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- W4385301829 abstract "Amino acid geochronology is a well-established dating technique used in a wide range of Quaternary sciences. The primary geochronometer is the extent of racemization of amino acids preserved in a variety of organic remains. As a relative-dating tool, it is used to distinguish and correlate units, identify unconformities, and quantify the distribution of ages within fossil assemblages, among other applications. As a calibrated-dating method, it is used to estimate numerical ages by calibrating the rate of racemization against other dating techniques in a regional context. Where ages are known, the method can also be used for paleothermometry." @default.
- W4385301829 created "2023-07-28" @default.
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- W4385301829 date "2023-01-01" @default.
- W4385301829 modified "2023-09-23" @default.
- W4385301829 title "Amino acid geochronology" @default.
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- W4385301829 doi "https://doi.org/10.1016/b978-0-323-99931-1.00078-7" @default.
- W4385301829 hasPublicationYear "2023" @default.
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