Human-induced prehistoric soil buried in the flood plain of Svratka River, Czech Republic
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F19%3A43915179" target="_blank" >RIV/62156489:43410/19:43915179 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67985831:_____/19:00504106 RIV/48511005:_____/19:N0000018 RIV/00216224:14310/19:00111301 RIV/44555601:13520/19:43894588 RIV/00216208:11310/19:10382704
Výsledek na webu
<a href="https://doi.org/10.1177/0959683618824785" target="_blank" >https://doi.org/10.1177/0959683618824785</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1177/0959683618824785" target="_blank" >10.1177/0959683618824785</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Human-induced prehistoric soil buried in the flood plain of Svratka River, Czech Republic
Popis výsledku v původním jazyce
The natural setting and prehistoric human activity on Holocene floodplains in Central Europe is a compelling issue from several points of view. This environment presents an important sedimentary archive reflecting past human behaviour in interactions with climate change. Two sedimentary sections recorded in the alluvial zone of Svratka River (Moravia) with a buried soil dated to the time span between the Neolithic and Late Bronze Age, and comprising one paleo-catena, were investigated using a multiproxy approach. The buried paleo-catena presents evidence of long-term (ancient) soil development, and the use of the site for human settlement and farming ca. 4500 BC until 1000 BC. Buried soil horizons indicate (climate) stability, which according to archaeological evidence lasted for at least 3500 years, until at least 1000 BC. The architecture and the lithology of the river floodplain changes approximately 0 AD. Anthropogenic settlement activity was not detected at the site in the subsequent period, and this is very likely to be associated with increased sedimentation rates and less optimal conditions for human settlement.
Název v anglickém jazyce
Human-induced prehistoric soil buried in the flood plain of Svratka River, Czech Republic
Popis výsledku anglicky
The natural setting and prehistoric human activity on Holocene floodplains in Central Europe is a compelling issue from several points of view. This environment presents an important sedimentary archive reflecting past human behaviour in interactions with climate change. Two sedimentary sections recorded in the alluvial zone of Svratka River (Moravia) with a buried soil dated to the time span between the Neolithic and Late Bronze Age, and comprising one paleo-catena, were investigated using a multiproxy approach. The buried paleo-catena presents evidence of long-term (ancient) soil development, and the use of the site for human settlement and farming ca. 4500 BC until 1000 BC. Buried soil horizons indicate (climate) stability, which according to archaeological evidence lasted for at least 3500 years, until at least 1000 BC. The architecture and the lithology of the river floodplain changes approximately 0 AD. Anthropogenic settlement activity was not detected at the site in the subsequent period, and this is very likely to be associated with increased sedimentation rates and less optimal conditions for human settlement.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10508 - Physical geography
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Holocene
ISSN
0959-6836
e-ISSN
—
Svazek periodika
29
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
13
Strana od-do
565-577
Kód UT WoS článku
000463639500003
EID výsledku v databázi Scopus
2-s2.0-85060947797