Image analysis in the morphological and morphometric study of teeth

The subject of this doctoral dissertation concerns the definition of a new methodology for the morphological and morphometric study of fossilized human teeth, and therefore strives to provide a contribution to the reconstruction of human evolutionary history that proposes to extend to the different species of hominid fossils. Standardized investigative methodologies are lacking both regarding the orientation of teeth subject to study and in the analysis that can be carried out on these teeth once they are oriented. The opportunity to standardize a primary analysis methodology is furnished by the study of certain early Neanderthal and preneanderthal molars recovered in two caves in southern Italy [Grotta Taddeo (Taddeo Cave) and Grotta del Poggio (Poggio Cave), near Marina di Camerata, Campania]. To these we can add other molars of Neanderthal and modern man of the upper Paleolithic era, specifically scanned in the paleoanthropology laboratory of the University of Arkansas (Fayetteville, Arkansas, USA), in order to increase the paleoanthropological sample data and thereby make the final results of the analyses more significant. The new analysis methodology is rendered as follows: 1. Standardization of an orientation system for primary molars (superior and inferior), starting from a scan of a sample of 30 molars belonging to modern man (15 M1 inferior and 15 M1 superior), the definition of landmarks, the comparison of various systems and the choice of a system of orientation for each of the two dental typologies. 2. The definition of an analysis procedure that considers only the first 4 millimeters of the dental crown starting from the collar: 5 sections parallel to the plane according to which the tooth has been oriented are carried out, spaced 1 millimeter between them. The intention is to determine a method that allows for the differentiation of fossilized species even in the presence of worn teeth. 3. Results and Conclusions. The new approach to the study of teeth provides a considerable quantity of information that can better be evaluated by increasing the fossil sample data. It has been demonstrated to be a valid tool in evolutionary classification that has allowed (us) to differentiate the Neanderthal sample from that of modern man. In a particular sense the molars of Grotta Taddeo, which up until this point it has not been possible to determine with exactness their species of origin, through the present research they are classified as Neanderthal.

Analisi del popolamento e delle dinamiche culturali del Neolitico nella Puglia Centrale : un approccio territoriale per la Bassa Murgia

L’obiettivo della ricerca condotta dal candidato è stato sin dal principio la proposta di un’analisi del popolamento e delle dinamiche culturali dell’età neolitica nella Puglia Centrale. Tale aspirazione derivava dal fatto che il territorio oggetto di tale ricerca è stato, negli ultimi decenni, assai meno investigato rispetto alle limitrofe aree, come la piana del Tavoliere ed il Salento in particolare. Questa mancanza di informazioni rendeva necessaria una rivisitazione delle ricerche e degli studi, attraverso la costruzione di un atlante del popolamento, al fine di colmare questo vuoto. Infatti, una valutazione del popolamento dell’età neolitica nell’Italia sud-orientale non può essere considerata per aree culturali distinte e geograficamente limitate. Nonostante vi siano importanti differenziazioni di facies archeologiche, è solo attraverso una visione complessiva e con un controllo articolato delle informazioni che è possibile descrivere i processi e le dinamiche che hanno portato ad un popolamento così imponente, dalla sua espansione al repentino collasso, causando la trasformazione del paesaggio pugliese. La scelta di guardare alla complessità neolitica di questo versante della Puglia si lega culturalmente, oltre che geograficamente, alla ricerca già effettuata sulla grande diffusione del neolitico nella piana del Tavoliere di Puglia, unico esempio europeo in quanto a colonizzazione capillare del territorio..Ciò ha permesso di disegnare un quadro globale, che al momento esclude solo la penisola salentina, del popolamento neolitico della Puglia settentrionale e centrale. Le caratteristiche che differenziano i due complessi, sono strettamente legate sia all’habitat insediativo, inteso come scelte insediamentali, che nella regione indagata appare organizzato su diversi livelli (area costiera adriatica, area prospiciente antichi alvei torrentizi, propaggini dell’altopiano delle Murge), che alle forme culturali, intese come produzione artigianale e soprattutto aspetti rituali connessi alla frequentazione delle grotte naturali.

Speleogenesis and secondary cave minerals in quartz-sandstone and quartzite environment

The main objective of this research is to improve the comprehension of the processes controlling the formation of caves and karst-like morphologies in quartz-rich lithologies (more than 90% quartz), like quartz-sandstones and metamorphic quartzites. In the scientific community the processes actually most retained to be responsible of these formations are explained in the “Arenisation Theory”. This implies a slow but pervasive dissolution of the quartz grain/mineral boundaries increasing the general porosity until the rock becomes incohesive and can be easily eroded by running waters. The loose sands produced by the weathering processes are then evacuated to the surface through processes of piping due to the infiltration of waters from the fracture network or the bedding planes. To deal with these problems we adopted a multidisciplinary approach through the exploration and the study of several cave systems in different tepuis. The first step was to build a theoretical model of the arenisation process, considering the most recent knowledge about the dissolution kinetics of quartz, the intergranular/grain boundaries diffusion processes, the primary diffusion porosity, in the simplified conditions of an open fracture crossed by a continuous flow of undersatured water. The results of the model were then compared with the world’s widest dataset (more than 150 analyses) of water geochemistry collected till now on the tepui, in superficial and cave settings. All these studies allowed verifying the importance and the effectiveness of the arenisation process that is confirmed to be the main process responsible of the primary formation of these caves and of the karst-like superficial morphologies. The numerical modelling and the field observations allowed evaluating a possible age of the cave systems around 20-30 million of years.