The money sinks...
So do diatoms once they die. Could this support the dredge theory?
Once the diatoms die, their "frustules" (outer walls) sink to the bottom of the body of water they are in, forming part of the sediment.
A few questions:
1) Are we looking at diatoms that entered the bills alive, or dead frustules of diatoms that made contact with the bills as a component of the river sediment?
2) if the Columbia's source is 1,200 miles away in B.C., and it is fed by lots of tributaries along the way, and these lakes and tributaries all produce diatoms, are we looking at the most recent summer's bloom of diatoms from the Vancouver area, or last season's corpses from elsewhere that traveled miles to get here? (I suppose this would extend to the money travelling as well). If the latter...
3) Can we use the varieties of diatoms found to "fingerprint" a specific stream or lake where the money sat? (probably covered already, but humor me)
The Citizen Sleuth website states, "
The modern bills soaked in the Columbia River were examined using a scanning electron microscope (SEM.) At least three different species of fresh water diatoms were found immediately. Subsequent examination of the Cooper bills found no diatoms. Not seeing any diatoms on the Cooper bills does not guarantee that they are not there, so any final conclusions on this would be speculative."
4) Why were no diatoms found on the FBI bills at the time of that examination, but plenty were found later on 377's solitary bill, when they all presumably came from the same source? Did I miss a post? (Serious question)
5) If the money was wet, and it was found, as Harold Ingram said on camera, "partially on top of the ground," how does the fragility of diatoms in sand disqualify Eric's belief that the bills were saturated in floodwater that would have possibly made direct contact? (Again, serious question.)
I hope my catch-up class is welcomed as a refresher course for some of you.