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Mid- to late Holocene climate-driven regime shifts inferred from diatom, ostracod and stable isotope records from Lake Son Kol (Central Tian Shan, Kyrgyzstan)

HoloceneQuaternary PeriodEngineeringStable Isotope RecordsCentral Tian ShanPaleoenvironmental ChangeGeographyGeologyGeochemistryGeochronologyPaleoclimatologyEarth ScienceEarth's ClimateLake Son Kol