Articles | Volume 8, issue 1
https://doi.org/10.5194/cp-8-135-2012
© Author(s) 2012. This work is distributed under the Creative Commons Attribution 3.0 License.
Research article
| 
19 Jan 2012
Research article |
| 19 Jan 2012
Change in dust variability in the Atlantic sector of Antarctica at the end of the last deglaciation
Cited articles
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Bory, A., Wolff, E., Mulvaney, R., Jagoutz, E., Wegner, A., Ruth, U., and Elderfield, H.: Multiple sources supply eolian mineral dust to the Atlantic sector of coastal Antarctica: Evidence from recent snow layers at the top of Berkner Island ice sheet, Earth Planet. Sc. Lett., 291, 138-148, https://doi.org/10.1016/j.epsl.2010.01.006, 2010.
De Deckker, P., Norman, M., Goodwin, I. D., Wain, A., and Gingele, F. X.: Lead isotopic evidence for an Australian source of Aeolian dust to Antarctica at times over the last 170 000 years, Palaeogeogr. Palaeocl., 285, 205–223, https://doi.org/10.1016/j.palaeo.2009.11.013, 2010.
Delmonte, B.: Quaternary origin and variations of continental dust in East Antarctica, Ph.D Thesis, University of Siena, Siena, Italy, Universite Joseph Fourier-Grenoble I, Grenoble, France, 2003.
Delmonte, B., Petit, J. R., Andersen, K. K., Basile-Doelseh, I., Maggi, V., and Lipenkov, V. Y.: Dust size evidence for opposite regional atmospheric circulation changes over east Antarctica during the last climatic transition, Clim. Dynam., 23, 427–438, https://doi.org/10.1007/s00382-004-0450-9, 2004a.
