Thanks for sticking with me on this. Your "conservation of energy" argument is clearly correct. If we presume a constant temperature for the moon, the constant incident energy from the sun has to be going somewhere. That which is reflected is reflected, and that which is absorbed is eventually emitted as infrared. But the details!
The first is that the applicable "mirror" question here whether the surface temperature of the sunlit side of a slow rotating astronomical body is independent of reflectivity, not whether the eventual core temperature of a uniformly lit body is independent. Are you confident that the same reasoning applies? I'm not yet.
Next, if we are phrasing our question as to whether one can start a fire with a magnifying glass, we clearly do care about the difference between visible sunlight and low temp infrared. For Munroe's argument to really work, the surface temperature needs to be proxy for the collectible visible light that would be used by a magnifying glass.
There's also the directionality: none of the visible light is going to be reflected toward the "dark" side. The thermal radiation is also directional, but not to the same extent. As we move toward greater reflectivity, presuming a bright full moon, we do get more of the total energy available on earth. How much more? I don't know.
Lastly, which we haven't discussed, there are options for insulating the heated object on earth that are optically transparent (to allow the concentrated light in) but infrared reflective (to prevent thermal radiation from escaping). I think this "privileges" the reflected sunlight so that we might indeed be able to achieve a higher temperature than the reflective moon surface in vacuum.
I feel like you recognize these factors also, by your caveats that you might be able to get "a little bit" higher than the surface temperature. Without committing to a number or methodology, your implication is that this "little" must is small relative to the surface temperature of the moon, rather than small relative to the optical temperature of the sun. While I agree that the surface temperature is related to the achievable temperature for collected reflected light, I still don't think that the exact temperature is a hard limit.
I'll try to bow out here and not take up more of your time. You've definitely helped me to think through the issues here. If you happen to be interested in a somewhat parallel situation, you might enjoy this article that describes a cyclical water collection system based on collecting solar energy through an aerogel during the day, then using a condenser optically coupled to the dark sky at night: https://www.nature.com/articles/s41467-018-03162-7. Only loosely related to Munroe's hypothetical, but shows a real application of some of the same concepts.
Edit: I just noticed a link on the second page of this thread that had some useful discussion that might interest you: https://physics.stackexchange.com/questions/370446/is-randal.... If you expand out all the comments on the answer, Shor seems to be making the same argument you are, and Lalinský is making a better version of mine.