Text 1
Many astrobiologists argue that the seasonal fluctuations of methane detected in Mars’s atmosphere are strong indicators of active microbial life beneath the Martian surface. Because methanogenic microbes on Earth release methane as a metabolic byproduct, these researchers hypothesize that similar underground organisms are responsible for the Martian gas. They point to the sharp, localized spikes in methane levels as evidence of biological activity, arguing that abiotic geological processes would result in a far more uniform, steady release of gas over time.
Text 2
Geologist Elena Vance and colleagues argue that atmospheric methane on Mars can be entirely explained by serpentinization, an abiotic reaction between water and olivine rocks deep within the crust. Vance's team simulated Martian subsurface conditions and demonstrated that this geochemical process occurs in bursts when shifting tectonic stresses fracture Martian rocks, exposing new mineral faces to trapped water. Consequently, Vance cautions against interpreting sudden spikes in Martian methane as signs of life, noting that geological stress cycles are naturally episodic rather than continuous.
Based on the passages, how would Elena Vance and colleagues (Text 2) most likely characterize the argument made by the astrobiologists (Text 1) regarding the significance of Mars's localized methane spikes?
- ABy arguing that Martian atmospheric methane levels do not actually undergo the seasonal fluctuations described in Text 1.
- By suggesting that the astrobiologists underestimate the capacity of abiotic reactions to produce non-continuous emissions of gas.Cevap
- CBy asserting that the presence of underground liquid water on Mars makes the existence of methanogenic microbes impossible.
- DBy concluding that the geological processes releasing methane are triggered by the activity of subsurface organisms.