LOESSFEST'09 | Aug. 31st – Sept. 3rd, 2009 |Novi Sad-Serbia

The Importance of Chronology in the Study of Loess: Developments in Luminescence Dating, and Future Challenges

Roberts, H. M.1

1Institute of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, Ceredigion, Wales, SY23 3DB

Intercalated deposits of loess and palaeosols are spread over vast geographic areas, and preserve important records of past climate change. Some key sites have been studied intensively over the years, revealing detailed fluctuations in various palaeoclimatic indicators. However, if these detailed site-specific studies are to be linked together in order to investigate the timing, nature, and extent of such palaeoclimatic fluctuations, it is essential to establish a reliable numerical chronology. Recent exciting developments in luminescence dating have revolutionised the dating technique, through significant improvements in both the precision and accuracy of optically stimulated luminescence (OSL) ages, and also as a result of the establishment and testing of new rigorous quality control checks for the OSL signals examined. The development of luminescence dating is inextricably linked to the study of loess deposits. Loess deposits have been an important testing ground for these newly developing luminescence dating techniques, and they continue to play a significant role today in developing the next generation of luminescence techniques.
The evolution of luminescence dating from the earliest days until the recent important technological advances will be outlined, and the current methods of choice will be explained. Having made significant advances in the dating of quartz, which is now almost considered routine in some geomorphological settings, attention has recently turned to new challenges. Current research is principally focussing on two key areas: 1) improving the reliability of dating using feldspars, which cover a longer dating range than quartz, but which still pose some potentially serious challenges for luminescence dating, and 2) using new luminescence signals to significantly extend the maximum age range achievable (e.g. by an order of magnitude). These more recent developments will be discussed, and likely future challenges will be considered.

Corresponding author: Helen Roberts| hmr@aber.ac.uk