T. Minster et al., MANGANESE AS AN INDICATOR OF THE INTENSITY OF ANOXIA DURING THE DEPOSITION OF THE SENONIAN OIL SHALES IN THE NEGEV, ISRAEL, Gorucie slancy, 14(1), 1997, pp. 5-18
The geochemical relationship of Mn to organic cai bon, il on and alumi
na was studied in Early Maastrichtian oil shales of southern Israel. T
he Mn concentration appeals to mirror the intensity of anoxia in the b
ottom waters of the depositional basin. If is proposed that the genera
l trend of increasing Mn stratigraphically upward through the organic-
rich sequence is a reflection of fluctuating redox conditions during t
he transition fr om an anoxic to a more oxidizing regime.