2024
Fluctuating nature of prehistoric settlement and land use preserved in sedimentary record of vanished gully
PETŘÍK, Jan, Katarína ADAMEKOVÁ, Michaela PRIŠŤÁKOVÁ, Libor PETR, Tomáš TENCER et. al.Základní údaje
Originální název
Fluctuating nature of prehistoric settlement and land use preserved in sedimentary record of vanished gully
Autoři
PETŘÍK, Jan, Katarína ADAMEKOVÁ, Michaela PRIŠŤÁKOVÁ, Libor PETR, Tomáš TENCER, Jan NOVÁK, Jakub VRÁNA, Marek KALÁBEK, Jaroslav PEŠKA a Peter MILO
Vydání
CATENA, GERMANY, ELSEVIER, 2024, 0341-8162
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
60102 Archaeology
Stát vydavatele
Německo
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 6.200 v roce 2022
Organizační jednotka
Filozofická fakulta
UT WoS
999
Klíčová slova anglicky
Prehistory; Geophysics; Erosion; Soil regeneration; Landscape formation
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 18. 7. 2024 11:06, Mgr. Marie Šípková, DiS.
Anotace
V originále
The long-inhabited Central European lowlands have exposed to significant erosion since prehistoric times, primarily due to deforestation and agricultural practices, leading to colluvium formation and erosional features. Infilled erosional gullies, particularly near abandoned settlements, may offer insights into landscape changes and settlement evolution. Our multidisciplinary research at the Přerov-Předmostí archaeological megasite in Czechia integrates geoarchaeological methods, geophysics and extensive development-driven excavations. This site, located on the migratory corridor between the Pannonian and Poland plains, serves as a focal point for studying the interplay between human settlement, land-use development and environmental changes in this region. By combining geophysics and excavation, we investigate settlement and land-use patterns, correlating these with the environmental and pedosedimentary record of an infilled gully. The incision of the gully represents initial phase of erosion at this site. Formed before 2300 BC, it is among the oldest in the region, likely triggered by Late Neolithic land use. Our findings also indicate a cyclical erosion pattern linked to four primary settlement peaks: the Early Bronze Age (2300–1600/1500 BC), the Young/Late Bronze Age (1500–900 BC), the Hallstatt period (900–400 BC) and the La Tène period (400 BC–50 BC/1 AD). These periods of heightened settlement activity alternated with times of reduced or no population pressure, leading to stabilisation and subsequent pedogenesis.
Návaznosti
TL03000537, projekt VaV |
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