Early Ediacaran Positive C-Isotope Anomaly in Limestones of the Chernaya Rechka Formation, Igarka Uplift (Northwestern Siberian Platform)

[1] Bold U.(2016)Neoproterozoic stratigraphy of the Zavkhan Terrane of Mongolia: the backbone for Cryogenian and Early Ediacaran chemostratigraphic record Am. J. Sci. 316 1-63

[2] Smith E.F.(2013)Vendian reference section of southern Middle Siberia Stratigr. Geol. Correl 21 359-382

[3] Rooney A.D.(2014)Assessing the utility of Fe/Al and Fe-speciation to record water column redox conditions in carbonate-rich sediments Chem. Geol. 382 111-122

[4] Chumakov N.M.(2016)Redox-dependent distribution of early macro-organisms: Evidence from the terminal Ediacaran Khatyspyt Formation in Arctic Siberia Palaeogeogr., Palaeoclimat., Palaeoecol. 461 122-139

[5] Semikhatov M.A.(2017)Was the Ediacaran Shuram Excursion a globally synchronized early diagenetic event? Insights from methan-derived authigenic carbonates in the uppermost Doushantuo Formation, South China Chem. Geol 450 59-80

[6] Sergeev V.N.(2018)The Neoproterozoic Hüttenberg δ Precambrian Res. 313 242-262

[7] Clarkson M.O.(2010)C anomaly: genesis and global implications Stratigr. Geol. Correl. 18 353-375

[8] Poulton S.W.(2020)Lower Vendian Microfossil Assemblages of East Siberia: Significance for Solving Regional Stratigraphic Problems Geol. Mag 157 22-34

[9] Guilbaud R.(2010)Quo vadis, Tommotian? Precambrian Res. 182 337-350

[10] Cui H.(2018)Neoproterozoic chemostratigraphy Earth Planet. Sci. Lett. 482 1-11

[1] Bold U.(2016)Neoproterozoic stratigraphy of the Zavkhan Terrane of Mongolia: the backbone for Cryogenian and Early Ediacaran chemostratigraphic record Am. J. Sci. 316 1-63

[2] Smith E.F.(2013)Vendian reference section of southern Middle Siberia Stratigr. Geol. Correl 21 359-382

[3] Rooney A.D.(2014)Assessing the utility of Fe/Al and Fe-speciation to record water column redox conditions in carbonate-rich sediments Chem. Geol. 382 111-122

[4] Chumakov N.M.(2016)Redox-dependent distribution of early macro-organisms: Evidence from the terminal Ediacaran Khatyspyt Formation in Arctic Siberia Palaeogeogr., Palaeoclimat., Palaeoecol. 461 122-139

[5] Semikhatov M.A.(2017)Was the Ediacaran Shuram Excursion a globally synchronized early diagenetic event? Insights from methan-derived authigenic carbonates in the uppermost Doushantuo Formation, South China Chem. Geol 450 59-80

[6] Sergeev V.N.(2018)The Neoproterozoic Hüttenberg δ Precambrian Res. 313 242-262

[7] Clarkson M.O.(2010)C anomaly: genesis and global implications Stratigr. Geol. Correl. 18 353-375

[8] Poulton S.W.(2020)Lower Vendian Microfossil Assemblages of East Siberia: Significance for Solving Regional Stratigraphic Problems Geol. Mag 157 22-34

[9] Guilbaud R.(2010)Quo vadis, Tommotian? Precambrian Res. 182 337-350

[10] Cui H.(2018)Neoproterozoic chemostratigraphy Earth Planet. Sci. Lett. 482 1-11