2018
Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic
NEJMAN, Ladislav, Lenka LISÁ, Nela DOLÁKOVÁ, Ivan HORÁČEK, Aleš BAJER et. al.Základní údaje
Originální název
Cave deposits as a sedimentary trap for the Marine Isotope Stage 3 environmental record: The case study of Pod Hradem, Czech Republic
Autoři
NEJMAN, Ladislav (203 Česká republika, garant), Lenka LISÁ (203 Česká republika), Nela DOLÁKOVÁ (203 Česká republika, domácí), Ivan HORÁČEK (203 Česká republika), Aleš BAJER (203 Česká republika), Jan NOVÁK (203 Česká republika), Duncan WRIGHT, Marjorie SULLIVAN, Rachel WOOD, R. H. GARGETT, Martina PACHER (40 Rakousko), Sandra SÁZELOVÁ (203 Česká republika, domácí), Miriam NÝVLTOVÁ FIŠÁKOVÁ (203 Česká republika, domácí), Jan ROHOVEC (203 Česká republika) a Miroslav KRÁLÍK (203 Česká republika)
Vydání
Palaeogeography, Palaeoclimatology, Palaeoecology, 2018, 0031-0182
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10600 1.6 Biological sciences
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.616
Kód RIV
RIV/00216224:14310/18:00102406
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000429513500016
Klíčová slova anglicky
Palaeoclimate; Geoarchaeology; Human occupation; Micromorphology; Geochemistry
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 2. 5. 2019 14:14, Mgr. Tereza Miškechová
Anotace
V originále
Pod Hradem Cave, located in the Moravian Karst, Czech Republic, offers an excellent opportunity for environmental reconstructions of Marine Isotope Stage 3 (MIS 3) in Central Europe due to its detailed sedimentary record dated 50,000 to 28,000 cal BP. Identifying the natural environments of the Middle to Upper Palaeolithic (MUP) transition is necessary to understand the settlement strategies and related behaviour of both Neanderthals and Anatomically Modern Humans, both of whom may have occupied the region at the same time. A multidisciplinary excavation was carried out between 2011 and 2016. Detailed analyses of the sediments, vertebrate microfauna, pollen and charcoal revealed minor but observable fluctuations in climate, with little change in the surrounding vegetation. The Pod Hradem palaeoenvironmental dataset is complex, but generally reflects a predominantly glacial climate with a range of vegetation types and habitats during the Late Pleistocene, followed by the warmer and more humid Holocene. The MUP transition as recorded in Pod Hradem Cave was a glacial environment interrupted by two relatively warmer periods. Central Europe experienced extreme climate fluctuations during MIS3, as recorded from different sedimentary archives, but it seems that the Pod Hradem Cave environment may have acted as a buffer zone, ameliorating those extremes, and providing a suitable refuge for both bears seeking winter hibernation dens and occasionally visiting humans.