Magmatic fluids in the Breccia-hosted epithermal Au-Ag deposit of Rosia Montana, Romania

The breccia-hosted epithermal Au-Ag deposit of Rosia Montana is located 7 kin northeast of Abrud, in the northern part of the South Apuseni Mountains, Romania. Estimated total reserves of 214.91 million metric toils (Mt) of ore at 1.46 g/t An and 6.9 g/t Ag (10.1 Moz of An and 47.6 Moz of Ag) make Rosia Montana one of the largest gold deposits in Europe. At this location, Miocene calc-alkaline magmatic and hydrothermal activity was associated with local extensional tectonics within a strike-slip regime related to the indentation of the Adriatic microplate into the European plate during the Carpathian orogenesis. The host rocks of the magmatic complex consist of pre-Mesozoic metamorphosed continental crust covered by Cretaceous turbiditic sediment (flysch). Magmatic activity at Rosia Montana and its surroundings occurred in several pulses and lasted about 7 m.y, Rosia Montana is a breccia-hosted epithermal system related to strong phreatomagmatic activity due to the shallow emplacement of the Montana dacite. The Montana dacite intruded Miocene volcaniclastic material (volcaniclastic breccias) and crops out at Cetate and Carnic Hills. Current mining is focused primarily on the Cetate open pit, which was mapped in detail, leading to the recognition of three distinct breccia bodies: the dacite breccia with a dominantly hydrothermal matrix, the gray polymict breccia with a greater proportion of sand-sized matrix support, and the black polymict breccia, which reached to the surface, contains carbonized tree trunks and has a dominantly barren elastic matrix. The hydrothermal alteration is pervasive. Adularia alteration with a phyllic overprint is ubiquitous; silicification and argillic alteration occur locally. Mineralization consists of quartz, adularia, carbonates (commonly Mn-rich), pyrite, Fe-poor sphalerite, galena, chalcopyrite, tetrahedrite, and native gold and occurs as disseminations, as well as in veins and filling vugs within the Montana dacite and the different breccias. The age of mineralization (12.85 +/- 0.07 Ma) was determined by Ar-40- Ar-39 dating on hydrothermal adularia crystals from vugs in the dacite breccia in the Cetate open pit. Microthermometric measurements of fluid inclusions in quartz phenocrysts from the Montana dacite revealed two fluid types that are absent from the hydrothermal breccia and must have been trapped at depth prior to dacite dome emplacement: brine inclusions (32-55 -wt % NaCl equiv, homogenizing at T-h > 460 degrees C) and intermediate density fluids (4.9-15.6 wt % NaCl equiv, T, between 345 degrees-430 degrees C). Secondary aqueous fluid inclusion assemblages in the phenocrysts have salinities of 0.2 to 2.2 wt percent NaCl equiv and T-h of 200 degrees to 280 degrees C. Fluid inclusion assemblages in hydrothermal quartz from breccias and veins have salinities of 0.2 to 3.4 wt percent NaCl equiv and T-h, from 200 degrees to 270 degrees C. The oxygen isotope composition of several zones of an ore-related epithermal quartz crystal indicate a very constant delta O-18 of 4.5 to 5.0 per mil for the mineralizing fluid, despite significant salinity and temperature variation over time. Following microthermometry, selected fluid inclusion assemblages were analyzed by laser ablation-inductively coupled-plasma mass spectrometry (LA-ICMS). Despite systematic differences in salinity between phenocryst-hosted fluids trapped at depth and fluids from quartz in the epithermal breccias, all fluids have overlapping major and trace cation ratios, including identical Na/K/Rb/Sr/Cs/Ba. Consistent with the constant near-magmatic oxygen isotope composition of the hydrothermal fluids, these data strongly indicate a common magmatic component of these chemically conservative solutes in all fluids. Cu, Pb, Zn, and Mn show variations in concentration relative to the relatively non-reactive alkalis, reflecting the precipitation of sulfide minerals together with An in the epithermal breccia, and possibly of Cu in an inferred subjacent porphyry environment. The magmatic-hydrothermal processes responsible for epithermal Au-Ag mineralization at Rosia Montana are, however, not directly related to the formation of the spatially associated porphyry Cu-Au deposit of Rosia Poieni, which occurred lout 3 m.y. later.

Youths carrying a weapon or using a weapon in a fight: what makes the difference?

The objective of this study was to characterize weapon-carrying adolescents and to assess whether weapon carriers differ from weapon users. Data were drawn from a cross-sectional school-based survey of 7548 adolescents aged 16-20 years in Switzerland. Youths carrying a weapon were compared with those who do not. Subsequently, weapon carriers were divided into those who had used it in a fight and those who had not. Individual, family, school and social factors were analyzed using bivariate and stepwise multivariate analysis. For both genders, delinquent behavior and being victim of physical violence were associated with weapon carrying. For males, quarreling while intoxicated, being an apprentice, being sensation seekers, having a tattoo, having a poor relationship with parents and practicing unsafe sex were also related to weapon carrying. Compared with weapon carriers, female weapon users were more likely to be regular smokers. Male weapon users were foreign born, urban and apprentices; had poor school connectedness; practiced unsafe sex and quarreled while intoxicated. Carrying a weapon is a relatively frequent behavior among youths in Switzerland and a sizeable proportion of weapon carriers have used it in a fight. Weapon carrying should be part of the clinical assessment and preventive counseling of adolescents. Preventive programs specific for at-risk youth groups need to be developed.

Report on the Iowa State Civil Rights Commission for the year ended June 30, 2014

Report on the Iowa State Civil Rights Commission for the year ended June 30, 2014

Pediatric drug-related problems: a multicenter study in four French-speaking countries.

BACKGROUND: Pediatric intensive care patients represent a population at high risk for drug-related problems. There are few studies that compare the activity of clinical pharmacists between countries. OBJECTIVE: To describe the drug-related problems identified and interventions by four pharmacists in a pediatric cardiac and intensive care unit. SETTING: Four pediatric centers in France, Quebec, Switzerland and Belgium. METHOD: This was a six-month multicenter, descriptive and prospective study conducted from August 1, 2009 to January 31, 2010. Drug-related problems and clinical interventions were compiled from four pediatric centers in France, Quebec, Switzerland and Belgium. Data on patients, drugs, intervention, documentation, approval and estimated impact were compiled. MAIN OUTCOME MEASURE: Number and type of drug-related problems encountered in a large pediatric inpatient population. RESULTS: A total of 996 interventions were recorded: 238 (24 %) in France, 278 (28 %) in Quebec, 351 (35 %) in Switzerland and 129 (13 %) in Belgium. These interventions targeted 270 patients (median 21 months old, 53 % male): 88 (33 %) in France, 56 (21 %) in Quebec, 57 (21 %) in Switzerland and 69 (26 %) in Belgium. The main drug-related problems were inappropriate administration technique (29 %), untreated indication (25 %) and supra-therapeutic dose (11 %). The pharmacists' interventions were mostly optimizing the mode of administration (22 %), dose adjustment (20 %) and therapeutic monitoring (16 %). The two major drug classes that led to interventions were anti-infectives for systemic use (23 %) and digestive system and metabolism drugs (22 %). Interventions mainly involved residents and all clinical staff (21 %). Among the 878 (88 %) proposed interventions requiring physician approval, 860 (98 %) were accepted. CONCLUSION: This descriptive study illustrates drug-related problems and the ability of clinical pharmacists to identify and resolve them in pediatric intensive care units in four French-speaking countries.

A comparison of pain scales in Thai children.

Three commonly used pain scales, the visual analogue scale, the Wong-Baker Faces Pain Scale, and the Faces Pain Scale Revised were administered to 122 Thai children, of whom half were HIV infected, in order to assess their validity. These scales presented moderate to good correlation and moderate agreement, sufficient for valid use in Thai children.

Measurement of the whole body clearance of infused glycerol as a test of liver function after major hepatectomy.

Major liver resection can be used in the treatment of liver cancer. The functional capacity of liver parenchyma needs to be evaluated preoperatively because it conditions the outcome. We assessed whether the whole body clearance of glycerol, a substrate essentially metabolized in liver cells, may be suitable as a simple test of liver function. Seven patients after major hepatectomy, six patients after colectomy and 12 healthy subjects were studied. Patients were investigated on the first day after surgery. All participants were studied during a 150-min basal period followed by a 120-min infusion of 16 mumol kg-1 min-1 13C-labelled glycerol. Whole body glycerol clearance was calculated from the change in plasma glycerol concentration. Whole body glucose production was measured with 6,6 2H2 glucose infused as a tracer in the basal state and during glycerol infusion. In addition, 13C glucose synthesis was monitored to quantitate gluconeogenesis from glycerol. Patients after liver resection had higher plasma glycerol concentrations and lower whole body glycerol clearance than healthy subjects and patients after colectomy. They also had higher plasma glucagon concentrations. Their fasting glucose production was mildly elevated in the fasting state and did not change after glycerol infusion, indicating a normal hepatic autoregulation of glucose production. These results indicate that whole body glycerol clearance can be simply determined from plasma glycerol concentrations during exogenous glycerol infusion. It is significantly reduced in patients after major hepatectomy, suggesting that it constitutes a sensitive test of hepatic function. Its use as a preoperative testing procedure remains to be evaluated.

Períodos de interferência de plantas daninhas na fase inicial de crescimento do eucalipto

O objetivo deste trabalho foi determinar os períodos de interferência de plantas daninhas no crescimento e desenvolvimento do eucalipto. O experimento foi realizado em campo, de agosto de 2006 a abril de 2008, com plantio de híbrido de Eucalyptus grandis x Eucalyptus urophylla, em delineamento de blocos ao acaso, com três repetições. Os tratamentos consistiram de períodos de convivência e de controle das plantas daninhas com o eucalipto. No tratamento com convivência, a cultura foi mantida em presença de plantas daninhas por intervalos iniciais crescentes de 0, 30, 60, 90, 120, 150, 180, 210, 240, 270, 300, 330 e 360 dias após o transplantio (DAT) do eucalipto. No tratamento controle, o eucalipto foi mantido livre de plantas daninhas, nos mesmos intervalos descritos para a convivência, e as plantas daninhas emergidas após esses intervalos não foram mais controladas. As avaliações foram realizadas aos 360 e aos 630 DAT. A competição com as plantas daninhas causou a redução do diâmetro e da massa de matéria seca de caules e ramos. Medidas de controle das plantas daninhas, no primeiro ano de implantação da cultura do eucalipto, devem ser adotadas ao final do período anterior à interferência, que ocorre aos 107 dias após o transplante da cultura.

1017-011 Tuttle Lake Watershed Final Report

The Tuttle Lake Watershed is approximately 125,000 acres and Tuttle Lake itself is 2,270 acres; 5,609 acres of the watershed lies in Iowa territory within Emmet County. It is a sub-watershed of the larger East Fork Des Moines River Watershed, also referred to as Hydrologic Unit Code 07100003. For the purpose of this document, grant money is only being applied for the project implementation in the Iowa portion of the Tuttle Lake Watershed. Tuttle Lake was placed on the 2002 EPA 303(d) Impaired Waters List due to a “very large population of suspended algae and very high levels of inorganic turbidity.” In 2004, the Iowa Department of Natural Resources (IDNR) completed a Total Maximum Daily Load (TMDL) study on Tuttle Lake and found excess sediment and phosphorus levels being the primary pollutants causing the algae and turbidity impairment. Although two point sources were located in Minnesota, IDNR determined that the influx of nutrients is likely from agricultural runoff and re-suspension of lake sediment. The condition of Tuttle Lake is such that the reduction of sediment, nutrients [phosphorus and nitrogen] and pathogens is the primary objective. To achieve that objective, wetlands will be constructed in this first phase to reduce the delivery of nitrogen, phosphorus, and sediment to Tuttle Lake.

UPLC-TOF-MS for plant metabolomics: a sequential approach for wound marker analysis in Arabidopsis thaliana.

The model plant Arabidopsis thaliana was studied for the search of new metabolites involved in wound signalling. Diverse LC approaches were considered in terms of efficiency and analysis time and a 7-min gradient on a UPLC-TOF-MS system with a short column was chosen for metabolite fingerprinting. This screening step was designed to allow the comparison of a high number of samples over a wide range of time points after stress induction in positive and negative ionisation modes. Thanks to data treatment, clear discrimination was obtained, providing lists of potential stress-induced ions. In a second step, the fingerprinting conditions were transferred to longer column, providing a higher peak capacity able to demonstrate the presence of isomers among the highlighted compounds.

Water stress before harvest of pepper-rosmarin

The objective of this work was to assess the effect of different periods of water stress before harvest of pepper-rosmarin (Lippia sidoides) on the contents of essential oil and flavonoids. The experiment was carried out during 270 days of cultivation, with drainage lysimeters, in a completely randomized block design with five treatments: 0, 2, 4, 6, and 8 days of water suppression before harvest, with four replicates. Fresh and dry matter yield, essential oil content, total flavonoids content, and water potential and temperature of leaves were determined. There was a decrease of approximately 50% in oil content and of 60% in total flavonoid content with the reduction of leaf water potential in 0.3 MPa. Essential oil is more sensitive to water stress than total flavonoids.

Oxidation of methane at the CH4/H2O-(CO2) transition zone in the external part of the Central Alps, Switzerland: Evidence from stable isotope investigations

With the aim of understanding the mechanisms that control the metamorphic transition from the CH4- to the H2O-(CO2)-dominated fluid zone in the Helvetic domain of the Central Alps of Switzerland, fluid inclusions in quartz, illite ``crystallinity'' index, vitrinite reflectance, and the stable isotope compositions of vein and whole rock minerals and fluids trapped in quartz were investigated along four cross-sections. Increasing temperature during prograde metamorphism led to the formation of dry gas by hydrocarbon cracking in the CH4-zone. Fluid immiscibility in the H2O-CH4-(CO2)-NaCl system resulted in cogenetic, CH4- and H2O-dominated fluid inclusions. In the CH4-zone, fluids were trapped at temperatures <= 270 +/- 5 degrees C. The end of the CH4-zone is markedby a sudden increase of CO2 content in the gas phase of fluid inclusions. At temperatures > 270 +/- 5 degrees C, in the H2O-zone, the total amount of volatiles within the fluid decreased below 1 mol% with no immiscibility. This resulted m total homogenization temperatures of H2O-(CO2-CH4)-NaCl inclusions below 180 degrees C. Hydrogen isotope compositions of methane in fluid inclusion have delta D values of less than -100 parts per thousand in the CH4-zone, typical for an origin through cracking of higher hydrocarbons, but where the methane has not equilibrated with the pore water. delta D values of fluid inclusion water are around -40 parts per thousand., in isotopic equilibrium with phyllosilicates of the whole rocks. Within the CH4 to H2O(CO2) transition zone, delta D(H2O) values in fluid inclusions decrease to -130 parts per thousand interpreted to reflect the contribution of deuterium depleted water from methane oxidation. In the H2O-zone, delta D(H2O) values increase again towards an average of -30 parts per thousand which is again consistent with isotopic equilibrium with host-rock phyllosilicates. delta C-13 values of methane in fluid inclusions from the CH4-zone are around -27 parts per thousand in isotopic equilibrium with calcite in veins and whole rocks. The delta C-13(CH4) values decrease to less than -35 parts per thousand at the transition to the H2O-zone and are no longer in equilibrium with the carbonates in the whole rocks. delta C-13 values of CO, are variable but too low to be in equilibrium with the wall rock fluids, compatible with a contribution of CO2 from closed system oxidation of methane. Differences in isotopic composition between host-rock and Alpine fissure carbonate are generally small, suggesting that the amount of CO2 produced by oxidation of methane was small compared to the C-budget in the rocks and local pore fluids were buffered by the wall rocks during precipitation of calcite within the fissures. (c) 2006 Elsevier B.V. All rights reserved.

Le Roman de Renart

F. 1-48. Le Roman de Renart. Le manuscrit, qui a été doté du sigle O dans les différentes éditions, est incomplet de la fin et mixte, proposant une structure relativement inédite. Il a récemment fait l’objet d’une édition critique par Aurélie Barre : Édition critique et littéraire du manuscrit O du « Roman de Renart » ( f. fr. 12583), doctorat, Université Lyon III, 2005. F. 1a-14b. Branche I.F. 1a-7e. [Branche Ia : « Le jugement de Renart »]. « Pierres qui son enging et s’art / Mist es vers faire de Renart…-… Tant qu’il [re]fu en sa santé / Com il avoit devant esté ». – F. 7e-10b. [Branche Ib : « Le Siège de Maupertuis »]. « Messires Nobles l’empereres / Vint au chastel ou Renart ere …-… Et Renart ainsi s’en eschape, / Des or gart bien chascun sa chape ! ». – F. 10b-14b. [Branche Ic : « Renart teinturier, Renart jongleur »]. « Li rois a fait son ban crier, / Par tout plevir et afier …-… Puis fu Renart lonc tens en mue ; / Ne va, ne vient, ne se remue » (éd. Barre, p.117-233, v. 1-3217). . F. 14b-20bBranche II. F. 14b-20b. [Branche II : « Le duel judiciaire »]. « Messires Nobles li lions / O lui avoit toz ses barons …-… Et autre redirai aprés, / A itant de cestui vos lés » (éd. Barre, p. 235-289, v. 1-1522). F. 20b-25c. Branche III.F. 20b-22a. [Branche IIIa : « Renart et Chantecler »]. « Seignors, oï avez maint conte, / Que maint contierres vos aconte …-… Dou coc qui li est eschapez, / Quant il ne s’en est saoulez ». – F. 22a-22f. [Branche IIIb : « Renart et la mésange »]. « Que que cil se plaint et demente, / Atant es vos une mesenge …-… Assez a grant travail eü / de ce dont li est mescheü ». – F. 22f-23c. [Branche IIIc. « Renart et Tibert »]. « Que qu’il se plaint de s’aventure, / Qui li avient et pesme et dure …-… Tornez s’en est a mout grant paine …-… Si com aventure le maine ». – F. 23c-24e. [Branche IIId : « Renart et l’andouille »]. «Renart qui mout sot de treslüe, / Et qui mout ot grant fain eüe …-… Esfondree ert entr’eus la guerre, / Mes ne velt trive ne pes querre ». – F. 24e-25c. [Branche IIIe : « Tibert et les deux prêtres »]. « Thibert li chaz, dont je a dit, / Doute Renart assez petit …-… Qui touz nos a enfantosmez : / A paine en sui vis eschapez ! » (éd. Barre, p. 291-340, v. 1-1265). F. 25c-27d. Branche IV. F. 25c-26a. [Branche IVa : « Renart et Tiercelin »]. « Entre .II. mons, en une plangne / Tout droit au pié d’une montaigne …-… Fuiant s’en va les sauz menuz : / Ses anemis a confonduz ». – F. 26a-27d. [Branche IVb : « Le viol d’Hersent »]. « Cis plaiz fu ainsi deffinez / Et Renars s’est acheminez …-… Et est venuz a sa mesnie / Qui soz la roche est entasnie » (éd. Barre, p. 341-359, v. 1-524). F. 27d-29d. Branche V. [« Renart et les anguilles »]. « Seignors, ce fu en cest termine / Que li douz tens d’esté decline …-…Que de Renart se vengera / Ne jamés jor ne l’amera » (éd. Barre, p. 361-378, v. 1-514). F. 29d-31e. Branche VI. [« Le puits »]. « Prime covient tel chose dire / Dont je vos puisse faire rire …-… Et il le puet prandre en sa marge, / Sachiez qu’i li fera domage ! » (éd. Barre, p. 379-396, v. 1-537).. 31e-39c. Branche VII. F. 31e-32e. [Branche VIIa : « Le jambon enlevé »]. « [U]n jour issit hors de la lande / Isengrins por querre viande …-… .XV. jours va a grant baudour, / Onques Renars n’i fist sejour ». – F. 32c-32e. [Branche VIIb : « Renart et le grillon »]. « Renart s’en va tout son chemin. / Or veut (en) engignier Isengrin …-… Tornez s’en est grant aleüre / Et vet aillors querre droiture ». – F. 32e-36e. [Branche VIIc : « L’Escondit »]. « Atant s’apense d’une chose / Dont il sa fame sovent chose …-…Tant defoulé et tant batu / Qu’a Malpertuis l’ont enbatu ». – F. 36e-39c. [Branche VIId : « La confession de Renart »]. « Foux est qui croit sa male pense : / Mout remaint de ce que fox panse …-…L’escofle lor donne a mengier, / Qu’il en avoient grant mestier (éd. Barre, p. 397-470, v. 1-1960). F. 36c-48e. Branche VIII. [« Renart et Liétart »]. « Uns prestres de la Croiz en Brie, / Que Damediex doint bone vie …-… Ou au chiés ou a la parclose, / Qui n’est aüsés de la chose » (éd. Barre, p. 471-554, v. 1-2470). F. 48e. Branche IX (v. 1-86). [« Les Vêpres de Tibert »]. « Oiez une novele estoire / Qui bien doit estre en mémoire …-… Jel conterai a Hameline, / La foi et la reconnoissance… » (éd. Barre, p. 555-557, v. 1-85).