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1876年布利特提出的冰后期气候分期方案认为,气温比现在向上或向下各波动1～2C。1969年拉姆认为,欧洲副热带高压轴移动约10个纬度,气温比前者高3～6倍。现今世界已发现一些全新世各高温期的物候证据,特别是中国发现的热带、亚热带的各种证据,在世界上是最多的。笔者发现,海滩岩的形成不仅代表热带气候(它成岩的年平均气温达到26.5°以上),而且它的每一个沉积成岩—沉积间断周期为500a左右,继而发现全新世海滩岩断代序列模式,又引伸出全新世热带、亚热带地层断代序列模式、全新世冰川地层断代序列模式,以及海岸升降周期断代序列模式等。笔者以中国历史的物候记载为旁证,又发现了中国全新世气候变化周期也是500a左右,即寒、暖半周期各为250a左右。距今10000～3100a期间的14个高温期。海滩岩的成岩区北界从西沙群岛以南逐渐“北进”,先后扩展到粤闽浙鲁等沿海;在距今2850a以来的6个小高温期的海滩岩成岩区北界先后“南移”到浙闽琼以南地区沉积成岩。在变寒半周期间,据目前所知,北纬40°至16°(西沙)海岸、岛屿皆不成岩。在高温期的海滩岩成岩区“北进”达到20多个纬度,变寒半周期的寒冷气候“南移”20多个纬度;热带动物反映的气候,“北进”和“南移”也18个纬度左右。表明海滩岩是研究古环境古气候的
In 1876, Brite proposed the post-ice climatic staging scheme to think that the temperature fluctuates from 1 to 2C upwards or downwards. 1969 Ram believes that the European subtropical high-pressure axis moves about 10 latitudes, the temperature is 3 to 6 times higher than the former. In the world today, some of the thermophilic evidences of all the Holocene periods have been discovered. In particular, the evidences of the tropical and subtropical regions found in China are the largest in the world. The author found that the formation of beach rocks not only represents the tropical climate (it is the annual average temperature of diagenesis reached 26.5 ° or more), and each of its depositional diagenesis - sedimentary interval of about 500a, and then found that the Holocene beach rock sequence model, and The extension of the Holocene tropical and subtropical stratigraphic sequence mode, Holocene glacial stratigraphic sequence mode, as well as the coast of the rise and fall of the sequence pattern. The author records the phenology of Chinese history as a circumstantial evidence and finds that the climate change cycle of the Holocene in China is also about 500 years, that is, the cold and warm half cycles are about 250 years each. 14 high temperature periods from 10000 to 3100a. Beach rock diagenetic zone north from the Xisha archipelago gradually “north”, has extended to Guangdong, Fujian and Zhejiang and other coastal areas; in 2850a since six small high-temperature beach rock pluton north boundary has “south To Zhejiang and Fujian Province Joan south sedimentary diagenesis. During the semi-chilling period, so far it is known that the islands between 40 ° and 16 ° N (Xisha) and the islands are not diagenetic. In the high-temperature period, the rocky diagenetic area of the beach reaches more than 20 latitudes northwards and over 20 latitudes for the cold climate of the cold-temperate half-period. The climate reflected by tropical animals, such as ”northward“ and ”southwardward" 18 latitude or so. Show that the beach rock is the ancient climate of ancient research