CHENYingying ，QIN Lin，LI Ruijie，et al. Paleohydrological variations revealed from the TMZ05 Borehole in the Qiantao Basin of the Yellow River[J]. Marine Geology & Quaternary Geology，xxxx，x(x)： x-xx. DOI: 10.16562/j.cnki.0256-1492.2025030301
Citation: CHENYingying ，QIN Lin，LI Ruijie，et al. Paleohydrological variations revealed from the TMZ05 Borehole in the Qiantao Basin of the Yellow River[J]. Marine Geology & Quaternary Geology，xxxx，x(x)： x-xx. DOI: 10.16562/j.cnki.0256-1492.2025030301
shu

Paleohydrological variations revealed from the TMZ05 Borehole in the Qiantao Basin of the Yellow River

  • 1.

    Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China

  • 2.

    Shiyang River Basin Scientific Observing Station, Gansu Province, Wuwei 733000, China

  • 3.

    Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China

  • 4.

    College of Resources and Environment, Gansu Agricultural University, Lanzhou 730070, China

More Information
  • Received Date: March 02, 2025
  • Revised Date: March 25, 2025
  • Accepted Date: March 25, 2025
  • Available Online: May 13, 2025
    Graphical Abstract
    • Abstract

  • Paleohydrology serves as a critical historical reference for studying and assessing flood risks in river basins. We analyzed a ～19 m deep borehole core (TMZ05) from Tumote Right Banner in the Qiantao Basin of the Yellow River and reconstructed the paleohydrological evolution over the past 19 ka using sediment grain size and geochemical proxies, including the grain-size U value (U=p(16～80 μm) / p(2～16 μm), flood energy index (FEI=(pEM4+pEM5)/(pEM3+pEM4+pEM5)) from grain size end-member components, and ln(Zr/Rb) values. Optically stimulated luminescence (OSL) and accelerator mass spectrometry (AMS) 14C dating were applied to establish the chronological framework. Results reveal that since the Last Glacial Maximum (LGM), the frequency and magnitude of paleohydrological events in the region have been generally decreased but exhibited distinct phases. Periods of 18.5～14 ka and 8.5～6 ka were characterized by low-frequency and low-amplitude fluctuations, while 14～8.5 ka showed intense high-frequency and high-amplitude hydrological variability. After 6 ka, both the intensity and variability of paleohydrology were gradually increased. Furthermore, five high-frequency and high-amplitude paleohydrological phases: 19～16.5 ka, 14～11.7 ka, 11～9.7 ka, 9.4～8.5 ka, and 4.2～1.6 ka indicated by high-resolution proxies (FEI and ln(Zr/Rb)), during which catastrophic flood events occurred frequently in the Yellow River Basin. Regional paleoenvironmental comparisons indicate that these high-frequency and high-amplitude hydrological phases corresponded to intensified flood disasters, and occurred mainly during the transitional periods of climate system, implying that the instability in hydroclimatic regime could seriously disrupt the equilibrium of fluvial morphology.

    • FullText(HTML)
    • References (61)
  • [1]
    Benito G, Macklin M G, Panin A, et al. Recurring flood distribution patterns related to short-term Holocene climatic variability[J]. Scientific Reports, 2015, 5(1):16398. doi: 10.1038/srep16398
    [2]
    Wilhelm B, Rapuc W, Amann B, et al. Impact of warmer climate periods on flood hazard in the European Alps[J]. Nature Geoscience, 2022, 15(2):118-123. doi: 10.1038/s41561-021-00878-y
    [3]
    Gregory K J, Benito G, Dikau R, et al. Past hydrological events related to understanding global change: an ICSU research project[J]. CATENA, 2006, 66(1-2):2-13. doi: 10.1016/j.catena.2005.11.011
    [4]
    Hudson P F, Colditz R R. Flood delineation in a large and complex alluvial valley, lower Pánuco basin, Mexico[J]. Journal of Hydrology, 2003, 280(1-4):229-245. doi: 10.1016/S0022-1694(03)00227-0
    [5]
    张鹏, 杨劲松, 赵华, 等. 黄河流域全新世古洪水研究进展及展望[J]. 海洋地质与第四纪地质, 2020, 40(6):178-188

    ZHANG Peng, YANG Jinsong, ZHAO Hua, et al. Research progress of the Holocene paleoflood in the Yellow River basin and a future prospect[J]. Marine Geology & Quaternary Geology, 2020, 40(6):178-188.]
    [6]
    Baker V R, Benito G, Brown A G, et al. Fluvial palaeohydrology in the 21st century and beyond[J]. Earth Surface Processes and Landforms, 2022, 47(1):58-81. doi: 10.1002/esp.5275
    [7]
    Toonen W H J, Winkels T G, Cohen K M, et al. Lower Rhine historical flood magnitudes of the last 450 years reproduced from grain-size measurements of flood deposits using End Member Modelling[J]. CATENA, 2015, 130:69-81. doi: 10.1016/j.catena.2014.12.004
    [8]
    Blöschl G, Hall J, Parajka J, et al. Changing climate shifts timing of European floods[J]. Science, 2017, 357(6351):588-590. doi: 10.1126/science.aan2506
    [9]
    Harden T, Macklin M G, Baker V R. Holocene flood histories in south-western USA[J]. Earth Surface Processes and Landforms, 2010, 35(6):707-716. doi: 10.1002/esp.1983
    [10]
    Munoz S E, Giosan L, Therrell M D, et al. Climatic control of Mississippi River flood hazard amplified by river engineering[J]. Nature, 2018, 556(7699):95-98. doi: 10.1038/nature26145
    [11]
    Camuera J, Ramos-Román M J, Jiménez-Moreno G, et al. Past 200 kyr hydroclimate variability in the western Mediterranean and its connection to the African Humid Periods[J]. Scientific Reports, 2022, 12(1):9050. doi: 10.1038/s41598-022-12047-1
    [12]
    Huang C C, Pang J L, Zha X C, et al. Extraordinary floods related to the climatic event at 4200 a BP on the Qishuihe River, middle reaches of the Yellow River, China[J]. Quaternary Science Reviews, 2011, 30(3-4):460-468. doi: 10.1016/j.quascirev.2010.12.007
    [13]
    Zhang Y Z, Huang C C, Pang J L, et al. Holocene palaeoflood events recorded by slackwater deposits along the middle Beiluohe River valley, middle Yellow River basin, China[J]. Boreas, 2015, 44(1):127-138. doi: 10.1111/bor.12095
    [14]
    Chen Y L, Huang C C, Zhang Y Z, et al. Palaeoflood events during the last deglaciation in the Yellow River source area on the northeast Tibetan Plateau[J]. Geological Journal, 2021, 56(8):4293-4309. doi: 10.1002/gj.4164
    [15]
    Yu S Y, Hou Z F, Chen X X, et al. Extreme flooding of the lower Yellow River near the Northgrippian-Meghalayan boundary: evidence from the Shilipu archaeological site in southwestern Shandong Province, China[J]. Geomorphology, 2020, 350:106878. doi: 10.1016/j.geomorph.2019.106878
    [16]
    Li T, Li J B, Zhang D D. Yellow River flooding during the past two millennia from historical documents[J]. Progress in Physical Geography: Earth and Environment, 2020, 44(5):661-678. doi: 10.1177/0309133319899821
    [17]
    Mackin J H. Concept of the graded river[J]. GSA Bulletin, 1948, 59(5):463-512. doi: 10.1130/0016-7606(1948)59[463:COTGR]2.0.CO;2
    [18]
    Aalto R, Lauer J W, Dietrich W E. Spatial and temporal dynamics of sediment accumulation and exchange along Strickland River floodplains(Papua New Guinea) over decadal‐to‐centennial timescales[J]. Journal of Geophysical Research: Earth Surface, 2008, 113(F1):F01S04.
    [19]
    Repasch M, Wittmann H, Scheingross J S, et al. Sediment transit time and floodplain storage dynamics in alluvial rivers revealed by meteoric 10Be[J]. Journal of Geophysical Research: Earth Surface, 2020, 125(7):e2019JF005419. doi: 10.1029/2019JF005419
    [20]
    Huffman M E, Pizzuto J E, Trampush S M, et al. Floodplain sediment storage timescales of the laterally confined meandering Powder River, USA[J]. Journal of Geophysical Research: Earth Surface, 2022, 127(1):e2021JF006313. doi: 10.1029/2021JF006313
    [21]
    师长兴. 黄河上游内蒙古段河床演变及其与水沙变化的关系[J]. 地理科学, 2016, 36(6):895-901

    SHI Changxing. Channel adjustments of the Inner Mongolia reach of the upper Huanghe River to changes in water discharge and sediment load[J]. Scientia Geographica Sinica, 2016, 36(6):895-901.]
    [22]
    国家地震局. 鄂尔多斯周缘活动断裂系[M]. 北京: 地震出版社, 1988: 39-71

    China Earthquake Administration. Active Fault System Around Ordos Massif[M]. Beijing: Seismological Press, 1988: 39-71.]
    [23]
    许炯心. 异源水沙对黄河上游兰州至头道拐河段悬移质泥沙冲淤的影响[J]. 泥沙研究, 2014(5):1-10

    XU Jiongxin. Channel sedimentation in the Lanzhou–Toudaoguai reach of the upper Yellow River influenced by runoff and sediment from different source areas[J]. Journal of Sediment Research, 2014(5):1-10.]
    [24]
    Konert M, Vandenberghe J. Comparison of laser grain size analysis with pipette and sieve analysis: a solution for the underestimation of the clay fraction[J]. Sedimentology, 1997, 44(3):523-535. doi: 10.1046/j.1365-3091.1997.d01-38.x
    [25]
    Wentworth C K. A scale of grade and class terms for clastic sediments[J]. The Journal of Geology, 1922, 30(5):377-392. doi: 10.1086/622910
    [26]
    Folk R L, Ward W C. Brazos River bar: a study in the significance of grain size parameters[J]. Journal of Sedimentary Petrology, 1957, 27(1):3-26. doi: 10.1306/74D70646-2B21-11D7-8648000102C1865D
    [27]
    Li F Q, Pan B T, Lai Z P, et al. Identifying the degree of luminescence signal bleaching in fluvial sediments from the Inner Mongolian reaches of the Yellow River[J]. Geochronometria, 2018, 45(1):82-96. doi: 10.1515/geochr-2015-0087
    [28]
    Maizels J K. Palaeovelocity and palaeodischarge determination for coarse gravel deposits[M]//Gregory K J. Background to Palaeohydrology: A Perspective. New York: Wiley, 1983: 101-139.
    [29]
    Wang H, Jia X, Li Y, et al. Selective deposition response to aeolian–fluvial sediment supply in the desert braided channel of the upper Yellow River, China[J]. Natural Hazards and Earth System Sciences, 2015, 15(9):1955-1962. doi: 10.5194/nhess-15-1955-2015
    [30]
    Paterson G A, Heslop D. New methods for unmixing sediment grain size data[J]. Geochemistry, Geophysics, Geosystems, 2015, 16(12):4494-4506. doi: 10.1002/2015GC006070
    [31]
    Weltje G J. End-member modeling of compositional data: numerical-statistical algorithms for solving the explicit mixing problem[J]. Mathematical Geology, 1997, 29(4):503-549. doi: 10.1007/BF02775085
    [32]
    Parris A S, Bierman P R, Noren A J, et al. Holocene paleostorms identified by particle size signatures in lake sediments from the northeastern United States[J]. Journal of Paleolimnology, 2010, 43(1):29-49. doi: 10.1007/s10933-009-9311-1
    [33]
    Weltje G J, Prins M A. Genetically meaningful decomposition of grain-size distributions[J]. Sedimentary Geology, 2007, 202(3):409-424. doi: 10.1016/j.sedgeo.2007.03.007
    [34]
    Peng F, Prins M A, Kasse C, et al. An improved method for paleoflood reconstruction and flooding phase identification, applied to the Meuse River in the Netherlands[J]. Global and Planetary Change, 2019, 177:213-224. doi: 10.1016/j.gloplacha.2019.04.006
    [35]
    Peng F, van Balen R, Beets C, et al. Rapid flood intensification and environmental response of the Lower Meuse during the Allerød-Younger Dryas climate transition[J]. Geomorphology, 2021, 372:107469. doi: 10.1016/j.geomorph.2020.107469
    [36]
    Jones A F, Macklin M G, Brewer P A. A geochemical record of flooding on the upper River Severn, UK, during the last 3750 years[J]. Geomorphology, 2012, 179:89-105. doi: 10.1016/j.geomorph.2012.08.003
    [37]
    Schulte L, Peña J C, Carvalho F, et al. A 2600-year history of floods in the Bernese Alps, Switzerland: frequencies, mechanisms and climate forcing[J]. Hydrology and Earth System Sciences, 2015, 19(7):3047-3072. doi: 10.5194/hess-19-3047-2015
    [38]
    Richter T O, van der Gaast S, Koster B, et al. The Avaatech XRF Core Scanner: technical description and applications to NE Atlantic sediments[J]. Geological Society, London, Special Publications, 2006, 267(1):39-50. doi: 10.1144/GSL.SP.2006.267.01.03
    [39]
    Berner Z A, Bleeck-Schmidt S, Stüben D, et al. Floodplain deposits: a geochemical archive of flood history – A case study on the River Rhine, Germany[J]. Applied Geochemistry, 2012, 27(3):543-561. doi: 10.1016/j.apgeochem.2011.12.007
    [40]
    Chen J, Chen Y, Liu L W, et al. Zr/Rb ratio in the Chinese loess sequences and its implication for changes in the East Asian winter monsoon strength[J]. Geochimica et Cosmochimica Acta, 2006, 70(6):1471-1482. doi: 10.1016/j.gca.2005.11.029
    [41]
    Fuller I C, Macklin M G, Toonen W H J, et al. A 2000 year record of palaeofloods in a volcanically-reset catchment: Whanganui River, New Zealand[J]. Global and Planetary Change, 2019, 181:102981. doi: 10.1016/j.gloplacha.2019.102981
    [42]
    Weltje G J, Tjallingii R. Calibration of XRF core scanners for quantitative geochemical logging of sediment cores: theory and application[J]. Earth and Planetary Science Letters, 2008, 274(3-4):423-438. doi: 10.1016/j.jpgl.2008.07.054
    [43]
    Gao W H, Li K F, Miao X D, et al. Holocene extreme flood distribution patterns in the upper and middle Yellow River: a review based on slackwater deposits[J]. Earth-Science Reviews, 2025, 261:105039. doi: 10.1016/j.earscirev.2024.105039
    [44]
    Zhang Z X, Zhang Z P, Xu J H, et al. A review of paleofloods in the middle-lower reaches of the Yangtze River during the Holocene: processes, causes and effects[J]. Quaternary Science Reviews, 2024, 345:109019. doi: 10.1016/j.quascirev.2024.109019
    [45]
    Knox J C. Sensitivity of modern and Holocene floods to climate change[J]. Quaternary Science Reviews, 2000, 19(1-5):439-457. doi: 10.1016/S0277-3791(99)00074-8
    [46]
    Starkel L, Soja R, Michczyńska D J. Past hydrological events reflected in Holocene history of Polish rivers[J]. CATENA, 2006, 66(1-2):24-33. doi: 10.1016/j.catena.2005.07.008
    [47]
    Wang Y J, Cheng H, Edwards R L, et al. A high-resolution absolute-dated late Pleistocene Monsoon record from Hulu Cave, China[J]. Science, 2001, 294(5550):2345-2348. doi: 10.1126/science.1064618
    [48]
    Alley R B, Meese D A, Shuman C A, et al. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event[J]. Nature, 1993, 362(6420):527-529. doi: 10.1038/362527a0
    [49]
    Svensson A, Andersen K K, Bigler M, et al. A 60000 year Greenland stratigraphic ice core chronology[J]. Climate of the Past, 2008, 4(1):47-57. doi: 10.5194/cp-4-47-2008
    [50]
    Berger A, Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Science Reviews, 1991, 10(4):297-317. doi: 10.1016/0277-3791(91)90033-Q
    [51]
    Herzschuh U. Palaeo-moisture evolution in monsoonal Central Asia during the last 50, 000 years[J]. Quaternary Science Reviews, 2006, 25(1-2):163-178. doi: 10.1016/j.quascirev.2005.02.006
    [52]
    王瑜, 宋长青, 孙湘君. 内蒙古土默特平原北部全新世古环境变迁[J]. 地理学报, 1997, 52(5):430-438 doi: 10.3321/j.issn:0375-5444.1997.05.007

    WANG Yu, SONG Changqing, SUN Xiangjun. Palynological record of paleovegetation change during Holocene at North Tumote Plain in Inner Mongolia, China[J]. Acta Geographica Sinica, 1997, 52(5):430-438.] doi: 10.3321/j.issn:0375-5444.1997.05.007
    [53]
    Dong H W, Xie M M, Shang W Y, et al. Plant-wax carbon isotopic evidence of Lateglacial and Holocene climate change from lake sediments in the Yin Mountains, inner Mongolia[J]. Quaternary International, 2022, 622:10-20. doi: 10.1016/j.quaint.2021.12.017
    [54]
    Chen F H, Xu Q H, Chen J H, et al. East Asian summer monsoon precipitation variability since the last deglaciation[J]. Scientific Reports, 2015, 5(1):11186. doi: 10.1038/srep11186
    [55]
    Wang H P, Chen J H, Zhang X J, et al. Palaeosol development in the Chinese Loess Plateau as an indicator of the strength of the East Asian summer monsoon: evidence for a mid-Holocene maximum[J]. Quaternary International, 2014, 334-335:155-164. doi: 10.1016/j.quaint.2014.03.013
    [56]
    Chen F H, Li G Q, Zhao H, et al. Landscape evolution of the Ulan Buh Desert in northern China during the late Quaternary[J]. Quaternary Research, 2014, 81(3):476-487. doi: 10.1016/j.yqres.2013.08.005
    [57]
    申洪源, 贾玉连, 郭峰. 内蒙古黄旗海湖泊沉积物磁化率特征及其环境意义[J]. 干旱区地理, 2010, 33(2):151-157

    SHEN Hongyuan, JIA Yulian, GUO Feng. Characteristics and environmental significance of the magnetic susceptibility in sediment of Huangqihai Lake, Inner Mongolia, China[J]. Arid Land Geography, 2010, 33(2):151-157.]
    [58]
    Chen L, Chen J, Shen Z W, et al. Drought in the Asian summer monsoon region is liked to a weakened inter-hemispheric temperature gradient[J]. Communications Earth & Environment, 2024, 5(1):432.
    [59]
    Pang H L, Jia Y X, Li F Q, et al. An improved method for paleoflood reconstruction from core sediments in the upper Yellow River[J]. Frontiers in Earth Science, 2023, 11:1149502. doi: 10.3389/feart.2023.1149502
    [60]
    Yu S Y, Li W J, Zhou L, et al. Human disturbances dominated the unprecedentedly high frequency of Yellow River flood over the last millennium[J]. Science Advances, 2023, 9(8):eadf8576. doi: 10.1126/sciadv.adf8576
    [61]
    陈耳东. 河套灌区水利简史[M]. 北京: 水利电力出版社, 1988

    CHEN Erdong. A Brief History of Water Conservancy in Hetao Irrigation District[M]. Beijing: Water Resources and Electric Power Press, 1988.]
    • Related Articles

  • Related Articles

    [1]DU linfen, SHI Lu, HUA Chunrong, WANG Yasu, JIANG Shijun. Paleoenvironmental evolution in the Guaymas Basin over the past 350 ka based on X-ray fluorescence scanning of sediment cores[J]. Marine Geology & Quaternary Geology. DOI: 10.16562/j.cnki.0256-1492.2024072701
    [2]ZHANG Hangyu, WANG Xiaqing, HUANG Ping’an, WAN Dejun, LIU Fenggui, TANG Xiangling, ZHOU Kehan. Reliability assessment and calibration of elemental signal values by XRF core scanning in Qinghai Lake[J]. Marine Geology & Quaternary Geology, 2024, 44(4): 200-211. DOI: 10.16562/j.cnki.0256-1492.2023100101
    [3]ZHANG Hongliang, HOU Yilin, LI Huayong, LI Zhihui, WANG Qian, YANG Yiping, XU Weidong, YU Zhengsong. Characteristics of X-ray fluorescence scanning element of modern flood sediments in northern Shandong Province and its geological indicative significance[J]. Marine Geology & Quaternary Geology, 2023, 43(3): 185-194. DOI: 10.16562/j.cnki.0256-1492.2022110801
    [4]XIAO Qianwen, FENG Xiuli, MIAO Xiaoming. Turbidity deposits and their provenance: evidence from core SH37 in Shenhu area of the South China Sea[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 101-111. DOI: 10.16562/j.cnki.0256-1492.2021011901
    [5]LU Yamin, SU Kefan, FU Fanfei, HUANG Baoqi, LIU Lejun, WANG Na. X-ray CT scanning technique and its application to the Core 01 in the northern South China Sea for sedimentary environment reconstruction[J]. Marine Geology & Quaternary Geology, 2021, 41(4): 215-221. DOI: 10.16562/j.cnki.0256-1492.2020110901
    [6]ZHAO Gege, TIAN Qingchun, DU Wuxi, PEI Yu, E Chongyi. End member model analysis of grain size for the loess in Linfen Basin, China[J]. Marine Geology & Quaternary Geology, 2021, 41(2): 192-200. DOI: 10.16562/j.cnki.0256-1492.2020082601
    [7]LIN Fanyu, YIN Xijie, HUANG Wei, HUANG Jiechao, LIANG Yuna. Application of micro-XRF technology to rapid and nondestructive detection of inorganic elements in ocean minerals[J]. Marine Geology & Quaternary Geology, 2021, 41(1): 223-232. DOI: 10.16562/j.cnki.0256-1492.2020071701
    [8]SHANG Guangchun, LI Liang, MA Chunmei, YI Shuangwen, ZHAO Lin, CUI Anning. Climatic and environmental changes since 2 kaBP by End Member Modeling analysis on grain size data from a peat core of Yuhua Mountain, Jiangxi Province[J]. Marine Geology & Quaternary Geology, 2020, 40(2): 165-173. DOI: 10.16562/j.cnki.0256-1492.2019011501
    [9]ZHANG Xiaonan, ZHANG Can, WU Duo, ZHOU Aifeng. ELEMENT GEOCHEMISTRY OF LAKE DEPOSITS MEASURED BY X-RAY FLUORESCENCECORE SCANNER IN NORTHWEST CHINA[J]. Marine Geology & Quaternary Geology, 2015, 35(1): 163-174. DOI: 10.3724/SP.J.1140.2015.01163
    [10]ZHU Yun, CHEN Ye, SHU Qiang, ZHAO Zhi-jun, XIAO Jia-yi, LI Ji-jun. CHROMA INDEX RECORD OF CORE XH1 AT NORTHERN JIANGSU BASIN AND THE CLIMATE SINCE MID-PLEISTOCENE[J]. Marine Geology & Quaternary Geology, 2007, 27(2): 23-31.

  • Cited by

    Periodical cited type(1)

    1. 谷浩然，杨俊钢，王斌，崔伟，陈前. 基于再分析数据的南海三维温盐结构特征分析. 数字海洋与水下攻防. 2024(01): 62-71 .

    Other cited types(1)

Catalog

    Get Citation
    PDF
    XML
    Article views (12) PDF downloads (2) Cited by(2)
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzbjb@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return