### Archean Atmospheric Composition
During the Archean Eon (approximately to billion years ago), the Sun's energy output was only to of its current value. Under these conditions, without a strong atmospheric greenhouse effect, Earth's surface water would have frozen completely. Yet, geological evidence shows that liquid oceans existed. Two scientists discuss the atmospheric conditions that resolved this "Faint Young Sun Paradox."
Scientist 1
The primary greenhouse gas keeping the Archean Earth warm was biogenic methane (), which was maintained at concentrations above by widespread methanogenic archaea. Carbon dioxide () was not abundant enough to prevent global glaciation. Basaltic rock weathering on the early continents was highly efficient, drawing out of the atmosphere and mineralizing it as carbonates. This weathering feedback restricted Archean atmospheric pressure to less than . Because atmospheric methane is unstable and rapidly destroyed by solar ultraviolet radiation (photodissociation), a continuous biological source was required. Without these methanogenic microbes, Earth would have immediately entered a global ice age.
Scientist 2
Methanogenic microbes had not yet evolved during the Archean, so biogenic methane was absent. Instead, Earth was kept warm by extremely high levels of carbon dioxide ()—reaching partial pressures of to —supplemented by volcanic hydrogen (). Basaltic weathering was negligible because continental landmasses were small and mostly submerged, preventing the drawdown of . Volcanic outgassing continuously supplied and to the atmosphere. Furthermore, collision-induced absorption between , , and significantly boosted the warming effect of these gases. The Archean climate was thus regulated entirely by abiotic, geochemical cycles.
According to the passage, Scientist 1 and Scientist 2 differ in their views regarding which of the following aspects of the Archean Earth?
- AThe presence of liquid oceans on the Earth's surface
- The atmospheric partial pressure of carbon dioxide ()Answer
- CThe percentage of current solar luminosity during the Archean Eon
- DThe vulnerability of methane molecules to photodissociation by solar ultraviolet radiation