The Middle Pleistocene site of Guado San Nicola (Monteroduni, Isernia) is an open-air site investigated in recent years by extensive excavations. Four anthropic layers have been recognized within a thick stratigraphic sequence attributed to the end of MIS 11 based on radiometric dating (40Ar/39Ar and ESR/U-Th combined) and the faunal assemblage composition. Numerous handaxes have been discovered in all the anthropic layers, together with bifacial shaping flakes referred to as the last stages of shaping/resharpening; the debitage component is characterized by the presence, among others, of a Levallois production. The faunal assemblage is composed by Ursus sp., Palaeoloxodon sp., Stephanorhinus kirchbergensis, Equus ferus ssp., Cervus elaphus acoronatus, Dama sp., Megacerini and Bos primigenius. Red deer and horses are the most frequent species. Aurochs are always documented within the anthropic layers, while rhinoceros are scarce. Bear, fallow deer and megaceros are rare, while cervids’ antlers are over-represented. The zooarchaeological analysis revealed that butchery activities were carried out on rhinoceros, horses, and aurochs. The taphonomic analysis made distinguishing the anthropic alterations from the edaphic ones possible. Several taphonomic factors modified the faunal remains: weathering, exfoliations, manganese, iron oxides, trampling, sediment abrasion, root-etching, and, in several cases, floating. Moreover, several notches were recognized at the base of shed antlers that could be referred to as their intentional use as hammers. In conclusion, the zooarchaeological and taphonomic analyses suggest that the assemblage represents the result of anthropic accumulations, subsequently modified by different post-depositional factors of edaphic nature.
Edaphic modifications vs anthropic activities at the Acheulean site of Guado San Nicola (Monteroduni, Isernia): a taphonomic perspective
Ursula Thun Hohenstein
;Brunella Muttillo;Giuseppe Lembo;Maria Chiara Turrini;Marta Arzarello;Benedetto Sala;Carlo Peretto
2023
Abstract
The Middle Pleistocene site of Guado San Nicola (Monteroduni, Isernia) is an open-air site investigated in recent years by extensive excavations. Four anthropic layers have been recognized within a thick stratigraphic sequence attributed to the end of MIS 11 based on radiometric dating (40Ar/39Ar and ESR/U-Th combined) and the faunal assemblage composition. Numerous handaxes have been discovered in all the anthropic layers, together with bifacial shaping flakes referred to as the last stages of shaping/resharpening; the debitage component is characterized by the presence, among others, of a Levallois production. The faunal assemblage is composed by Ursus sp., Palaeoloxodon sp., Stephanorhinus kirchbergensis, Equus ferus ssp., Cervus elaphus acoronatus, Dama sp., Megacerini and Bos primigenius. Red deer and horses are the most frequent species. Aurochs are always documented within the anthropic layers, while rhinoceros are scarce. Bear, fallow deer and megaceros are rare, while cervids’ antlers are over-represented. The zooarchaeological analysis revealed that butchery activities were carried out on rhinoceros, horses, and aurochs. The taphonomic analysis made distinguishing the anthropic alterations from the edaphic ones possible. Several taphonomic factors modified the faunal remains: weathering, exfoliations, manganese, iron oxides, trampling, sediment abrasion, root-etching, and, in several cases, floating. Moreover, several notches were recognized at the base of shed antlers that could be referred to as their intentional use as hammers. In conclusion, the zooarchaeological and taphonomic analyses suggest that the assemblage represents the result of anthropic accumulations, subsequently modified by different post-depositional factors of edaphic nature.I documenti in SFERA sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.