La costruzione della città medievale. Archeologia dell'edilizia storica e topografia urbana a Pistoia.

Pistoia rientra a buon diritto, nel quadro della Toscana medievale, in quella rete di centri urbani di antica origine e tradizione diocesana che riuscirono a costruire, nella dialettica fra città e territorio, un organismo politico autonomo, il comune cittadino. La ricerca prende in considerazione i resti materiali delle strutture conservate nel tessuto urbano attuale, in particolare l'edilizia civile, prediligendo la cosiddetta “edilizia minore”, ovvero gli edifici residenziali non monumentali che, proprio per questo motivo, sono generalmente poco conosciuti. Le strutture, censite ed inserite in una piattaforma GIS (Arpenteur), sono analizzate con metodo archeologico al fine di distinguere le diverse fasi costruttive, medievali e post-medievali, con cui sono giunte fino ad oggi. L'analisi stratigrafica, effettuata su rilievi realizzati mediante modellazione 3D (Photomodeler), ha permesso di costruire un primo “atlante” delle tipologie murarie medievali della città: i tipi murari assumono quindi la funzione di indicatori cronologici degli edifici analizzati. I dati stratigrafici, uniti al dato topologico dei complessi architettonici (localizzati prevalentemente nel centro storico, all'interno del circuito murario della metà del XII secolo), hanno fornito informazioni sia per quanto riguarda l'aspetto materiale degli edifici di abitazione (forma, dimensioni, materiali) sia per quanto riguarda temi di topografia storica (viabilità maggiore e minore, formazione dei borghi, orizzonte sociale degli abitanti, distribuzione della proprietà), nel periodo della “parabola” della Pistoia comunale (XII-XIII secolo). In conclusione, la ricerca vuole essere sia uno strumento di analisi per la storia delle trasformazioni delle città nel periodo comunale, sia uno strumento di conoscenza e tutela di un patrimonio storico-archeologico che, per la sua natura non-monumentale spesso sfugge all'attenzione di amministratori ed urbanisti.

Nuovi dati sulla sinagoga di bova marina nel contesto dell'archeologia ebraica della calabria tardo antica

L’obiettivo del lavoro di ricerca consiste nell’analisi dei dati archeologici della sinagoga di Bova marina (RC). Dopo una veloce descrizione della presenza ebraica in Italia, attraverso i reperti archeologici, si è passati ad analizzare i dati degli scavi degli anni ’80 del Novecento e successivamente si è proceduto a delle nuove analisi stratigrafiche per definire la cronologia della sinagoga e dell’intero sito di S. Pasquale. Nella tesi sono riportati i nuovi dati inerenti il rilievo della sinagoga, le nuove ipotesi interpretative delle due aree sepolcrali e la lettura di un nuovo edificio collegabile alla stessa fase di vita della sinagoga.

The stratigraphic record of the quaternary sea level fluctuations and the impact of the post-glacial sea level rise (Termination I) in the Adriatic basin (Mediterranean sea)

The modern stratigraphy of clastic continental margins is the result of the interaction between several geological processes acting on different time scales, among which sea level oscillations, sediment supply fluctuations and local tectonics are the main mechanisms. During the past three years my PhD was focused on understanding the impact of each of these process in the deposition of the central and northern Adriatic sedimentary successions, with the aim of reconstructing and quantifying the Late Quaternary eustatic fluctuations. In the last few decades, several Authors tried to quantify past eustatic fluctuations through the analysis of direct sea level indicators, among which drowned barrier-island deposits or coral reefs, or indirect methods, such as Oxygen isotope ratios (δ18O) or modeling simulations. Sea level curves, obtained from direct sea level indicators, record a composite signal, formed by the contribution of the global eustatic change and regional factors, as tectonic processes or glacial-isostatic rebound effects: the eustatic signal has to be obtained by removing the contribution of these other mechanisms. To obtain the most realistic sea level reconstructions it is important to quantify the tectonic regime of the central Adriatic margin. This result has been achieved integrating a numerical approach with the analysis of high-resolution seismic profiles. In detail, the subsidence trend obtained from the geohistory analysis and the backstripping of the borehole PRAD1.2 (the borehole PRAD1.2 is a 71 m continuous borehole drilled in -185 m of water depth, south of the Mid Adriatic Deep - MAD - during the European Project PROMESS 1, Profile Across Mediterranean Sedimentary Systems, Part 1), has been confirmed by the analysis of lowstand paleoshorelines and by benthic foraminifera associations investigated through the borehole. This work showed an evolution from inner-shelf environment, during Marine Isotopic Stage (MIS) 10, to upper-slope conditions, during MIS 2. Once the tectonic regime of the central Adriatic margin has been constrained, it is possible to investigate the impact of sea level and sediment supply fluctuations on the deposition of the Late Pleistocene-Holocene transgressive deposits. The Adriatic transgressive record (TST - Transgressive Systems Tract) is formed by three correlative sedimentary bodies, deposited in less then 14 kyr since the Last Glacial Maximum (LGM); in particular: along the central Adriatic shelf and in the adjacent slope basin the TST is formed by marine units, while along the northern Adriatic shelf the TST is represented by costal deposits in a backstepping configuration. The central Adriatic margin, characterized by a thick transgressive sedimentary succession, is the ideal site to investigate the impact of late Pleistocene climatic and eustatic fluctuations, among which Meltwater Pulses 1A and 1B and the Younger Dryas cold event. The central Adriatic TST is formed by a tripartite deposit bounded by two regional unconformities. In particular, the middle TST unit includes two prograding wedges, deposited in the interval between the two Meltwater Pulse events, as highlighted by several 14C age estimates, and likely recorded the Younger Dryas cold interval. Modeling simulations, obtained with the two coupled models HydroTrend 3.0 and 2D-Sedflux 1.0C (developed by the Community Surface Dynamics Modeling System - CSDMS), integrated by the analysis of high resolution seismic profiles and core samples, indicate that: 1 - the prograding middle TST unit, deposited during the Younger Dryas, was formed as a consequence of an increase in sediment flux, likely connected to a decline in vegetation cover in the catchment area due to the establishment of sub glacial arid conditions; 2 - the two-stage prograding geometry was the consequence of a sea level still-stand (or possibly a fall) during the Younger Dryas event. The northern Adriatic margin, characterized by a broad and gentle shelf (350 km wide with a low angle plunge of 0.02° to the SE), is the ideal site to quantify the timing of each steps of the post LGM sea level rise. The modern shelf is characterized by sandy deposits of barrier-island systems in a backstepping configuration, showing younger ages at progressively shallower depths, which recorded the step-wise nature of the last sea level rise. The age-depth model, obtained by dated samples of basal peat layers, is in good agreement with previous published sea level curves, and highlights the post-glacial eustatic trend. The interval corresponding to the Younger Dyas cold reversal, instead, is more complex: two coeval coastal deposits characterize the northern Adriatic shelf at very different water depths. Several explanations and different models can be attempted to explain this conundrum, but the problem remains still unsolved.

Statistical analysis of the error associated with the simplification of the stratigraphy in geotechnical models

The uncertainties in the determination of the stratigraphic profile of natural soils is one of the main problems in geotechnics, in particular for landslide characterization and modeling. The study deals with a new approach in geotechnical modeling which relays on a stochastic generation of different soil layers distributions, following a boolean logic – the method has been thus called BoSG (Boolean Stochastic Generation). In this way, it is possible to randomize the presence of a specific material interdigitated in a uniform matrix. In the building of a geotechnical model it is generally common to discard some stratigraphic data in order to simplify the model itself, assuming that the significance of the results of the modeling procedure would not be affected. With the proposed technique it is possible to quantify the error associated with this simplification. Moreover, it could be used to determine the most significant zones where eventual further investigations and surveys would be more effective to build the geotechnical model of the slope. The commercial software FLAC was used for the 2D and 3D geotechnical model. The distribution of the materials was randomized through a specifically coded MatLab program that automatically generates text files, each of them representing a specific soil configuration. Besides, a routine was designed to automate the computation of FLAC with the different data files in order to maximize the sample number. The methodology is applied with reference to a simplified slope in 2D, a simplified slope in 3D and an actual landslide, namely the Mortisa mudslide (Cortina d’Ampezzo, BL, Italy). However, it could be extended to numerous different cases, especially for hydrogeological analysis and landslide stability assessment, in different geological and geomorphological contexts.