Nannofossil biostratigraphy of ODP Hole 206-1256B sediments

Site 1256 of Ocean Drilling Program Leg 206 to the Guatemala Basin on the eastern flank of the East Pacific Rise yielded a near-complete, middle Miocene-Quaternary carbonate-rich section that provides an opportunity to study low-latitude biostratigraphic and paleoceanographic events. The sedimentary sequence in Hole 1256B has been zoned using calcareous nannofossils according to the biostratigraphic schemes by Martini of 1971 (modified by Martini and Müller in 1986) and Okada and Bukry of 1980. The nannofossil assemblage is characteristic of the low latitudes, with abundant Gephyrocapsa, Discoaster, and Sphenolithus, and is in general moderately to well preserved, depending on nannofossil abundance and the presence of diatoms. Age estimates for the first occurrence and last occurrence of Reticulofenestra rotaria were derived from biostratigraphy and magnetostratigraphy independently and assigned to 7.18 and 6.32 Ma, respectively. Linear sedimentation rates, calculated using 28 nannofossil datums and age estimates, are high in the middle Miocene, decrease from the late Miocene to the Pliocene, then increase upsection. The abrupt drop in carbonate mass accumulation rates during the early late Miocene is referred to as the "carbonate crash." This pattern reflects (1) the long-trend decrease of productivity as the site moves away from the upwelling system at the equatorial divergence as well as (2) fluctuation in the chemistry of the bottom waters associated with production of the North Atlantic Bottom Water and ventilation via the Panama Gateway. A basement age of 14.5 Ma was obtained by extrapolating the 39.1-m/m.y. rate in the middle Miocene to the basement at 250.7 meters below seafloor, and is consistent with the ~15-Ma age of the oceanic crust estimated from marine magnetic anomalies. Reworked nannofossils and lithologic changes were used to unravel postdepositional history, and three episodes were recognized, one of which in the latest Miocene can be widely correlated.

K-Ar age and chemical composition of volcanites from the Sea of Okhotsk

Volcanogenic rocks from the Sea of Okhotsk are divided into seven age complexes: Late Jurassic, Early Cretaceous, Late Cretaceous, Eocene, Late Oligocene, Late Miocene, and Pliocene-Pleistocene. All these complexes are united into two groups - Late Mesozoic and Cenozoic. Each group reflects a certain stage of development of the Sea of Okhotsk region. Late Mesozoic volcanites build the geological basement of the Sea of Okhotsk, and their petrochemical features are similar to those of the volcanic rocks from the Okhotsk-Chukotka Volcanogen. Pliocene-Pleistocene volcanites reflect stages of tectono-magmatic activity; the latter destroyed the continental margin and produced riftogenic troughs. Geochemical features of volcanites from the Sea of Okhotsk indicate influence of the sialic crust on magma formation and testify formation of the Okhotsk Sea Basin on the destructive margin of the Asian continent.

Nonlinear and Scaling Processes in Hydrology and Soil Science

Hydrology is the study of the properties, distribution and effects of water on the Earth?s soil, rocks and atmosphere. It also encompasses the study of the hydrologic cycle of precipitation, runoff, infiltration, storage, and evaporation, including the physical, biological and chemical reaction of water with the earth and its relation to life?.

Mechanical behavior and residual stress field of dissimilar laser welded joints

The present investigation addresses the mechanical behavior and residual stress field of dissimilar joints produced by laser welding. Microstructure characterization and residual strain scanning, carried out by neutron diffraction, were used to assess the joints features. It was found that the heat source position influences the base metals dilution and the residual stress field associated to the welding process. The tensile behavior of the joint, different zones achieved by using a video-image based system (VIC-2D) reveals that the residual stress field, together with the positive difference in yield between the weld metal and the base materials protects the joint from being plastically deformed.

Fracture micromechanisms and residual stresses of a highly resistant duplex stainless steel

The paper presents some preliminary results of an ongoing research intended to qualify a highly resistant duplex stainless steel wire as prestressing steel and, gets on insight on (he wires' fracture micromechanism and residual stresses field. SEM fractographic analysis of the stainless steel wires indicates an anisotropic fracture behavior in tension, in presence of surface flaws, attributed to the residual stresses generated through the fabrication process. The residual stresses magnitude influences the damage tolerance, its knowledge being a key issue in designating/qualifying the wires as prestressing steels.

Detecção de DNA de HPV no plasma para potencial identificação precoce de recidiva de câncer do colo de útero

O câncer do colo do útero constitui a terceira neoplasia maligna mais comum na população feminina, com aproximadamente 520 mil novos casos e 260 mil óbitos por ano e origina-se a partir da infecção genital persistente pelo Papiloma Vírus Humano (HPV) oncogênico. Os principais HPVs considerados de alto risco oncogênico são os tipos HPV-16 e 18, responsáveis por cerca de 70% de todos os casos de cânceres cervicais (CC) no mundo. Pacientes com CC apresentam taxa de recidiva variando de 8% a 49%. Dentro de dois anos de seguimento, 62% a 89% das recidivas são detectadas. Atualmente, os testes usados para detecção de recidiva são a citopatologia da cúpula vaginal e exames de imagem, porém ainda não estão disponíveis testes específicos. O DNA livre-circulante (cf-DNA) representa um biomarcador não-invasivo facilmente obtido no plasma e soro. Vários estudos mostram ser possível detectar e quantificar ácidos nucléicos no plasma de pacientes com câncer e que as alterações no cfDNA potencialmente refletem mudanças que ocorrem durante a tumorigênese. Essa ferramenta diagnóstica não-invasiva pode ser útil no rastreio, prognóstico e monitoramento da resposta ao tratamento do câncer. Portanto, o desenvolvimento e a padronização de testes laboratoriais não invasivos capazes de identificar marcadores tumorais e diagnosticar precocemente a recidiva da doença aumentam a chance de cura através da utilização dos tratamentos preconizados. Sendo assim, este estudo tem o objetivo de detectar o DNA de HPV no plasma de pacientes com CC para avaliar sua potencial utilidade como marcador precoce de recidiva. Um fragmento de tumor e sangue de pacientes com CC, atendidas no ICESP e HC de Barretos, foram coletados antes do tratamento. Entraram no estudo 137 pacientes nas quais o tumor foi positivo para HPV-16 ou 18, sendo 120 amostras positivas para HPV-16 (87,6%), 12 positivas para HPV-18 (8,8%) e cinco positivas para HPV-16 e 18 (3,6%). A média de idade das pacientes deste estudo foi de 52,5 anos. Plasma de 131 pacientes com CC da data do diagnóstico e de 110 pacientes do seguimento foram submetidas ao PCR em Tempo Real HPV tipo específico. A presença do DNA de HPV no plasma pré-tratamento foi observada em 58,8% (77/131) com carga viral variando de 204 cópias/mL a 2.500.000 cópias/mL. A positividade de DNA no plasma pré-tratamento aumentou com o estadio clínico do tumor: I - 45,2%, II - 52,5%, III - 80,0% e IV - 76,9%, (p=0,0189). A presença do DNA de HPV no plasma pós-tratamento foi observada em 27,3% (30/110). A média de tempo das recidivas foi de 3,1 anos (2,7 - 3,5 anos). O DNA de HPV foi positivo até 460 dias antes do diagnóstico clínico da recidiva. As pacientes com DNA de HPV no plasma apresentaram pior prognóstico, tanto sobrevida como o tempo livre de doença, em relação às que foram negativas. Nas pacientes com CC a presença de HPV no plasma de seguimento pode ser um marcador precoce útil para o monitoramento da resposta terapêutica e detecção de pacientes com risco aumentado de recidiva e progressão da doença.

Tercüme-yi Sıhahu'l-Cevherî

[tercüme eden] Mehmet bin Mustafa el-Vanî.

Corrélats neuronaux de la mémoire de travail en magnétoencéphalographie à l’état de repos

Purpose: There are few studies demonstrating the link between neural oscillations in magnetoencephalography (MEG) at rest and cognitive performance. Working memory is one of the most studied cognitive processes and is the ability to manipulate information on items kept in short-term memory. Heister & al. (2013) showed correlation patterns between brain oscillations at rest in MEG and performance in a working memory task (n-back). These authors showed that delta/theta activity in fronto-parietal areas is related to working memory performance. In this study, we use resting state MEG oscillations to validate these correlations with both of verbal (VWM) and spatial (SWM) working memory, and test their specificity in comparison with other cognitive abilities. Methods: We recorded resting state MEG and used clinical neuropsychological tests to assess working memory performance in 18 volunteers (6 males and 12 females). The other neuropsychological tests of the WAIS-IV were used as control tests to assess the specificity of the correlation patterns with working memory. We calculated means of Power Spectrum Density for different frequency bands (delta, 1-4Hz; theta, 4-8Hz; alpha, 8-13Hz; beta, 13-30Hz; gamma1, 30-59Hz; gamma2, 61-90Hz; gamma3, 90-120Hz; large gamma, 30-120Hz) and correlated MEG power normalised for the maximum in each frequency band at the sensor level with working memory performance. We then grouped the sensors showing a significant correlation by using a cluster algorithm. Results: We found positive correlations between both types of working memory performance and clusters in the bilateral posterior and right fronto-temporal regions for the delta band (r2 =0.73), in the fronto-middle line and right temporal regions for the theta band (r2 =0.63) as well as in the parietal regions for the alpha band (r2 =0.78). Verbal working memory and spatial working memory share a common fronto-parietal cluster of sensors but also show specific clusters. These clusters are specific to working memory, as compared to those obtained for other cognitive abilities and right posterior parietal areas, specially in slow frequencies, appear to be specific to working memory process. Conclusions: Slow frequencies (1-13Hz) but more precisely in delta/theta bands (1-8Hz), recorded at rest with magnetoencephalography, predict working memory performance and support the role of a fronto-parietal network in working memory.

(Table 1) Mean grain sizes and standard deviations of gas hydrate samples

Methane hydrates are present in marine seep systems and occur within the gas hydrate stability zone. Very little is known about their crystallite sizes and size distributions because they are notoriously difficult to measure. Crystal size distributions are usually considered as one of the key petrophysical parameters because they influence mechanical properties and possible compositional changes, which may occur with changing environmental conditions. Variations in grain size are relevant for gas substitution in natural hydrates by replacing CH4 with CO2 for the purpose of carbon dioxide sequestration. Here we show that crystallite sizes of gas hydrates from some locations in the Indian Ocean, Gulf of Mexico and Black Sea are in the range of 200-400 µm; larger values were obtained for deeper-buried samples from ODP Leg 204. The crystallite sizes show generally a log-normal distribution and appear to vary sometimes rapidly with location.

Musique de chambre pour piano seul.

For piano; originally for various combinations of instruments.

Quatuors für 2 Violinen, Viola und Violoncell /

Each part paged continuously.

Faune de France : contenant la description des espèces indigèns disposées en tableaux analytiques ; et illustrée de figures représentant les types caractéristiques des genres /

Ink stamps in v.3 "Property of Z.P. Metcalf".