Most possibly, instead of warm-water carbonates, the invasion of cool climate might lead the accumulation of temperate carbonates in the region around the turn.
随着寒冷气候的侵入，代替暖水碳酸盐的最可能是该界面附近的温带碳酸盐的堆积。
Most possibly, instead of warm-water carbonates, the invasion of cool climate might lead the accumulation of temperate carbonates in the region around the turn.
随着寒冷气候的侵入，代替暖水碳酸盐的最可能是该界面附近的温带碳酸盐的堆积。
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