Final evolutionary stage of late Cenozoic floras of the Turgay ecological type in Primorye

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Abstract

Based on the comparison of the Late Oligocene-Miocene floras of Primorye (floras of Nezhino and Dorozhny quarry) with the well-known Late Oligocene flora of Ashutas Mountain in Kazakhstan, which is one of the most typical floras of the Turgay ecological type, it is proven that Primorye floras also belong to the above-mentioned type. Comments are given on the use of the concepts of vegetation, flora, and species distribution. Photographs of the most typical plants from a new locality of the Ust-Suifun flora (pt. 9155) are presented with brief free-form comments.

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About the authors

Boris I. Pavlyutkin

Far East Geological Institute, FEB RAS

Author for correspondence.
Email: pavlyutkin@fegi.ru
ORCID iD: 0009-0003-8297-1985

Doctor of Sciences in Geology and Mineralogy, Leading Researcher

Russian Federation, Vladivostok

Igor Yu. Chekryzhov

Far East Geological Institute, FEB RAS

Email: chekr2004@mail.ru
ORCID iD: 0000-0002-0319-8759

Researcher

Russian Federation, Vladivostok

Tatyana I. Petrenko

Far East Geological Institute, FEB RAS

Email: tipetro@fegi.ru
ORCID iD: 0000-0002-4921-8938

Researcher

Russian Federation, Vladivostok

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2. Fig. 1. Location of the Dorozhny quarry, t. 9155

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3. Fig. 2. Leaves and fruits from the location of the Ust-Suifun flora, t. 9155. A

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