Figure 9. Distribution of turbidite constituents deposited during (A) sea-level highstand and (B) sea-level lowstand at Site 1007 (Miocene). Note the higher abundance of deep-water benthic foraminifers (rotaliids), bioclasts, green algae, and red algae during sea-level highstand. The lowstand constituents show a high abundance of ooids, lithoclasts, intraclasts, and mollusks.