(Table T1) Stable oxygen and carbon isotopic composition of benthic foraminif...
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The transition from the late Oligocene warm period into the early Miocene was marked by a series of rapid and brief episodes of cryospheric expansion and global cooling. We...
渐新世（Oligocene）晚期温暖期向中新世（Miocene）早期的过渡，以一系列快速且短暂的冰冻圈（cryospheric）扩张与全球变冷事件为标志。我们……
