XRF-XANES characterization of deep ice core insoluble dust

An analytical protocol based on X-ray spectroscopic measurements (XRF and Fe and Ti K-edges XAS) has been applied to evaluate the mineralogical phase composition of dust trapped in deep ice cores. Information on the insoluble dust composition and local and species-selective information as oxidation and coordination states has been obtained to recognize the main mineralogical families of aerosol particles contained in deep ice cores. In this framework we point out the possibility to obtain the mineralogical characterization of dust from deep ice core samples from Antarctica by means of XANES spectroscopy.

[1]  S. Joussaume,et al.  Comments on the origin of dust in East Antarctica for present and ice age conditions , 1992 .

[2]  A. Marcelli,et al.  Local and average Fe distribution in trioctahedral micas: Analysis of Fe K-edge XANES spectra in the phlogopite-annite and phlogopite-tetra-ferriphlogopite joins on the basis of single-crystal XRD refinements , 2002 .

[3]  P. Smedley,et al.  Arsenic associations in sediments from the loess aquifer of La Pampa, Argentina , 2005 .

[4]  J. Rehr,et al.  TI K-EDGE XANES STUDIES OF TI COORDINATION AND DISORDER IN OXIDE COMPOUNDS: COMPARISON BETWEEN THEORY AND EXPERIMENT , 1997 .

[5]  J. S. Lee,et al.  Linear combination of XANES for quantitative analysis of Ti-Si binary oxides. , 2001, Journal of synchrotron radiation.

[6]  B. Delmonte,et al.  Defining the geochemical composition of the EPICA Dome C ice core dust during the last glacial‐interglacial cycle , 2008 .

[7]  P. Gabrielli,et al.  Atmospheric iron fluxes over the last deglaciation: Climatic implications , 2006 .

[8]  D. Gaiero Dust provenance in Antarctic ice during glacial periods: From where in southern South America? , 2007 .

[9]  A. Marcelli,et al.  First combined total reflection X-ray fluorescence and grazing incidence X-ray absorption spectroscopy characterization of aeolian dust archived in Antarctica and Alpine deep ice cores ☆ , 2008 .

[10]  G. M. Young,et al.  Early Proterozoic climates and plate motions inferred from major element chemistry of lutites , 1982, Nature.

[11]  M. Bigler,et al.  Dust-climate couplings over the past 800,000 years from the EPICA Dome C ice core , 2008, Nature.

[12]  A. Schilt,et al.  Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years , 2007, Science.

[13]  M. Lavelle,et al.  Late Cretaceous–Cenozoic climatic variations of the northern Antarctic Peninsula: new geochemical evidence and review , 1998 .

[14]  V. Maggi,et al.  PIXE and PIGE techniques for the analysis of Antarctic ice dust and continental sediments , 2008 .

[15]  F. Brunet,et al.  A uniform isotopic and chemical signature of dust exported from Patagonia: Rock sources and occurrence in southern environments , 2007 .

[16]  A. Dia,et al.  Loess geochemistry and its implications for particle origin and composition of the upper continental crust , 1998 .

[17]  I. Fung,et al.  Wintertime phytoplankton bloom in the subarctic Pacific supported by continental margin iron , 2006 .