INVESTIGADORES
GAIERO Diego Marcelo
artículos
Título:
Dust provenance in Antarctic ice during glacial periods: From where in
Autor/es:
DIEGO M. GAIERO
Revista:
GEOPHYSICAL RESEARCH LETTERS
Editorial:
American Geophysical Union
Referencias:
Año: 2007 vol. 34 p. 1 - 6
ISSN:
0094-8276
Resumen:
The origin of dust deposited in East Antarctica is not
fully understood yet. This study demonstrates that, contrary
to Nd, Sr isotopes are strongly fractionated in the finestsized
material representing potential dust sources in South
America. Analysis of Nd isotopes suggests that Argentine
loess, Southern Ocean sediments and Antarctic dust, may all
have a related origin or can represent comparable
mechanisms of eolian sediment transport and deposition.
This analysis also concludes that the Patagonian signature
can explain a high proportion of the isotopic composition of
dust trapped in Antarctic ice during glacial periods. The
Puna-Altiplano plateau emerges as the second possible
important sediment contributor explaining the crustal-like
signature found in East Antarctic dust and should be
considered as a potential source area when Quaternary
paleoclimate is reconstructed from Argentine loess, Antarctic
dust and South Atlantic sediment records.