四、五十年前,正当中国罹难文革浩劫的岁月里,国际地球科学界却在深海海底取得了几十万年的沉积记录,证实了冰期旋回受地球轨道周期控制,将古气候学推进到机理研究的新阶段.改革开放之后不久,我国以黄土研究为核心的古气候研究,很快与国际接轨,成为我国地球科学的一大亮点,国际的第四纪研究出现了深海、黄土与冰芯三足鼎立的新局面.跨入21世纪,我国的古气候研究呈现出全方位发展的繁荣景象,国际地位蒸蒸日上,学术战线捷报频传.但与此同时,如何进一步依靠我国独特的自 Forty years ago, just as China was plagued by the Cultural Revolution, China’s international geoscience community recorded hundreds of thousands of years of sedimentary records on the deep seabed, confirming that the glacial cycles were controlled by the Earth orbit cycle and pushed paleoclimate research to The new phase of mechanism research.After the reform and opening up, the paleoclimate research centering on the loess research in our country soon became one of the highlights of the earth science in our country, and the international Quaternary studies showed the deep sea, loess and ice In the 21st century, the study of paleoclimate in our country has shown a prosperous all-around development, with its flourishing international status and its academic front. However, at the same time, how to further rely on China’s unique self-