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On Mon, 4 Nov 1996, Mike Simmons wrote: > I'm wondering if subscribers to PaleoNet or Micropal might be able to > help and advise me. > > Along with colleagues at University College London, the Natural > History Museum and Moscow State University, I'm looking at the > earliest planktonic foraminfera (Middle Jurassic - Early Cretaceous). > Taxonomic revision and synthesis is well in hand, but in the course > of our work, we've been analysing the composition of the tests of > these forms. Following on from observations from Russian workers, > we're able to confirm that (some) of these taxa had aragonitic tests. > Others are calcitic, but this may well we secondary (work is ongoing). > As far as I know (correct me if I'm wrong) all modern planktonic > foraminifera are primary calcite as are Late Cretaceous and Tertiary > forms. > > My major question here is what governs if an organism secretes a > calcitic or aragonitic shell? I've tried to investigate this topic but so > far all the references I've seen are vague. Perhaps this is an area in > which palaeontologists should be talking more with cell biologists? > Maybe someone out there is working on this problem or can point me > in the direction of someone who is. Is there an obvious reference I > have missed? Dear Mike, concerning calcite and aragonite, did you check Falini, Albeck, Weiner&Addadi (Control of aragonite or calcite polymorphism by Mollusc Shell Macromolecules) in Science, January 5th, 1996? To~nu Meidla University of Tartu tmeidla@math.ut.ee
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