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Quantifying time scales of pedogenic calcrete formation using U-series disequilibria

Candy, I., Black, S. ORCID: and Sellwood, B. W. (2004) Quantifying time scales of pedogenic calcrete formation using U-series disequilibria. Sedimentary Geology, 170 (3-4). pp. 177-187. ISSN 0037-0738

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To link to this item DOI: 10.1016/j.sedgeo.2004.07.003


Time scales of pedogenic calcrete development are quantified by subsampling carbonate from within a mature (stage V) pedogenic calcrete profile from southeast Spain and dating the material by U-series disequilibria. The location of the earliest and latest cements can be estimated by comparing previous studies of calcrete morphological development with micromorphological analysis of the study profile. Carbonate was sampled and dated from three locations within the profile: (1) below the lower surface of clasts within the hardpan (representing the earliest cement present-207 +/- 11 ka), (2) from the centre of cement filled pores within the hardpan (reflecting the final plugging of the calcrete hardpan-155 +/- 9 ka) and (3) from the laminar calcrete overlying the hardpan (representing the latest cement-112 +/- 15 ka). These results show that the hardpan took between 73 and 31 ka to form, whilst the mature stage V profile took between 121 and 69 ka to form. This is the first time that rates of mature calcrete development have been established by direct radiometric dating of the authigenic carbonate. The technique is appropriate for dating mature calcretes in dryland regions worldwide and offers the opportunity of increasing our understanding of the spatial and temporal variability in rates of pedogenic calcrete development. (C) 2004 Elsevier B.V. All rights reserved.

Item Type:Article
Divisions:Science > School of Archaeology, Geography and Environmental Science > Department of Archaeology
Science > School of Archaeology, Geography and Environmental Science > Scientific Archaeology
ID Code:3342
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