Detailed Information on Publication Record
2022
Landscape evolution around the oppidum of Bibracte (Northern Massif Central, France) from the Late Iron Age to the Post-Mediaeval period
PETŘÍK, Jan, Katarína ADAMEKOVÁ, Libor PETR, Isabelle JOUFFROY-BAPICOT, Petr KOČÁR et. al.Basic information
Original name
Landscape evolution around the oppidum of Bibracte (Northern Massif Central, France) from the Late Iron Age to the Post-Mediaeval period
Authors
PETŘÍK, Jan (203 Czech Republic, guarantor, belonging to the institution), Katarína ADAMEKOVÁ (703 Slovakia, belonging to the institution), Libor PETR (203 Czech Republic, belonging to the institution), Isabelle JOUFFROY-BAPICOT (250 France), Petr KOČÁR (203 Czech Republic), Romana KOČÁROVÁ (203 Czech Republic, belonging to the institution), Petra GOLÁŇOVÁ (203 Czech Republic, belonging to the institution) and Vincent GUICHARD (250 France)
Edition
Quaternary International, Elsevier Ltd, 2022, 1040-6182
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
60102 Archaeology
Country of publisher
United Kingdom of Great Britain and Northern Ireland
Confidentiality degree
není předmětem státního či obchodního tajemství
References:
Impact factor
Impact factor: 2.200
RIV identification code
RIV/00216224:14310/22:00124936
Organization unit
Faculty of Science
UT WoS
000862796700001
Keywords in English
Morvan massif; Floodplain geoarchaeology; Anthropogenic impact; Metal pollution; Vegetation history
Tags
Tags
International impact, Reviewed
Změněno: 7/11/2022 09:47, Mgr. Marie Šípková, DiS.
Abstract
V originále
The considerable intensification of human activity in the second and first centuries BC in Central Europe was related to the sudden appearance of a network of large fortified towns, which are known as oppida. Bibracte was one of the most important oppida in France, but knowledge about the evolution of its hinterland is still incomplete. This article addresses the evolution of the landscape surrounding this oppidum. Our research was based on a study of sedimentary profiles sampled around the archaeological site and examined by physical, geochemical and palaeoecological analyses. Sediment sequences indicate that the first humans caused erosion and associated geomorphological change in the 4th–1st century BC. Geochemical results indicate ancient mining and metallurgy in the catchment during the same time. Palaeoecological proxies from the same period point to a mosaic of an open cultural landscape with locally suppressed forest vegetation and prevailing pastoralism. Anthropogenic impact resurged in the 11th–13th centuries AD and was associated with livestock grazing and rye (Secale cereale) cultivation. Thereafter, the reconstructed human impact from the 15th century AD onwards was probably related to forest management focused on timber floating as well as to the cultivation of chestnut (Castanea sativa) and hemp (Cannabis sativa).
Links
EF16_013/0001708, research and development project |
| ||
GA19-02606S, research and development project |
|