渐新世(Oligocene)是地质时代中古近纪个最后一个主要分期,大约开始于3400万年前,终于2300万年前,介拉始新世(Eocene)搭新近纪个中新世(Miocene)之间。比起其他比较古老个地质时期,用岩床来确认渐新世比较准确,但精确个起始搭结束辰光仍弗确定。
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