Accumulation Features of Debris in Mature Pine Forests of Middle Taiga in the Republic of Karelia

Author(s):  
S.A. Moshnikov ◽  
◽  
V.A. Anan’yev ◽  
V.A. Matyushkin
2018 ◽  
Vol 19 (4) ◽  
pp. 1194-1206 ◽  
Author(s):  
ALEXANDER B. RUCHIN ◽  
ANDREY P. MIKHAILENKO

Ruchin A, Mikhailenko AP. 2018. Fauna of mantids and orthopterans (Insecta: Mantodea, Orthoptera) of the Mordovia StateNature Reserve, Russia. Biodiversitas 19: 1194-1206. The data on the distribution and habitat confinement of one Mantodea species and44 Orthoptera species in the Mordovia State Nature Reserve are given. Of these, one species of Orthoptera (Calliptamus italicus) isrecorded for the first time for the Mordovia State Nature Reserve, four species (Mantis religiosa, Phaneroptera falcata, Conocephalusfuscus, Tettigonia caudata) are recently penetrated, one species (Conocephalus fuscus) is reported in the Republic of Mordovia for thefirst time. In the fauna of mantids and orthopterans of the Mordovia Reserve, three ecological groups were identified: polytopic, notconfined to certain biotopes (14 species), hygrophilous representatives of intrazonal habitats (5 species) and xerophiles. Among thelatter, there are species of extrazonal habitats (13 species) and confined to dry pine forests (7 species). The steppe group was notrepresented. For the three key habitats with the largest number of identified species, brief botanical descriptions are given. Factorsinfluencing the species composition and current state of fauna of mantises and orthopterans of the Mordovia Reserve are discussed, andmeasures are proposed for the conservation of vulnerable species.


2007 ◽  
pp. 32-39
Author(s):  
N. N. Goncharova ◽  
T. K. Yurkovskaya

The complex studies of mesotrophic and aapa mires in the Luza R. basin (subzone of middle taiga, Republic of Komi) have been carried out. The aapa mires have been recorded in this region for the first time, it was considered earlier that the southern boundary of distribution of aapa mires in the Republic went near the Peteldin settlement (southward of the Ust-Schugor R.). The general characteristics of different mire types has been given, the rare species of the Red Book of RK have been revealed. The decifering of aerial photos has been made and geobotanical maps have been compiled.


2007 ◽  
pp. 61-81 ◽  
Author(s):  
O. V. Morozova ◽  
L. B. Zaugolnova ◽  
L. G. Isaeva ◽  
V. A. Kostina

Results of a syntaxonomical study of the oligotrophic forests of northern European Russia are presented. The main forest types have been classified into 2 orders of the class Vaccinio-Piceetea, 4 alliances, 6 associations and 1 community. The new alliance Empetro-Piceion all. nov., which includes zonal spruce and birch northern forest association Empetro-Piceetum, has been established. These communities are formed according to cold temperature and high (sometimes temporarily) soil moisture and are characterized by the lower tree canopy, mosaic herb and moss-lichen layers with boreal mosses, sphagnum and lichens. In the middle taiga subzone these communities are replaced by Eu-Piceetum myrtilletosum. The forests with lichens are referred to order Cladonio-Vaccinietalia and divided into 4 associations. Lichen pine forests of the north-west of boreal zone were described as ass. Flavocetrario nivalis—Pinetum ass. nov. This association with a great number of lichens is differentiated by Cladonia arbuscula subsp. mitis, Flavocetraria nivalis, Cetraria ericetorum, Stereocaulon grande, Dicranum fuscescens, D. drummondii, Nephroma arcticum and species of Cladonia. The ass. Cadonio arbusculae—Pinetum (Caj. 1921) K.-Lund 1967 contains lichen pine forests with lower number of lichens and is distributed mostly in middle part of the taiga zone. The spruce-pine forests with mixed moss-lichen cover correspond to ass. Vaccinio-Pinetum. Ass. Hedysaro-Laricetum represents rich and well differentiated larch forests in the east of European Russia.


Author(s):  
Nimazhap Bayarzhapovich Badmaev ◽  
Aleksandr Vladimirovich Bazarov ◽  
Roman Sergeevich Sychev

The chapter presents the results of research in the Republic of Buryatia, where the number and area of fires have increased over the past 20 years due to the rise in temperature and aridity. Most of the fires are registered in the large river valleys where pine forests are formed, which have low soil moisture capacity. Fewer fires occurred on the Eastern Sayans, Khamar-Daban ridges, and the Stanovoye Highlands, where the precipitation maximum falls. A correlation analysis was carried out between meteorological parameters and fires in climate-contrasting forests. The lack of precipitation at the end of the previous summer, combined with the hot and dry spring weather of the current year, have a significant impact on fires in the arid ecosystems of the Transbaikal middle mountains. In the humid coastal climate of the Eastern Baikal region, the high temperature of the air determines the fires, but there is no precipitation.


Author(s):  
Irina Nikolaevna Bezkorovaynaya ◽  
Pavel Albertovich Tarasov ◽  
Irina Gennadievna Gette ◽  
Irina Andreevna Mogilnikova

2011 ◽  
Vol 44 (7) ◽  
pp. 731-738 ◽  
Author(s):  
P. A. Tarasov ◽  
V. A. Ivanov ◽  
G. A. Ivanova ◽  
E. N. Krasnoshchekova
Keyword(s):  

2020 ◽  
pp. 3-25
Author(s):  
I. A. Likhanova ◽  
G. S. Shushpannikova ◽  
G. V. Zheleznova ◽  
T. N. Pystina

Plant communities of sandy (quarry 3 — 62°05ʹ26ʺ N, 48°43ʹ56ʺ E; 6 — 61°57ʹ35ʺ N, 50°36ʹ22ʺ E) and sandy loam (1 — 62°06ʹ28ʺ N, 48°48ʹ48ʺ E; 2 — 62°06ʹ19ʺ N, 48°48ʹ42ʺ E; 4 — 62°04ʹ36ʺ N, 48°34ʹ55ʺ E; 8d — 61°44ʹ00ʺ N, 50°39ʹ05ʺ E) quarries and the surrounding lichen and green-moss pine forests quarries are charaterized. The research has been performed in the middle taiga subzone of the European North-East of Russia. Floristic classification (Braun-Blanquet, 1964) was made for 91 relevés. The Ellenberg ecological values (Ellenberg, 1974) were used to assess moisture (F), acidity (R) and nitrogen content (N). Ordination was made by NMS approach using ExcelToR software. Plant communities of renewing and young pine stands at the quarries as well as of surrounding middle aged and mature stands are assigned to the alliance Cladonio stellaris–Pinion sylvestris Kielland-Lund ex Ermakov et Morozova 2011 order Pinetalia sylvestris Oberdorfer 1957 class Vaccinio-Piceetea Br.-Bl. in Br.-Bl. et al. 1939 (Ermakov, Morozova, 2011) while communities of meadow succession stage to the union Cynosurion cristati Tx. 1947 order Arrhenatheretalia elatioris class Molinio-Arrhenatheretea Tx. 1937 (Mirkin, Naumova, 2012). Five associations, two subassociations, one variants, two subvarants and one community are established within two classes (among these, two associations. one variants, two subvariants and one community are new). Community Polytrichum piliferum (Table 3, rel. 1–7). DS: Ceratodon purpureus, Cladonia subulata, C. fimbriata, Niphotrichum canescens, Polytrichum piliferum, Salix acutifolia. These are pioneer communities at the second decade stage of succession on sandy substrate. (quarry 3) with recovering Pinus sylvestris tree layer, absence of herb-dwarf shrub layer and. presence of pioneer mosses (Polytrichum piliferum, Ceratodon purpureus), algal crusts, and lichen thalli of Cladonia, Peltigera, and Stereocaulon. Number of species — 32 (13–20). Ass. Polytricho piliferi–Pinetum sylvestris ass. nov. hoc loco (Table 3, rel. 8–30; nomenclature type (holotypus hoc loco) — rel. 18; Fig. 4). DS: Ceratodon purpureus, Cladonia gracilis ssp. turbinata, C. fimbriata, C. subulata, C. verticillata, Niphotrichum canescens, Peltigera malacea, Polytrichum piliferum, Salix acutifolia, Stereocaulon tomentosum. These are renewing pine forests at 3rd and 5th decades of succession with ground cover dominated by pioneer mosses and lichens in sandy quarries 3 and 6, and in the most drained habitats of sandy loam quarries 1, 2, 4 (slopes). Pine canopy density is 0.1–0.3, its height — 3–6 m. Herb-dwarf shrub layer is scarce (1– 10 %), that of moss-lichen is of 20–80 %. Number of species — 111 (27–45). Subass. Deschampsio–Agrostietum tenuis typicum Turubanova 1986. D S : Agrostis tenuis, Deschampsia cespitosa, Galium mollugo, Hieracium umbellatum, Leucanthemum vulgare, Pimpinella saxifraga, Stellaria graminea. These are communities of short meadow succesion stage at the sandy loam quarries 1, 2, 4, 8d. Unlike meadows of abandoned lands and pastures, described by L. P. Turubanova (1986) as subass. Deschampsio–Agrostietum tenuis typicum, the communities on technogenic habitats have lower abundance of meadow species and higher diversity of synanthropic and xerophylous species, as well as tree invasion. This is a reason to establish variant Calamagrostis epigeios (Table 4, Fig. 5) within the subass. typicum. Its DS: Betula pendula/pubescens, Calamagrostis epigeios, Ceratodon purpureus, Chamaenerion angustifolium, Erigeron acris, Pinus sylvestris, Tussilago farfara. Multispecies herb layer is mainly formed by meadow species and weeds (20–80 %). PC of moss layer — 1–50 %. Number of species — 103 (30–41). Duration of meadow stage is responsible for differences between subvariants Amoria hybrida and Trifolium medium. Ass. Polytricho juniperini–Pinetum sylvestris ass. nov. hoc loco (Table 5, nomenclature type (holotypus hoc loco) — rel. 9; Fig. 6). D S : Agrostis tenuis, Amoria repens, Brachythecium salebrosum, Orthilia secunda, Peltigera didactyla, Polytrichum juniperinum, Pyrola media, Trifolium medium, Vicia sepium. These communities are young pine stands at the third decade of succession on sandy loam in quarries 1, 2, 4, 8d. Canopy density of pines — 0.4–0.8, height — 4–8 m. There is a lot of species typical for meadow succession stage in scarce herb layer (5–40 %). as well as an occurrence of forest dwarf shrubs, and few species indicative to ass. Linnaeo borealis–Pinetum sylvestris. Moss-lichen layer (10–60 %) is formed by pioneer species and forest mosses. Number of species — 137 (27–67). NMS-ordination (Fig. 7) and data on substrate preferences of syntaxa as well as information about the duration of recovery process is the reason to built a scheme of vegetation succession in quarries in place of reduced pine trees after the cutting of lichen and green moss pine forests (Fig. 8). Series 1. Community Polytrichum piliferum (F 4.1, N 3.5, R 3.8) → ass. Polytricho piliferi–Pinetum sylvestris (F 4.1, N 3.5, R 4.1) → ??? → subass. Cladonio arbusculae–Pinetum sylvestris typicum (F 3.8, N 2.5, R 2.4). Series 2. Subvar. Amoria hybrida var. Calamagrostis epigeios subass. Deschampsio–Agrostietum tenuis typicum (F 4.4, N 4.8, R 5.4) → subvar. Trifolium medium var. Calamagrostis epigeios subass. Deschampsio–Agrostietum tenuis typicum (F 4.7, N 4.6, R 4.9) → асс. Polytricho juniperini–Pinetum sylvestris (F 4.5, N 3.9, R 4.3) → ??? → ass. Linnaeo borealis–Pinetum sylvestris (F 4.3, N 3.1, R 2.8). Additional studies are necessary to reveal the duration of succession period and intermediate stages of transition from ass. Polytricho piliferi–Pinetum sylvestris and Polytricho juniperini–Pinetum sylvestris to ass. Cladonio arbusculae–Pinetum sylvestris and Linnaeo borealis–Pinetum sylvestris. Thus, the restoration of lichen pine forests of subass. Cladonio arbusculae–Pinetum sylvestris typicum at sandy quarries passes through the stage of pine forests of ass. Polytricho piliferi–Pinetum sylvestris, which is preceded by pioneer vegetation of сommunity Polytrichum piliferum. The restoration of green moss pine forests (ass. Linnaeo borealis–Pinetum sylvestris) at sandy loam quarries passes through the stage of young pine stands (ass. Polytricho juniperini–Pinetum sylvestris), which is preceded by meadows of subvariantas Amoria hybrida and Trifolium medium var. Calamagrostis epigeios subass. Deschampsio–Agrostietum tenuis typicum.


The Holocene ◽  
2021 ◽  
pp. 095968362097279
Author(s):  
Kirill V Babeshko ◽  
Anna Shkurko ◽  
Andrey N Tsyganov ◽  
Elena E Severova ◽  
Mariusz Gałka ◽  
...  

A better understanding of past long-term environmental changes in the subarctic region is crucial for mitigation of the possible negative effects of climate warming in this vulnerable region. This study provides a new multi-proxy reconstruction of regional vegetation changes and peatland development for north-eastern Fennoscandia (Russia) during most of the Holocene. To that purpose, we performed plant macrofossil, pollen, testate amoebae, peat humification, loss on ignition and radiocarbon analyses of the peat deposits from a mire around Vodoprovodnoe Lake (the Kindo Peninsula, the Republic of Karelia). Our data indicate that the peat deposits started accumulating before 9147 ± 182 cal. yr. BP. The vegetation cover in the area was mainly typical for the northern taiga zone, except for the period ~7800–5600 cal. yr. BP, when it generally resembled the middle taiga zone. The vegetation cover and peatland were greatly affected by reoccurring fires, which can be partly related to human activity. These events were associated with an increased proportion of birch in the vegetation cover (as a pioneer species) and/or water level decreases. By 600 cal. yr. BP, the peatland and the surrounding vegetation reached its current state and only minor changes had been recorded since that time. Overall, our results suggest a considerable and unexpected role of fires in the postglacial dynamics of subarctic peatlands.


2018 ◽  
Vol 7 (1) ◽  
pp. 64-70
Author(s):  
Ecaterina Andreevna Luginina ◽  
Tatiana Leonidovna Egoshina

The paper presents data on phytocoenotic confinement and resource parameters of Arctostaphylos uva-ursi in Kirov Region. The species is close to phytocoenotic optimum in pine herbaceous-lichen forests in coniferous-broadleaved forests sub zone. The highest productivity of A. uva-ursi coenopopulations is marked in pine hebaceous-lichen forests (56,1 4,2 g/ m) where the species has maximum coverage (16,8 1,1%) and shoot length (17,7 0,8 cm). Presence of A. uva-ursi in communities increases southwards within the Region. A. uva-ursi is restricted to sandy and sabulous soils with high acidity level (pH 3,4-4,0), humus poor and insignificant content of phosphorus, potassium, calcium and magnesium. Reliable relation (р 0,05) between A. uva-ursi leaves productivity and Mg content in soil (r = 0,85) was defined. We have also determined straight and reliable connection between coverage, shoots number and productivity (R = 0,71-0,97). Raw material productivity can be presented by regression equation: P = Ао + А1C + А2N, где: P - Productivity (raw weight, g/m), C - coverage (%), N - number of shoot (per m). Biological stock (BS) of A. uva-ursi in Kirov Region reaches 285,5 t. Distribution of BS among vegetative subzones and administrative regions is uneven: 51% of BS (144,7 t) is concentrated in middle taiga subzone. Exploitation stock (ES) in the Region reaches 109,1 t. Volume of possible annual collection - 7,9 t, which is enough for local needs. In lichen pine forests with areas of A. uva-ursi in Kirov Region when 75% of peripheral shoots are cut , it does not recover within 5-years period between collections.


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