The intial cement appears to be isopachus marine rims. This underwent diagenesis and was superimposed on by meniscus spar cements related to evaporation of freshwater charged with dissolved aragonite within these marine sediments. These grains formed on an exposed carbonate shelf and were transported by waves to their current postion in a now uplifted Pleistocene beach. The aragonite ooids have concentric layering of cortex about bioclasts and micritized peloid nulceae (some after ooids). Botryoidal grains are transported grapestones that form nucleae and are enclosed by aragonite ooid coating. Darkened spots within ooid layers are cyanobacteria colonies that cause local micritization.