In the last stage of the Late Pleistocene, the main features of the sedimentary environment in China continental shelf were cold and dry.
在晚更新世末期，中国陆架环境的最显著特点是寒冷而干燥。
In the last stage of the Late Pleistocene, the main features of the sedimentary environment in China continental shelf were cold and dry.
在晚更新世末期，中国陆架环境的最显著特点是寒冷而干燥。
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