If the "depositions" took that long of a time to slowly deposit around the bones...the bones would have been scavenged or rotted away long before becoming buried..
You DO realize that we
know many animal remains are lost precisely because they are not sequestered quickly enough from scavengers right?
As for the "rotted away" part, well that's a lot more complex than you are likely aware. Let's take coal (the area of my dissertation). Coal is formed
in part precisely because some anaerobic bacteria get to munch on the organic material. The key is that the organics are sequestered from oxidative processes early on. If aerobic bacteria or oxygen can get to the plant materials the materials will oxidize away leaving nothing or very different material. (as an aside actually we can see evidence of fires in coal forming bogs! The wood and plant material is charred and oxidized and when it is turned into coal it is known as
fusinite or
fusain and has a very unique appearance with a very high reflectivity under the microscope!)
Now for
bones we are talking inorganic material with organics shot through it. The inorganic material will not necessarily "rot away" (so even today you can find bones of animals that died in the forest). The bones are buried and
permineralized in most cases (meaning they are replaced, very slowly, by minerals carried dissolved in ground water.
Think about how slowly groundwater moves through the earth. Now imagine that you have groundwater that has tiny amounts of silica or calcium carbonate dissolved in it that move through, dissolve the old bone material and replace it with
new minerals. That takes time, no matter how you slice it.
Even if your wildest dreams of "rapid burial" were the norm for all fossils you'd still have to account for those that are permineralized.
You will have to know the following things:
1. What is the replacement mineral?
2. What is the chemistry of the groundwater?
3. What is the solubility of the replacement mineral in the given groundwater chemistry (pH, Eh, etc.)
4. What is the
permeability and porosity of the rock through which the ground water had to pass?
If you know
how much permineralization has occurred and you know how
soluble that new mineral is in the groundwater, and you know how quickly the groundwater could move through the rock, you will have an estimate of the taphonomic processes.