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- W2949291400 abstract "Abstract Reconstructing the Plio-Pleistocene sedimentary history of the Yellow Sea, is important for understanding the long-term influence of the Yellow River (Huanghe) and/or Yangtze River (Changjiang) on the Asian marginal seas and to further constrain any links between river development, regional paleoenvironmental change, tectonic deformation and/or global climate change. Here we present the first high-resolution clay mineral record combined with Sr-Nd isotopic compositions from a 300-m long sediment core recovered in the western South Yellow Sea. Our study suggests that large-scale transgression in the Yellow Sea occurred after ∼0.8 Ma, possibly related to tectonic subsidence of eastern China coast and the Min-Zhe Uplift. In contrast, the sedimentary environment of Bohai and Yellow Seas was mainly dominated by fluvial/lacustrine deposits at 3.5–0.8 Ma. Provenance analysis suggests a major change in sediment provenance from the Yangtze River to the Yellow River at ∼0.8 Ma, which corresponds to the timing of the final integration of the Yellow River in its present form. At the same time the major channels of the Yangtze River migrated from the South Yellow Sea to the modern Yangtze River delta due to the subsidence of east China coast. The consistence in timing of the provenance transition and large-scale regional marine transgression suggests that tectonic deformation, rather than climate change, is the first-order control on the evolution of the Yellow and Yangtze Rivers and sedimentary environmental change in the Bohai and Yellow Seas." @default.
- W2949291400 created "2019-06-27" @default.
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- W2949291400 date "2019-07-01" @default.
- W2949291400 modified "2023-10-18" @default.
- W2949291400 title "History of Yellow River and Yangtze River delivering sediment to the Yellow Sea since 3.5 Ma: Tectonic or climate forcing?" @default.
- W2949291400 cites W1189960998 @default.
- W2949291400 cites W1533743728 @default.
- W2949291400 cites W1543840266 @default.
- W2949291400 cites W1567579476 @default.
- W2949291400 cites W1644409812 @default.
- W2949291400 cites W1670467877 @default.
- W2949291400 cites W1968175026 @default.
- W2949291400 cites W1970108402 @default.
- W2949291400 cites W1973333589 @default.
- W2949291400 cites W1974945390 @default.
- W2949291400 cites W1983571957 @default.
- W2949291400 cites W1983602215 @default.
- W2949291400 cites W1984173773 @default.
- W2949291400 cites W1995642042 @default.
- W2949291400 cites W1997070870 @default.
- W2949291400 cites W1998750657 @default.
- W2949291400 cites W2000077199 @default.
- W2949291400 cites W2003767587 @default.
- W2949291400 cites W2005488723 @default.
- W2949291400 cites W2009148447 @default.
- W2949291400 cites W2020415754 @default.
- W2949291400 cites W2021266129 @default.
- W2949291400 cites W2026220107 @default.
- W2949291400 cites W2029276637 @default.
- W2949291400 cites W2035681393 @default.
- W2949291400 cites W2046094311 @default.
- W2949291400 cites W2047168195 @default.
- W2949291400 cites W2050230801 @default.
- W2949291400 cites W2050585743 @default.
- W2949291400 cites W2056048650 @default.
- W2949291400 cites W2058606455 @default.
- W2949291400 cites W2063128565 @default.
- W2949291400 cites W2066300646 @default.
- W2949291400 cites W2074989052 @default.
- W2949291400 cites W2076566162 @default.
- W2949291400 cites W2079900432 @default.
- W2949291400 cites W2085719790 @default.
- W2949291400 cites W2087509591 @default.
- W2949291400 cites W2089012876 @default.
- W2949291400 cites W2090240681 @default.
- W2949291400 cites W2090919705 @default.
- W2949291400 cites W2098009133 @default.
- W2949291400 cites W2099335229 @default.
- W2949291400 cites W2103930806 @default.
- W2949291400 cites W2114647769 @default.
- W2949291400 cites W2116921785 @default.
- W2949291400 cites W2117037809 @default.
- W2949291400 cites W2148518454 @default.
- W2949291400 cites W2150484768 @default.
- W2949291400 cites W2153985161 @default.
- W2949291400 cites W2154142710 @default.
- W2949291400 cites W2164411979 @default.
- W2949291400 cites W2169415627 @default.
- W2949291400 cites W2262257212 @default.
- W2949291400 cites W2299551566 @default.
- W2949291400 cites W2306139046 @default.
- W2949291400 cites W2318168004 @default.
- W2949291400 cites W2396787056 @default.
- W2949291400 cites W2465969137 @default.
- W2949291400 cites W2531169012 @default.
- W2949291400 cites W2552279620 @default.
- W2949291400 cites W2560257251 @default.
- W2949291400 cites W2563694176 @default.
- W2949291400 cites W2593929300 @default.
- W2949291400 cites W2619167193 @default.
- W2949291400 cites W2626524797 @default.
- W2949291400 cites W2734210534 @default.
- W2949291400 cites W2734626516 @default.
- W2949291400 cites W2735513025 @default.
- W2949291400 cites W2770362582 @default.
- W2949291400 cites W2775002788 @default.
- W2949291400 cites W2794487628 @default.
- W2949291400 cites W2903359843 @default.
- W2949291400 doi "https://doi.org/10.1016/j.quascirev.2019.06.002" @default.
- W2949291400 hasPublicationYear "2019" @default.
- W2949291400 type Work @default.