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@article{1413245,
author = {Musil, Rudolf and Děkanovský, Ondřej and Ivanov, Martin and Doláková, Nela and Mrázek, Jan and Juřičková, Lucie and Lundberg, Joyce},
article_location = {Oxford},
article_number = {February},
doi = {http://dx.doi.org/10.1016/j.quaint.2018.03.029},
keywords = {Vertebrates; Micromammals; Molluscs; Palynology; Environmental change; Cromerian interglacials},
language = {eng},
issn = {1040-6182},
journal = {Quaternary International 137},
title = {Dagmar Cave (Czech Republic, Moravian Karst), a unique palaeontological site of the Cromerian Interglacial},
url = {https://www.sciencedirect.com/science/article/pii/S104061821731460X},
volume = {504},
year = {2019}
}
TY - JOUR
ID - 1413245
AU - Musil, Rudolf - Děkanovský, Ondřej - Ivanov, Martin - Doláková, Nela - Mrázek, Jan - Juřičková, Lucie - Lundberg, Joyce
PY - 2019
TI - Dagmar Cave (Czech Republic, Moravian Karst), a unique palaeontological site of the Cromerian Interglacial
JF - Quaternary International 137
VL - 504
IS - February
SP - 56-69
EP - 56-69
PB - Pergamon Press
SN - 10406182
KW - Vertebrates
KW - Micromammals
KW - Molluscs
KW - Palynology
KW - Environmental change
KW - Cromerian interglacials
UR - https://www.sciencedirect.com/science/article/pii/S104061821731460X
L2 - https://www.sciencedirect.com/science/article/pii/S104061821731460X
N2 - Dagmar Cave, Czech Republic, is the first locality in the Moravian Karst where sediments of Cromerian age have been discovered and it is the first locality with such a large number of species of molluscs of this age. It was originally a swallow hole initiated in the Neogene, which has since accumulated sediments. Basal sediments are palaeontologically-sterile stream boulders, originating from weathered Lower Carboniferous rock. After this, fossiliferous, loamy sediments were carried in from the entrance by streams and/or gravity. Molluscan and vertebrate assemblages, along with palynological remains, are indicative of interglacial conditions. Faunal analysis determined that this could only consist of one interglacial, either Cromerian III or IV. This is the first record of Middle Pleistocene molluscan fauna in the Moravian Karst. Palynology demonstrated a humid and thermophilic vegetation typical of a Cromerian interglacial, with forest, and probably water, and an open grassy/bushy area close to the cave. The age is constrained by a MIS 7 U-Th date (182 ka) on the calcite flowstone that overlies the interglacial material and underlies the palaeontologically more sterile upper sediments.
ER -
MUSIL, Rudolf, Ondřej DĚKANOVSKÝ, Martin IVANOV, Nela DOLÁKOVÁ, Jan MRÁZEK, Lucie JUŘIČKOVÁ a Joyce LUNDBERG. Dagmar Cave (Czech Republic, Moravian Karst), a unique palaeontological site of the Cromerian Interglacial. \textit{Quaternary International 137}. Oxford: Pergamon Press, 2019, roč.~504, February, s.~56-69. ISSN~1040-6182. Dostupné z: https://dx.doi.org/10.1016/j.quaint.2018.03.029.
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