Earth: Atmospheric Evolution of a Habitable Planet

Reference work entry


Our present-day atmosphere is often used as analog for potentially habitable exoplanets, but Earth’s atmosphere has changed dramatically throughout its 4.5-billion-year history. For example, molecular oxygen is abundant in the atmosphere today but was absent on the early Earth. Meanwhile, the physical and chemical evolution of Earth’s atmosphere has also resulted in major swings in surface temperature, at times resulting in extreme glaciation or warm greenhouse climates. Despite this dynamic and occasionally dramatic history, the Earth has been persistently habitable – and, in fact, inhabited – for roughly four billion years. Understanding Earth’s momentous changes and its enduring habitability is essential as a guide to the diversity of habitable planetary environments that may exist beyond our solar system and for ultimately recognizing spectroscopic fingerprints of life elsewhere in the universe.

Here, we review long-term trends in the composition of Earth’s atmosphere as it relates to both planetary habitability and inhabitation. We focus on gases that may serve as habitability markers (CO2, N2) or biosignatures (CH4, O2), especially as related to the redox evolution of the atmosphere and the coupled evolution of Earth’s climate system. We emphasize that in the search for Earth-like planets, we must be mindful that the example provided by the modern atmosphere merely represents a single snapshot of Earth’s long-term evolution. In exploring the many former states of our own planet, we emphasize Earth’s atmospheric evolution during the Archean, Proterozoic, and Phanerozoic eons, but we conclude with a brief discussion of potential atmospheric trajectories into the distant future, many millions to billions of years from now. All of these “alternative Earth” scenarios provide insight to the potential diversity of Earth-like, habitable, and inhabited worlds.


Earth Habitability Biosignatures Astrobiology Oxygen 



The authors gratefully acknowledge the support from the NASA Astrobiology Institute, including support from the Alternative Earths team under Cooperative Agreement Number NNA15BB03A and the Virtual Planetary Laboratory under Cooperative Agreement Number NNA13AA93A. EWS also acknowledges support from the NASA Postdoctoral Program, administered by the Universities Space Research Association.


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Copyright information

© Springer International Publishing AG, part of Springer Nature 2018

Authors and Affiliations

  1. 1.NASA Astrobiology Institute and Department of Earth SciencesUniversity of California RiversideRiversideUSA
  2. 2.School of Earth and Atmospheric ScienceGeorgia Institute of TechnologyAtlantaUSA
  3. 3.Department of Earth SciencesUniversity of CaliforniaRiversideUSA
  4. 4.Blue Marble Space Institute of ScienceSeattleUSA

Section editors and affiliations

  • Victoria Meadows
    • 1
  • Rory Barnes
    • 2
  1. 1.Astronomy DepartmentUniversity of WashingtonSeattleUSA
  2. 2.Astronomy DepartmentUniversity of WashingtonSeattleUSA

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