We have investigated the surface morphology and chemistry of zircon in sedi
ments and soils of the Amazon basin (Brazil). The extent of metamictization
in the near-surface region of these zircons was previously determined by R
aman micro-probe. Scanning electron microscopy (SEM) reveals scarce dissolu
tion features and numerous marks related to the sedimentary transport of th
e zircon grains, which attest to the high resistance of these zircons to tr
opical weathering. Rutherford backscattering (RBS) micro-analysis and X-ray
photoelectron spectroscopy (XPS) failed to reveal any strong chemical chan
ge at the surface of the zircon grains. In particular no Zr enrichment was
detected, which excludes the occurrence of a protecting layer of Zr oxide o
r hydroxide at the zircon surface. This result suggests that the slow weath
ering rate of zircon could be the principal factor limiting the Zr mobility
in the investigated weathering environments. (C) 2001 Elsevier Science B.V
. All rights reserved.