猛犸象在第四纪晚期灭绝了。
晚期(第四纪)为塌陷阶段,造成了贝加尔凹陷的现代构造。
The later stage (Anthropogene) was marked by collapses, which were responsible for the present structure of the Baikal depression.
第四纪早期湖深水淡,晚期湖浅水咸。
In late Quaternary the lake shallowed and its water became salt-water.
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