Relocation of the Yellow River as revealed by sedimentary isotopic and elemental signals in the East China Sea.
The Yellow River (YR) supplies a large amount of nutrients and fresh water to the northern Chinese marginal seas, and greatly influences the ecosystem and current patterns. The relocation of the YR outlet from the southern Yellow Sea (YS) to the Bohai Sea in 1855 was demonstrated using northern East China Sea (ECS) sediment characteristics. Both isotopic (delta(13)C, delta(15)N) signals and C/N ratios in the organic matter (OM) indicate that prior to 1750, the predominant source of OM to the sediments was terrestrial. The terrestrial influences continuously weakened until 1855, when the YR estuary moved; after 1855, the OM was characterized by oceanic sources. Major elements (Al, Ti, Fe, Mn) and trace elements (Ni, Cr, Cu, Pb) had a much closer association with Malan loess prior to 1855, as >90% of the YR sediment was loess-derived. These results reveal that the relocation of the YR induced significant changes in the current patterns of the northern China Seas in the last 250years; however, more studies are needed to further examine these linkages.
Department of Oceanography, Xiamen University, Xiamen 361005, China. wyang@xmu.edu.cn
Weifeng
W
Yang
Min
M
Chen
Guangxue
G
Li
Jianping
J
Cao
Zhigang
Z
Guo
Qiang
Q
Ma
Jiang
J
Liu
Junhong
J
Yang
D002247:Carbon Isotopes; D002681:China; D004784:Environmental Monitoring; D019015:Geologic Sediments / Q000737:chemistry; D008670:Metals / Q000032:analysis; D009587:Nitrogen Isotopes; D009792:Oceans and Seas; D045483:Rivers / Q000737:chemistry*; D014131:Trace Elements / Q000032:analysis; D014874:Water Pollutants, Chemical / Q000032:analysis*
D002247:Carbon Isotopes; D008670:Metals; D009587:Nitrogen Isotopes; D014131:Trace Elements; D014874:Water Pollutants, Chemical