Tetravalent Uranium in Calcite
N. C. Sturchio,
M. R. Antonio,
L. Soderholm,
S. R. Sutton,
J.
C. Brannon
X-ray absorption spectroscopy and x-ray fluorescence microprobe
studies of 35-million-year-old calcite from a Mississippi Valley-type
zinc ore deposit indicate substitution of tetravalent uranium for
divalent calcium. Thus, tetravalent uranium has a stable location in
calcite deposited under reducing conditions. This result validates
uranium-series dating methods (including uranium/lead dating) for
ancient calcite and shows that calcite provides a sink for uranium in
deep groundwater aquifers and anoxic lacustrine and marine basins.
N. C. Sturchio, M. R. Antonio, L. Soderholm, Argonne
National Laboratory, Argonne, IL 60439, USA. S. R. Sutton,
Consortium for Advanced Radiation Sources and Department of Geophysical
Sciences, University of Chicago, Chicago, IL 60637, USA. J. C. Brannon, Department of Earth and Planetary Sciences, Washington
University, St. Louis, MO 63130, USA.