The Poisson-exponential regression model under different latent activation schemes

In this paper, a new family of survival distributions is presented. It is derived by considering that the latent number of failure causes follows a Poisson distribution and the time for these causes to be activated follows an exponential distribution. Three different activation schemes are also considered. Moreover, we propose the inclusion of covariates in the model formulation in order to study their effect on the expected value of the number of causes and on the failure rate function. Inferential procedure based on the maximum likelihood method is discussed and evaluated via simulation. The developed methodology is illustrated on a real data set on ovarian cancer.

A new long-term lifetime distribution induced by a latent complementary risk framework

In this paper, we proposed a new three-parameter long-term lifetime distribution induced by a latent complementary risk framework with decreasing, increasing and unimodal hazard function, the long-term complementary exponential geometric distribution. The new distribution arises from latent competing risk scenarios, where the lifetime associated scenario, with a particular risk, is not observable, rather we observe only the maximum lifetime value among all risks, and the presence of long-term survival. The properties of the proposed distribution are discussed, including its probability density function and explicit algebraic formulas for its reliability, hazard and quantile functions and order statistics. The parameter estimation is based on the usual maximum-likelihood approach. A simulation study assesses the performance of the estimation procedure. We compare the new distribution with its particular cases, as well as with the long-term Weibull distribution on three real data sets, observing its potential and competitiveness in comparison with some usual long-term lifetime distributions.

Differential MiRNA expression in childhood acute lymphoblastic leukemia and association with clinical and biological features

The present study aimed to analyze the expression profile of the microRNAs previously described as associated with childhood ALL, miR-92a, miR-100, miR-125a-5p, miR-128a, miR-181b, miR-196b and let-7e, and their association with biological/prognostic features in 128 consecutive samples of childhood acute lymphoblastic leukemia (ALL) by quantitative real-time PCR. A significant association was observed between higher expression levels of miR-196b and T-ALL, miR-100 and patients with low white blood cell count at diagnosis and t(12;21) positive ALL. These findings suggest a potential activity of these microRNAs in pediatric ALL biology. (C) 2011 Elsevier Ltd. All rights reserved.

Correlation between carotid bifurcation calcium burden on non-enhanced CT and percentage stenosis, as confirmed by digital subtraction angiography

Objectives: Previous evidence supports a direct relationship between the calcium burden (volume) on post-contrast CT with the percent internal carotid artery (ICA) stenosis at the carotid bifurcation. We sought to further investigate this relationship by comparing non-enhanced CT (NECT) and digital subtraction angiography (DSA). Methods: 50 patients (aged 41-82 years) were retrospectively identified who had undergone cervical NECT and DSA. A 64-multidetector array CT (MDCT) scanner was utilised and the images reviewed using preset window widths/levels (30/300) optimised to calcium, with the volumes measured via three-dimensional reconstructive software. Stenosis measurements were performed on DSA and luminal diameter stenoses >40% were considered "significant". Volume thresholds of 0.01, 0.03, 0.06, 0.09 and 0.12 cm(3) were utilised and Pearson's correlation coefficient (r) was calculated to correlate the calcium volume with percent stenosis. Results: Of 100 carotid bifurcations, 88 were available and of these 7 were significantly stenotic. The NECT calcium volume moderately correlated with percent stenosis on DSA r=0.53 (p<0.01). A moderate-strong correlation was found between the square root of calcium volume on NECT with percent stenosis on DSA (r=0.60, p<0.01). Via a receiver operating characteristic curve, 0.06 cm(3) was determined to be the best threshold (sensitivity 100%, specificity 90.1%, negative predictive value 100% and positive predictive value 46.7%) for detecting significant stenoses. Conclusion: This preliminary investigation confirms a correlation between carotid bifurcation calcium volume and percent ICA stenosis and is promising for the optimal threshold for stenosis detection. Future studies could utilise calcium volumes to create a "score" that could predict high grade stenosis.

Ultrasonic tissue characterization of vulnerable carotid plaque: correlation between videodensitometric method and histological examination

Abstract Background To establish the correlation between quantitative analysis based on B-mode ultrasound images of vulnerable carotid plaque and histological examination of the surgically removed plaque, on the basis of a videodensitometric digital texture characterization. Methods Twenty-five patients (18 males, mean age 67 ± 6.9 years) admitted for carotid endarterectomy for extracranial high-grade internal carotid artery stenosis (≥ 70% luminal narrowing) underwent to quantitative ultrasonic tissue characterization of carotid plaque before surgery. A computer software (Carotid Plaque Analysis Software) was developed to perform the videodensitometric analysis. The patients were divided into 2 groups according to symptomatology (group I, 15 symptomatic patients; and group II, 10 patients asymptomatic). Tissue specimens were analysed for lipid, fibromuscular tissue and calcium. Results The first order statistic parameter mean gray level was able to distinguish the groups I and II (p = 0.04). The second order parameter energy also was able to distinguish the groups (p = 0,02). A histological correlation showed a tendency of mean gray level to have progressively greater values from specimens with < 50% to >75% of fibrosis. Conclusion Videodensitometric computer analysis of scan images may be used to identify vulnerable and potentially unstable lipid-rich carotid plaques, which are less echogenic in density than stable or asymptomatic, more densely fibrotic plaques.

Histological composition and progression of carotid plaque

Abstract Background To analyse histological composition and progression of carotid plaque. Methods Thirty-one patients (22 males, mean age 68.03 ± 7.3 years) admitted for carotid endarterectomy for extracranial high-grade internal carotid artery stenosis (≥ 70% luminal narrowing) were enrolled. The patients were divided into 2 groups according to symptomatology (group I, 17 symptomatic patients; and group II, 14 asymptomatic patients). A histological analysis and inflammatory cell quantification of each excised carotid plaque was made. Nine carotid arteries were removed from human cadavers that were not preselected for carotid artery disease. These specimens were used as a control tissue without any macroscopic signs of atherosclerotic plaques. Results Fifty eight percent of all carotid plaques were classified as complex plaque with possible surface defect, hemorrhage or thrombus. The inflammatory cells concentration did not differ between the two groups. All specimens from human cadavers were classified as preatheroma with extracellular lipid pools. Conclusion Asymptomatic and symptomatic patients could have the same histological components on their carotid plaques. Fibrotic and calcific plaques could become vulnerable as complex plaques with surface defect, hemorrhage and thrombus could remain silent. Asymptomatic carotid stenosis should be followed close with no invasive diagnostic methods and clinical evaluation.

Redundant nerve roots of the cauda equina: review of the literature

In imaging diagnosis, redundant nerve roots of the cauda equina are characterized by the presence of elongated, enlarged and tortuous nerve roots in close relationship with a high-grade lumbar spinal canal stenosis. This is not an independent entity, but it is believed to be a consequence of the chronic compression at the level of the lumbar canal stenosis and thus may be part of the natural history of lumbar spinal stenosis. The present paper is aimed at reviewing the histopathological, electrophysiological and imaging findings, particularly at magnetic resonance imaging, as well as the clinical meaning of this entity. As the current assessment of canal stenosis and root compression is preferably performed by means of magnetic resonance imaging, this is the imaging method by which the condition is identified. The recognition of redundant nerve roots at magnetic resonance imaging is important, particularly to avoid misdiagnosing other conditions such as intradural arteriovenous malformations. The literature approaching the clinical relevance of the presence of redundant nerve roots is controversial. There are articles suggesting that the pathological changes of the nerve roots are irreversible at the moment of diagnosis and therefore neurological symptoms are less likely to improve with surgical decompression, but such concept is not a consensus.

Konditionale Expression von HER-2, H-Ras oder BXB-Raf1 in einem Maustumormodell

Es ist bekannt, dass die Überexpression eines einzigen Onkogens im Tumorgewebe einen maligneren Phänotyp zur Folge haben kann. Ein Beispiel hierfür ist die Rezeptortyrosinkinase HER-2. Besonders in Mamma- und Ovarialkarzinomen tritt häufig eine HER-2 Überexpression auf, die mit einer schlechteren Prognose für die Patientinnen einhergeht. Die HER-2 blockierende Therapie mit Trastuzumab (Herceptin®) konnte zu einer signifikanten Verbesserung der Überlebenszeit bei Patientinnen mit metastasierendem Mammakarzinom führen. Es ist deshalb von großem Interesse herauszufinden, ob ein Tumor durch gezielte Blockade eines bestimmten Onkogens sein tumorigenes Potential verlieren kann, und dadurch das Tumorwachstum zumindest zeitweise unterbunden wird. Die Frage ist also, ob ein Tumor reversibel sein kann, wenn die Expression seiner Onkogene blockiert wird. Frühere Arbeiten meiner Arbeitsgruppe haben gezeigt, dass Tumore, die konditional humanes HER-2 exprimierten, nach Ausschalten von HER-2 tatsächlich in Remission gingen, d.h. reversibel waren. Tumorgrößenabhängig konnte sogar eine vollständige Tumorremission beobachtet werden. Die vorliegende Arbeit soll nun helfen, die beobachtete Remission nach Ausschalten von HER-2 besser verstehen zu können. Von Interesse sind dabei vor allem die molekularen Mechanismen, die in dem Tumor nach Ausschalten der HER-2 Expression ablaufen. Die konditionale Expression von HER-2 wurde mit Hilfe des TET-OFF Systems in NIH3T3 Mausfibroblasten erreicht. Mit dieser Technik wurde ein Maustumormodell etabliert, das ermöglichte, die Veränderungen in den Tumoren nach Ausschalten von HER-2 zu untersuchen. Ein besonderes Augenmerk wurde dabei auf zwei der durch HER-2 vermittelten Signalwege gerichtet, den Ras-MAP Kinase Signalweg und die Aktivierung von Akt über die Phosphoinositol-3 Kinase. Beide wurden nach Ausschalten der HER-2 Expression deaktiviert. Um herausfinden zu können, welcher der beiden Wege eine wichtigere Rolle bei der Tumorremission spielt, wurden in der vorliegenden Arbeit zwei weitere Maustumormodelle zur konditionalen Expression von humanem H-Ras bzw. einer Form des humanen c-Raf-1 (BXB-Raf1) etabliert. Die Modelle funktionierten auf dieselbe Weise wie das HER-2 Maustumormodell und es wurden auch dieselben Faktoren untersucht. Ras und Raf sind Mitglieder des Ras-MAP Kinase Signalweges. Raf ist aber im Gegensatz zu HER-2 und Ras nicht in der Lage, Akt zu aktivieren. Durch Vergleich der Ergebnisse der drei Maustumormodelle war es deshalb möglich zu differenzieren, ob Einflüsse auf die Tumorentwicklung über denn Ras-MAP Kinase oder den PI3K/Akt Signalweg vermittelt wurden. Auch Ausschalten von H-Ras oder BXB-Raf1 führte zu einer raschen Tumorremission. Damit wurde erneut die Frage nach der Reversibilität eines Tumors beantwortet. Ob die Remission auf einer Induktion von Apoptose beruhte, konnte nicht endgültig geklärt werden, da es zwar nach Ausschalten von HER-2 zu einer Erhöhung der Apoptoserate kam, nicht jedoch nach Ausschalten von H-Ras oder BXB-Raf1. Aufgrund der vorhandenen Ergebnisse wird vermutet, dass es zu einer Störung des Gleichgewichtes zwischen proliferationsfördernden und apoptotischen Faktoren nach Ausschalten der Onkogene kam. Die in den Tumoren vorhandene Spontanapoptose könnte dann ausreichen, den Prozess der Tumorremission auszulösen. Die Untersuchungen haben gezeigt, dass ERK bzw. der Ras-MAP Kinase Signalweg die bedeutendere Rolle bei der Tumorremission spielte. Zum einen wurde dies belegt durch die Beobachtung, dass die Tumorverläufe von HER-2 und BXB-Raf1 nahezu identisch waren. Zum anderen kam es in allen drei Modellen zu einer Dephosphorylierung von ERK, die der Tumorremission vorausging. Akt schien dagegen keine Rolle zu spielen, da das Ausschalten der HER-2, H-Ras oder BXB-Raf1 Expression zu keiner einheitlichen Veränderung des Posphorylierungsgrades von Akt führte. Demnach ist die Blockade des Ras-MAP Kinase Signalweges, der hauptsächlich proliferationsfördernde Eigenschaften besitzt, wichtiger für die Tumorremission als die Blockade des PI3K/Akt Signalweges, der hauptsächlich anti-apoptotische Eigenschaften vermittelt.

Geochronological and structural evolution of the western and central Kaoko Belt in NW Namibia

This thesis focusses on the tectonic evolution and geochronology of part of the Kaoko orogen, which is part of a network of Pan-African orogenic belts in NW Namibia. By combining geochemical, isotopic and structural analysis, the aim was to gain more information about how and when the Kaoko Belt formed. The first chapter gives a general overview of the studied area and the second one describes the basis of the Electron Probe Microanalysis dating method. The reworking of Palaeo- to Mesoproterozoic basement during the Pan-African orogeny as part of the assembly of West Gondwana is discussed in Chapter 3. In the study area, high-grade rocks occupy a large area, and the belt is marked by several large-scale structural discontinuities. The two major discontinuities, the Sesfontein Thrust (ST) and the Puros Shear Zone (PSZ), subdivide the orogen into three tectonic units: the Eastern Kaoko Zone (EKZ), the Central Kaoko Zone (CKZ) and the Western Kaoko Zone (WKZ). An important lineament, the Village Mylonite Zone (VMZ), has been identified in the WKZ. Since plutonic rocks play an important role in understanding the evolution of a mountain belt, zircons from granitoid gneisses were dated by conventional U-Pb, SHRIMP and Pb-Pb techniques to identify different age provinces. Four different age provinces were recognized within the Central and Western part of the belt, which occur in different structural positions. The VMZ seems to mark the limit between Pan-African granitic rocks east of the lineament and Palaeo- to Mesoproterozoic basement to the west. In Chapter 4 the tectonic processes are discussed that led to the Neoproterozoic architecture of the orogen. The data suggest that the Kaoko Belt experienced three main phases of deformation, D1-D3, during the Pan-African orogeny. Early structures in the central part of the study area indicate that the initial stage of collision was governed by underthrusting of the medium-grade Central Kaoko zone below the high-grade Western Kaoko zone, resulting in the development of an inverted metamorphic gradient. The early structures were overprinted by a second phase D2, which was associated with the development of the PSZ and extensive partial melting and intrusion of ~550 Ma granitic bodies in the high-grade WKZ. Transcurrent deformation continued during cooling of the entire belt, giving rise to the localized low-temperature VMZ that separates a segment of elevated Mesoproterozoic basement from the rest of the Western zone in which only Pan-African ages have so far been observed. The data suggest that the boundary between the Western and Central Kaoko zones represents a modified thrust zone, controlling the tectonic evolution of the Kaoko belt. The geodynamic evolution and the processes that generated this belt system are discussed in Chapter 5. Nd mean crustal residence ages of granitoid rocks permit subdivision of the belt into four provinces. Province I is characterised by mean crustal residence ages <1.7 Ga and is restricted to the Neoproterozoic granitoids. A wide range of initial Sr isotopic values (87Sr/86Sri = 0.7075 to 0.7225) suggests heterogeneous sources for these granitoids. The second province consists of Mesoproterozoic (1516-1448 Ma) and late Palaeo-proterozoic (1776-1701 Ma) rocks and is probably related to the Eburnian cycle with Nd model ages of 1.8-2.2 Ga. The eNd i values of these granitoids are around zero and suggest a predominantly juvenile source. Late Archaean and middle Palaeoproterozoic rocks with model ages of 2.5 to 2.8 Ga make up Province III in the central part of the belt and are distinct from two early Proterozoic samples taken near the PSZ which show even older TDM ages of ~3.3 Ga (Province IV). There is no clear geological evidence for the involvement of oceanic lithosphere in the formation of the Kaoko-Dom Feliciano orogen. Chapter 6 presents the results of isotopic analyses of garnet porphyroblasts from high-grade meta-igneous and metasedimentary rocks of the sillimanite-K-feldspar zone. Minimum P-T conditions for peak metamorphism were calculated at 731±10 °C at 6.7±1.2 kbar, substantially lower than those previously reported. A Sm-Nd garnet-whole rock errorchron obtained on a single meta-igneous rock yielded an unexpectedly old age of 692±13 Ma, which is interpreted as an inherited metamorphic age reflecting an early Pan-African granulite-facies event. The dated garnets survived a younger high-grade metamorphism that occurred between ca. 570 and 520 Ma and apparently maintained their old Sm-Nd isotopic systematics, implying that the closure temperature for garnet in this sample was higher than 730 °C. The metamorphic peak of the younger event was dated by electronmicroprobe on monazite at 567±5 Ma. From a regional viewpoint, it is possible that these granulites of igneous origin may be unrelated to the early Pan-African metamorphic evolution of the Kaoko Belt and may represent a previously unrecognised exotic terrane.

Characterization of igneous terranes by zircon dating: implications for the UHP relicts occurrences and suture identification in the Central Rhodope, Northern Greece

One of the key for the understanding of an orogenic belt is the characterization of the terranes involved and the identification of the suture(s) separating crustal blocks: these are essential information for large-scale paleo-reconstructions. In addition, the structural relationships between the terranes involved in the collisional processes and the eventual UHP relicts may provide first order inputs to exhumation models of subducted rocks. The structure of the Rhodope Massif (northern Greece and southern Bulgaria) results from the stacking of high-grade nappes during a continental collision, which age is comprised between Latest-Jurassic and Early-Cenozoic. UHP and HP relicts, associated with oceanic and ultramafic material, suggest the presence of a dismembered suture zone within the massif. The location of this suture remains unclear; furthermore, up to now, the UHP and eclogitic localities represent isolated spots and no synthesis on their structural position within the massif has been proposed. The first aim of this work is to define the relationships between HP-UHP relicts, crustal blocks, shear zones and amphibolitic material. To achieve this objective, we characterized the accreted blocks in terms of protoliths ages of the orthogneisses mainly along two cross sections on the Greek part of the belt. Geochemical affinities of meta-igneous rocks served as a complementary tool for terrane characterization and geodynamic interpretation. Single-zircon Pb-Pb evaporation and zircon U-Pb SHRIMP dating of orthogneiss protoliths define two groups of intrusion-ages: Permo-Carboniferous and Late Jurassic-Early Cretaceous. Structurally, these two groups correspond to distinct units: the Late Jurassic gneissic complex overthrusts the one bearing the Permo-Carboniferous orthogneisses. Mylonites, eclogites, amphibolites of oceanic affinities, and UHP micaschists, mark a “melange” zone, intensively sheared towards the SW, which separates the two units. Thus, we interpret them as two distinct terranes, the Rhodope and Thracia terranes, separated by the Nestos suture. The correlation of our findings in northern Greece to the Bulgarian part of the Massif suggests a northern rooting of the Nestos Suture. This configuration results of the closure of a marginal oceanic basin of the Tethys system by a north-directed subduction. This interpretation is supported by the geochemical affinities of the orthogneisses: the Late-Jurassic igneous rocks formed by subduction-related magmatism, pprobably the same north-directed subduction that gave rise to the UHP metamorphism of the metasediments of the “melange” zone. It is noteworthy that the UHP-HP relicts seem to be restricted to the contact between the two terranes suggesting that the UHP relicts are exhumed only within the suture zone. Furthermore, the singularity of the suture suggests that the Late-Jurassic subduction explains the occurrence of UHP and eclogite relicts in the Central Rhodope despite the large age range previously attributed the UHP and/or HP stage.

Die Re-Definition der Wirklichkeit durch Motto-Events

Eine aktuelle Ausprägung der Veranstaltungslandschaft sind die so genannten Motto-Events, die die Inszenierung einer Anderswelt-Konstruktion einsetzen, um emotionale und kommunikatorische Ziele zu erreichen. Dabei werden themengebundene Entwürfe räumlich und inhaltlich in die lebensweltliche Wirklichkeit transportiert und auf diese Weise eine dynamische und integrative Scheinwelt erschaffen. In dieser konstruierten Welt können schließlich Abenteuer erlebt und heroische Taten begangen werden. Durch die reziproke Beeinflussung von Inszenierung und Handlung befinden sich die Akteure außerhalb der gesellschaftlichen Norm, sie erleben innerhalb der "gated community" der Motto-Veranstaltung eine re-definierte Wirklichkeit. Aus einer Kombination von aktiven und passiven Elementen werden homogene Klischees inszeniert, die durch ihren Bekanntheitsgrad eine hohe Anschlussfähigkeit der Teilnehmer garantieren. Die vorliegende Arbeit beschäftigt sich mit den Mechanismen, die diese re-definierte Wirklichkeit in Szene setzen. Dadurch wird es möglich, in einer zusammenfassenden Betrachtung die Rezeption verschiedener Event-Modelle zu beschreiben und Handlungsempfehlungen zu geben.

Partial melting within the lower crust – Constraints from bulk rock geochemical data and trace element mineral analyses of granulites and migmatites from Central Finland

This PhD thesis concerns geochemical constraints on recycling and partial melting of Archean continental crust. A natural example of such processes was found in the Iisalmi area of Central Finland. The rocks from this area are Middle to Late Archean in age and experienced metamorphism and partial melting between 2.7-2.63 Ga. The work is based on extensive field work. It is furthermore founded on bulk rock geochemical data as well as in-situ analyses of minerals. All geochemical data were obtained at the Institute of Geosciences, University of Mainz using X-ray fluorescence, solution ICP-MS and laser ablation-ICP-MS for bulk rock geochemical analyses. Mineral analyses were accomplished by electron microprobe and laser ablation ICP-MS. Fluid inclusions were studied by microscope on a heating-freezing-stage at the Geoscience Center, University Göttingen. Part I focuses on the development of a new analytical method for bulk rock trace element determination by laser ablation-ICP-MS using homogeneous glasses fused from rock powder on an Iridium strip heater. This method is applicable for mafic rock samples whose melts have low viscosities and homogenize quickly at temperatures of ~1200°C. Highly viscous melts of felsic samples prevent melting and homogenization at comparable temperatures. Fusion of felsic samples can be enabled by addition of MgO to the rock powder and adjustment of melting temperature and melting duration to the rock composition. Advantages of the fusion method are low detection limits compared to XRF analyses and avoidance of wet-chemical processing and use of strong acids as in solution ICP-MS as well as smaller sample volumes compared to the other methods. Part II of the thesis uses bulk rock geochemical data and results from fluid inclusion studies for discrimination of melting processes observed in different rock types. Fluid inclusion studies demonstrate a major change in fluid composition from CO2-dominated fluids in granulites to aqueous fluids in TTG gneisses and amphibolites. Partial melts were generated in the dry, CO2-rich environment by dehydration melting reactions of amphibole which in addition to tonalitic melts produced the anhydrous mineral assemblages of granulites (grt + cpx + pl ± amph or opx + cpx + pl + amph). Trace element modeling showed that mafic granulites are residues of 10-30 % melt extraction from amphibolitic precursor rocks. The maximum degree of melting in intermediate granulites was ~10 % as inferred from modal abundances of amphibole, clinopyroxene and orthopyroxene. Carbonic inclusions are absent in upper-amphibolite facies migmatites whereas aqueous inclusion with up to 20 wt% NaCl are abundant. This suggests that melting within TTG gneisses and amphibolites took place in the presence of an aqueous fluid phase that enabled melting at the wet solidus at temperatures of 700-750°C. The strong disruption of pre-metamorphic structures in some outcrops suggests that the maximum amount of melt in TTG gneisses was ~25 vol%. The presence of leucosomes in all rock types is taken as the principle evidence for melt formation. However, mineralogical appearance as well as major and trace element composition of many leucosomes imply that leucosomes seldom represent frozen in-situ melts. They are better considered as remnants of the melt channel network, e.g. ways on which melts escaped from the system. Part III of the thesis describes how analyses of minerals from a specific rock type (granulite) can be used to determine partition coefficients between different minerals and between minerals and melt suitable for lower crustal conditions. The trace element analyses by laser ablation-ICP-MS show coherent distribution among the principal mineral phases independent of rock composition. REE contents in amphibole are about 3 times higher than REE contents in clinopyroxene from the same sample. This consistency has to be taken into consideration in models of lower crustal melting where amphibole is replaced by clinopyroxene in the course of melting. A lack of equilibrium is observed between matrix clinopyroxene / amphibole and garnet porphyroblasts which suggests a late stage growth of garnet and slow diffusion and equilibration of the REE during metamorphism. The data provide a first set of distribution coefficients of the transition metals (Sc, V, Cr, Ni) in the lower crust. In addition, analyses of ilmenite and apatite demonstrate the strong influence of accessory phases on trace element distribution. Apatite contains high amounts of REE and Sr while ilmenite incorporates about 20-30 times higher amounts of Nb and Ta than amphibole. Furthermore, trace element mineral analyses provide evidence for magmatic processes such as melt depletion, melt segregation, accumulation and fractionation as well as metasomatism having operated in this high-grade anatectic area.

Identificazione di fattori trascrizionali associati al differenziamento neurale in cellule di sarcoma di Ewing: ruolo di NF-kB

Il sarcoma di Ewing (ES) è un tumore maligno pediatrico dell’apparato scheletrico; è associato a una traslocazione specifica codificante la proteina di fusione EWS-FLI1 e all’alta espressione di CD99, una glicoproteina di membrana fisiologicamente coinvolta in diversi processi biologici. EWS-FLI1 e CD99, sono riportati avere ruoli divergenti nella modulazione della malignità e del differenziamento di ES. CD99 inoltre è riportato modulare il pathway di MAPK, il quale interagendo con molteplici fattori di trascrizione partecipa a processi di proliferazione e differenziamento. In questo studio abbiamo investigato in due linee cellulari di ES silenziate per CD99 (TC-71shCD99 e IOR/CARshCD99) l’attività basale di diversi fattori trascrizionali quali: NF-kBp65, AP1, Elk-1, E2F e CREB. L’unico fattore trascrizionale statisticamente significativo è risultato essere NF-kBp65 e abbiamo valutato il suo ruolo nel differenziamento neurale di cellule di ES e la relazione con EWS-FLI1 e CD99. L’attività trascrizionale di NF-kB è stata valutata attraverso gene reporter assay in linee cellulari di ES a diversa espressione di CD99, EWS-FLI1 e NF-kB stesso. Il differenziamento neurale è stato valutato come espressione di βIII-Tubulin in immunofluorescenza. Il silenziamento di CD99 induce una down-modulazione dell’attività trascrizionale di NF-kB, mentre il knockdown di EWS-FLI1 ne induce un’aumento. Inoltre, il silenziamento di EWS-FLI1 non è in grado di contrastare la riduzione dell’attività di NF-kB osservata dopo silenziamento di CD99, suggerendo un ruolo dominante del CD99 nel signaling di NF-kB. Cellule deprivate di CD99 ma non di EWS-FLI1, mostrano un fenotipo differenziato in senso neurale, fenotipo che viene perso quando le cellule sono indotte a sovraesprimere NF-kB. Inoltre, in cellule CD99 positive, il silenziamento di NF-kB induce un leggero differenziamento neurale. In conclusione, questi dati hanno evidenziato il ruolo di NF-kB nel differenziamento di cellule di ES e che potrebbe essere un potenziale target nel ridurre la progressione di questo tumore.

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.

Entwicklung des Emirates Qatar : Strategien - Probleme - Erfolge

Qatar boomt. Da es hierzu keine ganzheitlichen Forschungsarbeiten gibt, werden in dieser Arbeit die neuesten Entwicklungen und Planungen mit hoher Aktualität und Praxisrelevanz erstmals erfasst und analysiert. Der Autor führt Informationssplitter von internationalen Organisationen und eigene Recherchen in ein ganzheitliches Bild zusammen. Qatar ist sich bewusst, dass Wachstum endlich sein kann. Welche Möglichkeiten hat das kleine Qatar von der Globalisierung zu profitieren und für sich Vorteile für die Zukunft nach dem Öl zu generieren? Der Fokus der Arbeit liegt auf den ökonomische und ökologischen Stellschrauben der Transformation unter wirtschaftsgeographischen, soziodemographischen und strategischen Gesichtspunkten mit lokalen, regionalen und internationalen Betrachtungsweisen in den Themenfeldern (Welt-) Wirtschaft, Bildung, Infrastruktur und Umwelt. Ausgewählte Faktorungleichgewichte werden in Bezug auf Aussenwirtschaft und Binnenwirtschaft erläutert sowie die Nutzung von korankonformen Finanzierungsinstrumenten und Direktinvestitionen von und in Qatar.rnrnKeywords: Qatar / Katar / Peak-Oil / Emirat / FDI / Qatarisches Modell / Masterplan / Wohlfahrtsmehrung / Disparität / Nachhaltigkeit / Islamic Banking / Agglomeration / Akkumulation / Globalisierung / Arabische Halbinsel / Persischer Golf / Faktor- Gleichgewichte / Doha / Aluminium / LNG / Gas / best practicern