Boron isotope geochemistry of a brine-carbonate system in the Qaidam Basin, western China

• Published in: Sedimentary geology Vol. 383; pp. 293 - 302
• Main Authors: Zhang, Xiangru, Li, Qingkuan, Qin, Zhanjie, Fan, Qishun, Du, Yongsheng, Wei, Haicheng, Gao, Donglin, Shan, Fashou
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.04.2019
• Subjects: Boron isotopic composition; Brine-carbonate system; Influencing factors; Qaidam Basin; Salinity; Boron isotopic composition; Brine-carbonate system; Influencing factors; Qaidam Basin; Salinity
• ISSN: 0037-0738
• DOI: 10.1016/j.sedgeo.2019.02.011

The boron (B) isotope-pH proxy for marine carbonates has been widely used to reconstruct past ocean pH values. Unlike seawater, the apparent dissociation constant of boric acid (KB) and the δ11B values of brines from the terrestrial salt lakes in western China vary. However, relevant studies concerning the B isotope geochemistry of brine-carbonate systems in terrestrial salt lakes are limited. In this study, thirty-nine clastic samples from a sediment core (ISL1A) from the Qarhan Salt Lake in the Qaidam Basin were collected. These carbonates were analyzed for δ11B, B, Mg, Sr and Ca. Using our new data as well as published pH values, total dissolved solids (TDS), element concentrations, and δ11B values of brines in western China, we reached the following conclusions. (1) During evaporation process, salinity increases, the δ11B values of brines in salt lakes increase, and the pKB (−logKB) and pH values simultaneously decrease. (2) The large heterogeneity in the δ11B values of the carbonates (−2.74‰ to +7.64‰) from core ISL1A is mainly due to the δ11B values of the brines, rather than pKB and pH. (3) B isotopic fractionation with a small αcarbonate-brine of 0.997 in a brine-carbonate system conforms to the Rayleigh fractionation model. (4) Our comparison of the δ11B values of these carbonates with other records from core ISL1A suggests that the δ11B values of the carbonates in the arid Qaidam Basin can be used as a new proxy for the salinity of paleo-lake water. •δ11B and B, Mg, Sr, Ca concentrations of carbonates in ISL1A were analyzed.•δ11B of carbonates are influenced by δ11B of brine rather than pH or pKB.•B isotopic fractionation in a brine-carbonate system conforms to Rayleigh model.•High (low) δ11B correspond to high (low) Mg/Ca, Sr/Ca ratios of carbonates.•δ11B of carbonates in salt lakes can indicate salinity of lake water.