Soil and Crop Sciences, School of Integrative Plant Science, Cornell University, Ithaca, NY, 14850, USA.
Department of Environmental Science and Forestry, The Connecticut Agricultural Experiment Station, New Haven, CT, 06511, USA.
Nat Commun. 2023 Oct 19;14(1):6609. doi: 10.1038/s41467-023-42291-6.
Calcium (Ca) can contribute to soil organic carbon (SOC) persistence by mediating physico-chemical interactions between organic compounds and minerals. Yet, Ca is also crucial for microbial adhesion, potentially affecting colonization of plant and mineral surfaces. The importance of Ca as a mediator of microbe-mineral-organic matter interactions and resulting SOC transformation has been largely overlooked. We incubated Ca labeled soils with CN labeled leaf litter to study how Ca affects microbial transformation of litter and formation of mineral associated organic matter. Here we show that Ca additions promote hyphae-forming bacteria, which often specialize in colonizing surfaces, and increase incorporation of litter into microbial biomass and carbon use efficiency by approximately 45% each. Ca additions reduce cumulative CO production by 4%, while promoting associations between minerals and microbial byproducts of plant litter. These findings expand the role of Ca in SOC persistence from solely a driver of physico-chemical reactions to a mediator of coupled abiotic-biotic cycling of SOC.
钙 (Ca) 可以通过介导有机化合物和矿物质之间的物理化学相互作用来促进土壤有机碳 (SOC) 的持久性。然而,Ca 对于微生物的附着也很关键,可能会影响植物和矿物质表面的定殖。Ca 作为微生物-矿物质-有机质相互作用的介质以及由此产生的 SOC 转化的重要性在很大程度上被忽视了。我们用 CN 标记的叶凋落物孵育 Ca 标记的土壤,以研究 Ca 如何影响凋落物的微生物转化和与矿物相关的有机质的形成。在这里,我们表明 Ca 的添加促进了菌丝形成细菌,这些细菌通常专门定殖在表面,并将凋落物分别增加大约 45%的微生物生物量和碳利用效率。Ca 的添加将累积 CO2 的产生减少了 4%,同时促进了矿物质和植物凋落物微生物副产物之间的结合。这些发现将 Ca 在 SOC 持久性中的作用从仅仅是物理化学反应的驱动因素扩展到 SOC 耦合的非生物-生物循环的介质。