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@ARTICLE{Striewski:5022,
      author       = {Striewski, B. and Mayr, C. and Flenley, J. and Naumann, R.
                      and Turner, G. and Lücke, A.},
      title        = {{M}ulti-proxy evidence of late {H}olocene human-induced
                      environmental changes at {L}ake {P}upuke, {A}uckland ({N}ew
                      {Z}ealand)},
      journal      = {Quaternary international},
      volume       = {202},
      issn         = {1040-6182},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {PreJuSER-5022},
      year         = {2009},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {New Zealand was the last major landmass in the world to be
                      colonised by people. Despite the short time-depth of human
                      presence in the country there is ongoing debate about the
                      date of earliest arrival of people that resulted in the
                      emergence of two contrasting colonisation hypotheses: the
                      Early hypothesis and the Short prehistory. To decide between
                      both hypotheses we employed a range of multi-proxy
                      investigations (geochemistry, stable isotopes and mineral
                      magnetism) on a lacustrine sequence from Lake Pupuke, a maar
                      lake in the city of Auckland and an area potentially among
                      the first places in New Zealand to have been colonised by
                      early people. The environmental history reconstructed from
                      the multi-proxy evidence identified a clear lack of
                      catchment disturbance from c. 2000 B.P. until several
                      decades before the eruption of the Rangitoto volcano. The
                      nature and abruptness of disturbance unambiguously point to
                      anthropogenic forcings and are likely to mark the onset of
                      prehistoric human colonisation at the site. Linear
                      interpolation between independently dated
                      tephrochronostratigraphic marker beds present in the
                      sediments allowed to date this event to c. 610 cal yr B.P.
                      This date is in compliance with the Short prehistory for
                      this region. (C) 2009 Elsevier Ltd and INQUA. All rights
                      reserved.},
      keywords     = {J (WoSType)},
      cin          = {ICG-4},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB793},
      pnm          = {Terrestrische Umwelt},
      pid          = {G:(DE-Juel1)FUEK407},
      shelfmark    = {Geography, Physical / Geosciences, Multidisciplinary},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000267570100008},
      doi          = {10.1016/j.quaint.2009.01.013},
      url          = {https://juser.fz-juelich.de/record/5022},
}