Earth Through Time as an Exoplanet: Lessons for Exoplanet Astrobiology
Abstract
The Archean Earth represents the most alien biosphere for which we have data. Oxygenic photosynthesis was not the dominant primary production metabolism at the surface, as it is on modern-day Earth. Due to this, the atmospheric composition, climate, and ocean chemistry of the planet were all dramatically different than they are on today's planet, even though life was present at the time. These dramatic differences are instructive on biology in a planetary context. Furthermore, they provide an example of a "working inhabited planet" that would have different biosignatures, climates, and spectral features. We can thus use the lessons from the rock record to inform us about the possibilities for and improve our ability to search for life. When we do that, we discover that by looking strictly for the "traditional" biosignatures from methane, oxygen, and ozone, we may conclude dead planets to be alive and living planets to be dead. In some cases, we may not even be looking for life on the right planets. In this talk, we will discuss these issues and their implications for future space-based observatories designed to search for life beyond the solar system.
- Publication:
-
Habitable Worlds Across Time and Space
- Pub Date:
- April 2014
- Bibcode:
- 2014hwat.confP..10D