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.Základní údaje
Originální název
Landscape evolution around the oppidum of Bibracte (Northern Massif Central, France) from the Late Iron Age to the Post-Mediaeval period
Autoři
PETŘÍK, Jan (203 Česká republika, garant, domácí), Katarína ADAMEKOVÁ (703 Slovensko, domácí), Libor PETR (203 Česká republika, domácí), Isabelle JOUFFROY-BAPICOT (250 Francie), Petr KOČÁR (203 Česká republika), Romana KOČÁROVÁ (203 Česká republika, domácí), Petra GOLÁŇOVÁ (203 Česká republika, domácí) a Vincent GUICHARD (250 Francie)
Vydání
Quaternary International, Elsevier Ltd, 2022, 1040-6182
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
60102 Archaeology
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.200
Kód RIV
RIV/00216224:14310/22:00124936
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000862796700001
Klíčová slova anglicky
Morvan massif; Floodplain geoarchaeology; Anthropogenic impact; Metal pollution; Vegetation history
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 7. 11. 2022 09:47, Mgr. Marie Šípková, DiS.
Anotace
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).
Návaznosti
EF16_013/0001708, projekt VaV |
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GA19-02606S, projekt VaV |
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