Volume 39 Issue 4
Apr.  2020
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Zhongqiao Li, Ying Wu, Liyang Yang, Jinzhou Du, Bing Deng, Jing Zhang. Carbon isotopes and lignin phenols for tracing the floods during the past 70 years in the middle reach of the Changjiang River[J]. Acta Oceanologica Sinica, 2020, 39(4): 33-41. doi: 10.1007/s13131-020-1543-y
Citation: Zhongqiao Li, Ying Wu, Liyang Yang, Jinzhou Du, Bing Deng, Jing Zhang. Carbon isotopes and lignin phenols for tracing the floods during the past 70 years in the middle reach of the Changjiang River[J]. Acta Oceanologica Sinica, 2020, 39(4): 33-41. doi: 10.1007/s13131-020-1543-y

Carbon isotopes and lignin phenols for tracing the floods during the past 70 years in the middle reach of the Changjiang River

doi: 10.1007/s13131-020-1543-y
Funds:  The National Natural Science Foundation of China under contract Nos 41021064, 41276081 and 41606211; the 111 Project under contract No. B08022; the Scientific Research Fund of Second Institute of Oceanography, MNR under contract No. JG1806.
More Information
  • Corresponding author: E-mail: wuying@sklec.ecnu.edu.cn
  • Received Date: 2019-02-23
  • Accepted Date: 2019-06-10
  • Available Online: 2020-12-28
  • Publish Date: 2020-04-25
  • The Lake Tian E Zhou (TEZ, an oxbow lake) was formed during the rerouting of the Changjiang River in 1972, with strong influences from the main river channel and flood events. Herein, a sediment core was collected from the Lake TEZ for the measurements of carbon isotopes and biomarkers, including stable carbon isotopes (δ13C), radiocarbon composition (∆14C), and lignin phenols, as well as lead-210 to reconstruct recent heavy flood events over the past 70 years. At the 24–26 cm interval, the sediment contained the highest OC%, TN%, and lignin phenols content, as well as significantly depleted 13C but enriched 14C, corresponding to the extreme flood event in 1998. In addition, statistics from t-test showed that lignin phenols normalized to OC (Λ8), the concentration of 3, 5-dihydroxy benzoic acid (3, 5-BD), and the ratio of p-hydroxy benzophenone to total hydroxyl phenols (PHB/HP) were all significantly different between the layers containing flood deposits and the layers deposited under normal non-flood conditions (p<0.05). These results indicate that the later three parameters are highly related to flood events and can be used as compelling proxies, along with sediment chronology, for hydrological changes and storm/flood events in the river basin and coastal marine environments.
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  • [1]
    Bianchi T S, Galy V, Rosenheim B E, et al. 2015. Paleoreconstruction of organic carbon inputs to an oxbow lake in the Mississippi River watershed: effects of dam construction and land use change on regional inputs. Geophysical Research Letters, 42(19): 7983–7991. doi: 10.1002/2015GL065595
    [2]
    Bianchi T S, Garcia-Tigreros F, Yvon-Lewis S A, et al. 2013. Enhanced transfer of terrestrially derived carbon to the atmosphere in a flooding event. Geophysical Research Letters, 40(1): 116–122. doi: 10.1029/2012GL054145
    [3]
    Bronson F. 2003. Validation of the accuracy of the LabSOCS software for mathematical efficiency calibration of Ge detectors for typical laboratory samples. Journal of Radioanalytical and Nuclear Chemistry, 255(1): 137–141. doi: 10.1023/A:1022248318741
    [4]
    Chen C T A, Zhai Weidong, Dai Minhan. 2008. Riverine input and air–sea CO2 exchanges near the Changjiang (Yangtze River) Estuary: status quo and implication on possible future changes in metabolic status. Continental Shelf Research, 28(12): 1476–1482. doi: 10.1016/j.csr.2007.10.013
    [5]
    Dalzell B J, Filley T R, Harbor J M. 2005. Flood pulse influences on terrestrial organic matter export from an agricultural watershed. Journal of Geophysical Research, 110(G2): G02011. doi: 10.1029/2005JG000043
    [6]
    Dhillon G S, Inamdar S. 2013. Extreme storms and changes in particulate and dissolved organic carbon in runoff: entering uncharted waters?. Geophysical Research Letters, 40(7): 1322–1327. doi: 10.1002/grl.50306
    [7]
    Dittmar T, Lara R J, Kattner G. 2001. River or mangrove? Tracing major organic matter sources in tropical Brazilian coastal waters. Marine Chemistry, 73(3–4): 253–271
    [8]
    Ertel J R, Hedges J I. 1985. Sources of sedimentary humic substances: vascular plant debris. Geochimica et Cosmochimica Acta, 49(10): 2097–2107. doi: 10.1016/0016-7037(85)90067-5
    [9]
    Falkowski P, Scholes R J, Boyle E, et al. 2000. The global carbon cycle: a test of our knowledge of earth as a system. Science, 290(5490): 291–296. doi: 10.1126/science.290.5490.291
    [10]
    Farella N, Lucotte M, Louchouarn P, et al. 2001. Deforestation modifying terrestrial organic transport in the Rio Tapajós, Brazilian Amazon. Organic Geochemistry, 32(12): 1443–1458. doi: 10.1016/S0146-6380(01)00103-6
    [11]
    Feng Xiaojuan, Simpson M J. 2007. The distribution and degradation of biomarkers in Alberta grassland soil profiles. Organic Geochemistry, 38(9): 1558–1570. doi: 10.1016/j.orggeochem.2007.05.001
    [12]
    Hedges J I, Keil R G, Benner R. 1997. What happens to terrestrial organic matter in the ocean?. Organic Geochemistry, 27(5–6): 195–212
    [13]
    Hedges J I, Mann D C. 1979a. The characterization of plant tissues by their lignin oxidation products. Geochimica et Cosmochimica Acta, 43(11): 1803–1807. doi: 10.1016/0016-7037(79)90028-0
    [14]
    Hedges J I, Mann D C. 1979b. The lignin geochemistry of marine sediments from the southern Washington coast. Geochimica et Cosmochimica Acta, 43(11): 1809–1818. doi: 10.1016/0016-7037(79)90029-2
    [15]
    Jia Tiefei, Wang Feng, Yuan Shifei. 2015. Oxbow lake sedimentary characteristics and their environmental significance in Tianezhou and Zhongzhouzi lakes in the middle Yangtze River. Geographical Research (in Chinese), 34(5): 861–871
    [16]
    Korponai J, Gyulai I, Braun M, et al. 2016. Reconstruction of flood events in an oxbow lake (Marótzugi-Holt-Tisza, NE Hungary) by using subfossil cladoceran remains and sediments. Advances in Oceanography and Limnology, 7(2): 125–135
    [17]
    Lin Jing, Wu Ying, Zhang Jing, et al. 2007. Seasonal variation of organic carbon fluxes in the Yangtze River and influence of Three-Gorges engineering. China Environmental Science (in Chinese), 27(2): 246–249
    [18]
    Luo Xiangxing, Yang Shilun, Zhang Jing. 2012. The impact of the Three Gorges Dam on the downstream distribution and texture of sediments along the middle and lower Yangtze River (Changjiang) and its estuary, and subsequent sediment dispersal in the East China Sea. Geomorphology, 179: 126–140. doi: 10.1016/j.geomorph.2012.05.034
    [19]
    Shi Yafeng, Jiang Tong, Su Buda, et al. 2004. Preliminary analysis on the relation between the evolution of heavy floods in the yangtze river catchment and the climate changes since 1840. Journal of Lake Sciences (in Chinese), 16(4): 289–297. doi: 10.18307/2004.0401
    [20]
    Still C J, Berry J A, Collatz G J, et al. 2003. Global distribution of C3 and C4 vegetation: carbon cycle implications. Global Biogeochemical Cycles, 17(1): 1006. doi: 10.1029/2001GB001807
    [21]
    Tareq S M, Tanaka N, Ohta K. 2004. Biomarker signature in tropical wetland: lignin phenol vegetation index (LPVI) and its implications for reconstructing the paleoenvironment. Science of the Total Environment, 324(1–3): 91–103
    [22]
    Trefethen J M. 1950. Classification of sediments. American Journal of Science, 248: 55–62. doi: 10.2475/ajs.248.1.55
    [23]
    van Metre P C, Horowitz A J. 2013. An 80-year record of sediment quality in the lower Mississippi River. Hydrological Processes, 27(17): 2438–2448. doi: 10.1002/hyp.9336
    [24]
    Wang Jianjun, Chen Liqi, Li Li, et al. 2014. Preliminary identification of palaeofloods with the alkane ratio C31/C17 and their potential link to global climate changes. Scientific Reports, 4: 6502
    [25]
    Wang Minjie, Zheng Hongbo, Xie Xin, et al. 2011. A 600-year flood history in the Yangtze River drainage: comparison between a subaqueous delta and historical records. Chinese Science Bulletin, 56(2): 188–195. doi: 10.1007/s11434-010-4212-2
    [26]
    Wu Y, Zhang J, Liu S M, et al. 2007. Sources and distribution of carbon within the Yangtze River system. Estuarine, Coastal and Shelf Science, 71(1–2): 13–25
    [27]
    Yu Hao, Wu Ying, Zhang Jing, et al. 2011. Impact of extreme drought and the Three Gorges Dam on transport of particulate terrestrial organic carbon in the Changjiang (Yangtze) River. Journal of Geophysical Research, 116(F4): F04029. doi: 10.1029/2011JF002012
    [28]
    Zhan Wang, Yang Shouye, Liu Xiaoli, et al. 2010. Reconstruction of flood events over the last 150 years in the lower reaches of the Changjiang River. Chinese Science Bulletin, 55(21): 2268–2274. doi: 10.1007/s11434-010-3263-8
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