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Cosmic microspheres in the Carboniferous deposits of the Usolka section (Urals foredeep)
Authors:RKh Sungatullin  GM Sungatullina  MI Zakirov  VA Tsel’movich  MS Glukhov  AI Bakhtin  YuN Osin  VV Vorob’ev
Institution:1. Kazan Federal University, ul. Kremlevskaya 18, Kazan, 420008, Russia;2. Borok Geophysical Observatory of the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, 142, Borok Village, Yaroslavl, Region, 152742, Russia
Abstract:Magnetite microspheres from the Carboniferous deposits of the Usolka reference section were studied by probe microanalysis, with comparison of the distributions of chemical elements and microspheres. The presence of microspheres in sedimentary strata is considered to be an additional factor for stratigraphic correlation between sedimentary sections. The microspheres are shown to be of cosmic nature. The Late Paleozoic paleoclimatic changes (extreme cooling) and biotic crises were caused by the periodical Solar System motion in the Galaxy, cosmic-dust fallout, and meteorite bombardments of the Earth.
Keywords:Carboniferous  cosmic bombardment  magnetite microspheres  chemical composition  paleoclimate  Urals foredeep
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