DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA

DONG Xu-Hui, YANG Xiang-Dong

DONG Xu-Hui, YANG Xiang-Dong. DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA[J]. 水生生物学报, 2006, 30(6): 702-710.
引用本文: DONG Xu-Hui, YANG Xiang-Dong. DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA[J]. 水生生物学报, 2006, 30(6): 702-710.

DIATOM COMMUNITY SUCCESSION AND NUTRIENT EVOLUTION RECORDED FROM A SEDIMENT CORE OF THE LONGGAN LAKE, A LARGE SHALLOW LAKE IN EAST CHINA

Funds: 

the Scientific Innovation Projects of Chinese Academy of Sciences(KZCX1-SW-12)andthe 973 projects(2002CB412300)

  • Abstract: The Longgan Lake is a shallow mesotrophic macrophyte-dominated lake. According to the high-resolution diatom research from its sediment core, the diatom community succession was built, and the total phosphorus (TP) and chlorophylla (Chl-a) con-centration were quantitatively reconstructed for the past 2000 years, based on the diatom-TP and diatom-Chla transfer functions. The shifts of diatom assemblages also mirrored the developments of aquatic plant, reflecting the characters of aquatic ecosystem evolution. The inferred epilimnetic TP concentrationfluctuated within a small range of 36 to 62 g/L, indicating the lake remained a relative stable mesotrophic status in the long historical period. The periodical variationsof the diatom assemblage and trophic status suggest a mitigatingfunction of shallow macrophyte-dominated lakes to nutrient input. The changesof lakestrophic status don t linearly respond to the human disturbance in the catchment. The dynamics mechanism of phosphorus in macrophyte dominated lakes, as inferredfrom diatoms, will provide a scientific foundationfor the prediction of trophic status change in a shallow lake, as well as the lake ecological restoration and management decisions.
  • [1]

    Melzer, A., 1999. Aquatic macrophytes as tools for lake management. Hydrobiologia 395/ 396:181-190

    [2]

    Pu, P. M., G. X. Wang., Z. K. Li, C. H. Hu, B. J. Chen,X. Y. Cheng, B. Li, S. Z. Zhang & Y. Q. Fan, 2001. Degradation of Healthy aquatic ecosystem and its remediation:theory, technology and application. Journal of Lake Science 13:193-203 (inChinese)

    [3]

    Scheffer,M.,1998. Ecology of shallow lakes,Population and Community Biology Sciences 22,Chapman and Hall,London:pp.357

    [4]

    Moss, B., 1990. Engineering and biological approaches to therestoration from eutrophication of shallow lakes in which aquaticplant communities are important components. Hydrobiologia 200/201:367-377

    [5]

    Kauppila, T., T. Moisioet &V. Saionen, 2002. A diatom-basedinference model for autumn epilimnetic total phosphorus concentrationand its application to a presently eutrophic boreal lake. Journal of Paleolimnology 27:261-273

    [6]

    Bennion, H., C. A. Duigan, E. Y. Haworth, T. E. H. Allott,N. J. Anderson, S. Juggins & N. Monteith, 1996. The Angleseylakes, Wales, UK-changes in trophic status of three standing watersas inferred from diatom transfer functions and their implications forconservation. Aquatic Conservation:Marine and Freshwater Ecosys-tems 6:81-92

    [7]

    Anderson, N. J., 1997. Reconstructing historical phosphorus con-centrations in rural lakes using diatom models. In:Tunney H et al.(editors), Phosphorus loss from soil to water. CAB International,Oxford:95-118

    [8]

    Bennion, H., 1994. A diatom-phosphorus transfer function for shal-low, eutrophic ponds in southeast England. Hydrobiologia 275:391-410

    [9]

    Lotter, A. F., H. J. B. Birks, W. Hofmann & A. Marchetto,1998. Modern diatom, cladocera, chironomid, and chrysophyte cystassemblages as quantitative indicators for the reconstruction of pastenvironmental conditions in the Alps. П. Nutrients. Journal of Pale-olimnology 19:443-463

    [10]

    Pienitz, R., J. P. Smol & G. M. MacDonald, 1999. Paleolimno-logical reconstructionof Holocene climatic trendsfromtwo boreal tree-line lakes, Northwest Territories, Canada. Antarctic Alpine Research31:82-93

    [11]

    Bradshaw, E. G., N. J. Anderson, J. P. Jensen & E. Jeppesen,2002. Phosphorus dynamics in Danish lakes and the implications for6 期DONG Xu-Hui et al. :DIATOM COMMUNITYSUCCESSION AND NUTRIENT EVOLUTION RECORDED FROMA SEDIMENT CORE OF THELONGG AN LAKE, A LARGE SHALLOWLAKE IN EAST CHINA709 diatom ecology and palaeoecology. Freshwater Biology 47: 1963-1975

    [12]

    Anderson, N. J. &B. Odgaard, 1994. Recent palaeolimnology ofthree shallow Danish lakes. Hydrobiologia 275/ 276:411-422

    [13]

    Karst, T. L. &J. P. Smol, 2000. Paleolimnological evidence oflimnetic nutrient concentration equilibrium in a shallow, macrophyte-dominated lake. Aquatic Sciences 62:20-38

    [14]

    Wang, S. & H. Dou, 1998. Lakes in China. Science Press, Bei-jing:88-471 (in Chinese)

    [15]

    Zhang, S., H. Dou &J. Jiang, 1996. The aquatic vegetation ofLonggan Lake. Journal of Lake Sciences 8:161-167 (in Chinese)

    [16]

    Dong, X., X. Yang & Pan H., 2004. The distribution of the sur-face sedimentary diatom from the lakes of middle and lower reach ofYangtze River. Journal of Lake Science 16:420-425 (in Chinese)

    [17]

    Battarbee, R. W., 1986. Diatom analysis. In B. E. Berglund (ed-itor), Handbookof Holocene palaeoecology and palaeohydrology. Wi-ley, Chichester :527-570

    [18]

    Krammer, K. & H. Lange-Bertalot, 1986, 1988, 1991a, 1991b.Bacillariophyceae(1-4Teil). Ettl H, Gerloff J, Heynig H. Suβwasserflora von Mitteleuropa. Stuttgart/Jena :Gustav Fischer Verlag

    [19]

    Yang, X., S. Wang, J. Shen, et al., 2002. Lacustrine environ-ment responses to human activities in the past 300 years in LongganLake catchment, southeast China. Science in China (Series D) 45:709-718

    [20]

    T ong, G., R. Wu, X. Yang, et al., 1997. vegetation and climaticquantitative reconstructionof LongganLake since the past 3000 years.Marine Geology &Quaternary Geology 17:53-61 (in Chinese)

    [21]

    Qu, W., R. Wu, X. Yang, et al., 1998. The palaeoenvironmentaland Palaeoclimatic Changes of Longgan Lake since the past 3000years. Journal of Lake Science 10:37-43 (in Chinese)

    [22]

    Yang, X., 2004. Diatom transfer functions and quantitative recon-structions of environments: Case studies of lakes in Qinghai-Xizang(Tibetan ) Plateau and the middle and lower reaches of Yangtze Riv-er. Nanjing Institute of Geography and Limnology, the ChineseAcademy of Science, Nanjing:36-52 (in Chinese)

    [23]

    K orsman, T. & H. J. B. Birks, 1996. Diatom based water chem-istry reconstructions from northern Sweden: a comparison of recon-struction techniques. Journal of Paleolimnology 15:65-77

    [24]

    Juggins, S., 1997. CALIBRATE version 0. 70-A C+ +problem foranalysing and visualising species environment relationships and forpredicting environmental values from species assemblages, user guideversion 1. 0. Department of Geography, University of Newcastle,UK:pp. 23

    [25]

    Hill, M. O., 1973. Diversity and evenness:a unifying notation andits consequences. Ecology 54:427-432

    [26]

    Jin, X., H. Liu, Q. T u, et al., 1994. Lake Eutrophication in China.China Environment Science Press, Beijing:13-135 (in Chinese)

    [27]

    Bennion, H., 1995. Surface-sediment diatom assemblages in shal-low, artificial, enriched ponds, and implications for reconstructingtrophic status. Diatom Research 10:1-19

    [28]

    Douglas, M. S. V. &J. P. Smol, 1995. Periphytic diatom assem-blages from high arctic ponds. Journal of Phycology 31:60-69

    [29]

    Kufel, L. & T. Ozimek, 1994. Can Chara control phosphorus cy-cling in Lake Tuknajno (Poland) ? Hydrobiologia 275/ 276:277-284

    [30]

    Y u, D., M. T u,L. Liu, et al., 1998. Changesof floristic compositionof aquatic plants in a shallow, eutrophic Chinese lake (Donghu Lake)from 1954 to 1994. Acta Hydrobiologia Sinica 22:219-228 (in Chinese)

    [31]

    Holtan, H., L. Kamp-Nielsen &A. O. Stuanes, 1988. Phosphorusin soil, water and sediment :an overview. Hydrobiologia 170:19-34

    [32]

    Anderson, N. J., 1993. Nature versus anthropogenic change in lakes:the role of the sediment record. T rends Ecology & Evolution 8:356-361

    [33]

    Hall, R. &J. P. Smol, 1999. Diatom as indicatorsof lake eutroph-ication. Eugene F. The diatom:Applicationfor the environmental andearth science. Cambridge university Press, London:128-168

    [34]

    Organisation for Economic Co-operation and Development, OECD.1982. Eutrophication of waters:monitoring, assessment and control.OECD, Paris:1-154

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出版历程
  • 收稿日期:  2004-11-03
  • 修回日期:  2006-03-08
  • 发布日期:  2006-11-24

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