8. Evidence for Lysocline Shoaling at the Paleocene/Eocene Thermal Maximum on Shatsky Rise, Northwest Pacific

ABSTRACT

INTRODUCTION

METHODOLOGY

RESULTS

Stable Isotope Ratios

Weight Percent Coarse Fraction

Weight Percent Calcium Carbonate

Foraminiferal Fragmentation

Benthic/Planktonic Ratios

Percent Pyrite

Percent Fish Debris

Preservational Survey

DISCUSSION

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

CHAPTER NOTE

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