CTCF-T, a paralogue of CTCF, directs sequence specific DNA methylation of the imprinting control region of Igf2/H19

SUMMARY Genomic imprinting is an epigenetic mechanism of transcriptional regulation that ensures restriction of expression of a subset of mammalian genes to a single parental allele. The best studied example of imprinted gene regulation is the Igf2/H19 locus, which is also the most commonly altered by loss of imprinting (LOT) in cancer. LOT is associated with numerous hereditary diseases and several childhood, and adult cancers. Differential expression of reciprocal H19 and 1gf2 alleles in somatic cells depends on the methylation status of the imprinting control region (ICR) which regulates binding of CTCF, an ubiquitously expressed 11-zinc finger protein that binds specifically to non-methylated maternal ICR and thereby attenuates expression of Igf2, while it does not bind to methylated paternal ICR, which enables Igf2 expression. Initial ICR methylation occurs during gametogenesis by an as yet unknown mechanism. The accepted hypothesis is that the event of differential maternal and paternal DNA methylation depends on germ-line specific proteins. Our Laboratory identified a novel 11-zinc-finger protein CTCF-T (also known as CTCFL and BORIS) that is uniquely expressed in the male germ-line and is highly homologous within its zinc-finger region with CTCF. The amino-acid sequences flanking the zinc-finger regions of CTCF and CTCF-T have widely diverged, suggesting that though they could bind to the same DNA targets (ICRs) they are likely to have different functions. Interestingly, expression of CTCF-T and CTCF is mutually exclusive; CTCF-T-positive (CTCF-negative) cells occur in the stage of spermatogenesis that coincides with epigenetic reprogramming, including de novo DNA methylation. In our study we demonstrate the role that CTCF-T plays in genomic imprinting. Here we show that CTCF-T binds in vivo to the ICRs of Igf2/H19 and Dlk/Gt12 imprinted genes. In addition, we identified two novel proteins interacting with CTCF-T: a protein arginine methyltransferase PRMT7 and an arginine-rich histone H2A variant that we named trH2A. These interactions were confirmed and show that the two proteins interact with the amino-teiminal region of CTCF-T. Additionally, we show interaction of the amino- terminal region of CTCF-T with histones H1, H2A and H3. These results suggest that CTCF-T is a sequence-specific DNA (ICR) binding protein that associates with histones and recruits PRMT7. Interestingly, PRMT7 has a histone-methyltransferase activity. It has been shown that histone methylation can mark chromatin regions thereby directing DNA-methylation; thus, our hypothesis is that the CTCF-T protein-scaffold directs PRMT7 to methylate histone(s) assembled on ICRs, which marks chromatin for the recruitment of the de novo DNA methyltransferases to methylate DNA. To test this hypothesis, we developed an in vivo DNA-methylation assay using Xenopus laevis' oocytes, where H19 ICR and different expression cDNAs, including CTCF-T, PRMT7 and the de novo DNA methyltransferases (Dnmt3a, Dnmt3b and Dnmt3L) are microinjected into the nucleus. The methylation status of CpGs within the H19 ICR was analysed 48 or 72 hours after injection. Here we demonstrate that CpGs in the ICR are methylated in the presence of both CTCF-T and PRMT7, while control oocytes injected only with ICR did not show any methylation. Additionally, we showed for the first time that Dnmt3L is crucial for the establishment of the imprinting marks on H19 ICR. Moreover, we confirmed that Dnmt3a and Dnmt3b activities are complementary. Our data indicate that all three Dnmt3s are important for efficient de novo DNA methylation. In conclusion, we propose a mechanism for the establishment of de novo imprinting marks during spermatogenesis: the CTCF-T/PRMT7 protein complex directs histone methylation leading to sequence-specific de novo DNA methylation of H19 ICR. RESUME L'empreinte génomique parentale est un mécanisme épigénétique de régulation transcriptionelle qui se traduit par une expression différentielle des deux allèles de certains gènes, en fonction de leur origine parentale. L'exemple le mieux caractérisé de gènes soumis à l'empreinte génomique parentale est le locus Igf2/H19, qui est aussi le plus fréquemment altéré par relaxation d'empreinte (en anglais: loss of imprinting, LOI) dans les cancers. Cette relaxation d'empreinte est aussi associée à de nombreuses maladies héréditaires, ainsi qu'à de nombreux cancers chez l'enfant et l'adulte. Dans les cellules somatiques, les différences d'expression des allèles réciproques H19 et Ig12 est sous le contrôle d'une région ICR (Imprinting Control Region). La méthylation de cette région ICR régule l'ancrage de la protéine à douze doigts de zinc CTCF, qui se lie spécifiquement à l'ICR maternel non-méthylé, atténuant ainsi l'expression de Igf2, alors qu'elle ne s'ancre pas à l'ICR paternel méthyle. Le mécanisme qui accompagne la méthylation initiale de la région ICR durant la gamétogenèse n'a toujours pas été élucidé. L'hypothèse actuelle propose que la différence de méthylation entre l'ADN maternel et paternel résulte de l'expression de protéines propres aux zones germinales. Notre laboratoire a récemment identifié une nouvelle protéine à douze doigts de zinc, CTCF-T (aussi dénommée CTCFL et BORRIS), qui est exprimée uniquement dans les cellules germinales mâles, dont la partie à douze doigts de zinc est fortement homologue à la protéine CTCF. La séquence d'acides aminés de part et d'autre de cette région est quant à elle très divergente, ce qui implique que CTCF-T se lie sans doute au même ADN cible que CTCF, mais possède des fonctions différentes. De plus, l'expression de CTCF-T et de CTCF s'oppose mutuellement; l'expression de la protéine CTCF-T (cellules CTCF-T positives, CTCF negatives) qui a lieu pendant la spermatogenèse coïncide avec la reprogrammation épigénétique, notamment la méthylation de novo de l'ADN. La présente étude démontre le rôle essentiel joué par la protéine CTCF-T dans l'acquisition de l'empreinte génomique parentale. Nous montrons ici que CTCF-T s'associe in vivo avec les régions ICR des loci Igf2/H19 et Dlk/Gt12. Nous avons également identifié deux nouvelles protéines qui interagissent avec CTCF-T : une protéine arginine méthyl transférase PRMT7, et un variant de l'histone H2A, riche en arginine, que nous avons dénommé trH2A. Ces interactions ont été analysées plus en détail, et confinnent que ces deux protéines s'associent avec la région N-terminale de CTCF-T. Aussi, nous présentons une interaction de la région N-terminale de CTCF-T avec les histones H1, H2, et H3. Ces résultats suggèrent que CTCF-T est une protéine qui se lie spécifiquement aux régions ICR, qui s'associe avec différents histones et qui recrute PRMT7. PRMT7 possède une activité méthyl-tansférase envers les histones. Il a été montré que la méthylation des histones marque certains endroits de la chromatine, dirigeant ainsi la méthylation de l'ADN. Notre hypothèse est donc la suivante : la protéine CTCF-T sert de base qui dirige la méthylation des histones par PRMT7 dans les régions ICR, ce qui contribue à marquer la chromatine pour le recrutement de nouvelles méthyl transférases pour méthyler l'ADN. Afin de valider cette hypothèse, nous avons développé un système de méthylation de l'ADN in vivo, dans des oeufs de Xenopus laevis, dans le noyau desquels nous avons mico-injecté la région ICR du locus H19, ainsi que différents vecteurs d'expression pour CTCF-T, PRMT7, et les de novo méthyl transférases (Dnmt3a, Dnmt3b et Dnmt3L). Les CpGs méthyles de la région ICR du locus H19 ont été analysé 48 et 72 heures après l'injection. Cette technique nous a permis de démontrer que les CpGs de la région ICR sont méthyles en présence de CTCF-T et de PRMT7, tandis que les contrôles injectés seulement avec la région ICR ne présentent aucun signe de méthylation. De plus, nous démontrons pour la première fois que la protéine méthyl transférase Dnmt3L est déterminant pour l'établissement de l'empreinte génomique parentale au niveau de la région ICR du locus H19. Aussi, nous confirmons que les activités méthyl transférases de Dnmt3a et Dnmt3b sont complémentaires. Nos données indiquent que les trois protéines Dnmt3 sont impliquées dans la méthylation de l'ADN. En conclusion, nous proposons un mécanisme responsable de la mise en place de nouvelles empreintes génomiques pendant la spermatogenèse : le complexe protéique CTCF-T/PRMT7 dirige la méthylation des histones aboutissant à la méthylation de novo de l'ADN au locus H19.

Mutations in the cdc10 start gene of Schizosaccharomyces pombe implicate the region of homology between cdc10 and SWI6 as important for p85cdc10 function.

The cdc10 gene of the fission yeast Schizosaccharomyces pombe is required for traverse of start and commitment to the mitotic cell division cycle rather than other fates. The product of the gene, p85cdc10, is a component of a factor that is thought to be involved in regulating the transcription of genes that are required for DNA synthesis. In order to define regions of the p85cdc10 protein that are important for its function a fine structure genetic map of the cdc10 gene was derived and the sequences of 13 cdc10ts mutants determined. The 13 mutants tested define eight alleles. Eleven of the mutants are located in the region that contains the two copies of the cdc10/SWI6 repeat motif, implicating it as important for p85cdc10 function.

Identification of two steroid-responsive promoters of different strength controlled by the same estrogen-responsive element in the 5'-end region of the Xenopus laevis vitellogenin gene A1.

A structural and functional analysis of the 5'-end region of the Xenopus laevis vitellogenin gene A1 revealed two transcription initiation sites located 1.8 kilobases apart. A RNA polymerase II binding assay indicates that both promoters form initiation complexes efficiently. In vitro, using a transcription assay derived from a HeLa whole-cell extract, the upstream promoter is more than 10-fold stronger than the downstream one. In contrast, both promoters have a similar strength in a HeLa nuclear extract. In vivo, that is in estrogen-stimulated hepatocytes, it is the downstream promoter homologous to the one used by the other members of the vitellogenin gene family, which is 50-fold stronger than the upstream promoter. Thus, if functional vitellogenin mRNA results from this latter activity, it would contribute less than 1% to the synthesis of vitellogenin by fully induced Xenopus hepatocytes expressing the four vitellogenin genes. In contrast, both gene A1 promoters are silent in uninduced hepatocytes. Transfection experiments using the Xenopus cell line B3.2 in which estrogen-responsiveness has been introduced reveal that the strong downstream promoter is controlled by an estrogen responsive element (ERE) located 330 bp upstream of it. The upstream promoter can also be controlled by the same ERE. Since the region comprising the upstream promoter is flanked by a 200 base pair long inverted repeat with stretches of homology to other regions of the X. laevis genome, we speculate that it might have been inserted upstream of the vitellogenin gene A1 by a recombination event and consequently brought under control of the ERE lying 1.5 kilobases downstream.

Ligand binding transmits conformational changes across the membrane-spanning region to the intracellular side of the 5-HT3 serotonin receptor.

Conformational changes of channel activation: Five enhanced green fluorescent protein (EGFP) molecules (green cylinders) were integrated into the intracellular part of the homopentameric ionotropic 5-HT3 receptor. This allowed the detection of extracellular binding of fluorescent ligands (?) to EGFP by FRET, and also enabled the quantification of agonist-induced conformational changes in the intracellular region of the receptor by homo-FRET between EGFPs. The approach opens novel ways for probing receptor activation and functional screening of therapeutic compounds.

Sedimentology, geochemistry and mineralogy of the Paleocene-Eocene thermal maximum (PETM) : sediment records from Egypt, India and Spain

A gradual increase in Earth's surface temperatures marking the transition from the late Paleocene to early Eocene (55.8±0.2Ma), represents an extraordinary warming event known as Paleocene-Eocene Thermal Maximum (PETM). Both marine and continental sedimentary records during this period reveal evidences for the massive injection of isotopically light carbon. The carbon dioxide injection from multiple potential sources may have triggered the global warming. The importance of the PETM studies is due to the fact that the PETM bears some striking resemblances to the human-caused climate change unfolding today. Most notably, the culprit behind it was a massive injection of heat-trapping greenhouse gases into the atmosphere and oceans, comparable in volume to what our persistent burning of fossil fuels could deliver in coming centuries. The exact knowledge of what went on during the PETM could help us to foresee the future climate change. The response of the oceanic and continental environments to the PETM is different. Many factors might control the response of the environments to the PETM such as paleogeography, paleotopography, paleoenvironment, and paleodepth. To better understand the mechanisms triggering PETM events, two different environments were studied: 1) shallow marine to inner shelf environment (Wadi Nukhul, Sinai; and the Dababiya GSSP, Luxor, Egypt), and 2) terrestrial environments (northwestern India lignite mines) representing wetland, and fluvial environments (Esplugafreda, Spain) both highlighting the climatic changes observed in continental conditions. In the marine realm, the PETM is characterized by negative ö13Ccar and ô13Corg excursions and shifts in Ô15N to ~0%o values above the P/E boundary and persisting along the interval suggesting a bloom and high production of atmospheric N2-fixers. Decrease in carbonate contents could be due to dissolution and/or dilution by increasing detrital input. High Ti, K and Zr and decreased Si contents at the P/E boundary indicate high weathering index (CIA), which coincides with significant kaolinite input and suggests intense chemical weathering under humid conditions at the beginning of the PETM. Two anoxic intervals are observed along the PETM. The lower one may be linked to methane released from the continental shelf with no change in the redox proxies, where the upper anoxic to euxinic conditions are revealed by increasing U, Mo, V, Fe and the presence of small size pyrite framboids (2-5fim). Productivity sensitive elements (Cu, Ni, and Cd) show their maximum concentrated within the upper anoxic interval suggesting high productivity in surface water. The obtained data highlight that intense weathering and subsequent nutrient inputs are crucial parameters in the chain of the PETM events, triggering productivity during the recovery phase. In the terrestrial environments, the establishment of wetland conditions and consequence continental climatic shift towards more humid conditions led to migration of modern mammals northward following the extension of the tropical belts. Relative ages of this mammal event based on bio-chemo- and paleomagnetic stratigraphy support a migration path originating from Asia into Europe and North America, followed by later migration from Asia into India and suggests a barrier to migration that is likely linked to the timing of the India-Asia collision. In contrast, at Esplugafereda, northeastern Spain, the terrestrial environment reacted differently. Two significant S13C shifts with the lower one linked to the PETM and the upper corresponding to the Early Eocene Thermal Maximum (ETM2); 180/160 paleothermometry performed on two different soil carbonate nodule reveal a temperature increase of around 8°C during the PETM. The prominent increase in kaolinite content within the PETM is linked to increased runoff and/or weathering of adjacent and coeval soils. These results demonstrate that the PETM coincides globally with extreme climatic fluctuations and that terrestrial environments are very likely to record such climatic changes. - La transition Paléocène-Eocène (55,8±0,2 Ma) est marquée par un réchauffement extraordinaire communément appelé « Paleocene-Eocene Thermal Maximum » (PETM). Les données géochimiques caractérisant les sédiments marins et continentaux de cette période indiquent que ce réchauffement a été déclenché par une augmentation massive de CO2 lié à la déstabilisation des hydrates de méthane stockés le long des marges océaniques. L'étude des événements PETM constitue donc un bon analogue avec le réchauffement actuel. Le volume de CO2 émis durant le PETM est comparable avec le CO2 lié à l'activité actuelle humaine. La compréhension des causes du réchauffement du PETM peut être cruciale pour prévoir et évaluer les conséquences du réchauffement anthropogénique, en particulier les répercussions d'un tel réchauffement sur les domaines continentaux et océaniques. De nombreux facteurs entrent en ligne de compte dans le cas du PETM, tels que la paléogéographie, la paléotopographie et les paléoenvironnement. Pour mieux comprendre les réponses environnementales aux événements du PETM, 2 types d'environnements ont été choisis : (1) le domaine marin ouvert mais relativement peu profond (Wadi Nukhul. Sinai, Dababiya, Luxor, Egypte), (2) le milieu continental marécageux humide (mines de lignite, Inde) et fluviatile, semi-aride (Esplugafreda, Pyrénées espagnoles). Dans le domaine marin, le PETM est caractérisé par des excursions négatives du ô13Ccar et ô13Corg et un shift persistant des valeurs de 815N à ~ 0 %o indiquant une forte activité des organismes (bactéries) fixant l'azote. La diminution des carbonates observée durant le PETM peut-être due à des phénomènes de dissolution ou une augmentation des apports terrigènes. Des taux élevés en Ti, K et Zr et une diminution des montants de Si, reflétés par des valeurs des indices d'altération (CIA) qui coïncident avec une augmentation significative des apports de kaolinite impliquent une altération chimique accrue, du fait de conditions plus humides au début du PETM. Deux événements anoxiques globaux ont été mis en évidence durant le PETM. Le premier, situé dans la partie inférieur du PETM, serait lié à la libération des hydrates de méthane stockés le long des talus continentaux et ne correspond pas à des variations significatives des éléments sensibles aux changements de conditions redox. Le second est caractérisé par une augmentation des éléments U, Mo, V et Fe et la présence de petit framboids de pyrite dont la taille varie entre 2 et 5pm. Le second épisode anoxique est caractérisé par une forte augmentation des éléments sensibles aux changements de la productivité (Cu, Ni et Co), indiquant une augmentation de la productivité dans les eaux de surface. Les données obtenues mettent en évidence le rôle crucial joué par l'altération et les apports en nutriments qui en découlent. Ces paramètres sont cruciaux pour la succession des événements qui ont conduit au PETM, et plus particulièrement l'augmentation de la productivité dans la phase de récupération. Durant le PETM, le milieu continental est caractérisé par l'établissement de conditions humides qui ont facilité voir provoqué la migration des mammifères modernes qui ont suivi le déplacement de ces ceintures climatiques. L'âge de cette migration est basé sur des arguments chimiostratigraphiques (isotopes stables), biostratigraphiques et paléomagnétiques. Les données bibliographiques ainsi que celles que nous avons récoltées en Inde, montrent que les mammifères modernes ont d'abord migré depuis l'Asie vers l'Europe, puis dans le continent Nord américain. Ces derniers ne sont arrivés en Inde que plus tardivement, suggérant que le temps de leur migration est lié à la collision Inde-Asie. Dans le Nord-Est de l'Espagne (Esplugafreda), la réponse du milieu continental aux événements PETM est assez différente. Comme en Inde, deux excursions signicatives en ô13C ont été observées. La première correspond au PETM et la seconde est corrélée avec l'optimum thermique de l'Eocène précoce (ETM2). Les isotopes stables de l'oxygène mesurés 2 différents types de nodules calcaires provenant de paléosols suggère une augmentation de 10°C pendant le PETM. Une augmentation simultanée des taux de kaolinite indique une intensification de l'altération chimique et/ou de l'érosion de sols adjacents. Ces résultats démontrent que le PETM coïncide globalement avec des variations climatiques extrêmes qui sont très aisément reconnaissables dans les dépôts continentaux.

Two monoclonal rat antibodies with specificity for the beta-chain variable region V beta 6 of the murine T-cell receptor.

Two rat monoclonal antibodies (mAbs), 44-22-1 and 46-6B5, which recognize an alloreactive cytotoxic clone, 3F9, have been further tested on a panel of T hybridomas and cytotoxic T-cell clones for binding and functional activities. The mAbs recognized only those cells sharing the expression of the T-cell receptor beta-chain variable region gene V beta 6 with 3F9. All V beta 6+ cells were activated by these mAbs under cross-linking conditions and their antigen-specific activation was blocked by soluble mAb. Furthermore, depletion of 46-6B5+ normal lymph node T cells eliminated all cells expressing the epitope recognized by 44-22-1 and V beta 6 mRNA.

Enhancement of autophagic flux after neonatal cerebral hypoxia-ischemia and its region-specific relationship to apoptotic mechanisms.

The multiplicity of cell death mechanisms induced by neonatal hypoxia-ischemia makes neuroprotective treatment against neonatal asphyxia more difficult to achieve. Whereas the roles of apoptosis and necrosis in such conditions have been studied intensively, the implication of autophagic cell death has only recently been considered. Here, we used the most clinically relevant rodent model of perinatal asphyxia to investigate the involvement of autophagy in hypoxic-ischemic brain injury. Seven-day-old rats underwent permanent ligation of the right common carotid artery, followed by 2 hours of hypoxia. This condition not only increased autophagosomal abundance (increase in microtubule-associated protein 1 light chain 3-11 level and punctuate labeling) but also lysosomal activities (cathepsin D, acid phosphatase, and beta-N-acetylhexosaminidase) in cortical and hippocampal CA3-damaged neurons at 6 and 24 hours, demonstrating an increase in the autophagic flux. In the cortex, this enhanced autophagy may be related to apoptosis since some neurons presenting a high level of autophagy also expressed apoptotic features, including cleaved caspase-3. On the other hand, enhanced autophagy in CA3 was associated with a more purely autophagic cell death phenotype. In striking contrast to CA3 neurons, those in CA1 presented only a minimal increase in autophagy but strong apoptotic characteristics. These results suggest a role of enhanced autophagy in delayed neuronal death after severe hypoxia-ischemia that is differentially linked to apoptosis according to the cerebral region.

Biostratigraphy, mineralogy and geochemistry of the Trabakua Pass and Ermua sections in Spain: Paleocene-Eocene transition

Isotopic, geochemical and bulk mineralogical analyses in the Trabakua and Ermua sections, Basque Basin, reveal major changes across the Paleocene-Eocene transition. Expanded sedimentary records exhibit a gradual decrease of 1.0 parts per thousand in delta(13)C values in the lower part of Zone P5 followed by a more rapid 3 parts per thousand negative excursion. The 3 parts per thousand delta(13)C excursion is associated with an abrupt decrease in carbonate sedimentation, increased detrital flux and decreased grain size which suggest changes in marine/atmospheric currents and/or size and structure of the ocean carbon reservoir. The clays recognized at Trabakua record a deep burial diagenesis as indicated by two generations of chlorite, the presence of mixed-layers chlorite-smectite and illite-smectite, the absence of smectite and the near absence of kaolinite. The very low delta(18)O values (<-3.5 parts per thousand) throughout the Trabakua and Ermua sections reflect diagenetic alteration rather than paleotemperatures. Because of deep burial diagenesis and very poorly preserved microfossils, the Trabakua Pass and Ermua sections are not optimal potential stratotypes for the Paleocene-Eocene boundary.

Catabolic ornithine carbamoyltransferase of Pseudomonas aeruginosa. Importance of the N-terminal region for dodecameric structure and homotropic carbamoylphosphate cooperativity.

Pseudomonas aeruginosa has an anabolic (ArgF) and a catabolic (ArcB) ornithine carbamoyltransferase (OTCase). Despite extensive sequence similarities, these enzymes function unidirectionally in vivo. In the dodecameric catabolic OTCase, homotropic cooperativity for carbamoylphosphate strongly depresses the anabolic reaction; the residue Glu1O5 and the C-terminus are known to be essential for this cooperativity. When Glu1O5 and nine C-terminal amino acids of the catabolic OTCase were introduced, by in vitro genetic manipulation, into the closely related, trimeric, anabolic (ArgF) OTCase of Escherichia coli, the enzyme displayed Michaelis-Menten kinetics and no cooperativity was observed. This indicates that additional amino acid residues are required to produce homotropic cooperativity and a dodecameric assembly. To localize these residues, we constructed several hybrid enzymes by fusing, in vivo or in vitro, the E. coli argF gene to the P. aeruginosa arcB gene. A hybrid enzyme consisting of 101 N-terminal ArgF amino acids fused to 233 C-terminal ArcB residues and the reciprocal ArcB-ArgF hybrid were both trimers with little or no cooperativity. Replacing the seven N-terminal residues of the ArcB enzyme by the corresponding six residues of E. coli ArgF enzyme produced a dodecameric enzyme which showed a reduced affinity for carbamoylphosphate and an increase in homotropic cooperativity. Thus, the N-terminal amino acids of catabolic OTCase are important for interaction with carbamoylphosphate, but do not alone determine dodecameric assembly. Hybrid enzymes consisting of either 26 or 42 N-terminal ArgF amino acids and the corresponding C-terminal ArcB residues were both trimeric, yet they retained some homotropic cooperativity. Within the N-terminal ArcB region, a replacement of motif 28-33 by the corresponding ArgF segment destabilized the dodecameric structure and the enzyme existed in trimeric and dodecameric states, indicating that this region is important for dodecameric assembly. These findings were interpreted in the light of the three-dimensional structure of catabolic OTCase, which allows predictions about trimer-trimer interactions. Dodecameric assembly appears to require at least three regions: the N- and C-termini (which are close to each other in a monomer), residues 28-33 and residues 147-154. Dodecameric structure correlates with high carbamoylphosphate cooperativity and thermal stability, but some trimeric hybrid enzymes retain cooperativity, and the dodecameric Glu1O5-->Ala mutant gives hyperbolic carbamoylphosphate saturation, indicating that dodecameric structure is neither necessary nor sufficient to ensure cooperativity.

The social transition of risk factors for cardiovascular disease in the African region: evidence from three cross-sectional surveys in the Seychelles.

OBJECTIVES: To examine the association between socioeconomic status (SES) and several cardiovascular disease risk factors (CVRFs) and to assess whether this association has changed over a 15-year observation period. METHODS: Three independent population-based surveys of CVRFs were conducted in representative samples of all adults aged 25-64 years in the Seychelles, a small island state located east to Kenya, in 1989 (N=1081), 1994 (N=1067) and 2004 (N=1255). RESULTS: Among men, current smoking and heavy drinking were more prevalent in the low versus the high SES group, and obesity was less prevalent. The socioeconomic gradient in diabetes reversed over the study period from lower prevalence in the low versus the high SES group to higher prevalence in the low SES group. Hypercholesterolemia was less prevalent in the low versus the high SES group in 1989 but the prevalence was similar in the two groups in 2004. Hypertension showed no consistent socioeconomic pattern. Among women, the SES gradient in smoking tended to reverse over time from lower prevalence in the low SES group to lower prevalence in the high SES group. Obesity and diabetes were more common in the low versus the high SES group over the study period. Heavy drinking, hypertension and hypercholesterolemia were not socially patterned among women. CONCLUSION: The prevalence of several CVRFs was higher in low versus high SES groups in a rapidly developing country in the African region, and an increase of the burden of these CVRFs in the most disadvantaged groups of the population was observed over the 15 years study period.