Luminescence dating of lacustrine sediments from T angra Y umco (southern T ibetan P lateau) using post‐ IR IRSL signals from polymineral grains

Radiocarbon dating of bulk organic matter is the most commonly used method for establishing chronologies of lake sediments for palaeoclimate reconstructions on the T ibetan P lateau. However, this method is likely to be problematic because the dated material often suffers from old carbon contamination. Recently, advances in luminescence‐based chronological techniques have provided new options for dating lacustrine sediments. In the current study, we tested for the first time the applicability of a new post‐ IR IRSL ( pIRIR ) measurement protocol for dating fine‐grained polymineral material from a deep‐lake sediment core from the central part of T angra Y umco, on the southern T ibetan P lateau. Our results show that: (i) radioactive disequilibria in the uranium decay chain were observed in the studied lake sediments, and thus taken into account for dose rate calculation by using a dynamic modelling approach; (ii) the suitability and robustness of the pIRIR protocol measured at 150°C ( pIRIR 150 ) for our samples are confirmed by a set of luminescence characteristic tests as well as the agreement with an independent age control; (iii) turbidite deposition partly caused an insufficient resetting of luminescence signals and thus apparent overestimation in luminescence dating; (iv) compared with the luminescence‐based age‐depth model, the 14 C ages of bulk organic matter from the studied core generally yielded an age difference of ∼2 ka, which is attributed to hardwater reservoir effects in T angra Y umco. This study highlights the need for multi‐dating approaches of lake sedimentary archives on the T ibetan P lateau.