Fossil dripwater in stalagmites reveals Holocene temperature and rainfall variation in Amazonia

Most proxy records used for reconstruction of Holocene climate of Amazonia are unable to quantitatively distinguish between the effect of temperature and rainfall amounts. We present a new isotope technique applied to a ∼ 13,500 yr stalagmite archive from Peruvian Amazonia. By analysing the coupled...

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Veröffentlicht in:	Earth and planetary science letters 2008-10, Vol.275 (1), p.54-60
Hauptverfasser:	van Breukelen, M.R., Vonhof, H.B., Hellstrom, J.C., Wester, W.C.G., Kroon, D.
Format:	Artikel
Sprache:	eng
Schlagworte:	fluid inclusions South America speleothem stable isotope
Online-Zugang:	Volltext
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