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Magnetic susceptibility (χ) was measured on more than four hundred samples collected from a five meter high section of fine grained sediments deposited during flood events in the interior of Spiralka Cave. Spiralka Cave is located in the northeastern portion of the Moravian Karst, Czech Republic. In the upper 1.5 meters of this profile, mineral magnetic (χfe, ARM/SIRM, S-ratio, χ(T)) and other nonmagnetic measurements, heavy mineral concentration, loss on ignition and particle grain size) indicate that χ variations are controlled by the concentration of magnetite and by magnetic grain size, i.e. increased magnetic susceptibility results from increased concentration of coarse grained magnetite. A positive correlation with Ti and Zr concentrations in this part of the profile with our magnetic susceptibility record is a detrital signal responding to changing environmental conditions in the catchment area. Furthermore, a comparison of our susceptibility record to the record of winter temperature anomalies constructed from both instrumental and historical

Paleoenvironmental reconstructions from cave sediments of the Moravian Karst, Czech Republic / by Pavel Sroubek.