15. COUPLED EARLY PLIOCENE-MIDDLE MIOCENE BIO-CYCLOSTRATIGRAPHY OF SITE 1006 REVEALS ORBITALLY INDUCED CYCLICITY PATTERNS OF GREAT BAHAMA BANK CARBONATE PRODUCTION

ABSTRACT

INTRODUCTION

RESULTS: MIDDLE MIOCENE TO EARLY PLIOCENE BIOSTRATIGRAPHY AND CYCLOSTRATIGRAPHY

Planktonic Foraminiferal Events

Nannofossil Events

SEDIMENTATION RATES BASED ON PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHIC EVENTS

EARLY PLIOCENE-MIDDLE MIOCENE CYCLOSTRATIGRAPHY

DISCUSSION AND CONCLUSIONS

ACKNOWLEDGEMENTS

REFERENCES

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