Características químicas do solo sob algodoeiro em área que recebeu água residuária da suinocultura

A crescente geração de efluentes líquidos e o seu lançamento no meio ambiente tem-se constituído numa preocupação mundial devido aos impactos negativos gerados. O objetivo deste trabalho foi avaliar os possíveis impactos da aplicação do efluente proveniente da suinocultura, após seu tratamento, nos atributos químicos do solo, em área cultivada com algodão. O experimento foi realizado no Perímetro Irrigado Formoso, no município de Bom Jesus da Lapa, BA, em área experimental da Companhia de Desenvolvimento dos Vales do São Francisco e do Parnaíba - CODEVASF. Foram testados cinco tratamentos: MC - manejo convencional = água de "boa qualidade" + adubação química; ET100 = 100 % de efluente tratado; ET75:25 = 75 % de efluente tratado + 25 % de água boa; ET50:50 = 50 % de efluente tratado + 50 % de água boa; ET25:75 = 25 % de efluente tratado + 75 % de água boa. O delineamento experimental foi em blocos ao acaso com quatro repetições. Os atributos químicos do solo avaliados foram: pH, condutividade elétrica, teores de N, P, K, Ca, Mg, Na, Zn, Fe, Mn e Cu. Em geral, quanto aos atributos químicos do solo, a adoção do manejo com efluente tratado apresentou resultados semelhantes aos obtidos com o MC, favorecendo a melhoria da fertilidade do solo e constituindo-se em uma fonte alternativa de fertilização de baixo custo. O efluente tratado, independentemente do fator de diluição, também demonstrou ser uma fonte alternativa de água.

Fungos micorrízicos arbusculares em um latossolo vermelho sob manejos e usos no cerrado

As modificações nas comunidades de fungos micorrízicos arbusculares (FMAs) induzidas por mudança de uso do solo e por diferentes usos agrícolas ainda são insuficientemente estudadas, particularmente no Cerrado. O presente estudo teve como objetivo avaliar como a interferência antrópica pelo manejo e mudança de uso do solo atua sobre a densidade de esporos e diversidade dos FMAs em um Latossolo Vermelho distroférrico de Cerrado. O estudo avaliou cinco áreas: Mata Ciliar (MC), Borda da Mata (BM), Pastagem (Past), Plantio Direto (PD) e Área Desmatada (AD). Foram retirados 20 pontos amostrais, em delineamento inteiramente casualizado, para avaliação da densidade de esporos e diversidade de FMAs. Cada ponto amostral representava uma área de 250 m² dentro de cada área. A área com o sistema de PD e a AD apresentaram menor densidade de esporos recuperados e baixa colonização micorrízica em relação às demais áreas devido à baixa quantidade de plantas vegetando nelas. As famílias de FMAs que apresentaram maior ocorrência nas áreas estudadas foram Acaulosporaceae, Glomeraceae e Gigasporaceae, sendo as duas primeiras dominantes nos ambientes menos antropizados de MC e BM. As espécies de FMAs de maior ocorrência foram Acaulospora scrobiculata, Glomus macrocarpum e Acaulospora tuberculata; as duas primeiras apareceram em todas as áreas, e a terceira apenas não ocorreu na área de PD. Essas espécies mostraram grande capacidade de adaptação aos ambientes alterados. As espécies Acaulospora rehmii, Acaulospora sp.3, Glomus etunicatum, Glomus tortuosum, Glomus sp.1, Gigaspora sp.2 e Scutellospora heterogama apresentaram baixa ocorrência, sendo recuperadas somente em uma das áreas estudadas. A área com maior densidade e ocorrência de espécies foi a Past, com 414 esporos (indivíduos) e 11 espécies. As áreas extremas quanto à diversidade de Shannon (H') foram a Past e a BM, com maior e menor índices, respectivamente. A análise de componentes principais indicou a formação de três grupos, sendo o primeiro formado pela MC e BM; o segundo, por AD e PD; e o terceiro, somente por Past. Conclui-se que a mudança no uso do solo promove alterações na comunidade de FMAs, podendo a densidade e diversidade de esporos ser ampliadas, no caso da pastagem, ou reduzidas, no caso de desmatamento.

Compaction of an Oxisol and chemical composition of palisadegrass

Compaction is an important problem in soils under pastoral land use, and can make livestock systems unsustainable. The objective of this research was to study the impact of soil compaction on yield and quality of palisade (UROCHLOA BRIZANTHA cv. Marandu). The experiment was conducted on an Oxisol in the State of Mato Grosso, Brazil. Treatments consisted of four levels of soil compaction: no compaction (NC), slight compaction (SC), medium compaction (MC) and high compaction (HC). The following soil properties were evaluated (layers 0-0.05 and 0.05-0.10 m): aggregate size distribution, bulk density (BD), macroporosity, microporosity, total porosity (TP), relative compaction (RC), and the characteristics of crude protein (CP), neutral detergent fiber (NDF), acid detergent fiber (ADF) and dry matter yield (DMY) of the forage. Highly compacted soil had high BD and RC, and low TP (0-0.05 m). Both DMY and CP were affected by HC, and both were strongly related to BD. Higher DMY (6.96 Mg ha-1) and CP (7.8 %) were observed in the MC treatment (BD 1.57 Mg m-3 and RC 0.91 Mg m-3, in 0-0.05 m). A high BD of 1.57 Mg m-3 (0-0.05 m) did not inhibit plant growth. The N concentration in the palisade biomass differed significantly among compaction treatments, and was 8.72, 11.20, 12.48 and 10.98 g kg-1 in NC, SC, MC and HC treatments, respectively. Increase in DMY and CP at the MC level may be attributed to more absorption of N in this coarse-textured soil.

Soil physical properties and grape yield influenced by cover crops and management systems

The use of cover crops in vineyards is a conservation practice with the purpose of reducing soil erosion and improving the soil physical quality. The objective of this study was to evaluate cover crop species and management systems on soil physical properties and grape yield. The experiment was carried out in Bento Gonçalves, RS, Southern Brazil, on a Haplic Cambisol, in a vineyard established in 1989, using White and Rose Niagara grape (Vitis labrusca L.) in a horizontal, overhead trellis system. The treatments were established in 2002, consisting of three cover crops: spontaneous species (SS), black oat (Avena strigosa Schreb) (BO), and a mixture of white clover (Trifolium repens L.), red clover (Trifolium pratense L.) and annual rye-grass (Lolium multiflorum L.) (MC). Two management systems were applied: desiccation with herbicide (D) and mechanical mowing (M). Soil under a native forest (NF) area was collected as a reference. The experimental design consisted of completely randomized blocks, with three replications. The soil physical properties in the vine rows were not influenced by cover crops and were similar to the native forest, with good quality of the soil structure. In the inter-rows, however, there was a reduction in biopores, macroporosity, total porosity and an increase in soil density, related to the compaction of the surface soil layer. The M system increased soil aggregate stability compared to the D system. The treatments affected grapevine yield only in years with excess or irregular rainfall.

Erosão hídrica em semeadura direta de milho e soja nas direções da pendente e em contorno ao declive, comparada ao solo sem cultivo e descoberto

Dados de perdas de água e solo obtidos em estudos de erosão hídrica são necessários nos planos de conservação do solo. Mesmo com o advento do sistema de semeadura direta, difundido no Brasil a partir dos anos de 1970, ainda se fazem necessárias práticas conservacionistas para o efetivo controle da erosão hídrica, como o uso do cultivo em contorno e o terraceamento, especialmente em regiões com altos volumes de chuva. Outra opção para o controle da erosão é o uso de culturas protecionistas do solo. O objetivo deste trabalho consistiu em quantificar as perdas de água e solo por erosão hídrica, em um solo cultivado com soja e milho sob semeadura direta, nas direções da pendente e em contorno ao declive. O experimento foi realizado em um Cambissolo Húmico alumínico léptico, no período de 2010-2011, sob a aplicação de quatro testes de chuva simulada. Estudaram-se cinco tratamentos, com duas repetições, sendo eles: semeadura de soja no sentido do declive (SD); semeadura de soja no sentido da curva de nível (SC); semeadura de milho no sentido do declive (MD); semeadura de milho no sentido da curva de nível (MC); e testemunha - solo sem cultivo e descoberto (T). Os cultivos foram implantados sobre resíduo cultural de trigo, no sistema de semeadura direta. A semeadura da soja em contorno foi mais eficaz no controle das perdas de solo do que a semeadura dessa no sentido do declive. A cultura do milho foi mais eficaz no controle das perdas de solo do que a soja, independentemente da forma de semeadura, e ambas foram mais eficazes do que a testemunha. As perdas de água foram influenciadas apenas pela forma de semeadura e relacionaram-se negativamente com a umidade do solo antes do início das chuvas e com o tempo de início da enxurrada.

Comparing the artificial neural network with parcial least squares for prediction of soil organic carbon and pH at different moisture content levels using visible and near-infrared spectroscopy

Visible and near infrared (vis-NIR) spectroscopy is widely used to detect soil properties. The objective of this study is to evaluate the combined effect of moisture content (MC) and the modeling algorithm on prediction of soil organic carbon (SOC) and pH. Partial least squares (PLS) and the Artificial neural network (ANN) for modeling of SOC and pH at different MC levels were compared in terms of efficiency in prediction of regression. A total of 270 soil samples were used. Before spectral measurement, dry soil samples were weighed to determine the amount of water to be added by weight to achieve the specified gravimetric MC levels of 5, 10, 15, 20, and 25 %. A fiber-optic vis-NIR spectrophotometer (350-2500 nm) was used to measure spectra of soil samples in the diffuse reflectance mode. Spectra preprocessing and PLS regression were carried using Unscrambler® software. Statistica® software was used for ANN modeling. The best prediction result for SOC was obtained using the ANN (RMSEP = 0.82 % and RPD = 4.23) for soil samples with 25 % MC. The best prediction results for pH were obtained with PLS for dry soil samples (RMSEP = 0.65 % and RPD = 1.68) and soil samples with 10 % MC (RMSEP = 0.61 % and RPD = 1.71). Whereas the ANN showed better performance for SOC prediction at all MC levels, PLS showed better predictive accuracy of pH at all MC levels except for 25 % MC. Therefore, based on the data set used in the current study, the ANN is recommended for the analyses of SOC at all MC levels, whereas PLS is recommended for the analysis of pH at MC levels below 20 %.

The distribution of the dinucleotide CpG and cytosine methylation in the vitellogenin gene family.

Sequence data from regions of five vertebrate vitellogenin genes were used to examine the frequency, distribution, and mutability of the dinucleotide CpG, the preferred modification site for eukaryotic DNA methyltransferases. The observed level of the CpG dinucleotide in all five genes was markedly lower than that expected from the known mononucleotide frequencies. CpG suppression was greater in introns than in exons. CpG-containing codons were found to be avoided in the vitellogenin genes, but not completely despite the redundancy of the genetic code. Frequency and distribution patterns of this dinucleotide varied dramatically among these otherwise closely related genes. Dense clusters of CpG dinucleotides tended to appear in regions of either functional or structural interest (e.g., in the transposon-like Vi-element of Xenopus) and these clusters contained 5-methylcytosine (5 mC). 5 mC is known to undergo deamination to form thymidine, but the extent to which this transition occurs in the heavily methylated genomes of vertebrates and its contribution to CpG suppression are still unclear. Sequence comparison of the methylated vitellogenin gene regions identified C----T and G----A substitutions that were found to occur at relatively high frequencies. The predicted products of CpG deamination, TpG and CpA, were elevated. These findings are consistent with the view that CpG distribution and methylation are interdependent and that deamination of 5 mC plays an important role in promoting evolutionary change at the nucleotide sequence level.

SOMATIC MUTATIONS IN THE KREBS CYCLE ENZYME ISOCITRATE DEHYDROGENASE 1 (IDH1) CAUSE METAPHYSEAL ENCHONDROMATOSIS WITH D-2-HYDROXYGLUTARIC ACIDURIA

Metaphyseal chondromatosis with hydroxyglutaric aciduria (MC-HGA) is a generalized skeletal dysplasia, accompanied by urinary excretion of D-2- hydroxyglutarate (HGA), and variable cerebral involvement. By wholeexome sequencing 2 unrelated patients with MC-HGA, we have found mutations in isocitrate dehydrogenase 1 (IDH1) at codon 132, as apparent somatic mosaicism. IDH1 is a key enzyme of the Krebs cycle, which converts isocitrate into alpha-ketoglutarate (a-KG). Mutations at IDH1 Arg132 residue have originally been identified in different tumour types (isolated gliomas, leukemias, and chondrosarcomas). These mutations trans-specify the enzyme activity resulting in HGA accumulation and a-KG depletion. This induces activation of hypoxia-inducible factor 1-alpha (HIF-1a), an important regulator of chondrocyte proliferation at the growth plate. Differently from Arg132 somatic mutations found in isolated tumours, themutation in our patientsmust have occurred very early in embryogenesis to cause a generalized dysplasia with involvement of all long bones metaphyses and mutation detectability in blood. Identical mutations have subsequently been identified in chondromas excised from patients with multiple chondromatosis (Ollier disease). Tissue distribution of themutationmay explain variable cerebral involvement and the susceptibility to develop tumours in other organs. The postulated pathophysiology ofMC-HGA points out the link between Krebs cycle, hypoxia sensing and bone growth.

Monte Carlo simulation of a whole-body counter using IGOR phantoms.

Whole-body counting is a technique of choice for assessing the intake of gamma-emitting radionuclides. An appropriate calibration is necessary, which is done either by experimental measurement or by Monte Carlo (MC) calculation. The aim of this work was to validate a MC model for calibrating whole-body counters (WBCs) by comparing the results of computations with measurements performed on an anthropomorphic phantom and to investigate the effect of a change in phantom's position on the WBC counting sensitivity. GEANT MC code was used for the calculations, and an IGOR phantom loaded with several types of radionuclides was used for the experimental measurements. The results show a reasonable agreement between measurements and MC computation. A 1-cm error in phantom positioning changes the activity estimation by >2%. Considering that a 5-cm deviation of the positioning of the phantom may occur in a realistic counting scenario, this implies that the uncertainty of the activity measured by a WBC is ∼10-20%.

Alexandre Sauvaige. L'Etiquette du temps.

Manuscrit orné de dessins à la plume et aux armes de François de Rochechouart, gouverneur du Gênes sous Louis XII. Anciennes collections Mc Carthy, Georges Hilbert, Robert Hoe et comte Paul Durrieu.

Horae secundum usum romanum.

F. A-B. Bifolium contenant la fin de l’office du Saint Esprit ; cf. le même texte aux ff. 156-156v. XVe siècle. Copie inachevée dont les initialesont été laissées en blanc. Le f. B réglé est blanc. La justification est la même que celle du corps du manuscrit.F. 1-12v. Calendrier écrit à l’encre rouge et bleue et à l’or: nombreux saints méridionaux, en particulier de la vallée du Rhône et du Languedoc : « Fulcrani ep. [Lodevensis] » (13 févr.) ; « translatio s. Pauli » (20 février) ; « translatio s.Augustini » (28 février) ; « Pauli archi. Narbo[nensis] » (22 mars) ; « translatio b. Ferreoli [ ?] (1er avril) ; « Baudilii mart. [Nemausiensis] (20 mai) ; « Quiterie (21 mai) ; « Eutropii [ep. Arausicani] (27 mai) ; « translatio s. Saturnini » (22 juin) ; « Petri de Lucemburgo » (5 juillet) ; « Roqui mart. [Montispessulani] » (16 août) ; « Ludovici regis fratris [ep. Toletani]» (19 août) ; « Privati conf. [ep. Gabalitanus (Gévaudan)] » (21 août) ; « Fereoli mart. [Viennae] (18 sept.) ; « Apolinaris ep. [Valentinensis] » (10 oct.) ; « Firmini ep. [Ucetensis] » (11 oct.] ; « Florencii ep. [Arausicani] » (17 oct.] ; « Amancii ep. [Ruthenensis] » (5 nov.) ; « Restituti ep. [Tricastini] » (8 nov.) ; « Rufi ep. [Avenionensis] » (14 nov.) ; « Pauli ep. [Narbonensis] » (11 déc.) ; « Dominici conf. [de Silos] » (20 déc.). Mentions zodiacales et de comput, parmi lesquelles on note une « renovatio indicionum », le 24 septembre. F. 13-17. Extraits des quatre Evangiles : Io (13-14) ; Lc (14-15) ; Mt (15-16v) ; Mc (16v-17).F. 17v-71. [Horae beatae Mariae virginis secundum usum romanum]. [Ad matutinas], psaumes répartis selon les jours de la semaine (18-32v) ; — « In laudibus » (32v-42v) ; — « Ad primam » (43-46v) ; — « Ad tertiam » (46v-49) ; — « Ad sextam » (49v-52) ; « Ad IXa » (52-55) ; — « Ad vesperas » (55-60) ; — « Ad comple[c]torium » (60-64) ; — Antiennes, psaumes, leçons et répons pour les différents temps de l’année (64v-71) .F. 71-77v. Messe votive. « Missa beate Marie virginis ». « Salve sancta parens... » F. 78-85. Prières et hymnes. [Septem gaudia spiritualia b. Mariae virginis], incomplet des quatre premiers vers par lacune matérielle. « [Gaude flore virginali...] et sanctorum decoratum//...-... per eterna secula » (AH, XXXI, n° 198) ; « O sponsa Dei electa// Esto nobis via recta... » ; « ...Oratio. Domine Jhesu Christe qui beatissimam gloriosam virginem...-... pervenire mereamur » ; « Gaudia. Gaude virgo mater Christi// Que per aurem concepisti// ...-... perhemni gaudio. » (AH, XXIV, n° 57) ; cf. Leroquais, Livres d’heures, I, XXVI-XXVII ; « ... Oratio. Deus qui beatissimam virginem Mariam in consceptu... pervenire. Per... » ; « Gaudia beate Marie spiritualia. Gaude stirpe regis nata// Ab angelo saluta[ta]...-... et celorum mansio » (AH, XXXI, n° 182) ; « Oratio. Consolator mitissime Deus... sempiternis perfrui. Per... » ; « Alia oratio. Deus qui Gabrielem archangelum... mereamur habere. Qui... » ; « Devota oratio ad beatam virginem Mariam. Obsecro te domina... et michi famulo tuo pauperrimo N. ... » (Leroquais, Livres d’heures, II, 346-347).F. 85v blanc.F.86-91v. [Horae Trinitatis].F.91v-93v. Messe votive. « Missa de Trinitate ».F. 93v-97. « Devota oratio. Deus omnipotens propicius esto michi peccatori, custos mei omnibus diebus et horis vite mee, Deus Abraham... Omnes sancti angeli et archangeli Dei succurrite et subvenite michi peccatori... horis vite mee » ; cf. Leroquais, Livres d’heures, II, 396 ; — « O bone Jhesu illumina oculos meos ne unquam obdormiam... impietatem peccati mei » ; cf. Leroquais, Livres d’heures, I, XXX-XXXI ; — « Omnipotens, sempiterne et clementissime Deus qui Ezechie regi ... merear et optinere. Per... », à la forme masculine ; cf. Leroquais, Livres d’heures, II, 438 ; — « Oratio. Omnipotens sempiterne Deus te supplices exoramus ut celesti... consequantur. Per... » (Corpus orationum, VI, n° 4076).F. 97v blanc.F. 98-108. [Psaumes de la pénitence]. F. 108-117v. « Letania ». A noter parmi les confesseurs, la séquence inattendue de trois évêques de Toul honorés en Lorraine : « ... s. Mansuete, s. Gerarde, s. Aper ». Parmi les saintes : « ... s. Martha, s. Eulalia... s. Radegundis... ». — Oraisons diverses : « Propicius esto, parce nobis Domine... ut michi indigno famulo tuo N... exaudire digneris » ; — ... « Omnipotens sempiterne Deus miserere michi indigno famulo tuo N.... perficiat. Per... » ; — « Pie et exaudibilis domine Jhesu Christe Deus noster clementiam tuam... digneris eternam » ; cf. Leroquais, Psautiers, I, 25 ; — « Pietate tua quesumus Domine nostrorum solve vincula delictorum et intercedente pro nobis... virgine Dei genitrice Maria cum beatis apostolis tuis Petro et Paulo atque Andrea... eternam concede. Per... » (Corpus orationum, VI, n° 4227)...F. 118-145. [Officium mortuorum secundum usum romanum]F. 145-147v. Messe votive. « Missa pro omnibus fidelibus defunctis ». F. 148-151. [Horae sancti Spiritus].F. 151-153v. Messe votive. « Missa de sancto Spiritu », incomplet de la fin par lacune matérielle.F. 154-156v. [Horae omnium sanctorum], incomplet du premier feuillet.F. 156v-159v. Messe votive. « Missa de omnibus sanctis. F. 160-162v. [Horae sancti Sacramentis], incomplet du début par lacune matérielle. F. 162v-164v. Messe votive. « Missa de corpore Christi ».F. 164v-169v. Prières et hymnes. « ... salutatio sacratissimi corporis domini nostri Jhesu Christi. Ave Jhesu Christe verbum Patris filius [Virginis] agnus Dei...-... requies nostra vita perhemnis » ; cf. ms NAL 3211, 342 ; — « Alia oratio. Salve sancta caro Dei per quam salvi...-... da michi sedem justorum. Qui... » (ed. Leroquais, Livres d’heures, II, 348) ; — In elevatione corporis Christi. Anima Christi sanctifica me // Corpus Christi salva me... secula seculorum. Amen » ; (ed. Leroquais, Livres d’heures, II, 340 variantes) ; — « Alia. Ave verum corpus natum... o pia... ora pro nobis » (AH, LIV, n° 257) ; — « Alia devota oratio. Domine Jhesu Christe qui hanc sacratissimam carnem tuam... et periculis et in eternum » ; cf.ms NAL 3203, 26v ; — « Dum volueris communicare dic orationem. Omnipotens et misericors Deus ecce accedo ad sacratissimum accedo inquam infirmus ad medicum...-... tutela finalis in morte. Qui... » ; — « Alia oratio ante communionem. Domine sancte Pater, omnipotens eterne Deus, da mihi corpus et sanguinem... in infinita secula... » ; cf. Leroquais, Livres d’heures, II, 108 ; — « Post communionem. Gratias tibi ago Domine sancte pater omnipotens eterne Deus qui me peccatorem indignum famulum tuum saciare... et gaudium sempiternum... » ; cf. Leroquais, Livres d’heures, I, 51 ; — « Post communionem ad beatam Virginem. Serenissima Virgo et inclita mater nostri Jhesu Christi, sancta Maria regina celi et terre que eundem creatorem... hodie veracis [incomplet de la fin par lacune matérielle] ; cf. Leroquais, Livres d’heures, I, 156, 299.F. 170-173. [Horae sanctae Crucis], incomplet du début.F. 173-178. Messe votive. « Missa in honore sancte Crucis ». « Crucem tuam adoramus et veneramur domine Jhesu Christe, et per ipsam tuam sanctissimam recolimus passionem...-...defunctis vitam et gloriam sempiternam... » ; — « Alia oratio. Domine Jhesu Christe plasmator tocius creature, rex glorie obsecro miserere mei quia locutus sum... semper benedictus... » ; — « Alia oratio. Domine Jhesu Christe qui voluisti pro redemptione mundi nasci et circumcidi... ego miserrimus, vilissimus, nequissimus atque indignissimus peccator...-... latronem crucifixum. Qui... » ; — « Alia oratio. Precor te, piissime domine Jhesu Christe, per illam eximiam caritatem qua tu rex celestis... mihi tribuere digneris. Qui... » ; — « Alia oratio. Deus propicius esto michi peccatori. Quid est Jhesus nisi salvator ergo Jhesus per te ipsum redemptus sum... miserere michi Deus » ; — « Dic totum deinde dic oracionem. Tribulacionem nobis [sic], quesumus, Domine propicius respice... clementer averte. Per... ». F. 178-200. « ... suffragia sanctorum ». « ... de Trinitate » ; — « De sancto Michaele archangelo » ; — « De sancto Johanne Baptista » ; — « De sancto Petro et Paulo » ; — « De sancto Andrea apostolo » ; — « De sancto Johanne evangelista » ; — « De sancto Jacobo minori » ; — « Sanctorum Philippi et Jacobi » ; — « De innocentibus » ; — « De apostolis et evvangelistis » ; — « De sancto Stephano » ; — « De sancto Laurencio » ; — « De sancto Eutropio... Eutropium martyrem tuum (f. 183v)... » ; — « De sancto Georgio » ; — « De sancto Blasio » ; — « De sancto Dyonisio » ; — « De sancto Yppolito » ; — « De sancto Christophoro » ; — « De sancto Sebastiano. Omnipotens sempiterne Deus qui meritis beati Sebastiani martyris gloriosissimi quemdam pestem epydimie generalem hominibus mortiferam revocasti, presta supplicibus tuis ut qui hanc orationem super se portavit aut in domibus vel mansionibus scriptam aut alias de ea in tuo nomine memoriam habuerint sive in die aut in nocte legerint a simili a peste et morbo epydimie sub ejus confidencia ad te confugerint ipsius meritis et precibus ab ipsis peste et morbo epydimie et ab omnibus nocumentis venenosis necnon ab omnibus periculis corporis et anime atque a subitanea et improvisa morte et ab omnibus inimicis visibilibus et invisibilibus singulis diebus et noctibus horis atque momentis liberemur. Per Dominum. Pater noster. Ave Maria. Credo. Salva regina. Ave stella matutina, rosa sine spinis, cum reliquis ». — « Unius martyris communis » ; — « De martyribus communis » ; — « De sancto Martino » ; — « De sancto Nicholao » ; — « De sancto Anthonio » ; — « De sancto Lazaro » ; — « De sancto Restituto... Deus qui per merita beati Restituti confessoris atque pontificis a multorum oculis dolorem sanas, labem removes et visum clarificas... (189v-190) » ; — « Unius confessoris » ; — « De confessoribus communis » ; — « De beata Maria Magdalena prosa. Gaude pia Magdalena // Spes salutis // Vite vena // Lapsorum fiducia // Gaude dulcis advocata // ... » ; — « De beata Catherina. Gaude virgo Catherina /// Quam refecit lux divina // Ter quaternis noctibus //... » ; — « De beata Lucia » ; — « De beata Apollonia » ; — « De beata Agatha » ; — « De virginibus » ; — « De omnibus sanctis » ; — « De pace » ; — « De sancto Petro de Lucemburgo » ; le suffrage commence par la prière attribuée à s. Pierre de Luxembourg : « Deus pater qui creasti // Mundum et illuminasti // Suscipe...-... requiescant in pace. Amen » ; cf.ms NAL 3196, 152.F. 200v-204, feuillets réglés blancs.

Elemental and isotopic zoning in natural alpine quartz

THESIS ABSTRACT : Stable isotope geochemistry is used to help resolve a large number of geological questions. In order to do this, it is essential to understand the different mechanisms that govern isotopic fractionation processes between different phases and to identify the conditions required to reach equilibrium fractionation. However, at low temperatures, these processes are poorly constrained and many factors can induce differential partitioning of the isotopes between sectors of a mineral species and the fluid during mineral growth. This can result in so-called 'sector zoning' of a mineral species. The aim of this thesis is to evaluate the occurrence of sector zoning of the oxygen isotopes and trace elements in natural α-quartz crystals and to identify the reasons for such zoning. The implications for the fluid-mineral interactions are studied in the context of the Alpine metamorphism. The approach chosen has focused on examining the crystal structure, cathodoluminescence appearance (CL), and on relating elemental (e.g. Li, Na, Al, P, K, Ca, Ge, Ti, Fe) to stable oxygen isotope compositions between and along different growth sectors. Low temperature quartz samples were selected from Alpine veins in different localities, where growth conditions have already been well constrained. The mineralogy as well as the isotopic compositions of the host rocks were also investigated, in order to interpret the variations obtained between the different growth stages in the framework of fluid-rock interaction during Alpine metamorphism. Depending on the growth conditions, most of the studied quartz is strongly zoned in CL, and it reveals corresponding zonations in the trace element content (e.g. growth zoning). Aluminium, substituting for Si in the lattice, was found in concentrations up to 1000's ppma, and its distribution is strongly related to Li and H and to a lesser extent, to Ge. Elemental sector zoning is evident from the distribution of these three elements since they exhibit differences in their respective concentrations between faces for distinct growth zones, with prismatic faces having the lowest Al contents. Quartz from veins in magmatic rocks, for example, tend to have lower Al concentrations and similar concentrations of Li and Ti suggesting also a contribution of these elements from the host rock. The relationship between Al and Li is still correlated. Only Alpine crystals grown at higher temperatures (~400°C) without any CL zoning feature are free of these impurities and do not show such zoning characteristics. Differences in the δ18O values were measured between different faces principally in the AIenriched growth zones or stages. These results were confirmed by the means of two different methods (in situ/non in situ). However, it was determined that the Al concentrations do not affect significantly oxygen isotope fractionations at 300°C. The results altogether suggest that the presence of sector zoning in quartz crystals is real, but not universal, and henceforth should be taken into consideration for any use of these systems. The occurrence of disequilibrium partitioning has been enhanced and is possibly related to kinetic processes as well as structural effects that do not affect similarly trace element incorporation and isotopic fractionation. In situ measurements also revealed fine scale δ18O zonations along growth paths that are useful to constrain fluid-rock interactions during Alpine metamorphism. Variations in the δ18O values present along growth vectors indicate changes in the fluid composition and origin. Association with oxygen isotope composition of the host rock allows for the deduction of interactions between rocks, veins and consequently fluids, as well as fluid regimes. RESUME DE LA THESE : A basses températures, (i.e. <400°C) les différents mécanismes qui régissent le fractionnement isotopique ainsi que les conditions nécessaires pour établir un état d'équilibre sont peu connus et nombre de paramètres peuvent entraîner un partitionnement chimique différentiel entre différents secteurs d'un minéral et le fluide en contact. Ainsi, ce travail de thèse a pour but d'évaluer la possible présence de zonages sectoriels en isotopes de l'oxygène mais aussi en éléments traces dans des cristaux naturels de quartz-α de basses températures, ainsi que les raisons d'un tel phénomène et enfin ses implications sur les interactions fluide-roche, principalement dans le cadre du métamorphisme Alpin. La structure et l'apparence en cathodoluminescence (CL) des échantillons ont été caractérisées avant de retracer en détail les compositions en élément traces (Li, Na, Al, P, K, Ca, Ge, Ti, Fe) et en isotopes de l'oxygène, le long et entre différents secteurs. Les échantillons de quartz sélectionnés proviennent majoritairement de veines Alpine de différentes localités, où les conditions de croissance ont été déjà bien caractérisées. Les compositions minéralogiques et isotopiques de la roche encaissante ont aussi été examinées, pour contraindre les variations obtenues dans un contexte Alpin. Selon leurs conditions de croissance, la plupart des cristaux étudiés sont fortement zonés, ce qui est souligné par un zonage des concentrations en éléments traces (e.g. zonage de croissance). L'Aluminium, qui peut se substituer à la Silice dans le réseau cristallin, a été retrouvé jusqu'en très grandes concentrations dans certaines zones (plusieurs milliers de ppma). De plus, la distribution en Al est fortement liée à celles de Li et H, ainsi que dans une moindre mesure à Ge. La présence de zonage sectoriel est évidente au niveau de ces éléments qui montrent de larges différences de concentrations entre différentes faces pour une même zone de croissance, avec les concentrations les plus basses retrouvées dans les faces prismatiques. Les quartz de veines situées dans des roches magmatiques par exemple possèdent des concentrations en Li et Ti de même ordre de grandeur, confirmant le rôle de la composition de la roche encaissante. La relation Li/Al est toujours fortement présente, mais ce rapport est fonction de la face mesurée. Seuls les cristaux Alpins de plus hautes températures (400°C) ne possédant pas de zones en CL ne présentent aucune de ces caractéristiques. Des différences dans les valeurs de δ18O de zones identiques enrichies en Al ont clairement été mesurées entre les différentes faces r, z, et m, mais aussi au sein d'une même seule zone, indiquant que le fractionnement a probablement eu lieu en déséquilibre. Il a été déterminé que la présence d'Al dans ces teneurs n'avait qu'un faible effet sur le fractionnement isotopique de l'oxygène. L'utilisation de deux méthodes différentes a permis d'obtenir des résultats in situ et non in situ concordants. La comparaison des résultats obtenus permet de démontrer que le zonage sectoriel est bien présent dans certains cristaux de quartz, et dépend des conditions de formation. La présence d'un partitionnement différentiel des éléments traces peut être due à des effets cinétiques aussi bien que structuraux, alors que le zonage sectoriel des isotopes de l'oxygène aurait d'autres origines. Il est alors évident que la possibilité de zonage sectoriel doit être désormais pris en considération avant toute interprétations de données isotopiques de cristaux zonés. Les mesures in situ ont de plus permis de distinguer de fines variations des valeurs δ18O au cours de la croissance, qui peuvent aider à retracer la circulations des fluides dans les Alpes durant cette période. En association avec les compositions des roches encaissantes, ii est possible de déduire les interactions entre roches, veines, et par conséquent fluides, au cours de différentes étapes. RESUME GRAND PUBLIC : La géochimie des isotopes stables a pris beaucoup d'importance depuis ces dernières années pour aider à résoudre nombre de questions géologiques, en se basant sur les caractéristiques du fractionnement isotopiques pour différents systèmes. Il est donc nécessaire d'avoir une connaissance approfondie des mécanismes qui s'appliquent au fractionnement isotopique entre les minéraux et les fluides à partir desquels ils se forment. Ces mécanismes ont été bien approchés par différents types de calibrations pour des systèmes à hautes températures, cependant cela n'est pas aussi évident pour les systèmes à des températures inférieures à 400-500°C. Ce travail de thèse a pour but d'aider à la description et la compréhension des phénomènes qui peuvent affecter le fractionnement isotopique à basses températures, ainsi que leurs implications, à partir de l'étude de cristaux de quartz. Le choix des échantillons s'est porté sur des cristaux naturels formés à des températures inférieures ou égales à 400°C, provenant majoritairement de fissures hydrothermales Alpines dont les conditions de formation ont déjà été déterminées. L'étude des cristaux Alpin permet de plus de replacer les résultats obtenus dans le contexte du métamorphisme Alpin au cours du Miocène (21-13 Ma). Après examen de la structure et de la morphologie des cristaux, et leur caractérisation par cathodoluminescence (CL), des analyses chimiques détaillées sur les éléments en traces pouvant entrer dans le réseau cristallin du quartz comme impuretés (i.e. Li, Na, Al, P, K, Ca, Ge, Ti), et des isotopes stables de l'oxygène, ont été menées. En fonction des conditions de croissance, la plupart des cristaux présentent des zonations, qui peuvent être facilement reliées à la distribution des éléments traces analysés par microsonde électronique, sonde ionique (SIMS) et LA-ICPMS. De fortes concentrations d'Aluminium (plusieurs milliers de parties par million atomique) ont pu être observées dans les zones les plus externes des cristaux. De plus, les concentrations en Al et en Li sont toujours corrélées; la présence d'Hydrogène déduite à partir d'analyses par FTIR suit cette même tendance. Les différentes faces des cristaux présentent des concentrations distinctes d'Al, Li et H pour des mêmes zones de croissance, avec par exemple les concentrations les plus faibles dans les zones des faces prismatiques. Cela implique la présence d'un zonage sectoriel, qui a déjà été observé principalement dans des carbonates mais jamais décrit auparavant pour des quartz. Seuls les cristaux alpins homogènes en CL dont la croissance s'est faite à plus haute température (400°C) ne présentent aucune de ces caractéristiques. Par analogie avec le zonage sectoriel en Al, élément qui se substitue au Si dans le réseau cristallin du quartz, il est possible de penser qu'un zonage sectoriel pourrait aussi s'appliquer aux isotopes de l'oxygène. Des précédentes études avaient en effet émis cette hypothèse. Nos résultats ont été obtenus à partir d'analyses à la fois in- situ par SIMS, et par extraction assistée par laser-CO2 sur des parties de quartz soigneusement séparées, et sont en accord entre les deux méthodes. Un zonage sectoriel est en effet bien présent pour les cristaux alpins, mais principalement au niveau des zones très riches en Aluminium. Cependant, il a été déterminé que la présence d'Al dans ces teneurs avait un effet plus que minimal sur le fractionnement isotopique de l'oxygène. Des différences importantes ont été observées entre les faces r & z mais aussi au sein d'une même et seule zone, indiquant que le fractionnement a pu avoir lieu en déséquilibre, ce qui est aussi visible au niveau des valeurs totalement opposées entre faces pour la dernière phase de croissance de certains cristaux. Ainsi l'association de ces résultats laisse suggérer que la présence d'un zonage sectoriel peut être liée à différents paramètres tels que le taux de croissance ou la structure de surface du cristal, mais qui n'affectent pas de la même façon l'incorporation des éléments traces et le fractionnement isotopique. La possibilité d'un zonage sectoriel est importante à prendre en compte lors de toute interprétation de données isotopiques. Les analyses des isotopes de l'oxygène effectuées par SIMS ont aussi permis de distinguer des variations importantes à petite échelle au cours de la croissance. Des mesures faites par laser CO2 sur certaines roches encaissantes, ont permis distinguer plusieurs étapes dans la croissance des minéraux et de déduire le rôle de l'encaissant et le type de fluide. En association avec de précédentes études, il a été ainsi possible de mieux contraindre la formation de ces cristaux dans le contexte alpin et la circulation de fluide au cours du métamorphisme alpin durant le Miocène.

Alternative Flexible Overlays, HR-229, 1988

The objective of this project was to determine if any of several cutback and emulsified asphalt plant mixed and road mixed overlays had the ability to resist thermal cracking at low temperatures without inducing shoving and/or ruttinq at high temperatures. A 2.6 mile section of Osceola County road A-34 and a 7.0 mile section of A-46 were divided into 14 test sections of various lengths. After six years, results show an MC-3000 asphalt cutback cold mix can reduce the amount of reflective cracking when compared to an AC-5 hot mix. This can be done without inducing high temperature related problems. Cold road mixing can be effective in reducing cracking on low volume roads. However, more experience is required if the full benefits of road mixing are to be realized.

Association between melanism, physiology and behaviour: a role for the melanocortin system.

The melanocortin system is implicated in the expression of many phenotypic traits. Activation of the melanocortin MC(1) receptor by melanocortin hormones induces the production of brown/black eumelanic pigments, while activation of the four other melanocortin receptors affects other physiological and behavioural functions including stress response, energy homeostasis, anti-inflammatory and sexual activity, aggressiveness and resistance to oxidative stress. We recently proposed the hypothesis that some melanocortin-physiological and -behavioural traits are correlated within individuals. This hypothesis predicts that the degree of eumelanin production may, in some cases, be associated with the regulation of glucocorticoids, immunity, resistance to oxidative stress, energy homeostasis, sexual activity, and aggressiveness. A review of the zoological literature and detailed experimental studies in a free-living population of barn owls (Tyto alba) showed that indeed melanic coloration is often correlated with the predicted physiological and behavioural traits. Support for predictions of the hypothesis that covariations between coloration and other phenotypic traits stem from pleiotropic effects of the melanocortin system raises a number of theoretical and empirical issues from evolutionary and pharmacological point of views.

Association of major and minor ECG abnormalities with coronary heart disease events.

CONTEXT: In populations of older adults, prediction of coronary heart disease (CHD) events through traditional risk factors is less accurate than in middle-aged adults. Electrocardiographic (ECG) abnormalities are common in older adults and might be of value for CHD prediction. OBJECTIVE: To determine whether baseline ECG abnormalities or development of new and persistent ECG abnormalities are associated with increased CHD events. DESIGN, SETTING, AND PARTICIPANTS: A population-based study of 2192 white and black older adults aged 70 to 79 years from the Health, Aging, and Body Composition Study (Health ABC Study) without known cardiovascular disease. Adjudicated CHD events were collected over 8 years between 1997-1998 and 2006-2007. Baseline and 4-year ECG abnormalities were classified according to the Minnesota Code as major and minor. Using Cox proportional hazards regression models, the addition of ECG abnormalities to traditional risk factors were examined to predict CHD events. MAIN OUTCOME MEASURE: Adjudicated CHD events (acute myocardial infarction [MI], CHD death, and hospitalization for angina or coronary revascularization). RESULTS: At baseline, 276 participants (13%) had minor and 506 (23%) had major ECG abnormalities. During follow-up, 351 participants had CHD events (96 CHD deaths, 101 acute MIs, and 154 hospitalizations for angina or coronary revascularizations). Both baseline minor and major ECG abnormalities were associated with an increased risk of CHD after adjustment for traditional risk factors (17.2 per 1000 person-years among those with no abnormalities; 29.3 per 1000 person-years; hazard ratio [HR], 1.35; 95% CI, 1.02-1.81; for minor abnormalities; and 31.6 per 1000 person-years; HR, 1.51; 95% CI, 1.20-1.90; for major abnormalities). When ECG abnormalities were added to a model containing traditional risk factors alone, 13.6% of intermediate-risk participants with both major and minor ECG abnormalities were correctly reclassified (overall net reclassification improvement [NRI], 7.4%; 95% CI, 3.1%-19.0%; integrated discrimination improvement, 0.99%; 95% CI, 0.32%-2.15%). After 4 years, 208 participants had new and 416 had persistent abnormalities. Both new and persistent ECG abnormalities were associated with an increased risk of subsequent CHD events (HR, 2.01; 95% CI, 1.33-3.02; and HR, 1.66; 95% CI, 1.18-2.34; respectively). When added to the Framingham Risk Score, the NRI was not significant (5.7%; 95% CI, -0.4% to 11.8%). CONCLUSIONS: Major and minor ECG abnormalities among older adults were associated with an increased risk of CHD events. Depending on the model, adding ECG abnormalities was associated with improved risk prediction beyond traditional risk factors.