Quartz ITL and TT-OSL signals were tested for dating of Amazonian sediments.
TT-OSL and ITL signals of quartz were well bleached in the modern sediments.
TT-OSL signal showed higher saturation doses and better results to determine burial ages.
Age uncertainties may result from dose rate changes through time.
The Xingu River had bottom channel 15–25 m higher than the current level during the Middle Pleistocene.