-sigh- yeah. We've heard it all before. But stratigraphy isn't quite as simple as all that. First off, the presence of "polystrate fossils" (not a technical term used in geology) was not a problem for 19th century geologists and, indeed, you don't just assume that all formations all accumulate at a slow rate. There is some evidence that occasionally formations accumulate relatively quickly. It doesn't really change the overall view of "deep time", but it does show that sedimentology can work over a variety of timescales.
You can learn more about it here:
"Polystrate" Tree Fossils
And again, even today we occasionally see rapid burial of items.
This was a surprise and interestingly enough there's a couple reasons for this:
1. Few people had bothered to check for organic preservation in rocks that old because, as one geologist noted: if you assume it isn't there why go to the effort to dig up these fossils only to digest them and crush them and destroy them looking for it?
2. The science indicates that there is a role for iron in preserving some of these materials. It has apparently been tested in the lab, so it's a workable hypothesis that doesn't in any way cause problems with deep time.
You might want to actually read what the scientists think about this stuff.
Role of iron in soft tissue preservation | Proceedings of the Royal Society of London B: Biological Sciences
I love reading the words of people who don't have the discipline to study science for years and find a way to complain that their ignorance of the science is somehow a valid critique of the science. "Baffle-gab". Truly excellent term.
What it
really means is: "I don't understand it so it must be wrong." Well, for those of us who
bothered to get a PhD in geochemistry it really isn't all that "Baffling".
It already has been. It already has been.