Stratigraphy and Palaeontology of the Late Cretaceous Wapiti Formation, west-central Alberta, Canada

A complete stratigraphic assessment and revision of the middle Campanian to upper Maastrichtian Wapiti Formation in north-western Alberta and north-eastern British Columbia is the main aim of this research project. The study area encompasses an area of approximately 200X180 km in the Grande Prairie County (west-central Alberta) and easternmost British Columbia, Canada. Results presented here indicate that the 1300m thick succession currently reported in the literature as “undifferentiated lithostratigraphic unit”, consists of five lithostratigraphic units and four unconformity-bounded depositional sequences; their study and description have been documented integrating several geological disciplines, including sequence stratigraphic methods, well-log signatures, facies analysis, and fossil associations. On the whole, particular attention has been given to 1) age and nature of both basal and upper contacts of the Wapiti Formation, 2) effective mappability of lithostratigraphic units and depositional sequences in western Alberta, and 3) the identification of previously undetermined maximum flooding surface of the Bearpaw seaway and Drumheller Marine Tongue, which are reference marine unit in central and southern Alberta. A second, but not less important, guideline for the project has been the rich paleontological record of the Wapiti deposits. Detailed paleoenvironmental and taxonomical information on old and new finds have been the base for correlation with well known associations of Alaska, southern Alberta, and Montana. Newly discovered rich fossil localities documented an extraordinarily diverse fauna during the latest Cretaceous, including dinosaurs, squamates, and fresh-water fishes and reptiles. Lastly, in order to better characterize the Wapiti Formation, major marker beds were described: these include several bentonites (altered volcanic ash deposits) which have been documented over an area of almost 30.000 km2, as well as four major coal zones, characterized by tabular coal seams with an overall thickness of 2 meters. Such marker beds represent a formidable tool for high-resolution chronology and regional correlations within the Late Cretaceous Alberta foreland basin.

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.

Untersuchung des murinen, nukleären pSS- und SLE-Autoantigens La/SS-B unter physiologischen und pathophysiologischen Bedingungen

Zusammenfassung der Dissertation von Christian Schörner 'Untersuchung des murinen, nukleären pSS- und SLE-Autoantigens La/SS-B unter physiologischen und pathophysiologischen Bedingungen' am Fachbereich Biologie der Johannes Gutenberg-Universität Mainz Seren von Patienten mit Kollagenosen, wie SLE und pSS, enthalten Antikörper gegen das Autoantigen La/SS-B. Im murinen Tiermodell musste die Expression des La/SS-B verstanden werden. Das murine Strukturgen codierte für 13 Exons, das Start-AUG befand sich im Exon 2. Die alternativen mRNAs unterschieden sich nur in ihrer 5'-UTR. Das Exon 1b war im Vergleich zum Exon 1a am 3'-Ende um 27 Nukleotide verlängert. Die alternativen mRNAs entstanden durch einen Promotorwechsel in Kombination mit einem alternativen Spleißvorgang. Die Polyadenylierung erfolgte an zwei alternativen Polyadenylierungssequenzen. Die mRNAs waren vollständig gesplissen, zytoplasmatisch und funktionell. Die Exon 1a- und die Exon 1c-mRNA wurden ubiquitär exprimiert, die Exon 1b-mRNA dagegen nur in proliferierenden Zellen. Im C-Terminus fand sich eine Nager-spezifische Insertion sowie eine -deletion. Das Protein besaß mit 16 isoelektrischen Proteinformen eine hohe Ladungsheterogenität. NO steigerte die Proteinexpression um das 5fache und bewirkte eine Translokation des Proteins vom Zellkern in das Zytoplasma. Das humane La/SS-B-Neoepitop induzierte in Versuchstieren die Bildung von Antikörper gegen das Neoepitop und natives La/SS-B.

Preliminary studies for the establishment of a tsunami early detection algorithm to be used in the frame of a Tsunami Warning System

This thesis presents and discusses TEDA, an algorithm for the automatic detection in real-time of tsunamis and large amplitude waves on sea level records. TEDA has been developed in the frame of the Tsunami Research Team of the University of Bologna for coastal tide gauges and it has been calibrated and tested for the tide gauge station of Adak Island, in Alaska. A preliminary study to apply TEDA to offshore buoys in the Pacific Ocean is also presented.

Valutazione dell'impatto della farmacogenetica in ambito di Sanità Pubblica. Analisi del polimorfismo genetico dell'enzima CYP2D6 metabolizzante xenobiotici.

Pharmacogenetic testing provides an outstanding opportunity to improve prescribing safety and efficacy. In Public health policy pharmacogenetics is relevant for personalized therapy and to maximize therapeutic benefit minimizing adverse events. CYP2D6 is known to be a key enzyme responsible for the biotransformation of about 25-30% of extensively used drugs and genetic variations in genes coding for drug-metabolizing enzymes might lead to adverse drug reactions, toxicity or therapeutic failure of pharmacotherapy. Significant interethnic differences in CYP2D6 allele distribution are well established, but immigration is reshaping the genetic background due to interethnic admixture which introduces variations in individual ancestry resulting in distinct level of population structure. The present thesis deals with the genetic determination of the CYP2D6 alleles actually present in the Emilia-Romagna resident population providing insights into the admixture process. A random sample of 122 natives and 175 immigrants from Africa, Asia and South America where characterized considering the present scenario of migration and back migration events. The results are consistent with the known interethnic genetic variation, but introduction of ethnic specific variants by immigrants predicts a heterogeneous admixed population scenario requiring, for drugs prescription and pharmacogenetics studies, an interdisciplinary approach applied in a properly biogeographical and anthropological frame. To translate pharmacogenetics knowledge into clinical practice requires appropriated public health policies, possibly guiding clinicians to evaluate prospectively which patients have the greatest probability of expressing a variant genotype.

Atherosklerose und Apoptose

Subendothelial in den Arterienwänden abgelagertes LDL kann einer enzymatischen Modifikation unterliegen, die es in einen cytotoxischen Partikel überführt. In vitro Behandlung von LDL mit Proteasen (Trypsin) und Cholesterinesterase führt zu einem dem läsionalen LDL ähnlichen Produkt. Die Behandlung von humanen Endothelzellen mit enzymatisch verändertem LDL (E-LDL), das einen hohen Gehalt an freiem Cholesterin und freien Fettsäuren aufweist, führt zur Auslösung der Apoptose via ASK1 (apoptosis signal-regulating kinase 1) –abhängiger p38-Phosphorylierung. Durch eine Aktivierung der Effektor-Caspasen-3/-7 kommt es zur Fragmentierung der DNA und zur Spaltung des nukleären Enzyms Poly-(ADP-ribose)-Polymerase. Phosphatidylserin ist an der äußeren Zellmembran mittels Annexin-Bindung detektierbar. Natives oder oxidiertes LDL induziert bei gleicher Konzentration keinen programmierten Zelltod. In Depletions- und Rekonstitutionsexperimenten wurden freie Fettsäuren aus E-LDL als Auslöser der Apoptose identifiziert. In nativem LDL ist der Anteil an freien Fettsäuren gering, deshalb ist das Lipoprotein nicht cytotoxisch. E-LDL induziert weiterhin eine Erhöhung bzw. eine Hemmung der transkriptionellen Aktivität eines AP-1- bzw. NF-κB-Luciferase Reporterplasmids. Die Ausschaltung von ASK1 mittels RNA-Interferenz bzw. die Hemmung von p38 mit dem Inhibitor SB203580 rettet die Zellen vor dem programmierten Zelltod. E-LDL kann in Endothelzellen oxidativen Stress auslösen. Durch Vorbehandlung mit N-Acetyl-Cystein wird die Aktivierung sowohl von ASK1 als auch von p38 unterdrückt.

Bedeutung und Regulation von Apolipoprotein J in atherosklerotischen Läsionen

Apolipoprotein J (ApoJ) ist ein heterodimeres sekretiertes Glycoprotein, welchem sowohl antiapoptotische als auch antiinflammatorische Eigenschaften zugeschrieben werden. Es wird unter vielen pathophysiologischen Zuständen verstärkt exprimiert. Dazu zählen viele Krankheiten wie z.B. Krebs, M. Alzheimer, Creuzfeldt Jakob und Atherosklerose. Die vorliegende Arbeit befasst sich zum Einen mit der Funktion von ApoJ bei Atherosklerose und zum Anderen mit der Regulation von ApoJ durch in atherosklerotischen Läsionen vorkommende Bestandteile. Für die Untersuchungen der Funktion von ApoJ bei der Atherosklerose wurde die „Mainzer Hypothese“ zugrunde gelegt, die davon ausgeht, dass enzymatisch verdautes LDL (high density lipoprotein) (E-LDL) ursächlich für die Entstehung von atherosklerotischen Läsionen ist. In der vorliegenden Arbeit konnte gezeigt werden, dass ApoJ zwar an E-LDL bindet, nicht aber an natives LDL und dass durch diese Bindung die zytotoxische Wirkung von E-LDL auf glatte Muskelzellen der Ratte unterdrückt wird. Mittels Annexinfärbung und Caspase-Messung konnte gezeigt werden, dass ApoJ in diesem Fall eine antiapoptotische Funktion aufweist. Durch immunhistochemische Untersuchungen an humanen Gewebsschnitten aus frühen atherosklerotischen Läsionen konnte eine Kolokalisation von ApoJ und E-LDL nachgewiesen werden. Diese Ergebnisse unterstreichen die Mainzer Hypothese. Durch eine Behandlung von glatten Muskelzellen der Ratte mit den Lipoproteinen LDL/E-LDL und nekrotischen Zellen sollte die Regulation von ApoJ durch in atherosklerotischen Läsionen vorhandenen Stimuli untersucht werden. Frühere Arbeiten unserer Arbeitsgruppe konnten bereits zeigen, dass eine Behandlung mit nekrotischen Zellen zu einer vermehrten Expression der ApoJ-mRNA führt und dass diese Regulation in Korrelation mit der Expression von Toll-like Rezeptoren (TLR) der verschiedenen Zellen steht. In dieser Arbeit konnte RNA aus nekrotischen Zellen als ApoJ-induzierende Komponente identifiziert werden. Durch Inhibition der TLR3-Signalwege konnten erste Hinweise darüber gewonnen werden, über welche Signaltransduktionswege die ApoJ Regulation erfolgt. Eine Behandlung der Zellen mit E LDL und LDL hingegen führte zu einer Repression der ApoJ-Sekretion. Diese Ergebnisse deuten darauf hin, dass in atherosklerotischen Läsionen sowohl ApoJ induzierende wie auch repremierende Stimuli vorhanden sind.

Rituali indigeni in Mesoamerica. La festa di Petición de Lluvias nella Montaña di Guerrero (Messico)

Questa tesi di carattere antropologico in ambito dottorale riguarda i rituali comunitari nelle comunità indigene messicane. Il principale oggetto della ricerca è il rituale della pioggia o di Petición de Lluvia, caratterizzato sia dal sacrificio animale che da una specifica relazione di causa-effetto con l’ambiente circostante. La ricerca etnografica è cominciata dall’ipotesi di voler verificare la persistenza nel tempo, e dunque nell’attualità, di procedure cerimoniali non appartenenti, almeno nella loro forma più lineare, alla religione cattolico-cristiana. Il luogo nel quale è avvenuta tale ricerca è la regione La Montaña di Guerrero, situata nel Messico sud-occidentale, e più precisamente la zona in cui vivono le comunità di etnia Nahua di San Pedro Petlacala, Acuilpa, e Xalpatláhuac che si trovano nelle vicinanze della cittadina di Tlapa de Comonfort. In un contesto ambientale profondamente rurale come quello della Montaña di Guerrero, la persistenza dei rituali evidenzia come le risorse naturali e gli agenti atmosferici - pioggia, vento, nubi - continuino a rappresentare gli elementi centrali che condizionano le variabili economiche di sussistenza e della riproduzione sociale. Il rituale di Petición de Lluvia rappresenta il momento di congiunzione tra la stagione secca e quella piovosa, tra la semina ed il raccolto del mais. Definito come una pratica religiosa nella quale il gruppo si identifica e partecipa con varie donazioni (ofrenda o deposito rituale), suddivisibili in alimenti/oggetti/preghiere ed azioni rituali, la cerimonia esprime l’auspicio di piogge abbondanti, con le quali irrigare i campi e continuare le attività umane. Il destinatario dell’offerta è la stessa divinità della pioggia, Tlaloc per le antiche civiltà mesoamericane, invocato sotto le mentite spoglie del santo patrono del 25 aprile, San Marcos. Il rituale è contraddistinto per tutta la sua durata dalla presenza del principale specialista religioso, sacerdote in lingua spagnola oppure «Tlahmáquetl» in lingua náhuatl.

High-resolution reconstruction of Holocene climate variability and environmental changes in the North Pacific using bivalve shells

Bivalve mollusk shells are useful tools for multi-species and multi-proxy paleoenvironmental reconstructions with a high temporal and spatial resolution. Past environmental conditions can be reconstructed from shell growth and stable oxygen and carbon isotope ratios, which present an archive for temperature, freshwater fluxes and primary productivity. The purpose of this thesis is the reconstruction of Holocene climate and environmental variations in the North Pacific with a high spatial and temporal resolution using marine bivalve shells. This thesis focuses on several different Holocene time periods and multiple regions in the North Pacific, including: Japan, Alaska (AK), British Columbia (BC) and Washington State, which are affected by the monsoon, Pacific Decadal Oscillation (PDO) and El Niño/Southern Oscillation (ENSO). Such high-resolution proxy data from the marine realm of mid- and high-latitudes are still rare. Therefore, this study contributes to the optimization and verification of climate models. However, before using bivalves for environmental reconstructions and seasonality studies, life history traits must be well studied to temporally align and interpret the geochemical record. These calibration studies are essential to ascertain the usefulness of selected bivalve species as paleoclimate proxy archives. This work focuses on two bivalve species, the short-lived Saxidomus gigantea and the long-lived Panopea abrupta. Sclerochronology and oxygen isotope ratios of different shell layers of P. abrupta were studied in order to test the reliability of this species as a climate archive. The annual increments are clearly discernable in umbonal shell portions and the increments widths should be measured in these shell portions. A reliable reconstruction of paleotemperatures may only be achieved by exclusively sampling the outer shell layer of multiple contemporaneous specimens. Life history traits (e.g., timing of growth line formation, duration of the growing season and growth rates) and stable isotope ratios of recent S. gigantea from AK and BC were analyzed in detail. Furthermore, a growth-temperature model based on S. gigantea shells from Alaska was established, which provides a better understanding of the hydrological changes related to the Alaska Coastal Current (ACC). This approach allows the independent measurement of water temperature and salinity from variations in the width of lunar daily growth increments of S. gigantea. Temperature explains 70% of the variability in shell growth. The model was calibrated and tested with modern shells and then applied to archaeological specimens. The time period between 988 and 1447 cal yrs BP was characterized by colder (~1-2°C) and much drier (2-5 PSU) summers, and a likely much slower flowing ACC than at present. In contrast, the summers during the time interval of 599-1014 cal yrs BP were colder (up to 3°C) and fresher (1-2 PSU) than today. The Aleutian Low may have been stronger and the ACC was probably flowing faster during this time.

Biofunktionalisierung oxidischer Titanoberflächen über eine spezifische Anbindung von biotinyliertem Fibronektin für die medizinische Anwendung

In der hier vorliegenden Dissertation wird die Entwicklung und Charakterisierung einer biomimetischen Beschichtung für Titanimplantatoberflächen, insbesondere Dentalimplantate, beschrieben. Ziel war es, die Adhäsion und Aktivität von Osteoblasten auf Titanoberflächen zu steigern und so eine Beschleunigung der Implantatintegration in das Knochengewebe zu erreichen. Hierfür wurde eine spezielle Art der biomimetischen Beschichtung entwickelt, bei der biotinyliertes Fibronektin (bFn) über Streptavidin auf eine biotinylierte TiOX-Modelloberfläche immobilisiert wurde. Die Biotinmodifizierung der TiOX-Oberfläche erfolgte hierbei über einen „Self-Assembly-Prozess“ durch sequenzielle Chemiesorption von N-(6-aminohexyl)aminopropyltrimethoxysilan sowie verschiedenen Sulfo-NHS-Biotin-Derivaten, welche den Aufbau einer Streptavidin-Monolage ermöglichten. Als ein wichtiges Resultat zeigte sich, dass die Streptavidin-Monolage effektiv die unspezifische Adsorption von Proteinen an die TiOX-Oberfläche unterbindet und hierdurch die Adhäsion von Osteoblasten auf dieser unterdrückt. Dies hat den Vorteil, dass auf eine antiadhäsive Basisbeschichtung, welche für eine spezifische Zellreaktion wichtig ist, verzichtet werden kann. Dieses osteoblastere Adhäsionsverhalten änderte sich signifikant nach Anbindung von bFn an die Streptavidin-Monolage, mit dem Ergebnis, einer drastischen Steigerung der Osteoblastenadhäsion. Weiterhin besaßen Osteoblasten auf diesen Oberflächen ein Proteinexpressionsmuster, das auf eine erhöhte Osteoinduktion schließen lässt. Es zeigte sich darüber hinaus eine verstärkte Zelladhäsion sowie eine Steigerung des osteoinduktiven Effekts auf Substraten, bei denen bFn über eine Streptavidin-Monolage immobilisiert wurde, gegenüber mit nativem Fibronektin (Fn) modifizierten TiOX-Oberflächen. Ein wesentlicher Schwerpunkt bestand daher in der Analyse der Zusammensetzung und Struktur der biomimetischen Beschichtung über „Surface Plasmon Spectroscopy“ und „Atomic Force Microscopy“. Diese ergab, dass bFn und natives Fn auf den jeweiligen Oberflächen eine unterschiedliche Konformation einnimmt. Im Gegensatz zu nativem Fn, das bei der Adsorption unter physiologischen Bedingungen auf TiOX-Oberflächen eine kompakte Konformation besitzt, nimmt bFn auf einer Streptavidin-Monolage eine entfaltete Konformation ein. Bei letzterer handelt es sich um dieselbe, welche Fn in vivo innerhalb der extrazellulären Matrix besitzt. Sie unterscheidet sich von der kompakten Fn-Konformation dahingehend, dass entlang der Fn-Achse weitere Proteinbindestellen zugänglich werden und hierdurch die Zellaffinität von Fn gesteigert wird. Die nachgewiesene Konformationsänderung kann somit als Grund für die gesteigerte Osteoblasten-Adhäsion und Aktivität auf Oberflächen mit bFn angenommen werden. Diese Kenntnisse konnten weiterhin für die Optimierung des biomimetischen Schichtsystems genutzt werden. So war es möglich, durch alternierendes Inkubieren der Biotin-aktivierten Oberfläche mit Streptavidin und bFn, ein Multilayersystem gezielt aufzubauen. Der Vorteil dieses Multilayersystems gegenüber einer einfachen Monolage aus bFn besteht in einer erhöhten Stabilität der biomimetischen Beschichtung, wodurch eine Anwendung in der Praxis erleichtert würde.

"A la búsqueda de nuevos horizontes". La scrittura della migrazione africana in Spagna

La migrazione genera spesso nei soggetti migranti forme di spaesamento, poiché lo spostamento fisico condiziona la sfera emotiva: in loro può emergere il senso di nostalgia verso la patria e il desiderio del ritorno, oppure la volontà di annullare le proprie radici e di conformarsi ai modelli della società ricevente. Spesso tali sensazioni di spaesamento possono essere superate grazie alla pratica creativa della scrittura; è per questo che nelle varie realtà di immigrazione ha preso campo la pratica della scrittura migrante, dove si dà spazio all’altro che cerca di far sentire la propria voce, ricorrendo alla lingua del Paese d’arrivo, senza rinunciare ai tratti distintivi della sfera culturale d’origine, creando testi ibridi, che disegnano un ponte tra le culture. Focus della ricerca è la scrittura della migrazione africana in Spagna, studiata sia in prospettiva generale che specifica, mediante quattro autori e le relative opere selezionate: Laila (2010) della marocchina Laila Karrouch, Las tres vírgenes de Santo Tomás (2008) dell’equatoguineana Guillermina Mekuy, Una vida de cuento (2006) del camerunese Boniface Ofogo, Amina (2006) del senegalese Sidi Seck. L’analisi dei testi è effettuata sulla base di due filoni tematici, la famiglia e il rapporto con la società d’arrivo, ed è corredata dallo studio del lessico relativo ai due temi di riferimento. Leggere fra le righe il microcosmo della famiglia significa porre l’attenzione sulle diverse dinamiche affettive che stanno dietro alla parola “migrazione” e sulle particolari dimensioni familiari che caratterizzano la vita odierna, dove spesso avviene il contatto fra più culture. Un contatto che si riflette nel macrocontesto della realtà ospite dove si ha modo di avviare un dialogo fra nativi e stranieri, poiché spesso le iniziali forme di contrasto si tramutano in sete di conoscenza e volontà di avvicinarsi, facendo emergere l’idea che la diversità non separa ma arricchisce.

Lysosomaler Transport kationischer Aminosäuren durch Mitglieder der SLC7-Familie

Lysosomaler Transport kationischer Aminosäuren (KAS) stellt einen Rettungsweg in der Cystinose-Therapie dar. Ein solches Transportsystem wurde in humanen Hautfibroblasten beschrieben und mit System c benannt. Des Weiteren stellt lysosomales Arginin eine Substratquelle für die endotheliale NO-Synthase (eNOS) dar. Das von der eNOS gebildete NO ist ein wichtiges vasoprotektiv wirkendes Signalmolekül. Ziel war es daher, herauszufinden, ob Mitglieder der SLC7-Unterfamilie hCAT möglicherweise System c repräsentieren.rnIn dieser Arbeit konnte ich die lysosomale Lokalisation verschiedener endogener, sowie als EGFP-Fusionsproteine überexprimierter CAT-Isoformen nachweisen. Mittels Fluoreszenz-mikroskopie wurde festgestellt, dass die in U373MG-Zellen überexprimierten Fusionsproteine hCAT-1.EGFP sowie SLC7A14.EGFP mit dem lysosomalen Fluoreszenz-Farbstoff LysoTracker co-lokalisieren. Eine Lokalisation in Mitochondrien oder dem endoplasmatischem Retikulum konnte mit entsprechenden Fluoreszenz-Farbstoffen ausgeschlossen werden. Zusätzlich reicherten sich die überexprimierten Proteine hCAT-1.EGFP, hCAT-2B.EGFP und SLC7A14.EGFP in der lysosomalen Fraktion C aus U373MG-Zellen zusammen mit den lysosomalen Markern LAMP-1 und Cathepsin D an. Gleiches galt für den endogenen hCAT-1 in der lysosomalen Fraktion C aus EA.hy926- und U373MG-Zellen sowie für den SLC7A14 in den humanen Hautfibroblasten FCys5. Mit dem im Rahmen dieser Arbeit generierte Antikörper gegen natives SLC7A14 konnte erstmals die endogene Expression und Lokalisation von SLC7A14 in verschiedenen Zelltypen analysiert werden.rnObwohl eine Herunterregulation des hCAT-1 in EA.hy926-Endothelzellen nicht zu einer Reduktion der Versorgung der eNOS mit lysosomalem Arginin führte, ist eine Funktion von hCAT-1 im Lysosom wahrscheinlich. Sowohl die [3H]Arginin- als auch die [3H]Lysin-Aufnahme der Fraktion C aus U373MG-hCAT-1.EGFP war signifikant höher als in die Fraktion C aus EGFP-Kontrollzellen. Dies konnte ebenfalls für den hCAT-2B.EGFP gezeigt werden. Zusätzlich zeigten lysosomale Proben aus U373MG-hCAT-2B.EGFP-Zellen in der SSM-basierten Elektrophysiologie eine elektrogene Transportaktivität für Arginin. Das Protein SLC7A14.EGFP zeigte in keiner der beiden durchgeführten Transportstudien eine Aktivität. Dies war unerwartet, da die aus der Diplomarbeit stammende und im Rahmen dieser Dissertation erweiterte Charakterisierung der hCAT-2/A14_BK-Chimäre, die die „funktionelle Domäne“ des SLC7A14 im Rückgrat des hCAT-2 trug, zuvor den Verdacht erhärtet hatte, dass SLC7A14 ein lysosomal lokalisierter Transporter für KAS sein könnte. Diese Studien zeigten allerding erstmals, dass die „funktionelle Domäne“ der hCATs die pH-Abhängigkeit vermittelt und eine Rolle in der Substraterkennung spielt.rnZukünftig soll weiter versucht werden auch endogen eine Transportaktivität der hCATs für KAS im Lysosom nachzuweisen und das Substrat für das intrazellulär lokalisierte Waisen-Protein SLC7A14 zu finden. Eine mögliche Rolle könnte SLC7A14 als Transporter für Neurotransmitter spielen, da eine sehr prominente Expression im ZNS festgestellt wurde.rn

Dinamica di una faglia con due asperità in presenza di accoppiamento viscoelastico

Il lavoro di tesi si propone di analizzare l'evoluzione dinamica di una faglia caratterizzata da due asperità complanari contraddistinte da diverso attrito (modello asimmetrico) e da accoppiamento viscoelastico. Il modello reologico assunto per la crosta terrestre è di tipo Maxwelliano: lo sforzo trasferito da un'asperità all'altra in occasione degli scorrimenti delle asperità stesse subisce parziale rilassamento durante il periodo intersismico, con conseguente anticipo o ritardo degli eventi sismici successivi. Lo studio del sistema viene condotto tramite un modello di faglia discreto, in cui lo stato della faglia è determinato da tre variabili che rappresentano i deficit di scorrimento delle asperità e il loro accoppiamento viscoelastico. Scopo principale della tesi è quello di caratterizzare i differenti modi dinamici del sistema, determinando equazioni del moto e orbite nello spazio delle fasi e confrontando i risultati ottenuti con i modelli precedentemente sviluppati, con particolare riferimento al caso simmetrico (asperità caratterizzate dallo stesso attrito) studiato in [Amendola e Dragoni (2013)] e al caso di accoppiamento puramente elastico analizzato in [Dragoni e Santini (2012)]. Segue l'applicazione del modello all'evento sismico verificatosi in Alaska nel 1964, generato dallo scorrimento delle asperità di Kodiak Island e Prince William Sound: lo studio verte in particolare sulla valutazione dello stato di sforzo sulla faglia prima e dopo il terremoto, la determinazione della funzione sorgente (moment rate) a esso associata e la caratterizzazione della possibile evoluzione futura del sistema. Riferimenti bibliografici Amendola, A. & Dragoni, M., “Dynamics of a two-fault system with viscoelastic coupling”. Nonlinear Processes in Geophysics, 20, 1–10, 2013. Dragoni, M. & Santini, S., “Long-term dynamics of a fault with two asperities of different strengths”. Geophysical Journal International, 191, 1457–1467, 2012.

Active processes, morphology, and dynamics of icy debris fans: Landform evolution along rapidly degrading escarpments in alpine regions undergoing recent deglaciation

In the past few decades the impacts of climate warming have been significant in alpine glaciated regions. Many valley glaciers formerly linked as distributary glaciers to high-level icecaps have decoupled at their icefalls, exposing major escarpments and generating a suite of dynamic landforrns dominated by mass wasting. Ice-dominated landforms, here termed icy debris fans, develop rapidly by ice avalanching, rockfall, and icy debris flow. Field-based reconnaissance studies at two alpine settings, the Wrangell Mountains of Alaska and the Southern Alps of New Zealand, provide a preliminary morphogenetic model of spatial and temporal evolution of icy debris fans in a range of alpine settings. The influence of these processes on landform evolution is largely unrecognized in the literature dealing with post-glacial landform adjustment known as the paraglacial. A better understanding of these dynamic processes will be increasingly important because of the extreme geohazards characterizing these areas. Our field studies show that after glacier decoupling, icy debris fans begin to form along the base of bedrock escarpments at the mouths of catchments and prograde over valley glaciers. The presence of a distinct catchment, apex, and fan morphology distinguishes these landforms from other landforms common in periglacial hillslope settings receiving abundant clastic debris and ice. Ice avalanching is the most abundant process involved in icy debris fan formation. Fans developed below weakly incised catchments are dominated by ice avalanching and are composed primarily of ice with minor lithic detritus. Typically, avalanches fall into the fan catchments where sediments transform into grainflows that flow onto the fans. Once on the fans, avalanche deposits ablate rapidly, flattening and concentrating lithic fragments at the surface. Icy debris fans may become thick enough to become glaciers with splay crevasse systems. Fans developed below larger, more complex catchments are composed of higher proportions of lithic detritus resulting from temporary storage of ice and lithic detritus deposits within the catchment. Episodic outbursts of meltwater from the icecap may mix with the stored sediments and mobilize icy debris flows (mixture of ice and lithic clasts) onto the fans. Our observations indicate that the entire evolutionary cycle of icy debris fans probably occurs during an early paraglacial interval (i.e., decades to 100 years). Observations comparing avalanche frequency, volume, and fan morphologic evolution at the Alaska site between 2006 and 2010 illustrate complex response between icy debris fans even within the same cirque - where one fan may be growing while others are downwasting because of differences in ice supply controlled by their respective catchments and icecap contributions. As ice supply from the icecap diminishes through time, icy debris fans rapidly downwaste and eventually evolve into talus cones that receive occasional but ephemeral ice avalanches.

Miocene basin development and volcanism along a strike-slip to flat-slab subduction transition: Stratigraphy, geochemistry, and geochronology of the central Wrangell volcanic belt, Yakutat-North America collision zone

New geochronologic, geochemical, sedimentologic, and compositional data from the central Wrangell volcanic belt (WVB) document basin development and volcanism linked to subduction of overthickened oceanic crust to the northern Pacific plate margin. The Frederika Formation and overlying Wrangell Lavas comprise >3 km of sedimentary and volcanic strata exposed in the Wrangell Mountains of south-central Alaska (United States). Measured stratigraphic sections and lithofacies analyses document lithofacies associations that reflect deposition in alluvial-fluvial-lacustrine environments routinely influenced by volcanic eruptions. Expansion of intrabasinal volcanic centers prompted progradation of vent-proximal volcanic aprons across basinal environments. Coal deposits, lacustrine strata, and vertical juxtaposition of basinal to proximal lithofacies indicate active basin subsidence that is attributable to heat flow associated with intrabasinal volcanic centers and extension along intrabasinal normal faults. The orientation of intrabasinal normal faults is consistent with transtensional deformation along the Totschunda-Fairweather fault system. Paleocurrents, compositional provenance, and detrital geochronologic ages link sediment accumulation to erosion of active intrabasinal volcanoes and to a lesser extent Mesozoic igneous sources. Geochemical compositions of interbedded lavas are dominantly calc-alkaline, range from basaltic andesite to rhyolite in composition, and share geochemical characteristics with Pliocene-Quaternary phases of the western WVB linked to subduction-related magmatism. The U/Pb ages of tuffs and Ar-40/Ar-39 ages of lavas indicate that basin development and volcanism commenced by 12.5-11.0 Ma and persisted until at least ca. 5.3 Ma. Eastern sections yield older ages (12.5-9.3 Ma) than western sections (9.6-8.3 Ma). Samples from two western sections yield even younger ages of 5.3 Ma. Integration of new and published stratigraphic, geochronologic, and geochemical data from the entire WVB permits a comprehensive interpretation of basin development and volcanism within a regional tectonic context. We propose a model in which diachronous volcanism and transtensional basin development reflect progressive insertion of a thickened oceanic crustal slab of the Yakutat microplate into the arcuate continental margin of southern Alaska coeval with reported changes in plate motions. Oblique northwestward subduction of a thickened oceanic crustal slab during Oligocene to Middle Miocene time produced transtensional basins and volcanism along the eastern edge of the slab along the Duke River fault in Canada and subduction-related volcanism along the northern edge of the slab near the Yukon-Alaska border. Volcanism and basin development migrated progressively northwestward into eastern Alaska during Middle Miocene through Holocene time, concomitant with a northwestward shift in plate convergence direction and subduction collision of progressively thicker crust against the syntaxial plate margin.