Timmermann Tania, Yip Christopher, Yang Yun-Ya, Wemmer Kimberly A, Chowdhury Anupam, Dores Daniel, Takayama Taichi, Nademanee Sharon, Traag Bjorn A, Zamanian Kazem, González Bernardo, Breecker Daniel O, Fierer Noah, Slessarev Eric W, Fuenzalida-Meriz Gonzalo A
Andes Ag, Inc., Alameda, California, USA.
Institute of Earth System Sciences, Section Soil Science, Leibniz University of Hannover, Hannover, Germany.
Glob Chang Biol. 2025 May;31(5):e70216. doi: 10.1111/gcb.70216.
Anthropogenic carbon emissions contribute significantly to the greenhouse effect, resulting in global warming and climate change. Thus, addressing this critical issue requires innovative and comprehensive solutions. Silicate weathering moderates atmospheric CO levels over geological time, but it occurs too slowly to counteract anthropogenic emissions effectively. Here, we show that the microorganism Bacillus subtilis strain MP1 promotes silicate weathering across different experimental setups with various levels of complexity. First, we found that MP1 was able to form a robust biofilm in the presence of feldspar and significantly increased (p < 0.05) silicate dissolution rates, pH, and calcium carbonate formation in culture experiments. Second, in mesocosm experiments, we found that MP1 enhanced the silicate weathering rate in soil by more than six times compared to the untreated control. In addition, soil inorganic carbon increased by 20%, and the concentrations of ions, including calcium, magnesium, and iron, were also elevated under the MP1 treatment. More importantly, when applied as a seed treatment on eight soybean fields, we found that MP1 significantly (p < 0.05) boosted soil inorganic carbon, leading to a gross accrual of 2.02 tonnes of inorganic carbon per hectare annually. Our findings highlight the potential of enhancing native silicate weathering with microorganisms in agricultural fields to increase soil inorganic carbon, contributing to climate change mitigation.
人为碳排放对温室效应有重大影响,导致全球变暖和气候变化。因此,解决这一关键问题需要创新和全面的解决方案。硅酸盐风化在地质时期可调节大气中的二氧化碳水平,但其发生速度过慢,无法有效抵消人为排放。在此,我们表明,微生物枯草芽孢杆菌MP1菌株在不同复杂度的实验设置中均能促进硅酸盐风化。首先,我们发现MP1在长石存在的情况下能够形成坚固的生物膜,并在培养实验中显著提高(p < 0.05)硅酸盐溶解速率、pH值和碳酸钙形成。其次,在中宇宙实验中,我们发现与未处理的对照相比,MP1使土壤中的硅酸盐风化速率提高了六倍以上。此外,土壤无机碳增加了20%,在MP1处理下,包括钙、镁和铁在内的离子浓度也有所升高。更重要的是,当在八个大豆田作为种子处理剂施用时,我们发现MP1显著(p < 0.05)提高了土壤无机碳,导致每年每公顷无机碳净增加2.02吨。我们的研究结果突出了利用微生物增强农田原生硅酸盐风化以增加土壤无机碳的潜力,有助于缓解气候变化。