Reply to Comment by Xu et al. on “Sr-Nd isotope composition and clay mineral assemblages in eolian dust from the central Philippine Sea over the last 600 kyr: Implications for the transport mechanism of Asian dust” by Seo et al.
Author:
Affiliation:
1. Deep-sea and Seabed Mineral Resources Research Center; Korea Institute of Ocean Science and Technology; Ansan South Korea
2. School of Earth and Environmental Sciences; Seoul National University; Seoul South Korea
Funder
Ministry of Oceans and Fisheries, Republic of Korea
Korea Institute of Ocean Science and Technology
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016JD025444/fullpdf
Reference39 articles.
1. The effect of source area and atmospheric transport on mineral aerosol collected over the North Pacific Ocean;Arnold;Global Planet. Change,1998
2. Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans;Biscaye;Geol. Soc. Am. Bull.,1965
3. Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, Greenland;Biscaye;J. Geophys. Res.,1997
4. Saharan dust: Clay ratio as a relevant tracer to assess the origin of soil-derived aerosols;Caquineau;Geophys. Res. Lett.,1998
5. Clay Sedimentology
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