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The Upper Cretaceous Phosphate Formation in the Western Desert of Egypt displays a characteristic facies association that includes marine phosphorites interbedded with black shales and glauconitic sandstones. The upper part of the formation is characterized by the presence of thin phosphatic beds, which are filled-extensively-with disordered and non stoichiometric (mean MgCO3=41.4 +/- 0.34 mol%) authigenic dolomite cement. SEM and the back scattered images of these coarse crystalline dolomite cements reveal that they display planar euhedral crystal boundaries, polymodal crystal size distribution and variable inclusion pattern. The relatively low and wide ranged delta O-18 (-0.87 to -4.15 parts per thousand VPDB) values of the dolomite cements coupled with their depleted Sr (mean= 187 +/- 26 ppm)and high iron and manganese values (mean=6851 554 ppm and 11599 +/- 229 ppm respectively) invoke that they were formed from mixed hypo-saline fluids within a mixing marine-meteoric zone probably during a low stand period at the vicinity of the Maastrichtian/Early Tertiary unconformity. Meanwhile, their negative delta C-13 (-1.31 to -3.56 parts per thousand VPDB) values argue for a possible involvement of isotopically light carbon, derived from degradation of organic matter, during their precipitation. (c) 2007 Elsevier B.V. All rights reserved.