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@ARTICLE{Long:41624,
      author       = {Long, St. P. and Ainsworth, E. A. and Rogers, A. K. and
                      Ort, D. R.},
      title        = {{R}ising atmospheric carbon dioxide: {P}lants {FACE} the
                      future},
      journal      = {Annual Review of Plant Biology},
      volume       = {55},
      issn         = {1040-2519},
      address      = {Palo Alto, Calif.},
      publisher    = {Annual Reviews Inc.},
      reportid     = {PreJuSER-41624},
      pages        = {591 - 628},
      year         = {2004},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Atmospheric CO(2) concentration ([CO(2)]) is now higher
                      than it was at any time in the past 26 million years and is
                      expected to nearly double during this century. Terrestrial
                      plants with the C(3) photosynthetic pathway respond in the
                      short term to increased [CO(2)] via increased net
                      photosynthesis and decreased transpiration. In the longer
                      term this increase is often offset by downregulation of
                      photosynthetic capacity. But much of what is currently known
                      about plant responses to elevated [CO(2)] comes from
                      enclosure studies, where the responses of plants may be
                      modified by size constraints and the limited life-cycle
                      stages that are examined. Free-Air CO(2) Enrichment (FACE)
                      was developed as a means to grow plants in the field at
                      controlled elevation of CO(2) under fully open-air field
                      conditions. The findings of FACE experiments are
                      quantitatively summarized via meta-analytic statistics and
                      compared to findings from chamber studies. Although trends
                      agree with parallel summaries of enclosure studies,
                      important quantitative differences emerge that have
                      important implications both for predicting the future
                      terrestrial biosphere and understanding how crops may need
                      to be adapted to the changed and changing atmosphere.},
      keywords     = {Acclimatization / Air: analysis / Atmosphere: analysis /
                      Carbon Dioxide: analysis / Photosynthesis / Plants:
                      metabolism / Carbon Dioxide (NLM Chemicals) / J (WoSType)},
      cin          = {ICG-III},
      ddc          = {580},
      cid          = {I:(DE-Juel1)VDB49},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Biochemistry $\&$ Molecular Biology / Plant Sciences},
      typ          = {PUB:(DE-HGF)16},
      pubmed       = {pmid:15377233},
      UT           = {WOS:000222766000023},
      doi          = {10.1146/annurev.arplant.55.031903.141610},
      url          = {https://juser.fz-juelich.de/record/41624},
}