at ∼22 ka, ∼20–19 ka and from 18.2 ± 0.2 to 16.7 ± 0.2 ka that corresponds to the first part of HS1). The deglaciation was discontinuous in character, and similar in timing to that of the southern LIS margin, with moderate ice-sheet retreat (from 22.5 ± 0.2 ka in the Baltic lowlands) as soon as the northern summer insolation increase (from ∼23 ka) and an acceleration of the margin retreat thereafter (from ∼20 ka). Importantly, our results show that EIS retreat events and release of meltwater to the North Atlantic during the deglaciation coincide with AMOC destabilisation and interhemispheric climate changes. They thus suggest that the EIS, together with the LIS, could have played a critical role in the climatic reorganization that accompanied the last deglaciation. Finally, our data suggest that meltwater discharges to the North Atlantic produced by large-scale recession of continental parts of Northern Hemisphere ice sheets during HS, could have been a possible source for the oceanic perturbations (i.e., AMOC shutdown) responsible for the marine-based ice stream purge cycle, or so-called HE's, that punctuate the last glacial period.