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@ARTICLE{Haberzettl:57072,
      author       = {Haberzettl, T. and Wille, M. and Fey, M and Janssen, S. and
                      Lücke, A. and Mayr, C. and Ohlendorf, C. and Schäbitz, F.
                      and Schleser, G. H. and Zolitschka, B.},
      title        = {{E}nvironmental change and fire history of southern
                      {P}atagonia ({A}rgentina) during the last five centuries},
      journal      = {Quaternary international},
      volume       = {158},
      issn         = {1040-6182},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {PreJuSER-57072},
      pages        = {72 - 82},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Geochemical, geophysical, charcoal and pollen analyses from
                      the very poorly investigated southern Patagonian steppe area
                      show that in the vicinity of Laguna Potrok Aike (Santa Cruz
                      Province, Argentina) and north of the Strait of Magellan the
                      detectable impact of Europeans as explorers, settlers and
                      farmers on fire intensity, vegetation and lake ecosystems
                      started with first regional signs during the 1840s. A
                      massive anthropogenic impact on a supra-regional scale
                      followed as the result of the introduction of sheep farming
                      at the end of the 19th century. Furthermore, since the first
                      European explorations, fires in the steppe areas of
                      southernmost Patagonia as recorded at Laguna Potrok Aike
                      occurred contemporaneously in the steppe-forest ecotone
                      further west and probably also in the Andean forest itself.
                      Environmental changes which are not caused by anthropogenic
                      influence are also revealed and were most likely the result
                      of temperature variations and enhanced and reduced wind
                      speeds, respectively. A fire event around AD 1600, before
                      the arrival of European settlers, occurred during a dry
                      period in the forest and steppe-forest ecotone and followed
                      a wet phase in the steppe that caused favorable ignition
                      conditions in all environments. (c) 2006 Elsevier Ltd and
                      INQUA. All rights reserved.},
      keywords     = {J (WoSType)},
      cin          = {ICG-V},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB51},
      pnm          = {Geosysteme - Erde im Wandel},
      pid          = {G:(DE-Juel1)FUEK405},
      shelfmark    = {Geography, Physical / Geosciences, Multidisciplinary},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000242432600008},
      doi          = {10.1016/j.quaint.2006.05.029},
      url          = {https://juser.fz-juelich.de/record/57072},
}