Projecting the self to past and future in mental time

Introduction: Human experience takes place in the line of mental-time (MT) created through imagination of oneself in different time-points in past or future (self-projection in time). Here we manipulated self-projection in MT not only with respect to one's life-events but also with respect to one's faces from different past and future time-points. Methods: We here compared MTT with respect to one's facial images from different time points in past and future (study 1: MT-faces) as well as with respect to different past and future life events (study 2: MT-events). Participants were asked to make judgments about past and future face images and past and future events from three different time-points: the present (Now), eight years earlier (Past) or eight years later (Future). In addition, as a control task participants were asked to make recognition judgments with respect to faces and memory-related judgments with respect to events without changing their habitual self-location in time. Behavioral measures and functional magnetic resonance imaging (fMRI) activity after subtraction of recognition and memory related activities show both absolute MT and relative MT effects for faces and events, signifying a fundamental brain mechanism of MT, disentangled from episodic memory functions. Results: Behavioural and event-related fMRI activity showed three independent effects characterized by (1) similarity between past recollection and future imagination, (2) facilitation of judgments related to the future as compared to the past, and (3) facilitation of judgments related to time-points distant from the present. These effects were found with respect to faces and events suggesting that the brain mechanisms of MT are independent of whether actual life episodes have to be re-/pre-experienced and recruited a common cerebral network including the medial-temporal, precuneus, inferior-frontal, temporo-parietal, and insular cortices. Conclusions: These behavioural and neural data suggest that self-projection in time is a crucial aspect of MT, relying on neural structures encoding memory, mental imagery, and self. Furthermore our results emphasize the idea that mental temporal processing is more strongly directed to future prediction than to past recollection.

Dinâmica da matéria orgânica de um neossolo quartzarênico de cerrado convertido para cultivo em sucessão de soja e milheto

O uso e o manejo de Neossolos Quartzarênicos podem influenciar a matéria orgânica do solo (MOS), mas a magnitude dessas alterações ainda é pouco pesquisada nas condições de Cerrado. O objetivo deste trabalho foi estudar as variações que ocorrem na MOS em um Neossolo Quartzarênico, por consequência da conversão da vegetação original para o uso agrícola e cultivo sequencial de soja e milheto em sucessão. Em uma área de cultivo comercial em Alto Garças, MT, foram coletadas amostras de solo nas profundidades de 0-5, 0-10, 0-20 e 0-40 cm, em talhões que estavam sob sucessão soja-milheto durante 1, 2, 6, 8 e 10 anos e, como referência da vegetação original, amostras foram tomadas em área adjacente sob Cerrado nativo. Foram determinados os teores de carbono orgânico total (COT), carbono e nitrogênio total e o teor de carbono nas frações ácidos húmicos, ácidos fúlvicos e na matéria orgânica leve (MOL), além da relação isotópica do carbono na MOS. A conversão do Cerrado para cultivo agrícola elevou o teor de COT do solo, sobretudo em razão do aporte de MOL e fragmentos de carvão. O manejo desse solo com a sucessão soja-milheto, mesmo com o uso de gradagens pesadas, não causou reduções nos teores de COT, ao longo do tempo. Contudo, observou-se variação na distribuição do carbono nas diferentes frações da MOS ao longo do tempo de cultivo, indicando alterações significativas na qualidade da MOS. Notou-se aumento no percentual de carbono na forma de MOL e redução dos teores de carbono na forma de ácidos fúlvicos ao longo do tempo de cultivo, sugerindo a perda seletiva dos compostos mais solúveis. A relação isotópica do carbono do solo aumentou com o tempo de cultivo, indicando maior contribuição do carbono derivado do milheto para a manutenção dos teores de MOS. Os atributos da MOS relativos à camada de 0-20 cm foram mais sensíveis às variações em razão do tempo de cultivo do que os mesmos atributos avaliados nas demais camadas estudadas. As variáveis relacionadas ao fracionamento da MOS evidenciaram-se mais sensíveis às variações por causa do tempo de cultivo do que simplesmente do teor de COT do solo, apresentando o potencial de uso dessas variáveis como indicadores de qualidade do solo.

Water infiltration in an ultisol after cultivation of common bean

Water infiltration in the soil is an important hydrological process that occurs at the interface of the soil-atmosphere system; thus, the soil management practice used has a strong influence on this process. The aim of this study was to evaluate water infiltration in the soil and compare equations for estimating the water infiltration rate in an Ultisol after harvesting common bean (Phaseolus vulgaris L.) under simulated rainfall. Field tests with a rainfall simulator were carried out in three soil management systems: minimum tillage (MT), conventional tillage (CT), and no tillage (NT). In NT, four levels of plant residue on the soil surface were evaluated: 0, 3, 6, and 9 t ha-1. The models of Kostiakov-Lewis, Horton, and Philip were used to estimate the infiltration rate. In the MT system, the final infiltration rate was 54 mm h-1, whereas in the CT and NT systems with up to 3 t ha-1 of plant residue on the soil surface, the rate was near 17 mm h-1. In addition, the results indicated that in the NT system the infiltration rate increased with plant residue coverage greater than 6 t ha-1, i.e., there was a positive correlation between plant cover and the water infiltration rate. The Horton model was the most suitable in representing the water infiltration process in the soil. Therefore, this model can be recommended for estimation of this variable regardless of the soil tillage system used.

ADUBAÇÃO FOSFATADA E COMPACTAÇÃO DO SOLO: SISTEMA RADICULAR DA SOJA E DO MILHO E ATRIBUTOS FÍSICOS DO SOLO

Associadas aos benefícios no solo da semeadura direta, podem ocorrer a formação de gradiente vertical de fertilidade e a de uma camada compactada provocada pelo intenso tráfego de máquinas agrícolas, podendo modificar o crescimento radicular das culturas. O objetivo deste trabalho foi avaliar as doses e formas de aplicação da adubação fosfatada e a compactação do solo pelo tráfego de máquinas nos atributos físicos e no sistema radicular da soja e do milho nas condições da Chapada dos Parecis, MT. O estudo foi realizado em Latossolo Vermelho-Amarelo distrófico argiloso em delineamento em blocos casualizados, no esquema fatorial 2 × 4 × 4 e três repetições, sendo duas formas de adubação fosfatada (a lanço e no sulco), quatro doses de P2O5 (0, 50, 100 e 150 kg ha-1) e quatro níveis de compactação (PT0, PT2, PT4 e PT8 – semeadura direta com compactação induzida por tráfego de trator em zero, duas, quatro e oito passadas, respectivamente). O tráfego de máquinas ocasionou compactação do solo em semeadura direta, aumentando a densidade do solo (Ds) e resistência do solo à penetração (RSP) e reduzindo a macroporosidade e porosidade total, sem efeito da adubação fosfatada. A resposta das espécies à forma de adubação fosfatada foi diferenciada, não apresentando influência no crescimento radicular da soja. No milho, quando fornecida a lanço proporcionou maior área de raízes na camada de 0,00-0,05 m; e, quando no sulco, foram observadas entre as camadas menores diferenças na área radicular. Nas camadas de 0,05-0,10 e 0,10-0,20 m, a RSP de 1,48 e 1,84 MPa (Us = 0,28 m3 m-3) e Ds de 1,32 e 1,35 kg dm-3, respectivamente, proporcionaram redução de 19 e 27 % no diâmetro médio das raízes do milho e aumento de 110 e 49 % no diâmetro das raízes da soja.

EFFECT OF SOIL TILLAGE AND PLANT RESIDUE ON SURFACE ROUGHNESS OF AN OXISOL UNDER SIMULATED RAIN

Surface roughness of the soil is formed by mechanical tillage and is also influenced by the kind and amount of plant residue, among other factors. Its persistence over time mainly depends on the fundamental characteristics of rain and soil type. However, few studies have been developed to evaluate these factors in Latossolos (Oxisols). In this study, we evaluated the effect of soil tillage and of amounts of plant residue on surface roughness of an Oxisol under simulated rain. Treatments consisted of the combination of the tillage systems of no-tillage (NT), conventional tillage (CT), and minimum tillage (MT) with rates of plant residue of 0, 1, and 2 Mg ha-1 of oats (Avena strigosa Schreb) and 0, 3, and 6 Mg ha-1 of maize (Zea mays L.). Seven simulated rains were applied on each experimental plot, with intensity of 60±2 mm h-1 and duration of 1 h at weekly intervals. The values of the random roughness index ranged from 2.94 to 17.71 mm in oats, and from 5.91 to 20.37 mm in maize, showing that CT and MT are effective in increasing soil surface roughness. It was seen that soil tillage operations carried out with the chisel plow and the leveling disk harrow are more effective in increasing soil roughness than those carried out with the heavy disk harrow and leveling disk harrow. The roughness index of the soil surface decreases exponentially with the increase in the rainfall volume applied under conditions of no tillage without soil cover, conventional tillage, and minimum tillage. The oat and maize crop residue present on the soil surface is effective in maintaining the roughness of the soil surface under no-tillage.

Fluid-rock-strain feedbacks in extensional shear zones

La présence de fluide météorique synchrone à l'activité du détachement (Farmin, 2003 ; Mulch et al., 2007 ; Gébelin et al., 2011), implique que les zones de cisaillement sont des systèmes ouverts avec des cellules de convections à l'échelle crustale et un intense gradient géothermique au sein du détachement (Morrison et Anderson, 1998, Gottardi et al., 2011). De plus, les réactions métamorphiques liées à des infiltrations fluides dans les zones de cisaillement extensionnel peuvent influencer les paramètres rhéologiques du système (White and Knipe, 1978), et impliquer la localisation de la déformation dans la croûte. Dans ce manuscrit, deux zones de cisaillement infiltrées par des fluides météoriques sont étudiées, l'une étant largement quartzitique, et l'autre de nature granitique ; les relations entre déformation, fluides, et roches s'appuient sur des approches structurales, microstructurales, chimiques et isotopiques. L'étude du détachement du Columbia river (WA, USA) met en évidence que la déformation mylonitique se développe en un million d'années. La phase de cisaillement principal s'effectue à 365± 30°C d'après les compositions isotopiques en oxygène du quartz et de la muscovite. Ces minéraux atteignent l'équilibre isotopique lors de leur recristallisation dynamique contemporaine à la déformation. La zone de cisaillement enregistre une baisse de température, remplaçant le mécanisme de glissement par dislocation par celui de dissolution- précipitation dans les derniers stades de l'activité du détachement. La dynamique de circulation fluide bascule d'une circulation pervasive à chenalisée, ce qui engendre localement la rupture des équilibres d'échange isotopiques. La zone de cisaillement de Bitterroot (MT, USA) présente une zone mylonitique de 600m d'épaisseur, progressant des protomylonites aux ultramylonites. L'intensité de la localisation de la déformation se reflète directement sur l'hydratation des feldspaths, réaction métamorphique majeure dite de « rock softening ». Une étude sur roche totale indique des transferts de masse latéraux au sein des mylonites, et d'importantes pertes de volume dans les ultramylonites. La composition isotopique en hydrogène des phyllosilicates met en évidence la présence (1) d'une source magmatique/métamorphique originelle, caractérisée par les granodiorites ayant conservé leur foliation magmatique, jusqu'aux protomylonites, et (2) une source météorique qui tamponne les valeurs des phyllosilicates des fabriques mylonitiques jusqu'aux veines de quartz non-déformées. Les compositions isotopiques en oxygène des minéraux illustrent le tamponnement de la composition du fluide météorique par l'encaissant. Ce phénomène cesse lors du processus de chloritisation de la biotite, puisque les valeurs des chlorites sont extrêmement négatives (-10 per mil). La thermométrie isotopique indique une température d'équilibre isotopique de la granodiorite entre 600-500°C, entre 500-300°C dans les mylonites, et entre 300 et 200°C dans les fabriques cassantes (cataclasites et veines de quartz). Basé sur les résultats issus de ce travail, nous proposons un modèle général d'interactions fluide-roches-déformation dans les zones de détachements infiltrées par des fluides météoriques. Les zones de détachements évoluent rapidement (en quelques millions d'années) au travers de la transition fragile-ductile ; celle-ci étant partiellement contrôlée par l'effet thermique des circulations de fluide météoriques. Les systèmes de détachements sont des lieux où la déformation et les circulations fluides sont couplées ; évoluant rapidement vers une localisation de la déformation, et de ce fait, une exhumation efficace. - The presence of meteoric fluids synchronous with the activity of extensional detachment zones (Famin, 2004; Mulch et al., 2007; Gébelin et al., 2011) implies that extensional systems involve fluid convection at a crustal scale, which results in high geothermal gradients within active detachment zones (Morrison and Anderson, 1998, Gottardi et al., 2011). In addition, the metamorphic reactions related to fluid infiltration in extensional shear zones can influence the rheology of the system (White and Knipe, 1978) and ultimately how strain localizes in the crust. In this thesis, two shear zones that were permeated by meteoric fluids are studied, one quartzite-dominated, and the other of granitic composition; the relations between strain, fluid, and evolving rock composition are addressed using structural, microstructural, and chemical/isotopic measurements. The study of the Columbia River detachment that bounds the Kettle core complex (Washington, USA) demonstrates that the mylonitic fabrics in the 100 m thick quartzite- dominated detachment footwall developed within one million years. The main shearing stage occurred at 365 ± 30°C when oxygen isotopes of quartz and muscovite equilibrated owing to coeval deformation and dynamic recrystallization of these minerals. The detachment shear zone records a decrease in temperature, and dislocation creep during detachment shearing gave way to dissolution-precipitation and fracturing in the later stages of detachment activity. Fluid flow switched from pervasive to channelized, leading to isotopic disequilibrium between different minerals. The Bitterroot shear zone detachment (Montana, USA) developed a 600 m thick mylonite zone, with well-developed transitions from protomylonite to ultramylonite. The localization of deformation relates directly to the intensity of feldspar hydration, a major rock- softening metamorphic reaction. Bulk-rock analyses of the mylonitic series indicate lateral mass transfer in the mylonite (no volume change), and significant volume loss in ultramylonite. The hydrogen isotope composition of phyllosilicates shows (1) the presence of an initial magmatic/metamorphic source characterized by the granodiorite in which a magmatic, and gneissic (protomylonite) foliation developed, and (2) a meteoric source that buffers the values of phyllosilicates in mylonite, ultramylonite, cataclasite, and deformed and undeformed quartz veins. The mineral oxygen isotope compositions were buffered by the host-rock compositions until chloritization of biotite started; the chlorite oxygen isotope values are negative (-10 per mil). Isotope thermometry indicates a temperature of isotopic equilibrium of the granodiorite between 600-500°C, between 500-300°C in the mylonite, and between 300 and 200°C for brittle fabrics (cataclasite and quartz veins). Results from this work suggest a general model for fluid-rock-strain feedbacks in detachment systems that are permeated by meteoric fluids. Phyllosilicates have preserved in their hydrogen isotope values evidence for the interaction between rock and meteoric fluids during mylonite development. Fluid flow generates mass transfer along the tectonic anisotropy, and mylonites do not undergo significant volume change, except locally in ultramylonite zones. Hydration of detachment shear zones attends mechanical grain size reduction and enhances strain softening and localization. Self-exhuming detachment shear zones evolve rapidly (a few million years) through the transition from ductile to brittle, which is partly controlled by the thermal effect of circulating surface fluids. Detachment systems are zones in the crust where strain and fluid flow are coupled; these systems. evolve rapidly toward strain localization and therefore efficient exhumation.

Shaping mechanisms of metal specificity in a family of metazoan Metallothioneins: evolutionary differentiation of Mollusc MTs.

Background: The degree of metal binding specificity in metalloproteins such as metallothioneins (MTs) can be crucial for their functional accuracy. Unlike most other animal species, pulmonate molluscs possess homometallic MT isoforms loaded with Cu+ or Cd2+. They have, so far, been obtained as native metal-MT complexes from snail tissues, where they are involved in the metabolism of the metal ion species bound to the respective isoform. However, it has not as yet been discerned if their specific metal occupation is the result of a rigid control of metal availability, or isoform expression programming in the hosting tissues or of structural differences of the respective peptides determining the coordinative options for the different metal ions. In this study, the Roman snail (Helix pomatia) Cu-loaded and Cd-loaded isoforms (HpCuMT and HpCdMT) were used as model molecules in order t o elucidate the biochemical and evolutionary mechanisms permitting pulmonate MTs to achieve specificity for their cognate metal ion. Results: HpCuMT and HpCdMT were recombinantly synthesized in the presence of Cd2+, Zn2+ or Cu2+ and corresponding metal complexes analysed by electrospray mass spectrometry and circular dichroism (CD) and ultra violet-visible (UV-Vis) spectrophotometry. Both MT isoforms were only able to form unique, homometallic and stable complexes (Cd6-HpCdMT and Cu12-HpCuMT) with their cognate metal ions. Yeast complementation assays demonstrated that the two isoforms assumed metal-specific functions, in agreement with their binding preferences, in heterologous eukaryotic environments. In the snail organism, the functional metal specificity of HpCdMT and HpCuMT was contributed by metal-specific transcription programming and cell-specific expression. Sequence elucidation and phylogenetic analysis of MT isoforms from a number of snail species revealed that they possess an unspecific and two metal-specific MT isoforms, whose metal specificity was achieved exclusively by evolutionary modulation of non-cysteine amino acid positions. Conclusion: The Roman snail HpCdMT and HpCuMT isoforms can thus be regarded as prototypes of isoform families that evolved genuine metal-specificity within pulmonate molluscs. Diversification into these isoforms may have been initiated by gene duplication, followed by speciation and selection towards opposite needs for protecting copper-dominated metabolic pathways from nonessential cadmium. The mechanisms enabling these proteins to be metal-specific could also be relevant for other metalloproteins.

Molecular evidence to suggest the origin of a colonization: Drosophila subobscura in America

Abstract The recent colonization of America by Drosophila subobscura represents a great opportunity for evolutionary biology studies. Knowledge of the populations from which the colonization started would provide an understanding of how genetic composition changed during adaptation to the new environment. Thus, a 793 nucleotide fragment of the Odh (Octanol dehydrogenase) gene was sequenced in 66 chromosomal lines from Barcelona (western Mediterranean) and in 66 from Mt. Parnes (Greece, eastern Mediterranean). No sequence of Odh fragment in Barcelona or Mt. Parnes was identical to any of those previously detected in America. However, an Odh sequence from Barcelona differed in only one nucleotide from another found in American populations. In both cases, the chromosomal lines presented the same inversion: O7, and the Odh gene was located within this inversion. This evidence suggests a possible western Mediterranean origin for the colonization. Finally, the molecular and inversion data indicate that the colonization was not characterized by multiple reintroductions.

O-chromosome lethal frequencies in Serbian and Montenegrin Drosophila subobscura populations

Lethal chromosomal frequencies were obtained from three Drosophila subobscura samples from the Mt. Avala (Serbia) population in September 2003 (0.218), June 2004 (0.204) and September 2004 (0.250). These values and those from other Balkan populations studied previously (Petnica, Kamariste, Zanjic and Djerdap) were used to analyze the possible effect of population, year, month and altitude above sea level on lethal chromosomal frequencies. According to ANOVAS no effect were observed. Furthermore, the lethal frequencies of the Balkan populations did not vary according to latitude. This is probably due to the relative proximity and high gene flow between these populations. From a joint study of all the Palearctic D. subobscura populations so far analyzed, it can be deduced that the Balkan populations are located in the central area of the species distribution. Finally, it seems that lethal chromosomal frequencies are a consequence of the genetic structure of the populations.

How the visual brain encodes and keeps track of time.

Time is embedded in any sensory experience: the movements of a dance, the rhythm of a piece of music, the words of a speaker are all examples of temporally structured sensory events. In humans, if and how visual cortices perform temporal processing remains unclear. Here we show that both primary visual cortex (V1) and extrastriate area V5/MT are causally involved in encoding and keeping time in memory and that this involvement is independent from low-level visual processing. Most importantly we demonstrate that V1 and V5/MT come into play simultaneously and seem to be functionally linked during interval encoding, whereas they operate serially (V1 followed by V5/MT) and seem to be independent while maintaining temporal information in working memory. These data help to refine our knowledge of the functional properties of human visual cortex, highlighting the contribution and the temporal dynamics of V1 and V5/MT in the processing of the temporal aspects of visual information.

La veille bibliographique. Partie 3, Un élément de surveillance

Les deux premières parties de cet article parues précédemment ont présenté la méthodologie ainsi que les premiers éléments du bilan réalisé sur la période allant de 2009 à 2012 de la veille bibliographique sur la surveillance biologique de l'exposition aux produits chimiques en milieu de travail (SBEPC MT) mise en place par un réseau francophone multidisciplinaire.

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.

New magnetotelluric data trough the boundary between the Ossa Morena and Centroiberian Zones

The south-western part of the Iberian Peninsula, including the southern branch of the Iberian Massif, has recently been the subject of several magnetotelluric (MT) studies. This area is made up of three different tectonic terranes: the South Portuguese Zone (SPZ), the Ossa Morena Zone (OMZ) and the Central Iberian Zone (CIZ). The boundaries between these zones are considered to be sutures, which appear as high electrical conductivity anomalies in the MT surveys. The OMZ is characterised by a conductive layer at middle-lower crustal levels. To investigate the continuity of this conductive layer into the CIZ, a new MT profile was carried out. This 75-km long ENE profile goes through the boundary between the OMZ and the CIZ. The results of a two-dimensional magnetotelluric inversion revealed a high-conductivity anomaly in the transition OMZ/CIZ (the so-called Central Unit), which is interpreted as due to interconnected graphite along shear planes. High-conductivity anomalies appeared in the middle crust of the CIZ, whose geometry and location are consistent with the conductive layer previously found in the OMZ, thus confirming the prolongation of the conductive layer into the CIZ. The top of this layer correlated spatially with a broad reflector detected by a seismic profile previously acquired in the same area. This, together with other geological and petrological evidence, points to a common origin for both features.

Deep crustal electromagnetic structure of Bhuj earthquake region (India) and its implications

The existence of fluids and partial melt in the lower crust of the seismically active Kutch rift basin (on the western continental margin of India) owing to underplating has been proposed in previous geological and geophysical studies. This hypothesis is examined using magnetotelluric (MT) data acquired at 23 stations along two profiles across Kutch Mainland Uplift and Wagad Uplift. A detailed upper crustal structure is also presented using twodimensional inversion of MT data in the Bhuj earthquake (2001) area. The prominent boundaries of reflection in the upper crust at 5, 10 and 20 km obtained in previous seismic reflection profiles correlate with conductive structures in our models. The MT study reveals 1-2 km thick Mesozoic sediments under the Deccan trap cover. The Deccan trap thickness in this region varies from a few meters to 1.5 km. The basement is shallow on the northern side compared to the south and is in good agreement with geological models as well as drilling information. The models for these profiles indicate that the thickness of sediments would further increase southwards into the Gulf of Kutch. Significant findings of the present study indicate 1) the hypocentre region of the earthquake is devoid of fluids, 2) absence of melt (that is emplaced during rifting as suggested from the passive seismological studies) in the lower crust and 3) a low resistive zone in the depth range of 5-20 km. The present MT study rules out fluidsand melt (magma) as the causative factors that triggered the Bhuj earthquake. The estimated porosity value of 0.02% will explain 100-500 ohm·m resistivity values observed in the lower crust. Based on the seismic velocities and geochemical studies, presence of garnet is inferred. The lower crust consists of basalts - probably generated by partial melting of metasomatised garnet peridotite at deeper depths in the lithosphere - and their composition might be modified by reaction with the spinel peridotites.

Estimating the apparent transverse relaxation time (R2(*)) from images with different contrasts (ESTATICS) reduces motion artifacts.

Relaxation rates provide important information about tissue microstructure. Multi-parameter mapping (MPM) estimates multiple relaxation parameters from multi-echo FLASH acquisitions with different basic contrasts, i.e., proton density (PD), T1 or magnetization transfer (MT) weighting. Motion can particularly affect maps of the apparent transverse relaxation rate R2(*), which are derived from the signal of PD-weighted images acquired at different echo times. To address the motion artifacts, we introduce ESTATICS, which robustly estimates R2(*) from images even when acquired with different basic contrasts. ESTATICS extends the fitted signal model to account for inherent contrast differences in the PDw, T1w and MTw images. The fit was implemented as a conventional ordinary least squares optimization and as a robust fit with a small or large confidence interval. These three different implementations of ESTATICS were tested on data affected by severe motion artifacts and data with no prominent motion artifacts as determined by visual assessment or fast optical motion tracking. ESTATICS improved the quality of the R2(*) maps and reduced the coefficient of variation for both types of data-with average reductions of 30% when severe motion artifacts were present. ESTATICS can be applied to any protocol comprised of multiple 2D/3D multi-echo FLASH acquisitions as used in the general research and clinical setting.