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

Foraminiferal I/Ca measurements from Miocene Sediments

古海洋氧化还原

中新世气候

The foraminiferal iodine-to-calcium proxy (I/Ca) can be used to reconstruct regional iodine speciation and redox conditions. This dataset contains new planktonic foraminiferal I/Ca measurements from m

PANGAEA00

Table1_Spatiotemporal Evolution and Genesis of the Late Ordovician—Early Silurian Marine Euxinia in Northeastern Upper Yangtze Basin, South China.XLS

古海洋氧化还原

黑色页岩形成机制

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

Research Data and Python code for Phanerozoic Redox Evolution

古海洋氧化还原

显生宙海洋地球化学演化

The repository contains geochemical datasets used to reconstruct Phanerozoic marine redox evolution, together with source code used to conduct data analyses.

NIAID Data Ecosystem10

Data for "Late Cretaceous cerium anomalies and globally distinctive redox responses before, during and after Oceanic Anoxic Event 2"

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