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@ARTICLE{Jinglu:61908,
      author       = {Jinglu, W. and Chengmin, H. and Haian, Z. and Schleser, G.
                      H. and Battarbee, R.},
      title        = {{S}edimentary evidence for recent eutrophication in the
                      northern basin of {L}ake {T}aihu, {C}hina: human impacts on
                      a large shallow lake},
      journal      = {Journal of paleolimnology},
      volume       = {38},
      issn         = {0921-2728},
      address      = {Dordrecht [u.a.]},
      publisher    = {Springer Science + Business Media B.V},
      reportid     = {PreJuSER-61908},
      pages        = {13 - 23},
      year         = {2007},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Environmental change in Lake Taihu and its catchment since
                      the early to middle part of the twentieth century has left a
                      clear geochemical record in the lake sediments. The human
                      activities in the lake and its catchment responsible for the
                      change include agriculture, fisher, urbanisay tion, sewage
                      and industrial waster disposal. Sediment cores were
                      collected from Meilian Bay of northern Lake Taihu to
                      investigate the record of anthropogenic impacts on the
                      lake's ecosystem and to assess its natural,
                      pre-eutrophication baseline state. Two marked stratigraphic
                      sediment units were identified on the basis of total
                      phosphorus concentration (TP), pigments, total organic
                      carbon (TOC)/total nitrogen (TN), delta C-13 and delta N-15
                      corresponding to stages in the lake history dominated by
                      phytoplankton, and by aquatic macrophytes. Results show that
                      as TP loading increased from the early 1950s the lake
                      produced sediments with increasing amounts of organic matter
                      derived from phytoplankton. In the early 1950s, the first
                      evidence for eutrophication at the Meilian Bay site is
                      recorded by an increase in C/N values and in sediment
                      accumulation rate, but there is little change in phosphorus
                      concentrations, pigments, delta C-13 and delta N-15 at this
                      time. After 1990 a more rapid increase in trophic status
                      took place indicated by increased levels of phosphorus,
                      pigments, delta N-15 and by decreased delta C-13 and TOC/TN
                      values in the lake sediments. The first increase in trophic
                      status of the early 1950s results mainly from agricultural
                      development in the catchment. In contrast, the acceleration
                      from ca. 1990 originates from the recent development of
                      fisheries and the urbanisation and industrialisation of the
                      catchment.},
      keywords     = {J (WoSType)},
      cin          = {ICG-5},
      ddc          = {930},
      cid          = {I:(DE-Juel1)VDB143},
      pnm          = {Nachhaltige Entwicklung und Technik},
      pid          = {G:(DE-Juel1)FUEK408},
      shelfmark    = {Environmental Sciences / Geosciences, Multidisciplinary /
                      Limnology},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000247530100002},
      doi          = {10.1007/s10933-006-9058-x},
      url          = {https://juser.fz-juelich.de/record/61908},
}