An ideal atmospheric biosignature gas has a strong, distinguishable spectral signature, can accumulate to a detectable abundance, and has a biologically plausible production flux. Its abiotic sources should be small or identifiable from the planet's environmental context; its lifetime must be long enough for detection but compatible with continuing replenishment. A useful diagnosis may be a disequilibrium combination of gases rather than a single molecule.
A primary metabolic byproduct comes from reactions needed for energy generation, growth or biomass synthesis. Examples include methane from methanogenesis and oxygen released by oxygenic photosynthesis. A secondary metabolic byproduct results from specialized functions such as chemical defense, signaling or stress responses; dimethyl sulfide and chloromethane are examples. Secondary products can be chemically more distinctive but are often produced in much smaller amounts.
For modern Earth, molecular oxygen (O2) and nitrous oxide (N2O) are characteristic, predominantly biologically maintained atmospheric gases: oxygenic photosynthesis maintains the former, and microbial nitrogen cycling produces much of the latter. Ozone (O3) is also a classic remote biosignature, but is made photochemically from O2 rather than being a second independent metabolic product. If O2/O3 are counted as a two-gas observational pair, they diagnose the same oxygen reservoir.
The word “unique” needs qualification: no one gas is guaranteed to be biogenic on every planet. An oxygen biosignature false positive can arise from water loss or CO2 photochemistry in suitable environments, and nonbiological N2O production is possible. The modern terrestrial source attribution does not remove the need for context when interpreting another world.
Articles by others on the same topic
There are currently no matching articles.