| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4725097 | Quaternary Geochronology | 2012 | 5 Pages |
Optically stimulated luminescence (OSL) dating technique is a reliable method to determine the ages of sand dune sediments. While it seems logical to assume that for these windblown materials (such as sand dune sediments) grains from different sized fractions are suitable for optical dating and would yield identical ages, this was not previously explicitly demonstrated yet. In this study, six samples were selected from the sand dunes intercalated in loess strata near Lanzhou, western Chinese Loess Plateau, and different grain-size quartz fractions (e.g. 38–63 μm, 90–150 μm, 150–200 μm, 200–250 μm and 250–300 μm) were extracted to compare the OSL ages of different grain-size quartz. The results show that: (1) quartz OSL ages derived from different grain-size fractions produce identical ages within errors, confirming that the ages resulting from both coarse silt-sized (or middle grain of 38–63 μm) and sand-sized (90–300 μm) quartz can represent the periods of sand dune accumulation; (2) the OSL ages of the selected sand dune samples fall into ca. 28–18 ka, suggesting that the sand dune accumulation occurred during the marine isotope stage 2 (MIS 2) in current study area, which might imply regional increased aridity on the western Chinese Loess Plateau.
► We compared quartz OSL ages of different grain-size fractions of sand dunes. ► OSL ages of different grain-size fractions produce identical ages within errors. ► Ages of silt-sized (38–63 μm) quartz represent the periods of sand dune accumulation. ► The OSL ages of the selected sand dune samples fall into ca. 28–18 ka. ► The sand dune accumulation might imply regional increased aridity during ca. 28–18 ka.
