A systematic analysis of INO80 in DNA replication

ATP-dependent chromatin remodeling has been shown to be critical for transcription and DNA repair. However, the involvement of ATP-dependent chromatin remodeling in DNA replication remains poorly defined. Interestingly, we found that the INO80 chromatin-remodeling complex is directly involved in the DNA damage tolerance pathways activated during DNA replication. DNA damage tolerance is important for genomic stability and is controlled by formation of either mono-ubiquitinated or multi-ubiquitinated PCNA, which respectively induce error prone or error-free replication bypass of the lesions. In addition, homologous recombination (HR) mediated by the Rad51 pathway is also involved in the DNA damage tolerance pathways. ^ We found that INO80 is specifically recruited to replication origins during S phase in a genome-wide fashion. In addition, DNA combing analysis shows INO80 is required for the resumption of replication at stalled forks induced by methyl methane-sulfonate (MMS). Mechanistically, we find that INO80 is required for PCNA ubiquitination as well as for Rad51 mediated processing of replication forks after MMS treatment. Furthermore, chromatin immunoprecipitation at specific ARSs indicates INO80 is necessary for Rad18 and Rad51 recruitment to replication forks after MMS treatment. Moreover, 2D gel analysis shows INO80 is necessary to process Rad51 mediated intermediates at impeded replication forks. ^ In conclusion, our findings establish a novel role of a chromatin-remodeling complex in DNA damage tolerance pathways and suggest that chromatin remodeling is fundamentally important to ensure faithful replication of DNA and genome stability in eukaryotes. ^

Mechanism of mRNA stability control mediated by AU -rich element: Characterization of cis-elements and trans-factors

Regulation of cytoplasmic deadenylation, the first step in mRNA turnover, has direct impact on the fate of gene expression. AU-rich elements (AREs) found in the 3′ untranslated regions of many labile mRNAs are the most common RNA-destabilizing elements known in mammalian cells. Based on their sequence features and functional properties, AREs can be divided into three classes. Class I or class III ARE directs synchronous deadenylation, whereas class II ARE directs asynchronous deadenylation with the formation of poly(A)-intermediates. Through systematic mutagenesis study, we found that a cluster of five or six copies of AUUUA motifs forming various degrees of reiteration is the key feature dictating the choice between asynchronous versus synchronous deadenylation. A 20–30 nt AU-rich sequence immediately 5 ′ to this cluster of AUUUA motifs can greatly enhance its destabilizing ability and is an integral part of the AREs. These two features are the defining characteristics of class II AREs. ^ To better understand the decay mechanism of AREs, current methods have several limitations. Taking the advantage of tetracycline-regulated promoter, we developed a new transcriptional pulse strategy, Tet-system. By controlling the time and the amount of Tet addition, a pulse of RNA could be generated. Using this new system, we showed that AREs function in both growth- and density-arrested cells. The new strategy offers for the first time an opportunity to investigate control of mRNA deadenylation and decay kinetics in mammalian cells that exhibit physiologically relevant conditions. ^ As a member of heterogeneous nuclear RNA-binding protein, hnRNP D 0/AUF1 displays specific affinities for ARE sequences in vitro . But its in vivo function in ARE-mediated mRNA decay is unclear. AUF1/hnRNP D0 is composed of at least four isoforms derived by alternative RNA splicing. Each isoform exhibits different affinity for ARE sequence in vitro. Here, we examined in vivo effect of AUF1s/hnRNP D0s on degradation of ARE-containing mRNA. Our results showed that all four isoforms exhibit various RNA stabilizing effects in NIH3T3 cells, which are positively correlated with their binding affinities for ARE sequences. Further experiments indicated that AUF1/hnRNP D0 has a general role in modulating the stability of cytoplasmic mRNAs in mammalian cells. ^

The functional role of the tumor suppressor MMAC /PTEN in glioblastoma multiforme and prostate cancer

Investigations into the molecular basis of glioblastoma multiforme led to the identification of a putative tumor suppressor gene, MMAC/ PTEN. Initial studies implicated MMAC/PTEN in many different tumor types, and identified a protein phosphatase motif in its sequence. This project aimed to identify the biological and biochemical functions of MMAC/PTEN by transiently expressing the gene in cancer cells that lack a functional gene product. ^ Expression of MMAC/PTEN mildly suppressed the growth of U251 human glioma cells and abrogated the growth advantage mediated by overexpression of the epidermal growth factor receptor (EGFR). Immunoblotting demonstrated that MMAC/PTEN expression did not affect the phosphorylation of the EGFR itself, or the intermediates of several downstream signaling pathways. However, MMAC/PTEN expression significantly reduced the phosphorylation and catalytic activity of the proto-oncogene Akt/PKB. While Akt/PKB regulates the survival of many cell types, expression of MMAC/PTEN did not induce apoptosis in adherent U251 cells. Instead, MMAC/PTEN expression sensitized the cells to apoptosis when maintained in suspension (anoikis). As the survival of suspended cells is one of the hallmarks leading to metastasis, MMAC/PTEN expression was examined in a system in which metastasis is more clinically relevant, prostate cancer. ^ Expression of MMAC/PTEN in both LNCaP and PC3-P human prostate cancer cells specifically inhibited Akt/PKB phosphorylation. MMAC/PTEN expression in LNCaP cells resulted in a profound inhibition of growth that was significantly greater than that achieved with expression of p53. Expression of MMAC/PTEN in PC3-P cells resulted in greater growth inhibition than was observed in U251 glioma cells, but less than was observed in LNCaP cells, or upon p53 expression. To determine if MMAC/PTEN could function as a tumor suppressor in vivo, the effects of MMAC/PTEN expression on PC3-P cells implanted orthotopically in nude mice were examined. The ex-vivo expression of MMAC/PTEN did not decrease tumor incidence, but it did significantly decrease tumor size and metastasis. In-vivo expression of MMAC/PTEN in pre-established PC3-P tumors did not significantly inhibit tumor incidence or size, but did inhibit metastasis formation. ^ These studies demonstrate that MMAC/PTEN is a novel and important tumor suppressor gene, which functions to downregulate an important cell survival signaling pathway. ^

Activation of c -Met contributes to growth and metastasis of human colorectal carcinoma

c-Met is the protein tyrosine kinase receptor for hepatocyte growth factor/scatter factor (HGF/SF) and mediates several normal cellular functions including proliferation, survival, and migration. Overexpression of c-Met correlates with progression and metastasis of human colorectal carcinoma (CRC). The goals of this study were to determine if overexpression of c-Met directly contributes to tumorigenicity and liver metastatic potential of colon cancer, and what are the critical pathways regulated by c-Met in this process. The studies used two colon tumor cell lines, KM12SM and KM20, which express high levels of constitutively active c-Met and are highly metastatic in nude mice. To examine the effects of c-Met overexpression, subclones of theses lines with reduced c-Met expression were obtained following transfection with a c-Met specific targeting ribozyme. Reduction of c-Met in KM12SM cells abolished liver metastases when cells were injected intrasplenically in an experimental metastasis assay. However, c-Met downregulation in theses clones was unstable. Three stable KM20 clones with a 25–35% reduction in c-Met protein levels but 60–90% reduction in basal c-Met autophosphorylation and kinase activity were obtained. While HGF increased c-Met kinase activity in the clones with reduced c-Met, the activity was less than that observed in parental or control transfected cells. Correlating with the reduction in c-Met kinase activity, subclones with reduced c-Met expression had significantly reduced in vitro growth rates, soft-agar colony forming abilities, and increased apoptosis. HGF/SF treatment did not affect anchorage-dependent growth or soft-agar colony forming abilities. Further, c-Met downregulation significantly impaired the ability of HGF/SF to induce migration. To examine the effects of reduced c-Met on tumor formation, parental and c-Met reduced KM20 cells were grown subcutaneously and intrahepatically in nude mice. c-Met downregulation delayed, but did not abolish growth at the subcutaneous site. When these cells were injected intrahepatically, both tumor incidences and size were significantly reduced. To further understand the molecular basis of c-Met in promoting tumor growth, the activation of several signaling intermediates that have been implicated in c-Met mediated growth, survival and migration were compared between KM20 parental cells and subclones with reduced c-Met expression levels. The expression and activity (as determined by phosphorylation) of AKT and Erk1/2 were unaltered. In contrast, Src kinase activity, as measured by immune complex kinase assay, was reduced 2–5 fold following c-Met downregulation. As Src has been implicated in growth, survival and migration, Src activation in c-Met overexpressing lines is likely contributing to the tumorigenic and metastatic capabilities of colon tumor cell lines that overexpress c-Met. Collectively, these results suggest that c-Met overexpression plays a causal role in the development of CRC liver metastases, and that c-Src and c-Met inhibitors may be of potential therapeutic benefit for late-stage colon cancer. ^

New Pliocene and Pleistocene acritarchs from the North Atlantic, Arctic Ocean and Bering Sea

Acritarchs have received limited attention in palynological studies of the Cenozoic, although they have much potential both for refining Neogene and Quaternary stratigraphy, especially in mid- and high northern latitudes, and developing palaeoceanographical reconstructions. Here we formally describe and document the stratigraphical and palaeotemperature ranges (from foraminiferal Mg/Ca) of four new acritarch species: Cymatiosphaera? aegirii sp. nov., Cymatiosphaera? fensomei sp. nov., Cymatiosphaera? icenorum sp. nov. and Lavradosphaera canalis sp. nov. In reviewing the stratigraphical distributions of all species of the genus Lavradosphaera De Schepper & Head, 2008, we demonstrate their correlation potential between the North Atlantic and Bering Sea in the Pliocene. Additionally, Lavradosphaera lucifer De Schepper & Head, 2008 and Lavradosphaera canalis sp. nov., while not themselves overlapping stratigraphically, have morphological intermediates that do partially overlap and may represent an evolutionary trend consequent upon climate cooling in the Late Pliocene. Finally, we show that the highest abundances of the acritarchs presented here were living in the eastern North Atlantic, in surface-water temperatures not very different from today.

Influencia del manejo del suelo y las coberturas vegetales en el microclima de la canopia de la vid, la composición de la uva y el vino

Para determinar la influencia del manejo del suelo sobre la composición de la uva y el vino se estableció un experimento en un viñedo de Cabernet Sauvignon conducido en doble cordón de pitones en espaldero alto. Se aplicaron tres tratamientos: TR-suelo sin maleza; CVP-cobertura de suelo espontánea y control del desarrollo vegetativo por desbrozado y CA-cobertura de flora espontánea y control del desarrollo vegetativo con aplicación de herbicida de contacto desecante. En la uva se determinó el contenido de azúcar, acidez total, pH y la composición fenólica (índice de polifenoles totales (IPT), grado de polimerización, flavonoles, flavan-3-oles, antocianos y proantocianidoles). Se elaboraron vinos que fueron evaluados físico-química y sensorialmente por jueces expertos. CVP tuvo el mayor contenido de antocianas y TR el de flavonoles, flavan-3-oles, proantocianidoles, IPT y grado de polimerización; CA presentó valores intermedios. Los vinos del tratamiento TR tuvieron mayor contenido de alcohol y menor de acidez total, con el color rojo (DO520) más bajo y una intensidad colorante más pequeña. Los vinos de CA y TR resultaron más amargos, más astringentes y más ásperos, y los de CVP tuvieron mayor carácter varietal. Resultó útil el empleo de coberturas de raíces superficiales y permanentemente desbrozadas para provocar cierta disminución en los valores de radiación reflejada y de la temperatura de la canopia. Las elevadas temperaturas y alta radiación solar son perjudiciales para la uva, porque aumentan la producción de quercetina y afectan el metabolismo y la degradación de antocianos.

Sulphur and iron species in Dvurechenskii mud volcano sediments

The deep Black Sea is known to be depleted in electron-acceptors for sulphide oxidation. This study on depth distributions of sulphur species (S(II), S(0),S(n)**2-,S2O3**2-,SO3**2-,SO4**2-) in the Dvurechenskii mud volcano, a cold seep situated in the permanently anoxic eastern Black Sea basin (Sorokin Trough, 2060 m water depth), showed remarkable concentrations of sulphide oxidation products. Sulphite concentrations of up to 11 µmol L**1-, thiosulphate concentrations of up to 22 µmol L**1-, zero-valent sulphur concentrations of up to 150 µmol L**1- and up to five polysulphide species were measured in the upper 20 cm of the sediment. Electron-acceptors found to be available in the Dvurechenskii mud volcano (DMV) for the oxidation of hydrogen sulphide to sulphide oxidation intermediates are iron-minerals, and probably also reactive manganese phases. Up to 60 µmol g**1- of reactive iron-minerals and up to 170 µmol L**1- dissolved iron was present in the central summit with the highest fluid upflow and fresh mud outflow. Thus, the source for the oxidative power in the DMV are reactive iron phases extruded with the mud from an ancient source in the deeply buried sediments, leading to the formation of various sulphur intermediates in comparably high concentrations. Another possible source of sulphide oxidation intermediates in DMV sediments could be the formation of zero-valent sulphur by sulphate dependent anaerobic microbial oxidation of methane followed by disproportionation of zero-valent sulphur. Sulphide oxidation intermediates, which are produced by these processes, do not reach thermodynamic equilibrium with rhombic sulphur, especially close to the active center of the DMV due to a short equilibration time. Thus, mud volcano sediments, such as in the DMV, can provide oxidizing niches even in a highly reduced environment like the abyssal part of the Black Sea.

Chiasmolithus species in middle Eocene and Oligocene sediments of ODP Holes 105-647A and 120-748B

In this preliminary biometric study of the calcareous nannofossil species Chiasmolithus expansus, Chiasmolithus oamaruensis, and Chiasmolithus altus from the upper middle Eocene to lower Oligocene of Sites 647 and 748, we document a complete gradation of forms among all three species. Chiasmolithus oamaruensis has significantly higher morphologic variance than the other species. The Chiasmolithus population at each site changes from C. expansus to C. oamaruensis and then to C. altus. This may not reflect a true evolutionary sequence because a major reversal in shape change of the central cross-bar structure accompanies this sequence, and because C. altus is morphologically closer to C. expansus than it is to C. oamaruensis. The change in the width of the cross-bar structure is primarily a result of changes in the alignment of the central connecting bar, rather than of changes in the cross-bar angle. At Site 748, two fluctuations in morphology produce sample populations intermediate between all three species. In addition, reported stratigraphic and paleogeographic occurrences of C. oamaruensis and C. altus show different latitudinal distributions. These morphological and distributional patterns may be explained by a continuous morphologic gradient between C. oamaruensis and C. altus, with C. oamaruensis occurring more commonly in cool-water paleoenvironments, and C. altus occurring more commonly in cold-water paleoenvironments. Thus, paleoenvironmental fluctuations at Site 748 may be the cause of the morphologic fluctuations in Chiasmolithus. This hypothesis can be tested against previously proposed evolutionary models by more detailed sampling of sections along a latitudinal transect.

La escuela intermedia revisitada : Racionalización y revisión curricular en la provincia de Buenos Aires durante la última dictadura militar

Este artículo pretende hacer un aporte al área de estudios sobre la educación bajo la última dictadura militar en la Argentina. En este trabajo presentaremos un aspecto poco visto por los investigadores, como es el análisis de las políticas educativas de "racionalización" y "revisión curricular" referidas a los niveles primario y secundario que fueron diseñadas e implementadas por los cinco ministros de educación de la provincia de Buenos Aires. Pretendemos mostrar dos cuestiones relacionadas, en primer lugar, que el argumento de la política de racionalización esgrimido por los funcionarios dictatoriales pretendió legitimar públicamente una serie de acciones que buscaba frenar la expansión del sistema. En segundo término, veremos que la revisión curricular pensada para el nivel secundario y algunas propuestas realizadas para los últimos años de la primaria contenían elementos del controvertido proyecto de la "escuela intermedia".

La escuela intermedia revisitada : Racionalización y revisión curricular en la provincia de Buenos Aires durante la última dictadura militar

Este artículo pretende hacer un aporte al área de estudios sobre la educación bajo la última dictadura militar en la Argentina. En este trabajo presentaremos un aspecto poco visto por los investigadores, como es el análisis de las políticas educativas de "racionalización" y "revisión curricular" referidas a los niveles primario y secundario que fueron diseñadas e implementadas por los cinco ministros de educación de la provincia de Buenos Aires. Pretendemos mostrar dos cuestiones relacionadas, en primer lugar, que el argumento de la política de racionalización esgrimido por los funcionarios dictatoriales pretendió legitimar públicamente una serie de acciones que buscaba frenar la expansión del sistema. En segundo término, veremos que la revisión curricular pensada para el nivel secundario y algunas propuestas realizadas para los últimos años de la primaria contenían elementos del controvertido proyecto de la "escuela intermedia".

La escuela intermedia revisitada : Racionalización y revisión curricular en la provincia de Buenos Aires durante la última dictadura militar

Este artículo pretende hacer un aporte al área de estudios sobre la educación bajo la última dictadura militar en la Argentina. En este trabajo presentaremos un aspecto poco visto por los investigadores, como es el análisis de las políticas educativas de "racionalización" y "revisión curricular" referidas a los niveles primario y secundario que fueron diseñadas e implementadas por los cinco ministros de educación de la provincia de Buenos Aires. Pretendemos mostrar dos cuestiones relacionadas, en primer lugar, que el argumento de la política de racionalización esgrimido por los funcionarios dictatoriales pretendió legitimar públicamente una serie de acciones que buscaba frenar la expansión del sistema. En segundo término, veremos que la revisión curricular pensada para el nivel secundario y algunas propuestas realizadas para los últimos años de la primaria contenían elementos del controvertido proyecto de la "escuela intermedia".

Origin and evolution of Cycladophora davisiana (Radiolaria) in DSDP Hole 19-192, Northwest Pacific

This paper documents the evolutionary history of Cycladophora davisiana Ehrenberg from an uppermost Miocene to Pleistocene sedimentary record in the high-latitude Northwest Pacific. It apparently evolved from C. sakaii Motoyama through a series of intermediates. C. sakaii has a relatively large shell with an external spongy layer. The evolutionary transition is characterized by a relatively rapid decrease in thorax size with a reduction of the spongy appendage. This change occurred during about 0.4 m.y. from 2.8 to 2.4 Ma without cladogenesis. Following this interval, a decrease in thorax size continued gradually up to the Recent, resulting in a very small morphology. Although the population of C. davisiana first appeared at about 2.5 Ma, some morphotypic specimens may occur in earlier periods as indistinguishable very small endmembers in the C. sakaii populations. Timing of the first appearance events both of morphotypic specimens and of a population of C. davisiana in Site 192 and previously reported cores does not disprove the idea that C. davisiana evolved first in the Northwest Pacific region, and later migrated into other regions of the world ocean. Biometrics clearly indicate no direct phylogenetic relationships between C. davisiana and C. cornutoides Kling in the studied core. Thus, the latter species, which was originally described as a variation and later elevated to a subspecies of the former species, is separated from the former species and raised to the species rank.

Pore water chemistry of ODP Sites 201-1225, 201-1226 and 201-1231

High-resolution analyses of the oxygen isotope ratio (18O/16O) of dissolved sulfate in pore waters have been made to depths of >400 meters below seafloor (mbsf) at open-ocean and upwelling sites in the eastern equatorial Pacific Ocean. d18O values of dissolved sulfate (d18O-SO4) at the organic-poor open-ocean Site 1231 gave compositions close to modern seawater (+9.5 per mil vs. Vienna-standard mean ocean water, providing no chemical or isotopic evidence for microbial sulfate reduction (MSR). In contrast, the maximum d18O values at Sites 1225 and 1226, which contain higher organic matter contents, are +20 per mil and +28 per mil, respectively. Depth-correlative trends of increasing d18O-SO4, alkalinity, and ammonium and the presence of sulfide indicate significant oxidation of sedimentary organic matter by sulfate-reducing microbial populations at these sites. Although sulfate concentration profiles at Sites 1225 and 1231 both show similarly flat trends without significant net MSR, d18O-SO4 values at Site 1225 reveal the presence of significant microbial sulfur-cycling activity, which contrasts to Site 1231. This activity may include contributions from several processes, including enzyme-catalyzed equilibration between oxygen in sulfate and water superimposed upon bacterial sulfate reduction, which would tend to shift d18O-SO4 toward higher values than MSR alone, and sulfide oxidation, possibly coupled to reduction of Fe and Mn oxides and/or bacterial disproportionation of sulfur intermediates. Large isotope enrichment factors observed at Sites 1225 and 1226 (epsilon values between 42 per mil and 79 per mil) likely reflect concurrent processes of kinetic isotope fractionation, equilibrium fractionation between sulfate and water, and sulfide oxidation at low rates of sulfate reduction. The oxygen isotope ratio of dissolved pore water sulfate is a powerful tool for tracing microbial activity and sulfur cycling by the deep biosphere of deep-sea sediments.

Geochemistry of tetrapyrrole, tetraterpenoid, and perylene pigments in sediments from the Gulf of California

Results and discussion cover pigment analyses of 36 sediment samples recovered by Deep Sea Drilling Project Leg 64, and six samples from the Leg 64 site-survey cruise in the Guaymas Basin (Scripps Institution of Oceanography, Leg 3). Pigments investigated were tetrapyrroles, tetraterpenoids, and the PAH compound perylene. Traces of mixed nickel and copper ETIO-porphyrins were ubiquitous in all sediment samples, except for the very surface (i.e., <2 m sub-bottom), and their presence is taken as an indication of minor influxes of previously oxidized allochthonous (terrestrial) organic matter. Phorbides and chlorins isolated from Site 479 sediment samples (i.e., the oxygen-minimum locale, northeast of the Guaymas Basin) well represent the reductive diagenesis ("Treibs Scheme"; see Baker and Palmer, 1978; Treibs, 1936) of chlorophyll derivatives. Three forms of pheophytin-a, plus a variety of phorbides, were found to give rise to freebase porphyrins, nickel phylloerythrin, and nickel porphyrins, with increasing depth of burial (increasing temperature). Sediments from Sites 481, 10G, and 18G yielded chlorophyll derivatives characteristic of early oxidative alterations. Included among these pigments are allomerized pheophytin-a, purpurin-18, and chlorin-p6. The high thermal gradient imposed upon the late Quaternary sediments of Site 477 greatly accelerated chlorophyll diagenesis in the adjacent overlying sediments, that is, the production of large quantities of free-base desoxophylloerythroetioporphyrin (DPEP) occurred in a section (477-7-5) presently only 49.8 meters sub-bottom. Present depth and age of these sediments are such that only chlorins and phorbides would be expected. Carotenoid (i.e., tetraterpenoids) concentrations were found to decrease rapidly with increasing sub-bottom depth. Less deeply buried sediments (e.g., 0-30 m) yielded mixtures of carotenes and oxygen-substituted carotenoids. Oxygencontaining (oxy-, oxo-, epoxy-) carotenoids were found to be lost preferentially with increased depth of burial. Early carotenoid diagenesis is suggested as involving interacting reductions and dehydrations whereby dehydro-, didehydro-, and retro-carotenes are generated. Destruction of carotenoids as pigments may involve oxidative cleavage of the isoprenoid chain through epoxy intermediates, akin to changes in the senescent cells of plants. Perylene was found to be a common component of the extractable organic matter from all sediments investigated. The generation of alkyl perylenes was found to parallel increases in the existing thermal regime at all sites. Igneous sills and sill complexes within the sediment profile of Site 481 altered (i.e., scrambled) the otherwise straightforward thermally induced alkylation of perylene. The degree of perylene alkylation is proposed as an indicator of geothermal stress for non-contemporaneous marine sediments.

Oxygen Reduction Reaction on Pt Overlayers Deposited onto a Gold Film: Ligand, Strain, and Ensemble Effect

We study the oxygen reduction reaction (ORR), the catalytic process occurring at the cathode in fuel cells, on Pt layers prepared by electrodeposition onto an Au substrate. Using a nominal Pt layer by layer deposition method previously proposed, imperfect layers of Pt on Au are obtained. The ORR on deposited Pt layers decreases with increasing Pt thickness. In the submonolayer region, however, the ORR activity is superior to that of bulk Pt. Using density functional theory (DFT) calculations, we correlate the observed activity trend to strain, ligand, and ensemble effects. At submonolayer coverage certain atom configurations weaken the binding energies of reaction intermediates due to a ligand and ensemble effect, thus effectively increasing the ORR activity. At higher Pt coverage the activity is governed by a strain effect, which lowers the activity by decreasing the oxidation potential of water. This study is a nice example of how the influence of strain, ligand, and ensemble effects on the ORR can be deconvoluted.