Unveiling the enigma : Decoding human influence in soils with
poor development. Case of study: Celtic oppidum Bibracte

J 2024

Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte

POLEDNÍK MOHAMMADI, Sahar; Lenka LISÁ; Hana GRISON; Piotr MOSKA; Petra GOLÁŇOVÁ et al.

Základní údaje

Originální název

Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte

Autoři

POLEDNÍK MOHAMMADI, Sahar; Lenka LISÁ; Hana GRISON; Piotr MOSKA; Petra GOLÁŇOVÁ a Jiří GERŠL

Vydání

CATENA, ELSEVIER, 2024, 0341-8162

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

60102 Archaeology

Stát vydavatele

Nizozemské království

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 5.700

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14210/24:00137483

Organizační jednotka

Filozofická fakulta

Klíčová slova anglicky

Archaeology; Soil micromorphology; Magnetic susceptibility; Iron Age; Oppidum

Štítky

rivok

Příznaky

Recenzováno

Změněno: 24. 3. 2025 09:38, Mgr. Renata Macholdová

Anotace

V originále

The Late Iron Age Bibracte oppidum, established in the 2nd century BCE, features a distinct soil cover that does not align with typical long-term soil development or human activity patterns. These soils are affected by erosion, but it made them, on the other hand, unique concerning the preservation of information about the past. Single methods applied, as sedimentological, micromorphological and geochemical signals combined with the Optically Stimulated Luminescence (OSL) dating, brought only limited distinguishing patterns, but their combinations together with principal component showed to be crucial for the understanding the formation processes of the site. Significant variations in geochemical composition were observed, particularly in cultural layers, attributed to ashy deposition, pollution, and pedogenesis. Pedogenic magnetic particles, indicated by an increase in frequency dependent magnetic susceptibility, suggest changes in soil formation processes. Colluvial processes triggered naturally or anthropogenically 2 – 4 thousand years ago reveal, that the soil cover underwent repeatedly heavy erosion. Subsequently, some of these sediments were buried under anthropogenic terraces. This period spans from the Late Neolithic to the early Gallo-Roman Period, coinciding with the presence of the oppidum Bibracte during the Late Iron Age. Portable X-ray fluorescence device achieves the best results when combined with other geochemical and mineralogical analyses. This integrated approach ensures a more comprehensive understanding of the soil profile and the underlying site formation processes.

Návaznosti

GA19-02606S, projekt VaV

Název: Oppidum jako urbánní krajina: multidisciplinární přístup ke zkoumání prostorové struktury "intra muros" (Akronym: OPPUK)

Investor: Grantová agentura ČR, Oppidum jako urbánní krajina: multidisciplinární přístup ke zkoumání prostorové struktury "intra muros"

MUNI/A/1353/2023, interní kód MU

Název: Archeologické terénní prospekce, exkavace a dokumentace IV

Investor: Masarykova univerzita, Archeologické terénní prospekce, exkavace a dokumentace IV

Citovat

POLEDNÍK MOHAMMADI, Sahar; Lenka LISÁ; Hana GRISON; Piotr MOSKA; Petra GOLÁŇOVÁ a Jiří GERŠL. Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte. CATENA. ELSEVIER, 2024, roč. 247, Prosinec 2024, s. 1-14. ISSN 0341-8162. Dostupné z: https://doi.org/10.1016/j.catena.2024.108469.

@article{2447707,
   author = {Poledník Mohammadi, Sahar and Lisá, Lenka and Grison, Hana and Moska, Piotr and Goláňová, Petra and Geršl, Jiří},
   article_number = {Prosinec 2024},
   doi = {https://doi.org/10.1016/j.catena.2024.108469},
   keywords = {Archaeology; Soil micromorphology; Magnetic susceptibility; Iron Age; Oppidum},
   language = {eng},
   issn = {0341-8162},
   journal = {CATENA},
   title = {Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte},
   url = {http://dx.doi.org/10.1016/j.catena.2024.108469},
   volume = {247},
   year = {2024}
}

TY  - JOUR
ID  - 2447707
AU  - Poledník Mohammadi, Sahar - Lisá, Lenka - Grison, Hana - Moska, Piotr - Goláňová, Petra - Geršl, Jiří
PY  - 2024
TI  - Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte
JF  - CATENA
VL  - 247
IS  - Prosinec 2024
SP  - 1-14
EP  - 1-14
PB  - ELSEVIER
SN  - 03418162
KW  - Archaeology
KW  - Soil micromorphology
KW  - Magnetic susceptibility
KW  - Iron Age
KW  - Oppidum
UR  - http://dx.doi.org/10.1016/j.catena.2024.108469
N2  - The Late Iron Age Bibracte oppidum, established in the 2nd century BCE, features a distinct soil cover that does not align with typical long-term soil development or human activity patterns. These soils are affected by erosion, but it made them, on the other hand, unique concerning the preservation of information about the past. Single methods applied, as sedimentological, micromorphological and geochemical signals combined with the Optically Stimulated Luminescence (OSL) dating, brought only limited distinguishing patterns, but their combinations together with principal component showed to be crucial for the understanding the formation processes of the site. Significant variations in geochemical composition were observed, particularly in cultural layers, attributed to ashy deposition, pollution, and pedogenesis. Pedogenic magnetic particles, indicated by an increase in frequency dependent magnetic susceptibility, suggest changes in soil formation processes. Colluvial processes triggered naturally or anthropogenically 2 – 4 thousand years ago reveal, that the soil cover underwent repeatedly heavy erosion. Subsequently, some of these sediments were buried under anthropogenic terraces. This period spans from the Late Neolithic to the early Gallo-Roman Period, coinciding with the presence of the oppidum Bibracte during the Late Iron Age. Portable X-ray fluorescence device achieves the best results when combined with other geochemical and mineralogical analyses. This integrated approach ensures a more comprehensive understanding of the soil profile and the underlying site formation processes.
ER  -

POLEDNÍK MOHAMMADI, Sahar; Lenka LISÁ; Hana GRISON; Piotr MOSKA; Petra GOLÁŇOVÁ a Jiří GERŠL. Unveiling the enigma : Decoding human influence in soils with poor development. Case of study: Celtic oppidum Bibracte. \textit{CATENA}. ELSEVIER, 2024, roč.~247, Prosinec 2024, s.~1-14. ISSN~0341-8162. Dostupné z: https://doi.org/10.1016/j.catena.2024.108469.

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