Marine redox conditions and their dynamic changes were a major factor that controlled the formation of black shale and caused the late Ordovician marine extinction in the Upper Yangtze Basin (South Ch

NIAID Data Ecosystem30

Trace metal concentrations and isotope compositions from drill core OPH of th...

黑色页岩地球化学

古海洋氧化还原

This dataset contains molybdenum and uranium concentrations; uranium isotope compositions; pertinent major element concentrations; and total organic carbon contents of black...

B2FIND20

Does uranium speciation control uranium isotope signatures in marine sedimentary rocks? Advancing the paleoredox proxy

铀地球化学

古海洋氧化还原

Uranium (U) speciation controls its reactivity and transport in environmental systems and is modulated by redox conditions. U enrichment and isotopic composition in sedimentary rocks are a promising p

ESRF Portal2028-01-01 更新40

DataSheet3_Quantifying Iron Oxide Mineral Contents in Miocene Oceanic Red Beds for the Deep-Sea Oxidation Evolution in the South China Sea.XLSX

古海洋氧化还原

沉积物矿物学

The International Ocean Discovery Program (IODP) Expedition 349 recovered Miocene oceanic red beds overlying the basaltic basement in the South China Sea. The occurrence of oceanic red beds provides a

NIAID Data Ecosystem20

Data for: Oceanic redox conditions during the terminal Cambrian extinction event

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