The Pirro Nord palaeontological and archaeological locality has been the object of recent fi eld research to investigate the fossil content of its Early Pleistocene vertebrate palaeocommunities, and to understand the genesis of the karst network and related deposits that delivered the lithic industry representing the earliest human occupation of Europe known so far, spanning 1.7e1.3 Ma. The succession of the Pirro 10 site has been described in terms of facies and fossil vertebrate content of the 37 distinguished Sedi- mentary Units (SU). On the whole, the succession is made of chemical and clastic sediments that include debris fall and alluvial deposits. SU are distinguished according to lithology, colour, discontinuities, lamin...
International audienceDecades of fieldwork in the Frosinone-Ceprano basin (Latin Valley, Latium, cen...
Multidisciplinary investigations at Pagliare di Sassa (L’Aquila, central Italy) suggest that the loc...
New field data on the Late Pleistocene deposit of Ingarano (Foggia) allow us to hypothesise the occu...
The Pirro Nord palaeontological and archaeological locality has been the object of recent field rese...
Some flint lithic artifacts were discovered in the fissure fillings of the well-known Pirro Nord sit...
The fossiliferous karst deposits of the typical Pirro Nord Faunal Unit recently revived interest for...
The site of Pirro Nord (also known as Cava Pirro or Cava Dell'Erba) is known in literature since the...
Some flint lithic artifacts were discovered in the fissure fillings of the well-known Pirro Nord si...
The Pirro 13 karst fissure (Cava dell'Erba, Apricena, Foggia, Italy) shows a significant vertebrate ...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
Recent functional and zooarchaeological studies conducted on the archeological finds of Pirro Nord (...
Ever since their percolation from neighbour disciplines, archaeology has employed spatial statistics...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
Since the late 70s, the Early Pleistocene (Gelasian) site of Coste San Giacomo (Anagni Basin, centra...
International audienceDecades of fieldwork in the Frosinone-Ceprano basin (Latin Valley, Latium, cen...
Multidisciplinary investigations at Pagliare di Sassa (L’Aquila, central Italy) suggest that the loc...
New field data on the Late Pleistocene deposit of Ingarano (Foggia) allow us to hypothesise the occu...
The Pirro Nord palaeontological and archaeological locality has been the object of recent field rese...
Some flint lithic artifacts were discovered in the fissure fillings of the well-known Pirro Nord sit...
The fossiliferous karst deposits of the typical Pirro Nord Faunal Unit recently revived interest for...
The site of Pirro Nord (also known as Cava Pirro or Cava Dell'Erba) is known in literature since the...
Some flint lithic artifacts were discovered in the fissure fillings of the well-known Pirro Nord si...
The Pirro 13 karst fissure (Cava dell'Erba, Apricena, Foggia, Italy) shows a significant vertebrate ...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
Recent functional and zooarchaeological studies conducted on the archeological finds of Pirro Nord (...
Ever since their percolation from neighbour disciplines, archaeology has employed spatial statistics...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
The karstic areas of Apulia in SE Italy are characterized by fissures locally called ventarole, whic...
Since the late 70s, the Early Pleistocene (Gelasian) site of Coste San Giacomo (Anagni Basin, centra...
International audienceDecades of fieldwork in the Frosinone-Ceprano basin (Latin Valley, Latium, cen...
Multidisciplinary investigations at Pagliare di Sassa (L’Aquila, central Italy) suggest that the loc...
New field data on the Late Pleistocene deposit of Ingarano (Foggia) allow us to hypothesise the occu...