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

ABSTRACT

INTRODUCTION

METHODOLOGY

RESULTS

DISCUSSION

Proxy Validation

Theoretical Lysocline Shoaling Model

Significance of Pyrite and the Benthic Foraminiferal Extinction

CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

CHAPTER NOTE

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