Using a portable luminescence reader for rapid age assessment of aeolian sediments for reconstructing dunefield landscape evolution in southern Africa

被引:21
作者
Stone, A. [1 ]
Bateman, M. D. [2 ]
Burrough, S. L. [3 ]
Garzanti, E. [4 ]
Limonta, M. [4 ]
Radeff, G. [4 ]
Telfer, M. W. [5 ]
机构
[1] Univ Manchester, Dept Geog, Manchester M13 9PL, Lancs, England
[2] Univ Sheffield, Dept Geog, Winter St, Sheffield S10 2TN, S Yorkshire, England
[3] Univ Oxford, Sch Geog & Environm, South Parks Rd, Oxford OX1 3QY, England
[4] Univ Milano Bicocca, Dept Earth & Environm Sci, Lab Provenance Studies, I-20126 Milan, Italy
[5] Plymouth Univ, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England
关键词
OSL dating; Portable luminescence reader (POSL); Rapid age assessment; Dunefield dynamics; Aeolian sediments; Landscape evolution; Drylands; Quaternary environments; LINEAR DUNE ACCUMULATION; CANAL SEDIMENTS; GROWTH-CURVES; MEKONG DELTA; ANGKOR BOREI; QUARTZ; CHRONOLOGIES; KALAHARI; PALEOCLIMATE; FELDSPAR;
D O I
10.1016/j.quageo.2018.03.002
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Analysis of sedimentary materials using a portable luminescence reader (or portable optically stimulated luminescence reader POSL), is a useful, rapid (a few minutes per sample), cost-effective and safe (not requiring exposure to chemicals) way to establish relative sample age. Moving beyond information that guides initial field interpretations, or develops targeted sampling strategies for full laboratory-based dating protocols, toward rapid age assessment has been more challenging. This study is the first demonstration of a simple, elegant and practical calibration of POSL signals into sample age estimates. This involved measuring the POSL signals from 144 samples with established published ages from across southern Africa, and a regression analysis. The data show that a regional-specific approach to calibration is needed, with regional patterns in POSL signals that are supported by 148 further undated samples. Four broad regions are defined: the Namib Sand Sea (NSS), the northern Kalahari (barchan dunes on the floor of Makgadigadi) (Nnk-MBa), the western Kalahari (WK) and the southern Kalahari (SK). Sample composition data, such as quartz-to-feldspar ratios (Q/F) appears to account for the largest contrasts within the dataset, whilst inherent POSL signal brightness and grain coloured-coatings (iron and clay) may also influence signals. The strength of the regressions (R-2 of 0.99, 0.93, 0.81 and one moderate at 0.52 for the NSS, SK, WK and NnK-MBa respectively) between POSL signals and sample age, (for ages back to 118, 104 74 and 5 ka for the NSS, SK, WK and NnK-MBa respectively), demonstrates the practicality and huge value of this simple approach. The implication is that region-specific calibrations must be built prior to using the POSL reader for rapid age assessments. This approach is a cost and time-effective method for inter-dunefield landscape-scale analyses, which will cast light on the key climatic variables driving landscape change in sand-rich drylands during the Late Quaternary, and also has the potential for large-scale analysis within other geomorphic settings.
引用
收藏
页码:57 / 64
页数:8
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