氧烷
生物矿化
化学
胞外聚合物
X射线光电子能谱
高分辨率透射电子显微镜
矿物
透射电子显微镜
化学工程
材料科学
光谱学
纳米技术
有机化学
生物膜
地质学
工程类
古生物学
物理
量子力学
细菌
作者
Jian Xiao,Zhi-Lai Chi,Xiaodan Huang,Guanghui Yu
出处
期刊:Chemosphere
[Elsevier]
日期:2024-11-01
卷期号:367: 143660-143660
标识
DOI:10.1016/j.chemosphere.2024.143660
摘要
Extracellular polymeric substances (EPS), which envelop on fungal hyphae surface, interact strongly with minerals and play a crucial role in the formation of nanoscale minerals during biomineralization in nature environments. However, it remains poorly understood about the molecular mechanisms of nanominerals (i.e., iron nanominerals) formation in fungal EPS halos during fungus-mineral interactions. This process is vital because fungi typically grow attached to various mineral surfaces in nature. According to the changes of thickness of the fungal cell and EPS layers during the Trichoderma guizhouense NJAU 4742 and hematite cultivation experiments in this study, we found that fungal biomineralization could trigger the formation of EPS layers. Fe-dominated nanominerals, aromatic C (283-286.1 eV), alkyl C (287.6-288.3 eV), and carboxylic C (288.4-289.1 eV) were the dominant chemical groups on the EPS layers, as determined by nanoscale secondary ion mass spectrometry (NanoSIMS), high-resolution transmission electron microscope (HRTEM), and carbon 1s near-edge X-ray absorption fine structure (NEXAFS) spectroscopy. Further, evidence from Fe K-edge X-ray absorption near-edge structure (XANES) and X-ray photoelectron spectroscopy (XPS) spectra indicated that oxygen vacancy (O
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