Based on observations from seven measured stratigraphic sections and 230 thin sections over 37.3 kilometers, we recognize two sequences that encompass six parasquences and six distinct facies. The facies include bioturbated peloidal packstones, containing ostracods, rare occurrences of planar laminations, plane tabular cross bedding, microbial laminations and fine grain silt and sand. This facies is inferred to have been deposited in a semi-restricted...