Soil physicochemical parameters, including temperature, moisture, and electrical conductivity were measured on site with a handheld Thermometer (DT-847U; OneTemp Pty Ltd, Adelaide, SA, Australia) and a HydroSense II Soil Moisture Measurement System (Campbell Scientific Pty Ltd, Garbutt, QND, Australia). Soil pH was determined in deionized water by a pH/EC meter (900-P; TPS Pty Ltd, Brisbane, QND, Australia). Element composition of the soils was analyzed by inductively coupled plasma mass spectrometry (ICP-MS) (
Nexion 300Q; Perkin Elmer, Waltham, MA, USA) at LabWest Mineral Analysis Pty Ltd. in Perth, Australia. Detection limits for all elements were at the ng g
−1 level. Gold concentrations in soil samples were determined by the aqua regia method
23 (link). Briefly, soil samples were ground to 200 μm, mixed with 100% aqua regia (HCl:HNO
3 = 3:1), and digested at room temperature for 24 h. The supernatant obtained by centrifugation was analyzed by ICP-MS. Total carbon and nitrogen were analyzed by CSBP Lab (CSBP Fertilizers, Kwinana, WA, Australia) using the Dumas high temperature combustion method
50 (link).
Bohu T., Anand R., Noble R., Lintern M., Kaksonen A.H., Mei Y., Cheng K.Y., Deng X., Veder J.P., Bunce M., Power M, & Verrall M. (2019). Evidence for fungi and gold redox interaction under Earth surface conditions. Nature Communications, 10, 2290.