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• W2118139101 startingPage "109" @default.
• W2118139101 abstract "This pilot study shows that some calcrete nodules from the base of palaeosols in the Chinese loess sequences can be dated by U-series isochron methods. The ages obtained suggest that the nodules did not form during interglacial climate stages; rather, they formed either during interglacial/glacial transitions or glacial climate stages. Thus, the nodules appear not to have formed contemporaneously with the soils beneath which they immediately lie but significantly post-date them. Post-pedogenic injection of carbonate into stratigraphically lower horizons is therefore identified. This finding contradicts previous assumptions regarding the timing of nodule formation. Carbon and oxygen isotope analyses of the nodules identify isotopic compositions which independently suggest that climatic conditions cooler and possibly drier than at present prevailed at the time of nodule formation." @default.
• W2118139101 created "2016-06-24" @default.
• W2118139101 creator A5054536707 @default.
• W2118139101 creator A5068665443 @default.
• W2118139101 date "2000-03-01" @default.
• W2118139101 modified "2023-10-18" @default.
• W2118139101 title "‘Cold’ stage formation of calcrete nodules in the Chinese Loess Plateau: evidence from U-series dating and stable isotope analysis" @default.
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• W2118139101 doi "https://doi.org/10.1016/s0031-0182(99)00157-1" @default.
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