我国东部沿海平原和丘陵山地在第四系地层及地貌上留有明显的海面变化证据。十多年来研究资料日益增加,逐步深入,并多同第四纪冰期进行了联系。但在对比中往往局限于阿尔卑斯的经典冰期概念,对于全新世的高海面尚有不同意见。本文拟就已发表的成果,对我国第四纪海平面的变化及其同冰期旋迴的关系提出尝试性的对比,供进一步研究。 Evidence of sea surface changes in the Quaternary stratigraphy and topography of eastern China’s coastal plains and hilly and mountainous areas remains evident. More than a decade of research data is increasing, gradually deepening, and more with the Quaternary ice age were linked. However, in contrast, the concept of classic ice ages in the Alps is often confined and there are different opinions on the high sea level of the Holocene. This article intends to make a tentative comparison of the published achievements with the changes of Quaternary sea level in China and its relationship with the glacial cycles, for further study.