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DOI | 10.1111/gbi.12375 |
The evolving redox chemistry and bioavailability of vanadium in deep time | |
Moore E.K.; Hao J.; Spielman S.J.; Yee N. | |
发表日期 | 2020 |
ISSN | 14724677 |
起始页码 | 127 |
结束页码 | 138 |
卷号 | 18期号:2 |
英文摘要 | The incorporation of metal cofactors into protein active sites and/or active regions expanded the network of microbial metabolism during the Archean eon. The bioavailability of crucial metal cofactors is largely influenced by earth surface redox state, which impacted the timing of metabolic evolution. Vanadium (V) is a unique element in geo–bio-coevolution due to its complex redox chemistry and specific biological functions. Thus, the extent of microbial V utilization potentially represents an important link between the geo- and biospheres in deep time. In this study, we used geochemical modeling and network analysis to investigate the availability and chemical speciation of V in the environment, and the emergence and changing chemistry of V-containing minerals throughout earth history. The redox state of V shifted from a more reduced V(III) state in Archean aqueous geochemistry and mineralogy to more oxidized V(IV) and V(V) states in the Proterozoic and Phanerozoic. The weathering of vanadium sulfides, vanadium alkali metal minerals, and vanadium alkaline earth metal minerals were potential sources of V to the environment and microbial utilization. Community detection analysis of the expanding V mineral network indicates tectonic and redox influence on the distribution of V mineral-forming elements. In reducing environments, energetic drivers existed for V to potentially be involved in early nitrogen fixation, while in oxidizing environments vanadate ((Formula presented.)) could have acted as a metabolic electron acceptor and phosphate mimicking enzyme inhibitor. The coevolving chemical speciation and biological functions of V due to earth's changing surface redox conditions demonstrate the crucial links between the geosphere and biosphere in the evolution of metabolic electron transfer pathways and biogeochemical cycles from the Archean to Phanerozoic. © 2020 John Wiley & Sons Ltd |
关键词 | alkali metalalkaline earth metalbioactivityenzymeenzyme activityinhibitormetabolismmicrobial activitynetwork analysisphosphateproteinredox conditionsreductionspeciation (chemistry)vanadium |
语种 | 英语 |
来源机构 | Geobiology |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/133193 |
推荐引用方式 GB/T 7714 | Moore E.K.,Hao J.,Spielman S.J.,et al. The evolving redox chemistry and bioavailability of vanadium in deep time[J]. Geobiology,2020,18(2). |
APA | Moore E.K.,Hao J.,Spielman S.J.,&Yee N..(2020).The evolving redox chemistry and bioavailability of vanadium in deep time.,18(2). |
MLA | Moore E.K.,et al."The evolving redox chemistry and bioavailability of vanadium in deep time".18.2(2020). |
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