Rb、Sr是一对亲石分散元素,由于它们独特的化学性质,在表生地球化学作用过程中,表现了特殊的地球化学行为。所以在地学研究中应用非常广泛,如矿物年龄的测定、古气候古环境的恢复、火成岩类岩石成因的研究等等。本文主要总结了以黄土沉积纪录为信息载体,利用Rb、Sr恢复古气候古环境变化信息方面的研究进展及存在问题,并提出今后在利用Rb、Sr指标再现古气候古环境的主要发展方向。 Rb, Sr is a pair of lithophile disperse elements that, due to their unique chemical properties, exhibit particular geochemical behavior during epigenetic geochemical processes. Therefore, it is widely used in geosciences research, such as the determination of mineral age, the restoration of palaeoclimate and paleoenvironment, the research of the genesis of igneous rock and so on. This paper mainly summarizes the research progress and existing problems of using loess sedimentary records as information carriers and utilizing Rb and Sr to restore paleoclimate and paleoenvironmental change information, and puts forward the future development direction of using paleobolism paleoenvironment using Rb and Sr indicators.