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@ARTICLE{Parplies:60409,
      author       = {Parplies, J. and Lücke, A. and Vos, H. and Mingram, J. and
                      Stebich, M. and Radtke, U. and Han, J. and Schleser, G. H.},
      title        = {{L}ate glacial environment and climate development in
                      northeastern {C}hina derived from geochemical and isotopic
                      investigations of the varved sediment record from {L}ake
                      {S}ihailongwan ({J}ilin {P}rovince)},
      journal      = {Journal of paleolimnology},
      volume       = {40},
      issn         = {0921-2728},
      address      = {Dordrecht [u.a.]},
      publisher    = {Springer Science + Business Media B.V},
      reportid     = {PreJuSER-60409},
      pages        = {471 - 487},
      year         = {2008},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Total organic carbon (TOC) content, total nitrogen (TN)
                      content, stable nitrogen isotope (delta(15)) and stable
                      organic carbon isotope (delta C-13(org)) ratios were
                      continuously analysed on a high resolution sediment profile
                      from Lake Sihailongwan (SHL), covering the time span between
                      16,500 and 9,500 years BP. Strong variations of the
                      investigated proxy parameters are attributed to great
                      climatic fluctuations during the investigated time period.
                      Variations in organic carbon isotope ratios and the ratio of
                      TOC/TN (C/N ratio) are discussed with respect to changing
                      proportions of different organic matter (OM) sources to bulk
                      sedimentary OM. Phases of high TOC content, high TN content,
                      depleted delta C-13(org) values and high delta N-15 values
                      are interpreted as times with increased productivity of
                      lacustrine algae in relation to input of terrigenous organic
                      matter. Two distinct phases of enriched nitrogen isotope
                      ratios from 14,200 to 13,700 and 11,550 to 11,050 years BP
                      point towards a reduced phytoplankton discrimination against
                      N-15 due to a diminished dissolved inorganic nitrogen pool.
                      The combination of geochemical (TOC, TN, C/N ratio) and
                      isotopic (delta C-13(org), delta N-15) proxy parameters
                      points to a division of climate development into four
                      stages. A cold and dry stage before 14,200 years BP, a warm
                      optimum stage with high phytoplankton productivity from
                      14,200 to 12,450 BP, a colder and drier stage from 12,450 to
                      11,600 BP and a stage of climatic amelioration with high
                      variability in TOC and TN contents after 11,600 BP. These
                      results are discussed in relation to monsoon variability and
                      Northern Hemisphere climate development of the late
                      glacial.},
      keywords     = {J (WoSType)},
      cin          = {ICG-5},
      ddc          = {930},
      cid          = {I:(DE-Juel1)VDB143},
      pnm          = {Geosysteme - Erde im Wandel},
      pid          = {G:(DE-Juel1)FUEK405},
      shelfmark    = {Environmental Sciences / Geosciences, Multidisciplinary /
                      Limnology},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000257208600031},
      doi          = {10.1007/s10933-007-9176-0},
      url          = {https://juser.fz-juelich.de/record/60409},
}