SROVNÁVACÍ STUDIE POVRCHU KŘEMENNÝCH ZRN NA LOKALITÁCH JIŽNÍ A JIHOVÝCHODNÍ MORAVY
Roč.23,č.1-2(2016)
Between 2013–2014, archeological researches at the Mikulčice site were performed. During these researches, necessity of a quartz grains surface study in the Moravian Sahara arose. There is a significant archaeological monument situated near the village of Mikulčice – a Slavic settlement, whose youngest bedrock is formed by fluvial sediments of extinct riverarms of the river Morava, and sand dunes composed of wind-blown sands of the Moravian Sahara. On these sand dunes, the most important churches and palaces of the settlement are found. The sandy sediments can reach up to 30 m thickness in the area of the Moravian Sahara.
Samples of sandy sediments were taken from several locations of this site, and also from several other sites of south Moravia, which are sedimentary genetically different from the studied area. One sample of aeolian sand from the desert Rub-al Khali of Arabian Peninsula was provided for comparison.
After gathering this small collection of sand grain samples, they were individually modified to the required study form and analyzed according to the demands of the method of exoscopy. At first, one hundred quartzgrains were separated from each sample of the collection using a stereo microscope. After that a detailed study and imaging with the scanning electronmicroscope (SEM) followed.
The collection of sands from Mikulčice of the same genetical origin was compared to other samples of genetically known origin (fluvial, eolian...). The final comparison of all samples was performed by the method of multivariate analysis with NMDS. The results show that development of sediments at the archeological site Mikulčice most probably took place in very similar sedimentary environment. In this environment, the eolian transport and the fluvial transport with lower kinetic energy played important role.
Mikulčice; Eolian Sediments; Fluvial Sediments; Exoscopy; SEM; NMDS
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