Provenance of the Loess in Shandong Province (Eastern China) during the Last Ice Age: Constraints from the U-Pb Age of Detrital Zircons
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摘要: 胶东半岛北部海滨和山东中部山区北麓沉积了典型的风尘黄土，详细记录了晚更新世以来的气候变化，然而有关这些黄土究竟来自哪里，目前仍处于争议之中.锆石是黄土中常见的副矿物，其U-Pb年龄谱对比被广泛用于黄土的物源示踪研究.基于此，利用激光剥蚀电感耦合等离子质谱仪（LA-ICP-MS）对上述地区晚更新世典型的黄土剖面开展碎屑锆石（n=420）微区原位U-Pb年龄分析，结合Kolmogorov-Smirnov统计方法的多维判别图和前人已经发表的研究结果，发现胶东半岛北部海岸和山东中部山地北麓东段的晚更新世黄土主要来自渤海裸露的大陆架和华北平原的碎屑物质，受中国西北内陆干旱区的影响较小，但由于地理位置的差异，山东中部山地北麓西段的晚更新世黄土具有黄河下游和黄土高原的物质信号，而与晚更新世渤海末次冰期裸露在海底的沉积物的物源关系较弱.Abstract: The thick loess-palaeosol sequences in the Jiaodong Peninsula and Central Shandong mountains provide high-resolution records of Late Quaternary climate change of the Shandong Province. However, it is still controversial as to where they came from. This study presents systematically the detrital zircon U-Pb age (n=420) and multi-dimensional discrimination diagram results of statistical method. It is shown that the North China Plain and Bohai shelf material served as a major dust supply for the loess in the Jiaodong Peninsula and eastern parts of the Central Shandong mountains during the Late Pleistocene. By contrast, the major dust source for the loess in the western parts of the Central Shandong mountains is mainly derived from the sediments exposed on the floodplain of the lower reaches of the Yellow River and the Loess Plateau during the Late Pleistocene. They have no provenance relationship with the sediments exposed on the sea floor in the Bohai Sea at the same time.
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Key words:
- Jiaodong Peninsula /
- Central Shandong Mountains /
- loess /
- zircon U-Pb age /
- Quaternary /
- stratigraphy
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图 1 中国主要沙漠、戈壁和黄土位置分布(a)，山东黄土位置分布(b)
底图a修改自Sun et al.（2008）、Nie et al.（2014）和Li et al.（2020b），图中数字1~7（1：Xie and Ding, 2007，Rittner et al., 2016；2：Pullen et al., 2011；3：Zhang et al., 2016；4：Stevens et al., 2010, Nie et al., 2014；5：Gong et al., 2017；6：Xiong et al.，2021；7：Stevens et al., 2010）代表沙漠、戈壁、黄土碎屑锆石采集地，8~11（8：林旭等，2020；9：Yang et al., 2009；10：Yang et al., 2009, Nie et al., 2015；11：Nie et al., 2015）为华北克拉通河流碎屑锆石采样位置；图b中1~3为渤海钻孔锆石数据（1和2：Huang et al., 2020；3：Sun et al., 2020），a~f为渤海钻孔气候数据（Yao et al., 2014, 岳保静等，2020）
Fig. 1. Location distribution of major deserts, gobi and loess in China (a); distribution diagram of loess locations in Shandong Province (b)
图 2 晚更新世以来黄海及其邻近地区海平面变化曲线
图修改自赵希涛等（1979）、岳保静等（2020）
Fig. 2. Curve of sea-level changes of Yellow Sea and adjacent areas since 120 ka
图 3 晚更新世山东黄土及其年龄分布柱状图
芝罘岛结果据黎武标等（2019a）；林格庄结果据徐树建和王涛（2011）；朱里结果据李强（2014）；傅家庄结果据彭淑贞等（2010）；埠西结果据徐树建等（2014）；平阴结果据徐树建等（2016）.张家崖顶剖面采样点年龄通过与其邻近傅家庄剖面进行对比，限定在晚更新世
Fig. 3. Histogram of Shangdong loess in the Late Pleistocene and its age distribution.
图 4 山东黄土锆石CL图像
图中圆圈代表分析点位置
Fig. 4. CL images of zircon grains from the loess of Shandong Province
图 5 山东黄土碎屑锆石U-Pb年龄与Th/U比二维散点图
Fig. 5. Two-dimensional scatter plots of U-Pb age and Th/U ratio of detrital zircons from Shandong Province
图 6 山东黄土碎屑锆石U-Pb年龄频率分布
Fig. 6. U-Pb age frequency distribution map of loess zircons from Shandong Province
图 7 山东黄土和潜在物源区的锆石U-Pb年龄频率分布
a、d、h、j、l、n.本次研究；b. Liu et al.（2013）；c. Sun et al.（2020）；e. 张田和张岳桥（2008）；f. Huang et al.（2020）；g. Zhang et al.（2019）；i、k、m、o.林旭未发表数据；p. Yang et al.（2009）、Nie et al.（2015）；q. Yang et al.（2009）、林旭等（2020）；r. Xie and Ding（2007）、Rittner et al.（2016）；s. Stevens et al.（2010）；t. Zhang et al.（2016）；u. Stevens et al.（2010）；Nie et al.（2014）、Gong et al.（2017）、Xiong et al.（2021）；v. Zhang et al.（2016）；w. Pullen et al.（2011）. 图中黄色、蓝色和红色分别代表黄土剖面、近源区、远源区
Fig. 7. U-Pb age frequency distribution of zircons from the loess and potential provenance regions of the Shandong Province
图 8 山东黄土锆石U-Pb年龄之间的K-S距离MDS图
图中黄色、蓝色和红色分别代表黄土剖面、近源区、远源区
Fig. 8. MDS plot showing the K-S distances between the zircon U-Pb ages of Shandong Province
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