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Summarizes much of the geologic, paleoecologic, and oceanographic evidence for global environmental and climactic changes during the last 18,000 years.
Traces the evolution of the global climate since the last period of glacial maximum approximately 18,000 years ago. Examines how changes in climate have transformed Earth's biomes in this period and how this change has influenced the evolution of life.
Summarizes much of the geologic, paleoecologic, and oceanographic evidence for global environmental and climactic changes during the last 18,000 years.