I think yes. First, in this scenario there really isn't much concept of environmental temperature, being a perfect vacuum. Perhaps you could say the CMB is there, then the environment is at 3 K or whatever it is, so lets go with that. This kind of radiation temperature is fairly different from the log being in some gaseous medium at 3K though.
Anyway, here is my vague reasoning. Say we have some infinitesimally thin slice of this log. The change in temperature of this part of the log is some function of the change in heat energy of the slice, I think just linear but it doesn't matter.
I figure a vague equation describing the change in heat energy of this slice is:
where

is the change in heat energy of the slice,

and

are radiative and conductive constants which depend on the wood etc,

is the temperature gradient of the slice and

is the average temperature of the slice.
Now if we go to a really long log then the temperature gradient in the slice goes to zero far from the heat source, so conduction is suppressed. At this point if the T is anything other than zero K then heat is lost (or if there is some environmental temperature until that temperature is reached). Basically a long log isolates the far end from the heat source, no matter how awesome a conductor of heat it is. Of course how long your log needs to be to achieve this condition depends a lot on how good a conductor it is.
Admittedly my equation above is kind of dodgy, not in the least because it doesn't take area into account, and an infinitesimal slice can't radiate out of the log because the exposed surface area is zero, but I think the logic more or less works. If we assume it is a bigger chunk, not so infinitesmal, then my argument is a bit more solid.