洛川黄土剖面末次冰期晚期以来蜗牛化石类型百分含量数据集（40ka BP以来）
收藏国家地球系统科学数据中心2016-09-02 更新2024-03-04 收录
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资源简介：
通过对黄土高原洛川剖面蜗牛化石记录的研究并结合长武和渭南剖面，探讨末次冰期晚期这一地区气候变化的特点。研究结果表明末次冰期晚期时黄土高原的气候是极不稳定的，其变化趋势与东北太平洋Tanner孔有孔虫含量及GRIP2冰芯氧同位素记录有很好的可比性，从而为探索黄土高原区末次冰期气候不稳定性的原因提供了新的思路。
By analyzing the snail fossil records from the Luochuan Section on the Loess Plateau and combining with the Changwu and Weinan sections, this study investigates the characteristics of regional climate change during the late Last Glacial Period. The results show that the climate of the Loess Plateau was highly unstable during this period, and its change trends have good comparability with the foraminifera content in the Tanner Core of the Northeastern Pacific and the oxygen isotope records from the GRIP2 ice core, thus providing new insights into exploring the causes of climate instability in the Loess Plateau region during the Last Glacial Period.
提供机构：
中科院地球环境研究所
创建时间：
2016-09-02
