DETERMINING THE DEPOSITIONAL SETTING OF A LIMESTONE UNIT IN BIG BEND RANCH STATE PARK, TEXAS
The absence of any Cenozoic marine units in the region suggests a lacustrine depositional setting for the limestone. The thinness of the unit, the light color (lack of organics) and the lack of variation in the carbonate facies indicates a closed lake. Stromatolites, lime mudstone rip-ups, and oncoids also indicate very shallow conditions. Birdseye structures appear to be of both stromatolite and travertine origin. An ephemeral lake or playa may have been fed by inflow from springs and groundwater seepage which would explain the lack of clastics. The minor amount of clay-sized clastics is likely due to eolian processes. Besides seasonal variations, longer term changes in climate can cause the level of the water table to rise and fall through time causing a lake to form and then revert back to a clastic setting when the water table drops. The lake may have been similar to modern playas in tectonically active areas which contain travertine and grade laterally into alluvial plains or fans.