Climate Change Data Portal
DOI | 10.1111/gbi.12317 |
A sluggish mid-Proterozoic biosphere and its effect on Earth's redox balance | |
Ozaki K.; Reinhard C.T.; Tajika E. | |
发表日期 | 2019 |
ISSN | 14724677 |
起始页码 | 3 |
结束页码 | 11 |
卷号 | 17期号:1 |
英文摘要 | The possibility of low but nontrivial atmospheric oxygen (O 2 ) levels during the mid-Proterozoic (between 1.8 and 0.8 billion years ago, Ga) has important ramifications for understanding Earth's O 2 cycle, the evolution of complex life and evolving climate stability. However, the regulatory mechanisms and redox fluxes required to stabilize these O 2 levels in the face of continued biological oxygen production remain uncertain. Here, we develop a biogeochemical model of the C-N-P-O 2 -S cycles and use it to constrain global redox balance in the mid-Proterozoic ocean–atmosphere system. By employing a Monte Carlo approach bounded by observations from the geologic record, we infer that the rate of net biospheric O 2 production was 3.5 -1.1 +1.4 Tmol year −1 (1σ), or ~25% of today's value, owing largely to phosphorus scarcity in the ocean interior. Pyrite burial in marine sediments would have represented a comparable or more significant O 2 source than organic carbon burial, implying a potentially important role for Earth's sulphur cycle in balancing the oxygen cycle and regulating atmospheric O 2 levels. Our statistical approach provides a uniquely comprehensive view of Earth system biogeochemistry and global O 2 cycling during mid-Proterozoic time and implicates severe P biolimitation as the backdrop for Precambrian geochemical and biological evolution. © 2018 The Authors. Geobiology Published by John Wiley & Sons Ltd |
关键词 | biogeochemical cyclebiogeochemistrybiosphereMonte Carlo analysisPrecambrianredox conditionssea waterastronomyatmospherebiodiversitychemistryoxidation reduction reactionseatheoretical modelAtmosphereBiodiversityEarth (Planet)Evolution, PlanetaryModels, TheoreticalOceans and SeasOxidation-ReductionSeawater |
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/133254 |
推荐引用方式 GB/T 7714 | Ozaki K.,Reinhard C.T.,Tajika E.. A sluggish mid-Proterozoic biosphere and its effect on Earth's redox balance[J]. Geobiology,2019,17(1). |
APA | Ozaki K.,Reinhard C.T.,&Tajika E..(2019).A sluggish mid-Proterozoic biosphere and its effect on Earth's redox balance.,17(1). |
MLA | Ozaki K.,et al."A sluggish mid-Proterozoic biosphere and its effect on Earth's redox balance".17.1(2019). |
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。