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- W2799690764 endingPage "175" @default.
- W2799690764 startingPage "161" @default.
- W2799690764 abstract "The reconstruction of the long-term evolution of the East Asian Monsoon remains controversial. In this study, we aim to give a new outlook on this evolution by studying a 400 kyr long sediment record (U1429) from the northern East China Sea recovered during IODP Expedition 346. Neodymium isotopic ratios and rare earth element concentrations of different grain-size fractions reveal significant provenance changes of the sediments in the East China Sea between East Asian continental sources (mainly Yellow River) and sediment contributions from the Japanese Archipelago. These provenance changes are interpreted as the direct impact of sea level changes, due to the reorganization of East Asian river mouth locations and ocean circulation on the East China Sea shelf, and latitudinal shifts of the intertropical convergence zone (ITCZ) from the interior of Asia to the western North Pacific Ocean. Our data reveal the dominance of winter and summer monsoons during glacial and interglacial periods, respectively, except for glacial MIS 6d (∼150–180 ka) during which unexpected summer monsoon dominated conditions prevailed. Finally, our data suggests a possible strengthening of the interglacial summer monsoon rainfalls over the East Asian continent and Japan throughout the past 400 kyr, and between MIS 11 and MIS 5 in particular. This could result from a gradual northward migration of the ITCZ." @default.
- W2799690764 created "2018-05-17" @default.
- W2799690764 creator A5020337856 @default.
- W2799690764 creator A5058929466 @default.
- W2799690764 creator A5069974015 @default.
- W2799690764 creator A5071151967 @default.
- W2799690764 creator A5090695206 @default.
- W2799690764 date "2018-06-01" @default.
- W2799690764 modified "2023-09-30" @default.
- W2799690764 title "Geochemical provenance of sediments from the northern East China Sea document a gradual migration of the Asian Monsoon belt over the past 400,000 years" @default.
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