Neoproterozoic to middle Palaeozoic evolution of the Central Asian Orogenic Belt in south-central Mongolia: chronological and geochemical perspectives

Mongolia occupies a central position within the eastern branch of the large accretionary Central Asian Orogenic Belt (CAOB) or Altaids. The present work aims to outline the geodynamic environment and possible evolution of this part of the eastern CAOB, predominantly from the Cambrian to the middle Palaeozoic. The investigation primarily focussed on zircon geochronology as well as whole-rock geochemical and Sm–Nd isotopic analyses for a variety of metaigneous rocks from the southern Hangay and Gobi-Altai regions in south-central Mongolia. The southern slope of the Hangay Mountains in central Mongolia exposes a large NWSE-trending middle Neoproterozoic ophiolitic complex (c. 650 Ma), which is tectonically integrated within an accretionary complex developed between the Precambrian Baydrag and Hangay crustal blocks. Formation of the entire accretionary system along the north-eastern margin of the Baydrag block mainly occurred during the early Cambrian, but convergence within this orogenic zone continued until the early Ordovician, because of on-going southward subduction-accretion of the Baydrag block. An important discovery is the identification of a late Mesoproterozoic to early Neoproterozoic belt within the northern Gobi-Altai that was reworked during the late Cambrian and throughout the late Ordovician/Devonian. Early Silurian low-grade mafic and felsic metavolcanic rocks from the northern Gobi-Altai display subduction-related geochemical features and highly heterogeneous Nd isotopic compositions, which suggest an origin at a mature active continental margin. Early Devonian protoliths of granodioritic and mafic gneisses from the southern Gobi-Altai display geochemical and Nd isotopic compositions compatible with derivation and evolution from predominantly juvenile crustal and mantel sources and these rocks may have been emplaced within the outboard portion of the late Ordovician/early Silurian active continental margin. Moreover, middle Devonian low-grade metavolcanic rocks from the southwestern Gobi-Altai yielded geochemical and Nd isotopic data consistent with emplacement in a transitional arc-backarc setting. The combined U–Pb zircon ages and geochemical data obtained from the Gobi-Altai region suggest that magmatism across an active continental margin migrated oceanwards through time by way of subduction zone retreat throughout the Devonian. Progressive extension of the continental margin was associated with the opening of a backarc basin and culminated in the late Devonian with the formation of a Japan-type arc front facing a southward open oceanic realm (present-day coordinates).

Studio della sicurezza stradale nelle zone di transizione: gli interventi sulla sp 610 "selice-montanara"

Studio della sicurezza stradale nelle zone di transizione: gli interventi sulla sp 610 "selice-montanara"

Biologia riproduttiva di Paracentrotus lividus (Lamarck, 1816) in due zone della Sardegna

Paracentrotus lividus è un echinoderma bentonico marino appartenente alla classe Echinoidea, comune in tutto il Mar Mediterraneo e lungo le coste atlantiche dalla Scozia al Marocco. Questa specie è estremamente importante dal punto di vista ecologico in quanto specie chiave nella strutturazione della comunità bentonica macroalgale. Inoltre in tempi recenti il mercato delle sue gonadi ha subito una forte espansione rendendolo una specie di interesse economico in numerosi paesi europei. Il crescente prelievo sta gradualmente portando al depauperamento della risorsa, per questo motivo il riccio di mare è oggetto di numerosi studi e programmi a fini conservazionistici. Una maggiore conoscenza del ciclo riproduttivo della specie potrebbe risultare utile per una migliore gestione della risorsa. Pertanto, questo studio si propone di indagare sulla biologia di P. lividus in due aree distinte della Sardegna: Su Pallosu, nella Penisola del Sinis Sardegna centro-occidentale, e nell’Area Marina Protetta di Tavolara – Punta Coda Cavallo, Sardegna nordorientale, al fine di far luce sulle dinamiche del ciclo riproduttivo. Le informazioni bibliografiche a riguardo evidenziano l’influenza dei fattori ambientali quali fotoperiodo, idrodinamismo, temperatura e tipologia di pascolo sull’andamento del ciclo biologico e il momento di spawning. Diversi autori hanno osservato in Mar Mediterraneo sia un unico ciclo riproduttivo che due eventi riproduttivi annuali a conferma dell’ampia variabilità dell’andamento gonadico. Nel presente lavoro al fine di mettere in relazione le caratteristiche dell’habitat con il ciclo riproduttivo delle popolazioni in oggetto è stato analizzato l’andamento dell’Indice Gonadosomatico (IGS) su individui di diverse taglie/età, come rapporto fra il peso delle gonadi e il peso dell’individuo; inoltre a conferma dello stadio di maturazione è stata effettuata l’analisi istologica delle gonadi su campioni fissati e inclusi in paraffina, sezionati a 7μm e colorati con ematossilina-eosina prima di essere osservati al microscopio ottico. Mediante analisi d’immagine di foto subacquee utilizzando il programma Seascape è stata caratterizzata la componente macroalgale bentonica e la componente abiotica degli habitat (sabbia e roccia non vegetata) con particolare attenzione al calcolo della percentuale di ricoprimento delle specie vegetali. Inoltre i siti sono stati caratterizzati rispetto all’esposizione dei venti dominanti con elaborazione dei dati del periodo di campionamento per direzione, frequenza e intensità.

Muster und Prozesse in einer Microcebus-Hybridzone in Südostmadagaskar

Im Rahmen dieser Doktorarbeit wurde in zwei Schwerpunktanalysen mit eine Teil- und Gesamtdatensatz die Untersuchung der Hybridisierung zwischen den beiden Microcebus-Arten M. murinus und M. griseorufus im Ökoton Südostmadagaskars umfangreich und vertieft untersucht. Für die genetischen Analysen wurden die maternal vererbte mitochondriale Hypervariable Region I (HVR 1) und neun nukleäre biparental vererbte Mikrosatellitenmarker eingesetzt. Als weiterer Datensatz wurden morphometrische Daten verwendet. Für die erste Schwerpunktanalyse wurde ein bereits vorhandener Teildatensatz (Hapke 2005 & Gligor 2006) mit Daten von insgesamt 162 Individuen aus neun Populationen der Dornbuschzone, der Übergangswaldzone und des Küstenwaldgebietes eingesetzt. In der zweiten Schwerpunktanalyse wurde eine umfangreiche Untersuchung der Microcebus griseoruus-M. murinus- Hybridzone vorgenommen. Für diese detaillierte Charakterisierung der Hybridzone wurde eine ausgedehnte und fein auflösende Probennahme in einem als Kernzone definierten Bereich, der die gesamte Übergangswaldzone und die dazu benachbarten Dornbuschgebiete umfasste, durchgeführt. Die morphometrischen und genetischen Daten der neu beprobten Individuen dieser Kernzone wurden mit den Daten des Teildatensatzes und weiteren Daten aus Küstenwaldpopulationen (Hapke 2005) zu einem Gesamtdatensatz zusammengefasst. Die Integration des Teildatensatzes in den Gesamtdatensatz erforderte umfassende und zeitintensive Labor- und Analysearbeiten, die im Rahmen dieser Doktorarbeit durchgeführt wurden. Der Gesamtdatensatz umfasste insgesamt 569 Individuen der Gattung Microcebus aus 29 Untersuchungsstandorten. Die mit beiden Datensätzen durchgeführte Analyse morphometrischer Daten zeigte deutlich, dass die Mehrzahl der Individuen aus der Übergangswaldzone einen intermediären Morphotyp aufweist. Durch die mit den Daten des Teildatensatzes durchgeführten Bayes’schen Clusteranalysen und Assignment-Tests, das vornehmlich in den Populationen der Übergangszone beobachtete signifikante Kopplungsungleichgewicht und Heterozygotendefizit, die festgestellte Verteilung der mitochondrialen Haplotypen und das kontrastierende Muster zwischen nukleären Mikrosatellitengenotypen und mitochondrialen Haplotypen in den Übergangswaldpopulationen konnte erstmals das Vorkommen einer Hybridzone zwischen Microcebus-Arten wissenschaftlich fundiert festgestellt werden. Die Ergebnisse dieser Schwerpunktanalyse wurden in der Fachzeitschrift Molecular Ecology publiziert (Gligor et al. 2009). Die in der ersten Schwerpunktanalyse festgestellte Hybridzone konnte durch die zweite Schwerpunktanalyse mit den genetischen und morphometrischen Daten des Gesamtdatensatzes nicht nur bestätigt werden, sondern auch auf die gesamte Übergangswaldzone erweitert werden. Ferner wurden starke Hinweise auf eine Hybridisierung beider Microcebus-Arten an einigen Dornbuschstandorten der Kernzone gefunden. Durch die große Datenmenge des Gesamtdatensatzes, vor allem aus der Kernzone des Untersuchungsgebietes, war es möglich eine fundierte Charakterisierung der Microcebus griseoruus-M. murinus- Hybridzone durchzuführen. Die Übereinstimmung der Hybridzone mit dem beobachteten Vegetationsmosaik zusammen mit den Ergebnissen der PCA, der PCoA und der Bayes’schen Clusteranalyse sprechen für das Modell der „Mosaik Hybridzone“, während die Einzelbetrachtung der mosaikartig verteilten intermediären Übergangswälder eine hohe Abundanz der Hybride aufzeigte und somit eher das „Bounded Hybrid Superiority model“ unterstützt. Der gewählte geographische Beprobungsmaßstab könnte somit einen Einfluss auf die beobachtete Struktur einer Hybridzone haben. Eines der markantesten Muster in der Hybridzone ist das stark kontrastierende cyto-nukleäre Muster. Der seit ca. 3000 Jahren fortschreitende Klimawandel in Südmadagaskar und die damit verbundene Expansion des Verbreitungsgebietes der Art Microcebus griseorufus nach Osten, das in dieser Arbeit festgestellte „male-biased dispersal“ bei M. griseorufus und der Einfluss exogener Selektion sprechen stark für eine massive asymmetrische nukleäre Genintrogression von M. griseorufus-Allelen in M. murinus-Populationen, verbunden mit einer potentiellen Verdrängung der Art M. murinus aus der Übergangswaldzone. In den jeweiligen Kerngebieten Dornbusch und Küstenwald bleibt jedoch die Diskretheit beider Arten gewahrt.

Granulite facies metamorphism and partial melting processes in the Ivrea Zone, Northern Italy

The Ivrea Zone in northern Italy has been the focus of numerous petrological, geochemical and structural studies. It is commonly inferred to represent an almost complete section through the mid to lower continental crust, in which metamorphism and partial melting of the abundant metapelites was the result of magmatic underplating by a large volume of mantle-derived magma. This study concerns amphibolite and granulite facies metamorphism in the Ivrea Zone with focus on metapelites and metapsammites/metagreywackes from Val Strona di Omegna and metapelites from Val Sesia and Val Strona di Postua, with the aim to better constrain their metamorphic evolution as well as their pressure and temperature conditions via phase equilibria modelling.rnrnIn Val Strona di Omegna, the metapelites show a structural and mineralogical change from mica-schists with the common assemblage bi-mu-sill-pl-q-ilm ± liq at the lowest grades, through metatexitic migmatites (g-sill-bi-ksp-pl-q-ilm-liq) at intermediate grades, to complex diatexitic migmatites (g-sill-ru-bi-ksp-pl-q-ilm-liq) at the highest grades. Within this section several mappable isograds occur, including the first appearance of K-feldspar in the metapelites, the first appearance of orthopyroxene in the metabasites and the disappearance of prograde biotite from the metapelites. The inferred onset of partial melting in the metapelites occurs around Massiola. The prograde suprasolidus evolution of the metapelites is consistent with melting via the breakdown of first muscovite then biotite. Maximum modelled melt fractions of 30–40 % are predicted at the highest grade. The regional metamorphic field gradient in Val Strona di Omegna is constrained to range from conditions of 3.5–6.5 kbar at T = 650–730 °C to P > 9 kbar at T > 900 °C. The peak P–T estimates, particularly for granulite facies conditions, are significantly higher (around 100 °C) than those of most previous studies. In Val Sesia and Val Strona di Postua to the south the exposure is more restricted. P–T estimates for the metapelites are 750–850 °C and 5–6.5 kbar in Val Sesia and approximately 800–900 °C and 5.5–7 kbar in Val Strona di Postua. These results show similar temperatures but lower pressure than metapelites in Val Strona di Omegna. Metapelites in Val Sesia in contact with the Mafic Complex exhibit a metatexitic structure, while in Val Strona di Postua diatexitic structures occur. Further, metapelites at the contact with the Mafic Complex contain cordierite (± spinel) that overprint the regional metamorphic assemblages and are interpreted to have formed during contact metamorphism related to intrusion of the Mafic Complex. The lower pressures in the high-grade rocks in Val Sesia and Val Strona di Postua are consistent with some decompression from the regional metamorphic peak prior to the intrusion of the Mafic Complex, suggesting the rocks followed a clockwise P–T path. In contrast, the metapelites in Val Strona di Omegna, especially in the granulite facies, do not contain any cordierite or any evidence for a contact metamorphic overprint. The extrapolated granulite facies mineral isograds are cut by the rocks of the Mafic Complex to the south. Therefore, the Mafic Complex cannot have caused the regional metamorphism and it is unlikely that the Mafic Complex occurs in Val Strona di Omegna.

L’interprete nelle zone di conflitto: situazione attuale e prospettive per il futuro

In quest'elaborato si affronterà l'analisi dell'interprete nelle zone di conflitto, una figura che è sempre più al centro dell'interesse di media internazionali, studenti e professori. Dopo un'introduzione al ruolo e alle funzioni dell'interprete, si analizzerà la tipologia dell'interpretazione di comunità e, successivamente, si punteranno i riflettori sull'interprete nelle aree instabili del pianeta. Particolare rilievo verrà dato a come muti la sua immagine a seconda delle varie parti in guerra e quanto la sua vita sia molto spesso in pericolo. In conclusione, si analizzeranno i progetti di alcune università di interpretazione che hanno risposto piuttosto prontamente alla necessità di una formazione professionalizzante per le figure di interpreti e mediatori interculturali nelle aree sensibili della terra, senza dimenticare le iniziative internazionali volte alla loro protezione.

Le Zone Franche Urbane: Mercato europeo e Ordinamenti tributari

Lo studio delle Zone Franche Urbane all’interno del Diritto tributario europeo non ha potuto prescindere da una introduttiva delimitazione del lavoro, capace di distinguere le diverse tipologie di zone franche esistenti nei Paesi intra/extra Ue. Attraversando i casi-studio di Madeira, delle Azzorre, fino alla istituenda Zona Franca di Bruxelles, Zone d’Economie Urbaine stimulée (ZEUS), si è giunti alla constatazione dell’assenza di una definizione di Zona Franca Urbana: analizzando le esperienze normative vissute in Francia e in Italia, si è potuto tratteggiare il profilo territoriale, soggettivo e oggettivo del sistema agevolativo rivolto al recupero delle aree urbane degradate. La funzione strumentale della fiscalità, esplicitata per mezzo delle ZFU, ha condotto ad una verifica di diritto interno per controllare la legittimità delle scelte nazionali in ragione dei principi costituzionali nazionali, come anche una di diritto europeo per evitare che le scelte nazionali, anche se legittime sul piano interno, possano per gli stessi effetti incentivanti alle attività d'impresa presentarsi come una forma territoriale di aiuti di Stato fiscali. Evidenziando il rapporto tra le ZFU e il Mercato europeo si è voluto, da un lato, effettuare una ricostruzione sistemica necessaria per un’interpretazione delle ZFU che metta in luce le componenti di tale strumento orientate al perseguimento di un interesse socioeconomico, che in prima battuta generi una contraddizione, una deroga ai principi costituzionali e comunitari, per poi “sciogliersi” in una coerente applicazione degli stessi; dall’altro, tentare di elevare le ZFU a misura sistemica dell’Ordinamento europeo. Si è svolto, infine, un ragionamento in termini di federalismo fiscale con riferimento alle ZFU, trovando una adeguata collocazione nel percorso di devoluzione intrapreso dal legislatore nazionale, avendo quali interlocutori privilegiati le Regioni a Statuto Speciale.

Stratigraphic study and analysis of the barchan dunefield of the Laguna coastal zone in Santa Catarina, Brazil

The association of several favorable factors has resulted in the development of a wide barchan dune field that stands out as a fundamental element in the coastal landscape of southern Santa Catarina state in Brazil. This original ecosystem is being destroyed and highly modified, due to urbanization. This work identifies and discusses its basic characteristics and analyzes the favorable factors for its preservation, in the foreseen of both a sustainable future and potential incomes from ecotourism. The knowledge of the geologic evolution allows to associate this transgressive Holocene dunes formation to more dissipative beach conditions. Spatial differences on morphodynamics are related to local and regional contrasts in the sediment budget, with an influence on gradients of wave attenuation in the inner shelf and consequently with influence in the level of coastal erosion. The link between relative sea level changes and coastal eolian sedimentation can be used to integrate coastal eolian systems to the sequence stratigraphy model. The main accumulation phase of eolian sediments would occur during the final transgressive and highstand systems tracts. Considering the global character of Quaternary relative sea level changes, the Laguna transgressive dune field should be correlated with similar eolian deposits developed along other parts of the Brazilian coast compatibles with the model of dunefield initiation during rising and highstand sea level phases.

Studio e progettazione di un capannone ad alta mobilità e facilità di montaggio per zone terremotate

Capannone ad alta mobilità e facilità di montaggio per zone terremotate.

Observations and modeling of the Marginal Ice Zone

Global climate change in recent decades has strongly influenced the Arctic generating pronounced warming accompanied by significant reduction of sea ice in seasonally ice-covered seas and a dramatic increase of open water regions exposed to wind [Stephenson et al., 2011]. By strongly scattering the wave energy, thick multiyear ice prevents swell from penetrating deeply into the Arctic pack ice. However, with the recent changes affecting Arctic sea ice, waves gain more energy from the extended fetch and can therefore penetrate further into the pack ice. Arctic sea ice also appears weaker during melt season, extending the transition zone between thick multi-year ice and the open ocean. This region is called the Marginal Ice Zone (MIZ). In the Arctic, the MIZ is mainly encountered in the marginal seas, such as the Nordic Seas, the Barents Sea, the Beaufort Sea and the Labrador Sea. Formed by numerous blocks of sea ice of various diameters (floes) the MIZ, under certain conditions, allows maritime transportation stimulating dreams of industrial and touristic exploitation of these regions and possibly allowing, in the next future, a maritime connection between the Atlantic and the Pacific. With the increasing human presence in the Arctic, waves pose security and safety issues. As marginal seas are targeted for oil and gas exploitation, understanding and predicting ocean waves and their effects on sea ice become crucial for structure design and for real time safety of operations. The juxtaposition of waves and sea ice represents a risk for personnel and equipment deployed on ice, and may complicate critical operations such as platform evacuations. The risk is difficult to evaluate because there are no long-term observations of waves in ice, swell events are difficult to predict from local conditions, ice breakup can occur on very short time-scales and wave-ice interactions are beyond the scope of current forecasting models [Liu and Mollo-Christensen, 1988,Marko, 2003]. In this thesis, a newly developed Waves in Ice Model (WIM) [Williams et al., 2013a,Williams et al., 2013b] and its related Ocean and Sea Ice model (OSIM) will be used to study the MIZ and the improvements of wave modeling in ice infested waters. The following work has been conducted in collaboration with the Nansen Environmental and Remote Sensing Center and within the SWARP project which aims to extend operational services supporting human activity in the Arctic by including forecast of waves in ice-covered seas, forecast of sea-ice in the presence of waves and remote sensing of both waves and sea ice conditions. The WIM will be included in the downstream forecasting services provided by Copernicus marine environment monitoring service.

Stability of Contour Augmentation and Esthetic Outcomes of Implant Supported Single Crowns in the Esthetic Zone. 3-Year Results of a Prospective Study With Early Implant Placement Post Extraction

Early implant placement is one of the treatment options after tooth extraction. Implant surgery is performed after a healing period of 4 to 8 weeks and combined with a simultaneous contour augmentation using the guided bone regeneration technique to rebuild stable esthetic facial hard- and soft-tissue contours.

Genome-wide DNA profiling of marginal zone lymphomas identifies subtype-specific lesions with an impact on the clinical outcome

Marginal zone B-cell lymphomas (MZLs) have been divided into 3 distinct subtypes (extranodal MZLs of mucosa-associated lymphoid tissue [MALT] type, nodal MZLs, and splenic MZLs). Nevertheless, the relationship between the subtypes is still unclear. We performed a comprehensive analysis of genomic DNA copy number changes in a very large series of MZL cases with the aim of addressing this question. Samples from 218 MZL patients (25 nodal, 57 MALT, 134 splenic, and 2 not better specified MZLs) were analyzed with the Affymetrix Human Mapping 250K SNP arrays, and the data combined with matched gene expression in 33 of 218 cases. MALT lymphoma presented significantly more frequently gains at 3p, 6p, 18p, and del(6q23) (TNFAIP3/A20), whereas splenic MZLs was associated with del(7q31), del(8p). Nodal MZLs did not show statistically significant differences compared with MALT lymphoma while lacking the splenic MZLs-related 7q losses. Gains of 3q and 18q were common to all 3 subtypes. del(8p) was often present together with del(17p) (TP53). Although del(17p) did not determine a worse outcome and del(8p) was only of borderline significance, the presence of both deletions had a highly significant negative impact on the outcome of splenic MZLs.

"Device landing zone" calcification, assessed by MSCT, as a predictive factor for pacemaker implantation after TAVI

After trans-catheter aortic valve implantation (TAVI), the need for postinterventional pacemaker (PM) implantation can occur in as many as 10-50% of cases, but it is not yet clear, how this need can be predicted. The aim of this study was to assess the possible predictive factors of post TAVI PM implantation based on Computed Tomography (CT) measured aortic valve calcification and its distribution.

Correlation of Device landing zone calcification and acute procedural success in patients undergoing transcatheter aortic valve implantations with the self-expanding CoreValve prosthesis

The aim of this study was to assess the influence of amount and distribution of calcifications of the aortic valve and the left ventricular outflow tract on the acute procedural outcome of patients undergoing transcatheter aortic valve implantation (TAVI).