湖泊碳酸盐在过去环境变化研究中的应用

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国内外的研究成果表明,湖泊沉积碳酸盐矿物及其微量元素、同位素分布特征记录了全球或区域古气候环境演变历史,可以从中提取大量定量化的古气候参数。因此,可以根据湖泊碳酸盐矿物的含量和碳、氧同位素变化等信息推知其形成时期的气候环境,重建古环境,揭示气候环境演变的规律。湖泊碳酸盐是一种研究古环境演化重要的代用指标,在过去气候环境变化研究中有广阔的应用前景。

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语种: 中文   

基金中国科学院知识创新重要方向项目(KZCX2-SW-118)

关键词湖泊碳酸盐 碳、氧同位素 古气候 古湖泊环境


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