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渐新世／中新世之交有规律的气候波动ＪａｍｅｓＣ．Ｚａｃｈｏｓ等渐新世／中新世之交代表了新生代地球历史中一次有意义的气候变迁，自中—晚渐新世有大量的堆积作用以来，海洋温度缓慢上升大陆冰体积明显降低。氧同位素记录说明了开始于早中新世、持续到中中新世寒冷期...
Regular Climate Fluctuations at the Oligocene / Miocene Cliffs. The Oligocene / Miocene junctions of Zachos represent a significant climate change in the Cenozoic earth history. Since the middle-late Oligoceses accumulated a large amount of accumulation, the ocean temperature slowly increased and the ice volume in the mainland decreased significantly. Oxygen isotope records illustrate the onset of the Early Miocene and the continuation of the Mid-Miocene cold period ...