Holocene Climate Changes and Jomon Cultural Changes

例如，将Bond事件（8.2 ka, 5.8 ka, 4.3 ka, 2.8 ka）与绳纹陶器的校准放射性碳年代进行比较，表明每次气候变化都发生在四个考古阶段：早期绳纹到早期绳纹的最后阶段；早期绳文晚期至中期绳文早期；绳文中晚期至绳文晚期早期；绳纹晚期到弥生早期。特别是，8.2 ka事件的影响记录在日本列岛各地区的考古材料中，并反映在聚落模式的时间顺序上：(1)定居聚落的解体；(2)流浪;(3)重新适应定居主义。

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.