Soil formation under progressive accelerated succession of forest ecosystems in the North of Russia

2009 ◽  
Vol 2 (1) ◽  
pp. 66-71
Author(s):  
I. A. Likhanova ◽  
I. B. Archegova
2019 ◽  
Vol 13 (1) ◽  
pp. 125-132
Author(s):  
Kovalenko Ihor ◽  
Skliar Iurii ◽  
Klymenko Hanna ◽  
Kovalenko Nataliia

Background: The vitality level of the populations has turned out to be statistically reliably associated with such coenotic factors: age and density of forest stand. In general, the vitality spectra vary widely: the quality index Q of the populations ranges from 0,00 to 0,50, that is, it fully covers the theoretically possible scale of the values of this coefficient, which indicates the sensitivity of the vitality structure of the populations to the ecological-coenotic conditions and determines high informative value of the vitality analysis. Objective: The aim of the study is to assess the vitality structure of the populations of vegetative motile plant species – typical representatives of the grassy layer of forest ecosystems of the North-East of Ukraine as a factor that determines their stability and dynamics. Methods: The analysis of the vitality structure is based on the field studies of the populations of 4 vegetative motile species of plants – Aegopodium podagraria L., Asarum europaeum L., Carex pilosa Scop. and Stellaria holostea L. in forest ecosystems of the North-East of Ukraine. Vitality analysis was carried out according to Yu. A. Zlobin’s methodology. Vitality analysis procedure, classically, is carried out in three stages: 1) Selection of quantitative features that characterize the vital status of the individual plant; 2) Evaluation of vitality of individual plants that were included in the sample; 3) Integral assessment of the population’s vitality. Depending on the ratio in the population of plants of classes a, b and c, the population belongs to one of three vitality types: prosperous, equilibrium or depressive. Results: The obtained estimates of the vitality structure of populations of the clone-forming plants in the grass-shrub layer of forests of the North-East of Ukraine can be considered quite reliable, because they are based, in general, on a complete analysis of the morphological structure of about 13 thousand ramets of the studied species of plants. The statistical reliability of estimates of the population’s vitality structure is predominantly between 70 and 99% and only in some cases lower than 70%. As the clone grows older, its ramet’s vitality decreases and the clone degrades. New young clones, that start to form on the basis of genets, replace old ones. Such ramets have increased vitality, greater stress and competitive resistance. Due to the mechanisms of clone substitution in the living cover, the dominance of nemoralis herbs persists for a long time. Conclusion: The vitality spectra of the populations of the studied species of plants vary widely: the quality index Q of the populations ranges from 0,00 to 0,50, that is, it covers full theoretically possible scale of the values of this coefficient, which indicates the sensitivity of the vitality structure of the populations to the ecological-coenotic conditions and determines high informative value of vitality analysis. Prosperous populations: two populations A. europaeum of the associations Quercetum (roboris) coryloso (avellanae) – convallariosum (majalis) and Quercetum (roboris) coryloso (avellanae) – convallariosum (majalis), two populations A. podagraria of the associations – Pinetum (sylvestris) vacciniosum (myrtilli) and Querceto (roboris) – Pinetum (sylvestris) convallarioso (majalis) – vacciniosum (myrtilli), one population S. holostea of the association Querceto (roboris) – Pinetum (sylvestris) vacciniosum (myrtilli) and one population C. pilosa of the association Querceto (roboris) – Pinetum (sylvestris) vaccinioso (myrtilli) – convallariosum (majalis).


2002 ◽  
Vol 29 (4) ◽  
pp. 436-459 ◽  
Author(s):  
Robert S. Steneck ◽  
Michael H. Graham ◽  
Bruce J. Bourque ◽  
Debbie Corbett ◽  
Jon M. Erlandson ◽  
...  

Kelp forests are phyletically diverse, structurally complex and highly productive components of coldwater rocky marine coastlines. This paper reviews the conditions in which kelp forests develop globally and where, why and at what rate they become deforested. The ecology and long archaeological history of kelp forests are examined through case studies from southern California, the Aleutian Islands and the western North Atlantic, well-studied locations that represent the widest possible range in kelp forest biodiversity. Global distribution of kelp forests is physiologically constrained by light at high latitudes and by nutrients, warm temperatures and other macrophytes at low latitudes. Within mid-latitude belts (roughly 40–60° latitude in both hemispheres) well-developed kelp forests are most threatened by herbivory, usually from sea urchins. Overfishing and extirpation of highly valued vertebrate apex predators often triggered herbivore population increases, leading to widespread kelp deforestation. Such deforestations have the most profound and lasting impacts on species-depauperate systems, such as those in Alaska and the western North Atlantic. Globally urchin-induced deforestation has been increasing over the past 2–3 decades. Continued fishing down of coastal food webs has resulted in shifting harvesting targets from apex predators to their invertebrate prey, including kelp-grazing herbivores. The recent global expansion of sea urchin harvesting has led to the widespread extirpation of this herbivore, and kelp forests have returned in some locations but, for the first time, these forests are devoid of vertebrate apex predators. In the western North Atlantic, large predatory crabs have recently filled this void and they have become the new apex predator in this system. Similar shifts from fish- to crab-dominance may have occurred in coastal zones of the United Kingdom and Japan, where large predatory finfish were extirpated long ago. Three North American case studies of kelp forests were examined to determine their long history with humans and project the status of future kelp forests to the year 2025. Fishing impacts on kelp forest systems have been both profound and much longer in duration than previously thought. Archaeological data suggest that coastal peoples exploited kelp forest organisms for thousands of years, occasionally resulting in localized losses of apex predators, outbreaks of sea urchin populations and probably small-scale deforestation. Over the past two centuries, commercial exploitation for export led to the extirpation of sea urchin predators, such as the sea otter in the North Pacific and predatory fishes like the cod in the North Atlantic. The large-scale removal of predators for export markets increased sea urchin abundances and promoted the decline of kelp forests over vast areas. Despite southern California having one of the longest known associations with coastal kelp forests, widespread deforestation is rare. It is possible that functional redundancies among predators and herbivores make this most diverse system most stable. Such biodiverse kelp forests may also resist invasion from non-native species. In the species-depauperate western North Atlantic, introduced algal competitors carpet the benthos and threaten future kelp dominance. There, other non-native herbivores and predators have become established and dominant components of this system. Climate changes have had measurable impacts on kelp forest ecosystems and efforts to control the emission of greenhouse gasses should be a global priority. However, overfishing appears to be the greatest manageable threat to kelp forest ecosystems over the 2025 time horizon. Management should focus on minimizing fishing impacts and restoring populations of functionally important species in these systems.


2019 ◽  
Vol 92 ◽  
pp. 18008
Author(s):  
Víctor A. Rinaldi ◽  
Horacio V. Ibarra ◽  
Ricardo F. Viguera ◽  
Juan C. Harasimiuk

Seismic refraction technique is an increasingly useful geophysical tool for geotechnical studies in civil engineering work including the mapping of different soil formation of subsoil and detection of the bed rock. Additionally, wave velocity is a key parameter which correlates directly with significant geotechnical parameters of soils and rocks. Today, the evolution of the measurement technique in the field and the data processing allows to obtain tomographic images which increases its potential for applications to evaluate structuration of rock mass. This work describes the basic principles of seismic tomography and a case history of an application in civil works used to detect hidden faults in the sedimentary Gatun formation at the north of Panama. The correlation between the seismic profile and geologic profile obtained from boreholes showed very good agreement. Subsequent directed boreholes performed at the site confirmed the position and nature of the faults detected.


2020 ◽  
Author(s):  
Nikita Mergelov ◽  
Dmitry Petrov ◽  
Andrey Dolgikh ◽  
Elya Zazovskaya

<p>Soils and sediments serve as complementary sources of detailed information on paleofires in various ecosystems. Despite the abundance of charcoal material entrapped in soils they remain relatively less studied pyrogenic archives in comparison to the sedimentary paleofire records (e.g. lacustrine and peat deposits), and that is especially the case for the most territory of Russia. We report here on the numerous soil archives of the Holocene forest fires at the Kola Peninsula (66.347°N, 37.948°E) and the north of Arkhangelsk region (64.747°N, 43.387°E) in Russia. Series of buried Podzols (up to ten successive profiles) separated by the distinct charcoal layers were revealed in specific geomorphological traps like the thermokarst depressions inherited from the early stages of moraine sediments formation (Kola Peninsula), as well as in active and paleokarst sinkholes in carbonate and sulfate rocks (Arkhangelsk region). The maximum temporal depth of archives was estimated as 10261±40 cal yr BP for the key site in Arkhangelsk region, with up to 12 major pyrogenic events recorded at the local scale. Soil formation at the inter-pyrogenic stages maintained a uniform direction for at least 10 thousand years and profiles of Podzols were regularly replicated at all the key sites. We employ here a combination of soil morphological hierarchical analysis, study of geomorphological processes leading to the burial of pyrogenic carbon, 14C dating of charcoal and TOC derived from the soil organic matter, carbon and nitrogen isotope ratio mass spectrometry and anthracomass concentrations analysis to extract a set of paleoenvironmental information from these soil archives. The study of complementary pyrogenic archives in the three-component system of the karst landscape (including bottom and slopes of the funnels, as well as the flat elevated areas between them) helped to mitigate overestimation or underestimation of the anthracomass concentration and allowed to acquire a detailed dataset on paleopyrogenic events at the local scale. This study is supported by the Russian Foundation for Basic Research, Project No. 19-29-05238.</p>


2016 ◽  
Vol 11 (3) ◽  
pp. 36-40
Author(s):  
Сабиров ◽  
Ayrat Sabirov

The impact of productive activity of human on the ecological balance of nature. Ecological functions of soils of forest biogeocenoses. Regional features of the ecosystems functioning, soil formation factors. Organization of the soil cover state monitoring. Environmental monitoring of forest soils. Objectives of soil monitoring of forest ecosystems. Collection of the available information on forest ecosystems. Choice of monitoring objects. Soil and environmental hospitals. Fixed trial areas. Long-term and seasonal observations of soil properties. Temporary trial areas. Soil monitoring on the route courses. The use of satellite imagery in the environmental assessment of erosive landscapes. Controlled soil indicators. Research methods of soil properties and composition of pollutants. Processing of experimental data using information technology. Mathematical models of the spread of pollutants, the interrelation between soil indicators (in the soil), between soil properties and indicators of the characteristic of forest, the evolution of forest soil. Small-scale and medium-scale regional maps of land erosion, soil contamination by chemicals. Large-scale maps of physical degradation of soils, the content of macronutrients and micronutrients, acidity, humus condition of soils. Maps are accompanied by an explanatory note (soil sketch). Maximum permissible amount of the chemicals (maximum allowable concentrations) polluting the soil. Maximum permissible loading on forest soils under anthropogenic impact. Rational use and protection of forest ecosystems.


ÈKOBIOTEH ◽  
2020 ◽  
Vol 3 (4) ◽  
pp. 609-613
Author(s):  
B.I. Kochurov ◽  
◽  
N.A. Marunich ◽  

The article defines and calculates the geoenergetics of modern natural and anthropogenic forest ecosystems and landscapes. The geoenergetic approach and the developed technique were used for a detailed description and analysis of energy flows of the forest-steppe landscape of Pridnestrovien. On the example of the ecological network of oak tracts in the north of Pridnestrovien, the emergence of the forest is quantified, taking into account the spatial location. The forecast is made, taking into account the scenarios of economic development, quantitative changes in the emergence of forest ecosystems over time. Applying the geoenergetic matrix, the characteristic is given to the qualitative parameters of the forest-steppe landscape, affecting the formation of stability and self-organization of the natural system.


2015 ◽  
Vol 26 (3-4) ◽  
pp. 14-20
Author(s):  
I. N. Kovalenko

The species composition of herb and shrub layer of the major forest ecosystems of the north-eastern Ukraine has been analyzed at the level of vegetation classes, and individual ecological optimum of the main species of herbs and shrubs has been determined in order to predict the dynamics of their populations in the region. Literature data and results of our own studies for the period of 2000–2010 have shown that in accordance with the ecofloristic classification in the region, 6 classes of forest vegetation can be distinguished, such as: Querceto-Fagetea Br.-Bl. (1937), Vaccinio-Piceetea Br.-Bl. (1939), Pulsatillo-Pinetea sylvestris Oberdorfer (1992), Quercetea robori-petreae Br.-Bl. et. Tx. (1963), Salicetea purpureae Moor (1958), Alnetea glutinosae Br. Bl. ex Tx. (1943). The analysis of the general monographs on ecofloristic classification made in the north-eastern Ukraine (Klika, 1955; Matuszkiewicz, 2001; Shelyah-Sosonko, 2002; Grygora, 2005; Solomakha, 2008; Goncharenko, 2009, 2010; Rogova et al., 2005, etc.), provided an opportunity to review the composition of the characteristic species for the six classes of vegetation, registered in the region. Thereby, species, that hardly ever occur in the region or are very rare, have been excluded from the list of characteristic species. Plant species, peculiar to forest communities of the north-eastern Ukraine, have been added. Woody plants and shrubs have been excluded from the analysis. For each species of the three central classes its individual ecological optimum has been estimated considering six factors: 1 – light availability, 2 – temperature, 3 – continentality, 4 – soil moisture, 5 – soil acidity, 6 – soil fertility. The point scale of Ellenberg (Ellenberg, 1952, 1996) with 12 points for soil moisture and 9 points for other environmental regimes has been taken as a basis. Due to the fact that the scale of Ellenberg fails to include all these species, and has a lot of gaps in the assessment of individual regimes, it has been supplemented by the point scale of Landolt (Landolt, 1977), in which the number of species is greater and the assessment of their optimum is more complete. Considering that that in the scale of Landolt all environmental factors are divided into 5 points, transformation of points into 12- or 9-integrated assessment of environmental regimes has been made. The indicated pattern of wide ecological amplitude in characteristic species of higher syntaxonomic units in forest vegetation is useful adaptive trait from the phytocoenogenesis point of view. If there is any change in the general soil-climatic conditions, forest phytocoenoses retain their integrity due to the change in their great number and even the floristic composition in the lower tiers. Grouping of classes Querceto-Fagetea Br.-Bl. (1937), Vaccinio-Piceetea Br.-Bl. (1939) and Pulsatillo-Pinetea Sylvestris Oberdorfer (1992) play the leading role in the formation of forest ecosystems in the north- eastern Ukraine. Plant species, peculiar to these classes and being part of herb and shrub layer, provide wide ecological amplitudes, covering at least 3–5-point scales of the main environmental factors. Global warming may result in significant changes in the composition and structure of plant populations that form herb and shrub layer of forest phytocenoses of vegetation classes, peculiar to the north-eastern Ukraine.


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