Erosione e sollevamento nell'arco calabro-peloritano

The Calabrian-Peloritani arc represents key site to unravel evolution of surface processes on top of subducting lithosphere. During the Pleistocene, in fact the arc uplifted at rate of the order of about 1mm/yr, forming high-standing low-relief upland (figure 2). Our study is focused on the relationship between tectonic and land evolution in the Sila Massif, Messina strait and Peloritani Mts. Landforms reflect a competition between tectonic, climatic, and surficial processes. Many landscape evolution models that explore feedbacks between these competing processes, given steady forcing, predict a state of erosional equilibrium, where the rates of river incision and hillslope erosion balance rock uplift. It has been suggested that this may be the final constructive stage of orogenic systems. Assumptions of steady erosion and incision are used in the interpretation of exhumation and uplift rates from different geologic data, and in the formulation of fluvial incision and hillslope evolution models. In the Sila massif we carried out cosmogenic isotopes analysis on 24 samples of modern fluvial sediments to constrain long-term (~103 yr) erosion rate averaged on the catchment area. 35 longitudinal rivers profiles have been analyzed to study the tectonic signal on the landscape evolution. The rivers analyzed exhibit a wide variety of profile forms, diverging from equilibrium state form. Generally the river profiles show at least 2 and often 3 distinct concave-up knickpoint-bounded segments, characterized by different value of concavity and steepness indices. River profiles suggest three main stages of incision. The values of ks and θ in the lower segments evidence a decrease in river incision, due probably to increasing uplift rate. The cosmogenic erosion rates pointed out that old landscape upland is eroding slowly at ~0.1 mm/yr. In the contrary, the flanks of the massif is eroding faster with value from 0.4 to 0.5 mm/yr due to river incision and hillslope processes. Cosmogenic erosion rates mach linearly with steepness indices and with average hillslope gradient. In the Messina area the long term erosion rate from low-T thermochronometry are of the same order than millennium scale cosmogenic erosion rate (1-2 mm/yr). In this part of the chain the fast erosion is active since several million years, probably controlled by extensional tectonic regime. In the Peloritani Mts apatite fission-track and (U-Th)/He thermochronometry are applied to constraint the thermal history of the basement rock. Apatite fission-track ages range between 29.0±5.5 and 5.5±0.9 Ma while apatite (U-Th)/He ages vary from 19.4 to 1.0 Ma. Most of the AFT ages are younger than the overlying terrigenous sequence that in turn postdates the main orogenic phase. Through the coupling of the thermal modelling with the stratigraphic record, a Middle Miocene thermal event due to tectonic burial is unravel. This event affected a inner-intermediate portion of the Peloritani belt confined by young AFT data (<15 Ma) distribution. We interpret this thermal event as due to an out-of–sequence thrusting occurring in the inner portion of the belt. Young (U-Th)/He ages (c. 5 Ma) record a final exhumation stage with increasing rates of denudation since the Pliocene times due to postorogenic extensional tectonics and regional uplift. In the final chapter we change the spatial scale to insert digital topography analysis and field data within a geodynamic model that can explain surface evidence produced by subduction process.

La Pace Calda. La nascita del movimento antinucleare negli Stati Uniti e in Gran Bretagna, 1957-1963

The aim of this proposal is to offer an alternative perspective on the study of Cold War, since insufficient attention is usually paid to those organizations that mobilized against the development and proliferation of nuclear weapons. The antinuclear movement began to mobilize between the 1950s and the 1960s, when it finally gained the attention of public opinion, and helped to build a sort of global conscience about nuclear bombs. This was due to the activism of a significant part of the international scientific community, which offered powerful intellectual and political legitimization to the struggle, and to the combined actions of the scientific and organized protests. This antinuclear conscience is something we usually tend to consider as a fait accompli in contemporary world, but the question is to show its roots, and the way it influenced statesmen and political choices during the period of nuclear confrontation of the early Cold War. To understand what this conscience could be and how it should be defined, we have to look at the very meaning of the nuclear weapons that has deeply modified the sense of war. Nuclear weapons seemed to be able to destroy human beings everywhere with no realistic forms of control of the damages they could set off, and they represented the last resource in the wide range of means of mass destruction. Even if we tend to consider this idea fully rational and incontrovertible, it was not immediately born with the birth of nuclear weapons themselves. Or, better, not everyone in the world did immediately share it. Due to the particular climate of Cold War confrontation, deeply influenced by the persistence of realistic paradigms in international relations, British and U.S. governments looked at nuclear weapons simply as «a bullet». From the Trinity Test to the signature of the Limited Test Ban Treaty in 1963, many things happened that helped to shift this view upon nuclear weapons. First of all, more than ten years of scientific protests provided a more concerned knowledge about consequences of nuclear tests and about the use of nuclear weapons. Many scientists devoted their social activities to inform public opinion and policy-makers about the real significance of the power of the atom and the related danger for human beings. Secondly, some public figures, as physicists, philosophers, biologists, chemists, and so on, appealed directly to the human community to «leave the folly and face reality», publicly sponsoring the antinuclear conscience. Then, several organizations leaded by political, religious or radical individuals gave to this protests a formal structure. The Campaign for Nuclear Disarmament in Great Britain, as well as the National Committee for a Sane Nuclear Policy in the U.S., represented the voice of the masses against the attempts of governments to present nuclear arsenals as a fundamental part of the international equilibrium. Therefore, the antinuclear conscience could be defined as an opposite feeling to the development and the use of nuclear weapons, able to create a political issue oriented to the influence of military and foreign policies. Only taking into consideration the strength of this pressure, it seems possible to understand not only the beginning of nuclear negotiations, but also the reasons that permitted Cold War to remain cold.

Spaltspuranlyse von Uranoxidpartikeln

Kerntechnische Anlagen werden weltweit vonInspektoren der Atomenergiebehörden kontrolliert.Dabei werden in den Anlagen Wischtestproben genommen,die anschließend auf darin enthaltene Staubpartikeluntersucht werden. Die Zusammensetzung dieser Partikel- vor allem der U-235-Anreicherungsgrad in Uranoxidpartikeln -lassen wichtige Rückschlüsse auf die in den Anlagen durchgeführten Operationen zu. In dieser Arbeit wurde ein einfaches Screening-Verfahrenzur Lokalisierung von Uranoxidpartikeln in Wischtestprobenentwickelt. Dieses Verfahren basiert auf dem Prinzip derSpaltspuranalyse und erlaubt eine grobe Abschätzung desU-235-Anreicherungsgrades in Uranoxidpartikeln beibekanntem Partikeldurchmesser durch Auszählen der Spaltspuren je Partikel. Zur Entwicklung und Kalibrierung dieser Methode wurdenUranoxidpartikel mit definiertem Durchmesser und definierter Isotopenzusammensetzung hergestellt und mitder Rasterelektronenmikroskopie sowie der Sekundärionenmassenspektroskopie charakterisiert.

Effetto di un packaging innovativo sulla qualità di nettarine

L’imballaggio alimentare si pu�� definire come un sistema coordinato per disporre i beni per il trasporto, la distribuzione, la conservazione, la vendita e l’utilizzo. Uno dei materiali maggiormente impiegati, nell’industria alimentare, per la produzione di imballaggi sono le materie plastiche. Esse sono sostanze organiche derivanti da petrolio greggio, sono composti solidi allo stato finito, ma possono essere modellate allo stato fluido. Un imballaggio alimentare deve svolgere determinate funzioni tra cui: - contenimento del prodotto - protezione del prodotto da agenti esterni - logistica - comunicativa - funzionale - ecologica L'ultimo punto sopracitato è il principale problema delle materie plastiche derivanti dal petrolio greggio. Questi materiali sono difficilmente riciclabili perché spesso un imballaggio è composto da più materiali stratificati o perché si trova a diretto contatto con gli alimenti. Inoltre questi materiali hanno un lungo tempo di degradazione (da 100 a 1000 anni) che ne rendono difficile e costoso lo smaltimento. Per questo nell’ultimo decennio è cominciata la ricerca di un materiale plastico, flessibile alle esigenze industriali e nel contempo biodegradabile. Una prima idea è stata quella di “imitare la natura” cercando di replicare macromolecole già esistenti (derivate da amido e zuccheri) per ottenere una sostanza plastico-simile utilizzabile per gli stessi scopi, ma biodegradabile in circa sei mesi. Queste bioplastiche non hanno preso piede per l’alto costo di produzione e perché risulta impossibile riconvertire impianti di produzione in tutto il mondo in tempi brevi. Una seconda corrente di pensiero ha indirizzato i propri sforzi verso l’utilizzo di speciali additivi aggiunti in minima misura (1%) ai classici materiali plastici e che ne permettono la biodegradazione in un tempo inferiore ai tre anni. Un esempio di questo tipo di additivi è l’ECM Masterbatch Pellets che è un copolimero di EVA (etilene vinil acetato) che aggiunto alle plastiche tradizionali rende il prodotto finale completamente biodegradabile pur mantenendo le proprie caratteristiche. Scopo di questo lavoro di tesi è stato determinare le modificazioni di alcuni parametri qualitativi di nettarine di Romagna(cv.-Alexa®) confezionate-con-film-plastici-tradizionali-e-innovativi. I campioni di nettarine sono stati confezionati in cestini in plastica da 1 kg (sigillati con un film flow-pack macroforato) di tipo tradizionale in polipropilene (campione denominato TRA) o vaschette in polipropilene additivato (campione denominato BIO) e conservati a 4°C e UR 90-95% per 7 giorni per simulare un trasporto refrigerato successivamente i campioni sono stati posti in una camera a 20°C e U.R. 50% per 4 giorni al fine di simulare una conservazione al punto vendita. Al tempo 0 e dopo 4, 7, 9 e 11 giorni sono state effettuate le seguenti analisi: - coefficiente di respirazione è stato misurata la quantità di CO2 prodotta - indice di maturazione espresso come rapporto tra contenuto in solidi solubili e l’acidità titolabile - analisi di immagine computerizzata - consistenza della polpa del frutto è stata misurata attraverso un dinamometro Texture Analyser - contenuto in solidi totali ottenuto mediante gravimetria essiccando i campioni in stufa sottovuoto - caratteristiche sensoriali (Test Accettabilità) Conclusioni In base ai risultati ottenuti i due campioni non hanno fatto registrare dei punteggi significativamente differenti durante tutta la conservazione, specialmente per quanto riguarda i punteggi sensoriali, quindi si conclude che le vaschette biodegradabili additivate non influenzano la conservazione delle nettarine durante la commercializzazione del prodotto limitatamente ai parametri analizzati. Si ritiene opportuno verificare se il processo di degradazione del polimero additivato si inneschi già durante la commercializzazione della frutta e soprattutto verificare se durante tale processo vengano rilasciati dei gas che possono accelerare la maturazione dei frutti (p.e. etilene), in quanto questo spiegherebbe il maggiore tasso di respirazione e la più elevata velocità di maturazione dei frutti conservati in tali vaschette. Alimentary packaging may be defined as a coordinate system to dispose goods for transport, distribution, storage, sale and use. Among materials most used in the alimentary industry, for the production of packaging there are plastics materials. They are organic substances deriving from crude oil, solid compounds in the ended state, but can be moulded in the fluid state. Alimentary packaging has to develop determinated functions such as: - Product conteniment - Product protection from fieleders agents - logistic - communicative - functional - ecologic This last term is the main problem of plastic materials deriving from crude oil. These materials are hardly recyclable because a packaging is often composed by more stratified materials or because it is in direct contact with aliments. Beside these materials have a long degradation time(from 100 to 1000 years) that make disposal difficult and expensive. For this reason in the last decade the research for a new plastic material is begin, to make industrial demands more flexible and, at the same time, to make this material biodegradable: At first, the idea to “imitate the nature” has been thought, trying to reply macromolecules already existents (derived from amid and sugars) to obtain a similar-plastic substance that can be used for the same purposes, but it has to be biodegradable in about six months. These bioplastics haven’t more success bacause of the high production cost and because reconvert production facilities of all over the wolrd results impossible in short times. At second, the idea to use specials addictives has been thought. These addictives has been added in minim measure (1%) to classics plastics materials and that allow the biodegradation in a period of time under three years. An example of this kind of addictives is ECM Masterbatch Pellets which is a coplymer of EVA (Ethylene vinyl acetate) that, once it is added to tradizional plastics, make final product completely biodegradable however maintaining their own attributes. The objective of this thesis work has been to determinate modifications of some Romagna’s Nectarines’ (cv. Alexa®) qualitatives parameters which have been packaged-with traditional and innovative-plastic film. Nectarines’ samples have been packaged in plastic cages of 1 kg (sealed with a macro-drilled flow-pack film) of traditional type in polypropylene (sample named TRA) or trays in polypropylene with addictives (sample named BIO) and conservated at 4°C and UR 90-95% for 7 days to simulate a refrigerated transport. After that, samples have been put in a camera at 20°C and U.R. 50% for 4 days to simulate the conservation in the market point. At the time 0 and after 4, 7, 9 and 11 days have been done the following analaysis: - Respiration coefficient wherewith the amount CO2 producted has been misurated - Maturation index which is expressed as the ratio between solid soluble content and the titratable acidity - Analysis of computing images - Consistence of pulp of the fruit that has been measured through Texture Analyser Dynanometer - Content in total solids gotten throught gravimetry by the drying of samples in vacuum incubator - Sensorial characteristic (Panel Test) Consequences From the gotten results, the two samples have registrated no significative different scores during all the conservation, expecially about the sensorial scores, so it’s possible to conclude that addictived biodegradable trays don’t influence the Nectarines’ conservation during the commercialization of the product qualifiedly to analized parameters. It’s advised to verify if the degradation process of the addicted polymer may begin already during the commercialization of the fruit and in particular to verify if during this process some gases could be released which can accelerate the maturation of fruits (p.e. etylene), because all this will explain the great respiration rate and the high speed of the maturation of fruits conservated in these trays.

Evoluzione Morfotettonica delle Aree Alpine "Sempione" e "Brennero" attraverso Studi Termocronologici di bassa temperatura

E’ mostrata l’analisi e la modellazione di dati termocronologici di bassa temperatura da due regioni Alpine: il Sempione ed il Brennero. Le faglie distensive presenti bordano settori crostali profondi appartenenti al dominio penninico: il duomo metamorfico Lepontino al Sempione e la finestra dei Tauri al Brennero. I dati utilizzati sono FT e (U-Th)/He su apatite. Per il Sempione i dati provengono dalla bibliografia; per il Brennero si è provveduto ad un nuovo campionamento, sia in superficie che in sotterraneo. Gli attuali lavori per la galleria di base del Brennero (BBT), hanno consentito, per la prima volta, di raccogliere dati di FT e (U-Th)/He in apatite in sottosuolo per la finestra dei Tauri occidentale. Le analisi sono state effettuate tramite un codice a elementi finiti, Pecube, risolvente l’equazione di diffusione del calore per una topografia evolvente nel tempo. Il codice è stato modificato per tener conto dei dati sotterranei. L’inversione dei dati è stata effettuata usando il Neighbourhood Algorithm (NA), per ottenere il più plausibile scenario di evoluzione morfotettonico. I risultati ottenuti per il Sempione mostrano: ipotetica evoluzione dello stile tettonico della faglia del Sempione da rolling hinge a low angle detachment a 6.5 Ma e la cessazione dell’attività a 3 Ma; costruzione del rilievo fino a 5.5 Ma, smantellamento da 5.5 Ma ad oggi, in coincidenza dei cambiamenti climatici Messiniani e relativi all’inizio delle maggiori glaciazioni; incremento dell’esumazione da 0–0.6 mm/anno a 0.6–1.2 mm/anno a 2.4 Ma nell’emisfero settentrionale. I risultati al Brennero mostrano: maggiore attività tettonica della faglia del Brennero (1.3 mm/anno), maggiore attività esumativa (1–2 mm/anno) prima dei 10 Ma; crollo dell’attività della faglia del Brennero fra 10 Ma e oggi (0.1 mm/anno) e dell’attività esumativa nello stesso periodo (0.1–0.3 mm/anno); nessun aumento del tasso esumativo o variazioni topografiche negli ultimi 5 Ma.

Capacità di sviluppo di Diabrotica virgifera virgifera Leconte su ospiti alternativi al mais

Diabrotica virgifera virgifera LeConte (Coleoptera: Chrysomelidae) è una specie esotica invasiva di origine centro americana e introdotta in Europa agli inizi degli anni ’90, in Italia nel 1998. Considerata negli Stati Uniti la principale avversità del mais (Zea mais L.), è oggi presente in quasi tutti i Paesi europei dove è presente tale coltura. Poiché il mais risulta l’ospite prioritario di Diabrotica, attualmente il principale metodo di contenimento consiste nella rotazione con una coltura non ospite. L’obiettivo del lavoro è stato quello di indagare sulle piante ospiti alternative al mais nel nostro ambiente, accertando il ruolo che possono avere le infestanti o altre Poaceae coltivate nella biologia della Diabrotica. Tali essenze sono state scelte tra specie mai sottoposte a sperimentazione e tra quelli già oggetto di indagini, ma su cui si sono ottenuti esiti discordi o non soddisfacenti. Sono state allestite prove con infestazione artificiale in ambiente controllato e prove in campo per valutare la sopravvivenza larvale e il completamento del ciclo, nonché le prestazioni biologiche degli individui ottenuti. Le ricerche hanno permesso di osservare sopravvivenza di Diabrotica su numerose graminacee, in particolare cereali. Tale capacità è confermata dalla presenza di larve di diversa età e in alcuni casi di pupe sulle specie ospiti alternative, sia con infestazione artificiale che in campo. Tuttavia crescita e sviluppo su queste piante sono stati più lenti del mais e gli stadi giovanili trovati hanno mostrato caratteristiche morfometriche inferiori rispetto a quelli del mais. Adulti non sono mai stati raccolti in campo, mentre questo si è verificato in condizioni controllate. Le specie che meritano maggior attenzione sono i cereali Triticum spelta e Panicum miliaceum e l’infestante Sorghum halepense. Si potrebbe dunque ipotizzare che alcune specie vegetali possano fungere da ospite secondario quando non è presente il mais riducendo l’efficacia dell’avvicendamento.

Host race formation in Hyalesthes obsoletus (Signoret 1865)

Die Winden-Glasflügelzikade Hyalesthes obsoletus (Cixiidae, Glasflügelzikaden) nutzte in Deutschland ursprünglich die Ackerwinde Convolvulus arvensis als Wirtspflanze, allerdings nahm in den letzten zwei Dekaden die Abundanz auf der Großen Brennnessel Urtica dioica stark zu, zusammen mit der Inzidenz der Schwarzholzkrankheit Bois noir auf Weinreben. Bois noir wird durch ein Phytoplasma verursacht, das durch H. obsoletus von C. arvensis und U. dioica auf Weinreben übertragen wird. Es stellte sich daher die Frage, ob H. obsoletus Wirtsrassen entwickelt hat, die möglicherweise die Bois noir-Epidemiologie beeinflussen. In der vorliegenden Studie wurden folgende Fragestellungen bearbeitet: rn(1) Gibt es in Deutschland und Europa genetisch unterscheidbare Wirtsrassen von H. obsoletus auf den beiden Wirtspflanzen C. arvensis und U. dioica? Es wurden sieben Mikrosatellitenmarker entwickelt und etabliert, um H. obsoletus Populationen aus Deutschland und Europa genetisch zu analysieren. Es zeigte sich eine deutliche Differenzierung zwischen Populationen von beiden Wirtspflanzen in Deutschland, jedoch nicht in den historischen Ursprungsgebieten der deutschen Populationen, in der Schweiz, Italien oder Slovenien.rn(2) Wo sind die deutschen Wirtsrassen von H. obsoletus entstanden? Eine Einwanderung von südlichen, bereits an U. dioica angepassten Individuen stand einer lokalen Wirtsrassenevolution gegenüber. Die engere genetische Verwandtschaft der deutschen Population auf U. dioica zu denen auf C. arvensis, im Vergleich zu den übrigen Populationen auf U. dioica, impliziert einen lokalen Prozess im nördlichen Verbreitungsgebiet. Eine Immigration südlicher Tiere scheint nicht zur Diversifizierung beigetragen zu haben, führte aber möglicherweise einen U. dioica-spezifischen Phytoplasma-Stamm ein. Durch Wirtsrassenevolution entwickelten sich spezifische, vektorbasierte epidemiologische Kreisläufe der Schwarzholzkrankheit Bois noir. rn(3) Welche Präferenzen zeigen die beiden Wirtsrassen von H. obsoletus für die Wirtspflanzen C. arvensis und U. dioica und unterscheiden sich diese? Die Präferenz von H. obsoletus aus beiden deutschen Wirtsrassen in Bezug auf den Geruch der Wirtspflanzen wurde in einem Y-Olfaktometer untersucht, zusätzlich wurden beide Pflanzen direkt zur Wahl gestellt. Bei beiden Untersuchungen zeigte die Population von C. arvensis eine signifikante Präferenz für ihre native Wirtspflanze. Die Population von U. dioica wies dagegen keine Präferenz für den Geruch einer Wirtspflanze auf, bevorzugte im direkten Test jedoch signifikant ihre native Wirtspflanze. Dies weist darauf hin, dass die Anpassung an den „neuen“ Wirt noch nicht vollständig ist.rn

Longest available clinical outcomes after drug-eluting stent implantation for unprotected left main coronary artery disease: the DELFT (Drug Eluting stent for LeFT main) Registry

OBJECTIVES: The purpose of this study was to investigate the long-term safety and efficacy of percutaneous coronary intervention (PCI) with drug-eluting stent (DES) implantation for unprotected left main coronary artery (ULMCA) disease. BACKGROUND: Long-term clinical outcomes after DES implantation for ULMCA disease have not yet been ascertained. METHODS: From April 2002 to April 2004, 358 consecutive patients who underwent PCI with DES implantation for de novo lesions on ULMCA were retrospectively selected and analyzed in 7 European and U.S. tertiary care centers. No patients were excluded from the analysis, and all patients had a minimum follow-up of 3 years. RESULTS: Technical success rate was 100%. Procedural success rate was 89.6%. After 3 years, major adverse cardiovascular events (MACE)-free survival in the whole population was 73.5%. According to the Academic Research Consortium definitions, cardiac death occurred in 9.2% of patients, and reinfarction, target lesion revascularization (TLR), and target vessel revascularization (TVR) occurred in 8.6%, 5.8%, and 14.2% of patients, respectively. Definite stent thrombosis occurred in 2 patients (specifically at 0 and 439 days). In elective patients, the 3-year MACE-free survival was 74.2%, with mortality, reinfarction, TLR, and TVR rates of 6.2%, 8.3%, 6.6%, and 16%, respectively. In the emergent group the 3-year MACE-free survival was 68.2%, with mortality, reinfarction, TLR, and TVR rates of 21.4%, 10%, 2.8%, and 7.1%, respectively. CONCLUSIONS: Routine DES implantation in ULMCA disease seems encouraging, with favorable long-term clinical results.

Genetic diversity in tef [Eragrostis tef (Zucc.) Trotter]

Tef Eragrostis tef (Zucc.) Trotter is a cereal crop resilient to adverse climatic and soil conditions, and possessing desirable storage properties. Although tef provides high quality food and grows under marginal conditions unsuitable for other cereals, it is considered to be an orphan crop because it has benefited little from genetic improvement. Hence, unlike other cereals such as maize and wheat, the productivity of tef is extremely low. In spite of the low productivity, tef is widely cultivated by over six million small-scale farmers in Ethiopia where it is annually grown on more than three million hectares of land, accounting for over 30% of the total cereal acreage. Tef, a tetraploid with 40 chromosomes (2n=4x=40), belongs to the Family Poaceae and, together with finger millet (Eleusine coracana Gaertn), to the Subfamily Chloridoideae. It was believed to have originated in Ethiopia. There are about 350 Eragrostis species of which E. tef is the only species cultivated for human consumption. At the present time, the gene bank in Ethiopia holds over five thousand tef accessions collected from geographical regions diverse in terms of climate and elevation. These germplasm accessions appear to have huge variability with regard to key agronomic and nutritional traits. In order to properly utilize the variability in developing new tef cultivars, various techniques have been implemented to catalog the extent and unravel the patterns of genetic diversity. In this review, we show some recent initiatives investigating the diversity of tef using genomics, transcriptomics and proteomics and discuss the prospect of these efforts in providing molecular resources that can aid modern tef breeding.

Age of cleft monazites in the eastern Tauern Window: constraints on crystallization conditions of hydrothermal monazite

Monazite-bearing Alpine clefts located in the Sonnblick region of the eastern Tauern Window, Austria, are oriented perpendicular to the foliation and lineation. Ion probe (SIMS) Th–Pb and U���Pb dating of four cleft monazites yields crystallization ages of different growth domains and aggregate regions ranging from 18.99 ± 0.51 to 15.00 ± 0.51 Ma. The crystallization ages obtained are overlapping or slightly younger than zircon fission track ages but older than zircon (U���Th)/He cooling ages from the same area. This constrains cleft monazite crystallization in this area to *300–200 �C. LA-ICP-MS data of dated hydrothermal monazites indicate that in graphite-bearing, reduced host lithologies, cleft monazite is poor in As and has higher La/Yb values and U concentrations, whereas in oxidised host rocks opposite trends are observed. Monazites show negative Eu anomalies and variable La/Yb values ranging from 520 to 6050. The positive correlation between Ca and Sr concentration indicates dissolution of plagioclase or carbonates as the source of these elements. The data show that early exhumation and cleft formation in the Tauern is related to metamorphic dome formation caused by the collision of the Adriatic with the European plate and that monazite crystallization in the clefts occurred later. Our data also demonstrate that hydrothermal monazite ages offer great potential in helping to constrain the chronology of exhumation in collisional orogens.

The application of principal component analysis on human development indicators: Temporal approach from 1999 to 2010

Background and Objective. Ever since the human development index was published in 1990 by the United Nations Development Programme (UNDP), many researchers started searching and corporative studying for more effective methods to measure the human development. Published in 1999, Lai’s “Temporal analysis of human development indicators: principal component approach” provided a valuable statistical way on human developmental analysis. This study presented in the thesis is the extension of Lai’s 1999 research. ^ Methods. I used the weighted principal component method on the human development indicators to measure and analyze the progress of human development in about 180 countries around the world from the year 1999 to 2010. The association of the main principal component obtained from the study and the human development index reported by the UNDP was estimated by the Spearman’s rank correlation coefficient. The main principal component was then further applied to quantify the temporal changes of the human development of selected countries by the proposed Z-test. ^ Results. The weighted means of all three human development indicators, health, knowledge, and standard of living, were increased from 1999 to 2010. The weighted standard deviation for GDP per capita was also increased across years indicated the rising inequality of standard of living among countries. The ranking of low development countries by the main principal component (MPC) is very similar to that by the human development index (HDI). Considerable discrepancy between MPC and HDI ranking was found among high development countries with high GDP per capita shifted to higher ranks. The Spearman’s rank correlation coefficient between the main principal component and the human development index were all around 0.99. All the above results were very close to outcomes in Lai’s 1999 report. The Z test result on temporal analysis of main principal components from 1999 to 2010 on Qatar was statistically significant, but not on other selected countries, such as Brazil, Russia, India, China, and U.S.A.^ Conclusion. To synthesize the multi-dimensional measurement of human development into a single index, the weighted principal component method provides a good model by using the statistical tool on a comprehensive ranking and measurement. Since the weighted main principle component index is more objective because of using population of nations as weight, more effective when the analysis is across time and space, and more flexible when the countries reported to the system has been changed year after year. Thus, in conclusion, the index generated by using weighted main principle component has some advantage over the human development index created in UNDP reports.^

Sm-Nd isotopic investigation for rocks of Prince Charles Mountains, East Antarctica

The Prince Charles Mountains have been subject to extensive geological and geophysical investigations by former Soviet, Russian and Australian scientists from the early 1970s. In this paper we summarise, and review available geological and isotopic data, and report results of new isotopic studies (Sm-Nd, Pb-Pb, and U-Pb SHRIMP analyses); field geological data obtained during the PCMEGA 2002/2003 are utilised. The structure of the region is described in terms of four tectonic terranes. Those include Archaean Ruker, Palaeoproterozoic Lambert, Mesoproterozoic Fisher, and Meso- to Neoproterozoic Beaver Terranes. Pan-African activities (granite emplacement and probably tectonics) in the Lambert Terrane are reported. We present a summary of the composition of these terranes, discuss their origin and relationships. We also outline the most striking geological features, and problems, and try to draw attention to those rocks and regional geological features which are important in understanding the composition and evolution of the PCM and might suggest targets for further investigations.

Geochemistry of phosphatic crusts from the shelf off Peru

Authigenic phosphorite crusts from the shelf off Peru (9°40°S to 13°30°S) consist of a facies with phosphatic coated grains covered by younger phosphatic laminite. The crusts are composed of carbonate fluorapatite, which probably formed via an amorphous precursor close to the sediment water interface as indicated by low F/P2O5 ratios, Sr and Ca isotopes, as well as rare earth element patterns agreeing with seawater-dominated fluids. Small negative Ce anomalies and U enrichment in the laminite suggest suboxic conditions close to the sediment-water interface during its formation. Increased contents of chalcophilic elements and abundant sulfide minerals in the facies with phosphatic coated grains as well as in the laminite denote sulfate reduction and, consequently, point to episodical development of anoxic conditions during phosphogenesis. The Peruvian phosphorites formed episodically over an extended period of time lasting from Middle Miocene to Pleistocene. Individual phosphatic coated grains show a succession of phosphatic layers with varying contents of organic matter and sulfide-rich phosphatic layers. Coated grains supposedly formed as a result of episodic suspension caused by high turbulence and shifting redox conditions. Episodic anoxia in the pore water induced pyritization in the outermost carbonate fluorapatite layer. Phosphatic coated grains were later transported to the place of crust formation, where subsequent laminite formation was favored under lower energy conditions. A similar succession of phosphatic layers with varying contents of organic matter and sulfide-rich layers in the laminite suggests a formation mechanism analogous to that of individual coated grains.

Geochemistry of sediment cores of the Southern Ocean

We examine the possibility that glacial increase in the areal extent of reducing sediments might have changed the oceanic Cd inventory, thereby decoupling Cd from PO4. We suggest that the precipitation of Cd-sulfide in suboxic sediments is the single largest sink in the oceanic Cd budget and that the accumulation of authigenic Cd and U is tightly coupled to the organic carbon flux into the seafloor. Sediments from the Subantarctic Ocean and the Cape Basin (South Atlantic), where oxic conditions currently prevail, show high accumulation rates of authigenic Cd and U during glacial intervals associated with increased accumulation of organic carbon. These elemental enrichments attest to more reducing conditions in glacial sediments in response to an increased flux of organic carbon. A third core, overlain by Circumpolar Deep Water (CPDW) as are the other two cores but located south of the Antarctic Polar Front, shows an approximately inverse pattern to the Subantarctic record. The contrasting patterns to the north and south of the Antarctic Polar Front suggest that higher accumulation rates of Cd and U in Subantarctic sediments were driven primarily by increased productivity. This proposal is consistent with the hypothesis of glacial stage northward migration of the Antarctic Polar Front and its associated belt of high siliceous productivity. However, the increase in authigenic Cd and U glacial accumulation rates is higher than expected simply from a northward shift of the polar fronts, suggesting greater partitioning of organic carbon into the sediments during glacial intervals. Lower oxygen content of CPDW and higher organic carbon to biogenic silica rain rate ratio during glacial stages are possible causes. Higher glacial productivity in the Cape Basin record very likely reflects enhanced coastal up-welling in response to increased wind speeds. We suggest that higher productivity might have doubled the areal extent of suboxic sediments during the last glacial maximum. However, our calculations suggest low sensitivity of seawater Cd concentrations to glacial doubling of the extent of reducing sediments. The model suggests that during the last 250 kyr seawater Cd concentrations fluctuated only slightly, between high levels (about 0.66 nmol/kg) on glacial initiations and reaching lowest values (about 0.57 nmol/kg) during glacial maxima. The estimated 5% lower Cd content at the last glacial maximum relative to modern levels (0.60 nmol/kg) cannot explain the discordance between Cd and delta13C, such as observed in the Southern Ocean. This low sensitivity is consistent with foraminiferal data, suggesting minimal change in the glacial Cd mean oceanic content.