Landscape evolution is an important aspect of global change; it spans the same time-scale as global tectonics, biological evolution, and major climatic change.
景观演化与全球构造、生物演变和主要气候变化具有相同的时间尺度，是长期全球变化的一个重要方面。
The climatic evolution since the late glacial epoch in the Zoigê area reflected by sporopollen records may be well correlated with the global climate change.
孢粉记录所反映的若尔盖地区晚冰期以来的气候演化与全球气候变化具有较好的可比性。
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