% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Fichtler:201141,
      author       = {Fichtler, Esther and Helle, Gerhard and Worbes, Martin},
      title        = {{S}table-{C}arbon {I}sotope {T}ime {S}eries from {T}ropical
                      {T}ree {R}ings {I}ndicate a {P}recipitation {S}ignal},
      journal      = {Tree-ring research},
      volume       = {66},
      number       = {1},
      issn         = {1536-1098},
      address      = {Tucson, Ariz.},
      publisher    = {Tree-Ring Society with the cooperation of the Laboratory of
                      Tree-Ring Research, the University of Arizona},
      reportid     = {FZJ-2015-03446},
      pages        = {35 - 49},
      year         = {2010},
      abstract     = {Although studies on stable-carbon isotopes in trees from
                      temperate zones provide abundant paleoclimatic data,
                      tropical trees are still understudied in this context.
                      Therefore this study examined the variability of intra- and
                      inter-annual stable-carbon isotopic pattern in several tree
                      species from various tropical climates. The δ13C values of
                      samples of 12 broadleaved trees (seven species) from various
                      paleotropical and neotropical sites along a climatic
                      moisture gradient were investigated. The inter-annual
                      variability between species and sites was studied. Further
                      the relationship between δ13C and precipitation time series
                      was analyzed. Results show that tropical tree species show a
                      similar variability in carbon isotopic composition as
                      temperate tree species. Significant correlations between
                      annual precipitation and tree-ring δ13C time series were
                      negative. Successful crossdating of a tree-ring δ13C time
                      series highlights the potential of carbon isotope
                      measurements for tropical tree-ring analytical studies.
                      Tropical broadleaved trees are able to capture a carbon
                      isotopic signal in their annual rings even under everwet
                      conditions and show good potential for paleoclimatic
                      research.},
      cin          = {IBG-3},
      ddc          = {580},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {246 - Modelling and Monitoring Terrestrial Systems: Methods
                      and Technologies (POF2-246) / 255 - Terrestrial Systems:
                      From Observation to Prediction (POF3-255)},
      pid          = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000274162400003},
      doi          = {10.3959/2008-20.1},
      url          = {https://juser.fz-juelich.de/record/201141},
}