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The Younger Dryas chronozone, recognised in northern high-latitude areas as a cold event between 11 000 and 10 000 14 C yr BP (12 900–11 600 cal. yr BP), seems to manifest itself globally in different ways. Here, we examine well-dated stratigraphic sequences together with high-resolution proxy data plots from sites across our study area, the arid–semi-arid transition zone in northern China...
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