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@ARTICLE{Heyng:203171,
      author       = {Heyng, Alexander M. and Mayr, Christoph and Lücke, Andreas
                      and Moschen, Robert and Wissel, Holger and Striewski, Bernd
                      and Bauersachs, Thorsten},
      title        = {{M}iddle and {L}ate {H}olocene paleotemperatures
                      reconstructed from oxygen isotopes and {GDGT}s of sediments
                      from {L}ake {P}upuke, {N}ew {Z}ealand},
      journal      = {Quaternary international},
      volume       = {374},
      issn         = {1040-6182},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {FZJ-2015-05176},
      pages        = {3 - 14},
      year         = {2015},
      abstract     = {Quantitative Holocene temperature reconstructions for
                      Southern Hemisphere terrestrial environments are still
                      restricted to few records, and multi-proxy methods are
                      rarely applied to the same system. Here, we test the
                      applicability and comparability of temperature
                      reconstructions inferred from different methodological
                      approaches. We combined sedimentary cellulose and diatom
                      oxygen isotope data from Lake Pupuke (North Island New
                      Zealand) to derive a record of lake water temperatures. This
                      record is complemented with mean annual air temperatures
                      derived from the branched GDGT index MBT measured on the
                      same sedimentary record. The datasets of both
                      reconstructions show little temperature variation for the
                      period 1320–7110 cal. BP. The exceptions are a warmer
                      period culminating between 1700 and 1600 cal. BP reflected
                      in both proxies and centennial-scale intervals with cooler
                      water temperatures at 3380 and 2750 cal. BP recorded in the
                      oxygen-isotope-based temperature reconstruction but not in
                      the MBT-inferred air temperature estimates. We suggest that
                      variations in lake circulation are the likely reason for
                      deviations between temperature reconstructed from different
                      proxies.},
      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:000356452500002},
      doi          = {10.1016/j.quaint.2014.12.040},
      url          = {https://juser.fz-juelich.de/record/203171},
}