土(古典元素)
矿物
地质学
碳纤维
天体生物学
地球科学
环境科学
地球化学
材料科学
冶金
数学
生物
复合材料
复合数
数学物理
作者
Ke‐Qing Xiao,Mingyu Zhao,Oliver Moore,Yao Zhao,Xinnan Li,Clare Woulds,Peyman Babakhani,Benjamin Mills,William B. Homoky,Karen L. Johnson,Alessandro Tagliabue,Chao Liang,Yong‐Guan Zhu,Caroline L. Peacock
出处
期刊:The Innovation
[Elsevier BV]
日期:2024-11-19
卷期号:6 (1): 100737-100737
被引量:13
标识
DOI:10.1016/j.xinn.2024.100737
摘要
The balance between the degradation and preservation of organic carbon (OC) is vital for the modulation of atmospheric CO2 and O2 in the Earth system, which regulates short-term climate as well as oxygenation of the early Earth. The mineral carbon pump (MnCP) was recently proposed to describe how soil minerals enhance the persistence and accumulation of OC, where interactions with minerals stabilize labile OC against microbial degradation (including via sorption, occlusion, aggregation, geopolymerization, and redox reactions).1 Given the widespread occurrence of metal (oxyhydr)oxides and clay minerals in terrestrial and marine environments and building on recent progress in mineral-OC interactions, we suggest that the MnCP occurs across the Earth system, where it plays a key role in OC preservation and hence the global carbon and oxygen cycles (Figure 1).
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