Abstract
Solar radiation and geological processes over the first few million
years of Earth’s history, followed soon thereafter by the origin of
life, steered our planet towards an evolutionary trajectory of
long-lived habitability that ultimately enabled the emergence of complex
life. We review the most important conditions and feedbacks over the
first 2 billion years of this trajectory, which perhaps represent the
best analogue for other habitable worlds in the galaxy. Crucial aspects
included: (1) the redox state and volatile content of Earth’s building
blocks, which determined the longevity of the magma ocean and its
ability to degas H2O and other greenhouse gases, in particular CO2,
allowing the condensation of a water ocean; (2) the chemical properties
of the resulting degassed mantle, including oxygen fugacity, which
would have not only affected its physical properties and thus its
ability to recycle volatiles and nutrients via plate tectonics, but also
contributed to the timescale of atmospheric oxygenation; (3) the
emergence of life, in particular the origin of autotrophy, biological N2
fixation, and oxygenic photosynthesis, which accelerated sluggish
abiotic processes of transferring some volatiles back into the
lithosphere; (4) strong stellar UV radiation on the early Earth, which
may have eroded significant amounts of atmospheric volatiles, depending
on atmospheric CO2/N2 ratios and thus impacted the
redox state of the mantle as well as the timing of life’s origin; and
(5) evidence of strong photochemical effects on Earth’s sulfur cycle,
preserved in the form of mass-independent sulfur isotope fractionation,
and potentially linked to fractionation in organic carbon isotopes. The
early Earth presents itself as an exoplanet analogue that can be
explored through the existing rock record, allowing us to identify
atmospheric signatures diagnostic of biological metabolisms that may be
detectable on other inhabited planets with next-generation telescopes.
We conclude that investigating the development of habitable conditions
on terrestrial planets, an inherently complex problem, requires
multi-disciplinary collaboration and creative solutions.
Original language | English |
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Article number | 31 |
Number of pages | 37 |
Journal | Space Science Reviews |
Volume | 216 |
DOIs | |
Publication status | Published - 16 Mar 2020 |
Keywords
- Early Earth
- Biosignatures
- Atmospheric evolution