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

نویسندگان

چکیده

Marine redox conditions and their dynamic changes were a major factor that controlled the formation of black shale caused late Ordovician marine extinction in Upper Yangtze Basin (South China). However, spatiotemporal variation potential controlling factors this area remain unclear. We analyzed whole-rock geochemistry pyrite sulfur isotopes ( ? 34 S py ) 47 samples from Late Katian to Rhuddanian shelf-to-slope (Qianjiang Shaba section Wc-1 well) region northeastern Basin, reconstructed water column during Ordovician–Early Silurian Transition. The geochemical characteristics shale, including ratio elements, discriminant function ternary diagram location study suggest passive continental margin sedimentary environment, wherein terrigenous detritus is mainly derived felsic igneous rocks upper crust, showing near-source deposition. indices (Fe speciation, C org /P, U EF , Mo showed development anoxic water, especially euxinia, has obvious heterogeneity. Under high availability active organic carbon limited sulfate supply, Fe input strong biological irrigation shallow may effectively remove H 2 produced by microbial reduction, conducive prevalence ferruginous columns. for deep area, rapid accumulation rate matter, decrease dissolved (caused upwelling open sea), seawater stratification rising sea level) promoted euxinic column. This inference supported covariant relationship between rate, chemical index alteration, Co × Mn, . Our highlights control effects level change, weathering on

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ژورنال

عنوان ژورنال: Frontiers in Earth Science

سال: 2021

ISSN: ['2296-6463']

DOI: https://doi.org/10.3389/feart.2021.788349