Geoarchaeological studies carried out on the sequence of Caverna degli Orsi - Medvedja Jama (Trieste, Italy), corroborate the hypothesis -based on biostratigraphy- that the deposit formed in the time span between the end of the last Interglacial (MIS 5) and the end of the early-middle Pleniglacial (MIS 4). The studied sequence includes ceiling breakdown deposits, loess, debrisfall/debrisflow, and organic phosphates deriving mainly from the decay of cave bear bones.
Bears and sediments at Caverna degli Orsi/Medvedja Jama (Trieste, Italy).
BOSCHIAN, GIOVANNI;
2011-01-01
Abstract
Geoarchaeological studies carried out on the sequence of Caverna degli Orsi - Medvedja Jama (Trieste, Italy), corroborate the hypothesis -based on biostratigraphy- that the deposit formed in the time span between the end of the last Interglacial (MIS 5) and the end of the early-middle Pleniglacial (MIS 4). The studied sequence includes ceiling breakdown deposits, loess, debrisfall/debrisflow, and organic phosphates deriving mainly from the decay of cave bear bones.File in questo prodotto:
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