Constraints on the thermal evolution of the Adriatic margin during Jurassic continental break-up: U–Pb dating of rutile from the Ivrea–Verbano Zone, Italy

The Ivrea–Verbano Zone (IVZ), northern Italy, exposes an attenuated section through the Permian lower crust that records high-temperature metamorphism under lower crustal conditions and a protracted history of extension and exhumation associated partly with the Jurassic opening of the Alpine Tethys ocean. This study presents SHRIMP U–Pb geochronology of rutile from seven granulite facies metapelites from the base of the IVZ, collected from locations spanning ~35 km along the strike of Paleozoic fabrics. Rutile crystallised during Permian high-temperature metamorphism and anatexis, yet all samples give Jurassic rutile U–Pb ages that record cooling through 650–550 °C. Rutile age distributions are dominated by a peak at ~160 Ma, with a subordinate peak at ~175 Ma. Both ~160 and ~175 Ma age populations show excellent agreement between samples, indicating that the two distinctive cooling stages they record were synchronous on a regional scale. The ~175 Ma population is interpreted to record cooling in the footwall of rift-related faults and shear zones, for which widespread activity in the Lower Jurassic has been documented along the western margin of the Adriatic plate. The ~160 Ma age population postdates the activity of all known rift-related structures within the Adriatic margin, but coincides with extensive gabbroic magmatism and exhumation of sub-continental mantle to the floor of the Alpine Tethys, west of the Ivrea Zone. We propose that this ~160 Ma early post-rift age population records regional cooling following episodic heating of the distal Adriatic margin, likely related to extreme lithospheric thinning and associated advection of the asthenosphere to shallow levels. The partial preservation of the ~175 Ma age cluster suggests that the post-rift (~160 Ma) heating pulse was of short duration. The regional consistency of the data presented here, which is in contrast to many other thermochronometers in the IVZ, demonstrates the value of the rutile U–Pb technique for probing the thermal evolution of high-grade metamorphic terrains. In the IVZ, a significant decoupling between Zr-in-rutile temperatures and U–Pb ages of rutile is observed, with the two systems recording events ~120 Ma apart.

"Citizenship Lite" revisited

In a small book and article published in 2010, I argued that citizenship in the West was undergoing a process of "lightening": it has become easier to obtain, connotes fewer rights exclusively attached to it, and is capped by thin and thinning identities. In my presentation, I review the `citizenship lite` hypothesis in light of recent trends and scholarship.

Analysis of Synthetic Diamond Wafer Interferograms Using a Parallelized Simulated Annealing Algorithm

Diamonds are known for both their beauty and their durability. Jefferson National Lab in Newport News, VA has found a way to utilize the diamond's strength to view the beauty of the inside of the atomic nucleus with the hopes of finding exotic forms of matter. By firing very fast electrons at a diamond sheet no thicker than a human hair, high energy particles of light known as photons are produced with a high degree of polarization that can illuminate the constituents of the nucleus known as quarks. The University of Connecticut Nuclear Physics group has responsibility for crafting these extremely thin, high quality diamond wafers. These wafers must be cut from larger stones that are about the size of a human finger, and then carefully machined down to the final thickness. The thinning of these diamonds is extremely challenging, as the diamond's greatest strength also becomes its greatest weakness. The Connecticut Nuclear Physics group has developed a novel technique to assist industrial partners in assessing the quality of the final machining steps, using a technique based on laser interferometry. The images of the diamond surface produced by the interferometer encode the thickness and shape of the diamond surface in a complex way that requires detailed analysis to extract. We have developed a novel software application to analyze these images based on the method of simulated annealing. Being able to image the surface of these diamonds without requiring costly X-ray diffraction measurements allows rapid feedback to the industrial partners as they refine their thinning techniques. Thus, by utilizing a material found to be beautiful by many, the beauty of nature can be brought more clearly into view.

Stand Structure Governs the Crown Collisions of Lodgepole Pine

We investigated tree sway and crown collision behavior of even-aged lodgepole pine (Pinus contorta Dougl. ex Loud. var. latifolia Engelm.) stands of different structure in Alberta, Canada, to examine how these factors might affect loss of leaf area as stands mature. The Two Creeks stand (TC) had high density and slender trees, while the Chickadee stand (CH) had stout trees. The TC stand was then thinned (TCT) to reduce the stand density. For each stand, simultaneous tree sways of a group of 10 trees were monitored with biaxial clinometers during wind speed of 5 m/s (canopy top). Crown collisions were reconstructed by combining sway displacement of individual trees with their respective crown dimensions. Comparing the sway statistics between stands with contrasting mean bole slenderness (TC and CH) indicated that more slender trees have greater sway displacements, faster sway speeds, and a greater depth of collision. Disturbance by thinning increased sway displacements, sway speeds, and depth of collisions at TCT. Tree sway patterns were circular in shape and not aligned with wind direction, but patterns were elongated after thinning. This demonstrates the high frequency of crown collision experienced by stands with slender trees and supports the notion that crown collisions result in empty space between crowns of trees.

A conditional Mdm2 allele shows the importance of Mdm2 in heart development

Over 50% of sporadic tumors in humans have a p53 mutation highlighting its importance as a tumor suppressor. Considering additional mutations in other genes involved in p53 pathways, every tumor probably has mutant p53 or impaired p53-mediated functions. In response to a variety of cellular and genotoxic stresses, p53, mainly through its transcriptional activity, induces pathways involved in apoptosis and growth arrest. In these circumstances and under normal situations, p53 must be tightly regulated. Mdm2 is an important regulator of p53. Mdm2 inhibits p53 function by binding and blocking its transactivation domain. In addition, Mdm2 helps target p53 for degradation through its E3 ligase activity. Mdm2 null mice are embryonic lethal due to apoptosis in the blastocysts. However, a p53 null background rescues this lethality demonstrating the importance of the p53-Mdm2 interaction, particularly during development. The lethality of the Mdm2 null mouse prior to implantation limits the ability to investigate the role of Mdm2 in regulating p53 in a temporal and tissue specific manner. Does p53 need to be regulated in all tissues throughout the life of a mouse? Does Mdm2 always have to regulate it? To address these questions, we created a conditional Mdm2 allele. The conditional allele, Mdm2FM, in the presence of Cre recombinase results in the deletion of exons 5 and 6 of Mdm2 (most of the p53 binding domain) and represents a null allele. ^ The Mdm2FM allele was crossed with a heart muscle specific Cre expressing mouse (α-myosin heavy chain promoter driven Cre) to ask whether Mdm2 acts as a negative regulator of p53 in the heart. The heart is the most prominent organ early in embryogenesis and is shaped by cell death and proliferation. p53 does not appear to be active in the heart in response to some types of stress, so it remained to be determined if it has to be regulated in normal heart development. Loss of Mdm2 in the heart results in heart defects as early as E9.5. Loss of Mdm2 results in stabilized p53 and apoptosis. This apoptosis leads to a thinning of the myocardial wall particularly in the ventricles and abnormal ventricular structure. Eventually the abnormal heart fails resulting in lethality by E13.5. The embryonic lethality is rescued in a p53 null background. Thus, Mdm2 is important in regulating p53 in the development of the heart. ^

Abnormal expression of E2F1 and E2F4 results in hyperproliferation of the ependyma and lethal hydrocephalus

The proliferative role of E2F has been under investigation for several years. However, while it is known that E2F1 and E2F4 play a part in development and differentiation, research has not been centered on determining the exact functions these E2Fs play in brain development, given there high expression levels throughout embryogenesis. A GFAP-E2F1 mouse model directing human E2F1 transgene expression to glial cells, such as ependymal cells, was used in the present study in combination with an E2F4 mutant mouse model. Interestingly, 20% of tgE2F1; E2F4 null mice developed a phenotype consisting of domed head, hunched posture, seizures, tremors, hyperactivity or hypeactivity, dysnea, and low body weight. These mice died during the first three weeks of severe hydrocephalus. Similarly, tgE2F1; E2F4 heterozygous mice also develop severe hydrocephalus, although this occurs at 6 weeks at a 2% frequency. Pathological examination of the brains of those animals uncovered enlarged cerebral ventricles with marked thinning of the cerebral cortices, confirming the diagnosis of three-ventricle hydrocephalus, and the absence of tumors. Careful examination of the aqueduct shows an excess of proliferating cells that may cause a blockage of CSF. Of significance, 44% of ependymal cells in hydrocephalic tgE2F1;E2F4-/- mouse brains were positive for BrdU incorporation. Studies determining the molecular rationale for the hydrocephalic phenotype suggest proliferative ependymal cells may not be exclusively related to dysregulated cell cycle in conjuction with E2F activity. Due in part to the deficiency of E2F4 in this mouse model, we find that differentiation of these ependymal cells is not complete and instead undergoes maturation arrest. This suggestion is confirmed by the expression of genes found in neural stem cells or precursor cell populations, in the ependymal cell region of tgE2F1; E2F4-/-. Therefore, from this study, we conclude that dysregulated E2F1 expression in combination with deficient E2F4 expression results in an undifferentiated ependymal cell population that is hyperproliferative in the ventricular system causing an impediment of CSF circulation. It is further concluded that normal E2F1 and E2F4 expression in brain development is crucial for the proper formation and function of the ventricular system.^

Heavy mineral content of ODP Leg 107 holes

Analyses of rock clasts and of heavy minerals in upper Miocene coarse detrital units drilled along the East Sardinia passive-type continental margin (Sites 654, 653, 652, and 656) reveal that the stretched basement contains quite complex rock suites. Taking also into account previous sampling data, in moving from west to east across the margin, the nature of the basement changes drastically. To the west there are mostly Hercynian basement rocks with their cover, referable to the alpine foreland of the Corsica-Sardinia block. To the east, along the lower margin, where crustal thinning is quite severe, the basement contains rock suites referable to a pre-upper Tortonian orogenized zone with units constituting parts of the Alpine and Apenninic chains (presumably with thickened continental crust prior to stretching). Largest thinning and ocean forming occurred then, in a rather short time, mostly at the expense of unstable crust just thickened by orogenetic/tectogenetic processes.

Ice and snow measurements during Nathaniel B. Palmer cruise NBP0709 (SIMBA experiment)

The Sea Ice Mass Balance in the Antarctic (SIMBA) experiment was conducted from the RVIB N.B. Palmer in September and October 2007 in the Bellingshausen Sea in an area recently experiencing considerable changes in both climate and sea ice cover. Snow and ice properties were observed at 3 short-term stations and a 27-day drift station (Ice Station Belgica, ISB) during the winter-spring transition. Repeat measurements were performed on sea ice and snow cover at 5 ISB sites, each having different physical characteristics, with mean ice (snow) thicknesses varying from 0.6 m (0.1 m) to 2.3 m (0.7 m). Ice cores retrieved every five days from 2 sites and measured for physical, biological, and chemical properties. Three ice mass-balance buoys (IMBs) provided continuous records of snow and ice thickness and temperature. Meteorological conditions changed from warm fronts with high winds and precipitation followed by cold and calm periods through four cycles during ISB. The snow cover regulated temperature flux and controlled the physical regime in which sea ice morphology changed. Level thin ice areas had little snow accumulation and experienced greater thermal fluctuations resulting in brine salinity and volume changes, and winter maximum thermodynamic growth of ~0.6 m in this region. Flooding and snow-ice formation occurred during cold spells in ice and snow of intermediate thickness. In contrast, little snow-ice formed in flooded areas with thicker ice and snow cover, instead nearly isothermal, highly permeable ice persisted. In spring, short-lived cold air episodes did not effectively penetrate the sea ice nor overcome the effect of ocean heat flux, thus favoring net ice thinning from bottom melt over ice thickening from snow-ice growth, in all cases. These warm ice conditions were consistent with regional remote sensing observations of earlier ice breakup and a shorter sea ice season, more recently observed in the Bellingshausen Sea.

Varved sediments of the Arabian Sea

The upper Holocene marine section from a kasten core taken from the oxygen minimum zone off Karachi (Pakistan) at water depth 700 m contains continuously laminated sediments with a sedimentation rate of 1.2 mm/yr and a unique record of monsoonal climatic variability covering the past 5000 years. Our chronostratigraphy is based on varve counts verified by conventional and AMS14C dating. Individual hemipelagic varve couplets are about 0.8-1.5 mm thick, with light-colored terrigenous laminae (A) deposited mainly during the winter monsoon alternating with dark-colored laminae (B) rich in marine organic matter, coccoliths, and fish debris that reflect deposition during the high-productivity season of the late summer monsoon (August-October). Precipitation and river runoff appear to control varve thickness and turbidite frequency. We infer that precipitation decreased in the river watershed (indicated by thinning varves) after 3500-4000 yr B.P. This is about the time of increasing aridification in the Near East and Middle East, as documented by decreasing Nile River runoff data and lake-level lowstands between Turkey and northwestern India. This precipitation pattern continued until today with precipitation minima about 2200-1900 yr B.P., 1000 yr B.P., and in the late Middle Ages (700-400 yr B.P.), and precipitation maxima in the intervening periods. As documented by spectral analysis, the thickness of varve couplets responds to the average length of a 250-yr cycle, a 125-yr cycle, the Gleissberg cycle of solar activity (95 yr), and a 56-yr cycle of unknown origin. Higher frequency cycles are also present at 45, 39, 29-31, and 14 yr. The sedimentary gray-value also shows strong variability in the 55-yr band plus a 31-yr cycle. Because high-frequency cyclicity in the ENSO band (ca. 3.5 and 5 yr) is only weakly expressed, our data do not support a straightforward interaction of the Pacific ENSO with the monsoon-driven climate system of the Arabian Sea.

Raleo de racimos en Vitis Vinifera Cv. Malbec : efecto sobre los componentes del rendimiento y la composición polifenólica de las bayas

En Mendoza es cada vez más común ralear racimos con el propósito de afectar la composición de las uvas. No obstante, el conocimiento local sobre cómo lograr un equilibrio adecuado de los distintos atributos de calidad mediante el raleo es escaso. El objetivo de esta investigación fue evaluar la relación entre el raleo de racimos en diferentes intensidades y épocas, y los componentes del rendimiento y la composición fenólica de la uva. Para este estudio, que se realizó en un viñedo de Agrelo, Luján de Cuyo, Mendoza (Argentina), se eligió la cultivar Malbec por ser el cepaje emblemático de Argentina y el típico de la Denominación de Origen Controlado (DOC) Luján de Cuyo. En las plantas de dicha cultivar, conducidas en espaldero alto y podadas en cordón Royat bilateral, el raleo fue manual, en tres momentos del ciclo: 1) cuando los granos tenían el tamaño de una arveja; 2) en envero y 3) a 21 °Brix. La intensidad de raleo fue de 25 y 50 % de los racimos. Se comprobó la hipótesis planteada en relación con que el raleo aumenta el tamaño de la baya y mejora la calidad de la uva, por cuanto incrementa la biosíntesis de los polifenoles. En los componentes del rendimiento aumenta el peso del racimo y el tamaño de la baya cuando el raleo se hace temprano y con una intensidad elevada. En cuanto a la influencia en la biosíntesis de los polifenoles se demuestra que el raleo temprano e intenso mejora la concentración de antocianas, catequinas y proantocianidinas. La concentración azucarina se vio incrementada cuando el raleo se hizo en envero y fue intenso.

La época de raleo como factor de rentabilidad en duraznos conserveros de maduración temprana

Del total de la superficie implantada con duraznos conserveros en la provincia de Mendoza, el 27% corresponde a cultivares de maduración temprana, en los que el raleo de frutos es un factor crítico de manejo. Para determinar la incidencia de diferentes épocas de raleo sobre la rentabilidad del cultivo se realizó un ensayo en un monte comercial de durazneros cvs. Fortuna y Carson. Se utilizaron árboles injertados sobre portainjerto Nemaguard, conducidos en vaso tipo californiano e implantados a 6 m entre hileras y a 5 m entre plantas, que fueron raleados en tres épocas diferentes: a los 40 días después de plena floración, en inicio de endurecimiento de carozo y 10 días después, en la fecha de referencia. Se realizaron evaluaciones de producción por planta y calidad de frutos. También se determinó el valor de la producción y la relación entre éste y las distintas fechas de raleo. En ambos cultivares, los árboles raleados en época temprana obtuvieron mayor peso de frutos, producción total y producción destinada a mitades. En el cv. Fortuna, este tratamiento produjo un aumento significativo del porcentaje de frutos con carozo partido.El raleo temprano de frutos aumentó significativamente el valor de la cosecha, logrando un incremento de $ 3636.ha-1 y $ 3441.ha-1en los cvs. Fortuna y Carson, respectivamente, en relación con el tratamiento en fecha de referencia.

Raleo de frutos en kiwi

Durante la temporada 1999-2000 un lote de plantas de kiwi (Actinidia deliciosa (A. Chev.) C. F. Liang et A. R. Ferguson var. deliciosa cv Hayward) fue sometido a tres intensidades de raleo: 30, 40 y 50 frutos/m2 a los 19 días post-floración. Se evaluó la calidad de los frutos desarrollados en 3 tipos de ramificación lateral: fuerte, medio y débil. Se registró la evolución del crecimiento del fruto. Se determinó peso, contenido de sólidos solubles, firmeza de la pulpa y pH del jugo al momento de cosecha. • Las intensidades de raleo de 30, 40 y 50 frutos/m2 produjeron frutos de peso promedio 125, 121 y 113 g respectivamente. En los tres casos se superó el peso mínimo exigido para exportación. • Los laterales de tipo débil produjeron los frutos de menor peso y más blandos a cosecha. No se encontraron diferencias entre laterales en contenido de sólidos solubles y pH. • Los raleos intensos favorecieron la tasa de crecimiento del fruto pero la mayor intensidad de raleo (30 frutos/m2) comprometió el rendimiento del cultivo.