Articles | Volume 12, issue 5
https://doi.org/10.5194/cp-12-1165-2016
https://doi.org/10.5194/cp-12-1165-2016
Research article
 | 
13 May 2016
Research article |  | 13 May 2016

A high-altitude peatland record of environmental changes in the NW Argentine Andes (24 ° S) over the last 2100 years

Karsten Schittek, Sebastian T. Kock, Andreas Lücke, Jonathan Hense, Christian Ohlendorf, Julio J. Kulemeyer, Liliana C. Lupo, and Frank Schäbitz

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Cited articles

Abbott, M. B., Seltzer, G. O., Kelts, K. R., and Southon, J.: Holocene paleohydrology of the tropical Andes from lake records, Quaternary Res., 47, 70–80, https://doi.org/10.1006/qres.1996.1874, 1997.
Aldous, A. R.: Nitrogen retention by Sphagnum mosses: responses to atmospheric nitrogen deposition and drought, Can. J. Bot., 80, 721–731, https://doi.org/10.1139/b02-054, 2002.
Asada, T., Warner, B. G., and Aravena, R.: Nitrogen isotope signature variability in plant species from open peatland, Aquat. Bot., 83, 297–307, https://doi.org/10.1016/j.aquabot.2005.05.005, 2005.
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Short summary
Cushion peatlands are versatile climate archives for the study of past environmental changes. We present the environmental history for the last 2100 years of Cerro Tuzgle peatland, which is located in the NW Argentine Puna. The results reflect prominent late Holocene climate anomalies and provide evidence that Northern Hemisphere climate oscillations were extensive. Volcanic forcing at the beginning of the 19th century seems to have had an impact on climatic settings in the Central Andes
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