微观世界
土壤水分
土壤碳
总有机碳
磷
生态系统
土壤科学
土壤有机质
环境化学
农学
土壤肥力
化学
环境科学
土壤生态学
土壤质量
氮气
有机质
大块土
土工试验
土壤结构
碳纤维
自行车
土壤pH值
土壤形态
土壤功能
生态学
生物地球化学
土壤分类
生物地球化学循环
土壤化学
营养物
碳循环
作者
Peilei Hu,Wei Zhang,Wolfgang Wanek,Ji Chen,Diego Ábalos,Jie Zhao,Dan Xiao,Xinyu Hou,Juan Li,Hongsong Chen,Jun Xiao,Xionghui Liao,Tiangang Tang,Hanqing Wu,Kelin Wang
标识
DOI:10.1038/s43247-025-02761-9
摘要
Parent material shapes soil properties, yet its effects on soil functions and microbial networks remain unclear. Here we investigate these relationships using a large-scale field survey comparing soils derived from calcium-rich carbonate rocks and calcium-poor clastic rocks, complemented by a microcosm experiment. Soils from calcium-rich parent materials contained 33% higher organic carbon, 58% higher total nitrogen, and 55% higher total phosphorus than calcium-poor soils, yet lower labile carbon and several hydrolytic enzyme activities, with similar water retention. Calcium-rich soils exhibited greater bacterial network complexity, which associated with enhanced soil functions. Within calcium-rich soils, rock and soil calcium were primary drivers of increased carbon, nitrogen, and phosphorus storage and bacterial network complexity. The microcosm experiment confirmed that calcium-rich rock addition stimulated soil carbon and nitrogen cycling and enhanced bacterial network complexity, even in calcium-rich soils. These findings indicate calcium-rich parent materials can play a pivotal role in improving soil ecosystem services. Soils from calcium-rich parent materials contained 33% higher organic carbon, 58% higher total nitrogen, and 55% higher total phosphorus than calcium-poor soils enhanced bacterial network complexity and soil functions, according to a large-scale field survey in Guangxi and Guizhou, China.
科研通智能强力驱动
Strongly Powered by AbleSci AI