Oxygen and Carbon stable isotope ratios for Site U1334
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The Oligocene-Miocene transition (OMT) (~23 Ma) is interpreted as a transient global cooling event, associated with a large-scale Antarctic ice sheet expansion. Here we present...
渐新世-中新世过渡期（Oligocene-Miocene Transition, OMT，约23 Ma）被视作一次短暂的全球变冷事件，与大规模南极冰盖扩张密切相关。本文呈现……
