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Middle Jurassic continental biota and paleolandscape in the Dubinino locality (Sharypovo area, Krasnoyarsk Krai) S. V. Ivantsov, L. I. Bystritskaya, S. A. Krasnolutskii [et.al.]

Contributor(s): Ivantsov, Stepan V | Krasnolutskii, S. A | Lyalyuk, K. P | Frolov, A. O | Alekseev, A. S | Bystritskaya, L. IMaterial type: ArticleArticleSubject(s): биота | палеоландшафты | юрский период | палеогеографияGenre/Form: статьи в журналах Online resources: Click here to access online In: Stratigraphy and geological correlation Vol. 24, № 5. P. 486-502Abstract: On the basis of the lithological-facies analysis, it was established that deposits of the Upper Itat Subformation, comprising the Dubinino locality of the Middle Jurassic flora and insects (Sharypovo district, Krasnoyarsk krai), accumulated in alluvial and lacustrine and, to a lesser extent, floodplain environments (floodplain and alluvial fan facies). The occurrence of remains of insects, macroremains of flora, spores, and pollen allowed us to make a paleoreconstruction of an area with a strongly dissected relief: continental fresh-water reservoir (lake) with varying degree of overflow, surrounded by hills covered with gymnospermous and ginkgo forests.
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Библиогр.: с. 501-502

On the basis of the lithological-facies analysis, it was established that deposits of the Upper Itat Subformation, comprising the Dubinino locality of the Middle Jurassic flora and insects (Sharypovo district, Krasnoyarsk krai), accumulated in alluvial and lacustrine and, to a lesser extent, floodplain environments (floodplain and alluvial fan facies). The occurrence of remains of insects, macroremains of flora, spores, and pollen allowed us to make a paleoreconstruction of an area with a strongly dissected relief: continental fresh-water reservoir (lake) with varying degree of overflow, surrounded by hills covered with gymnospermous and ginkgo forests.

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