Sediments of Biśnik Cave (Poland): Lithology and stratigraphy of the Middle Palaeolithic site

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F14%3A00427465" target="_blank" >RIV/67985831:_____/14:00427465 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quaint.2013.10.017" target="_blank" >http://dx.doi.org/10.1016/j.quaint.2013.10.017</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quaint.2013.10.017" target="_blank" >10.1016/j.quaint.2013.10.017</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Sediments of Biśnik Cave (Poland): Lithology and stratigraphy of the Middle Palaeolithic site

Popis výsledku v původním jazyce

Biśnik Cave is an important Palaeolithic site located in the Kraków-Częstochowa Upland. The cave fill is a complex well-stratified sequence composed of 35 layers/sublayers interrupted by number of hiatuses and ranging from Pliocene till modern times. Fifteen Middle Palaeolithic horizons, some of them among the oldest in Poland, represent the most important part of the sequence from an archaeological point of view. The sedimentary sequences in particular parts of the cave have been studied for more than20 years to investigate the chronostratigraphy and palaeoenvironment. The recent multi-proxy study is based on the application of new methods for the site: analysis of sedimentary and post-sedimentary structures, and weathering stage of limestone rubbleand fossil bones, pollen analysis, molecular biomarkers, palaeomagnetic analysis and radiometric dating. Results indicated a more intensive role of re-working and re-deposition in the cave. Older sediments were transported into some strat

Název v anglickém jazyce

Sediments of Biśnik Cave (Poland): Lithology and stratigraphy of the Middle Palaeolithic site

Popis výsledku anglicky

Biśnik Cave is an important Palaeolithic site located in the Kraków-Częstochowa Upland. The cave fill is a complex well-stratified sequence composed of 35 layers/sublayers interrupted by number of hiatuses and ranging from Pliocene till modern times. Fifteen Middle Palaeolithic horizons, some of them among the oldest in Poland, represent the most important part of the sequence from an archaeological point of view. The sedimentary sequences in particular parts of the cave have been studied for more than20 years to investigate the chronostratigraphy and palaeoenvironment. The recent multi-proxy study is based on the application of new methods for the site: analysis of sedimentary and post-sedimentary structures, and weathering stage of limestone rubbleand fossil bones, pollen analysis, molecular biomarkers, palaeomagnetic analysis and radiometric dating. Results indicated a more intensive role of re-working and re-deposition in the cave. Older sediments were transported into some strat

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/IAA300130701" target="_blank" >IAA300130701: Paleomagnetický výzkum krasových sedimentů: paleotektonické a geomorfologické využití</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary International

ISSN

1040-6182

e-ISSN

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Svazek periodika

326/327

Číslo periodika v rámci svazku

April

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

14

Strana od-do

6-19

Kód UT WoS článku

000334095700002

EID výsledku v databázi Scopus

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