渡渡鸟是全新世晚期不会飞翔的鸟类。

Dodos are flightless birds from the late Holocene.

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研究结果表明，所研究的柱样沉积物下部形成于中全新世晚期，上部属于晚全新世。

The results show that the core sediments studied were formed in the late stage of Middle Holocene for the lower part and in Late Holocene for the upper part.

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西部地区地层中的粗颗粒含量相对较高，指示该地沙尘暴强度较大，这在全新世晚期表现尤为明显。

In late Holocene, relatively high crude particle content of the middle region section instructs the intensity of sandstorm of this place to be greater than the middle region.

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