Micropaleontological and Lithogeochemical Characteristics of the Turtas Formation (Upper Oligocene), Western Siberia

[11] Iakovleva A.I.(2004)First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia) Dokl. Earth Sci 394 14-18

[12] Radionova E.P.(2008)Stratigraphy and palynological characterization of Oligocene–Miocene deposits recovered by drilling (borehole 01-BP) in the Omsk Region near Irtysh, West Siberia Stratigr. Geol. Correl 16 540-552

[13] Aleksandrova G.N.(2003)First dinoflagellate finds in Upper Oligocene continental sediments of the Zhuravka Formation (Western Siberia) Geol. Geofiz 44 348-363

[14] Oreshkina T.V.(2017)Palynostratigraphy of Oligocene–Miocene continental deposits in Southwestern Siberia Stratigr. Geol. Correl 25 342-361

[15] Smirnov P.V.(2017)Upper Cretaceous and Cenozoic microphytofossils and magnetostratigraphy of the southeastern part of the West Siberian lowland Dokl. Earth Sci 474 620-623

[16] Konstantinov A.O.(2003)New data on stratigraphy (palynomorphs, ostracods, paleomagnetism) of Cenozoic continental deposits of the Ishim plain, Western Siberia Lithol. Miner. Resour 38 427-446

[17] Kuz’mina O.B.(1982)Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia Nature 299 715-717

[18] Benson M.L.(2018)Lithological, lithochemical, and geochemical indicators of paleoclimate: Evidence from Riphean of the Southern Urals Nova Hedwigia 147 183-192

[19] Kociolek J.P.(1989)Early Proterozoic climates and plate motions inferred from major element chemistry of lutites Dokl. Akad. Nauk SSSR 308 428-431

[20] Spaulding S.A.(1990)Transfer of extant non-marine diatom Bot. Zh 75 1565-1567

[11] Iakovleva A.I.(2004)First findings of dinocysts in the upper Oligocene Turtas formation in Southern Tyumen oblast (West Siberia) Dokl. Earth Sci 394 14-18

[12] Radionova E.P.(2008)Stratigraphy and palynological characterization of Oligocene–Miocene deposits recovered by drilling (borehole 01-BP) in the Omsk Region near Irtysh, West Siberia Stratigr. Geol. Correl 16 540-552

[13] Aleksandrova G.N.(2003)First dinoflagellate finds in Upper Oligocene continental sediments of the Zhuravka Formation (Western Siberia) Geol. Geofiz 44 348-363

[14] Oreshkina T.V.(2017)Palynostratigraphy of Oligocene–Miocene continental deposits in Southwestern Siberia Stratigr. Geol. Correl 25 342-361

[15] Smirnov P.V.(2017)Upper Cretaceous and Cenozoic microphytofossils and magnetostratigraphy of the southeastern part of the West Siberian lowland Dokl. Earth Sci 474 620-623

[16] Konstantinov A.O.(2003)New data on stratigraphy (palynomorphs, ostracods, paleomagnetism) of Cenozoic continental deposits of the Ishim plain, Western Siberia Lithol. Miner. Resour 38 427-446

[17] Kuz’mina O.B.(1982)Reasons for the outbreak of microphytoplankton productivity in the late Oligocene Turtas Lake–Sea, Western Siberia Nature 299 715-717

[18] Benson M.L.(2018)Lithological, lithochemical, and geochemical indicators of paleoclimate: Evidence from Riphean of the Southern Urals Nova Hedwigia 147 183-192

[19] Kociolek J.P.(1989)Early Proterozoic climates and plate motions inferred from major element chemistry of lutites Dokl. Akad. Nauk SSSR 308 428-431

[20] Spaulding S.A.(1990)Transfer of extant non-marine diatom Bot. Zh 75 1565-1567