Cui, H.Kaufman, Alan J.Xiao, S.Grazhdankin, D. V.Peek, S.Martin, A. J.Bykova, N. V.Rogov, V. I.Liu, X. M.Zhang, F.Romaniello, S. J.Anbar, A. D.Peng, Y.Cai, Y.Schiffbauer, J. D.Meyer, M.Gilleaudeau, Geoffrey J.Plummer, Rebecca E.Sievers, N. E.Goderis, S.Claeys, P.2020-03-062020-03-062019-11-220367-0449e097http://hdl.handle.net/10919/97230The terminal Ediacaran contains dramatic changes in biogeochemical cycles, many of which are closely coupled with evolutionary transitions in the corresponding fossil records. Dynamic redox conditions may have caused a profound impact on early animal evolution. Our work highlights the significance of integrated bio-, litho-, and chemo-stratigraphy in geobiology research of the deep time.application/pdfenCreative Commons CC0 1.0 Universal Public Domain DedicationChemostratigraphyRedox conditionEarly macroorganismsBiogeochemical cyclesGeobiologyAnimal biomineralizationAlkalinityCloudinaArticle - Refereedhttps://doi.org/10.3989/egeol.43586.5527521988-3250