11. Abundance Variations of Planktonic Foraminifers during the Mid-Pleistocene Climate Transition at ODP Site 1144, Northern South China Sea
ABSTRACT
INTRODUCTION
MATERIAL AND METHODS
RESULTS
DISCUSSION
Glacial–Interglacial Faunal Contrasts during the Mid-Pleistocene Transition
Upper Water Stratification and Thermocline
Astronomically Forcing Faunal Responses to Climate Change
Comparison between Northern and Southern South China Sea Records
SUMMARY
ACKNOWLEDGMENTS
REFERENCES
APPENDIX
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