Properties of patchy colloidal particles close to a surface: a Monte Carlo and density functional study

We investigate the behavior of a patchy particle model close to a hard-wall via Monte Carlo simulation and density functional theory (DFT). Two DFT approaches, based on the homogeneous and inhomogeneous versions of Wertheim's first order perturbation theory for the association free energy are used. We evaluate, by simulation and theory, the equilibrium bulk phase diagram of the fluid and analyze the surface properties for two isochores, one of which is close to the liquid side of the gas-liquid coexistence curve. We find that the density profile near the wall crosses over from a typical high-temperature adsorption profile to a low-temperature desorption one, for the isochore close to coexistence. We relate this behavior to the properties of the bulk network liquid and find that the theoretical descriptions are reasonably accurate in this regime. At very low temperatures, however, an almost fully bonded network is formed, and the simulations reveal a second adsorption regime which is not captured by DFT. We trace this failure to the neglect of orientational correlations of the particles, which are found to exhibit surface induced orientational order in this regime.

Formation of chlorite during thrust fault reactivation. Record of fluid origin and P-T conditions in the Monte Perdido thrust fault (southern Pyrenees)

The chemical and isotopic compositions of clay minerals such as illite and chlorite are commonly used to quantify diagenetic and low-grade metamorphic conditions, an approach that is also used in the present study of the Monte Perdido thrust fault from the South Pyrenean fold-and-thrust belt. The Monte Perdido thrust fault is a shallow thrust juxtaposing upper Cretaceous-Paleocene platform carbonates and Lower Eocene marls and turbidites from the Jaca basin. The core zone of the fault, about 6 m thick, consists of intensely deformed clay-bearing rocks bounded by major shear surfaces. Illite and chlorite are the main hydrous minerals in the fault zone. Illite is oriented along cleavage planes while chlorite formed along shear veins (< 50 mu m in thickness). Authigenic chlorite provides essential information about the origin of fluids and their temperature. delta O-18 and delta D values of newly formed chlorite support equilibration with sedimentary interstitial water, directly derived from the local hanging wall and footwall during deformation. Given the absence of large-scale fluid flow, the mineralization observed in the thrust faults records the P-T conditions of thrust activity. Temperatures of chlorite formation of about 240A degrees C are obtained via two independent methods: chlorite compositional thermometers and oxygen isotope fractionation between cogenetic chlorite and quartz. Burial depth conditions of 7 km are determined for the Monte Perdido thrust reactivation, coupling calculated temperature and fluid inclusion isochores. The present study demonstrates that both isotopic and thermodynamic methods applied to clay minerals formed in thrust fault are useful to help constrain diagenetic and low-grade metamorphic conditions.

Caracterização de reservatórios siliciclásticos neoaptianos: um estudo do membro carmópolis no campo de Camorim, sub-bacia de Sergipe, Brasil

The Camorim Oilfield, discovered in 1970 in the shallow water domain of the Sergipe Sub-basin, produces hydrocarbons from the Carmópolis Member of the Muribeca Formation, the main reservoir interval, interpreted as siliciclastics deposited in an alluvial-fluvial-deltaic context during a late rifting phase of Neoaptian age, in the Sergipe-Alagoas Basin. The structural setting of the field defines different production blocks, being associated to the evolution of the Atalaia High during the rift stage and subsequent reactivations, encompassing NE-SW trending major normal faults and NWEW trending secondary faults. The complexity of this field is related to the strong facies variation due to the interaction between continental and coastal depositional environments, coupled with strata juxtaposition along fault blocks. This study aims to geologically characterize its reservoirs, to provide new insights to well drilling locations in order to increase the recovery factor of the field. Facies analysis based on drill cores and geophysical logs and the 3D interpretation of a seismic volume, provide a high resolution stratigraphic analysis approach to be applied in this geodynamic transitional context between the rift and drift evolutionary stages of the basin. The objective was to define spatial and time relations between production zones and the preferential directions of fluid flow, using isochore maps that represent the external geometry of the deposits and facies distribution maps to characterize the internal heterogeneities of these intervals, identified in a 4th order stratigraphic zoning. This work methodology, integrated in a 3D geological modelling process, will help to optimize well drilling and hydrocarbons production. This methodology may be applied in other reservoirs in tectonic and depositional contexts similar to the one observed at Camorim, for example, the oil fields in the Aracaju High, Sergipe Sub-basin, which together represent the largest volume of oil in place in onshore Brazilian basins

Bandamento em cromossomos de peixes: discussão sobre o conceito de compartimentalização cromossômica

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Identifizierung, Sequenzierung und Charakterisierung des Dmxl1-Gen in Mus musculus sowie die funktionelle Analyse durch Knock-Out

Identifizierung, Sequenzierung und Charakterisierung des Dmxl1-Gen in Mus musculus sowie die funktionelle Analyse durch Knock-OutrnrnBei Dmxl1 handelt es sich um ein neuartiges Gen aus Mus musculus. Das ebenfalls in der vorliegenden Arbeit bioinformatisch untersuchte Gen DMXL1 ist das zu Dmxl1 homologe Gen des Menschen. Beide Gene bestehen aus 43 Exons, das murine Dmxl1 codiert für eine mRNA von 10992 bp bzw. 12210 bp, das humane DMXL1 kodiert für eine cDNA von 11082 bp, der offene Leserahmen umfasst bei der Maus 9042 bp. In der Maus konnte ein mögliches alternatives Polyadenylierungssignal identifiziert werden. Zwischen beiden Spezies sind die Exonpositionen und ihre Längen hoch konserviert. Dmxl1 liegt auf dem Crick-Strang von Chromosom 18 Bande C, der translatierte Bereich erstreckt sich auf genomischer Ebene über 129558 bp und die Orientierung verläuft in Richtung Centromer. Dmxl1 und DMXL1 gehören damit zu den größten bekannten Genen in Maus und Mensch. Bei beiden Spezies liegen die DmX-Homologen genomisch innerhalb eines Bereichs der Isochoren-Klasse L1 in einer Gen-armen Region. Die Anzahl der repetitiven Elemente innerhalb der Genregion von Dmxl1 liegt 6% unter dem erwarteten Wert eines L1 Isochors, die Anzahl beim Menschen liegt 4% über dem erwarteten Wert. Um die mögliche Promotorstruktur von Dmxl1 darzustellen, wurden umfangreiche in silico-Analysen der Region um den putativen Transkriptionsstart vorgenommen. Mit Hilfe der gewonnenen Daten konnte ein Transkriptionstartpunkt identifiziert werden. Zudem wurde eine Promotorstruktur erarbeitet, bei der angenommen werden kann, dass sie eine gute Näherung an die tatsächlich vorhandenen Bindungsstellen von Transkriptionsfaktoren darstellt. Die mit bioinformatischen Werkzeugen erzeugte virtuelle Promotor- und Enhancerstruktur zeigt das Potenzial, Dmxl1 basal und ubiquitär zu exprimieren. Gleichzeitig zeigen diese Daten, dass Dmxl1 vermutlich in einigen Geweben der Keimbahn, im Fettgewebe, dem blutbildenen System und während der Embryogenese hochkomplex reguliert werden kann. Eine regulierte Expression zur Steuerung des Energiestoffwechsels ist ebenfalls wahrscheinlich. Diese Ergebnisse passen sehr gut zu den experimentell ermittelten Daten und den beobachteten Phänotypen Dmxl1-chimärer Mäuse.rnDie abgeleitete Aminosäuresequenz umfasst in der Maus 3013 AS, im Menschen 3027 AS, der Vergleich der abgeleiteten Aminosäuresequenzen zeigt eine Identität von 89,3 % und eine Similarität von 94,7 % zwischen beiden Spezies. Im Dmxl1/DMXL1-Protein von Maus und Mensch konnten mindestens 24 und maximal 36 WD-Wiederholungseinheiten identifiziert werden, zudem wurden eine Reihe weiterer konservierter Proteinmotive gefunden. Die in silico-Strukturanalysen beider abgeleiteter Aminosäuresequenzen lässt vermuten, dass sich C- und N-terminal WD-Propellerstrukturen befinden. In dieser Arbeit gelang eine C-terminale Rekonstruktion einer 10-blättrigen Propellerstruktur, denkbar ist jedoch auch eine Struktur mit mindestens drei WD-Propellern, wenn eine prädominante Struktur mit Propellern aus jeweils sieben Propellerblättern angenommen wird.rnDas primäre Ziel dieser Arbeit, die Etablierung einer stabilen Mauslinie mit diruptiertem Dmxl1-Gen konnte aufgrund einer beobachteten Haploinsuffizienz nicht erreicht werden. Trotz zahlreicher Transformationen von Maus-Stammzelllinien konnte letztlich nur eine stabil transformierte Linie mit einem Dmxl1-Null-Allel identifiziert werden, was auch zu den theoretischen Daten und den angenommenen Aufgaben von Dmxl1 als komplex und diffizil reguliertes Multifunktions-Protein passt. Aus der transformierten Mauszelllinie konnten chimäre Mäuse entwickelt werden, die in Abhängigkeit von dem Ausmaß des Chimärismus phänotypisch massive Schädigungen aufwiesen. Neben einer Teilsterilität wurden massive Fettleibigkeit und ein ausgeprägter Hypogonadismus beobachtet. Keines der Tiere war in der Lage das Dmxl1-Null-Allel zu transduzieren. Die Tiere waren nur sehr eingeschränkt fertil, die wenigen Nachkommen entsprachen genotypisch und phänotypisch ausschließlich den verwendeten Blastocysten.rn

Chemistry of fluid inclusions in rock samples from Dronning Maud Land

Dense, CO2-rich fluid inclusions hosted by plagioclases, An45 to An54, of the O.-v.-Gruber- Anorthosite body, central Dronning Maud Land, East Antarctica, contain varying amounts of small calcite, paragonite and pyrophyllite crystals detected by Raman microspectroscopy. These crystals are reaction products that have formed during cooling of the host and the original CO2-rich H2O-bearing enclosed fluid. Variable amounts of these reaction products illustrates that the reaction did not take place uniformly in all fluid inclusions, possibly due to differences in kinetics as caused by differences in shape and size, or due to compositional variation in the originally trapped fluid. The reaction albite + 2anorthite + 2H2O + 2CO2 = pyrophyllite + paragonite + 2calcite was thermodynamically modelled with consideration of different original fluid compositions. Although free H2O is not detectable in most fluid inclusions, the occurrence of OH-bearing sheet silicates indicates that the original fluid was not pure CO2, but contained significant amounts of H2O. Compared to an actual fluid inclusion it is obvious, that volume estimations of solid phases can be used as a starting point to reverse the retrograde reaction and recalculate the compositional and volumetrical properties of the original fluid. Isochores for an unmodified inclusion can thus be reconstructed, leading to a more realistic estimation of P-T conditions during earlier metamorphic stages or fluid capturing.

New data on the ophiolitic VMS deposits of Moeche (Cabo Ortegal Complex, NW Spain)

As a result of the variscan collision, several allochtonous complexes were emplaced on the Iberian margin in Devonian times, among them the Cabo Ortegal Complex comprising the Moeche ophiolitic sequence. Copper has been won from several mines (Piquitos I & II, Barqueira, Maruxa) from disseminated ores and thin massive sulphide layers in the Moeche Unit, a strongly deformed meta-volcanic sequence comprising mainly quartz-chlorite schists and mylonites, which defines the top of the ophiolite. The ores were metamorphosed and strongly deformed under brittle conditions (for pyrite), but their textures are often apparently post-deformational, due to very common solution-transfer processes; they are composed mostly of pyrite and chalcopyrite, with minor sphalerite, pyrrhotite, etc., and with traces of native gold and PGE. The geology, mineralogy, and geochemistry of the orebodies relate closely to VMS of the Cu-Zn (Cyprus) type. Fluid inclusion studies allowed an estimation of metamorphic conditions at pressures of 2/2’5 kb and T 325/350ºC. New determinations using the chlorite geothermometer yield temperatures around 320 ºC, corresponding to pressures near 2 kb according to the isochores deduced from the fluid inclusion study, although in the Barqueira mine higher temperatures, up to 350 ºC, are found, corresponding to presssures up to 2’5 kb. Pb isotopic compositions of pyrite point to a double source of Pb, i.e. a main mantle and a subordinate crustal source. The values for 87SR/86Sr in pyrite support this interpretation, but some results suggest later mobilization in an open system, corresponding to solution-transfer. Age determinations of pyrite deduced from the Pb isotope uranogenic graph, ≈ 480 Ma, do not fit with the metamorphic ages published for the Moeche Unit, and might point to the age of Pb extraction from the mantle.

A compositional map of human chromosome band Xq28.

The molar fractions of guanine plus cytosine (GC) in DNA were determined for 36 yeast artificial chromosomes (YACs) which almost completely cover human chromosome band Xq28, a terminal reverse band, corresponding to about 8 Mb of DNA. This allowed the construction of the most complete compositional map to date of a chromosomal band; three regions were observed: (i) a proximal 3.5-Mb region formed by GC-poor L and GC-rich H1 isochores; (ii) a middle 2,2-Mb region essentially formed by a GC-rich H2 isochore and a very GC-rich H3 isochore separated by a GC-poor L isochore, YACs from this region being characterized by a striking compositional heterogeneity and instability; and (iii) a distal 1.3-Mb region exclusively formed by GC-poor L isochores. Gene and CpG island concentrations increased with the GC levels of the isochores, as expected. Xq28 exemplifies a subset of reverse bands which are different from the two other subsets, namely from telomeric bands, which are characterized by specific cytogenetic properties and by the predominance of H2 and H3 isochores, and from the majority of reverse bands, which do not contain H2 and H3 isochores.

The gene distribution of the maize genome.

Previous investigations from our laboratory showed that the genomes of plants, like those of vertebrates, are mosaics of isochores, i.e., of very long DNA segments that are compositionally homogeneous and that can be subdivided into a small number of families characterized by different GC levels (GC is the mole fraction of guanine+cytosine). Compositional DNA fractions corresponding to different isochore families were used to investigate, by hybridization with appropriate probes, the gene distribution in vertebrate genomes. Here we report such a study on the genome of a plant, maize. The gene distribution that we found is most striking, in that almost all genes are present in isochores covering an extremely narrow (1-2%) GC range and only representing 10-20% of the genome. This gene distribution, which seems to characterize other Gramineae as well, is remarkably different from the gene distribution previously found in vertebrate genomes.

A generalized Markov sampler

A recent development of the Markov chain Monte Carlo (MCMC) technique is the emergence of MCMC samplers that allow transitions between different models. Such samplers make possible a range of computational tasks involving models, including model selection, model evaluation, model averaging and hypothesis testing. An example of this type of sampler is the reversible jump MCMC sampler, which is a generalization of the Metropolis-Hastings algorithm. Here, we present a new MCMC sampler of this type. The new sampler is a generalization of the Gibbs sampler, but somewhat surprisingly, it also turns out to encompass as particular cases all of the well-known MCMC samplers, including those of Metropolis, Barker, and Hastings. Moreover, the new sampler generalizes the reversible jump MCMC. It therefore appears to be a very general framework for MCMC sampling. This paper describes the new sampler and illustrates its use in three applications in Computational Biology, specifically determination of consensus sequences, phylogenetic inference and delineation of isochores via multiple change-point analysis.