N. Fiet, BLACK SHALES, A HIGH-RESOLUTION CHRONOLOG ICAL TOOL - CASE-STUDY OF THE ALBIAN FROM THE UMBRIA-MARCHE BASIN (CENTRAL ITALY), Bulletin de la Societe geologique de France, 169(2), 1998, pp. 221-231
An analysis of the cyclostratigraphic potential of black shales is pro
posed from the study of the Albian part of the Marne a Fucoidi Formati
on of the Umbria-Marche basin (Central Italy). The succession, about 6
5 tn thick, is constituted by marl-limestone alternations in which are
intercalated numerous black shales (150). Firstly, the spatial arrang
ement of black shales was studied on an interval approximatively 42 m
thick along a 40 km transect in order to verify the homogeneity of the
succession. Secondly, a cyclostratigraphic approach was applied on th
e temporal distribution of black shales. The genetic significance of b
lack levels was discussed from their petrologic characteristics (miner
alogic, palynologic and geochemical).The depositional model obtained w
as compared with the model of deposition for the Mio-Pliocene sapropel
s of the Mediterranean. A temporal significance of black shales is the
n advanced. A potential use of the spatio-temporal distribution of the
se singular levels in pelagic realm is purposed.