2025
Highland transformation: Human impact in the Bukov Brook valley (Bohemian-Moravian Highlands) from Prehistory to the modern era
PETŘÍK, Jan; Libor PETR; Miroslav DEJMAL; Michaela PRIŠŤÁKOVÁ; Michal VÁGNER et. al.Základní údaje
Originální název
Highland transformation: Human impact in the Bukov Brook valley (Bohemian-Moravian Highlands) from Prehistory to the modern era
Autoři
PETŘÍK, Jan (203 Česká republika, garant, domácí); Libor PETR (203 Česká republika, domácí); Miroslav DEJMAL ORCID (203 Česká republika, domácí); Michaela PRIŠŤÁKOVÁ (703 Slovensko, domácí); Michal VÁGNER ORCID (203 Česká republika, domácí); Petr KOČÁR (203 Česká republika); Klára ŠABATOVÁ (203 Česká republika, domácí); Marcin FRĄCZEK; Aleš BAJER (203 Česká republika); Katarína ADAMEKOVÁ (703 Slovensko) a Mojmír HRÁDEK (203 Česká republika)
Vydání
Anthropocene, Elsevier Ltd, 2025, 2213-3054
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
Impakt faktor
Impact factor: 3.900 v roce 2024
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001480511800001
EID Scopus
2-s2.0-105003187389
Klíčová slova anglicky
Landscape dynamics; Mining; Water reservoir; Deforestation; Erosion; Archaeology; Mediaeval
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 17. 7. 2025 08:25, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
The history of human activities in the Central European mid-mountains differs significantly from the intensively inhabited lowlands. The Bohemian-Moravian Highlands are believed to have been settled during the onset of metal mining in the 13th century AD. Our evidence from the floodplain deposits of Bukov Brook demonstrates deforestation and sporadic human settlement activities during the prehistoric era, already occurring as early as the Bronze Age, as evidenced by pottery, charcoal and Lens culinaris cf. in the alluvial fan sediments. In this period, the landscape was covered by Abies and Fagus. Since the 10th–12th centuries AD, an agricultural landscape with mild deforestation has been inferred from buried floodplain sediments, despite limited archaeological evidence of settlement. Significant geomorphological changes were observed in the 11th–13th centuries AD, driven by prospecting, mining activities, pond construction, and intensive deforestation, accompanied by the limited presence of cultivated grain. Between the 13th and 16th centuries AD, mining activities ceased, anthropogenic influence increased, and the deforested landscape became more conducive to agriculture, grain cultivation, and grazing. From the 16th century AD onwards, erosion from fine washouts of fields and pastures became prevalent, and the once-functional pond vanished. This comprehensive picture underscores the role of smaller catchments in mid-mountain regions like the Bohemian-Moravian Highlands highlighting their significance in the research of landscape transformation, resource exploitation, and land-use practices. It also sets the stage for further exploration into the evolving dynamics of human-environment interactions across various historical periods.
Návaznosti
CZ.02.01.01/00/22_008/0004593, interní kód MU |
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EH22_008/0004593, projekt VaV |
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