长江中下游地区网纹红土中的古气候记录，在第四纪全球变化研究中具有十分重要的意义。
The paleoclimate records of the vermicular red earth in the Middle-Lower Yangtze Region is of great significance to the study of the global changes in Quaternary.
因而许多气候学家使用气候模式进一步研究，发现在古气候记录与轨道参数变化之间具有显著关系；
Thus, many climatologists have made further investigations in terms of climatic models and found significant correlation between paleoclimatic records and orbital parameter variations.
这与华北地区古文史资料记录的古气候变化有较好的一致性，并具有全球变化意义。
Such climatic fluctuations well accord with the historical records and may be of a global significance.
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