传统的历史,往往关注线性历史(linear history)与循环历史(cyclical history), 而在王明珂的研究中,他另辟蹊径,研究的是“根基历史”。何为“根基历史”?
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Recent studies of sediment in the North Atlantic's deep waters reveal possible cyclical patterns in the history of Earth's climate.
最近对北大西洋深海沉积物的研究揭示了地球气候历史上可能的循环模式。
There are many theories and hypotheses that attempt to explain this type of crisis and the dynamics behind the cyclical pattern of history (24).
也有许多理论和假设试图解释这种历史循环背后的危机以及波动的规律(24)。
This is also the fundamental reason for his cyclical theory of history.
这也是造成其历史循环论的根本原因。
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