High-resolution stratigraphy of Central and Southern Adriatic Quaternary deposits of sub-Milankovian climate change on Mediterranean circulation

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)).

Paesaggi agrari. Nuove prospettive per i sistemi territoriali: agricoltura ecologica, saperi tradizionali, scambio locale

Il paesaggio, e così anche il paesaggio agrario, può essere considerato come segno del rapporto uomo/natura, come costrutto storico che testimonia il succedersi delle diverse civilizzazioni che l'hanno generato, ma anche come spazio per l'immaginazione territoriale, come progetto per il futuro del territorio. In questo lavoro si trattano le relazioni tra questa visione del paesaggio e le forme di produzione e consumo dei prodotti agricoli, nell'ambito delle trasformazioni che l'ambito rurale sta subendo a partire dagli ultimi decenni, tra pressione dell'urbano, da un lato, e abbandono e crisi dell'agricoltura, dall'altro. Particolare attenzione è riservata a quelle esperienze che, attraverso la produzione biologica e lo scambio locale, esprimono un nuovo progetto di territorio, che prende avvio dal contesto rurale ma che pervade anche le città, proponendo anche nuove relazioni tra città e campagna. Nelle reti della filiera corta e dell'economia solidale che si concretizzano soprattutto come esperienze “dal basso”, di autogestione e partecipazione, si diffondono insieme prodotti e valori. In quest'ottica la sostenibilità ambientale non appare più come una fonte di limitazioni e esternalità negative, per dirla con il linguaggio dell'economia, ma diventa un valore aggiunto di appartenenza collettiva (equilibri ecologici, paesaggio) e un'occasione per nuove relazioni sociali e territoriali.

Lexis paidike. L'infanzia in Origene

La tesi considera la trattazione del tema dell’infanzia nell’opera di Origene di Alessandria attraverso l’analisi dei testi trasmessi nell’originale greco e delle traduzioni latine di Rufino e Gerolamo. Il motivo dell’infanzia è considerato nei suoi molteplici significati, a più livelli: esegetico, antropologico, filosofico, teologico. La ricerca non si limita dunque ad un’analisi di taglio storico, ma ambisce a definire la concezione e la considerazione della prima età dal punto di vista di Origene e nel contesto più ampio della letteratura coeva. Attraverso una lettura estensiva del corpus dell’Alessandrino sono stati isolati tutti i passi che si riferiscono all’infanzia a livello letterale e metaforico. Ne emerge una trattazione complessa del tema: il bambino è per Origene, in linea con le contemporanee dottrine filosofiche, un essere eminentemente irrazionale. Il pieno sviluppo della facoltà razionale si colloca al termine di questa prima fase dell’esistenza. L’irrazionalità infantile previene nei più piccoli l’insorgere delle passioni. A questa dottrina, di matrice stoica, si ricollegano alcuni sviluppi di grande rilievo: la non-imputabilità dei minori ed il legame tra razionalità e responsabilità individuale; la riflessione sulla sofferenza dei bambini e la ricerca di una sua causa, che non intacchi il principio della giustizia divina; l’ipotesi della preesistenza delle anime. Sul piano teologico la ricerca si focalizza sulle nozioni di paternità e filiazione e sul tema, centrale nell’orizzonte origeniano, della pedagogia. Origene concepisce la pedagogia umana, sul modello di quella divina, come una rete dinamica di relazioni che ricalca i rapporti parentali. A fianco di questi ambiti d’interesse principali l’analisi considera aspetti ulteriori: risalto è concesso, in particolare, all’elemento biografico ed all’aspetto linguistico e letterario della prosa origeniana, quest'ultimo spesso trascurato dalla critica. Lo studio mostra inoltre la vitalità di alcuni modelli esegetici origeniani nella tradizione successiva.