ABSTRACT

INTRODUCTION

CONSTRAINTS ON THE ORIGIN OF SHATSKY RISE

Cretaceous Oceanic Anoxic Events: Production of Highly Organic Rich Horizons

Late Cretaceous and Paleogene Deepwater Circulation: Identifying Switches in Source Regions

New Interpretations for Extinction Events at the Cretaceous/Tertiary Boundary

Paleocene/Eocene Thermal Maximum on Shatsky Rise: Biotic, Climatic, and Oceanographic Signatures

Abrupt Warming Events: "Hyperthermals" in the Paleogene

Neogene

ACKNOWLEDGMENTS

REFERENCES

CHAPTER NOTES

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