Climatically Driven Changes in the Supply of Terrigenous Sediment to the East China Sea

Author:

Anderson C. H.1ORCID,Murray R. W.1,Dunlea A. G.12,Giosan L.3,Kinsley C. W.4ORCID,McGee D.4ORCID,Tada R.5ORCID

Affiliation:

1. Department of Earth and Environment; Boston University; Boston MA USA

2. Now at Department of Geology and Geophysics; Woods Hole Oceanographic Institution; Woods Hole MA USA

3. Department of Geology & Geophysics; Woods Hole Oceanographic Institution; Woods Hole MA USA

4. Department of Earth, Atmospheric and Planetary Sciences; Massachusetts Institute of Technology; Cambridge MA USA

5. Graduate School of Science; University of Tokyo; Tokyo Japan

Funder

U.S. National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference58 articles.

1. Pleistocene forced regressions and tidal sand ridges in the East China Sea;Berné;Marine Geology,2002

2. Direct correlation of Chinese speleothem 18O and South China Sea planktonic 18O: Transferring a speleothem chronology to the benthic marine chronology;Caballero-Gill;Paleoceanography,2012

3. Geochemistry of recent oxic and anoxic marine sediments: Implications for the geological record;Calvert;Marine Geology,1993

4. Behaviours of REE and other trace elements during pedological weathering- Evidence from chemical leaching of loess and palaeosol from th Luochuan section in Central China;Chen;Acta Geologica Sinica,1996

5. Chemical weathering intensity and element migration features of the Xiashu loess profile in Zhenjiang, Jiangsu province;Chen;Journal of Geographical Sciences,2008

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