LAUSR

Trace elements (and their isotopes) in carbonates are commonly used to reconstruct paleoenvironment and paleoclimate. Understanding the processes and mechanisms of element incorporation into carbonates is thus crucial for using such geochemical parameters as paleoclimate proxies. In contrast to laboratory-based experimental results, the partitioning of trace metals between solid and solution phases in natural carbonate precipitation systems has rarely been reported. In this study, we investigated the partition coefficients of metal ions between solid and solution in the channel of the natural Baishuitai travertine system, Yunnan, China. Our results show that the partition coefficients of Li + , Na + , Mg 2+ , Sr 2+ and Ba 2+ are < 1, that of Ni 2+ is approximately 1, and those of Co 2+ , Mn 2+ , Zn 2+ and Cu 2+ are > 1, consistent with the results found in previous experimental studies. Although the substitution for Ca 2+ is likely the main uptake process of these metals into calcite, depending on their ionic radius and charge, trace elements may also be incorporated by adsorption or physical entrapment. Our study shows that unlike laboratory experiments performed under specific conditions, the partitioning of metals between two phases in the natural travertine system could be controlled by several, even multiple, environmental factors (e.g., carbonate deposition rate, temperature, and pH), which should be taken into account when using trace metals (and their isotopes) in carbonate archives as a paleoclimate proxy.