Podhradem Interstadial. A critical review of the middle and late MIS 3 (Denekamp, Hengelo) in Moravia, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F18%3A00486226" target="_blank" >RIV/67985831:_____/18:00486226 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00094862:_____/18:N0000013

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quascirev.2017.12.024" target="_blank" >http://dx.doi.org/10.1016/j.quascirev.2017.12.024</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quascirev.2017.12.024" target="_blank" >10.1016/j.quascirev.2017.12.024</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Podhradem Interstadial. A critical review of the middle and late MIS 3 (Denekamp, Hengelo) in Moravia, Czech Republic

Popis výsledku v původním jazyce

Knowledge of global climatic fluctuations in the last glacial period has been instrumental for understanding evolution of the landscape and human behavior. Regional environmental responses to these fluctuations are influenced by many factors and their identification at the regional level usually results in local chronostratigraphic schemes. The term Podhradem Interstadial was introduced to the scientific community in 1966 on the basis of the results of an interdisciplinary excavation at Pod Hradem Cave in the Moravian Karst (Czech Republic). Brown soil horizons preserved in the upper part of the section were interpreted as evidence for a warmer period in the last glacial period. The upper part of this soil complex contained fauna remains and lithic artefacts indirectly dated to the time range 28.2–33.3 14C ka BP. Although based on contemporary state of knowledge, the Podhradem Interstadial had no stratigraphic equivalent in loess profiles of former Czechoslovakia and Lower Austria, the term was occasionally used in the European literature. The new interdisciplinary excavations of Pod Hradem Cave (2011–2016) yielded new data, which we use to re-evaluate the concept of the Podhradem Interstadial. In light of the new results, it seems that the original definition of Podhradem Interstadial has a number of problems. It does not fulfill stratigraphic standards and it is evident that the contemporaneous sediments differ lithologically in different parts of the cave. Furthermore, when we take into account the current availability of sophisticated climatostratigraphic schemes for the MIS 3 period, the continuing use of the Podhradem Interstadial should be considered redundant.

Název v anglickém jazyce

Podhradem Interstadial. A critical review of the middle and late MIS 3 (Denekamp, Hengelo) in Moravia, Czech Republic

Popis výsledku anglicky

Knowledge of global climatic fluctuations in the last glacial period has been instrumental for understanding evolution of the landscape and human behavior. Regional environmental responses to these fluctuations are influenced by many factors and their identification at the regional level usually results in local chronostratigraphic schemes. The term Podhradem Interstadial was introduced to the scientific community in 1966 on the basis of the results of an interdisciplinary excavation at Pod Hradem Cave in the Moravian Karst (Czech Republic). Brown soil horizons preserved in the upper part of the section were interpreted as evidence for a warmer period in the last glacial period. The upper part of this soil complex contained fauna remains and lithic artefacts indirectly dated to the time range 28.2–33.3 14C ka BP. Although based on contemporary state of knowledge, the Podhradem Interstadial had no stratigraphic equivalent in loess profiles of former Czechoslovakia and Lower Austria, the term was occasionally used in the European literature. The new interdisciplinary excavations of Pod Hradem Cave (2011–2016) yielded new data, which we use to re-evaluate the concept of the Podhradem Interstadial. In light of the new results, it seems that the original definition of Podhradem Interstadial has a number of problems. It does not fulfill stratigraphic standards and it is evident that the contemporaneous sediments differ lithologically in different parts of the cave. Furthermore, when we take into account the current availability of sophisticated climatostratigraphic schemes for the MIS 3 period, the continuing use of the Podhradem Interstadial should be considered redundant.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10511 - Environmental sciences (social aspects to be 5.7)

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2018

Kód důvěrnosti údajů

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

Název periodika

Quaternary Science Reviews

ISSN

0277-3791

e-ISSN

—

Svazek periodika

182

Číslo periodika v rámci svazku

15 February

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

11

Strana od-do

191-201

Kód UT WoS článku

000425200900015

EID výsledku v databázi Scopus

2-s2.0-85041298012