Using the Worldgen process I did for IMTU, I ended up with a fair amount of worlds with methane atmospheres and sophisticated enough biospheres for animals.
What would the big differences be in plant and animal life with methane?
Just saw a science vid mentioning that methane is a low entropy molecule in an oxygen-nitrogen mix. Perhaps internal oxygen cycles cracking methane via photosynthesis?
I have the following methane-cycle in my notes (that I think came from a TML post back in the late-90s) though I can't vouch for the feasibility:
Asimov suggested plants could use an analog of photoshythesis to split water into H and O, react the O with CH4 to form carbohydrates, and release H2 to the atmosphere. H2 breathing animals could eat the plants for the carbohydrates and exhale methane and water vapor. Such a process would lead to an atmosphere consisting largely of H2, NH4 and CH4.
I have the following methane-cycle in my notes (that I think came from a TML post back in the late-90s) though I can't vouch for the feasibility:
Asimov suggested plants could use an analog of photoshythesis to split water into H and O, react the O with CH4 to form carbohydrates, and release H2 to the atmosphere. H2 breathing animals could eat the plants for the carbohydrates and exhale methane and water vapor. Such a process would lead to an atmosphere consisting largely of H2, NH4 and CH4.
I think the underlying idea behind that quote was that this would be an "H abundant" planet so we have H off-gassing going on.
In any event, seeing this in a super earth or sub-Jovian is probably right. Also, density tends to rise with planet size (up to a point) so that helps make this plausible too on an Earth+ sized planet.
But as I wrote at the outset, I can't really vouch strongly one way or the other - this stuff ain't in my domain.
... but oxygen would be in short supply- perhaps its cheap to burn the methane for heat...