摘要
///The alkenone unsaturation paleothermometer has been successfully and widely applied to reconstructing SST in most oceanographic settings.The utility of the alkenone unsaturation index in the marine system has stirred the interest in the study of LCK in the limnic system, in the hope that it can also be used as a paleotemperature proxy in lacustrine sediments. Empirical relationships between the alkenone unsaturation index U37k’and different tempera-ture sets(mean annual air temperature, mean annual air temperature in different seasons,and lake surface water temperature of July)were tested. The authors’ studies show that the alkenone unsaturation index U37k’is strongly controlled by environmental temperature the precursor organisms live in, and can be used for palaeoclimate reconstruction. This supports the suggestion that the biosynthetic pathway of alkenones and the mechanism of their temperature signal may be similar in both marine and limnic systems. LCK might be used as an important paleotemperature proxy in the limnic environment.