Articles | Volume 12, issue 5
Clim. Past, 12, 1165–1180, 2016
https://doi.org/10.5194/cp-12-1165-2016

Special issue: Climate change and human impact in Central and South America...

Clim. Past, 12, 1165–1180, 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 et al.

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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.
Baker, P. A., Seltzer, G. O., Fritz, S. C., Dunbar, R. B., Grove, M. J., Tapia, P. M., Cross, S. L., Rowe, H. D., and Broda, J. P.: The history of South American tropical precipitation for the past 25 000 years, Science, 291, 640–643, https://doi.org/10.1126/science.291.5504.640, 2001.
Binford, M. W., Kolata, A. L., Brenner, M., Janusek, J. W., Seddon, M. T., Abbott, M., and Curtis, J. H.: Climate variation and the rise and fall of an Andean civilization, Quaternary Res., 47, 235–248, https://doi.org/10.1006/qres.1997.1882, 1997.
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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