Matches in SemOpenAlex for { <https://semopenalex.org/work/W2962742482> ?p ?o ?g. }
- W2962742482 endingPage "474" @default.
- W2962742482 startingPage "463" @default.
- W2962742482 abstract "ABSTRACT A continuous sediment record since 12.3 cal ka bp from Lake Wuxu (south‐eastern Tibetan Plateau) was investigated in terms of the Holocene evolution of the Indian Summer Monsoon. The molar C/N ratio and stable C isotope were used to identify the source of the organic matter as well as climate conditions. The evolution of Lake Wuxu was summarized wihtin two periods. During the first period (early to mid‐Holocene), the lake received increased fluvially transported materials, reflecting variation in the summer monsoon with solar insolation. The lake level declined and water residence time increased because of reduced river discharge during the second period (late Holocene) corresponding to a weakening of the summer monsoon. The organic material revealed a major contribution from lake primary productivity, which showed identical patterns with a high‐resolution isotope record from Dongge Cave, as well as total solar irradiance. Our record from Lake Wuxu indicates that the Holocene evolution of the Indian Summer Monsoon has been driven by the solar forcing at decadal/centennial to millennial time scales. Furthermore, an abrupt decline in the monsoon was detected at around 4.0 cal ka bp , which is probably caused by an increased frequency of EI Nino‐Southern Oscillation events. Copyright © 2019 John Wiley & Sons, Ltd." @default.
- W2962742482 created "2019-07-30" @default.
- W2962742482 creator A5001342001 @default.
- W2962742482 creator A5006427956 @default.
- W2962742482 creator A5008476540 @default.
- W2962742482 creator A5040561037 @default.
- W2962742482 creator A5054754924 @default.
- W2962742482 creator A5069229762 @default.
- W2962742482 creator A5076703458 @default.
- W2962742482 date "2019-07-23" @default.
- W2962742482 modified "2023-10-16" @default.
- W2962742482 title "Holocene evolution of the Indian Summer Monsoon inferred from a lacustrine record of Lake Wuxu, south‐east Tibetan Plateau" @default.
- W2962742482 cites W1498526448 @default.
- W2962742482 cites W1557231701 @default.
- W2962742482 cites W1566527937 @default.
- W2962742482 cites W1602975826 @default.
- W2962742482 cites W1717650924 @default.
- W2962742482 cites W1926895964 @default.
- W2962742482 cites W1968588988 @default.
- W2962742482 cites W1970545835 @default.
- W2962742482 cites W1976289135 @default.
- W2962742482 cites W1982932887 @default.
- W2962742482 cites W1983175712 @default.
- W2962742482 cites W1984198610 @default.
- W2962742482 cites W1984207195 @default.
- W2962742482 cites W1990422409 @default.
- W2962742482 cites W1991766856 @default.
- W2962742482 cites W1993341938 @default.
- W2962742482 cites W1994007098 @default.
- W2962742482 cites W1996932107 @default.
- W2962742482 cites W2001938196 @default.
- W2962742482 cites W2002158982 @default.
- W2962742482 cites W2004208783 @default.
- W2962742482 cites W2006333290 @default.
- W2962742482 cites W2006768932 @default.
- W2962742482 cites W2009607369 @default.
- W2962742482 cites W2010580981 @default.
- W2962742482 cites W2013428409 @default.
- W2962742482 cites W2015395460 @default.
- W2962742482 cites W2016587496 @default.
- W2962742482 cites W2018030672 @default.
- W2962742482 cites W2023369407 @default.
- W2962742482 cites W2029530847 @default.
- W2962742482 cites W2036258677 @default.
- W2962742482 cites W2037850579 @default.
- W2962742482 cites W2040974937 @default.
- W2962742482 cites W2042386182 @default.
- W2962742482 cites W2050467115 @default.
- W2962742482 cites W2054777801 @default.
- W2962742482 cites W2059699700 @default.
- W2962742482 cites W2060830550 @default.
- W2962742482 cites W2067643634 @default.
- W2962742482 cites W2073068047 @default.
- W2962742482 cites W2080072873 @default.
- W2962742482 cites W2081011249 @default.
- W2962742482 cites W2083043680 @default.
- W2962742482 cites W2084661097 @default.
- W2962742482 cites W2085301764 @default.
- W2962742482 cites W2085715610 @default.
- W2962742482 cites W2091050774 @default.
- W2962742482 cites W2097481580 @default.
- W2962742482 cites W2100866593 @default.
- W2962742482 cites W2102687083 @default.
- W2962742482 cites W2107211406 @default.
- W2962742482 cites W2110116713 @default.
- W2962742482 cites W2111212031 @default.
- W2962742482 cites W2113608804 @default.
- W2962742482 cites W2120459028 @default.
- W2962742482 cites W2123793538 @default.
- W2962742482 cites W2124757012 @default.
- W2962742482 cites W2130719091 @default.
- W2962742482 cites W2140477756 @default.
- W2962742482 cites W2141353210 @default.
- W2962742482 cites W2144822575 @default.
- W2962742482 cites W2150524323 @default.
- W2962742482 cites W2154036078 @default.
- W2962742482 cites W2154919359 @default.
- W2962742482 cites W2163199010 @default.
- W2962742482 cites W2173251738 @default.
- W2962742482 cites W2191171771 @default.
- W2962742482 cites W2294467098 @default.
- W2962742482 cites W2295914767 @default.
- W2962742482 cites W2340546024 @default.
- W2962742482 cites W2406080870 @default.
- W2962742482 cites W2605968767 @default.
- W2962742482 cites W2626774371 @default.
- W2962742482 cites W2800443358 @default.
- W2962742482 cites W4246027503 @default.
- W2962742482 cites W4249751050 @default.
- W2962742482 cites W4306293736 @default.
- W2962742482 doi "https://doi.org/10.1002/jqs.3113" @default.
- W2962742482 hasPublicationYear "2019" @default.
- W2962742482 type Work @default.
- W2962742482 sameAs 2962742482 @default.
- W2962742482 citedByCount "7" @default.
- W2962742482 countsByYear W29627424822020 @default.
- W2962742482 countsByYear W29627424822021 @default.
- W2962742482 countsByYear W29627424822022 @default.