Reciproche influenze tra geomorfologia e popolamento antico presso le piane di foce dei fiumi tirrenici. Il caso del Fiume Garigliano

La Piana di foce del Garigliano (al confine tra Lazio e Campania) è caratterizzata, fino ad epoche recenti, dalla presenza di aree palustri e umide. Lo studio in corso cerca di ricostruire l’evoluzione dell’ambiente costiero mettendolo in relazione alla presenza dell’uomo, alla gestione del territorio, alle vicende storiche e alle variazioni climatiche utilizzando molteplici metodologie tipiche della geoarcheologia. Si tratta di un approccio multidisciplinare che cerca di mettere insieme analisi tipiche dell’archeologia, della topografia antica, della geomorfologia, della geologia e della paleobotanica. Fino all’età del Ferro l’unica traccia di popolamento viene da Monte d’Argento, uno sperone roccioso isolato lungo la costa, posto al limite occidentale di un ambiente sottostante che sembra una palude chiusa e isolata da apporti sedimentari esterni. Con il passaggio all’età del ferro si verifica un mutamento ambientale con la fine della grande palude e la formazione di una piccola laguna parzialmente comunicante con il mare. L’arrivo dei romani alla fine del III secolo a.C. segna la scomparsa dei grandi centri degli Aurunci e la deduzione di tre colonie (Sessa Aurunca, Sinuessa, Minturno). Le attività di sistemazione territoriale non riguardarono però le aree umide costiere, che non vennero bonificate o utilizzate per scopi agricoli, ma mantennero la loro natura di piccoli laghi costieri. Quest’epoca è dunque caratterizzata da una diffusione capillare di insediamenti, basati su piccole fattorie o installazioni legate allo sfruttamento agricolo. Poche sono le aree archeologiche che hanno restituito materiali successivi al II-III secolo d.C. La città resta comunque abitata fino al VI-VII secolo, quando l’instabilità politica e l’impaludamento dovettero rendere la zona non troppo sicura favorendo uno spostamento verso le zone collinari. Un insediamento medievale è attestato solo a Monte d’Argento e una frequentazione saracena dell’inizio del IX secolo è riportata dalle fonti letterarie, ma non vi è ancora nessuna documentazione archeologica.

The Architecture of the Persian Period in the Levant

The earliest scholars were not concerned about preparing extensive investigations linking the Persian-period building remains excavated in the entire Levant together. Moreover, the research interests of scholars caused some impediments to the study of this period viz in the last decades; the Achaemenid period has been neglected by the scholars who -in turn- focused on the earlier and later periods for religious reasons. Too, while some regions have been studied abundantly, but it was not the case in other areas, which makes our knowledge is incomplete. From the explanation side, some scholars try to interpret the architectural remains from an ethnic perspective or unsubstantiated personal fancies, so their arguments were utterly lacking any objectivity. This thesis explores what are the Persian architectural and ornamental impacts on the Levantine architecture and the relations between Persian-period sites in Syria-Palestine region. Too, the architectural remains and their contents benefited us to clarify the settlement patterns in the regions being discussed. The author analyzed the ground plans of the buildings and their architectural features and ornamental motifs by conducting a descriptive, analytical, and interpretative study. He also conducted comparisons with similar buildings outside the Levant, especially in Fars to obtain a more comprehensive and systematic study, and then extracting any direct or indirect Persian influences. This has given us a better understanding of the nature of the social, political, and religious life in the entire Levant and the knowledge gap has been bridged to a satisfying extent. This study has demonstrated a few of the Achaemenid impacts, especially on the northern coastline of the Levant.

Essays in Long-run Development and Spatial Economics

This thesis tries to further our understanding for why some countries today are more prosperous than others. It establishes that part of today's observed variation in several proxies such as income or gender inequality have been determined in the distant past. Chapter one shows that 450 years of (Catholic) Portuguese colonisation had a long-lasting impact in India when it comes to education and female emancipation. Furthermore I use a historical quasi-experiment that happened 250 years ago in order to show that different outcomes have different degrees of persitence over time. Educational gaps between males and females seemingly wash out a few decades after the public provision of schools. The male biased sex-ratios on the other hand stay virtually unchanged despite governmental efforts. This provides evidence that deep rooted son preferences are much harder to overcome, suggesting that a differential approach is needed to tackle sex-selective abortion and female neglect. The second chapter proposes improvements for the execution of Spatial Regression Discontinuity Designs. These suggestions are accompanied by a full-fledged spatial statistical package written in R. Chapter three introduces a quantitative economic geography model in order to study the peculiar evolution of the European urban system on its way to the Industrial Revolution. It can explain the shift of economic gravity from the Mediterranean towards the North-Sea ("little divergence"). The framework provides novel insights on the importance of agricultural trade costs and the peculiar geography of Europe with its extended coastline and dense network of navigable rivers.

High-resolution stratigraphy and seismic site characterization of late Quaternary paleovalley systems (Adriatic coastal plain, Italy)

In highly urbanized coastal lowlands, effective site characterization is crucial for assessing seismic risk. It requires a comprehensive stratigraphic analysis of the shallow subsurface, coupled with the precise assessment of the geophysical properties of buried deposits. In this context, late Quaternary paleovalley systems, shallowly buried fluvial incisions formed during the Late Pleistocene sea-level fall and filled during the Holocene sea-level rise, are crucial for understanding seismic amplification due to their soft sediment infill and sharp lithologic contrasts. In this research, we conducted high-resolution stratigraphic analyses of two regions, the Pescara and Manfredonia areas along the Adriatic coastline of Italy, to delineate the geometries and facies architecture of two paleovalley systems. Furthermore, we carried out geophysical investigations to characterize the study areas and perform seismic response analyses. We tested the microtremor-based horizontal-to-vertical spectral ratio as a mapping tool to reconstruct the buried paleovalley geometries. We evaluated the relationship between geological and geophysical data and identified the stratigraphic surfaces responsible for the observed resonances. To perform seismic response analysis of the Pescara paleovalley system, we integrated the stratigraphic framework with microtremor and shear wave velocity measurements. The seismic response analysis highlights strong seismic amplifications in frequency ranges that can interact with a wide variety of building types. Additionally, we explored the applicability of artificial intelligence in performing facies analysis from borehole images. We used a robust dataset of high-resolution digital images from continuous sediment cores of Holocene age to outline a novel, deep-learning-based approach for performing automatic semantic segmentation directly on core images, leveraging the power of convolutional neural networks. We propose an automated model to rapidly characterize sediment cores, reproducing the sedimentologist's interpretation, and providing guidance for stratigraphic correlation and subsurface reconstructions.