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@ARTICLE{Charman:200874,
      author       = {Charman, D. J. and Beilman, D. W. and Blaauw, M. and Booth,
                      R. K. and Brewer, S. and Chambers, F. M. and Christen, J. A.
                      and Gallego-Sala, A. and Harrison, S. P. and Hughes, P. D.
                      M. and Jackson, S. T. and Korhola, A. and Mauquoy, D. and
                      Mitchell, F. J. G. and Prentice, I. C. and van der Linden,
                      M. and De Vleeschouwer, F. and Yu, Z. C. and Alm, J. and
                      Bauer, I. E. and Corish, Y. M. C. and Garneau, M. and Hohl,
                      V. and Huang, Y. and Karofeld, E. and Le Roux, G. and
                      Loisel, J. and Moschen, R. and Nichols, J. E. and Nieminen,
                      T. M. and MacDonald, G. M. and Phadtare, N. R. and Rausch,
                      N. and Sillasoo, Ü. and Swindles, G. T. and Tuittila, E.-S.
                      and Ukonmaanaho, L. and Väliranta, M. and van Bellen, S.
                      and van Geel, B. and Vitt, D. H. and Zhao, Y.},
      title        = {{C}limate-related changes in peatland carbon accumulation
                      during the last millennium},
      journal      = {Biogeosciences},
      volume       = {10},
      number       = {2},
      issn         = {1726-4189},
      address      = {Katlenburg-Lindau [u.a.]},
      publisher    = {Copernicus},
      reportid     = {FZJ-2015-03242},
      pages        = {929 - 944},
      year         = {2013},
      abstract     = {Peatlands are a major terrestrial carbon store and a
                      persistent natural carbon sink during the Holocene, but
                      there is considerable uncertainty over the fate of peatland
                      carbon in a changing climate. It is generally assumed that
                      higher temperatures will increase peat decay, causing a
                      positive feedback to climate warming and contributing to the
                      global positive carbon cycle feedback. Here we use a new
                      extensive database of peat profiles across northern high
                      latitudes to examine spatial and temporal patterns of carbon
                      accumulation over the past millennium. Opposite to
                      expectations, our results indicate a small negative carbon
                      cycle feedback from past changes in the long-term
                      accumulation rates of northern peatlands. Total carbon
                      accumulated over the last 1000 yr is linearly related to
                      contemporary growing season length and photosynthetically
                      active radiation, suggesting that variability in net primary
                      productivity is more important than decomposition in
                      determining long-term carbon accumulation. Furthermore,
                      northern peatland carbon sequestration rate declined over
                      the climate transition from the Medieval Climate Anomaly
                      (MCA) to the Little Ice Age (LIA), probably because of lower
                      LIA temperatures combined with increased cloudiness
                      suppressing net primary productivity. Other factors
                      including changing moisture status, peatland distribution,
                      fire, nitrogen deposition, permafrost thaw and methane
                      emissions will also influence future peatland carbon cycle
                      feedbacks, but our data suggest that the carbon
                      sequestration rate could increase over many areas of
                      northern peatlands in a warmer future.},
      cin          = {IBG-3},
      ddc          = {570},
      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:000315093000018},
      doi          = {10.5194/bg-10-929-2013},
      url          = {https://juser.fz-juelich.de/record/200874},
}