17 samples were collected from aeolian and lacustrine profiles within the e
nvironment sensitive zone of the Loess Plateau, and an experimental method
was established which is suitable for pollen extraction from aeolian sedime
nt. A comparative study of pollen dating was carried out using the accelera
tor mass spectrometry (AMS) C-14 dating of known age samples, and then an e
xperiment with the pollen concentrates was performed. The results indicate
that pollen that has been deposited simultaneously with sediment in a stabl
e environment can provide reliable ages. This technique will provide a way
of improving the chronological framework for the Loess Plateau since the la
te Pleistocene. The C-14 dating was combined with field investigations, and
from the geological record within this zone, evidence was extracted of fou
r major monsoon precipitation changes during the transition from the late P
leistocene to Holocene.