the holocene megathermal in china 中国全新世大暖期
P. in age. These discoveries infer that the temperature during the formation of the ice-wedge casts and the thawing-freezing folds might have dropped remarkably to 6~7℃ and that there might exist a sharp temperature-drop event in the Megathermal.
尤其值得注意的是全新世中期的冰楔假型形成,表明了大暖期气温的不稳定性。
参考来源 - 黄河源区冰楔假型群的发育及其古气候意义·2,447,543篇论文数据,部分数据来源于NoteExpress
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