BAI Ying, SU Rongguo, HAN Xiurong, ZHANG Chuansong, SHI Xiaoyong. Investigation of seasonal variability of CDOM fluorescence in the southern Changjiang River Estuary by EEM-PARAFAC[J]. Acta Oceanologica Sinica, 2015, 34(10): 1-12. doi: 10.1007/s13131-015-0714-8
Citation: BAI Ying, SU Rongguo, HAN Xiurong, ZHANG Chuansong, SHI Xiaoyong. Investigation of seasonal variability of CDOM fluorescence in the southern Changjiang River Estuary by EEM-PARAFAC[J]. Acta Oceanologica Sinica, 2015, 34(10): 1-12. doi: 10.1007/s13131-015-0714-8

Investigation of seasonal variability of CDOM fluorescence in the southern Changjiang River Estuary by EEM-PARAFAC

doi: 10.1007/s13131-015-0714-8
  • Received Date: 2014-09-02
  • Rev Recd Date: 2014-12-09
  • The southern Changjiang River Estuary has attracted considerable attention from marine scientists because it is a highly biologically active area and is biogeochemically significant. Moreover, land-ocean interactions strongly impact the estuary, and harmful algal blooms (HABs) frequently occur in the area. In October 2010 and May 2011, water samples of chromophoric dissolved organic matter (CDOM) were collected from the southern Changjiang River Estuary. Parallel factor analysis (PARAFAC) was used to assess the samples' CDOM composition using excitation-emission matrix (EEM) spectroscopy. Four components were identified: three were humic-like (C1, C2 and C3) and one was protein-like (C4). Analysis based on spatial and seasonal distributions, as well as relationships with salinity, Chl a and apparent oxygen utilization (AOU), revealed that terrestrial inputs had the most significant effect on the three humic-like Components C1, C2 and C3 in autumn. In spring, microbial processes and phytoplankton blooms were also important factors that impacted the three components. The protein-like Component C4 had autochthonous and allochthonous origins and likely represented a biologically labile component. CDOM in the southern Changjiang River Estuary was mostly affected by terrestrial inputs. Microbial processes and phytoplankton blooms were also important sources of CDOM, especially in spring. The fluorescence intensities of the four components were significantly higher in spring than in autumn. On average, C1, C2, C3, C4 and the total fluorescence intensity (TFI) in the surface, middle and bottom layers increased by 123%-242%, 105%-195%, 167%-665%, 483%-567% and 184%-245% in spring than in autumn, respectively. This finding corresponded with a Chl a concentration that was 16-20 times higher in spring than in autumn and an AOU that was two to four times lower in spring than in autumn. The humification index (HIX) was lower in spring that in autumn, and the fluorescence index (FI) was higher in spring than in autumn. This result indicated that the CDOM was labile and the biological activity was intense in spring.
  • loading
  • Andersson C A, Bro R. 2000. The N-way Toolbox for MATLAB. Chem-ometrics and Intelligent Laboratory Systems, 52(1): 1-4
    Baber C B, Dobkin D P, Huhdanpaa H. 1996. The Quickhull al-gorithm for convex hulls. ACM Transaction Mathematical Soft-ware, 22(4): 469-483
    Birdwell J E, Engel A S. 2010. Characterization of dissolved organic matter in cave and spring waters using UV-vis absorbance and fluorescence spectroscopy. Organic Geochemistry, 41(3): 270-280
    Blough N V, Del Vecchio R. 2002. Chromophoric DOM in the coastal environment. In: Hansell D, Carlson C, eds. Biogeochemistry of Marine Dissolved Organic Matter. New York: Academic Press, 509-546
    Bro R. 1997. PARAFAC. Tutorial and applications. Chemometrics and Intelligent Laboratory Systems, 38(2): 149-171
    Coble P G. 1996. Characterization of marine and terrestrial DOM in seawater using excitation-emission matrix spectroscopy. Mar-ine Chemistry, 51(4): 325-346
    Coble P G. 2007. Marine optical biogeochemistry: the chemistry of ocean color. Chemical Reviews, 107(2): 402-418
    Cory R M, McKnight D M. 2005. Fluorescence spectroscopy reveals ubiquitous presence of oxidized and reduced quinones in dis-solved organic matter. Environment Science & Technology, 39(21): 8142-8149
    Gao Lei, Fan Daidu, Li Daoji, et al. 2010. Fluorescence characteristics of chromophoric dissolved organic matter in shallow water along the Zhejiang coasts, southeast China. Marine Environ-mental Research, 69(3): 187-197
    Guéguen C, Granskog M A, McCullough G, et al. 2011. Characterisa-tion of colored dissolved organic matter in Hudson Bay and Hudson Strait using parallel factor analysis. Journal of Marine Systems, 88(3): 423-433
    Guo Weidong, Stedmon C A, Han Yuchao, et al. 2007. The conservat-ive and non-conservative behavior of chromophoric dissolved organic matter in Chinese estuarine waters. Marine Chemistry, 107(3): 357-366
    Hargreaves B R. 2003. Water column optics and penetration of UVR. In: Helbling E W, Zagarese H E, eds. UV Effects in Aquatic Or-ganisms and Ecosystems. Cambridge UK: The Royal Society of Chemistry, 59-108
    Holbrook R D, Yen J H, Grizzard T J. 2006. Characterizing natural or-ganic material from the Occoquan Watershed (Northern Vir-ginia, US) using fluorescence spectroscopy and PARAFAC. Sci-ence of the Total Environment, 361(1-2): 249-266
    Huguet A, Vacher L, Saubusse S, et al. 2010. New insights into the size distribution of fluorescent dissolved organic matter in estuar-ine waters. Organic Geochemistry, 41(6): 595-610
    Kowalczuk P, Cooper W J, Durako M J, et al. 2010. Characterization of dissolved organic matter fluorescence in the South Atlantic Bight with use of PARAFAC model: Relationships between fluorescence and its components, absorption coefficients and organic carbon concentrations. Marine Chemistry, 118(1-2): 22-36
    Kowalczuk P, Durako M J, Young H, et al. 2009. Characterization of dissolved organic matter fluorescence in the South Atlantic Bight with use of PARAFAC model: interannual variability. Marine Chemistry, 113(3-4): 182-196
    Li Maotian, Xu Kaiqin, Watanabe M, et al. 2007. Long-term vari-ations in dissolved silicate, nitrogen, and phosphorus flux from the Yangtze River into the East China Sea and impacts on estu-arine ecosystem. Estuarine, Coastal and Shelf Science, 71(1-2): 3-12
    Lin Jing. 2007. Distributions of dissolved organic carbon and particu-late organic carbon in the Changjiang Estuary and its adjacent area (in Chinese) [dissertation]. Shanghai: East China Normal University
    Liu J P, Xu K H, Li A C, et al. 2007. Flux and fate of Yangtze River sedi-ment delivered to the East China Sea. Geomorphology, 85(3-4): 208-224
    Luciani X, Mounier S, Paraquetti H H M, et al. 2008. Tracing of dis-solved organic matter from the SEPETIBA Bay (Brazil) by PAR-AFAC analysis of total luminescence matrices. Marine Environ-mental Research, 65(2): 148-157
    Maie N, Yamashita Y, Cory R M, et al. 2012. Application of excitation emission matrix fluorescence monitoring in the assessment of spatial and seasonal drivers of dissolved organic matter com-position: Sources and physical disturbance controls. Applied Geochemistry, 27(4): 917-929
    McKnight D M, Boyer E W, Westerhoff P K, et al. 2001. Spectrofluoro-metric characterization of dissolved organic matter for indica-tion of precursor organic material and aromaticity. Limnology and Oceanography, 46(1): 38-48
    Murphy K R, Stedmon C A, Waite T D, et al. 2008. Distinguishing between terrestrial and autochthonous organic matter sources in marine environments using fluorescence spectroscopy. Mar-ine Chemistry, 108(1-2): 40-58
    Nieke B, Reuter R, Heuermann R, et al. 1997. Light absorption and fluorescence properties of chromophoric dissolved organic matter (CDOM), in the St. Lawrence estuary (Case 2 waters). Continental Shelf Research, 17(3): 235-252
    Ning X, Liu Z, Cai Y, et al. 1998. Physicobiological oceanographic re-mote sensing of the East China Sea: satellite and in situ obser-vations. Journal of Geophysical Research: Oceans, 103(C10): 21623-21635
    Ogawa H, Usui T, Koike I. 2003. Distribution of dissolved organic car-bon in the East China Sea. Deep-Sea Research Part II: Topical Studies in Oceanography, 50(2): 353-366
    Ohno T. 2002. Fluorescence inner-filtering correction for determin-ing the humification index of dissolved organic matter. Envir-onmental Science & Technology, 36(4): 742-746
    Parlanti E, Wörz K, Geoffroy L, et al. 2000. Dissolved organic matter fluorescence spectroscopy as a tool to estimate biological activ-ity in a coastal zone submitted to anthropogenic inputs. Organ-ic Geochemistry, 31(12): 1765-1781
    Shi Wei, Wang Menghua. 2012. Satellite views of the Bohai Sea, Yel-low Sea, and East China Sea. Progress in Oceanography, 104: 30-45
    Singh S, D'Sa E J, Swenson E M. 2010. Chromophoric dissolved or-ganic matter (CDOM) variability in Barataria Basin using excit-ation-emission matrix (EEM) fluorescence and parallel factor analysis (PARAFAC). Science of the Total Environment, 408(16): 3211-3222
    Stedmon C A, Bro R. 2008. Characterizing dissolved organic matter fluorescence with parallel factor analysis: a tutorial. Limnology and Oceanography: Methods, 6(11): 572-579
    Stedmon C A, Markager S. 2005a. Resolving the variability in dis-solved organic matter fluorescence in a temperate estuary and its catchment using PARAFAC analysis. Limnology and Ocean-ography, 50(2): 686-697
    Stedmon C A, Markager S. 2005b. Tracing the production and de-gradation of autochthonous fractions of dissolved organic mat-ter by fluorescence analysis. Limnology and Oceanography, 50(5): 1415-1426
    Stedmon C A, Markager S, Bro R. 2003. Tracing dissolved organic matter in aquatic environments using a new approach to fluor-escence spectroscopy. Marine Chemistry, 82(3-4): 239-254
    Tian R C, Hu F X, Martin J M. 1993. Summer nutrient fronts in the Changjiang (Yangtze River) estuary. Estuarine, Coastal and Shelf Science, 37(1): 27-41
    Wada S, Aoki M N, Tsuchiya Y, et al. 2007. Quantitative and qualitat-ive analyses of dissolved organic matter released from Ecklonia cava Kjellman, in Oura Bay, Shimoda, Izu Peninsula, Japan. Journal of Experimental Marine Biology and Ecology, 349(2): 344-358
    Wang Zhaoyu, Wang Jiangtao, Tan Liju. 2014. Variation in photosyn-thetic activity of phytoplankton during the spring algal blooms in the adjacent area of Changjiang River estuary. Ecological In-dicators, 45: 465-473
    Wang Baodong, Wang Xiulin, Zhan Run. 2003. Nutrient conditions in the Yellow Sea and the East China Sea. Estuarine, Coastal and Shelf Science, 58(1): 127-136
    Yamashita Y, Jaffé R, Maie N, et al. 2008. Assessing the dynamics of dissolved organic matter (DOM) in coastal environments by ex-citation emission matrix fluorescence and parallel factor ana-lysis (EEM-PARAFAC). Limnology and Oceanography, 53(5): 1900-1908
    Yang Liyang, Hong Huasheng, Chen C-T A, et al. 2013. Chromophor-ic dissolved organic matter in the estuaries of populated and mountainous Taiwan. Marine Chemistry, 157: 12-23
    Zepp R G, Sheldon W M, Moran M A. 2004. Dissolved organic fluoro-phores in southeastern US coastal waters: correction method for eliminating Rayleigh and Raman scattering peaks in excita-tion-emission matrices. Marine Chemistry, 89(1-4): 15-36
    Zhang Jing. 1996. Nutrient elements in large Chinese estuaries. Con-tinental Shelf Research, 16(8): 1023-1045
    Zhang Yunlin, Liu Xiaohan, Wang Mingzhu, et al. 2013. Composition-al differences of chromophoric dissolved organic matter de-rived from phytoplankton and macrophytes. Organic Geo-chemistry, 55: 26-37
    Zhang G L, Zhang J, Kang Y B, et al. 2004. Distributions and fluxes of methane in the East China Sea and the Yellow Sea in spring. Journal of Geophysical Research: Oceans, 109(C7): C07011
    Zhou Mingjiang, Shen Zhiliang, Yu Rencheng. 2008. Responses of a coastal phytoplankton community to increased nutrient input from the Changjiang (Yangtze) River. Continental Shelf Re-search, 28(12): 1483-1489
    Zhu Chun, Wang Zhanghua, Xue Bin, et al. 2011. Characterizing the depositional settings for sedimentary organic matter distribu-tions in the Lower Yangtze River-East China Sea Shelf System. Estuarine, Coastal and Shelf Science, 93(1): 182-191
    Zsolnay A, Baigar E, Jimenez M, et al. 1999. Differentiating with fluor-escence spectroscopy the sources of dissolved organic matter in soils subjected to drying. Chemosphere, 38(1): 45-50
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article views (1416) PDF downloads(837) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return