陆地和海洋大范围的古气候指标说明了中至晚白垩世早期（阿尔必—科尼亚阶）是过去２００Ｍａ中地球历史上最温暖的时期（全球平均表层水温比目前高６～１４℃）。然而，通常只基于低反照率和高气压（Ｐｃｏ２）的气候模型模拟产生了较高的赤道海洋表层水温（ＳＳＴｓ），... The wide range of paleoclimatic indicators on land and in the ocean shows that the mid-to-late Cretaceous (Arbil-Konya) is the warmest period in the history of the Earth in the past 200 Ma (the average global surface water temperature is 6-14 ° C higher than at present) . However, climatic models that are generally based on low albedo and high atmospheric pressure (Pco2) models produce higher equatorial ocean surface water temperatures (SSTs), ...