Comparison of the YM section records with various other regional and global environmental signals (IMAGE)
Caption
The climate records of the Yumin Site and others in the surrounding areas indicated a significant increase of precipitation during the early Holocene (Figure a-f), while the soil formation (Figure g), increased woody plants (Figure h) and organic matter (Figure i), and agricultural origin (Figure j) in the Yumin Site and its surrounding areas were discovered in the middle Holocene.
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