Search results for "Sicily ."
showing 10 items of 103 documents
Timing of the emergence of the Europe-Sicily bridge (40-17 cal ka BP) and its implications for the spread of modern humans
2014
The submerged sill in the Strait of Messina, which is located today at a minimum depth of 81 m below sea level (bsl), represents the only land connection between Sicily and mainland Italy (and thus Europe) during the last lowstand when the sea level locally stood at about 126 m bsl. Today, the sea crossing to Sicily, although it is less than 4 km at the narrowest point, faces hazardous sea conditions, made famous by the myth of Scylla and Charybdis. Through a multidisciplinary research project, we document the timing and mode of emergence of this land connection during the last 40 kyr. The integrated analysis takes into consideration morphobathymetric and lithological data, and relative sea…
Istituzioni ecclesiastiche e potere regio nel mediterraneo medievale. Scritti per Salvatore Fodale
2016
Il volume è un omaggio degli allievi al professore Salvatore Fodale. Il filo conduttore sono le Istituzioni ecclesiastiche e il potere regio tra l’età normanna e la fine del Medioevo. Uno spazio particolare è dedicato alla città di Messina, al centro dei saggi sulla religiosità tra Oriente e Occidente e su Raimondo Puyolis, arcivescovo catalano nel Trecento. Il rapporto tra Istituzioni ecclesiastiche e potere regio emerge negli articoli su Papato e propaganda di crociata nel Duecento e sul monastero di Santa Maria del Bosco di Calatamauro. Viene, inoltre, esaminata la complessa relazione tra Martino il Giovane e la comunità ebraica siciliana. Il regno di Alfonso il Magnanimo fa da sfondo ai…
Calcareous nannofossil assemblages from the Central Mediterranean Sea over the last four centuries: the impact of the Little Ice Age
2010
Abstract. We present decadal-scale calcareous nannofossil data from four short cores (Station 272, 37° 17' N, 12° 48' E, 226 m depth; St 342, 36° 42' N, 13° 55' E, 858.2 m depth; St 407, 36° 23' N, 14° 27' E, 345.4 m depth; C90-1M, 40° 36' N, 14° 42' E, 103.4 m depth) recovered in the central Mediterranean Sea (northern Sicily Channel and Tyrrhenian Sea), which, on the basis of 210Pb activity span the last 200–350 years. Assemblages are dominated by placoliths, mostly Emiliania huxleyi, while, at least in the Sicily Channel sediments, Florisphaera profunda was an important part of the coccolithophore community. The paleoenvironmental reconstruction, based on ecological preference of species…
Maestri e cantieri nella Sicilia interna tra XV e XVI secolo: le chiese Madri di Pietraperzia e Assoro
2014
The essay focuses on two yards of the interior of Sicily between the end of the fifteenth century and the first half of the sixteenth century: the mother church of Pietraperzia and that of Assoro. New documentary investigations allowed to set out the master builders involved in the construction process and to deduce some construction methods in use for churches basilica. These data, together with the direct observation of the buildings have allowed to hypothesize, in both cases, the original configuration of the churches. The hypotheses were supported by a comparison with contemporary building, similar to typological characteristics, and a re-reading of the archival documents referring to t…
Centennial- to millennial-scale climate oscillations in the Central-Eastern Mediterranean Sea between 20,000 and 70,000 years ago: Evidence from a hi…
2012
Abstract Here we present a high-resolution faunal, floral and geochemical (stable isotopes and trace elements) record from the sediments of Ocean Drilling Program Site 963 (central Mediterranean basin), which shows centennial/millennial-scale resemblance to the high-northern latitude rapid temperature fluctuations documented in the Greenland ice cores between 20 and 70 kyr BP. Oxygen and carbon isotopes, planktic foraminifera and calcareous nannofossil distributions suggest that Dansgaard–Oeschger (D/O) and Heinrich events (HE) are distinctly expressed in the Mediterranean climate record. Moreover, recurrent though subdued oscillations not previously identified in the Lateglacial Mediterran…
Surface and deep water conditions in the Sicily channel (central Mediterranean) at the time of sapropel S5 deposition
2011
New centennial-scale data of benthic foraminifera assemblages and of stable isotopes of foraminifera shells from the Sicily Channel, representative of surface and bottom waters, over the interval between about 140 and 110 kyr BP, are presented. During this period anoxia developed on the eastern Mediterranean basin and sapropel S5 deposited. Although anoxic sediments have not been deposited in the Sicily Channel, this area is strategic to study the character of intermediate waters, whose chemical-physical properties strongly precondition the eastern Mediterranean deep water formation. So far, no data from these water masses have been obtained, apart from the isotopic composition of shells of…
Differential Greek and northern African migrations to Sicily are supported by genetic evidence from the Y chromosome
2009
The presence or absence of genetic heterogeneity in Sicily has long been debated. Through the analysis of the variation of Y-chromosome lineages, using the combination of haplogroups and short tandem repeats from several areas of Sicily, we show that traces of genetic flows occurred in the island, due to ancient Greek colonization and to northern African contributions, are still visible on the basis of the distribution of some lineages. The genetic contribution of Greek chromosomes to the Sicilian gene pool is estimated to be about 37% whereas the contribution of North African populations is estimated to be around 6%. In particular, the presence of a modal haplotype coming from the southern…
Dynamics at the Strait of Sicily and Mediterranean Sapropels
2012
Millennial-scale paleoenvironmental changes in the central Mediterranean during the Last Interglacial: comparison with European and Mediterranean rec…
2008
Piano di Gestione UNESCO Isole EOLIE
2008
Nel Piano di gestione del sito UNESCO Isole Eolie sono definiti i criteri e le modalità per realizzare contemporaneamente l’obiettivo della tutela di un bene e uno sviluppo locale sostenibile. Il Piano contiene una mappatura dei Beni Culturali e Ambientali e Naturalistici, descrivendo un sistema territorio sotto il profilo economico-ambientale che contiene: - L’inquadramento storico, economico e antropologico del sito, l’uso finora fatto, i fattori di incidenza sui beni ambientali e culturali; - L’inquadramento attuale del sito, attraverso un’analisi degli strumenti legislativi e amministrativi e della loro conformità; - L’analisi dei processi produttivi critici e le relative interazioni co…