Il trattamento delle fratture e lussazioni vertebrali nei piccoli animali

Treatment of spinal fracture and luxation in small animals Traumatic spinal injuries usually result from a mechanic trauma. Spinal facture and luxations generally occur in the junction between and more mobile parts of the spinal column: close to the skull, thorax and pelvis. Fractures may occur alone or in combination with luxation as fracture/luxation. When the fractures are not stable the best solution is the surgical fixation. Internal and external fixation are the surgical methods for the treatment of vertebral fractures and luxations. The authors report the treatment of 12 cases of thoracic and lumbar vertebral fractures and luxations in small animals using the screws/pins and Polymethylmethacrylate technique. The analysis of results is a contribute I the valutation of surgical technique and complications in the post-surgical period.

Provenienza dei sedimenti arenitici nel bacino di Tracia (eo-oligocene, Turchia nord-occidentale e Grecia nord-orientale)

The Thrace Basin is the largest and thickest Tertiary sedimentary basin of the eastern Balkans region and constitutes an important hydrocarbon province. It is located between the Rhodope-Strandja Massif to the north and west, the Marmara Sea and Biga Peninsula to the south, and the Black Sea to the est. It consists of a complex system of depocenters and uplifts with very articulate paleotopography indicated by abrupt lateral facies variations. Its southeastern margin is widely deformed by the Ganos Fault, a segment of the North Anatolian strike-slip fault system . Most of the Thrace Basin fill ranges from the Eocene to the Late Oligocene. Maximum total thickness, including the Neogene-Quaternary succession, reaches 9.000 meters in a few narrow depocenters. This sedimentary succession consists mainly of basin plain turbiditic deposits with a significant volcaniclastic component which evolves upwards to shelf deposits and continental facies, with deltaic bodies prograding towards the basin center in the Oligocene. This work deals with the provenance of Eocene-Oligocene clastic sediments of the southern and western part of Thrace Basin in Turkey and Greece. Sandstone compositional data (78 gross composition analyses and 40 heavy minerals analyses) were used to understand the change in detrital modes which reflects the provenance and geodinamic evolution of the basin. Samples were collected at six localities, which are from west to est: Gökçeada, Gallipoli and South-Ganos (south of Ganos Fault), Alexandroupolis, Korudağ and North-Ganos (north of Ganos Fault). Petrologic (framework composition and heavy-mineral analyses) and stratigraphic-sedimentologic data, (analysis of sedimentologic facies associations along representative stratigraphic sections, paleocurrents) allowed discrimination of six petrofacies; for each petrofacies the sediment dispersal system was delineated. The Thrace Basin fill is made mainly of lithic arkoses and arkosic litharenites with variable amount of low-grade metamorphic lithics (also ophiolitic), neovolcanic lithics, and carbonate grains (mainly extrabasinal). Picotite is the most widespread heavy mineral in all petrofacies. Petrological data on analyzed successions show a complex sediment dispersal pattern and evolution of the basin, indicating one principal detrital input from a source area located to the south, along both the İzmir-Ankara and Intra-Pontide suture lines, and a possible secondary source area, represented by the Rhodope Massif to the west. A significant portion of the Thrace Basin sediments in the study area were derived from ophiolitic source rocks and from their oceanic cover, whereas epimetamorphic detrital components came from a low-grade crystalline basement. An important penecontemporaneous volcanic component is widespread in late Eocene-Oligocene times, indicating widespread post-collisional (collapse?) volcanism following the closure of the Vardar ocean. Large-scale sediment mass wasting from south to north along the southern margin of the Thrace Basin is indicated (i) in late Eocene time by large olistoliths of ophiolites and penecontemporaneous carbonates, and (ii) in the mid-Oligocene by large volcaniclastic olistoliths. The late Oligocene paleogeographic scenario was characterized by large deltaic bodies prograding northward (Osmancik Formation). This clearly indicates that the southern margin of the basin acted as a major sediment source area throughout its Eocene-Oligocene history. Another major sediment source area is represented by the Rhodope Massif, in particolar the Circum-Rhodopic belt, especially for plutonic and metamorphic rocks. Considering preexisting data on the petrologic composition of Thrace Basin, silicilastic sediments in Greece and Bulgaria (Caracciolo, 2009), a Rhodopian provenance could be considered mostly for areas of the Thrace Basin outside our study area, particularly in the northern-central portions of the basin. In summary, the most important source area for the sediment of Thrace Basin in the study area was represented by the exhumed subduction-accretion complex along the southern margin of the basin (Biga Peninsula and western-central Marmara Sea region). Most measured paleocurrent indicators show an eastward paleoflow but this is most likely the result of gravity flow deflection. This is possible considered a strong control due to the east-west-trending synsedimentary transcurrent faults which cuts the Thrace Basin, generating a series of depocenters and uplifts which deeply influenced sediment dispersal and the areal distribution of paleoenvironments. The Thrace Basin was long interpreted as a forearc basin between a magmatic arc to the north and a subduction-accretion complex to the south, developed in a context of northward subduction. This interpretation was challenged by more recent data emphasizing the lack of a coeval magmatic arc in the north and the interpretation of the chaotic deposit which outcrop south of Ganos Fault as olistoliths and large submarine slumps, derived from the erosion and sedimentary reworking of an older mélange unit located to the south (not as tectonic mélange formed in an accretionary prism). The present study corroborates instead the hypothesis of a post-collisional origin of the Thrace Basin, due to a phase of orogenic collapse, which generated a series of mid-Eocene depocenters all along the İzmir-Ankara suture (following closure of the Vardar-İzmir-Ankara ocean and the ensuing collision); then the slab roll-back of the remnant Pindos ocean played an important role in enhancing subsidence and creating additional accommodation space for sediment deposition.

The pre-alpine evolution of the basement of the Pelagonian Zone and the Vardar Zone, Greece

The Pelagonian Zone and the Vardar Zone in Greece represent the western part of the Hellenide hinterland (Internal Hellenides). While the Pelagonian Zone comprises predominantly crystalline basement and sedimentary cover rocks, the Vardar Zone has long been regarded as an ophiolite-decorated suture zone separating the Pelagonian Zone from the Serbo-Macedonian Massif to the east. Felsic basement rocks from both areas, with the main focus put on the Pelagonian Zone, were dated in order to identify the major crust-forming episodes and to improve the understanding of the evolutionary history of the region. The interpretation of the single-zircon geochronology results was aided by geochemical investigations. The majority of the basement rocks from the Pelagonian Zone yielded Permo-Carboniferous intrusion ages around 300 Ma, underlining the importance of this crust-forming event for the Internal Hellenides of Greece. Geochemically these basement rocks are classified as subduction-related granitoids, which formed in an active continental margin setting. An important result was the identification of a Precambrian crustal unit within the crystalline basement of the Pelagonian Zone. Orthogneisses from the NW Pelagonian Zone yielded Neoproterozoic ages of c. 700 Ma and are so far the oldest known rocks in Greece. These basement rocks, which are also similar to active margin granitoids, were interpreted as remnants of a terrane, the Florina Terrane, which can be correlated to a Pan-African or Cadomian arc. Since the gneisses contain inherited zircons of Middle to Late Proterozoic ages, the original location of the Florina Terrane was probably at the northwestern margin of Gondwana. In the Vardar Zone an important phase of Upper Jurassic felsic magmatism is documented by igneous formation ages ranging from 155 to 164 Ma. The chemical and isotopic composition of these rocks is also in accord with their formation in a volcanic-arc setting at an active continental margin. Older continental material incorporated in the Vardar Zone is documented by 319-Ma-old gneisses and by inherited zircons of mainly Middle Palaeozoic ages. The prevalence of subduction-related igneous rocks indicates that arc formation and accretion orogeny were the most important processes during the evolution of this part of the Internal Hellenides. The geochronological results demonstrate that most of the Pelagonian Zone and the Vardar Zone crystalline basement formed during distinct pre-Alpine episodes at c. 700, 300 and 160 Ma with a predominance of the Permo-Carboniferous magmatic phase.

Sistemi adesivi con applicazioni in campo biomedicale

Polymeric adhesives have been used for many applications like suture and embolization, instead of classic surgical methods or as for dental uses. In this work both subjects have been investigated and the results separated in two parts. In the first, new dentinal adhesives with different polymerizable groups (methacrylic or vinyl-ethereal) were synthesized. A low sensitivity to hydrolysis and equal or enhanced properties, compared to existing commercial products, were considered essentials. Moreover, these monomers need to polymerize by radical photopolymerization and functional groups of different characteristics were tested. All these products were characterized by microtensile bond strength test to determine the bonding strength between the adhesive and tooth. Concerning embolization, cyanoacrylates are nowadays the most-used adhesives in surgery. Thus, they must respond to several requirements. For instance, polymerization time and adhesive strength need to be low, to avoid diffusion of the products in the body and adhesion to the catheter. In order to overcome these problems we developed new cyanoacrylates, which practically instantly polymerize upon contact with blood but do not demonstrate strong adhesion to the catheter, thank to the presence of fluorine atoms, linked to the ester chain. The synthesis of these products was carried out in several steps, such as the depolymerization of the corresponding oligomers at high temperature in acid conditions. Two types of adhesion strengths were determined. Bonding strength between human veins and a microcatheter was determined in vitro by using organic materials as the most realistic model. Another test, on two layers of skin, was conducted to verify the possible use of these new cyanoacrylates as a glue for sutures. As a conclusion, we were able to demonstrate that some of the prepared monomers posses adhesive strength and polymerization time lower than the commercial product Glubran2.

Anatomy, phylogeny, and palaeoecology of the basal thalattosuchians (Mesoeucrocodylia) from the Liassic of Central Europe

In the marine Jurassic deposits of Europe, a group of marine crocodilians, the Thalattosuchia, belongs to the frequently found reptiles. Thalattosuchia are widely spread in Central Europe from the Jurassic to Lower Cretaceous, and some taxa are also distributed worldwide. The task of the work was to examine all taxa known from the Liassic of Europe. The most frequently known taxa Steneosaurus bollensis and Pelagosaurus typus are anatomically revised. New discoveries at the skull of Pelagosaurus typus e.g., the fact of a partly paired frontal are described by means of computed tomography investigations. In addition, juvenile specimens of this taxon are studied in detail for the first time. The rarely occurring taxon Platysuchus multiscrobiculatus is anatomically described in detail for the first time. It shows both in the skull and in the postcranial material morphological differences to Steneosaurus bollensis and Pelagosaurus typus. Thus Pl. multiscrobiculatus possesses, e.g., an ilium with a deeper acetabulum and a femur with a distinctly flexed femoral head. A juvenile specimen of Pl. multiscrobiculatus is now discovered and is described in parts for the first time, too. Furthermore, Steneosaurus gracilirostris and Steneosaurus brevior known from Lower Jurassic deposits of England are examined and in parts revised. In this work, Steneosaurs brevior is discovered with one specimen from the Upper Liassic of Holzmaden, Germany for the first time, and provides new evidence for the palaeobiogeographical distribution of the taxon. Because of the high number of investigated specimens, it is possible to study ontogenetic development from juvenile to adult stage in Steneosaurus bollensis, Pelagosaurus typus, and Platysuchus multiscrobiculatus. Biometric data are collected from thalattosuchians and extant crocodilians (e.g. Gavialis gangeticus) to investigate intraspecific variation, ontogenetic development, and taxa differentiation. The skulls of Platysuchus multiscrobiculatus and Steneosaurus bollensis are reconstructed three-dimensionally as wax models. The skull reconstructions form the basis of the jaw muscle restoration of Steneosaurus bollensis in connection with comparative studies at extant crocodilians. By means of functional morphologic analysis of the jaw musculature, the dentition, and the locomotor system of S. bollensis, possible conclusions are drawn for the prey options and the hunting behaviour. To clarify the relationships within the Thalattosuchia, a computer-based cladistic phylogenetic in-group analyse of 25 Thalattosuchia taxa is performed. For the analysis, following Thalattosuchia taxa are studied likewise at original material for comparisons: Metriorhynchus superciliosus, Metriorhynchus hastifer, Metriorhynchus leedsi, Geosaurus gracilis, Geosaurus giganteus, Teleidosaurus calvadosi, Teleidosaurus gaudryi, Teleosaurus cadomensis, Teleosaurus geoffroyi, Steneosaurus priscus, Steneosaurus edwardsi, Steneosaurus heberti, Steneosaurus leedsi, Steneosaurus boutilieri, Steneosaurus megarhinus, Steneosaurus obtusidens, and Machimosaurus hugii. The phylogenetic in-group analyse based on 115 characters, reveals a sister-group relationship of the monophyletic Teleosauridae and monophyletic Metriorhynchidae. Within the groups, some taxa are probably paraphyletic. The taxon Pelagosaurus typus is nested inside the Teleosauridae and not outside or within the Metriorhynchidae, as many authors suggested it so far. Based on these results, a tentative palaeobiogeographical-evolutionary scenario is developed.

Caratteristiche ortopediche-ortodontiche in pazienti affetti da Sindrome di Nooan

La sindrome di Noonan (SN) è una patologia a trasmissione autosomica dominante caratterizzata da bassa statura, difetti cardiaci congeniti, dismorfia facciale. In letteratura sono stati pubblicati pochi case reports riguardanti le condizioni orali-facciali in pazienti affetti da SN. Obiettivo. Individuare patologie di pertinenza ortopedico-ortodontica caratteristiche della sindrome utilizzando un campione di pazienti con diagnosi di SN. Metodi. Un gruppo di 10 pazienti affetti da SN è stato sottoposto a esame obiettivo extraorale ed intraorale, ortopantomografia, teleradiografia latero-laterale, impronte delle arcate dentarie. Le misurazioni sulle TLL sono state effettuate sulla base dell'analisi MBT; i valori palatali provengono dai modelli di studio dell’arcata superiore. È stata utilizzato il test t-Student per mettere a confronto il gruppo di studio e il gruppo di controllo riguardo le misure cefalometriche e i valori palatali. Risultati. Nel gruppo di studio sono state rilevate anomalie di numero (un dente deciduo soprannumerario e una agenesia di un dente permanente). Il test t-Student rivela differenze statisticamente significative per 7 variabili cefalometriche su 13 e per 2 variabili palatali. Conclusioni. Basandosi su questo studio è possibile concludere che i pazienti con SN mostrano II classe scheletrica di tipo mandibolare, crescita iperdivergente, tendenza al morso aperto scheletrico, palatoversione degli incisivi superiori, palato stretto. Questi risultati possono fornire informazioni utili sia per la diagnosi di SN sia per la pianificazione del corretto trattamento ortodontico.

Integrative Musterbildung kranialer Strukturen

Form und Gestalt kraniofazialer Strukturen sind primär beeinflusst durch die inhärente Integration der unterschiedlichsten Funktionssysteme und externer selektiver Einflüsse. Die Variabilität der Schädel-Morphe ist ein Indikator für solche Einflussfaktoren und damit ein idealer Gegenstand für vergleichende Analysen morphogenetischer Formbildung. Zur Ermittlung morphologisch-adaptiver Trends und Muster wurden sowohl Hypothesen zur morphologischen Differenziertheit als auch zu Korrelationen zwischen modularen Schädelkompartimenten (fazial, neurokranial, basikranial) untersucht. Zusätzlich wurden aus Schichtröntgenaufnahmen (CT) virtuelle Modelle rekonstruiert, welche die Interpretation der statistischen Befunde unterstützen sollten. Zur Berechnung der Gestaltunterschiede wurden mittels eines mechanischen Gelenkarm-Messgerätes (MicroScribe-G2) max. 85 ektokraniale Messpunkte (Landmarks) bzw. dreidimensionale Koordinaten an ca. 520 Schädeln von fünf rezenten Gattungen der Überfamilie Hominoidea (Hylobates, Pongo, Gorilla, Pan und Homo) akquiriert. Aus dem Datensatz wurden geometrische Störfaktoren (Größe, Translation, Rotation) mathematisch eliminiert und die verbleibenden Residuale bzw. ‚Gestalt-Variablen‘ diversen multivariat-statistischen Verfahren unterzogen (Faktoren, Cluster-, Regressions- und Korrelationsanalysen sowie statistische Tests). Die angewandten Methoden erhalten die geometrische Information der Untersuchungsobjekte über alle Analyseschritte hinweg und werden unter der Bezeichnung „Geometric Morphometrics (GMM)“ als aktueller Ansatz der Morphometrie zusammengefasst. Für die unterschiedlichen Fragestellungen wurden spezifische Datensätze generiert. Es konnten diverse morphologische Trends und adaptive Muster mit Hilfe der Synthese statistischer Methoden und computer-basierter Rekonstruktionen aus den generierten Datensätzen ermittelt werden. Außerdem war es möglich, präzise zu rekonstruieren, welche kranialen Strukturen innerhalb der Stichprobe miteinander wechselwirken, einzigartige Variabilitäten repräsentieren oder eher homogen gestaltet sind. Die vorliegenden Befunde lassen erkennen, dass Fazial- und Neurokranium am stärksten miteinander korrelieren, während das Basikranium geringe Abhängigkeiten in Bezug auf Gesichts- oder Hirnschädelveränderungen zeigte. Das Basikranium erweist sich zudem bei den nicht-menschlichen Hominoidea und über alle Analysen hinweg als konservative und evolutiv-persistente Struktur mit dem geringsten Veränderungs-Potential. Juvenile Individuen zeigen eine hohe Affinität zueinander und zu Formen mit einem kleinem Gesichts- und großem Hirnschädel. Während das Kranium des rezenten Menschen primär von Enkephalisation und fazialer Retraktion (Orthognathisierung) dominiert ist und somit eine einzigartige Gestalt aufweist, zeigt sich der Kauapparat als maßgeblich formbildendes Kompartiment bei den nicht-menschlichen Formen. Die Verbindung von GMM mit den interaktiven Möglichkeiten computergenerierter Modelle erwies sich als valides Werkzeug zur Erfassung der aufgeworfenen Fragestellungen. Die Interpretation der Befunde ist durch massive Interkorrelationen der untersuchten Strukturen und der statistisch-mathematischen Prozeduren als hoch komplex zu kennzeichnen. Die Studie präsentiert einen innovativen Ansatz der modernen Morphometrie, welcher für zukünftige Untersuchungen im Bereich der kraniofazialen Gestaltanalyse ausgebaut werden könnte. Dabei verspricht die Verknüpfung mit ‚klassischen’ und modernen Zugängen (z. B. Molekularbiologie) gesteigerte Erkenntnismöglichkeiten für künftige morphometrische Fragestellungen.

Risultati funzionali a lungo termine dopo sutura o plicatura del diaframma

Obbiettivo. Analizzare la funzionalità polmonare e diaframmatica dopo interventi di plicatura del diaframma con rete di rinforzo peri-costale eseguiti per relaxatio e riparazione di ernia transdiaframmatica cronica mediante riduzione e sutura diretta. Metodi. Dal 1996 al 2010, 10 pazienti con relaxatio unilaterale del diaframma e 6 pazienti con ernia transdiaframmatica cronica misconosciuta sono stati sottoposti a chirurgia elettiva. Gli accertamenti preoperatori e al follow-up di 12 mesi includevano prove di funzionalità respiratoria, misura della pressione massimale inspiratoria alla bocca in clino e ortostatismo, emogasanlisi, TC del torace e dispnea score. Risultati. I pazienti dei due gruppi non differivano in termini di funzionalità respiratoria preoperatoria nè di complicanze postoperatorie; al follow-up a 12 mesi il gruppo Eventrazione mostrava un significativo aumento del FEV1% (+18,2 – p<0.001), FVC% (+12,8 – p<0.001), DLCO% (+6,84 – p=0,04) e pO2 (+9,8 mmHg – p<0.001). Al contrario nrl gruppo Ernia solo il miglioramento della pO2 era significativo (+8.3 – p=0.04). Sebbene la massima pressione inspiratoria (PImax) fosse aumentata in entrambi i gruppi al follow-up, i pazienti operati per ernia mostravano un miglioramento limitato con persistente caduta significativa della PImax dall’ortostatismo al clinostatismo (p<0.001). Il Transitional dyspnoea score è stato concordante con tali miglioramenti pur senza differenze significative tra i due gruppi. La TC del torace ha evidenziato una sopraelevazione dell’emidiaframma suturato, senza recidiva di ernia, mentre i pazienti sottoposti a plicatura hanno mantenuto l’ipercorrezione. Conclusioni. L’utilizzo di un rinforzo protesico è sicuro e sembra assicurare risultati funzionali migliori a distanza in termini di flussi respiratori e di movimento paradosso del diaframma (valutato mediante PImax). Lacerazioni estese del diaframma coinvolgenti le branche principali di suddivisione del nervo frenico si associano verosimilmente a una relaxatio che può quindi ridurre il guadagno funzionale a lungo termine se non adeguatamente trattata mediante l’utilizzo di un rinforzo protesico.

UHP metamorphic rocks of the Eastern Rhodope Massif, NE Greece: new constraints from petrology, geochemistry and zircon ages

In this PhD thesis, a multidisciplinary study has been carried out on metagranitoids and paragneisses from the Eastern Rhodope Massif, northern Greece, to decipher the pre-Alpine magmatic and geodynamic evolution of the Rhodope Massif and to correlate the eastern part with the western/central parts of the orogen. The Rhodope Massif, which occupies the major part of NE Greece and S Bulgaria, represents the easternmost part of the Internal Hellenides. It is regarded as a nappe stack of high-grade units, which is classically subdivided into an upper unit and a lower unit, separated by a SSE-NNW trending thrust plane, the Nestos thrust. Recent research in the central Greek Rhodope Massif revealed that the two units correspond to two distinct terranes of different age, the Permo-Carboniferous Thracia Terrane, which was overthrusted by the Late Jurassic/Early Cretaceous Rhodope Terrane. These terranes are separated by the Nestos suture, a composite zone comprising metapelites, metabasites, metagranitoids and marbles, which record high-pressure and even ultrahigh-pressure metamorphism in places. Similar characteristic rock associations were investigated during this study along several well-constrained cross sections in vincity to the Ada, Sidiro and Kimi villages in the Greek Eastern Rhodope Massif. Field evidence revealed that the contact zone of the two terranes in the Eastern Rhodope Massif is characterized by a mélange of metapelites, migmatitic amphibolites/eclogites, strongly sheared orthogneisses and marbles. The systematical occurrence of this characteristic rock association between the terranes implies that the Nestos suture is a continuous belt throughout the Greek Rhodope Massif. In this study, a new UHP locality could be established and for the first time in the Greek Rhodope, metamorphic microdiamonds were identified in situ in their host zircons using Laser-Raman spectroscopy. The presence of the diamonds as well as element distribution patterns of the zircons, obtained by TOF-SIMS, indicate metamorphic conditions of T > 1000 °C and P > 4 GPa. The high-pressure and ultrahigh-pressure rocks of the mélange zone are considered to have formed during the subduction of the Nestos Ocean in Jurassic times at ~150 Ma. Melting of metapelitic rocks at UHP conditions facilitated the exhumation to lower crustal levels. To identify major crust forming events, basement granitoids were dated by LA-SF-ICPMS and SHRIMP-II U-Pb analyses of zircons. The geochronological results revealed that the Eastern Rhodope Massif consists of two crustal units, a structurally lower Permo-Carboniferous unit corresponding to the Thracia Terrane and a structurally upper Late Jurassic/Early Cretaceous unit corresponding to the Rhodope Terrane, like it was documented for the Central Rhodope Massif. Inherited zircons in the orthogneisses from the Thracia Terrane of the Eastern Rhodope Massif indicate the presence of a pre-existing Neoproterozoic and Ordovician-Silurian basement in this region. Triassic magmatism is witnessed by the zircons of few orthogneisses from the easternmost Rhodope Massif and is interpreted to be related to rifting processes. Whole-rock major and trace element analyses indicate that the metagranitoids from both terranes originated in a subduction-related magmatic-arc environment. The Sr-Nd isotope data for both terranes of the Eastern and Central Rhodope Massif suggest a mixed crust-mantle source with variable contributions of older crustal material as already indicated by the presence of inherited zircons. Geochemical and isotopic similarity of the basement of the Thracia Terrane and the Pelagonian Zone implies that the Thracia Terrane is a fragment of a formerly unique Permo-Carboniferous basement, separated by rifting and opening of the Meliata-Maliac ocean system in Triassic times. A branch of the Meliata-Maliac ocean system, the Nestos Ocean, subducted northwards in Late Jurassic times leading to the formation of the Late Jurassic/Early Cretaceous Rhodope magmatic arc on remnants of the Thracia Terrane as suggested by inherited Permo-Carboniferous zircons. The ~150 Ma zircon ages of the orthogneisses from the Rhodope Terrane indicate that subduction-related magmatism and HP/UHP metamorphism occurred during the same subduction phase. Subduction ceased due to the closure of the Nestos Ocean in the Late Jurassic/Early Cretaceous. The post-Jurassic evolution of the Rhodope Massif is characterized by the exhumation of the Rhodope core complex in the course of extensional tectonics associated with late granite intrusions in Eocene to Miocene times.

Thermochronological evolution of the Eastern Pontides and the Eastern Anatolian Plateau and NW Lesser Caucasus (Turkey, Georgia, Armenia)

The analysis of apatite fission tracks is applied to the study of the syn- and post-collisional thermochronological evolution of a vast area that includes the Eastern Pontides, their continuation in the Lesser Caucasus of Georgia (Adjara-Trialeti zone) and northern Armenia, and the eastern Anatolian Plateau. The resulting database is then integrated with the data presented by Okay et al. (2010) for the Bitlis Pütürge Massif, i.e. the western portion of the Bitlis-Zagros collision zone between Arabia and Eurasia. The mid-Miocene exhumation episode along the Black Sea coast and Lesser Caucasus of Armenia documented in this dissertation mirrors the age of collision between the Eurasian and Arabian plates along the Bitlis suture zone. We argue that tectonic stresses generated along the Bitlis collision zone were transmitted northward across eastern Anatolia and focused (i) at the rheological boundary between the Anatolian continental lithosphere and the (quasi)oceanic lithosphere of the Black Sea, and (ii) along major pre-existing discontinuities like the Sevan-Akera suture zone.The integration of both present-day crustal dynamics (GPS-derived kinematics and distribution of seismicity) and thermochronological data presented in this paper provides a comparison between short- and long-term deformation patterns for the entire eastern Anatolia-Transcaucasian region. Two successive stages of Neogene deformation of the northern foreland of the Arabia-Eurasia collision zone can be inferred. (i) Early and Middle Miocene: continental deformation was concentrated along the Arabia-Eurasia (Bitlis) collision zone but tectonic stress was also transferred northward across eastern Anatolia, focusing along the eastern Black Sea continent-ocean rheological transition and along major pre-existing structural discontinuities. (ii) Since Late-Middle Miocene time the westward translation of Anatolia and the activation of the North and Eastern Anatolian Fault systems have reduced efficient northward stress transfer.

Evaluation von Effektivität und Sicherheit der niederfrequenten, transkraniellen Ultraschalltherapie beim Schlaganfall

In den westlichen Ländern nimmt die Zahl der Schlaganfall-Patienten stetig zu und zählt mittlerweilernzu einer der häufigsten Todesursachen. Derzeit ist die Rekanalisationstherapie mit demrnFibrinolytikum rt-PA die einzig zugelassene Therapie. Die Rekanalisationsrate ist oftmals inkomplettrnund aufgrund von möglichen Blutungskomplikationen die Therapie nicht bei allen Patientenrnmöglich. Daher ist es wichtig, Alternativtherapieansätze (z.B. Ultraschallthrombolyse) zurnentwickeln. Blutgerinnsel können mit Hilfe von Ultraschall in Schwingung gebracht und sornlysiert oder die Wirkung von rt-PA verstärkt werden. Die vorliegende Arbeit hatte die Evaluationrnvon Bioeffekten von 60 kHz Ultraschall an gesundem und ischämischem Hirngewebe zum Ziel.rnNeben tierexperimentellen Methoden kamen auch molekular-biologische Techniken zur Anwendung.rnDie erste Studie beschäftigte sich mit der Wirkung von 60 kHz (Intensität: 0,2 W/cm2 undrnDuty Cycle 50%) auf ischämisches Hirngewebe (permanent ischämisch und nach Reperfusion).rnLediglich nach Reperfusion und Ultraschallbehandlung war das Läsionsvolumen signifikantrnerhöht, so dass von einer besonderen Vulnerabilität des Hirngewebes nach Reperfusionrnauszugehen ist (Penumbraschädigung). In der neurologischen Beurteilung der Tiere zeigte sichrnbei allen Tieren mit permanenter Okklusion und etwa einem Drittel der Tiere nach Reperfusionrnund Ultraschallbehandlung eine Hörminderung. In der anschließenden Studie wurde diernUltraschallintensität erniedrigt und der Duty Cycle variiert. In einer publizierten in vitro Studiernkonnte die zunehmende Lyserate mit steigendem Duty Cycle nachgewiesen werden. DiernAuswertung ergab eine Abhängigkeit des Läsionsvolumens von der Länge des Duty Cycles. Derrndritte Teil der Arbeit befasst sich mit der Wirkung von Ultraschall auf die Genexpression. Hierzurnwurden gesunde Ratten mit Ultraschall verschiedener Frequenzen (60 kHz, 488 kHz und 3 MHz)rntranskraniell behandelt und 4 h bzw. 24 h nach der Behandlung getötet. Proben von ischämischenrnTieren dienten als positive Kontrollen. Aufgrund von Literaturrecherchen wurden mehrerernKandidatengene ermittelt. Die Messung der Ischämieproben ergab eine weitgehende Übereinstimmungrnmit der Literatur. Die Messungen an den mit 60 kHz behandelten Proben ergabenrnkaum Anzeichen für eine differenzielle Genregulation. Die Frequenz von 488 kHz zeigte diernmeisten Regulationen, gefolgt von der Behandlung mit 3 MHz. Dieses Ergebnis lässt vermuten,rndass es sich bei den detektierten Veränderungen um protektive Mechanismen handelt, da diesernFrequenzen bislang im Tierversuch als nebenwirkungsarm beschrieben wurden. Die Auswertungrnvon 60 kHz-Proben mit Affymetrix Arrays ergab lediglich einige wenige differentiell regulierternGene. Die Array-Experimente konnten nicht durch qPCR-Messungen bestätigt werden.

Forensisch-anthropologische und traumatologische Untersuchungen an den menschlichen Skeletten aus der spätmittelalterlichen Schlacht von Dornach (1499 n. Chr.)

Der Forschungsgegenstand der vorliegenden Arbeit war die Identifikation und Interpretation von Traumata an menschlichen Skeletten. Neben einer umfassenden Darstellung des aktuellen Kenntnisstandes unter verschiedenen Gesichtspunkten wurden menschliche Überreste aus der Schlacht von Dornach 1499 n. Chr. untersucht. Ergänzend wurde eine Versuchsreihe mit Replika mittelalterlicher Waffen an Kunstköpfen durchgeführt. Für die Ansprache und Kategorisierung von Traumata an Skelettfunden existiert kein einheitliches und allgemein gebräuchliches System. Die verschiedenen Herangehensweisen und ihre Vor- und Nachteile wurden benannt und diskutiert. Nachfolgend wurden die Erscheinungsformen prä-, peri- und postmortaler Traumata bzw. Defekte sowie von Verletzungen durch stumpfe und scharfe Gewalt, Schussverletzungen und anderen Verletzungsarten dargestellt. Weitere besprochene Aspekte waren die Abgrenzung von Traumata gegen pathologische Veränderungen und anatomische Varianten sowie eine Diskussion der Methodik und Problematik der Erfassung von Verletzungsfrequenzen. Neben der Bestimmung von Geschlecht, Sterbealter und Körperhöhe wurden an den zur Untersuchung zur Verfügung stehenden Schädeln (N=106) und Femora (N=33) aus der Schlacht von Dornach 1499 n. Chr. pathologische und postmortale Veränderungen sowie als Schwerpunkt prä- und perimortale Traumata identifiziert und beschrieben. Die anthropologischen Befunde zeichneten das Bild einer in Hinsicht auf Sterbealter und Körperhöhe heterogenen Gruppe von Männern mit wenigen pathologischen Veränderungen. Die Ergebnisse wurden vor dem Hintergrund des spätmittelalterlichen Söldnerwesens diskutiert. An den Schädeln wurden insgesamt 417 perimortale Traumata identifiziert, wobei Hiebverletzungen stark überwogen. Die Entstehungsweise charakteristischer Merkmale von Hiebverletzungen konnte experimentell nachvollzogen werden. Weiter stellte sich heraus, dass Hiebverletzungen durch Schwerter und Hellebarden nur in Ausnahmefällen voneinander unterschieden werden können. Verletzungen durch punktuelle Einwirkungen und stumpfe Gewalt sowie Schussverletzungen wurden in weitaus geringerer Häufigkeit festgestellt. Experimentell konnte gezeigt werden, dass die Verletzungen durch punktuelle Einwirkungen mit einer Beibringung durch Langspiesse, Stossspitzen und Reisshaken von Hellebarden sowie Armbrustbolzen vereinbar sind, wobei beträchtliche Limitationen einer genaueren Waffenzuordnung offenkundig wurden. Die Verletzungen konnten als wohl typisch für die damalige Zeit bezeichnet werden, da sie das zeitgenössische Waffenspektrum deutlich widerspiegeln. Die Lokalisation der perimortalen Traumata am Schädel liess kein Muster erkennen, mit Ausnahme der Feststellung, dass grössere Schädelknochen mehr Verletzungen aufwiesen als kleinere. Diese regellose Verteilung wurde als Hinweis darauf verstanden, dass die Kampfweise keine „ritterliche“ gewesen sein dürfte, was in Einklang mit den damals geltenden Kriegsordnungen steht. Postmortale Veränderungen unterschiedlicher Art liessen vermuten, dass die untersuchten Individuen nicht bestattet wurden und dass die vom Schlachtfeld aufgesammelten Gebeine in Beinhäusern aufbewahrt wurden. Die Resultate bestätigten damit Angaben aus Schriftquellen und erlaubten die Zuordnung der Skelettreste zu Gefallenen des Reichsheeres. Beim Vergleich der Dornacher Stichprobe mit anderen mittelalterlichen Schlachtfeldserien traten sowohl hinsichtlich der anthropologischen Befunde als auch im Hinblick auf die Verletzungen und Verletzungsmuster deutliche Ähnlichkeiten zutage. Diese ergänzten nicht nur das lückenhafte Bild spätmittelalterlicher Heere und ihrer Kampfweise, sondern beleuchteten auch Unterschiede zwischen mittelalterlicher und neuzeitlicher Kriegsführung.

Guidelines of Special Care Dentistry in Patients with Chromosomal and Genetic syndromes

Chromosomal and genetic syndromes are frequently associated with dental and cranio-facial alterations. The aim of our study is to identify and describe the dental and craniofacial alterations typical of six genetic and chromosomal syndromes examined. Materials and Methods- A dental visit was performed to 195 patients referred from Sant’Orsola Hospital of Bologna, University of Bologna, to Service of Special Need Dentistry, Dental Clinic, Department of Biomedical and Neuromotor Science, University of Bologna. The patients recruited were 137 females and 58 males, in an age range of 3-49 years (mean age of 13.8±7.4). The total sample consisted of subjects affected with Down Syndrome (n=133), Familiar Hypophosphatemic Ricket (n=10), Muscular Dystrophies (n=12), Noonan Syndrome (n=13), Turner Syndrome (n=17), Williams Syndrome(n=10). A questionnaire regarding detailed medical and dental history, oral health and dietary habits, was filled by parents/caregivers, or patients themselves when possible. The intra-oral and extra-oral examination valued the presence of facial asymmetries, oral habits, dental and skeletal malocclusions, dental formula, dental anomalies, Plaque Index (Silness&LÖe Index), caries prevalence (dmft/DMFT index), gingivitis and periodontal disease, and mucosal lesions. Radiographic examinations (Intraoral radiographies, Orthopanoramic, Skull teleradiography) were executed according to patient’s age and treatment planning. A review of literature about each syndrome and its dental and cranio-facial characteristics and about caries, hygiene status and malocclusion prevalence on syndromic and non-syndromic population was performed. Results - The data of all the patients were collected in the “Data Collection Tables” created for each syndrome. General anamnesis information, oral hygiene habits and dmft/DMFT, PI, malocclusion prevalence were calculated and compared to syndromic and non-syndromic population results found in literature. Discussions and conclusions - Guidelines of Special Care dentistry were indicated for each syndrome, in relation to each syndrome features and individual patient characteristics.

Langzeitergebnisse nach Trabekulektomie bei Glaukompatienten

Hintergrund: Die antimetabolitgestützte Trabekulektomie stellt seit längeren denrnGoldstandard bei medikamentös nicht ausreichend therapierbaren Glaukomen dar. Kurz- und mittelfristige Erfolge wurden durch viele Studien bestätigt. Allerdings unterliegen diese sehr unterschiedlichen Erfolgsdefinitionen. Eine strikte Druckkontrolle ≤ 15 mm Hg ohne zusätzliche medikamentöse Therapie erscheint sinnvoll einen risikofreien Therapieerfolg zu bewerten. Es existieren nur wenige Langzeitstudien mit diesem Erfolgskriterium. Die durchgeführte Studie soll einen Eindruck der ophthalmologischen Versorgung trabekulektomierter Patienten an der Universitätsaugenklinik Mainz über einen bewusst langen Zeitraum bieten. Patienten und Methoden: In diese retrospektiven Studie wurden alle Patienten, die aufgrund einer fortgeschrittenen Glaukomerkrankung in den Jahren 1996, 2001 oder 2006 eine Trabekulektomie erhielten, aufgenommen. Von den 723 Augen der 664 Patienten dieser Jahrgänge konnten 447 (61,8%) nachverfolgt werden. Die Zusammensetzung der Patienten war mit anderen Studien vergleichbar. 28% konnten mindestens 7 Jahre, 10% sogar 10 Jahre nachverfolgt werden. Esrnwurde untersucht, ob ein signifikanter Zusammenhang zwischen dem ophthalomologisch-internistischem Entlassstatus (Visus, Tensio, Gesichtsfeld,rnGlaukomtyp, Voroperationen, Medikation, Vorerkrankungen, Art der Operation) undrnder erstrebten Kontrolle des Intraokulardruckes besteht. Ergebnisse: Die mittlere Nachbeobachtungszeit betrug 4,3 ± 3,4 Jahre. Nach 1, 3,rn5, 7 und 10 Jahren wiesen 217 (82,1%) (p < 0,001), 133 (67,7%) (p < 0,001), 70rn(50%) (p < 0,001), 59 (47,7%) (p = 0,056) und 16 (38,1%) (p = 0,06) Augen Intraokulardrücke ≤ 15 mm Hg ohne zusätzliche Antiglaukomatosa auf. Nichtrnstatistisch signifikant waren die 7- und 10-Jahresergebnisse. Mit Hilfe von Antiglaukomatosa waren es insgesamt, 225 (85,1%), 156 (79,7%), 87 (62,5%), 93 (75%) und 23 (54,7%) (alle p < 0,001). Die mediane Überlebenszeit für IOD ≤ 15 mm Hg ohne Medikation betrug 7,4 Jahre ± 5 Monate. Druckobergrenzen von ≤ 18 bzw. 21 mm Hg erfüllten bis zu 20% mehr Patienten. Der mittlere Visus von 0,32 ± 6 Stufen blieb nach einem mittleren postoperativen Abfall auf 0,25 ± 5 Stufen in den Folgeuntersuchungen stabil. Er zeigte ab dem 3-Jahresintervall keine statistisch signifikante Verschlechterung zum präoperativen Visus. 5,8 Jahre ± 80 Tage betrug die mediane Überlebenszeit für ein stabiles Gesichtsfeld. Gesichtsfelddaten, MD und PSD zeigten keine statistisch signifikante Verschlechterung (p > 0,05). Risikofaktoren für ein Scheitern der Operation waren Patientenalter (RR = 1,01, KI: 0,95 - 1,34, p = 0,043), arterielle Hypertonie (RR = 1,87, KI: 1,21-2,9, p = 0,005) und männliches Geschlecht (RR = 1,24; KI: 1,07 – 1,43; p = 0,004). Komplikationen waren passagere okuläre Hypotonien an 85 (19%), Fistulation an 46(10,2%), Aderhautschwellung an 29 (6,4%) –abhebung an 14 (3,1%), retinale Amotio an 9 (2%), hypotone Makulopathie an 5 (1,1%) und Hypertonien an 70 (15,6%) Augen. 150 (33,5%) Augen erhielten einen Folgeeingriff, 117 (26%) eine Phakoemulsifikation, 149 (33%) eine Fadenlockerung, 122 (27%) 5-FU-Injektionen, 42 (9,4%) eine Fadennachlegung, 33 (7,4%) ein Needling, 26 (5,8%) eine Zyklophotokoagulation, 19 (4,3%) eine Re-TE und 9 (2%) sonstige chirurgische Revisionen. Schlussfolgerung: Die Kontrolle des Augeninnendruckes ≤ 15 mm Hg ohne zusätzliche Medikation erreichten viele Patienten über einen langen Nachbeobachtungszeitraum. Die Häufigkeit der Komplikationen oder nötiger Folgeeingriffe war meist niedriger als in vergleichbaren Studien. Selbst Patienten mit hohem Risikoprofil hatten gute Ergebnisse. Aufgrund mangelnder Gesichtsfelddaten fanden sich keine Hinweise auf statistisch relevantes Fortschreiten des Glaukoms zur angestrebten medikationsfreien Druckkontrolle. Weitere Studien für einen Untersuchungszeitraum von 10 Jahren mit gleichen Erfolgskriterien wie in der vorliegenden Arbeit mit genauer Analyse der Gesichtsfelddaten wären wünschenswert, um zu belegen, dass die guten Langzeitergebnisse nach Trabekulektomie an der Universitätsaugenklinik Mainz auch eine Glaukomprogredienz dauerhaft verhindern. Damit stellt die an der Universitätsaugenklinik Mainz durchgeführte antimetabolitgestützte Trabekulektomie und deren postoperative Nachbetreuung an einer repräsentativen Population eine sichere und komplikationsarme Methode dar.

Studio sull'applicazione della piattaforma ForcetriadTM con sistema LigasureTM nella chirurgia oncologica e dei tessuti molli nel cane

Questo studio prospettico valuta l’efficacia e i vantaggi del sistema LigasureTM rispetto alle tecniche chirurgiche tradizionali, in quattro differenti procedure eseguite su 77 cani. I soggetti sono stati suddivisi in 4 gruppi, a seconda della chirurgia eseguita: Gruppo 1, 25 pazienti sottoposti a Splenectomia “aperta” semplice; Gruppo 2, 15 pazienti sottoposti a Splenectomia “aperta” complessa; Gruppo 3, 22 pazienti sottoposti ad Ovariectomia “aperta”. Gruppo 4: 18 pazienti sottoposti a Linfoadenectomia. Ciascun gruppo è stato a sua volta suddiviso in due sottogruppi: a (LigasureTM) e b (Tradizionale), a seconda della metodica utilizzata. Sono stati analizzati: il segnalamento, i parametri ematologici, le condizioni cliniche, le informazioni riguardanti l’intervento chirurgico e l’outcome. In tutti i gruppi il ricorso all’utilizzo di garze nonché dei fili da sutura sono risultati statisticamente inferiori nei pazienti operati con il sistema a radiofrequenza (Gruppo 1, P < 0.0001; Gruppo 2, P < 0,0014; Gruppo 3, P = 0,0001; Gruppo 4, P = 0,0148). Anche i tempi per la rimozione dell’organo sono significativamente ridotti in tutti i gruppi in cui è stato utilizzato il sistema LigasureTM (Gruppo 1 P < 0.0001; Gruppo 2 P < 0,0014; Gruppo 3 P = 0,0009; Gruppo 4 P = 0,0008), come i tempi chirurgici nei gruppi 1, 2 e 3 (P = 0,0287; P = 0,0064; e P = 0,0124) ed anestesiologici nei gruppi 1a e 2a (P = 0,0176; P = 0,0043). Tra le variabili analizzate, l’utilizzo del sistema di sintesi vascolare a radiofrequenza, è l’unico ad influenzare i tempi necessari per l’esecuzione della procedura. Questo studio dimostra, quindi, come il sistema LigasureTM sia sicuro ed efficace per le procedure chirurgiche esaminate, riducendo i tempi della chirurgia e limitando, quindi, i rischi per il paziente, indipendentemente dall’operatore, dall’esecuzione di altre procedure contemporanee e dalla natura della patologia splenica o linfonodale.