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A high resolution optical dating study of the Mosti??tea loess-palaeosol sequence (SE Romania) using sand-sized quartz

机译:使用沙子大小的石英对Mosti ??茶黄土古土壤序列(罗马尼亚)的高分辨率光学测年研究

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We report on SAR-OSL dating of closely-spaced samples from the loess-palaeosol sequence near Mosti??tea lake (Danube Plain, SE Romania). We used sand-sized quartz and a SAR protocol that involved a preheat of 10s at 220?°C and a test dose cutheat to 180?°C. It is shown that these thermal pretreatments isolate a quartz OSL signal that is dominated by the fast component. The behaviour of this signal in the SAR protocol is then documented. The ratio of the measured to given dose tends to lie slightly but systematically above unity (a??5% on average) and the recycling ratio below unity (a??6% on average); for all samples, the recuperated signal is negligible. Within analytical uncertainty, the nineteen optical ages are internally consistent and agree with the predictions from a palaeomagnetic age-depth model. Although it may be possible to optimize the SAR measurement procedure, the optical ages already confirm the chronostratigraphic position of the uppermost welldeveloped palaeosol in that it formed during MIS 5. The established chronology allows correlating the sequence near Mosti??tea lake with that near Mircea Vod?? that we investigated earlier.
机译:我们报告了从Mosti ?? tea湖(多瑙河平原,SE罗马尼亚)附近的黄土古土壤序列中的近距离样品的SAR-OSL测年。我们使用了沙子大小的石英和SAR协议,该协议涉及在220°C的温度下预热10秒,并将测试剂量削减到180°C的温度。结果表明,这些热预处理可以隔离石英OSL信号,该信号主要由快速分量控制。然后记录该信号在SAR协议中的行为。所测得的剂量与给定剂量之比趋于稍微但有系统地高于统一性(平均a ?? 5%)和回收率低于统一性(平均a ?? 6%)。对于所有样品,恢复的信号可以忽略不计。在分析不确定性范围内,十九个光学年龄在内部是一致的,并且与古磁性年龄-深度模型的预测一致。尽管有可能优化SAR测量程序,但光学年龄已经确定了最发育良好的最上古土壤的年代地层位置,因为它是在MIS 5期间形成的。建立的年代学可以将Mosti ?? tea湖附近的序列与Mircea附近的序列相关联。点播我们之前调查过的

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