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Provenance and paleoclimatic implications of loess deposits in Shandong Province, eastern China

Published online by Cambridge University Press:  13 January 2021

Yongda Wang Open the ORCID record for Yongda Wang [Opens in a new window] ,
Shiling Yang  and
Zhongli Ding
Yongda Wang
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China CAS Center for Excellence in Life and Paleoenvironment, Beijing100044, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China
Shiling Yang*
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China CAS Center for Excellence in Life and Paleoenvironment, Beijing100044, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing100049, China
Zhongli Ding
Affiliation:
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China
*
*Corresponding author at: Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing100029, China. E-mail address: [email protected] (S. Yang).
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Abstract

The loess deposits in Shandong Province in eastern China potentially provide valuable insights into past environmental changes. However, their precise provenance and paleoclimatic implications are unclear. We studied three loess sections located in the piedmont of the Central Shandong Mountains (PCSM) and in an offshore island in Bohai Gulf. Both the glacial loess and interglacial paleosol units are characterized by a coarse grain size, indicating a proximal sediment source. Using the “grain size–transport distance” model established for the Chinese Loess Plateau (CLP), the estimated source-sink distance is ~200–300 km for the PCSM loess and ~100–200 km for the coastal loess. This suggests that fluvial deposits of the Yellow River system in the North China Plain and sediments on the adjacent continental shelf are the major provenance for the Shandong loess. In contrast to the CLP, the Shandong loess does not show a consistent pattern of coarse grain size and low magnetic susceptibility values in glacial loess compared with interglacial paleosols, likely due to frequent changes in dust sources caused by diversions of the Yellow River and local hydroclimatic conditions. Nevertheless, the loess-paleosol alternations in the Shandong loess are a product of global glacial–interglacial cycles.

Keywords

LoessShandong ProvinceOSL datingGrain sizeMagnetic susceptibilityProvenancePaleoclimate
Type
Thematic Set: Eurasian Climate and Environment
Information
Quaternary Research , Volume 103 , September 2021 , pp. 88 - 98
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Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2021

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References

REFERENCES

Aitken, M.J., 1985. Thermoluminescence Dating. Academic Press, London.Google Scholar
An, Z., Kukla, G.J., Porter, S.C., Xiao, J., 1991. Magnetic susceptibility evidence of monsoon variation on the loess plateau of central China during the last 130,000 years. Quaternary Research 36, 29–36.CrossRefGoogle Scholar
Bateman, M.D., Boulter, C.H., Carr, A.S., Frederick, C.D., Peter, D., Wilder, M., 2007. Preserving the palaeoenvironmental record in drylands: Bioturbation and its significance for luminescence-derived chronologies. Sedimentary Geology 195, 5–19.CrossRefGoogle Scholar
Bureau of Geology and Mineral Resources of Shandong Province, 1991. Regional Geology of Shandong Province. [In Chinese.] Geology Press, Beijing.Google Scholar
Cai, G., 1989. The historical dust-fall documents in Shandong Province. [In Chinese.] Journal of Catastrophology 1, 59–63.Google Scholar
Cao, J., Li, P., Shi, N., 1987. Loess of Miaodao islands in Shandong. [In Chinese.] Science in China Series B 17, 1116–1123.Google Scholar
Cao, J., Liu, G., Shi, N., Chang, Y., Song, C., Yuan, H., Guo, X., 1993. Holocene loess of Miaodao islands in Shandong. [In Chinese with English abstract.] Quaternary Sciences 1, 25–33.Google Scholar
Cheng, Z., Fu, M., Ju, X., 1996. Geological significance of paleontological fossils in coastal loess in the Bohai Strait and Liaodong Peninsula. [In Chinese with English abstract.] Marine Geology & Quaternary Geology 16, 85–94.Google Scholar
Cheng, Z., Li, P., Lv, H., Ju, X., 1995. The radiolaia in the coastal loess in East Bohai Sea. [In Chinese with English abstract.] Marine Sciences 6, 59–64.Google Scholar
Chen, J., Li, G., Yang, J., Rao, W., Lu, H., Balsam, W., Ji, J., 2007. Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dust. Geochimica et Cosmochimica Acta 71, 3904–3914.CrossRefGoogle Scholar
Chen, Y., Syvitski, J.P.M., Gao, S., Overeem, I., Kettner, A.J., 2012. Socio-economic impacts on flooding: A 4000-year history of the Yellow River, China. Ambio: A Journal of the Human Environment 41, 682–698.CrossRefGoogle Scholar
Ding, X., Cao, W., Xu, S., Ni, Z., 2015. Characteristics of rare earth elements in Pingyin loess profile, Shandong Province and its implications for provenance. [In Chinese with English abstract.] Journal of Arid Land Resources and Environment 29, 188–192.Google Scholar
Ding, Z., Derbyshire, E., Yang, S., Sun, J., Liu, T., 2005. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution. Earth and Planetary Science Letters 237, 45–55.CrossRefGoogle Scholar
Ding, Z., Derbyshire, E., Yang, S., Yu, Z., Xiong, S., Liu, T., 2002. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea δ18O record. Paleoceanography 17, 5-1–5-21.CrossRefGoogle Scholar
Ding, Z., Rutter, N., Liu, T., 1993. Pedostratigraphy of Chinese loess deposits and climatic cycles in the last 2.5 Myr. Catena 20, 73–91.Google Scholar
Ding, Z., Sun, J., Liu, D., 1999. A sedimentological proxy indicator linking changes in loess and deserts in the Quaternary. Science in China Series D 42, 146–152.CrossRefGoogle Scholar
Ding, Z., Yu, Z., Rutter, N., Liu, T., 1994. Towards an orbital time scale for Chinese loess deposits. Quaternary Science Reviews 13, 39–70.CrossRefGoogle Scholar
Fu, M., Xu, X.S., Cheng, Z., Xu, X.W., 1994. The seasonal desertification-climate environment in the coastal areas of the Yellow Sea and Bohai Sea. [In Chinese with English abstract.] Journal of Desert Research 14, 31–40.Google Scholar
Gao, R., Wang, S., Zhang, X., Song, H., Gao, H., Zang, K., 2008. An analysis of the climatic characteristics of the gale in Bohai Straits. [In Chinese with English abstract.] Marine Forecasts 25, 7–15.Google Scholar
Hanson, P.R., Mason, J.A., Jacobs, P.M., Young, A.R., 2015. Evidence for bioturbation of luminescence signals in eolian sand on upland ridgetops, southeastern Minnesota, USA. Quaternary International 362, 108–115.CrossRefGoogle Scholar
Heller, F., Liu, T., 1984. Magnetism of Chinese loess deposits. Geophysical Journal of the Royal Astronomical Society 77, 125–141.CrossRefGoogle Scholar
Jia, G., Xu, S., Kong, F., Ding, X., 2016. Characteristics and significance of rare earth elements in loess of Shandong region. [In Chinese with English abstract.] Journal of Zaozhuang University 33, 129–134.Google Scholar
Kang, S., Wang, X., Lu, Y., 2013. Quartz OSL chronology and dust accumulation rate changes since the Last Glacial at Weinan on the southeastern Chinese Loess Plateau. Boreas 42, 815–829.Google Scholar
Kong, F., 2018. Fabric characteristics of gravel layer in the loess of the Zhangqiu, Shandong Province. [In Chinese with English abstract.] Master's thesis, Shandong Normal University, Jinan.Google Scholar
Kong, F., Xu, S., Jia, G., 2017. Climatic and environmental evolution with multi-index records of the loess in the Focun, Zibo, Shandong Province. [In Chinese with English abstract.] Journal of Earth Environment 8, 407–418.Google Scholar
Kong, F., Xu, S., Jia, G., 2019. Research progress of gravel layer in Shandong Loess. [In Chinese with English abstract.] Journal of Stratigraphy 43, 81–88.Google Scholar
Li, G., Li, L., Xu, S., Li, X., Chen, J., 2017. Dust source of the loess deposits in the eastern China constrained by uranium comminution age. [In Chinese with English abstract.] Quaternary Sciences 37, 1037–1044.Google Scholar
Li, G., Li, P., Liu, Y., Qiao, L., Ma, Y., Xu, J., Yang, Z., 2014. Sedimentary system response to the global sea level change in the East China Seas since the last glacial maximum. Earth Science Reviews 139, 390–405.CrossRefGoogle Scholar
Li, J., Li, R., Yang, S., Chen, X., Chen, S., 2018. Pollen spore assemblages and induced palaeoenvironmental changes in the western Bohai Sea since Late Pleistocene. [In Chinese with English abstract.] Marine Geology & Quaternary Geology 38, 115–128.Google Scholar
Liu, E., Zhang, Z., Shen, J., 2004. Spore-pollen records of environmental change on south coast plain of Laizhou Bay since the Late Pleistocene. [In Chinese with English abstract.] Journal of Palaeogeography 6, 78–84.Google Scholar
Liu, L., Li, P., Wang, Y., 2000. The grain-size properties and genesis of the loess in central Shandong Province. [In Chinese with English abstract.] Marine Geology & Quaternary Geology 20, 81–86.Google Scholar
Liu, T., 1965. The Loess Deposits in China. [In Chinese.] China Science Press, Beijing.Google Scholar
Liu, T., 1985. Loess and the Environment. China Ocean Press, Beijing.Google Scholar
Liu, Z., Xia, D., 1992. Sedimental characteristics of ancient desert in Bohai Sea. [In Chinese with English abstract.] Acta Sedimentologica Sinica 10, 94–99.Google Scholar
Li, W., Li, Z., Wang, Z., Ma, Z., Wang, Z., Liang, L., 2019. Climatic environment changes during the last interglacial-glacial cycle in Zhifu loess section: Revealed by grain-size end-member algorithm. [In Chinese with English abstract.] Marine Geology & Quaternary Geology 39, 177–187.Google Scholar
Li, W., Zhao, Q., 1981. Preliminary study of the Quaternary sediments in Miaodao Islands. [In Chinese with English abstract.] Marine Sciences 3, 20–22.Google Scholar
Lu, Y., Fang, X., Friedrich, O., Song, C., 2018. Characteristic grain-size component: A useful process-related parameter for grain-size analysis of lacustrine clastics? Quaternary International 479, 90–99.CrossRefGoogle Scholar
Lu, Y., Wang, X., Wintle, A.G., 2007. A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau. Quaternary Research 67, 152–160.CrossRefGoogle Scholar
Lu, Y., Zhang, J., Xie, J., 1988. Thermoluminescence dating of loess and paleosols from the Lantian section, Shaanxi Province, China. Quaternary Science Reviews 7, 245–250.Google Scholar
Miao, X., Hanson, P.R., Wang, H., Young, A.R., 2010. Timing and origin for sand dunes in the Green River Lowland of Illinois, upper Mississippi River Valley, USA. Quaternary Science Reviews 29, 763–773.CrossRefGoogle Scholar
Pearson, H.S., 1928. Chinese fossil Suidae. Palaeontologia Sinica C 5, 1–75.Google Scholar
Peng, S., Hao, Q., Wang, L., Ding, M., Zhang, W., Wang, Y., Guo, Z., 2016. Geochemical and grain-size evidence for the provenance of loess deposits in the Central Shandong Mountains region, northern China. Quaternary Research 85, 290–298.CrossRefGoogle Scholar
Peng, S., Zhu, L., Xiao, G., Qiao, Y., Gao, Z., Chen, D., 2011. Magnetostratigraphy and provenance of the Qingzhou loess in Shandong Province. Journal of Arid Land 3, 184–190.CrossRefGoogle Scholar
Skertchly, S.B.L., 1895. Concerning about loess and other deposits of North China. The Quarterly Journal of the Geological Society of London 51, 11–20.CrossRefGoogle Scholar
Sun, J., 2002. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau. Earth and Planetary Science Letters 203, 845–859.CrossRefGoogle Scholar
Sun, Y., Tada, R., Chen, J., Liu, Q., Toyoda, S., Tani, A., Ji, J., Isozaki, Y., 2008. Tracing the provenance of fine-grained dust deposited on the central Chinese Loess Plateau. Geophysical Research Letters 35, L01804.CrossRefGoogle Scholar
Tian, S., Sun, J., Lü, L., Cao, M., Zhang, Z., Lü, T., 2019. Optically stimulated luminescence dating of late Quaternary loess deposits in the coastal region of North China: Provenance and paleoclimatic implications. Quaternary Science Reviews 218, 160–177.CrossRefGoogle Scholar
Tsakalos, E., Christodoulakis, J., Charalambous, L., 2016. The dose rate calculator (DRc) for luminescence and ESR dating—A java application for dose rate and age determination. Archaeometry 58, 347–352.CrossRefGoogle Scholar
Wang, R., 2005. Northward removal channels of the Huanghe River and prehistoric disaster event: Discussion with Mr. Ren Mei -E. [In Chinese with English abstract.] Scientia Geographica Sinica 25, 294–298.Google Scholar
Wang, X., Lu, Y., Li, X., 2005. Luminescence dating of fine-grained quartz in Chinese loess—Simplified Multiple Aliquot Regenerative-dose (MAR) protocol. [In Chinese with English abstract.] Seismology and Geology 27, 615–622.Google Scholar
Wang, Y., Peng, S., Feng, Z., Zhang, W., Ding, M., 2014. Grain-size characteristics of loess deposits and its implication in the northern piedmont of the central Shandong mountainous region. [In Chinese with English abstract.] Journal of Arid Land Resources and Environment 28, 156–160.Google Scholar
Wu, C., Xu, Q., Yang, X., 2000. Ancient drainage system of the Yellow River on North China Plain. [In Chinese with English abstract.] Journal of Geomechanics 6, 1–9.Google Scholar
Wu, C., Xu, Q., Zhang, X., Ma, Y., 1996. Palaeochannels on the North China Plain: Types and distributions. Geomorphology 18, 5–14.Google Scholar
Xin, L., 2005. Characteristics of the composition of the Zhangxia loess and its origin. [In Chinese with English abstract.] Geology in China 32, 55–61.Google Scholar
Xu, Q., Wu, C., Zhu, X., Yang, X., 1996. Palaeochannels on the North China Plain: Stage division and palaeoenvironments. Geomorphology 18, 15–25.Google Scholar
Xu, S., Ding, X., Yu, L., Ni, Z., 2015. Palaeoclimatic implications of aeolian sediments on the Miaodao Islands, Bohai Sea, East China, based on OSL dating and proxies. Aeolian Research 19, 259–266.CrossRefGoogle Scholar
Xu, S., Kong, F., Jia, G., Miao, X., Ding, X., 2018. An integrated OSL chronology, sedimentology and geochemical approach to loess deposits from Tuoji Island, Shandong Province: Implications for the late quaternary paleoenvironment in East China. Aeolian Research 31, 105–116.CrossRefGoogle Scholar
Xu, S., Ni, Z., Ding, X., 2016. Geochemical characteristics of major elements of the Pingyin loess in Shandong Province. [In Chinese with English abstract.] Bulletin of Mineralogy, Petrology and Geochemistry 35, 353–359.Google Scholar
Yang, S., Ding, Z., 2004. Comparison of particle size characteristics of the Tertiary ‘red clay’ and Pleistocene loess in the Chinese Loess Plateau: Implications for origin and sources of the ‘red clay’. Sedimentology 51, 77–93.CrossRefGoogle Scholar
Yang, S., Ding, Z., 2008. Advance–retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial–interglacial cycles. Earth and Planetary Science Letters 274, 499–510.CrossRefGoogle Scholar
Yang, S., Ding, Z., 2010. Drastic climatic shift at ~2.8 Ma as recorded in eolian deposits of China and its implications for redefining the Pliocene–Pleistocene boundary. Quaternary International 219, 37–44.CrossRefGoogle Scholar
Yang, S., Ding, Z., 2014. A 249 kyr stack of eight loess grain size records from northern China documenting millennial-scale climate variability. Geochemistry, Geophysics, Geosystems 15, 798–814.CrossRefGoogle Scholar
Yang, S., Ding, Z., 2017. Spatial changes in grain size of loess deposits in the Chinese Loess Plateau and implications for paleoenvironment. [In Chinese with English abstract.] Quaternary Sciences 37, 934–944.Google Scholar
Yang, Z., 1936. On the Cenozoic geology of Itu, Changlo and Linchv, Shantung. Bulletin of the Geological Society of China 15, 171–187.Google Scholar
Yan, Y., Sun, Y., Chen, H., Ma, L., 2014. Oxygen isotope signatures of quartz from major Asian dust sources: Implications for changes in the provenance of Chinese Loess. Geochimica et Cosmochimica Acta 139, 399–410.CrossRefGoogle Scholar
Yi, L., Yu, H., Ortiz, J.D., Xu, X., Qiang, X., Huang, H., Shi, X., Deng, C., 2012. A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis. Sedimentary Geology 281, 88–100.CrossRefGoogle Scholar
Zdansky, O., 1925. Fossil Hirsche Chinas. Palaeontologia Sinica C 2, 1–94.Google Scholar
Zhang, Z., Xin, L., Jiang, L., Jiang, L., Huang, P., 2005. Sedimentary characteristics and genetic analysis of Zhangxia Loess in Jinan, Shandong Province. [In Chinese with English abstract.] Journal of Palaeogeography 7, 98–106.Google Scholar
Zhang, Z., Xin, L., Nie, X., 2004. A summary of loessial researches in Shandong. [In Chinese with English abstract.] Scientia Geographica Sinica 24, 746–752.Google Scholar
Zhao, Q., 1996. Re-analysis of microfossils in Miaodao loess, Bohai Sea. [In Chinese.] Science in China Series D 26, 445–451.Google Scholar
Zheng, H., Zhu, Z., Huang, B., Lu, L., 1994. A study on loess geochronology of Shandong Peninsula and northern part of Jiangsu and Anhui Provinces. [In Chinese with English abstract.] Marine Geology & Quaternary Geology 14, 63–68.Google Scholar
Zheng, L., 2018. Provenances of the major loess deposits in eastern China based on Sr and Nd isotopic characteristics. [In Chinese with English abstract.] Geological Journal of China Universities 24, 246–250.Google Scholar