Articles | Volume 11, issue 2
https://doi.org/10.5194/cp-11-265-2015
https://doi.org/10.5194/cp-11-265-2015
Research article
 | 
17 Feb 2015
Research article |  | 17 Feb 2015

Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea

Y. Kubota, R. Tada, and K. Kimoto

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Cited articles

An, Z., Porter, S. C., Kutzbach, J. E., Wu, X., Wang, S., Liu, X., Li, X., and Zhou, W.: Asynchronous Holocene optimum of the East Asian monsoon, Quaternary Sci. Rev., 19, 743–762, 2000.
Barker, S., Greaves, M., and Elderfield, H.: A study of cleaning procedures used for foraminiferal Mg / Ca paleothermometry, Geochem. Geophy. Geosy., 4, 8407, https://doi.org/10.1029/2003GC000559, 2003.
Beardsley, R. C., Limburber, R., Yu, H., and Cannon, G. A.: Discharge of the Changjiang (Yangtze River) into the East China Sea, Cont. Shelf Res., 4, 57–55, 1985.
Boyle, E. A. and Keigwin, L. D.: Comparison of Atlantic and Pacific paleochemical records for the last 215000 years: changes in deep ocean circulation and chemical inventories, Earth Planet. Sc. Lett., 76, 135–150, 1985.
Chang, C. P., Zhang, Y., and Li, T.: Interannual and Interdecadal Variations of the East Asian Summer Monsoon and Tropical Pacific SSTs, Part I: Roles of the Subtropical Ridge, J. Climate, 13, 4310–4325, 2000.