According to the Deer-Howie-Zussman, glauconite pellets may form from
various starting materials (forams, fecal pellets,...) The sedimentation
conditions seem the critical factor (low sedimentation rate, slightly
reducing, shallow waters).
Here in Belgium are tertiary sand layers rich in nearly black glauconite
pellets. A large fraction of the green-black material is HCl-soluble, and
what is left is a silica-skeletton.
I observed fecal pellets in the Mansfeld Kupferschiefer, which were highly
phosphatic (and uraniferous, for that matter).
This discussion brings also to my mind the meter-size sand castles built
in Central African savanas by termites, which accidentally dig out gold
grains.
This is thus a case of a ROCK built by insects.
J.J.
> >> Yes, minerals are castles built by insects !
> >
[quoted text clipped - 4 lines]
> If I remember correctly, glauconite forms from fecal pellets and other organic
> debris, though not likely from insects. Does that sound right, Jo?
George - 11 Feb 2005 06:09 GMT
> According to the Deer-Howie-Zussman, glauconite pellets may form from
> various starting materials (forams, fecal pellets,...) The sedimentation
[quoted text clipped - 14 lines]
>
> J.J.
Interesting. The glauconite that occurs around where I live is paleozoic
(middle Mississippian - carboniferous) in age, and consists of bright green
flakes, sometimes forming thin layers at formation contacts. A few formations I
have seen have flakes of glauconite throughout. One in particular is also rich
in Mississippian-aged shark teeth, which occurs at the contacts of very rich
crinoid beds.
>> >> Yes, minerals are castles built by insects !
>> >
[quoted text clipped - 5 lines]
> organic
>> debris, though not likely from insects. Does that sound right, Jo?