An assessment and comparison of 230Th and AMS 14C ages for lacustrine sediments from Qarhan Salt Lake area in arid western China

The age framework of Qarhan Salt Lake in arid western China is still controversial due in part to (1) age discrepancy between conventional ¹⁴C and ²³⁰Th dating results, and (2) no AMS ¹⁴C ages of organic carbon from drilling cores in Qarhan Salt Lake were reported until now. In order to discuss these chronological problems, upper 54.50 m lacustrine sediments from a drilling core (ISL1A) recovered from Qarhan Salt Lake were dated based on ²³⁰Th and AMS ¹⁴C dating techniques. Results show that (1) AMS ¹⁴C ages of total organic carbon (TOC) from 4.65 to 30.29 m are almost in stratigraphic order and consistent with ²³⁰Th ages of halite in the corresponding layers; (2) AMS ¹⁴C ages of TOC from 30.29 to 54.50 m are younger with increasing depth. This phenomenon was also found in Shell Bar in the study area, suggesting that AMS ¹⁴C ages from upper 30.29 m are more reliable while those from lower 24.21 m in ISL1A may be underestimated; (3) ²³⁰Th ages of halite from lower 24 m lacustrine sediments are obviously older than AMS ¹⁴C ages of TOC in the corresponding layers, which results into different age framework of salt lake sediments in Qarhan Salt Lake; (4) if extrapolating these reliable AMS ¹⁴C ages in ISL1A, similar age framework with ²³⁰Th ages in this core confirms that ²³⁰Th ages are much close to the true ages of these sediments, which suggests that the forming timing of the bottom salt layer is ~50 ka.