SALINE LAKE DIAGENESIS AS REVEALED BY COUPLED MINERALOGY AND GEOCHEMISTRY OF MULTIPLE ULTRAFINE CLAY PHASES: PLIOCENE OLDUVAI GORGE, TANZANIA

Mineralogical and geochemical analyses of ultrafine (< 0.1 mu m) extracts of Pliocene clays from Olduvai Gorge reveal the complexities of clay diagenesis in saline, alkaline paleo-waters. Multiple authigenic phases are routinely present; these may be distinguished and quantified by decomposition of XRD (060) peaks coupled with geochemical (microprobe, HRTEM-AEM) and crystallographic (IR) investigation. By assigning geochemistry based on XRD results, we identify three principal phases by octahedral composition: dioctahedral Al-rich, dioctahedral relatively Fe-rich, and Mg-rich with a trioctahedral component. Average octahedral formulae are Al-1.30 Fe-0.57 Mg-0.13 (Al-rich), Al-0.56 Fe-0.80 Mg-0.62 (Fe-rich), and Al-0.09 Fe-0.23 Mg-2.09 (Mg-rich) per half formula unit. IR analyses support these octahedral structures. The Mg-rich phase either has coexisting dioctahedral and trioctahedral domains within individual sheets, or a homogeneous octahedral sheet of intermediate composition. This is, to our knowledge, the first report of an intermediate octahedral occupancy in a 2:1 phyllosilicate. HRTEM observations indicate both solid state octahedral and illitization reactions and dissolution-precipitation. Layer charge and interlayer cations suggest that during illitization, layer charge increase was due to interaction with Na-rich brines, but later K uptake may have been with either saline or fresher fluids with higher K/Na ratios. All three phases occur throughout the basin; relative proportions and octahedral compositions vary. Total Mg content of bulk < 0.1 mu m clay fractions, (a paleochemical indicator in this and other basins) is the product of both the relative abundance and the Mg content of the Mg-rich phase. In addition to shedding light on the crystal chemistry of authigenic 2:1 phyllosilicates, these results demonstrate the paleolimnologic importance of discriminating the presence of multiple authigenic clay phases in lacustrine deposits.