在干旱半干旱地区，封闭湖泊的湖水盐度对气候变化反应敏感。
The salinity of lake water is a sensitive monitor of climate in arid and semiarid region.
湖泊纹泥和湖相页岩主要沉积于湖水明显分层的条件下，湖水的分层受气候、盐度、水体深度等多方面的控制。
Lacustrine laminae are mainly deposited in lake water with obvious layering. Such factors as temperature, salinity and depth control the water layering.
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