Figure F9. Photomicrograph of a fine sand-sized skeletal grainstone with abundant small benthic foraminifers and common fragments of coralline algae, suggesting skeletal particles are derived from a neritic source area (Sample 194-1197B-32R-1, 0-4 cm). Planktonic foraminifers are present and often overgrown by fine dolomitic cements.

Figure F9. Photomicrograph of a fine sand-sized skeletal grainstone with abundant small benthic foraminifers and common fragments of coralline algae, suggesting skeletal particles are derived from a neritic source area (Sample 194-1197B-32R-1, 0-4 cm). Planktonic foraminifers are present and often overgrown by fine dolomitic cements.