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- W2777350448 abstract "We present a history of late Quaternary coastal evolution based on the study of a 41.9-m-long sediment core from the Oujiang Delta. Multiple analytical methods are employed, including sedimentary facies analysis, radiocarbon dating, and the investigations of grain size, elemental, microfossil and pollen compositions. Two transgression-regression sequences, separated by a paleosol layer, are identified. Several lines of evidence indicate that the lower sequence was deposited during the mid-early MIS 3 stage, under a relatively warm and wet climate. An elevated MIS 3 highstand sea level (higher than − 24 m) is observed. The upper sequence was created after the paleosol was flooded during a marine transgression at ~ 9.5 cal kyr BP. Seven weak East Asian Summer Monsoon (EASM) events are identified with central years of ~ 8.4, 7.7, 6.3, 5.7, 4.7, 2.8 and 1.8 cal kyr BP. These coincide with those from the ECS sediment cores and the Dongge Cave δ18O record, indicating that EASM precipitation is a major controlling factor of sedimentation rates in the region. The Oujiang Delta is also subject to typhoon impacts and East Asian winter monsoon (EAWM)-induced coastal currents. Active typhoons and a relatively enhanced EAWM occurred during the weak EASM period between 4.9 and 6.4 cal kyr BP, producing high sedimentation rates in the middle Holocene. We emphasize the high sensitivity of small Asian river deltas as archives of the EASM, EAWM and typhoons. Such environments merit further as a means to understand past changes as well as future responses to projected climatic and sea-level change." @default.
- W2777350448 created "2018-01-05" @default.
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- W2777350448 date "2018-03-01" @default.
- W2777350448 modified "2023-10-15" @default.
- W2777350448 title "Late Quaternary environmental change in Oujiang delta along the northeastern Zhe-Min Uplift zone (Southeast China)" @default.
- W2777350448 cites W1606679120 @default.
- W2777350448 cites W1892250996 @default.
- W2777350448 cites W1924599695 @default.
- W2777350448 cites W1929061949 @default.
- W2777350448 cites W1955935479 @default.
- W2777350448 cites W1970840639 @default.
- W2777350448 cites W1972571388 @default.
- W2777350448 cites W1974399951 @default.
- W2777350448 cites W1974579278 @default.
- W2777350448 cites W1978433101 @default.
- W2777350448 cites W1980362876 @default.
- W2777350448 cites W1982994601 @default.
- W2777350448 cites W1983325553 @default.
- W2777350448 cites W1985472313 @default.
- W2777350448 cites W1985957539 @default.
- W2777350448 cites W1986890964 @default.
- W2777350448 cites W1987706091 @default.
- W2777350448 cites W1990469714 @default.
- W2777350448 cites W1991575260 @default.
- W2777350448 cites W1992661052 @default.
- W2777350448 cites W1995367450 @default.
- W2777350448 cites W1996932107 @default.
- W2777350448 cites W1997333129 @default.
- W2777350448 cites W2003868383 @default.
- W2777350448 cites W2004237957 @default.
- W2777350448 cites W2009411107 @default.
- W2777350448 cites W2013430677 @default.
- W2777350448 cites W2019646264 @default.
- W2777350448 cites W2019786695 @default.
- W2777350448 cites W2020293415 @default.
- W2777350448 cites W2023474451 @default.
- W2777350448 cites W2023777374 @default.
- W2777350448 cites W2027056089 @default.
- W2777350448 cites W2031341274 @default.
- W2777350448 cites W2041786212 @default.
- W2777350448 cites W2045971570 @default.
- W2777350448 cites W2051644507 @default.
- W2777350448 cites W2055909881 @default.
- W2777350448 cites W2056864037 @default.
- W2777350448 cites W2060325732 @default.
- W2777350448 cites W2062312345 @default.
- W2777350448 cites W2064327957 @default.
- W2777350448 cites W2067513078 @default.
- W2777350448 cites W2067724181 @default.
- W2777350448 cites W2070312095 @default.
- W2777350448 cites W2071897799 @default.
- W2777350448 cites W2074187050 @default.
- W2777350448 cites W2080347274 @default.
- W2777350448 cites W2080670467 @default.
- W2777350448 cites W2080912283 @default.
- W2777350448 cites W2082376648 @default.
- W2777350448 cites W2083033755 @default.
- W2777350448 cites W2083904754 @default.
- W2777350448 cites W2084014771 @default.
- W2777350448 cites W2088382012 @default.
- W2777350448 cites W2090948017 @default.
- W2777350448 cites W2092234296 @default.
- W2777350448 cites W2094173026 @default.
- W2777350448 cites W2094413158 @default.
- W2777350448 cites W2099581206 @default.
- W2777350448 cites W2099826005 @default.
- W2777350448 cites W2101096368 @default.
- W2777350448 cites W2107087656 @default.
- W2777350448 cites W2109459276 @default.
- W2777350448 cites W2110581289 @default.
- W2777350448 cites W2127201634 @default.
- W2777350448 cites W2134098494 @default.
- W2777350448 cites W2140629748 @default.
- W2777350448 cites W2140973288 @default.
- W2777350448 cites W2152352310 @default.
- W2777350448 cites W2156128994 @default.
- W2777350448 cites W2165812778 @default.
- W2777350448 cites W2167451751 @default.
- W2777350448 cites W2280624662 @default.
- W2777350448 cites W2299551566 @default.
- W2777350448 cites W2414824932 @default.
- W2777350448 cites W2535421968 @default.
- W2777350448 cites W2553988397 @default.
- W2777350448 cites W2594616905 @default.
- W2777350448 cites W2605349361 @default.
- W2777350448 cites W2749416095 @default.
- W2777350448 cites W4249751050 @default.
- W2777350448 doi "https://doi.org/10.1016/j.palaeo.2017.12.012" @default.
- W2777350448 hasPublicationYear "2018" @default.
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