作者: Joyce Lundberg , Rudolf Musil , Martin Sabol
DOI: 10.1016/J.QUAINT.2013.04.006
关键词: Biostratigraphy 、 Geology 、 Marine Isotope Stage 11 、 Palynology 、 Paleontology 、 Pleistocene 、 Ursus deningeri 、 Archaeology 、 Holocene 、 Interglacial 、 Cave
摘要: Za Hajovnou Cave in the Javoricko Karst (Moravia, Czech Republic) has a rich record of Middle Pleistocene, typical Holsteinian, flora and fauna dominated by bear Ursus deningeri. Sedimentological, geochemical, mineralogical, geophysical, palynological zoopalaeontological analyses sediments along with U-Th dating flowstones place deposits into a numerical timeframe. The cave origin dates to period before the mid-Miocene Badenian transgression. oldest (fluvial) deposits are Lower spanning Brunhes/Matuyama boundary. later (terrestrial) range from Middle Pleistocene Holocene. most important result U-Th dating is that main (Holsteinian senso lato) fossil bed can be correlated MIS 9. lower probably MIS 11, upper 5e. This represents one the still-relatively-few numerically dated Holsteinian sites, contradicts Global Chronostratigraphical Correlation Table that places only 11, supports the concept not single unit likely not confined interglacial. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.