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@ARTICLE{Kock:873925,
      author       = {Kock, Sebastian T. and Schittek, Karsten and Mächtle,
                      Bertil and Maldonado, Antonio and Vos, Heinz and Lupo,
                      Liliana C. and Kulemeyer, Julio J. and Wissel, Holger and
                      Schäbitz, Frank and Lücke, Andreas},
      title        = {{M}ulti‐{C}entennial‐{S}cale {V}ariations of {S}outh
                      {A}merican {S}ummer {M}onsoon {I}ntensity in the {S}outhern
                      {C}entral {A}ndes (24–27°{S}) {D}uring the {L}ate
                      {H}olocene},
      journal      = {Geophysical research letters},
      volume       = {47},
      number       = {4},
      issn         = {1944-8007},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2020-01100},
      pages        = {e2019GL084157},
      year         = {2020},
      abstract     = {Oxygen isotope records of cushion‐plant peat cellulose
                      from the southern central Andes capture evidence for
                      significant environmental changes. We observe that the
                      δ18Ocell peatland record from Cerro Tuzgle (24°S) is in
                      high conformity with the respective Lagunillas peatland
                      record (27°S). During the late Holocene, two significant
                      fluctuations occurred and are interpreted as regional
                      moisture signals with increased precipitation amounts
                      indicated during multi‐centennial phases from 1,530 to
                      1,270 cal. yr BP and from 470 to 70 cal. yr BP. These
                      fluctuations can be best explained by changes in the
                      strength of the South American summer monsoon (SASM). This
                      interpretation is further supported by consistency with
                      northern Andean paleoclimate records (10–13°S) and very
                      high correlation (R2 = 0.76) with the Southern Oscillation
                      Index. The congruent precipitation signals suggest the
                      persistent climatic control of the SASM‐strength in this
                      latitudinal band during the last 1,800 years.},
      cin          = {IBG-3 / IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)IEK-7-20101013},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255) / 243 - Tropospheric trace substances and their
                      transformation processes (POF3-243)},
      pid          = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-243},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000529120100040},
      doi          = {10.1029/2019GL084157},
      url          = {https://juser.fz-juelich.de/record/873925},
}