New insights on the late Pleistocene-Holocene lithic industry in East Kalimantan (Borneo) ; contribution of three rock shelter sites in the karstic area of the Mangkalihat Peninsula - Archive ouverte HAL Accéder directement au contenu
Article Dans Une Revue Quaternary International Année : 2016

New insights on the late Pleistocene-Holocene lithic industry in East Kalimantan (Borneo) ; contribution of three rock shelter sites in the karstic area of the Mangkalihat Peninsula

Résumé

The discovery of pottery dated to around 20ka cal BP, within terminal Pleistocene cave sites in South China has been heatedly debated over the past decades. While the dates and pottery itself gained great attention, the archaeological context in which these findings were made have received less attention due to language biases, making it difficult to address questions of how and why pottery emerged in this region. This paper summarized the major findings from South China pottery-bearing sites dated between 25 and 10ka cal BP, and critically evaluates the environmental, cultural and behavioral changes during and after the Last Glacial Maximum (LGM). The most up to date discoveries demonstrate that pottery appeared in South China right after the LGM, together with changes in lithic assemblages, the appearance of various bone and antler artefacts, as well as a transition to more sedentary lifeways with a heavier reliance on aquatic resources and small-sized animals, long before the appearance of early agriculture. These findings also reflect a more complex history and cultural diversity of different human groups in this area.
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Dates et versions

hal-01279937 , version 1 (28-02-2016)

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Michel Grenet, Josette Sarel, R. Fauzy, Adhi Agus Oktaviana, Bambang Sugiyanto, et al.. New insights on the late Pleistocene-Holocene lithic industry in East Kalimantan (Borneo) ; contribution of three rock shelter sites in the karstic area of the Mangkalihat Peninsula. Quaternary International, 2016, 416, pp.126-150. ⟨10.1016/j.quaint.2015.11.044⟩. ⟨hal-01279937⟩
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