scholarly journals Species diversity of grass and shrub layer under the canopy of artificial and natural spruce dendrocenoses in herb-moss spruce forest of Southern Taiga subzone in the Middle Urals

Author(s):  
G. G. Terekhov ◽  
◽  
E. M. Andreeva ◽  
S. K. Stetsenko ◽  
S. I. Konashova ◽  
...  
Author(s):  
M. A. Glazyrina ◽  
N. Yu. Barkova ◽  
N. V. Lukina ◽  
E. I. Filimonova

The article presents the results of studying the coenopopulations of Moneses uniflora (L.) A. Gray (familyEricaceae Juss.) found during the monitoring of vegetation formation on the dumps of the mining and processing industryof the Sverdlovsk region (Middle Urals, southern taiga subzone). Studies have shown that the M. uniflora (family EricaceaeJuss.) coenopopulations in plant communities formed on industrial dumps and in natural phytocenosis are normal, fullfledged, young. The morphological parameters of generative individuals are significantly influenced by coenotic andedaphic factors. Arbutoid mycorrhiza was found in the thin roots of M. uniflora in all the studied habitats.


Metals ◽  
2021 ◽  
Vol 11 (10) ◽  
pp. 1589
Author(s):  
Maria Dergacheva ◽  
Valentina Trunova ◽  
Olga Nekrasova ◽  
Tatyana Siromlya ◽  
Anton Uchaev ◽  
...  

The paper considers the macro- and micro- element composition of two ash dumps in the Middle Urals, where meadow and forest communities have been spontaneously forming for 50 years, as well as the effect of the plants on the changing composition of the ash. Higher contents of Cu, Co, Sn, Ga, and Yb were found in the deep ash layers of both dumps, while in the upper 20-cm layer, the trace element composition depended on the influence of different plant communities. Higher contents of Sr, Cr, Ni, Sn, and Co were revealed under meadows, and Ba, Zr, and La were found under the forest. The levels of element accumulation in the aboveground and underground parts of dominant plants were revealed. Increased content of Be, Ce, Ga, La, Sc, Y, and Yb was detected in areas where meadow plants were dominant and Zn and Ba in forest areas. The toxic elements Cd and Pb were highly accumulated in both communities, whereas Co was found only in meadows. The studied materials can serve as a base to assess the feasibility of processing and/or utilizing fly ash from ash dumps in the Middle Urals and similar ash dumps in other regions situated in the southern taiga.


2015 ◽  
pp. 85-107 ◽  
Author(s):  
N. N. Lashchinsky ◽  
A. Yu. Korolyuk

The dark-coniferous forests of the West Siberian southern taiga subzone are quite unique. They deter­mine a specific of the Ob’-Irtysh geobotanical field in a sense of V. B. Sochava (1948) together with the West Siberian zonation type (Shumilova, 1979). The main features of zonal southern taiga forests are: dominance of Abies sibirica in a tree layer; species-rich shrub layer; poor ground moss cover; well developed herb layer with a constant presence of nemoral species. We consider the southern taiga forests as hemi­boreal after L. Hдmet-Ahti (1963, 1981). We described the zonal dark-coniferous forests of southern taiga in Milio effusi–Abietetea sibiricae class first proposed by T. I. Zhitlukhina (1988) for the forests in the North-East Altai. Significant increasing of the area studied and existing syntaxa diversity make it necessary to change a diagnostic species group. A new combination of diagnostic species includes Abies sibirica, Padus avium, Lonicera xylosteum, Daphne mezereum, Rubus idaeus, Aconitum septentrionale, Dryopteris dilatata (incl. D. expansa), D. carthusiana, Urtica dioica, Milium effusum, Calamagrostis obtusata, Paris quadrifolia, Allium microdictyon, Stellaria bungeana, Oxalis acetosella, Circaea alpina. Most of Milio effusi–Abietetea sibiricae class communities occur in the West Siberian plain, which is relatively geologicaly young. Due to this fact a flora of southern taiga is mostly allochtonic formed by species migrations fr om the Eastern Europe and the Southern Siberian mountains. Among the diagnostic species the main dominants of tree layer (Abies sibirica) and herb layers (Calamagrostis obtusata and Aconitum septentrionale) have the North Asian distribution. Two shrub species Lonicera xylosteum and Daphne mezereum are European ones and two herbaceous species (Allium microdictyon and Stellaria bungeana) are represented in Europe by vicariant species. All other diagnostic species are Eurasian or Holarctic. Wide distribution of few species, in particular ferns, could be explained by the antiquity of taiga flora (Tolmachev, 1954). Typical habitats of Milio effusi–Abietetea sibiricae forests are the most humid areas with annual precipitation about 500–600 mm on plains and more than 800 mm in mountains. Soils on plains developed under these communities are deeply podzolised type with second humus horizon. In the low-mountains the deeply podzolised soddy-podzolic soils correlate to the area of Milio effusi–Abietetea sibiricae forests distribution. The northern lim it of southern taiga perfectly coincides with the southern border of the largest Pleistocene glaciations. The low mountains of Altai-Sayan system were never glaciated. The thick loess deposits help to survive some nemoral plant species in the isolated refuges. Milio effusi–Abietetea sibiricae class consists of two orders. The order Carici macrourae–Abietetalia sibiri­cae comprises zonal dark-coniferous forests of the West Siberian southern taiga subzone and their successional variants. Diagnostic species are the same as for Carici macrourae–Abietion sibiricae alliance and Aegopodio podagrariae–Abietetum sibiricae association: Gymnocarpium dryopteris, Rubus saxa­tilis, Carex macroura, Aegopodium podagraria, Viola selkirkii, Galium triflorum, Atragene sibirica, Actaea erythrocarpa, Ribes spicata, Stellaria holostea. It contains the alliance Carici macrourae–Abietion sibiricae and three associations. One of these was previously described by N. B. Ermakov but two others are new. Aegopodio podagrariae–Abietetum sibiricae association includes the primary zonal coniferous forests of the West Siberian southern taiga as well as successional stages after some catastrophic events (crown fires, windfall, etc.). Usually it is characterized by closed canopy with Abies sibirica dominance, species-rich shrub layer and well-developed herb layer with high coverage of Carex macroura, Aegopodium podagraria, Stellaria bungeana, Oxalis acetosella and Calamagrostis obtusata. Linnaeo borealis–Abietetum sibiricae association comprises the zonal coniferous forests grown in the northern part of southern taiga subzone. Its diagnostic species: Linnaea borealis, Trientalis europaea, Luzula pilosa, Orthilia secunda, Lycopodium annotinum, Vaccinium vitis-idaea are common for the Vaccinio-Piceetea class communities. In contrast with previous association Linnaeo borealis–Abietetum sibiricae communities are characterized by multi-dominant tree layer with slight predominance of Abies sibirica; shrub layer is sparse and not so species-rich, in herb layer the main dominants are Carex macroura, Oxalis acetosella, Calamagrostis obtusata, Gymnocarpium dryopteris and sometimes big ferns. Moss cover is about 20 to 40% of soil surface. The order Abietetalia sibiricae consists of low-mountain chernevaya taiga and dark-coniferous mountain forests of the Altai-Sayan humid sectors. A set of diagnostic species includes Ribes atropurpureum, Saussurea latifolia, Geranium albi­flo­­rom (incl. G. krylovii), Euphorbia lutescens, Myoso­tis krylovii, Viola uniflora, Dryopteris filix-mas, Heracleum dissectum, Trollius asiaticus, Anemonoides altaica, Corydalis bracteata, Erythronium sibiricum. The most of diagnostic species are north-Asian or south-Siberian ones. Many of them are mountainous restricted to the Altai-Sayan mountain system. This order includes one alliance Milio effusi–Abietion sibiricae previously described by T. I. Zhitlukhina and N. B. Ermakov. Seven associations belonging to this alliance were described and characterized by N. B. Ermakov (2003). When thinking about further development of the class syntaxonomy we expect the diversity increasing by serial communities of mixed and small-leaved forests and swampy forests on a plain. We do not discuss western and eastern class limits now. No doubt that distribution area of the new class is wider than the West Siberia but to describe its limits and an interaction with neighboring classes some additional materials are needed.


2020 ◽  
Vol 24 ◽  
pp. 00090
Author(s):  
Evgeniya Vasfilova ◽  
Tat’yana Vorob’eva

Under conditions of introduction into the subzone of the southern taiga of the Middle Urals, species that are little known as medicinal plants in European countries and in Russia have been studied. These species have a wide spectrum of pharmacological action and are promising for use. Success of introduction was the most for Agastache foeniculum (Pursh) Kuntze, A. scrophulariifolia (Willd.) Kuntze, A. urticifolia (Benth.) Kuntze, Echinacea pallida (Nutt.) Nutt., Campanula rapunculoides L., C. latifolia L. These species are characterized by high winter hardiness, stable fruiting, give self-seeding, accumulate a sufficiently large biomass, are not damaged by diseases and pests.


LITOSFERA ◽  
2020 ◽  
Vol 20 (2) ◽  
pp. 224-230
Author(s):  
V. N. Smirnov ◽  
K. S. Ivanov ◽  
T. V. Bayanova

Research subject. The article presents the results of dating two dolerite dikes differing in geochemical features from a section along the Iset river in the area of Smolinskoe settlement (the Eastern zone of the Middle Urals). Materials and methods. The dating was performed by an U-Pb ID-TIMS technique for single zircon grains using an artificial 205Pb/235U tracer in the laboratory of geochronology and isotope geochemistry of the Geological Institute of the Kola Science Centre of the Russian Academy of Sciences. The lead isotopic composition and uranium and lead concentrations were measured using a Finnigan-MAT (RPQ) seven-channel mass spectrometer in dynamic mode using a secondary electron multiplier and RPQ quadrupole in ion counting mode. Results. The dikes were dated 330 ± 3 Ma and 240 ± 2 Ma. Conclusions. The research results indicate different ages of dolerite dikes developed within the Eastern zone of the Middle Urals. The oldest of the two established age levels corresponds to the Early Carboniferous era. This fact, along with the proximity of the dolerites to the petrochemical features of the basaltoids of the Early Carboniferous Beklenischevsky volcanic complex, allows these bodies to be considered as hypabyssal comagmates of these volcanics. The youngest obtained age level – Triassic – indicates that the introduction of some dolerite dikes was associated with the final phases of the trapp formation developed rarely within the eastern outskirts of the Urals and widely further east in the foundation (pre-Jurassic basement) of the West-Siberian Plate.


2015 ◽  
Vol 46 (3) ◽  
pp. 213-221 ◽  
Author(s):  
T. V. Zhuikova ◽  
E. V. Meling ◽  
S. Yu. Kaigorodova ◽  
V. S. Bezel’ ◽  
V. A. Gordeeva

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