Holocene Climate Changes and Jomon Cultural Changes

比较整个全新世气候波动的峰值，例如，邦德事件，（8.2 ka、5.8 ka、4.3 ka、2.8 ka），对绳文陶器的放射性碳年代进行校准，表明每次气候变化都发生在四个考古阶段：绳文初期末期至绳文初期;绳文初期晚期至绳文中期早期;绳文中期晚期至绳文晚期早期;和晚终绳文到早弥生。特别是，8.2 ka事件的影响被记录在来自日本列岛各个地区的考古材料中，并反映在定居模式的时间顺序上：（1）定居定居点的解体;（2）游牧;（3）重新适应定居。

Comparing the peaks of climate fluctuations throughout the Holocene, for example, Bond events (8.2 ka, 5.8 ka, 4.3 ka, 2.8 ka), to calibrated radiocarbon dates of Jomon pottery indicates that each climatic change occurred during four archaeological phases: the final period of Incipient Jomon to Early Initial Jomon; Late Initial Jomon to Early Middle Jomon; Late Middle Jomon to Early Late Jomon; and Late Final Jomon to Early Yayoi. In particular, the influence of the 8.2 ka event was recorded in archaeological material from various areas in the Japanese archipelago and is reflected in the chronological order of settlement patterns: (1) disintegration of sedentary settlements; (2) nomadism; and (3) readaptation to sedentism.