Record details

Title
    A Late Pleistocene palaeoclimate record based on mineral magnetic properties of the entrance facies sediments of Kulna Cave, Czech Republic
Author
    Diehl, J. F.
    Kadlec, Jaroslav
    Šroubek, P.
    Valoch, K.
Language
    anglicky
Publication type
    článek v odborném periodiku
Source title - serial
    Geophysical Journal International
Vol./nr.
    Roč. 147, č. 2
Pages
    s. 247-262
Year
    2001
Notes
    Projekt: 95051, Czech/US Jouint Board for Science and Technology, XX
    Projekt: EAR-9705718, National Science Foundation, US
    Projekt: INT-9507137, National Science Foundation, US
    Rozsah: 16 s.
    Výzkumný záměr: CEZ:AV0Z3013912
Subject category
    Kulna Cave
    Moravian Karst
    Pleistocene
Keyword
    Based
    Cave
    Czech
    Entrance
    Facies
    Kulna
    Late
    Magnetic
    Mineral
    Palaeoclimate
    Pleistocene
    Properties
    Record
    Republic
    Sediments
Abstract (in english)
   Kulna Cave is located in the Moravian Karst. The entrance facies sediments in the cave consist of interbedded layers of silts (loess) and clay-rich silts (loam) that were either directly blown into the cave entrance or redeposited in the cave by slope processes during the Last Glacial Stage. Magnetic susceptibility was measured on approximately 700 samples. The Kulna pedogenic susceptibility record shows variations on both long and short timescales. The long-term trends are in good agreement with the deep-sea SPECMAP record.
Contributor
    AV ČR Brno, Geologický ústav
Contributor code
    AV ČR, GLÚ
Source format
    U
Import date
    8. 8. 2012