Thallium isotope ratios in shales from South China and northwestern Canada suggest widespread O₂ accumulation in marine bottom waters was an uncommon occurrence during the Ediacaran Period

Chadlin M. Ostrander, Jeremy D. Owens, Sune G. Nielsen, Timothy W. Lyons, Yunchao Shu, Xinming Chen, Erik A. Sperling, Ganqing Jiang, David T. Johnston, Swapan K. Sahoo, Ariel D. Anbar

Earth and Space Exploration, School of (SESE)

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Data for: Thallium isotope ratios in shales from South China and northwestern Canada suggest widespread O2 accumulation in marine bottom waters was an uncommon occurrence during the Ediacaran Period
Ostrander, C. M. (Contributor), Sperling, E. A. (Contributor), Nielsen, S. G. (Contributor), Chen, X. (Contributor), Anbar, A. (Contributor), Owens, J. D. (Contributor), Jiang, G. (Contributor), Sahoo, S. K. (Contributor), Shu, Y. (Contributor), Johnston, D. T. (Contributor) & Lyons, T. W. (Contributor), Mendeley Data, Aug 27 2020
DOI: 10.17632/2bkzpkxv6v.1, https://data.mendeley.com/datasets/2bkzpkxv6v
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Thallium isotope ratios in shales from South China and northwestern Canada suggest widespread O2 accumulation in marine bottom waters was an uncommon occurrence during the Ediacaran Period

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Data for: Thallium isotope ratios in shales from South China and northwestern Canada suggest widespread O2 accumulation in marine bottom waters was an uncommon occurrence during the Ediacaran Period

Thallium isotope ratios in shales from South China and northwestern Canada suggest widespread O₂ accumulation in marine bottom waters was an uncommon occurrence during the Ediacaran Period