Studio di fenomeni d'instabilità gravitativa sui fondali marini, con particolare riferimento all'isola di Stromboli

In the last decade the interest for submarine instability grew up, driven by the increasing exploitation of natural resources (primary hydrocarbons), the emplacement of bottom-lying structures (cables and pipelines) and by the development of coastal areas, whose infrastructures increasingly protrude to the sea. The great interest for this topic promoted a number of international projects such as: STEAM (Sediment Transport on European Atlantic Margins, 93-96), ENAM II (European North Atlantic Margin, 96-99), GITEC (Genesis and Impact of Tsunamis on the European Coast 92-95), STRATAFORM (STRATA FORmation on Margins, 95-01), Seabed Slope Process in Deep Water Continental Margin (Northwest Gulf of Mexico, 96-04), COSTA (Continental slope Stability, 00-05), EUROMARGINS (Slope Stability on Europe’s Passive Continental Margin), SPACOMA (04-07), EUROSTRATAFORM (European Margin Strata Formation), NGI's internal project SIP-8 (Offshore Geohazards), IGCP-511: Submarine Mass Movements and Their Consequences (05-09) and projects indirectly related to instability processes, such as TRANSFER (Tsunami Risk ANd Strategies For the European region, 06-09) or NEAREST (integrated observations from NEAR shore sourcES of Tsunamis: towards an early warning system, 06-09). In Italy, apart from a national project realized within the activities of the National Group of Volcanology during the framework 2000-2003 “Conoscenza delle parti sommerse dei vulcani italiani e valutazione del potenziale rischio vulcanico”, the study of submarine mass-movement has been underestimated until the occurrence of the landslide-tsunami events that affected Stromboli on December 30, 2002. This event made the Italian Institutions and the scientific community more aware of the hazard related to submarine landslides, mainly in light of the growing anthropization of coastal sectors, that increases the vulnerability of these areas to the consequences of such processes. In this regard, two important national projects have been recently funded in order to study coastal instabilities (PRIN 24, 06-08) and to map the main submarine hazard features on continental shelves and upper slopes around the most part of Italian coast (MaGIC Project). The study realized in this Thesis is addressed to the understanding of these processes, with particular reference to Stromboli submerged flanks. These latter represent a natural laboratory in this regard, as several kind of instability phenomena are present on the submerged flanks, affecting about 90% of the entire submerged areal and often (strongly) influencing the morphological evolution of subaerial slopes, as witnessed by the event occurred on 30 December 2002. Furthermore, each phenomenon is characterized by different pre-failure, failure and post-failure mechanisms, ranging from rock-falls, to turbidity currents up to catastrophic sector collapses. The Thesis is divided into three introductive chapters, regarding a brief review of submarine instability phenomena and related hazard (cap. 1), a “bird’s-eye” view on methodologies and available dataset (cap. 2) and a short introduction on the evolution and the morpho-structural setting of the Stromboli edifice (cap. 3). This latter seems to play a major role in the development of largescale sector collapses at Stromboli, as they occurred perpendicular to the orientation of the main volcanic rift axis (oriented in NE-SW direction). The characterization of these events and their relationships with successive erosive-depositional processes represents the main focus of cap.4 (Offshore evidence of large-scale lateral collapses on the eastern flank of Stromboli, Italy, due to structurally-controlled, bilateral flank instability) and cap. 5 (Lateral collapses and active sedimentary processes on the North-western flank of Stromboli Volcano), represented by articles accepted for publication on international papers (Marine Geology). Moreover, these studies highlight the hazard related to these catastrophic events; several calamities (with more than 40000 casualties only in the last two century) have been, in fact, the direct or indirect result of landslides affecting volcanic flanks, as observed at Oshima-Oshima (1741) and Unzen Volcano (1792) in Japan (Satake&Kato, 2001; Brantley&Scott, 1993), Krakatau (1883) in Indonesia (Self&Rampino, 1981), Ritter Island (1888), Sissano in Papua New Guinea (Ward& Day, 2003; Johnson, 1987; Tappin et al., 2001) and Mt St. Augustine (1883) in Alaska (Beget& Kienle, 1992). Flank landslide are also recognized as the most important and efficient mass-wasting process on volcanoes, contributing to the development of the edifices by widening their base and to the growth of a volcaniclastic apron at the foot of a volcano; a number of small and medium-scale erosive processes are also responsible for the carving of Stromboli submarine flanks and the transport of debris towards the deeper areas. The characterization of features associated to these processes is the main focus of cap. 6; it is also important to highlight that some small-scale events are able to create damage to coastal areas, as also witnessed by recent events of Gioia Tauro 1978, Nizza, 1979 and Stromboli 2002. The hazard potential related to these phenomena is, in fact, very high, as they commonly occur at higher frequency with respect to large-scale collapses, therefore being more significant in terms of human timescales. In the last chapter (cap. 7), a brief review and discussion of instability processes identified on Stromboli submerged flanks is presented; they are also compared with respect to analogous processes recognized in other submerged areas in order to shed lights on the main factors involved in their development. Finally, some applications of multibeam data to assess the hazard related to these phenomena are also discussed.

Sensitivity analysis of a parabolic-elliptic problem

We consider the heat flux through a domain with subregions in which the thermal capacity approaches zero. In these subregions the parabolic heat equation degenerates to an elliptic one. We show the well-posedness of such parabolic-elliptic differential equations for general non-negative L-infinity-capacities and study the continuity of the solutions with respect to the capacity, thus giving a rigorous justification for modeling a small thermal capacity by setting it to zero. We also characterize weak directional derivatives of the temperature with respect to capacity as solutions of related parabolic-elliptic problems.

Analisi dell'accrescimento giornaliero della Sardina pilchardus nel Canale di Sicilia

Lo studio effettuato riguarda l’accrescimento giornaliero della Sardina pilchardus, (Walbaum, 1792) tramite la lettura degli anelli di crescita giornaliera negli otoliti. Nel Mediterraneo centrale il lavoro svolto è il primo di questo tipo su S. pilchardus. Il campionamento è avvenuto durante la campagna oceanografica "Anchevatir 2012", 69 otoliti sono stati estratti da esemplari con lunghezza totale compresa tra 7 ed 12.5 cm e successivamente sottoposti ad inclusione, sezionamento e levigatura per la realizzazione di sezioni sottili. Sull’intero campione è stata stimata l’età con due metodi: lettura degli anelli giornalieri sotto microscopio e conteggio dei microincrementi tramite analisi d’immagine. L’età stimata è compresa tra i 90 e 230 giorni, tuttavia la maggior parte degli individui presenta un’età tra i 120 e 150 giorni. Inoltre è stata determinata la data di nascita degli esemplari, avvenuta tra Dicembre 2011 e Febbraio 2012. In seguito è stata condotta un’analisi della media dell’ampiezza degli incrementi per descrivere i pattern di crescita giornaliera: l’andamento risultante è crescente con il procedere dell’età fino a circa il 50° giorno, poi si stabilizza fino al 150°, infine i valori medi decrescono. La backcalculation ha permesso di stimare il tasso di accrescimento giornaliero della lunghezza del corpo. Sono state analizzate tre serie distinte per data di nascita (Dicembre 2011, Gennaio 2012 e Febbraio 2012); queste hanno mostrato pattern di accrescimento analogo. La crescita iniziale stimata è di 0.2 mm/d, raggiunge 0.6 mm/d intorno al 40° giorno, ed oltre il 100° si è osservato un decremento nell’accrescimento giornaliero, soprattutto nella serie di Dicembre. Le differenze più rilevanti nei pattern delle tre serie mensili sono state riscontrate nei valori medi fra Dicembre e Febbraio. L’analisi della temperatura media superficiale ha permesso di ipotizzare che questa crescita maggiore degli individui nati in Febbraio sia collegata all’aumento di temperatura registrato da Marzo in poi. Tale risultato suggerisce che le condizioni ambientali e quindi i ritmi metabolici e d’accrescimento nei mesi successivi a Febbraio sono più favorevoli rispetto ai mesi invernali.

Ringier (Familie)

Famille de pasteurs, politiciens et entrepreneurs de Zofingue, attestée pour la première fois en 1527, lorsque leur aïeul Jean, tonnelier originaire de Nîmes, obtint la bourgeoisie de Zofingue. Michael (1521-1605), avoyer, l'un de ses cinq fils, est l'ancêtre de la branche des imprimeurs et éditeurs. Après lui, de nombreux R. consolidèrent durablement l'influence de la famille. A partir du XVIIIe s., divers membres firent des carrières politiques, tels Samuel (1706-1786), avoyer, et Rudolf Friedrich (1805-1886), président de la ville. Les R. furent aussi très liés à l'Eglise. Le fils de Michael, Moritz (1557-1615), fut pasteur et doyen à Zofingue. Jusqu'au XIXe s., la famille compta une trentaine d'ecclésiastiques, essentiellement des pasteurs officiant sur le territoire bernois, tels Johann Heinrich ( -> 3) et Michael ( -> 8). Les conseillers Beat (1712-1778) et Niklaus (1734-1766) furent les premiers R. actifs dans la production protoindustrielle de drap. D'autres négociants suivirent jusqu'au milieu du XIXe s. L'architecte Niklaus Emanuel (1744-1815) construisit l'hôtel de ville de Zofingue (1792-1795) de style baroque tardif. Johann Rudolf ( -> 4) se distingua sous la République helvétique (1798-1803). Samuel (1767-1826), conseiller municipal de Zofingue, créa les armoiries du canton d'Argovie en 1803. Les R. s'affirmèrent sur le plan cantonal avec Karl Ludwig ( -> 6), chancelier, et Arnold ( -> 1), conseiller d'Etat et plusieurs fois landamman, et sur le plan fédéral avec Johann Rudolf ( -> 5), conseiller national, et Gottlieb ( -> 2), conseiller aux Etats et chancelier de la Confédération. Johann Rudolf (1803-1874) fonda, en 1833, l'imprimerie Ringier à Zofingue, reprise par son fils Franz Emil (1837-1898). A partir de 1898, Paul August ( -> 9), représentant de la troisième génération d'imprimeurs, agrandit l'entreprise dont il fit la principale imprimerie et maison d'édition de Suisse. Cette expansion se poursuivit après 1960 sous son fils Hans (1906-2003). Avec les fils de celui-ci, Christoph (naissance1941, dans la firme jusqu'en 1991) et Michael (naissance1949), Ringier devint, à partir de 1985, une entreprise multinationale et multimédia. Bibliographie – F. Schoder, Ortsbürger von Zofingen, 1962 – P. Meier, T. Häussler, Zwischen Masse, Markt und Macht, 2009

Novel baroreflex activation therapy in resistant hypertension: results of a European multi-center feasibility study

This study assessed the safety and efficacy of a novel implantable device therapy in resistant hypertension patients.

Coronary optical frequency domain imaging (OFDI) for in vivo evaluation of stent healing: comparison with light and electron microscopy

Coronary late stent thrombosis, a rare but devastating complication, remains an important concern in particular with the increasing use of drug-eluting stents. Notably, pathological studies have indicated that the proportion of uncovered coronary stent struts represents the best morphometric predictor of late stent thrombosis. Intracoronary optical frequency domain imaging (OFDI), a novel second-generation optical coherence tomography (OCT)-derived imaging method, may allow rapid imaging for the detection of coronary stent strut coverage with a markedly higher precision when compared with intravascular ultrasound, due to a microscopic resolution (axial approximately 10-20 microm), and at a substantially increased speed of image acquisition when compared with first-generation time-domain OCT. However, a histological validation of coronary OFDI for the evaluation of stent strut coverage in vivo is urgently needed. Hence, the present study was designed to evaluate the capacity of coronary OFDI by electron (SEM) and light microscopy (LM) analysis to detect and evaluate stent strut coverage in a porcine model.

Characterization of the first FGFRL1 mutation identified in a craniosynostosis patient

Fibroblast growth factor receptor-like 1 (FGFRL1) is a recently discovered transmembrane protein whose functions remain unclear. Since mutations in the related receptors FGFR1-3 cause skeletal malformations, DNA samples from 55 patients suffering from congenital skeletal malformations and 109 controls were searched for mutations in FGFRL1. One patient was identified harboring a frameshift mutation in the intracellular domain of this novel receptor. The patient showed craniosynostosis, radio-ulnar synostosis and genital abnormalities and had previously been diagnosed with Antley-Bixler syndrome. The effect of the FGFRL1 mutation was studied in vitro. In a reporter gene assay, the wild-type as well as the mutant receptor inhibited FGF signaling. However, the mutant protein differed from the wild-type protein in its subcellular localization. Mutant FGFRL1 was mainly found at the plasma membrane where it interacted with FGF ligands, while the wild-type protein was preferentially located in vesicular structures and the Golgi complex. Two motifs from the intracellular domain of FGFRL1 appeared to be responsible for this differential distribution, a tandem tyrosine based motif and a histidine-rich sequence. Deletion of either one led to the preferential redistribution of FGFRL1 to the plasma membrane. It is therefore likely that mutant FGFRL1 contributes to the skeletal malformations of the patient.

Toward a Better World: Finnish Utopian Communities since 1972

The utopian communities of Finns are linked to world history and the great ideological foundations behind numerous utopian endeavors. In the paper, Finnish utopian communities will be described, compared, and contrasted by their ideological backgrounds and in a global context. In addition, the reasons for the dissolution of these settlements are analyzed. Even though the Finnish utopian communities are not often mentioned together with More's Utopia, or with Fourier, Owen, Cabet, or Oneida, they have an interesting history reaching back to the 1792 “New Jerusalem” plan in Sierra Leone. While the best-known Finnish utopian ventures are Sointula in Canada (1901-1905) and Colonia Finlandesa (1906-1940) in Argentina there were, however, almost twenty similar Finnish ventures around the world based on nationalism, utopian socialism, cooperative movements, “tropic fevers,” and religious ideas.