第四纪冰期,使许多物种绝灭。
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.
它是第四纪冰川运动幸存下来的珍贵树种。
土壤发育受第四纪冰川影响明显,成土年龄短;
The glacier influence of Quaternary Period affect soil development obviously;
认为本区自晚第四纪以来属于轻微一中度上升地区。
依此对区内晚第四纪的地层及古气候环境进行了初步讨论。
Then a discussion has been done on the stratigraphic division and paleoclimate in this area.
依此对区内晚第四纪的地层及古气候环境进行了初步讨论。
Then a discussion has been done on the stratigraphic division and paleoclimate in this area.
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