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Indication of millennial-scale moisture changes by the temporal distribution of Holocene calcareous root tubes in the deserts of the Alashan Plateau, Northwest China

ClimatologyHoloceneEngineeringDesertificationGeomorphologyNorthwest ChinaGeographyDrylandsGeologyMillennial-scale Moisture ChangesAlashan PlateauGeochronologyPaleoecologyArid EnvironmentEarth ScienceSocial SciencesQuaternary Period