The date of the section bottom is 3.71±0.38ka BP, which indicates that the section is middle and late holocene horizon.
剖面底部年龄为3.71±0.38ka BP,表明该剖面覆盖了中全新世晚期及晚全新世以来的沉积地层。
参考来源 - 塔克尔莫乎尔沙漠晚全新世环境演变研究·2,447,543篇论文数据，部分数据来源于NoteExpress
最暖期不是在中全新世，而是在晚全新世。
The warmest stage was not in Middle Holocene but in Late Holocene.
晚全新世植被为森林草原或疏林草原，气候干旱偏暖—温凉干旱。
The vegetation of the middle Holocene was forest grassland and aciculignosa and aeslilignosa grassland, and the climate was warm and wet.
研究结果表明，所研究的柱样沉积物下部形成于中全新世晚期，上部属于晚全新世。
The results show that the core sediments studied were formed in the late stage of Middle Holocene for the lower part and in Late Holocene for the upper part.
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