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Hi everyone: I don't really want to flog a dead horse (so to speak) but I'd like to rehash our discussions a few months ago concerning the incorporation of trace metals, ions and isotopes into skeletal/biogenic apatite. Clive Trueman once asked about theories and ideas concerning the rate of uptake (slow vs. fast). I don't recall from my archive files if this was ever discussed or addressed. I'm also wondering about exchange flux, preferential uptakes and how this might effect the isotopic ratios (I am especially concerned with neodymium but this could equally apply for Ce, Sr etc). Also, are there any quantitative estimates about ionic bonding strength once these elements have replaced Ca++ in the lattice? I'm sure there are others out there who are interested in these questions so please respond to the Net. Many Thanks Cindy Cindy Wright School of Earth and Ocean Science Box 1700 University of Victoria Victoria, British Columbia V8W 2Y2
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