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@ARTICLE{Grieinger:862504,
      author       = {Grießinger, Jussi and Bräuning, Achim and Helle, Gerhard
                      and Schleser, Gerhard, Hans and Hochreuther, Philipp and
                      Meier, Wolfgang and Zhu, Haifeng},
      title        = {{A} {D}ual {S}table {I}sotope {A}pproach {U}nravels
                      {C}ommon {C}limate {S}ignals and {S}pecies-{S}pecific
                      {R}esponses to {E}nvironmental {C}hange {S}tored in
                      {M}ulti-{C}entury {T}ree-{R}ing {S}eries from the {T}ibetan
                      {P}lateau},
      journal      = {Geosciences},
      volume       = {9},
      number       = {4},
      issn         = {2076-3263},
      address      = {Basel},
      publisher    = {MDPI},
      reportid     = {FZJ-2019-02808},
      pages        = {151 -},
      year         = {2019},
      abstract     = {Tree-rings are recorders of environmental signals and are
                      therefore often used to reconstruct past environmental
                      conditions. In this paper, we present four annually
                      resolved, multi-centennial tree-ring isotope series from the
                      southeastern Tibetan plateau. The investigation site, where
                      juniper and spruce trees jointly occur, is one of the
                      highest known tree-stands in the world. Tree ring cellulose
                      oxygen (δ18O) and carbon (δ13C) isotopes were analyzed for
                      a common period of 1685–2007 AD to investigate
                      climate–isotope relationships. Therefore, various climate
                      parameters from a local meteorological station and from the
                      CRU 4.02 dataset were used. Tree-ring δ18O of both species
                      revealed highly significant sensitivities with a high degree
                      of coherence to hydroclimate variables during the growing
                      season. The obtained δ18O–climate relationships can even
                      be retained using a species mean. In contrast, the
                      individual δ13C series indicated a weaker and non-uniform
                      response to the tested variables. Underlying
                      species-specific responses and adaptations to the long-term
                      trend in atmospheric CO2 bias even after a trend correction
                      identified dominant environmental factors triggering the
                      tree-ring δ13C at our site. However, analysis of individual
                      intrinsic water-use efficiency in juniper and spruce trees
                      indicated a species-specific adaptation strategy to climate
                      change},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000467305900006},
      doi          = {10.3390/geosciences9040151},
      url          = {https://juser.fz-juelich.de/record/862504},
}