A 5 million year reconstruction of sea level, temperature, and sea water δ¹⁸O
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Marine sediment records from the Oligocene and Miocene reveal clear 400,000-year (400-kyr) climate cycles related to variations in orbital eccentricity. These cycles are also...
渐新世（Oligocene）与中新世（Miocene）的海洋沉积记录清晰揭示出与轨道偏心率变化相关的40万年（400-kyr）气候周期。这些周期亦……
