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Published on: July 24, 2016
Eukaryogenesis and oxygen in Earth history
Daniel B Mills1,2,3, Richard A Boyle4, Stuart J Daines4
1Department of Geological Sciences, Stanford University, Stanford, CA, USA. dbmills@stanford.edu.
The origin of mitochondria and early eukaryotes likely occurred in anoxic deep seas, not due to surface oxygenation. This challenges the long-held aerobic hypothesis for early mitochondrial evolution.
Area of Science:
- Origin of life
- Eukaryogenesis
- Biogeochemistry
Background:
- The endosymbiotic origin of mitochondria is traditionally linked to Earth's oxygenation.
- This view presumes an aerobic lifestyle for bacterial ancestors of mitochondria.
- Recent findings challenge this oxygen-centric perspective.
Purpose of the Study:
- To re-evaluate the environmental conditions and metabolic drivers of early eukaryogenesis and mitochondrial origin.
- To investigate the timing of eukaryogenesis relative to planetary redox transitions.
Main Methods:
- Analysis of fossil and molecular clock data.
- Integration of recent advances in Earth and life sciences.
- Consideration of metabolic evidence from Asgard archaea.
Main Results:
- Mitochondria-bearing eukaryotes predate the permanent rise of atmospheric oxygen and deep-sea anoxia.
- Eukaryogenesis is linked to anoxic deep-sea environments.
- Metabolic evidence suggests syntrophic H2 exchange between archaea and alpha-proteobacteria under anoxia.
Conclusions:
- The earliest stages of eukaryogenesis and mitochondrial origin are decoupled from surface oxygen levels.
- Obligate aerobiosis in eukaryotes is likely a derived trait, not ancestral.
- Early eukaryogenesis occurred in anoxic environments, challenging traditional views.
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