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ISSN: 2542-2006

Ecology and dynamics

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Ecology and dynamics
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Articles. No.2, 2025

REVIEW OF SOILSALINIZATIONINTHE RUSSIAN NORTH FOR THE PERIOD OF 1933-2024

Ecology and dynamics Опубликовано 18 августа, 2025 автором admin7 ноября, 2025

Chernousenko G.I. Review of Soil Salinization in the Russian North for the Period of 1933-2024  // Ecosystems: ecology and dynamics. No 2. 2025. P. 43-78. | Abstract | PDF | Reference

 

 

Marsh soils: a) on the coast of the Laptev Sea, b) on the coast of the East Siberian Sea (National Report …, 2024)
Saline soils of permafrost areas of Yakutia, in the Lena River valley (photo by G.I.Chernousenko)
Valley of the Lena River, Yakutia (photo by G.I.Chernousenko)

Preparation for the study of saline soils in the Lena River valley, Yakutia (photo by G.I.Chernousenko)
Study of cultivated saline soils in the Lena River valley, Yakutia (photo by G.I.Chernousenko)
Landscapes with saline soils in the permafrost areas of Buryatia, Barguzin Basin (photo by G.I.Chernousenko)

In this article the works on the soil salinization of the Arctic coast, adjacent subarctic regions of Russia and the Arctic Oceanislands are summarizes, and the definitions of saline soils and saline grounds are explained. Additionally, the distribution and types of frozen saline rocks in coastal zones, sources of salts and factors that determine the specifics of soil formation, including salinization methods and processes (such as leaching of rocks, exchange reactions, desulfation, freezing/thawing), are considered. The existing classifications of coastal soils are analyzed. The distribution, chemistry and degree of soil salinization are studiedusingthe analytical data: starting from the coast of the White Sea and the Ainov Islands of the Barents Sea in the west, to the Chukchi coast and Wrangel Island in the east. Salinization was registered on the coast of the White, Barents, Kara, East Siberian and Laptev Seas, on the Yugorsk and the Yamal Peninsulas, on Vaygach, Sharapovy Koshki, Bolshevik, Bolshoy and Maly Lyakhovsky, Faddeyevsky, Wrangel, Dunay islands, and the Severnaya Zemlya archipelago. The chemistry of soil salinization was thoroughly considered to find out that chloride-sodium chemistry dominates closer to the sea, in the peat soils and soils with a heavier granulometric composition. Meanwhile, on lighter rocks further from the coast, as well as inthe soils on marine terraceswith mobile chlorides washed out from the profile, sulfates begin to predominate, and their chemistry is mostly chloride-sulfate, sometimes with gypsum. In soils with gypsum, the proportion of magnesium is higher, or even dominant in some cases. Soil salinization varies from weak to solonchaks. The ongoing climate aridization will eventually redistributethe saline territories and, possibly, reduce their area due to permafrost degradation and a probable increase in precipitation. Aridization of the northern regions might change the dominant chemistry of salinization, meaning that the predominantly chloride type will most likelychange to chloride-sulfate or sulfate magnesium-sodium.

Keywords: chemistry, degree of salinization, genesis of salts, analytical data, climate change.

DOI: 10.24412/2542-2006-2025-2-43-78

EDN: BLLZXW

Метки: analytical data, chemistry, climate change, degree of salinization, genesis of salts

EMPIRICAL-SIMULATION PREDICTIVE MODELING OF FOREST ECOSYSTEMS IN THEIR CLIMATOGENIC MONITORING

Ecology and dynamics Опубликовано 18 августа, 2025 автором admin7 ноября, 2025

Kolomyts E.G. Empirical-simulation Predictive Modeling of Forest Ecosystems in Their Climatogenic Monitoring // Ecosystems: ecology and dynamics. No 2. 2025. P. 79-104. | Abstract | PDF | Reference

The article presents a strategy for studying the mechanisms of functional and structural organization of forest ecosystems as objects of terrestrial geosystem monitoring. The spatial-functional monitoring of forests is based on empirically established local and regional landscape-ecological connections, which are considered as mechanisms of metabolic reactions of forest ecosystems to certain climatic trends. This is the novelty of the basic and predictive empirical-simulation concept of regional and local geoecological monitoring developed by the author. Ordination analysis of landscape connections is aimed at identifying transitions of forest communities to critical states according to the main discrete parameters of biological circulation. Catenary landscape-ecological structures that form regional systems of localized natural zonality are capable of imitating the main directions and scales of geosystemic restructurings. Landscape-ecological forecasting is experimental in nature. It is presented as a system of operations with ecological (hydrothermal) niches of the objects under study. In calculation models, the course of predicted processes is reproduced using their empirical imitation by spatially distributed parameters of basic ecological niches. The description of future states of biogeocoenotic systems is carried out according to their current spatial organization in accordance with the fundamental properties of ergodicity of the natural environment. The ambiguous nature of the transformation of forest topogeosystems is revealed at a fixed value of the regional geophysical trend, when their new state can have features of not one, but several basic states. A working algorithm for predictive landscape-ecological calculations is presented. Based on geoecological forecasts, the problem of regulating the quality of the natural environment under global climate change through carbon balances and the functional stability of forest ecosystems is covered.

Keywords: climate change, forest ecosystems, geoecological monitoring, empirical-statistical modeling, ordination analysis, empirical simulation of regional climatic trends, polyzonality of biogeocoenological systems, landscape-ecological forecasting.

DOI: 10.24412/2542-2006-2025-2-79-103

EDN: TXDHTT

Метки: climate change, empirical simulation of regional climatic trends, empirical-statistical modeling, forest ecosystems, geoecological monitoring, landscape-ecological forecasting, ordination analysis, polyzonality of biogeocoenological systems

POPULATION INDICES AND FAUNA COMPOSITION OF SMALL MAMMALS IN THE ZEYA NATURE RESERVE AND ITS ADJACENT TERRITORIES UNDER THE INFLUENCE OF NATURE AND HYDRAULIC CONSTRUCTION

Ecology and dynamics Опубликовано 18 августа, 2025 автором admin7 ноября, 2025

Podolsky S.A., Levik L.Yu., Pavlova K.P., Chemirskaya D.S., Chervova  L.V. Population Indices and Fauna Composition of Small Mammals in the Zeya Nature Reserve and Its Adjacent Territories under the Influence of Nature and Hydraulic Construction // Ecosystems: ecology and dynamics. No 2. 2025. P. 105-130. | Abstract | PDF | Reference

 

Roe deer at the ford on the Nora River (photo by S.A.Podolsky) 2. Swimming fawns of roe deer (photo by S.A.Podolsky)
Swimming fawns of roe deer (photo by S.A.Podolsky)
Lenok, or Asiatic trout (photo by S.A.Podolsky)
Oriental stork (photo by S.A.Podolsky)

Red-crownedcranes (photo by S.A.Podolsky)
Hooded crane taking off (photo by S.A.Podolsky)
Hooded cranes (photo by S.A.Podolsky)
A hut flooded by the Bureya water reservoir (photo by S.A.Podolsky)

The construction of large water reservoirs in the Amur Region causes numerous negative environmental consequences, changing the boundaries of species’ ranges, as well as reducing the species diversity in zoocomplexes and the number of many animal species. In addition, populations and communities under the influence of reservoirs continue to experience fluctuations due to natural processes. A reliable group of indicators for studying the impact of hydroelectric construction on terrestrial animals are small mammals, such as Rodentia and Eulipotyphla, most of which undergo frequent generational changes and, therefore, have a quick response to changes in their habitats.

In this article, we consider the main natural factors influencing the dynamics of the number of Rodentia and Eulipotyphla in the Zeya Nature Reserve, as well as changes in the abundance and fauna composition of small mammal communities on the shores of the Zeya Water Reservoir and in the influence zone of the Lower Zeya Hydroelectric Complex which is currently under construction. In the reserve and on the reservoir shores, we discovered 16 Rodentia species and 6 Eulipotyphla species. The dynamics of Rodentia number was studied on the basis of data obtained in 1982-2024, namely, from the censuses conducted on 27 trap-lines, with a total volume of about 48.5 thousand spring-loaded bar trap-days. The dynamics of Eulipotyphla was studied on the basis of data from 2003-2024, i.e., the censuses conducted on 8 trap-lines, with a total volume of about 22.9 thousand pitfall trap-days. In the reserve, we picked a zone on the mountainous shores for experimental observations, and another one that included low mountains outside the shores for background observations,

The main impact factors of the hydroelectric construction on the marginal and rare species of small mammals in the upper pool of the Zeya Reservoir are the flooding of valley habitats and the isolation of small groups of animals in the remaining habitats in the estuary areas of the valleys of the reservoir’s tributaries. Due to that the fauna of Rodentia and Eulipotyphla is already significantly depleted on the shores. The following species have disappeared from the area almost entirely: long-tailed ground squirrel (Urocitellus undulatus Pallas, 1779), reed vole (Alexandromys fortis Buchner, 1889), Amur lemming (Lemmus lemmus amurensis Vinogradov, 1924), slender shrew (Sorex gracillimus Thomas, 1907), Eurasian least shrew (Sorex minutissimus Zimmermann, 1780). Meanwhile, such species as the Maximowicz’s vole (Alexandromys maximowiczii Schrenk, 1859), tundra vole (Alexandromys oeconomus Pallas, 1776), striped field mouse (Apodemus agrarius Pallas, 1771), harvest mouse (Micromys minutus Pallas, 1771), flat-skulled shrew (Sorex roboratus Hollister, 1913), and Siberian large-toothed shrew (Sorex daphaenodon Thomas, 1907) changed their “common” or “numerous” status to “very rare”. Similar changes should be expected to occur on the shores of the Nizhne-Zeyskoye Reservoir, which is currently under construction.

The most significant influence factor of a large reservoir on the background species, such as the northern red-backed vole (Myodes rutilus Pallas, 1779), grey red-backed vole (Craseomys rufocanus Sundevall, 1846), and Laxmann’s shrew (Sorex caecutiens Laxmann, 1788), is its climate impact on the biotopes of the shores. It occurs at the same time with the natural number fluctuations of small mammals associated with the main abiotic natural factors, e.g., solar activity, precipitation and temperatures during the period of most active reproduction and the beginning of vegetation (May-June), as well as with the depth of snow cover. Both Rodentia and Eulipotyphla have an inverse correlation between the population dynamic and the amount of precipitation in May-June, as well as a direct correlation between the population dynamic and average temperatures in May-June. At the same time, for the influence zone of the Zeya Reservoir, a close and direct connection has been established between long-term changes in solar activity and precipitation in May-June.

Aside from short 3-4-year fluctuations, Rodentia species go through a long, almost 30-year-long cycle, occurring in an antiphase with similar fluctuations of the Wolf number curve; the population dynamic of Eulipotyphla is in an antiphase with 10-11-year-long cycles of solar activity.

The coasts of the Zeya Reservoir, we have discovered the deepest depressions and maximum amplitudes of population fluctuations both for Rodentia and Eulipotyphla. Moreover, shores such as these tend to become a zone of low abundance of small mammals. In Zeya, average annual losses compared to the background indicators are 8.7-16.2% for Rodentia, and 22.1% for Eulipotyphla. This causes deterioration in the food supply of many birds of prey and Mustelidae that feed on small mammals.

We have established that hydroelectric construction in the north of the Amur Region significantly reduces the species abundance and productivity of small mammal communities, which entails further losses in biodiversity. Due to both natural and anthropogenic factors, the coasts of large manmade water reservoirs turn into zones of reduced abundance of Rodentia and Eulipotyphla.

Acknowledgements. We are grateful to the management of the Zeya Nature Reserve for their help with organization and research.

Funding. This work was carried out for the Water Problems Institute of the Russian Academy of Sciences, theme No. FMWZ-2025-0002 “Researching the Formation Processes of the Surface and Ground Waters Quality, Natural and Anthropogenic Mechanisms of Ecological Changes in the Water Bodies, Development of Methods and Technologies for Managing Water Resources and Water Quality”, theme No. 1-22-37-1 of the Zeya Nature Reserve “Dynamics of Phenomena and Processes in the Ecosystems of the Zeya Nature Reserve and the Tokinsko-Stanovoy National Park”, state task No. 121051100137-4 of the Lomonosov Moscow State University (MSU) “Spatio-temporal Organization of Ecosystems under Environmental Change”; additionally, it was supported by the Development Program of the Interdisciplinary Scientific and Educational School of MSU “Future of the Planet and Global Environmental Change” and the Development Program of MSU (P. 1220).

Keywords: Rodentia, Eulipotyphla, fauna composition, population dynamic, influence zone of water reservoir, solar activity, precipitation, air temperature.

DOI: 10.24412/2542-2006-2025-2-104-129

EDN: YUUIHG

Метки: air temperature, Eulipotyphla, fauna composition, influence zone of water reservoir, population dynamic, precipitation, Rodentia, solar activity

A REVIEW OF SOME PROBLEMS REGARDING THE RESEARCH OF EUTROPHICATION OF FRESHWATER RESERVOIRS

Ecology and dynamics Опубликовано 18 августа, 2025 автором admin7 ноября, 2025

Datsenko Y.S. A Review of Some Problems Regarding the Research of Eutrophication of Freshwater Reservoirs // Ecosystems: ecology and dynamics. No 2. 2025. P. 131-144. | Abstract | PDF | Reference

 

 

Upper reaches of the Mozhaisk Reservoir (photo by Yu.S.Datsenko)
Hydrobiology (photo by Yu.S.Datsenko)
Hydrochemical sampling (photo by Yu.S.Datsenko)
Overgrowing shallow waters (photo by Yu.S.Datsenko)

Meteorological observations on a reservoir shore (photo by Yu.S.Datsenko)
Water sampling for chemical analysis (photo by Yu.S.Datsenko)
Sampling (photo by Yu.S.Datsenko)

Titration of water samples (photo by Yu.S.Datsenko)
Installation of sediment traps-1 (photo by Yu.S.Datsenko)
Blooming algae in a water reservoir (photo by Yu.S.Datsenko)

In this article we analyze the modern view on the effect that abiotic factors (hydrological, hydrophysical, hydrochemical) have on the primary productivity of water reservoirs, and the differences in the development of the eutrophication process in lakes and reservoirs, as well as the problems associated with assessing the trophic status of reservoirs. Using the results of model calculations performed for the Mozhaisk Reservoir, we show the features of the trend of changes in the state of the reservoir ecosystem.

Funding. This work was carried out as part of the state task for the Department of Land Hydrology of Moscow State University “Analysis, Modeling and Forecasting of Changes in Hydrological Systems, Water Resources and Quality of Surface Water” (I.10, TsITIS No. 121051400038-1)

Keywords: eutrophication, primary productivity, abiotic factors, reservoirs.

DOI: 10.24412/2542-2006-2025-2-130-143

EDN: ZZQFIN

Метки: abiotic factors, eutrophication, primary productivity, reservoirs

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