南岭及邻区第四纪地层分区与综合地层格架

史元润; 林晓; 徐亚东; 余舒超; 孙清泉

doi:10.19509/j.cnki.dzkq.2021.0309

南岭及邻区第四纪地层分区与综合地层格架

doi: 10.19509/j.cnki.dzkq.2021.0309

史元润^a,,
林晓^{a, b, ,},
徐亚东^{c, d},
余舒超^a,
孙清泉^a

基金项目:

中国地质调查局项目 DD20190811

国家自然科学基金项目 41571189

详细信息

作者简介:
史元润(1997-), 男, 现正攻读地理学专业硕士学位, 主要从事第四纪地质与环境变化的研究工作。E-mail: syr@cug.edu.cn

通讯作者:
林晓(1980-), 讲师, 主要从事第四纪地质与环境变化的研究工作。E-mail: linxiao@cug.edu.cn

中图分类号: P534.63;P535
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- 被引次数: 0
出版历程
- 收稿日期: 2020-12-21

Quaternary stratigraphic regionalization and comprehensive framework in Nanling and adjacent areas

Shi Yuanrun^a
,,
Lin Xiao^{a, b
, ,},
Xu Yadong^{c, d},
Yu Shuchao^a,
Sun Qingquan^a

摘要

摘要: 南岭及邻区的第四纪沉积以冲积物、残积物和洞穴堆积物为主，长期以来缺乏统一的地层格架和时间框架。基于剖面资料和实地调查，将南岭第四纪地层划分为永州-郴州、桂林-贺州、韶关-清远、赣州、道县-阳山等5个地层小区；通过厘定每个小区的岩石地层序列、生物地层和气候地层及其测年成果，建立了综合地层的对比格架。结果表明，南岭第四系与中国更新统泥河湾阶、周口店阶、萨拉乌苏阶和尚未建阶的全新统可一一对比；其生物地层以早更新世巨猿动物群和中更新世晚期以来的马坝人、道县人和柳江人等智人演化为特点；气候地层以洞穴石笋和高山泥炭重建的古气候记录为代表，主要反映东亚季风背景下的南岭局地气候。但由于测年数据较少，冲积层和残积层的对比仍然存在困难；生物演化阶段与气候变化之间也未能详细对比。因此，今后南岭的第四纪地层研究应围绕提高测年精度与建立统一的年代标尺开展，促进综合地层对比的精细化、延伸气候地层的时间尺度并拓展与南海海相地层的对比；这一基础性工作对水文、环境、工程等实践应用亦具有重要意义。
- 地层分区 /
- 地层对比 /
- 第四纪 /
- 南岭
Abstract: The Quaternary sediments in the Nanling and adjacent areas are dominated by alluvial, eluvium and cave deposits, which have lacked of a unified stratigraphic and chronological framework.Based on the results of field survey and research on profiles, the Quaternary strata of Nanling area has been divided into five stratigraphic minor regions: Yongzhou-Chenzhou, Guilin-Hezhou, Shaoguan-Qingyuan, Ganzhou and Daoxian-Yangshan minor region.Meanwhile, the framework of comprehensive strata determined by the lithostratigraphic sequence, biostratigraphy, chronostratigraphic and climatic data has also been established.The results show that the Quaternary System in Nanling area can be compared with the Nihewan Stage, Zhoukoudian Stage, Sarawusu Stage of Pleistocene Series and the unbuilt stage of Holocene Series in China.Its biostratigraphy is characterized by the Gigantopithecus Fauna of Early Pleistocene and the Homo sapiens such as Maba, Daoxian, Liujiang hominin since the late Middle Pleistocene.The climatic stratigraphy are represented by the glacial-interglacial cycle and the local climatic characters in the background of the East Asian monsoon, which were reconstructed by alpine peat and stalagmites deposited from the late Pleistocene.However, the comparison between alluvial and eluvium remains difficult due to the lack of dating data.There is also no detailed comparison between the biological evolution stages and climatic stages.Therefore, the Quaternary stratigraphic research in Nanling should focus on improving the dating precision and establishing a unified time scale in the future in order to promote the refinement of comprehensive stratigraphy comparison.The comparison between continental sediments and marine strata in the South China Sea should be expanded.And it can be used as the basis of applications in hydrological, environmental and engineering geology in Nanling and adjacent areas.
- stratigraphic regionalization /
- stratigraphic comparison /
- Quaternary /
- Nanling areas

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图 1 南岭及邻区地貌态势与第四纪地层分区

Figure 1. Landform and Quaternary stratigraphic regionalization of Nanling and adjacent areas

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图 2 南岭第四纪地层小区的岩石地层序列

Figure 2. Sedimentary sequence of Quaternary stratigraphic minor regions in Nanling and adjacent areas

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图 3 道县-阳山小区吉田镇社下河阶地实测剖面图

Qh^dl.全新统坡积物; Qh^al.全新统冲积物; Qp^3al.上更新统冲积物; S₃^yγδ.永和岩体

Figure 3. Measured stratigraphic profile and terraces in Shexia River in Jitian Town of Daoxian-Yangshan minor region

下载: 全尺寸图片幻灯片

图 4 南岭中更新世晚期以来的智人化石、文化层及其年代对比(数据来源和文献见表 1)

Figure 4. Comparison of chronology and cultural layers containing Homo sapiens' fossils in Nanling since the middle Pleistocene

下载: 全尺寸图片幻灯片

图 5 南岭泥炭的古气候代用指标及气候变化曲线(数据来源和文献见表 2；YD为新仙女木事件；H为海因里奇事件；B-A为博令-阿诺罗德暖期)

Figure 5. Paleoclimatic proxy indicators and changes reconstructed by environmental proxies of peat in Nanling area

下载: 全尺寸图片幻灯片

图 6 南岭第四纪综合地层对比格架

Figure 6. Comprehensive comparison of Quaternary stratigraphy in Nanling area

下载: 全尺寸图片幻灯片

表 1 南岭的哺乳动物化石地点及年代

Table 1. Original sites and dating value of mammal faunae in Nanling area

地区	地点	年代/ka	测年方法	资料来源
广西桂林	甑皮岩	12.5~7.6	¹⁴C	文献[51]
广东英德	牛栏洞	12~8	¹⁴C	文献[43]
广东英德	青塘洞穴群	20~10	¹⁴C	文献[52]
广西柳州	白莲洞	36~7	¹⁴C	文献[53-54]
广西柳州	通天岩(柳江人)	68	U	文献[55]
湖南永州	道县(道县人)	128~80	U	文献[13]
广东韶关	狮子岩(马坝人)	237~129	U	文献[12, 56]
广西贺州	吊钟岩	210	U	文献[57]
广西柳城	巨猿洞	1 206~940	ESR, U	文献[58]

下载: 导出CSV

表 2 南岭的冲积层、残积层及泥炭的测年

Table 2. Original sites and dating value of alluvium, eluvium and peat in Nanling area

成因类型	地点	测年位置	年龄/ka BP	测年方法	资料来源
冲积层	广东韶关	T₆阶地	819	TL	文献[40]
		T₅阶地	694	TL
		T₃阶地	426	TL
		T₁阶地	206~90.2	¹⁴C
残积层	湖南衡阳	褐黄色土层	2.23×10³~1.11×10³	古地磁	文献[31]
	江西赣州	网纹红土	104~87	ESR	文献[65]
	广西百色	红土中玻璃陨石	803	⁴⁰Ar/³⁹Ar	文献[66]
泥炭层	江西定南	大湖泥炭	16.6	AMS¹⁴C	文献[23, 67]
	湖南城步	古田泥炭	20.7	AMS¹⁴C	文献[25, 26]
	湖南城步	大坪泥炭	15.4	ESR, U	文献[68]
石笋	广西桂林	茅茅头大岩	385~112	²³⁴U/²³⁰Th(α)	文献[69]
		水南洞	229.1~80.7	U/²³⁰Th	文献[38]
		盘龙洞	11.08~0.48	计数定年, U(α)	文献[39]
		丰鱼洞	62.9~4.4	U/²³⁰Th(ICP-MS)	文献[70]
	福建连城	仙云洞	13.32~11.35	U/²³⁰Th(MC)	文献[71]

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