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@ARTICLE{Haberzettl:1495,
      author       = {Haberzettl, T. and Kück, B. and Wulf, S. and Anselmetti,
                      F. and Ariztegui, D. and Fey, M. and Janssen, S. and Lücke,
                      A. and Mayr, C. and Ohlendorf, C. and Schäbitz, F. and
                      Schleser, G. H. and Wille, M. and Zolitschka, B.},
      title        = {{H}ydrological variability and explosive volcanic activity
                      in southeastern {P}atagonia during {O}xygen {I}sotope
                      {S}tage 3 and the {H}olocene inferred from lake sediments of
                      {L}aguna {P}otrok {A}ike},
      journal      = {Palaeogeography, palaeoclimatology, palaeoecology},
      volume       = {259},
      issn         = {0031-0182},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {PreJuSER-1495},
      pages        = {213 - 229},
      year         = {2008},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Seismic reflection studies in the maar lake Laguna Potrok
                      Aike (51 degrees 58' S, 70 degrees 23' W) revealed an
                      erosional unconformity associated with a sub-aquatic
                      lake-level terrace at a water depth of 30m.
                      Radiocarbon-dated, multi-proxy sediment studies of a piston
                      core from this location indicate that the sediment below
                      this discontinuity has an age of 45kyr BP (Oxygen Isotope
                      Stage 3), and was deposited during an interval of high lake
                      level. In comparison to the Holocene section, geochemical
                      indicators of this older part of the record either point
                      towards a different sediment source or to a different
                      transport mechanism for Oxygen Isotope Stage 3 sediments.
                      Holocene sedimentation started again before 6790cal. yr BP,
                      providing a sediment record of hydrological variability
                      until the present. Geochemical and isotopic data indicate a
                      fluctuating lake level until 5310cal. yr BP. During the late
                      Holocene the lake level shows a receding tendency.
                      Nevertheless, the lake level did not drop below the 30m
                      terrace to create another unconformity. The geochemical
                      characterization of volcanic ashes reveals evidence for
                      previously unknown explosive activity of the Reclus and Mt.
                      Burney volcanoes during Oxygen Isotope Stage 3. (c) 2007
                      Elsevier B.V. All rights reserved.},
      keywords     = {J (WoSType)},
      cin          = {ICG-5},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB143},
      pnm          = {Geosysteme - Erde im Wandel},
      pid          = {G:(DE-Juel1)FUEK405},
      shelfmark    = {Geography, Physical / Geosciences, Multidisciplinary /
                      Paleontology},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000254695400009},
      doi          = {10.1016/j.palaeo.2007.10.008},
      url          = {https://juser.fz-juelich.de/record/1495},
}