研究结果表明，前陆盆地内发育有两种层序模式，即构造层序和气候层序。
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
较古老的冰川物质层之间是发育良好的土壤，它含有（生活在）温暖气候中的植物的化石。
Between the older layers of glacial material were well-developed soils containing fossils of warm-climate plants.
气候变化和臭氧层耗减就是其中最明显的例子。
Climate change and the depleted ozone layer are among the starkest examples.
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