High-resolution records of carbon isotope composition and grey level were analysed from a stalagmite, BW-1, from Beijing, China, deposited between c. 14 and 10.5 ka BP, the δ18O profile of which has been used to discuss the timing and structure of the Younger Dryas (YD) event in north China. The high grey level and low δ13C match the milk-white coloured locations on the polished stalagmite surface and coincide with enhanced luminescent bands within which the concentration of both impurities and the total organic carbon (TOC) are high. Additionally, the fluorescence of speleothems was derived from organic acids that have been flushed onto the stalagmite surface along with impurities from the overlying soil by heavy summer rain and co-precipitated with the speleothem calcite. Thus, predominantly low δ13C and high grey level values indicate increased summer precipitation that supports abundant vegetation and robust biological productivity. Consequently, three distinct time intervals are defined by the palaeoenvironmental conditions expressed in the δ13C and grey level records of stalagmite BW-1: (i) a warm-humid stage (Pre-YD, 13.97 to 12.85 ka BP, including a hiatus from 12.99 to 13.21 ka BP reported before); (ii) a cool-arid stage (YD, 12.85 to 11.56 ka BP); and (iii) a warm-humid stage (Post-YD, 11.56 to 10.39 ka BP). The inferences based on our research are generally consistent with other regional vegetation and climatic records.