Climate Change Data Portal
DOI | 10.1038/s41559-022-01733-y |
Eukaryogenesis and oxygen in Earth history | |
Mills D.B.; Boyle R.A.; Daines S.J.; Sperling E.A.; Pisani D.; Donoghue P.C.J.; Lenton T.M. | |
发表日期 | 2022 |
ISSN | 2397-334X |
起始页码 | 520 |
结束页码 | 532 |
卷号 | 6期号:5 |
英文摘要 | The endosymbiotic origin of mitochondria during eukaryogenesis has long been viewed as an adaptive response to the oxygenation of Earth’s surface environment, presuming a fundamentally aerobic lifestyle for the free-living bacterial ancestors of mitochondria. This oxygen-centric view has been robustly challenged by recent advances in the Earth and life sciences. While the permanent oxygenation of the atmosphere above trace concentrations is now thought to have occurred 2.2 billion years ago, large parts of the deep ocean remained anoxic until less than 0.5 billion years ago. Neither fossils nor molecular clocks correlate the origin of mitochondria, or eukaryogenesis more broadly, to either of these planetary redox transitions. Instead, mitochondria-bearing eukaryotes are consistently dated to between these two oxygenation events, during an interval of pervasive deep-sea anoxia and variable surface-water oxygenation. The discovery and cultivation of the Asgard archaea has reinforced metabolic evidence that eukaryogenesis was initially mediated by syntrophic H2 exchange between an archaeal host and an α-proteobacterial symbiont living under anoxia. Together, these results temporally, spatially and metabolically decouple the earliest stages of eukaryogenesis from the oxygen content of the surface ocean and atmosphere. Rather than reflecting the ancestral metabolic state, obligate aerobiosis in eukaryotes is most probably derived, having only become globally widespread over the past 1 billion years as atmospheric oxygen approached modern levels. ? 2022, Springer Nature Limited. |
语种 | 英语 |
scopus关键词 | oxygen; archaeon; atmosphere; eukaryote; fossil; human; hypoxia; metabolism; Archaea; Atmosphere; Eukaryota; Fossils; Humans; Hypoxia; Oxygen |
来源期刊 | Nature Ecology & Evolution
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257065 |
作者单位 | Department of Geological Sciences, Stanford University, Stanford, CA, United States; Department of Biology, Portland State University, Portland, OR, United States; The Penn State Extraterrestrial Intelligence Center, The Pennsylvania State University, University Park, PA, United States; Global Systems Institute, University of Exeter, Exeter, United Kingdom; Bristol Palaeobiology Group, School of Earth Sciences, University of Bristol, Bristol, United Kingdom; School of Biological Sciences, University of Bristol, Bristol, United Kingdom |
推荐引用方式 GB/T 7714 | Mills D.B.,Boyle R.A.,Daines S.J.,et al. Eukaryogenesis and oxygen in Earth history[J],2022,6(5). |
APA | Mills D.B..,Boyle R.A..,Daines S.J..,Sperling E.A..,Pisani D..,...&Lenton T.M..(2022).Eukaryogenesis and oxygen in Earth history.Nature Ecology & Evolution,6(5). |
MLA | Mills D.B.,et al."Eukaryogenesis and oxygen in Earth history".Nature Ecology & Evolution 6.5(2022). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。