Planktic carbon and oxygen isotopes and NGR-derived K, U and Th data
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An unusually short glaciation interrupted the warm Pliocene around 3.3 Ma (Marine Isotope Stage (MIS) M2). Different hypotheses exist to explain why this glaciation event was so...
约330万年前，一场异常短暂的冰期打断了温暖的上新世气候，该事件对应海洋同位素阶段（Marine Isotope Stage，缩写MIS）M2。目前存在多种假说，用以解释此次冰期事件为何如此……
