Matches in SemOpenAlex for { <https://semopenalex.org/work/W1609970259> ?p ?o ?g. }
- W1609970259 endingPage "77" @default.
- W1609970259 startingPage "61" @default.
- W1609970259 abstract "A compilation of many late Quaternary marine sediment records from the northern South China Sea (SCS) continental slope confirms 15–50% reductions in sedimentary calcium carbonate concentrations between 11.0 and 8.5 ka BP in the early Holocene. This low carbonate% event occurred at a time when the regional sea level rose from −50 m to −10 m, which drowned large areas of continental shelves especially those near and within the Taiwan Strait. This event is associated with a significant increase in bulk sedimentation rates on the upper continental slope and the relative abundance of fine-grained detritus. Sediment provenance analyses suggest a dominant terrigenous input from Taiwan and a minor contribution from Luzon during the low carbonate% event, similar to the background terrigenous deposition in other periods of the Holocene. Two comparable low carbonate% events, respectively from the beginning of marine isotope stages 5.5 and 7.3, have also been recognized, pointing to similar causal factors. While carbonate dissolution and carbonate accumulation rate should not have been responsible, increased terrigenous input and dilution is considered as the main cause for the recurrent low carbonate% events in early interglacials. We further hypothesize that, during early interglacials, fluvial sediment discharge from Taiwan and Luzon intensified due to stronger typhoon activities, and massive fine-grained sediments from these two end members may have been transported to the northern SCS continental slope via surface and deep ocean currents. The conjecture of strengthened typhoon activities over East Asia during the early Holocene is supported by high ocean heat contents in the West Pacific Warm Pool area with the prevailing La Niña-like conditions." @default.
- W1609970259 created "2016-06-24" @default.
- W1609970259 creator A5007493067 @default.
- W1609970259 creator A5011445872 @default.
- W1609970259 creator A5017303956 @default.
- W1609970259 creator A5019265493 @default.
- W1609970259 creator A5039267410 @default.
- W1609970259 creator A5060080750 @default.
- W1609970259 date "2015-10-01" @default.
- W1609970259 modified "2023-10-18" @default.
- W1609970259 title "Early interglacial carbonate-dilution events in the South China Sea: Implications for strengthened typhoon activities over subtropical East Asia" @default.
- W1609970259 cites W1514159251 @default.
- W1609970259 cites W1573547234 @default.
- W1609970259 cites W1770855718 @default.
- W1609970259 cites W1964238284 @default.
- W1609970259 cites W1967441125 @default.
- W1609970259 cites W1968588988 @default.
- W1609970259 cites W1975009543 @default.
- W1609970259 cites W1977850725 @default.
- W1609970259 cites W1978928221 @default.
- W1609970259 cites W1980098379 @default.
- W1609970259 cites W1981230700 @default.
- W1609970259 cites W1981413656 @default.
- W1609970259 cites W1989193940 @default.
- W1609970259 cites W1989676793 @default.
- W1609970259 cites W1996932107 @default.
- W1609970259 cites W2000687147 @default.
- W1609970259 cites W2003316825 @default.
- W1609970259 cites W2004587064 @default.
- W1609970259 cites W2013430677 @default.
- W1609970259 cites W2013591853 @default.
- W1609970259 cites W2016170233 @default.
- W1609970259 cites W2017024367 @default.
- W1609970259 cites W2022061231 @default.
- W1609970259 cites W2027385173 @default.
- W1609970259 cites W2030542241 @default.
- W1609970259 cites W2037764406 @default.
- W1609970259 cites W2041050882 @default.
- W1609970259 cites W2043942893 @default.
- W1609970259 cites W2045419467 @default.
- W1609970259 cites W2046771951 @default.
- W1609970259 cites W2047863137 @default.
- W1609970259 cites W2052446941 @default.
- W1609970259 cites W2052462309 @default.
- W1609970259 cites W2052814244 @default.
- W1609970259 cites W2053982496 @default.
- W1609970259 cites W2058337031 @default.
- W1609970259 cites W2061457957 @default.
- W1609970259 cites W2069531939 @default.
- W1609970259 cites W2071181221 @default.
- W1609970259 cites W2074379113 @default.
- W1609970259 cites W2077280380 @default.
- W1609970259 cites W2077927752 @default.
- W1609970259 cites W2080723971 @default.
- W1609970259 cites W2086648250 @default.
- W1609970259 cites W2093296565 @default.
- W1609970259 cites W2093904312 @default.
- W1609970259 cites W2096644508 @default.
- W1609970259 cites W2096807979 @default.
- W1609970259 cites W2097526162 @default.
- W1609970259 cites W2103229046 @default.
- W1609970259 cites W2103600357 @default.
- W1609970259 cites W2103608022 @default.
- W1609970259 cites W2104675631 @default.
- W1609970259 cites W2107383272 @default.
- W1609970259 cites W2112270077 @default.
- W1609970259 cites W2116921785 @default.
- W1609970259 cites W2120970192 @default.
- W1609970259 cites W2125275246 @default.
- W1609970259 cites W2131950692 @default.
- W1609970259 cites W2132520319 @default.
- W1609970259 cites W2148630126 @default.
- W1609970259 cites W2151492923 @default.
- W1609970259 cites W2151595123 @default.
- W1609970259 cites W2153401021 @default.
- W1609970259 cites W2153768021 @default.
- W1609970259 cites W2154650280 @default.
- W1609970259 cites W2163684082 @default.
- W1609970259 cites W2164564942 @default.
- W1609970259 cites W2166353767 @default.
- W1609970259 cites W2166813482 @default.
- W1609970259 cites W2188245901 @default.
- W1609970259 cites W2313812054 @default.
- W1609970259 cites W2503823564 @default.
- W1609970259 cites W2503937471 @default.
- W1609970259 cites W3149453667 @default.
- W1609970259 cites W4246027503 @default.
- W1609970259 cites W4249751050 @default.
- W1609970259 cites W4376453121 @default.
- W1609970259 doi "https://doi.org/10.1016/j.quascirev.2015.08.007" @default.
- W1609970259 hasPublicationYear "2015" @default.
- W1609970259 type Work @default.
- W1609970259 sameAs 1609970259 @default.
- W1609970259 citedByCount "16" @default.
- W1609970259 countsByYear W16099702592016 @default.
- W1609970259 countsByYear W16099702592017 @default.
- W1609970259 countsByYear W16099702592018 @default.
- W1609970259 countsByYear W16099702592019 @default.