Расчленение лугинецкого горизонта верхнего девона центральной части Западной Сибири С. Н. Макаренко, Л. Г. Перегоедов, С. А. Родыгин, Н. И. Савина
Material type: ArticleOther title: Dividing of the Luginetsk horizon of the Upper Devonian in the central part of Western Siberia [Parallel title]Subject(s): Западная Сибирь | лугинецкая свита | верхний девон | стратиграфические исследованияGenre/Form: статьи в сборниках Online resources: Click here to access online In: Эволюция жизни на Земле : материалы V Международного симпозиума, 12-16 ноября 2018 г С. 89-92Abstract: Based on a complex of paleontological materials, the Luginetsk horizon of the Upper Devonian is divided into two subhorizons. The Lower Luginetsk subhorizon corresponds to the Frasnian stage, and the Upper Luginetsk subhorizon corresponds to the Famennian stage. Both are characterized by beds with fauna or zones: foraminifers, ostracodes, conodonts, tentaculites, stromatoporoids, tabulates, brachiopods.Библиогр.: 5 назв.
Based on a complex of paleontological materials, the Luginetsk horizon of the Upper Devonian is divided into two
subhorizons. The Lower Luginetsk subhorizon corresponds to the Frasnian stage, and the Upper Luginetsk subhorizon
corresponds to the Famennian stage. Both are characterized by beds with fauna or zones: foraminifers, ostracodes, conodonts,
tentaculites, stromatoporoids, tabulates, brachiopods.
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