40 Years of Casal de' Pazzi in the framework of Pleistocene archeo-paleontological sites (400,000-40,000 BP): current knowledge and new research perspectives (original) (raw)
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FIFTH GEOARCHAEOLOGICAL CONFERENCE INFO_March 2018_1st call_3.pdf
Dear colleagues, We kindly invite You to the 5th Geoarchaeological conference: LATE ANTIQUITY AND MIGRATION PERIOD IN THE LIGHT OF GEOARCHAEOLOGICAL RECORDS FROM THE EASTERN MEDITERRANEAN, EASTERN ADRIATIC AND ADJACENT REGIONS - organized by the Institute of Archaeology, Cardinal Stefan Wyszynski University in Warsaw, the Institute of Archaeology in Zagreb and Faculty of Humanities and Social Sciences, University of Zagreb. The Conference will be held at the Library of the Faculty of Humanities and Social Sciences, Zagreb 23rd-24th of October 2018. Requests for detailed information please contact Dr Katarina Botic: kbotic@iarh.hr. We are looking forward to Your participation. Dr hab. Fabian Welc Institute of Archaeology, Cardinal Stefan Wyszynski University in Warsaw, Poland (President of the organizing committee) Dr. Katarina Botić Institute of Archaeology, Zagreb, Croatia (Vice-president of the organizing committee) Prof. Marcel Burić Department of Archaeology, Faculty of Humanities and Social Sciences, University of Zagreb, Croatia (Member of the organizing committee)
Quaternary International, 2011
Archeological and paleo-environmental researches carried on the Grotta Grande site illustrate the importance of a multidisciplinary approach among archeologists, palynologists and paleontologists. The archaeology, fauna, pollen and micro-charcoal recovered in two short sedimentary successions (trenches A, F) located close to the entrance of the cave are discussed. The cave opens directly on the Tyrrhenian Sea, 2 km from Scario (Salerno, Campania, Southern Italy). The morphology of the cave and sedimentary processes were controlled by eustatic fluctuations during the late Middle Pleistocene and the early Late Pleistocene. The sea repeatedly occupied the cave. The cave was frequented by humans of Middle Palaeolithic culture. Archaeological and faunal record of the two trenches can be positioned within the climatic fluctuation posterior to the warm interglacial MIS 5e peak. Pollen have been retrieved in the older series (bec) of trench A, referable to MIS 7e6.
INVITATION FOR THE FIFTH GEOARCHAEOLOGICAL CONFERENCE INFO_March 2018_1st call.pdf
Dear colleagues, We kindly invite You to the 5th Geoarchaeological conference: LATE ANTIQUITY AND MIGRATION PERIOD IN THE LIGHT OF GEOARCHAEOLOGICAL RECORDS FROM THE EASTERN MEDITERRANEAN, EASTERN ADRIATIC AND ADJACENT REGIONS - organized by the Institute of Archaeology, Cardinal Stefan Wyszynski University in Warsaw, the Institute of Archaeology in Zagreb and Faculty of Humanities and Social Sciences, University of Zagreb. The Conference will be held at the Library of the Faculty of Humanities and Social Sciences, Zagreb 23rd-24th of October 2018. Requests for detailed information please contact dr Katarine Botic: kbotic@iarh.hr We are looking forward to Your participation. Dr hab. Fabian Welc Institute of Archaeology, Cardinal Stefan Wyszynski University in Warsaw, Poland. President of the organizing committee Dr. Katarina Botić Institute of Archaeology, Zagreb, Croatia. Vice-president of the organizing committee Prof. Marcel Burić Department of Archaeology, Faculty of Humanities and Social Sciences, University of Zagreb, Croatia. Member of the organizing committee
Journal of Mediterranean Earth Sciences 15 (2023), 127-140
More than 40 years after the discovery of the Paleolithic open-air site of Casal De Pazzi (Rome, Italy), and about 35 years after the pioneering study of the lithic industry found at the site, the 2022 conference held in Rome [40 Years of Casal de' Pazzi in the framework of Pleistocene archeo-paleontological sites (400,000-40,000 BP): current knowledge and new research perspectives] provided the much-needed opportunity to resume a research that had been suspended for too long. Studies on the lithic industry were carried out in the late 1980s on a sample of approximately one-third of the whole assemblage found at the site, and they were conducted using methods and tools quite advanced for the time; thus, the results remain valid at the present day. In an era when computer tools were still extremely rare, a database was created with a substantial number of entries, both typological and technological. In recent years much has been done in the study field of lithic assemblages, promoting and expanding both the technological and taphonomic approaches. Furthermore, many reflections and studies have allowed for the in-depth exploration of issues related to fluvial deposits, which characterize a significant portion of the Lower-Middle Pleistocene sites in Europe and beyond. Subsequent inputs for new reflections on the aforementioned topics came from a further, albeit limited, excavation campaign carried out in 2013, which unearthed a section of a bank deposit that could be fully correlated with what was documented in the first excavation campaign. The new data have prompted a discussion on depositional setting and have allowed for a better understanding of the use and origins of the raw materials used. The objective of this work, based on the previous database, is to encourage a comprehensive study of the lithic assemblage and to correlate it with updated data on stratigraphy, possible more precise dating, and necessary investigations on faunal and floral assemblages.
Vallone Inferno rock-shelter is an archaeological site located in the Madonie mountain range in Sicily. Archaeological excavation and research have provided a long prehistoric and historic sequence from the Neolithic to the medieval period, this being the most complete work in this area at present. In this paper we present the preliminary data provided by a multidisciplinary study based on pottery, lithic, human, faunal and plant remains. Stratigraphic studies have identified four complexes, of which complex 3 has provided almost all the archaeological remains. 14 C AMS dates, obtained from four samples, place the human activities between 2601 cal BC and 644 cal AD. These dates are coherent with the cultural attribution of the ceramic and lithic remains. Macrofaunal and plant remains show a persistent use of the shelter for pastoral activities. Environmental data, obtained from microvertebrate and archaeobotanical remains, show the aridification and opening of the landscape from the base to the top of the sequence as a consequence of the human impact.
2001 - “Natural environment: geomorphological features and lithic resources” (Rome)
2001 - Claudio Caputo, Antonia Arnoldus-Huyzendveld & Franco Pugliese: “Natural environment: geomorphological features and lithic resources”
The landscape of the region surrounding Rome - of which the volcanic complexes of the Monti Sabatini and Alban Hills make part. The landscape of this region is the result of the combined action of volcanism and exogenous agents. The morphological aspect of these volcanic complexes is quite similar in the peripheral areas and rather different in their central parts. Denudational processes are mainly due to channelled running waters that show different drainage patterns. The resulting landforms consist of different shaped valleys often controlled by structural factors. A more detailed description is given for a particularly interesting sector of the Monti Sabatini. Flint resources for lithic tool production on pebble are scarse in the Roman area. They are limited to Pliocene and Quaternary fluvial and marine deposits. In a study of 1995, four gravel “flint provinces” were differentiated for central Latium, each characterized by a specific composition in flint types and percentages. The provenance of the chert material used in the two lower Paleolithic sites of La Polledrara di Cecanibbio and Rebibbia-Casal de’Pazzi could be related to these provinces.
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L'area del Mediterraneo, ed in particolare l'Italia, possiedono uno straordinario patrimonio culturale materiale e immateriale di eccezionale valore universale (OUV, sensu ICOMOS). Tale eredità deve essere protetta e conservata, con particolare attenzione verso i monumenti, gli edifici storico-architettonici, come ad esempio le chiese, le torri, palazzi, centri storici e siti archeologici, che testimoniano la memoria storica delle fasi di insediamento in diversi contesti geografici.