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- W2382808826 abstract "Barium in marine sediments derives from diverse sources,of which biogenic barium cycling is restricted by climate change and early diagenesis.The relationship between barium and titanium in the carbonate-free sediments of core ZHS-176drilled on the northern slope of the South China Sea indicates that the slope sediments contain a great fraction of biogenic barium,accounting for 50%~60%in the Last Glacial Maximum(LGM)and more than 60%since deglaciation(15Cal.ka BP).During Heinrich1,Younger Dryas and the cooling event at 8ka BP,the biogenic barium decreased abruptly,indicating that the sea level changes and the short-term climatic cooling events controlled the supply of biogenic barium to the sediments.During the climate-warming period(Blling/Allerd),however,a barium anormly corresponding exactly to the foraminifer negative carbon isotopic anormaly occurred obviously.This implies that the biogenic barium cycling in the slope sediments might be impacted by the early diagenesis related to the reaction between sulfate and methane." @default.
- W2382808826 created "2016-06-24" @default.
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- W2382808826 date "2013-01-01" @default.
- W2382808826 modified "2023-09-24" @default.
- W2382808826 title "Effects of Climate Change and Early Diagenesis on Barium Cycling in Sediments From the Northern Slope of the South China Sea" @default.
- W2382808826 hasPublicationYear "2013" @default.
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