Boyarina, N. 2023. The Late Pennsylvanian vegetation of the Donets Basin, Ukraine:
Syntaxonomy of plant communities. GEO&BIO,
25: 64–98. [In English, with Ukrainian summary]
The Late Pennsylvanian vegetation of the Donets Basin, Ukraine:
A reconstruction and classification of Kasimovian and Gzhelian plant communities of
the Donets Basin that constituted the Late Pennsylvanian
vegetation cover of the region is proposed. Reconstructions of palaeophytocoenoses are based on the identification of
the floristic сomposition of fossil assemblages and the lithological-facial
features of plant-bearing strata from 69
phytooryctocoenoses that were found in more than 30 plant fossil localities and 20 boreholes within the Bahmut and Kalmius–Torets depressions.
The plant remains were studed from lacustrine,
swamp, deltaic, floodplain and lagoonal
deposits that indicate biotopes corresponding to coastal lowlands,
deltaic plains, floodplains and river valley slopes. The
morphological and quantitative
characteristics of plant fossils
indicate that these palaeophytocoenoses in different time intervals of the Late Pennsylvanian belonged to four vegetation types,
namely to coastal semi-aquatic vegetation, wetland forests, wetland woodlands and seasonally dry woodlands. The classification of
plant communities was conducted using the ecological and floristic approach
for vegetation classification by the Braun-Blanquet method. The identification of plant community types (syntaxa) from the lowest rank (association)
to the higher ranks (alliance,
order, and class) was made as a result of an
analysis of the floristic composition and ecological conditions of palaeophytocoenoses.
The major criteria for determining the syntaxa are the
diagnostic species including characteristic and differential species, which are
considered as indicators of environmental conditions. The
newly compiled prodromus
of Kasimovian and Gzhelian plant
communities consists of 11 classes, 16 orders, 21 alliances and 21
associations. The prodromus
reveals the syntaxonomic composition of the Late Pennsylvanianvegetation cover of
the Donets Basin and provides an
understanding of past vegetation dynamics. The syntaxonomic changes of vegetation are traced in the four
time intervals that are correspond
to regional stratigraphic units, namely Toretskian (Kasimovian), Kalynovian
(early Gzhelian), Luganskian (middle Gzhelian), and Vyskrivskian (late Gzhelian), and are
characterised by the plant associations of certain classes and orders.
Nataliya Boyarina; Institute
of Geological Sciences, NAS of Ukraine; 55-b
Oles Honchar Street, Kyiv, 01054 Ukraine; Email: nboyarina@ukr.net
Article info
Submitted: 01.06.2023. Accepted: 30.06.2023.
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