15. COUPLED EARLY PLIOCENE-MIDDLE MIOCENE BIO-CYCLOSTRATIGRAPHY OF SITE 1006 REVEALS ORBITALLY INDUCED CYCLICITY PATTERNS OF GREAT BAHAMA BANK CARBONATE PRODUCTION
RESULTS: MIDDLE MIOCENE TO EARLY PLIOCENE BIOSTRATIGRAPHY AND CYCLOSTRATIGRAPHY
SEDIMENTATION RATES BASED ON PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHIC EVENTS