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Beryllium isotopes in sediments from Lake Maruwan Oike and Lake Skallen, East Antarctica, reveal substantial glacial discharge during the late Holocene

HoloceneEngineeringPaleoenvironmental ChangeGeographyLake Maruwan OikeCryosphereLake SkallenGlacial ProcessGeochronologyBeryllium IsotopesSedimentologyEarth ScienceQuaternary Period