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Updated: Jun 25, 2025

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Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
Published on: February 27, 2021
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Co-evolution of early Earth environments and microbial life
Timothy W Lyons1,2, Christopher J Tino3, Gregory P Fournier4
1Department of Earth and Planetary Sciences, University of California, Riverside, CA, USA. timothy.lyons@ucr.edu.
Nature Reviews. Microbiology
|May 29, 2024
Summary
Microbial life
Area of Science:
- Geobiology
- Geochemistry
- Molecular Biology
- Biospheric Evolution
Background:
- Earth's history is recorded in rocks and genomes.
- Early life is identified by isotopic fingerprints and biomarkers.
- Biospheric evolution is marked by the transition to an oxygen-rich world.
Purpose of the Study:
- To explore the history of microbial life on Earth.
- To understand how microbial life shaped and was shaped by Earth's chemical transitions.
- To examine early metabolic processes and their link to oxygenation.
Main Methods:
- Overlaying molecular lineages on geologic and geochemical records.
- Examining isotopic fingerprints, fossils, and organic biomarkers.
- Analyzing the coupling of metabolic processes with biogeochemical cycles.
Main Results:
- Microbial evolution is intrinsically linked to Earth's chemical and physical changes.
- Early metabolic processes influenced planetary environments.
- The oxygenation of the biosphere was a key transition driven by microbial life.
Conclusions:
- Microbial life played a pivotal role in shaping Earth's environment.
- The co-evolution of life and planet is evident through biogeochemical cycles.
- Understanding early metabolisms is crucial for comprehending Earth's history.
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