TRANSITION OF THE BOUSE FORMATION FROM A MARINE ESTUARY TO SALINE LAKE IN THE LATE MIOCENE TO EARLY PLIOCENE
Paleoecology of the bioclastic Bouse Formation in the Blythe basin based on foraminifer analysis suggests deposition in a marine estuary. Five foraminiferal biofacies are recognized which document: a transition from nearshore low-energy wave-dominated shallow marine environment (Buliminella and Elphidium biofacies), to neritic depths in a well-oxygenated water mass with normal to slightly brackish salinities (Rosalina biofacies), to neritic depths but with decreased oxygen conditions and a restricted marine connection (Streptochilus biofacies), and a final transition to a siliclastic saline lake (Ammonia biofacies). Isotope values in the bioclastic member suggest deposition in a marine estuary thus supporting the interpretation based on foraminifers. The transition to a saline lake marked by the DCL may represent the breaching of the paleodam, followed by a decline in salinity, reduction of the foraminiferal faunas to a single, low salinity tolerate species, an increase in continental ostracodes, and a decline in isotope values.
The Bouse Formation in the San Luis and Fortuna basins and the Imperial Formation in the Salton Trough record a similar ecological transition as low salinity water was released after breaching the paleodam at the southern end of the Blythe basin in the early Pliocene.