The First Finding of Foliar Flora Fossils in the Section of Cenozoic Deposits of Sardakh-Sise Island (Lena River Delta)
- Autores: Khazin L.B.1,2, Kuzmina O.B.1,2, Khazina I.V.1, Lashchinskiy N.N.1,3, Kartoziia A.A.1,2,4, Kashirtsev V.A.1,2
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Afiliações:
- Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences
- Novosibirsk State University
- Central Siberian Botanical Garden
- Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
- Edição: Volume 487, Nº 1 (2019)
- Páginas: 766-768
- Seção: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/195199
- DOI: https://doi.org/10.1134/S1028334X19070122
- ID: 195199
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Resumo
The first findings of well-preserved foliar flora (Platanus sp., Alnus sp., Fagus sp., Salix sp., and Magnolia sp.) have been recovered from the Late Cenozoic (Neogene) deposits on Sardakh-Sise Island, in the Lena River delta. The findings, which also include remains of coniferous wood, are hosted in ferruginized sandstones at the base of the section. The floral composition suggests that mixed forests incorporating coniferous, broad- and small-leaved deciduous trees, and shrubs (moderate and subtropical thermophytes) grew in this area. The deposits contain foliar flora could forms in the Early–Middle Miocene, not in the Pliocene as is presently believed. Most likely, the basal conglomerates and sandstones of the Sardakh-Sise Island section refer to the Urasalakh Fm. The finding site of Neogene foliar flora on Sardakh-Sise Island is now the northernmost location in Eurasia.
Sobre autores
L. Khazin
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Autor responsável pela correspondência
Email: lbkhazin@gmail.com
Rússia, Novosibirsk, 630090; Novosibirsk, 630090
O. Kuzmina
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Email: KashircevVA@ipgg.sbras.ru
Rússia, Novosibirsk, 630090; Novosibirsk, 630090
I. Khazina
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences
Email: KashircevVA@ipgg.sbras.ru
Rússia, Novosibirsk, 630090
N. Lashchinskiy
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Central Siberian Botanical Garden
Email: KashircevVA@ipgg.sbras.ru
Rússia, Novosibirsk, 630090; Novosibirsk,
630090
A. Kartoziia
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University; Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Email: KashircevVA@ipgg.sbras.ru
Rússia, Novosibirsk, 630090; Novosibirsk, 630090; Novosibirsk,
630090
V. Kashirtsev
Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences; Novosibirsk State University
Autor responsável pela correspondência
Email: KashircevVA@ipgg.sbras.ru
Rússia, Novosibirsk, 630090; Novosibirsk, 630090
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