Rock leachates were produced by adding 20 ml of sterile anoxic water to 10 g powdered core subsamples, incubating with a gentle stirring for 1 h at room temperature followed by centrifugation for 1 min at 10,000 rpm. The concentrations of inorganic anions and small molecular weight organic acids in the rock leachates were analysed by ion chromatography (Parro et al., 2011 (
link)). The pH of the water solutions was measured with an inoLab pH metre WTW (GmbH, Germany) after 24 h of solution stabilization. Fe
2+ and Fe
3+ were determined using the Reflectoquant test (Merk Millipore, Spain), and NH
4+ using a
DR6000 spectrophotometer and the reaction kit
LCK304 (HACH, USA) following the manufacturer's instructions. Total protein and sugar content were determined as follows: 1 g of sample (powder) was subjected to 3 × 1 min ultrasonic cycles in 2 ml of distilled water with 1–2 min stops by using a sonicator (Dr. Hielscher
50W DRH‐UP50H sonicator, Hielscher Ultrasonics, Germany). Samples were centrifuged at 2000
g to sediment the mineral particles, and the supernatants were directly assayed for protein concentration using the bicinchonitic acid protein assay reagent (Pierce, USA) (Smith et al., 1985 (
link)) and sugar content as described by Dubois et al. (1956 ), respectively. A NanoDropp (NanoDrop Int., USA) instrument was used for spectrophotometric measurements.
Amils R., Escudero C., Oggerin M., Puente Sánchez F., Arce Rodríguez A., Fernández Remolar D., Rodríguez N., García Villadangos M., Sanz J.L., Briones C., Sánchez‐Román M., Gómez F., Leandro T., Moreno‐Paz M., Prieto‐Ballesteros O., Molina A., Tornos F., Sánchez‐Andrea I., Timmis K., Pieper D.H, & Parro V. (2022). Coupled C, H, N, S and Fe biogeochemical cycles operating in the continental deep subsurface of the Iberian Pyrite Belt. Environmental Microbiology, 25(2), 428-453.