PROPERTIES OF THE LOWER PONTIAN IN THE SRBOVO BORE HOLE NEAR NEGOTIN,DACIAN BASIN

The hole was bored through the medium gray Lower Pontian silt with the yellowish sideritic intercalation and dark gray worm boring pack Diff erent sedimentary structures, like silt shadows and fish marks, are pr esent. The chemical, radiometric and other obtained values are in the accordance with the composition of the Earth's crust or close to it. P aradacna abichi, Carinatocongeria digitiferra, Valenciennius and other macrofauna were observed paleoecologicaly. Micropaleontological analy ses completed the sedimentological data Paleoenvironment: sheltered pa rt of basin no islands, on the edge of steady currents coming from sou th-east.