
The platform comprises three accommodation cycles in which each subsequent cycle experienced progressively greater influence of a long-term accommodation increase. Aggradation and progradation during the first cycle produced a flat, sheet-like platform. The coarsening and shallowing-upward sequence representing this first cycle is dominated by columnar stromatolitic thrombolites grading into massive and cross-bedded dolostones.
The second cycle features aggradation, formation of a distinct margin, and the development of a bucket geometry. The margin contained thrombolitic mounds and domes whereas the platform interior was dominated by columnar stromatolitic thrombolites. The final stage of platform development showed a deepening trend with initial aggradation and formation of well-bedded, thin deposits in the interior and mounds at the margins.

The overall geometric evolution of the platform from flat-topped to bucket with elevated margins is recorded in many Proterozoic and Phanerozoic isolated carbonate platforms. This study clearly illustrates that accommodation changes were fundamentally important to development of microbial-dominated carbonate platforms before the dawn of metazoan-dominated platforms.