897 resultados para Quantitative stratigraphy


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This volume is a collection of the work done in a three years-lasting PhD, focused in the analysis of Central and Southern Adriatic marine sediments, deriving from the collection of a borehole and many cores, achieved thanks to the good seismic-stratigraphic knowledge of the study area. The work was made out within European projects EC-EURODELTA (coordinated by Fabio Trincardi, ISMAR-CNR), EC-EUROSTRATAFORM (coordinated by Phil P. E. Weaver, NOC, UK), and PROMESS1 (coordinated by Serge Bernè, IFREMER, France). The analysed sedimentary successions presented highly expanded stratigraphic intervals, particularly for the last 400 kyr, 60 kyr and 6 kyr BP. These three different time-intervals resulted in a tri-partition of the PhD thesis. The study consisted of the analysis of planktic and benthic foraminifers’ assemblages (more than 560 samples analysed), as well as in preparing the material for oxygen and carbon stable isotope analyses, and interpreting and discussing the obtained dataset. The chronologic framework of the last 400 kyr was achieved for borehole PRAD1-2 (within the work-package WP6 of PROMESS1 project), collected in 186.5 m water depth. The proposed chronology derives from a multi-disciplinary approach, consisting of the integration of numerous and independent proxies, some of which analysed by other specialists within the project. The final framework based on: micropaleontology (calcareous nannofossils and foraminifers’ bioevents), climatic cyclicity (foraminifers’ assemblages), geochemistry (oxygen stable isotope, made out on planktic and benthic records), paleomagnetism, radiometric ages (14C AMS), teprhochronology, identification of sapropel-equivalent levels (Se). It’s worth to note the good consistency between the oxygen stable isotope curve obtained for borehole PRAD1-2 and other deeper Mediterranean records. The studied proxies allowed the recognition of all the isotopic intervals from MIS10 to MIS1 in PRAD1-2 record, and the base of the borehole has been ascribed to the early MIS11. Glacial and interglacial intervals identified in the Central Adriatic record have been analysed in detail for the paleo-environmental reconstruction, as well. For instance, glacial stages MIS6, MIS8 and MIS10 present peculiar foraminifers’ assemblages, composed by benthic species typical of polar regions and no longer living in the Central Adriatic nowadays. Moreover, a deepening trend in the paleo-bathymetry during glacial intervals was observed, from MIS10 (inner-shelf environment) to MIS4 (mid-shelf environment).Ten sapropel-equivalent levels have been recognised in PRAD1-2 Central Adriatic record. They showed different planktic foraminifers’ assemblages, which allowed the first distinction of events occurred during warm-climate (Se5, Se7), cold-climate (Se4, Se6 and Se8) and temperate-intermediate-climate (Se1, Se3, Se9, Se’, Se10) conditions, consistently with literature. Cold-climate sapropel equivalents are characterised by the absence of an oligotrophic phase, whereas warm-temeprate-climate sapropel equivalents present both the oligotrophic and the eutrophic phases (except for Se1). Sea floor conditions vary, according to benthic foraminifers’ assemblages, from relatively well oxygenated (Se1, Se3), to dysoxic (Se9, Se’, Se10), to highly dysoxic (Se4, Se6, Se8) to events during which benthic foraminifers are absent (Se5, Se7). These two latter levels are also characterised by the lamination of the sediment, feature never observed in literature in such shallow records. The enhanced stratification of the water column during the events Se8, Se7, Se6, Se5, Se4, and the concurring strong dilution of shallow water, pointed out by the isotope record, lead to the hypothesis of a period of intense precipitation in the Central Adriatic region, possibly due to a northward shift of the African Monsoon. Finally, the expression of Central Adriatic PRAD1-2 Se5 equivalent was compared with the same event, as registered in other Eastern Mediterranean areas. The sequence of substantially the same planktic foraminifers’ bioevents has been consistently recognised, indicating a similar evolution of the water column all over the Eastern Mediterranean; yet, the synchronism of these events cannot be demonstrated. A high resolution analysis of late Holocene (last 6000 years BP) climate change was carried out for the Adriatic area, through the recognition of planktic and benthic foraminifers’ bioevents. In particular, peaks of planktic Globigerinoides sacculifer (four during the last 5500 years BP in the most expanded core) have been interpreted, based on the ecological requirements of this species, as warm-climate, arid intervals, correspondent to periods of relative climatic optimum, such as, for instance, the Medieval Warm Period, the Roman Age, the Late Bronze Age and the Copper Age. Consequently, the minima in the abundance of this biomarker could correspond to relatively cooler and more rainy periods. These conclusions are in good agreement with the isotopic and the pollen data. The Last Occurrence (LO) of G. sacculifer has been dated in this work at an average age of 550 years BP, and it is the best bioevent approximating the base of the Little Ice Age in the Adriatic. Recent literature reports the same bioevent in the Levantine Basin, showing a rather consistent age. Therefore, the LO of G. sacculifer has the potential to be extended to all the Eastern Mediterranean. Within the Little Ice Age, benthic foraminifer V. complanata shows two distinct peaks in the shallower Adriatic cores analysed, collected hundred kilometres apart, inside the mud belt environment. Based on the ecological requirements of this species, these two peaks have been interpreted as the more intense (cold and rainy) oscillations inside the LIA. The chronologic framework of the analysed cores is robust, being based on several range-finding 14C AMS ages, on estimates of the secular variation of the magnetic field, on geochemical estimates of the activity depth of 210Pb short-lived radionuclide (for the core-top ages), and is in good agreement with tephrochronologic, pollen and foraminiferal data. The intra-holocenic climate oscillations find out in the Adriatic have been compared with those pointed out in literature from other records of the Northern Hemisphere, and the chronologic constraint seems quite good. Finally, the sedimentary successions analysed allowed the review and the update of the foraminifers’ ecobiostratigraphy available from literature for the Adriatic region, thanks to the achievement of 16 ecobiozones for the last 60 kyr BP. Some bioevents are restricted to the Central Adriatic (for instance the LO of benthic Hyalinea balthica , approximating the MIS3/MIS2 boundary), others occur all over the Adriatic basin (for instance the LO of planktic Globorotalia inflata during MIS3, individuating Dansgaard-Oeschger cycle 8 (Denekamp)).

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The increasing aversion to technological risks of the society requires the development of inherently safer and environmentally friendlier processes, besides assuring the economic competitiveness of the industrial activities. The different forms of impact (e.g. environmental, economic and societal) are frequently characterized by conflicting reduction strategies and must be holistically taken into account in order to identify the optimal solutions in process design. Though the literature reports an extensive discussion of strategies and specific principles, quantitative assessment tools are required to identify the marginal improvements in alternative design options, to allow the trade-off among contradictory aspects and to prevent the “risk shift”. In the present work a set of integrated quantitative tools for design assessment (i.e. design support system) was developed. The tools were specifically dedicated to the implementation of sustainability and inherent safety in process and plant design activities, with respect to chemical and industrial processes in which substances dangerous for humans and environment are used or stored. The tools were mainly devoted to the application in the stages of “conceptual” and “basic design”, when the project is still open to changes (due to the large number of degrees of freedom) which may comprise of strategies to improve sustainability and inherent safety. The set of developed tools includes different phases of the design activities, all through the lifecycle of a project (inventories, process flow diagrams, preliminary plant lay-out plans). The development of such tools gives a substantial contribution to fill the present gap in the availability of sound supports for implementing safety and sustainability in early phases of process design. The proposed decision support system was based on the development of a set of leading key performance indicators (KPIs), which ensure the assessment of economic, societal and environmental impacts of a process (i.e. sustainability profile). The KPIs were based on impact models (also complex), but are easy and swift in the practical application. Their full evaluation is possible also starting from the limited data available during early process design. Innovative reference criteria were developed to compare and aggregate the KPIs on the basis of the actual sitespecific impact burden and the sustainability policy. Particular attention was devoted to the development of reliable criteria and tools for the assessment of inherent safety in different stages of the project lifecycle. The assessment follows an innovative approach in the analysis of inherent safety, based on both the calculation of the expected consequences of potential accidents and the evaluation of the hazards related to equipment. The methodology overrides several problems present in the previous methods proposed for quantitative inherent safety assessment (use of arbitrary indexes, subjective judgement, build-in assumptions, etc.). A specific procedure was defined for the assessment of the hazards related to the formations of undesired substances in chemical systems undergoing “out of control” conditions. In the assessment of layout plans, “ad hoc” tools were developed to account for the hazard of domino escalations and the safety economics. The effectiveness and value of the tools were demonstrated by the application to a large number of case studies concerning different kinds of design activities (choice of materials, design of the process, of the plant, of the layout) and different types of processes/plants (chemical industry, storage facilities, waste disposal). An experimental survey (analysis of the thermal stability of isomers of nitrobenzaldehyde) provided the input data necessary to demonstrate the method for inherent safety assessment of materials.

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

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La conoscenza delle esigenze luminose (intensità, spettro, durata minima, massima ed ottimale del fotoperiodo di illuminazione) e della tolleranza alle condizioni degli interni delle piante ad uso decorativo, è di fondamentale importanza per una giusta tecnica di progettazione (dimensionamento e dislocazione dei punti luce) dell’indoor plantscaping. Il lungo periodo di condizionamento al quale queste piante vengono sottoposte, caratterizzato principalmente dalla scarsa disponibilità di luce naturale e dagli alti livelli di concentrazione di CO2 determina una forte influenza sui processi morfo-fisiologici. Il presente studio analizza il fattore luminoso ed è articolato su più punti quali; • caratterizzazione della riposta fotosintetica all’intensità luminosa di 21 delle principali specie a fogliame decorativo comunemente utilizzate nella realizzazione degli spazi verdi indoor, per stabilire quali siano i minimi ed ottimali livelli di PAR tali da garantire una fotosintesi netta positiva e nel complesso le condizioni di maggior benessere per le piante; • quantificazione dell’incremento fotosintetico netto dovuto ad una maggior concentrazione di CO2 negli interni rispetto alla concentrazione CO2 atmosferica esterna, all’aumentare dell’ intensità luminosa artificiale sulle precedenti specie; • monitoraggio dell’andamento delle attività fotosintetiche durante il periodo di illuminazione di 8 ore comunemente utilizzato in un interno ad uso lavorativo, a PAR costante e variabile in Ficus elastica e Dieffenbachia picta, al fine di stabilire quali possano essere le durate e le modalità di somministrazione della luce per rendere massima la fotosintesi netta riducendo al minimo i consumi energetici dovuti all’accensione delle lampade; • valutazione della risposta morfo-fisiologica e fotosintetica a modificazioni dello spettro luminoso mediante l’uso di LED monocromatici colorati ad emissione nel bianco, blu e rosso in Ficus benjamina e Iresine herbistii al fine di stabilire se questo tipo di lampade possano essere utilizzate come fonte integrativa e/o sostitutiva nella realizzazione degli spazi verdi interni. Vengono analizzati il punto si compensazione alla luce (g), il punto di saturazione alla luce (s), l’efficienza quantica (AQE), il punto di respirazione al buio (Rd) e la fotosintesi netta massima (A max) per (Aglaonema commutatum, Asplenium nidus, Anthurium andreanum, Begonia rex, Calathea luoise, Calathea veitchiana, Calathea rufibarba, Calathea zebrina, Codiaeum variegatum, Cthenanthe oppenheimiana, Dieffenbakia picta, Ficus benjamina, Ficus elatica, Ficus longifolia, Fittonia verschaffeltii, Iresine herbistii, Philodendron erubescens, Philodendron pertusum, Potos aureus, Spathiphillum wallisi, Syngonium podophillum ) e classificate le specie in funzione di Amax in quattro categorie; A max < 2 µmol CO2 m-2 s-1, A max compresa tra 2 e 4 µmol CO2 m-2 s-1, Amax cpmpresa tra 4 e 6 µmol CO2 m-2 s-1, Amax > 6 µmol CO2 m-2 s-1, al fine di mettere in risalto la potenzialità fotosintetiche di ogni singola specie. I valori di PAR compresi tra (g) ed (s) forniscono le indicazioni sulle quali basarsi per scegliere una giusta lampada o dimensionare un punto luce per ogni singola specie e/o composizione. È stimata l’influenza di due livelli di concentrazione di CO2 ambientale (400 e 800 ppm) all’incrementare dell’intensità luminosa sul processo fotosintetico delle specie precedenti. Per quasi tutte le specie 800 ppm di CO2 non favoriscono nessun incremento all’attività fotosintetica ad eccezione di Ficus benjamina, Ficus elatica e Syngonium podophillum se non accompagnati da una disponibilità luminosa superiore alle 10 µmol m-2 s-1. Viene monitorato l’andamento dell’attività fotosintetica a PAR costante e variabile (intervallando periodi di 8 minuti a PAR 40 e 80) durante 8 ore di illuminazione su Ficus elastica e Dieffenbachia picta al fine di stabilire la miglior modalità di somministrazione della luce. La fotosintesi netta cumulativa per l’intera durata di illuminazione a PAR costante mostra un calo dopo alcune ore dall’attivazione in Dieffenbackia, e un andamento oscillatorio in Ficus. L’illuminazione alternata consente di raggiungere i quantitativi di CO2 organicata a 80 µmol m-2 s-1 di PAR, dopo 5 ore e mezza sia in Ficus che Dieffenbackia sebbene le potenzialità fotosintetiche delle due piante siano molto differenti. È stato valutato l’effetto dell’illuminazione artificiale mediante LED (15W) a luce bianca, blu e rossa monocromatica in rapporto alla luce neon(36W) bianca tradizionale (con differenti abbinamenti tra le lampade) sui principali parametri morfologici e fisiologici, in Ficus benjamin ‘Variegata’ e Iresine herbistii per verificare se tali fonti possono rappresentare una valida alternativa nella sostituzione o integrazione di altre lampade per gli spazi verdi indoor. Tutte le combinazioni LED indagate possono rappresentare un’alternativa di sostituzione alla coltivazione con neon ed un risparmio energetico di oltre il 50%. Una PAR di 20,6 µmol m-2 s-1 della singola lampada LED bianco è sufficiente per mantenere la pianta in condizioni di sopravvivenza con un consumo di 15W a fronte dei 36W necessari per il funzionamento di ogni neon. La combinazione LED bianco + LED blu monocromatico favorisce il contenimento della taglia della pianta, caratteristica gradita nella fase di utilizzo indoor, una maggior produzione di sostanza secca e un’attività fotosintetica più elevata.

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Die murine embryonale Karzinomazellinie PCC7-Mz1 stellt ein Modell neuronaler Entwicklung dar, da nach RA-Gabe eine Differenzierung in neuronale, gliale und fibroblastoide Phänotypen erfolgt. Um die Expression von Neurotransmitterrezeptoren während der neuronalen Entwicklung zu untersuchen, wurde in dieser Arbeit eine quantitative Analyse der Expression verschiedener Neurotransmitterrezeptoren im Verlauf der RA-induzierten Differenzierung der PCC7-Mz1 Zellen durchgeführt. Zu diesem Zweck wurde eine kompetitive RT-PCR eingesetzt. Als Kompetitor wurde ein synthetisches Gen ( SG) konstruiert, das sich aus den Antisense- und Sense-Primersequenzen zur spezifischen Amplifikation des Dopaminrezeptors D2, des Serotoninrezeptors 5HT3, der GABAA-Untereinheiten ß1 und ß3, der metabotropen Glutamatrezeptoren mGluR1 und mGluR5, der 5 NMDA-Rezeptoruntereinheiten 1,2a,2b,2c und 2d, der Markerproteine Synaptophysin und GFAP, und der Untereinheiten a3, a4 und a7 des nikotinischen Acetylcholinrezeptors zusammensetzt. Mit diesem SG erfolgten die Quantifizierungen der Rezeptor-mRNA im Sättigungsbereich der PCR. Die erhaltenen Transkriptmengen wurden auf ein Neuron bezogen, wodurch eine Korrelation zur neuronalen Entwicklung erfolgen konnte.

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Beim Beobachten von nächtlichen Insektenschwärmen an Straßenbeleuchtungen kommt es zur Frage, inwieweit von einer Bedrohung eines geordneten Naturkreislaufes durch dieses Phänomen gesprochen werden kann. Am Beispiel der bedrohten Artenvielfalt aquatischer Insekten im Bereich anthropogen bedingt verschmutzter Fließgewässer wurde die Problematik umfassend untersucht. Die Freilandtests erstreckten sich von Sommer 1998 bis Sommer 2000. Die vorliegende Arbeit geht mehreren Fragestellungen nach:1. - Wie hoch ist der Anteil aquatischer Insekten, der von dem Ort seiner Emergenz aus von einer naheliegenden Straßenlaterne angezogen wird ?2. - Welcher Lampentyp lockt weniger Insekten an: OSRAM HQL (Weiß-Mischlicht) oder PHILIPPS SON (gelbes Licht) ?3. - Welche Wellenlängenbereiche des Lichts sind beim Anflug an die Lampe von besonderer Präferenz ? zu 1. - Aquatische Insekten wiesen kein einheitliches Verhalten im Anflug an künstliches Licht auf. In den Sommermonaten kam es bei einigen Insektengruppen, wie z.B. den Trichopteren, zu einem massenhaften Anflug an die eine, im Untersuchungsgebiet aufgestellte Straßenlaterne. In dieser Zeit ergaben sich im Mittelwert Fangzahlen in einer Nacht am Licht, die der Emergenz von 25 Metern Bachufer/72 Stunden entsprachen. Bei den Dipteren ergab der mittlere Wert eine Emergenz von knapp 10 Metern Uferlänge/72 Stunden. Aufgrund hoher Fangzahlen konnten folgende Ergebnisse auf Artniveau bei den Chironomiden erzielt werden. Bei den zehn häufigsten Arten aus Emergenz und Lichtfang zeigten sich starke Schwankungen: Der Fang am Licht entsprach im Maximum einer Schlupfrate von 61 Metern Ufer/ 72 Stunden bei einer Art, bei einer anderen Art wurde z.B. ein Lichtfang erzielt, der lediglich die Emergenz von 0,3 Metern/72 Stunden umfaßte.zu 2. - In dem ohne Lichtkonkurrenz stattfindenden Vergleich zwischen PHILIPPS SON 70W und OSRAM HQL 125W ergab sich eine Fangrelation von 1:1,6 (SON:HQL). Bei einem Parallelfang (30 Metern Abstand der Leuchten) mit SON/HQL flogen wesentlich mehr Tiere an die HQL: Hier betrug die Relation 1:3,97 (SON:HQL). Es fand somit bei Lichtkonkurrenz eine Abwanderung der Insekten zur 'attraktiveren' Lampe statt.zu 3. - Zuletzt wurde die Anlockwirkung dreier Farbspektren mit den Intensitätsmaxima einer Wellenlänge von 437nm, 579nm und 599nm getestet. 437nm war die in der HQL gemessene Intensitätsspitze im niedrigwelligen Bereich und nach verbreiteter Auffassung von besonderer Anlockwirkung. Der Wellenlängenbereich um 579nm stellte das Intensitätsmaximum der SON-Lampe dar (gelbes Licht); 599nm war als Alternative für anlockschwache Beleuchtungen ausgewählt worden. Hier ergab sich bei abwechselndem Fang (ohne Lichtkonkurrenz) eine Fangrelation von 1,8 : 3,4 : 1 (437nm : 579nm : 599nm).

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Food technologies today mean reducing agricultural food waste, improvement of food security, enhancement of food sensory properties, enlargement of food market and food economies. Food technologists must be high-skilled technicians with good scientific knowledge of food hygiene, food chemistry, industrial technologies and food engineering, sensory evaluation experience and analytical chemistry. Their role is to apply the modern vision of science in the field of human nutrition, rising up knowledge in food science. The present PhD project starts with the aim of studying and improving frozen fruits quality. Freezing process in very powerful in preserve initial raw material characteristics, but pre-treatment before the freezing process are necessary to improve quality, in particular to improve texture and enzymatic activity of frozen foods. Osmotic Dehydration (OD) and Vacuum Impregnation (VI), are useful techniques to modify fruits and vegetables composition and prepare them to freezing process. These techniques permit to introduce cryo-protective agent into the food matrices, without significant changes of the original structure, but cause a slight leaching of important intrinsic compounds. Phenolic and polyphenolic compounds for example in apples and nectarines treated with hypertonic solutions are slightly decreased, but the effect of concentration due to water removal driven out from the osmotic gradient, cause a final content of phenolic compounds similar to that of the raw material. In many experiment, a very important change in fruit composition regard the aroma profile. This occur in strawberries osmo-dehydrated under vacuum condition or under atmospheric pressure condition. The increment of some volatiles, probably due to fermentative metabolism induced by the osmotic stress of hypertonic treatment, induce a sensory profile modification of frozen fruits, that in some way result in a better acceptability of consumer, that prefer treated frozen fruits to untreated frozen fruits. Among different processes used, a very interesting result was obtained with the application of a osmotic pre-treatment driven out at refrigerated temperature for long time. The final quality of frozen strawberries was very high and a peculiar increment of phenolic profile was detected. This interesting phenomenon was probably due to induction of phenolic biological synthesis (for example as reaction to osmotic stress), or to hydrolysis of polymeric phenolic compounds. Aside this investigation in the cryo-stabilization and dehydrofreezing of fruits, deeper investigation in VI techniques were carried out, as studies of changes in vacuum impregnated prickly pear texture, and in use of VI and ultrasound (US) in aroma enrichment of fruit pieces. Moreover, to develop sensory evaluation tools and analytical chemistry determination (of volatiles and phenolic compounds), some researches were bring off and published in these fields. Specifically dealing with off-flavour development during storage of boiled potato, and capillary zonal electrophoresis (CZE) and high performance liquid chromatography (HPLC) determination of phenolic compounds.

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The Northern Apennines (NA) chain is the expression of the active plate margin between Europe and Adria. Given the low convergence rates and the moderate seismic activity, ambiguities still occur in defining a seismotectonic framework and many different scenarios have been proposed for the mountain front evolution. Differently from older models that indicate the mountain front as an active thrust at the surface, a recently proposed scenario describes the latter as the frontal limb of a long-wavelength fold (> 150 km) formed by a thrust fault tipped around 17 km at depth, and considered as the active subduction boundary. East of Bologna, this frontal limb is remarkably very straight and its surface is riddled with small, but pervasive high- angle normal faults. However, west of Bologna, some recesses are visible along strike of the mountain front: these perturbations seem due to the presence of shorter wavelength (15 to 25 km along strike) structures showing both NE and NW-vergence. The Pleistocene activity of these structures was already suggested, but not quantitative reconstructions are available in literature. This research investigates the tectonic geomorphology of the NA mountain front with the specific aim to quantify active deformations and infer possible deep causes of both short- and long-wavelength structures. This study documents the presence of a network of active extensional faults, in the foothills south and east of Bologna. For these structures, the strain rate has been measured to find a constant throw-to-length relationship and the slip rates have been compared with measured rates of erosion. Fluvial geomorphology and quantitative analysis of the topography document in detail the active tectonics of two growing domal structures (Castelvetro - Vignola foothills and the Ghiardo plateau) embedded in the mountain front west of Bologna. Here, tilting and river incision rates (interpreted as that long-term uplift rates) have been measured respectively at the mountain front and in the Enza and Panaro valleys, using a well defined stratigraphy of Pleistocene to Holocene river terraces and alluvial fan deposits as growth strata, and seismic reflection profiles relationships. The geometry and uplift rates of the anticlines constrain a simple trishear fault propagation folding model that inverts for blind thrust ramp depth, dip, and slip. Topographic swath profiles and the steepness index of river longitudinal profiles that traverse the anti- clines are consistent with stratigraphy, structures, aquifer geometry, and seismic reflection profiles. Available focal mechanisms of earthquakes with magnitude between Mw 4.1 to 5.4, obtained from a dataset of the instrumental seismicity for the last 30 years, evidence a clear vertical separation at around 15 km between shallow extensional and deeper compressional hypocenters along the mountain front and adjacent foothills. In summary, the studied anticlines appear to grow at rates slower than the growing rate of the longer- wavelength structure that defines the mountain front of the NA. The domal structures show evidences of NW-verging deformation and reactivations of older (late Neogene) thrusts. The reconstructed river incision rates together with rates coming from several other rivers along a 250 km wide stretch of the NA mountain front and recently available in the literature, all indicate a general increase from Middle to Late Pleistocene. This suggests focusing of deformation along a deep structure, as confirmed by the deep compressional seismicity. The maximum rate is however not constant along the mountain front, but varies from 0.2 mm/yr in the west to more than 2.2 mm/yr in the eastern sector, suggesting a similar (eastward-increasing) trend of the apenninic subduction.

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The present work provides an ex-post assessment of the UK 5-a-day information campaign where the positive effects of information on consumption levels are disentangled from the potentially conflicting price dynamics. A model-based estimate of the counterfactual (no-intervention) scenario is computed using data from the Expenditure and Food Survey between 2002 and 2006. For this purpose fruit and vegetable demand is modelled employing Quadratic Almost Ideal Demand System (QUAIDS) specification with demographic effects and controlling for potential endogeneity of prices and total food expenditure.

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In a previous study on maize (Zea mays, L.) several quantitative trait loci (QTL) showing high dominance-additive ratio for agronomic traits were identified in a population of recombinant inbred lines derived from B73 × H99. For four of these mapped QTL, namely 3.05, 4.10, 7.03 and 10.03 according to their chromosome and bin position, families of near-isogenic lines (NILs) were developed, i.e., couples of homozygous lines nearly identical except for the QTL region that is homozygote either for the allele provided by B73 or by H99. For two of these QTL (3.05 and 4.10) the NILs families were produced in two different genetic backgrounds. The present research was conducted in order to: (i) characterize these QTL by estimating additive and dominance effects; (ii) investigate if these effects can be affected by genetic background, inbreeding level and environmental growing conditions (low vs. high plant density). The six NILs’ families were tested across three years and in three Experiments at different inbreeding levels as NILs per se and their reciprocal crosses (Experiment 1), NILs crossed to related inbreds B73 and H99 (Experiment 2) and NILs crossed to four unrelated inbreds (Experiment 3). Experiment 2 was conducted at two plant densities (4.5 and 9.0 plants m-2). Results of Experiments 1 and 2 confirmed previous findings as to QTL effects, with dominance-additive ratio superior to 1 for several traits, especially for grain yield per plant and its component traits; as a tendency, dominance effects were more pronounced in Experiment 1. The QTL effects were also confirmed in Experiment 3. The interactions involving QTL effects, families and plant density were generally negligible, suggesting a certain stability of the QTL. Results emphasize the importance of dominance effects for these QTL, suggesting that they might deserve further studies, using NILs’ families and their crosses as base materials.