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	<title>№3 2023 &#8211; ВОПРОСЫ ЛЕСНОЙ НАУКИ/FOREST SCIENCE ISSUES</title>
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		<title>COMPARATIVE ASSESSMENT OF THE DECOMPOSITION RATE OF PLANT LITTERFALL IN SPRUCE AND PINE FORESTS AT THE NORTHERN DISTRIBUTION LIMIT</title>
		<link>https://jfsi.ru/en/6-3-2023-ivanova_et_al/</link>
		
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		<pubDate>Thu, 18 Apr 2024 11:27:39 +0000</pubDate>
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					<description><![CDATA[E. A. Ivanova1, 2, M. A. Danilova2, V. E. Smirnov2, V. V. Ershov1   1 Institute of North Industrial Ecology Problems KSC RAS Akademgorodok st. 14a, Apatity, Murmansk region, 184209, Russia   2 Center&#46;&#46;&#46;]]></description>
										<content:encoded><![CDATA[<p><a style="color: #000000;" href="http://jfsi.ru/wp-content/uploads/2024/04/6-3-2023-Ivanova_et_al.pdf"><img loading="lazy" class="size-full wp-image-1122 alignright" src="http://jfsi.ru/wp-content/uploads/2018/10/pdf.png" alt="" width="32" height="32" /></a></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>E. A. Ivanova<sup>1, 2</sup>, M. A. Danilova<sup>2</sup>, V. E. Smirnov<sup>2</sup>, V. V. Ershov<sup>1</sup></strong></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong> </strong></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em><sup>1</sup></em> <em>Institute of North Industrial Ecology Problems KSC RAS</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Akademgorodok st. 14a, Apatity, Murmansk region, 184209, Russia</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><sup>2</sup> <em>Center for Forest Ecology and Productivity of the Russian Academy of Sciences</em>,</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Profsoyuznaya st. 84/32 bldg. 14, Moscow, 117997, </em><em>Russia</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong><sup>*</sup></strong>E-mail: <a href="mailto:ea.ivanova@ksc.ru">ea.ivanova@ksc.ru</a></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Received: 16.08.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Revised: 19.09.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Accepted: 20.09.2023</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">A comparative assessment of the processes of initial stages of decomposition of plant residues (pine needles, spruce needles, leaves of boreal shrubs, moss thalli) in lichen-shrub pine forests and shrub-green-moss spruce forests formed under natural conditions at the northern limit of distribution was carried out. The characteristics of the litter initial composition, the rate of decomposition and changes in the chemical composition of plant residues in the process of destruction caused by the forest type were studied. The higher initial content of C<sub>org</sub> in the plant tissues of pine forest is associated with favorable lighting conditions under the forest canopy, while the high content of Mn in the tissues of ground cover plants in spruce forests is due to the direct influence of spruce needle litter rich in this nutrient. The results of the study clearly demonstrated that the forest type has a significant impact both on the initial quality of the litterfall of the same plant species and on the rate of decomposition: in the spruce forest spruce needles and lingonberry leaves with a higher content of nutrients (Mg, Mn, P) and narrow ratios of elements (C:N, C:P) were characterized by more active decomposition processes. However, green moss litter, despite its high quality in spruce forests, decomposed more actively in pine forests, which may be due to a large amount of precipitation in pine forests. Thus, differences in the rate of decomposition of plant residues are influenced by a combination of the plant material quality, temperature conditions and precipitation amount associated with the forest type.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>Key words:</strong> <em>forest type, decomposition of litter, plant residues, quality of litter</em></span></p>
<p>&nbsp;</p>
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<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
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		<title>QUALITY OF TREE LITTER AS AN INFORMATIVE INDICATOR  OF FUNCTIONAL CLASSIFICATION OF FORESTS</title>
		<link>https://jfsi.ru/en/6-3-2023-basova_et_al/</link>
		
		<dc:creator><![CDATA[lena]]></dc:creator>
		<pubDate>Tue, 02 Apr 2024 12:16:36 +0000</pubDate>
				<category><![CDATA[№3 2023]]></category>
		<guid isPermaLink="false">https://jfsi.ru/?p=6260</guid>

					<description><![CDATA[Original Russian Text © 2022 E. V. Basova, N. V. Lukina, A. I. Kuznetsova, A. V. Gornov, N. E. Shevchenko, E. V. Tikhonova, A. P. Geraskina, T. Yu. Braslavskaya, D. N. Tebenkova, D. L.&#46;&#46;&#46;]]></description>
										<content:encoded><![CDATA[<p><a style="color: #000000;" href="http://jfsi.ru/wp-content/uploads/2024/04/6-3-2023-Basova_et_al.pdf"><img loading="lazy" class="size-full wp-image-1122 alignright" src="http://jfsi.ru/wp-content/uploads/2018/10/pdf.png" alt="" width="32" height="32" /></a></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif; font-size: 10pt;">Original Russian Text © 2022 E. V. Basova, N. V. Lukina, A. I. Kuznetsova, A. V. Gornov, N. E. Shevchenko, E. V. Tikhonova, A. P. Geraskina, T. Yu. Braslavskaya, D. N. Tebenkova, D. L. Lugovaya published in Forest Science Issues <a href="https://jfsi.ru/5-3-2022-basova_et_al/">Vol. 5, No 3, Article 113</a>.</span></p>
<p style="text-align: center;"><strong><span style="font-family: 'times new roman', times, serif;">E. </span></strong><strong style="font-family: 'times new roman', times, serif;">V. Basova, N. V. Lukina, A. I. Kuznetsova, A. V. Gornov, N. E. Shevchenko, E. V. Tikhonova, A. P. Geraskina, T. Yu. Braslavskaya, D. N. Tebenkova, D. L. Lugovaya</strong></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><sup> </sup></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Center for Forest Ecology and Productivity of the RAS</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Profsoyuznaya St. 84/32 bldg. 14, Moscow, 117997, Russia</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">E-mail: lenabasova7@gmail.com</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Received: 01.09.2022</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Revised: 17.10.2022</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Accepted: 18.11.2022</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Relevance and goals.</em></strong> In the context of global climate change, the climate-regulating function of forests deserves special attention. There is still no functional classification of forests according to the effectiveness of carbon accumulation function. The aim of this paper is to discuss an approach to such classification based on the assessment of tree litter quality.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Objects and methods. </em></strong>To test the approach to the identification of functional types of forests based on the quality of tree litter, taking into account the location in the geochemically linked landscape and the mechanical composition of soil-forming rocks, data on soils and vegetation obtained at 23 testing sites in the subzone of coniferous-broadleaf forests of the European part of Russia on the territory of Bryansk Polesie and Moskvoretsko-Okskaya plain were used. For indirect (Landolt’s ecological scales using the SpeDiv program) assessment of differences in the soil richness in forests belonging to different functional types, the species composition at 160 geobotanical plots in forest sites in the Moscow, Bryansk, Smolensk, Kostroma Regions, Krasnodar Territory, and the Republic of Adygea (Northwestern Caucasus) were analyzed.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Results.</em></strong> Examples of functional forest types for coniferous — broad-leaved forests of the European part of Russia are given. The differences in soil carbon stock between forests belonging to different functional types were found, and a preliminary assessment of the influence of the location in the geochemically linked landscape and the mechanical composition of soils on the accumulation of carbon in soils in the same functional forest types is given.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Conclusion. </em></strong>Based on the quality of the tree litter, 15 functional forest types were identified, which are confirmed by examples of forests in the subzone of coniferous-broad-leaved forests of the European part of Russia and in the belt of coniferous-broad-leaved forests of the Northwestern Caucasus. The validity of identification of functional forest types for the efficiency of carbon accumulation in soils based on the quality of tree litter, taking into account the influence of “external factors” (the location of forests in the geochemically linked landscape and the mechanical composition of soil-forming rocks), was confirmed by data obtained at 23 sites. Using this approach allowed us to reveal differences in the soil carbon stock and related characteristics of soil fertility estimated on an ecological scale between the functional forest types, identified on the base of tree litter in the mixed, coniferous-broad-leaved forests at the same location in the geochemically linked landscape. Differences in soil carbon stocks in forest ecosystems of the same functional forest types formed on clay loam and sandy loam soil-forming rocks were also revealed. Differences in soil carbon stocks in forests belonging to the same functional type, but formed at different locations in the geochemically linked landscape, have been confirmed: soil carbon stocks were higher in forests at the transit landscapes compared to those in autonomous ones.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>Keywords:</strong><em> coniferous-broad-leaved forests, forest functional classification, functional types of forests, carbon stocks</em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Currently, attention is being increasingly focused on the forest ecosystem functions and services. Forests perform ecosystem functions/services of all four categories: regulating, providing supporting and cultural (Millennium Ecosystem Assestment, 2005). In this regard, it becomes important to develop new approaches to the functional classification of forest ecosystems based on the effectiveness of their various functions (Lukina et al., 2021).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In the context of global climate change associated with an increase in greenhouse gas emissions into the atmosphere, the climate-regulating function of forests deserves special attention. Forests can absorb greenhouse gases and store carbon in both biomass and soil pools. A number of studies have shown that the effectiveness of forests in performing the function of carbon accumulation, in particular carbon accumulation in the soil, can be influenced by various natural and anthropogenic factors (Mazhitova et al., 2003; Chestnyh et al., 2004; Mashika, 2005; Shchepashchenko et al., 2013; Bobkova et al., 2014; Baeva et al., 2017; Telesnina et al., 2017; Bakhmet, 2018; Dymov, 2018; Demakov et al., 2018; Chestnyh et al., 2020; Ryzhova et al., 2020; Akkumuljacija &#8230;, 2018; Lukina et al., 2020; Kuznetsova et al., 2021). Internal and external factors can be distinguished among natural factors. Internal factors include vegetation, soil microorganisms and animals, and other biota; external factors include abiotic factors such as soil-forming rocks, climate, and relief. Among anthropogenic factors, the regime of forest management and land use in general, the pollution-induced factor, and fires are important.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Vegetation as the main source of organic matter entering the soil determines the level of accumulation of soil organic matter. The dynamics of soil carbon pools caused by vegetation are influenced by the quantity and quality of tree species litter, both individually and jointly (Castellano et al., 2015; Kuznetsova et al., 2021).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The quality of the litter depends on the species composition and age structures of forest trees, as well as the stages of tree plant ontogenetic development, and is determined by the ratio of nutrients (nitrogen, phosphorus, potassium, calcium, magnesium, etc.) and secondary metabolites (polyphenols, lignin, etc.) in the litter; an important indicator is the C/N ratio (Berg, 2020). The quality of the litter regulates the rate of decomposition of plant residues — the main source of nutrients for saprophages (Krishna, 2017). According to the quality of the litter, functional types of plants can be distinguished (Cornelissen et al., 2007).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The functional classification of forest ecosystems according to the effectiveness of their carbon cycle regulation can be based on the quality of plant litter (Lukina et al., 2021). In coniferous-broad-leaved forests, a significant proportion of plant litter, which decisively affects the accumulation of soil carbon, is formed by tree plants. Low-quality litter, that is, with a low content of bases, nitrogen, high acidity, high content of lignin, and other secondary metabolites, as well as a wide C/N ratio, is characteristic of coniferous trees. Earlier, when comparing coniferous tree species with each other, it was noted that the litter in pine forests differed in a much wider C/N ratio than in spruce forests (Lukina et al., 2020). A number of studies of European (Lovett et al., 2004; Reich et al., 2005; Oostra et al., 2006) and North American (Finzi et al., 1998; Neirynck et al., 2000; Dijkstra, Fitzhugh, 2003; Hagen-Thorn et al., 2004) scientists showed differences in the litter quality , C stocks and C/N ratio between some broad-leaved forests forming by different tree species (<em>Fraxinus exelsior, Fagus orientalis</em> and the genera <em>Acer</em> and <em>Quercus)</em>: ash and maple are grouped into plants with high litter quality, while oak and beech are characterized by a relatively low N content in the litter, a wider C/N ratio, low decomposition rate<em>.</em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The aim of this paper is to discuss the results of the implementation of an approach to the functional classification of coniferous-broad-leaved forests based on the relationships between the quality of tree litter and carbon stocks in soils.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">At this stage of the work, we raised the scientific tasks as follows:</span></p>
<ul style="text-align: justify;">
<li><span style="font-family: 'times new roman', times, serif;">to determine which functional types of forests can be identified on the basis of tree litter quality in coniferous-broad-leaved forests of the European part of Russia;</span></li>
<li><span style="font-family: 'times new roman', times, serif;">to find out whether the functional types of forests identified on the basis of the proposed approach differ in terms of soil carbon stocks;</span></li>
<li><span style="font-family: 'times new roman', times, serif;">to demonstrate the influence of location in the geochemically linked landscape of forest ecosystems belonging to the same functional forest types (FFT) and of soil forming rocks on carbon accumulation in soils.</span></li>
</ul>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>MATERIALS AND METHODS</strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The analysis includes data on geobotanical descriptions of forest communities and soil characteristics of 23 sites representing forests in autonomous and transit locations in landscapes on soil-forming rocks of different mechanical compositions (sandy loam, clay loam) in the subzone of coniferous-broad-leaves forests of the European part of Russia. On loamy soil-forming rocks of the Moskvoretsko-Okskaya plain (MO), oak-spruce forests with lime and boreal-nemoral herbs were studied. On the sandy Bryansk forest area (BFA), polydominant broad-leaved forests with spruce and nemoral herbs, pine forests with dwarf shrubs and green mosses, and aspen-birch nemoral forests were studied.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Geobotanical descriptions were performed on 20×20 m permanent sample plots according to the standard methodology (Akkumuljacija &#8230;, 2018). Samples from the soil mineral horizons using a soil drill below and between the trees, and soil samples were taken up deeper, to a depth of 100 cm between the trees manually, using a shovel. Litter samples were taken at sites 0.25×0.25 m. All sample plots were established in triplicate. In the laboratory, samples from mineral horizons were dried and sieved through a 2 mm sieve, chemical analysis was carried out in samples of a fraction less than 2 mm. Litter samples were dried and weighed to determine the stock (Akkumuljacija &#8230;, 2018). The carbon and nitrogen content in all samples was determined using a CHN analyzer (EA 1110 (CHNS-O)).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">An indirect assessment of the soil fertility in forests belonging to different FFTs was carried out on the Landolt ecological scale using the SpeDiv program, the species compositions of 160 geobotanical plots of forest vegetation in the Moscow, Bryansk, Smolensk, Kostroma Regions, Krasnodar Territory, and the Republic of Adygea (Northwestern Caucasus) were analyzed.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The inventory of forest communities within the identofied FFTs was based on the materials of Forest cenofond within European Russia (Cenofond …, 2010), for the Northwestern Caucasus — based on the materials of the original database of geobotanical descriptions of forest communities of the Northwestern Caucasus (by Shevchenko) and published data (Francuzov, 2006).</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>RESULTS AND DISCUSSION</strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Based on the quality of the litter, the plants of the tree layer were divided into 4 main functional groups:</span></p>
<ul style="text-align: justify;">
<li><span style="font-family: 'times new roman', times, serif;">deciduous trees with fast decomposing litter (these include species of the genera <em>Acer, Fraxinus, Tilia, Ulmus, Betula, Alnus</em>);</span></li>
<li><span style="font-family: 'times new roman', times, serif;">deciduous trees with slow-decomposing litter (<em>Populus, Quercus, Fagus</em>);</span></li>
<li><span style="font-family: 'times new roman', times, serif;">dark coniferous trees (<em>Picea /Abies</em>);</span></li>
<li><span style="font-family: 'times new roman', times, serif;">light coniferous (<em>Pinus</em>).</span></li>
</ul>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Based on data from the Forest cenofond within European Russia (Cenofond …, 2010), up to 160 different taxonomic forest types can be identified in the subzone of coniferous-broad-leaved forests of European Russia. The tree layer of these forests can be monodominant, particularly at the early stages of natural succession or on plantations, but more often in the tree layer of forests of the subtaiga subzone, various species belonging to different functional groups in terms of the quality of litter are combined. In this regard, all the variety of forest taxonomical types found in the subzone of coniferous-broad-leaved forests of the European part of Russia can be attributed to 15 main functional types (Table 1), identified on the basis of the quality of plant litter affecting the level of carbon accumulation in the soil (Akkumuljacija &#8230;, 2018; Lukina et al., 2021; Kuznetsova, 2022). In the coniferous-broad-leaved forests of the Northwestern Caucasus, secondary after-logging communities with significant contribution of small-leaved tree species (hornbeam, alder, aspen, etc.) are developed over large areas. Old-age intact forests are formed, as a rule, by spruce, oak, beech, and fir (Akkumuljacija &#8230;, 2018). Based on the quality of the tree litter in the Northwestern Caucasus, 14 functional types of forest were identified.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>Table 1.</strong> Functional forest types (FFTs) and their corresponding groups of forest types in the subzone of coniferous-broad-leaved forests of the European part of Russia and in the belt of coniferous-broad-leaved forests of the Northwestern Caucasus</span></p>
<div style="overflow-x: auto;">
<table style="border: 1px #f1f1f1 solid; background-color: #ffffff;" width="663">
<tbody>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;"><strong>FFFT</strong></span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;"><strong>Tree layer composition</strong></span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;"><strong>Groups of forest types in the plains of the European part of Russia (according to Cenofond …, 2010)</strong></span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;"><strong>Types of forest, Northwestern Caucasus</strong></span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA1</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Deciduous species with fast decomposing litter predominate*</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Birch forests small-herb boreal, nemoral, nitrophilic and mesotrophic-marsh, lime forests and gray alder forests nemoral and nitrophilic, black alder forests and ash forests nitrophilic</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Hornbeam forests fescue, mixed herbs, honeysuckle-mixed herbs; alder forests ferns-tall herb</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA2</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Deciduous species with slow-decomposing litter predominate</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Oak, aspen-oak nemoral and nitrophilic; aspen boreal nemoral, nemoral and nitrophilic</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Beech forests mountain fescue, oak-beech forests mixed herbs (bedstraw)</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA3</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous species predominate</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Spruce forests dwarf-shrub and small-herb green-moss, small-grass-boreal, boreal-nemoral and nemoral; fir-spruce forests boreal-nemoral</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Fir forests oxalis, mixed grass (bedstraw), mixed herbs-ferns, mixed herbs-mountain fescue, oxalis-small-grass;</span></p>
<p><span style="font-family: 'times new roman', times, serif;">spruce-fir forests oxalis-small-grass</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA4</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Light coniferous species predominate</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests green-moss-lichen, xerophytic-dwarf-shrub- and small-herb green-moss, small-herb-boreal and nemoral, haircap-moss-sphagnum</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Pine forests with rhododendron, cereal (reed grass)</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA5</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">** Dark coniferous and deciduous species with fast decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Spruce forests with lime and maple nemoral and boreal-nemoral, fir-spruce with lime boreal-nemoral, spruce with birch dwarf-shrub green-mossy, birch with spruce small-herb boreal and nemoral, lime with spruce nemoral and nitrophilic</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Fir-hornbeam forests with rhododendron,</span></p>
<p><span style="font-family: 'times new roman', times, serif;">fir-hornbeam forests with <em>Pachyphragma</em>;</span></p>
<p><span style="font-family: 'times new roman', times, serif;">hornbeam forests with fir, small-grass with raspberry</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA6</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous and deciduous with slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Oak-spruce and spruce-oak nemoral and small-herb boreal</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Beech-fir forests with <em>Pachyphragma</em>, mixed-herbs, dead cover; fir-beech forests oxalis-small-herbs</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA7</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Light coniferous and deciduous species with fast decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests with lime nemoral and boreal-nemoral, pine forests with birch nemoral and dwarf-shrub green-moss</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Hornbeam-pine forests rhododendron-fescue</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA8</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Light coniferous and deciduous species with slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests with oak xerophytic green-moss, boreal-nemoral; complex pine forests boreal-nemoral</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Beech-pine forests with rhododendron</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA9</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Deciduous species with slow- and fast-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Birch-aspen with lime, aspen with lime, elm-lime-oak, lime-oak, lime-oak with ash, oak-lime, aspen-lime nemoral; oak with black alder nitrophilic</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Hornbeam-beech forests mixed-herbs, mixed-herbs-blackberry;</span></p>
<p><span style="font-family: 'times new roman', times, serif;">hornbeam-aspen forests mixed-herbs; aspen-hornbeam forests mixed-herbs; oak-hornbeam forests fescue; aspen-hornbeam forests ferns-mixed-herbs, honeysuckle-small-grass, bedstraw; hornbeam forests with aspen, beech, and ash</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA10</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous and light coniferous species are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests with spruce xerophytic, dwarf-shrub and small-herb green-moss, haircap-moss sphagnum</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Pine forests with fir and spruce nemoral mixed-herb; pine forests with fir reed grass-mixed-herb</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA11</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous and deciduous species with fast- and slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Lime-oak with spruce, oak-lime with spruce, spruce forests with lime and oak nemoral; oak-spruce with maple boreal-nemoral</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Beech-fir-hornbeam forests honeysuckle-mixed-herbs</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA12</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous, light coniferous and deciduous species with fast decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests with spruce and birch dwarf-shrub green-moss, xeromesophilic- herbaceous, small-herb boreal</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Pine forests with spruce, fir, and birch reed grass</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA13</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Dark coniferous, light coniferous and deciduous species with slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine forests with aspen and spruce dwarf-shrub and green-moss, spruce forests with pine and oak (aspen) small-grass and green-moss</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Pine-aspen-fir forests reed grass; pine forests with spruce, fir and aspen legumes-mixed herbs; pine forests with fir and beech rhododendron-dead cover</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA14</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Light coniferous and deciduous species with fast- and slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Complex pine forests boreal-nemoral, pine forests with birch and aspen dwarf-shrub and green-moss</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Pine-beech-hornbeam forests blackberry</span></td>
</tr>
<tr>
<td width="47"><span style="font-family: 'times new roman', times, serif;">AA15</span></td>
<td width="172"><span style="font-family: 'times new roman', times, serif;">Light coniferous, dark coniferous and deciduous species with fast- and slow-decomposing litter are combined</span></td>
<td width="284"><span style="font-family: 'times new roman', times, serif;">Pine with spruce (with birch, lime, and oak) xeromesophilic-herbaceous, spruce with pine (with birch and aspen, oak) small-herb boreal</span></td>
<td width="161"><span style="font-family: 'times new roman', times, serif;">Not identified</span></td>
</tr>
</tbody>
</table>
</div>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">* Here and further — the share of the predominant species in the total tree layer — is more than 90%;</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">** In the tree layer, species can be combined in a fairly wide range of ratios for the cover (50/50%, 90/10%).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">As it is known, nitrogen and carbon are closely related in organic matter, and the ratios between them are tissue-specific and species-specific. The conjugacy of nitrogen and carbon content in the soil of European part of Russia was also confirmed earlier in a number of our works (Akkumuljacija &#8230;, 2018; Kuznetsova et al., 2021). Based on this, for an indirect assessment of the effectiveness of the function of carbon accumulation in soils by forests belonging to different FFTs, a characteristic of nitrogen richness in soil was used, obtained on the basis of an analysis of species composition on the Landolt scale of soil richness. The geobotanical descriptions of the mountain forests of the Northwestern Caucasus and lowland forests of European Russia, attributed to the same FFT, were analyzed (Fig. 1).</span></p>
<div id="attachment_6271" style="width: 1047px" class="wp-caption aligncenter"><img aria-describedby="caption-attachment-6271" loading="lazy" class="size-full wp-image-6271" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1.jpg" alt="Figure 1. The richness of the soil with nitrogen (Landolt indicator values). The x-axis signatures represent the functional types of the forest (see Table 1)." width="1037" height="705" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1.jpg 1037w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1-300x204.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1-1024x696.jpg 1024w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1-150x102.jpg 150w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок1-768x522.jpg 768w" sizes="(max-width: 1037px) 100vw, 1037px" /><p id="caption-attachment-6271" class="wp-caption-text"><span style="font-family: 'times new roman', times, serif;"><strong>Figure 1</strong>. The richness of the soil with nitrogen (Landolt indicator values). The x-axis signatures represent the functional types of the forest (see Table 1).</span></p></div>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Note: The histogram is based on the average values of soil richness points based on the analysis of 160 geobotanical descriptions (10 descriptions for each functional type).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In the Northwestern Caucasus, the values of soil richness were higher in all FFTs except for A4 (light coniferous forests). The A4 type has the lowest values of soil richness for both the Northwestern Caucasus and the plains of the European part; the difference in values between the two regions was also minimal for this type. Despite the fact that the values of soil richness in forest ecosystems belonging to the same FFT differ in the regions, which was explained by differences in climatic, soil, and orographic conditions, both in the Northwestern Caucasus and on the plains of the European part of Russia, there is a similar tendency for soil richness indicators to change from type to type, which confirms the key role of vegetation and the quality of plant litter in the accumulation of organic matter in the soil.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Direct soil measurements were performed for forests belonging to functional types A4 (pine forests), A9 (mixed type, in layer A, deciduous tree species with slow and rapidly decomposing litter are combined) formed on sandy loam soils in the Bryansk forest area and A11 (mixed forests: in the tree layer, dark coniferous and deciduous species with fast- and slow-decomposing litter), growing in the Bryansk forest area, as well as on loams on the Moskvoretsko-Okskaya plain. Figure 2 shows the contribution of species of different functional groups in the tree layer cover of these 3 FFTs.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>a</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6261" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-a.jpg" alt="" width="640" height="417" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-a.jpg 640w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-a-300x195.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-a-150x98.jpg 150w" sizes="(max-width: 640px) 100vw, 640px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>b</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6262" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-b.jpg" alt="" width="627" height="404" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-b.jpg 627w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-b-300x193.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-b-150x97.jpg 150w" sizes="(max-width: 627px) 100vw, 627px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>c</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6263" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-c.jpg" alt="" width="603" height="437" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-c.jpg 603w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-c-300x217.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-2-c-150x109.jpg 150w" sizes="(max-width: 603px) 100vw, 603px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif; font-size: 10pt;"><strong>Figure 2.</strong> The ratio of the cover of tree species of different functional groups (DRD — deciduous trees with rapidly decomposing litter, DSD — deciduous trees with slowly decomposing litter, DC — dark coniferous trees, LC — light coniferous trees) in layer A in forests of functional types A4 (<strong>a</strong>), A9 (<strong>b</strong>), and A11 (<strong>c</strong>). On X-axis for <strong>a, b</strong>: ordinal numbers of sites; for <strong>c</strong>: BFA (1–3) — sites in the Bryansk forest area, MO (1–2) — sites on the Moskvoretsko-Okskaya plain</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In forests of A4 type, 90% of the tree layer cover was composed by light coniferous species (in this case <em>Pinus sylvestris</em>), in forests of A9 type deciduous trees of different functional groups were combined in different proportions.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In A11 forests, the contribution in the tree layer of trees of dark coniferous species (DC), deciduous with rapidly (DRD) and slowly decomposing (DSD) litter was different.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Soil measurements in the forests of the Bryansk forests, forming in similar landscape location and climatic conditions on soil-forming rocks of similar composition, also revealed a difference in the soil carbon stocks between the forests belonging to different FFTs (Fig. 3, 4).</span></p>
<p><span style="font-family: 'times new roman', times, serif;"><strong>(a)</strong></span></p>
<p><img loading="lazy" class="aligncenter size-full wp-image-6264" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-a.jpg" alt="" width="516" height="422" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-a.jpg 516w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-a-300x245.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-a-150x123.jpg 150w" sizes="(max-width: 516px) 100vw, 516px" /></p>
<p><span style="font-family: 'times new roman', times, serif;"><strong>(b)<img loading="lazy" class="aligncenter size-full wp-image-6265" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-b.jpg" alt="" width="547" height="421" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-b.jpg 547w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-b-300x231.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-3-b-150x115.jpg 150w" sizes="(max-width: 547px) 100vw, 547px" /></strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif; font-size: 10pt;"><strong>Figure 3</strong>. Carbon stock in the forest litter (<strong>a</strong>) and the mineral layer of the soil (<strong>b</strong>) in forest ecosystems of functional types A9 and A4 in autonomous landscapes, t/ha. On X-axis: L, FH — litter subhorizons, 0–30 cm, 30–100 cm — soil layers (mineral part)</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>(a)<img loading="lazy" class="aligncenter size-full wp-image-6266" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-a.jpg" alt="" width="534" height="430" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-a.jpg 534w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-a-300x242.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-a-150x121.jpg 150w" sizes="(max-width: 534px) 100vw, 534px" /></strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"> </span><span style="font-family: 'times new roman', times, serif;">(<strong>b</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6267" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-b.jpg" alt="" width="524" height="406" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-b.jpg 524w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-b-300x232.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-4-b-150x116.jpg 150w" sizes="(max-width: 524px) 100vw, 524px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif; font-size: 10pt;"><strong>Figure 4</strong>. Carbon stock in the forest litter (<strong>a</strong>) and the mineral layer of the soil (<strong>b</strong>) in forest ecosystems of functional types A9 and A4 in transit landscapes, t/ha</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In autonomous landscapes, the carbon stock in litter of aspen-birch forests (FFT A9) and pine forests (FFT A4) demonstrated some differences (p = 0.05) for both the L and the FH litter subhorizons, in the mineral profile the differences were also found in the upper (0–30 cm) layer (p = 0.05) (Fig. 4 (b)): carbon stock in the litter of A4 pine forests was higher, in soil mineral horizons, on the contrary, carbon stock was higher in A9 (Fig. 3 (b)).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In transit landscapes, carbon stock demonstrated significant differences between the two FFTs only in the FH subhorizon (p = 0.008), whereas no significant differences were found in the mineral profile (Fig. 4).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The influence of the mechanical composition of soil-forming rocks and location of forest in the geochemically linked landscape on the function of carbon accumulation in the soil of forests belonging to the same FFT has also been assessed.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">When comparing the soil carbon stock in A9 forests at different landscape locations, no differences were found in carbon stock in mineral layers: the average values of carbon stock were 36.2 t/ha, 6.5 t/ha, and 23.0 t/ha in mineral layers 0–15, 15–30, and 30–100 cm of soil, correspondingly, in autonomous landscape. In transit landscape, soil carbon stock averaged 33.0 t/ha, 13.9 t/ha, and 24.4 t/ha in layers 0–15, 15–30, and 30–100 cm, correspondingly. Perhaps, the lack of statistically significant differences was due to insufficient number of samples.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The expected pronounced differences in soil carbon stock between forests at autonomous and transit landscapes were found in forests of A4 type (light coniferous). In this case, the Mann-Whitney U test has confirmed the reliability of differences between carbon stock in forests formed in different location of geochemically linked landscapes in the soil layer of 0–30 cm and 30–100 cm (p = 0.037): 20.3 t/ha and 14.2 t/ha in transit conditions, respectively, and 55.9 t/ha and 39.2 t/ha in autonomous conditions, respectively.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Carbon stock in soils of A11 functional forest type formed on soil-forming rocks of different mechanical composition in the Bryansk forest area and on the Moskvoretsko-Okskaya plain in similar, autonomous landscapes differ in the litter and mineral layer 0–15 cm (Fig. 5).</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>a</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6270" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5a.jpg" alt="" width="492" height="362" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5a.jpg 492w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5a-300x221.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5a-150x110.jpg 150w" sizes="(max-width: 492px) 100vw, 492px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>b</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6268" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-b.jpg" alt="" width="553" height="478" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-b.jpg 553w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-b-300x259.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-b-150x130.jpg 150w" sizes="(max-width: 553px) 100vw, 553px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">(<strong>c</strong>)<img loading="lazy" class="aligncenter size-full wp-image-6269" src="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-c.jpg" alt="" width="619" height="456" srcset="https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-c.jpg 619w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-c-300x221.jpg 300w, https://jfsi.ru/wp-content/uploads/2024/04/Рисунок-5-c-150x111.jpg 150w" sizes="(max-width: 619px) 100vw, 619px" /></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif; font-size: 10pt;"><strong>Figure 5</strong>. Carbon stock in the forest litter (<strong>a</strong>) and mineral layers of the soil (<strong>b</strong>, <strong>c</strong>) in FFT A11, mt/ha. On the x-axis: L, FH — subhorizons of the litter; 0–15 cm, 15–30 cm, 30–50 cm — soil layers (mineral part)</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The carbon stock in the litter (subhorizon FH) was higher in forests on sandy loam soils, whereas in the mineral horizons of soils (in layers of 0–15 cm, 15–30 cm, and 30–50 cm) soil carbon stock was higher in forests on loam. The maximum differences (almost 2 times) were found in the soil layer from 30 to 50 cm, and visible differences were also revealed in the upper part of the mineral layer (0-15 cm).</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>CONCLUSION</strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The quality of plant litter is an important factor regulating the accumulation of soil organic matter and the dynamics of soil carbon pools, and can be an informative indicator for classifying forests according to the effectiveness of their carbon cycle regulation function.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In coniferous-broad-leaved forests, a significant proportion of plant litter is formed by tree plants. The quality of tree litter affects the accumulation of soil carbon in the forests of this subzone. Based on the litter quality, the plants of the tree layer can be divided into 4 main functional groups: deciduous trees with rapidly decomposing litter, deciduous trees with slowly decomposing litter, dark coniferous and light coniferous trees.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">In the subzone of coniferous-broad-leaved forests, both monodominant and polydominant forest communities are common, where species of different functional groups are combined in the tree layer. Taking into account the various combinations of such species in the forest stands, 15 FFTs have been preliminarily identified. All 15 FFTs were found on the plains of the European part of Russia; almost all similar FFTs were found in the belt of coniferous-broad-leaved forests of the Northwestern Caucasus. This paper only demonstrates the differences in soil carbon stock using direct measurements in forests belonging to different FFTs and also using an indirect assessment of soil richness based on an ecological scale.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The influence of soil-forming rocks on the accumulation of carbon in the soil was confirmed: a difference in soil carbon stock in forests of the same FFT on clay loam and sandy loam soils was found. Differences in soil carbon stock in forests formed at different  location in the geochemically linked landscape were also confirmed: in forests of functional type A4 (with a predominance of species of light coniferous trees) of transit landscapes, soil carbon stock was higher than that of  autonomous landscape, but in forests of functional type A9 (with a combination of species of deciduous trees with slow and rapidly decomposing litter), the influence of the position in the geochemically linked landscape has not been revealed.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">To verify the relationships between the FFT and carbon stocks in soils found in this study taking into account the mechanical composition of soil-forming rocks and forest location in the geochemically linked landscape, it is necessary to continue with using more number of testing forest sites.</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>FINANCING</strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The research was carried out as a part of the most important innovative project of national importance “Development of a system for ground-based and remote monitoring of carbon pools and greenhouse gas fluxes in the territory of the Russian Federation, ensuring the creation of recording data systems on the fluxes of climate-active substances and the carbon budget in forests and other terrestrial ecological systems” (Registration number: 123030300031-6).</span></p>
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<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>Reviewer:</strong> Doctor of Biological Sciences E. I. G</span></p>
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		<title>WOODY PLANTS GROWTH ON ABANDONED AGRICULTURAL LANDS: SCALE, CAUSES OF ABANDONMENT, WAYS OF USE. A REVIEW</title>
		<link>https://jfsi.ru/en/6-3-2023-gichan_tebenkova/</link>
		
		<dc:creator><![CDATA[lena]]></dc:creator>
		<pubDate>Tue, 19 Mar 2024 13:54:15 +0000</pubDate>
				<category><![CDATA[№3 2023]]></category>
		<guid isPermaLink="false">https://jfsi.ru/?p=6216</guid>

					<description><![CDATA[D. V. Gichan*, D. N. Tebenkova Center for Forest Ecology and Productivity of the RAS Profsoyuznaya st. 84/32 bldg. 14, Moscow, 117997, Russia   *E-mail: DmitriiGichan@yandex.ru Received: 11.08.2023 Revised: 15.09.2023 Accepted: 18.09.2023 The article&#46;&#46;&#46;]]></description>
										<content:encoded><![CDATA[<p><a style="color: #000000;" href="http://jfsi.ru/wp-content/uploads/2024/03/6-3-2023-Gichan_Tebenkova.pdf"><img loading="lazy" class="size-full wp-image-1122 alignright" src="http://jfsi.ru/wp-content/uploads/2018/10/pdf.png" alt="" width="32" height="32" /></a></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>D. V. Gichan<sup>*</sup>, D. N. Tebenkova</strong></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Center for Forest Ecology and Productivity of the RAS</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Profsoyuznaya st. 84/32 bldg. 14, Moscow, 117997, Russia</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong><sup>*</sup></strong>E-mail: DmitriiGichan@yandex.ru</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Received: 11.08.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Revised: 15.09.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Accepted: 18.09.2023</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The article presents an overview of Russian and foreign papers considering quantitative assessment of woody plants growth on abandoned agricultural lands and possible ways to utilise them. Particular attention is paid to analysing the causes for the abandonment of those lands and the legislation problems that limit the provision of such areas for commercial forest growing in Russia. According to various estimates, the area of abandoned agricultural land in the world varies from 150 to 472 million hectares, with 33 to 100 million hectares being in Russia. At the same time, there is a trend towards an increase in such lands’ area. The rate at which the area of abandoned agricultural lands is increasing is about 1% year<sup>-1 </sup>on average. It may vary over time and depend on the region. The main groups of factors contributing to the agricultural lands falling into disuse are social, economic, environmental, landscape and historical. The most promising is the involvement of such lands in climate-smart forestry activities, especially for agroforestry. This is due to the multiplier effect from on the one hand, obtaining forest goods, including bioenergy, and on the other hand services, including use in crop or livestock farming activities. Currently in Russia there is no legislative framework permitting commercial forest growing on agricultural lands, with the exception of planting shelterbelts and other protective structures, despite the active position of organizations and government structures involved, so its development proves to be a necessity.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong>Key words:</strong> <em>agricultural land, woody plants growth, woody plants growth factors, climate-smart forestry</em></span></p>
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		<title>METHODS AND OPEN SOURCE MACHINE LEARNING GIS TOOLS  FOR FOREST TRANSPORT MODELING</title>
		<link>https://jfsi.ru/en/6-3-2023-podolskaia/</link>
		
		<dc:creator><![CDATA[lena]]></dc:creator>
		<pubDate>Wed, 17 Jan 2024 06:29:48 +0000</pubDate>
				<category><![CDATA[№3 2023]]></category>
		<guid isPermaLink="false">https://jfsi.ru/?p=6166</guid>

					<description><![CDATA[ E. S. Podolskaia Center for Forest Ecology and Productivity of the Russian Academy of Sciences Profsoyuznaya st. 84/32 bldg. 14, Moscow, 117997, Russian Federation   E-mail: podols_kate@mail.ru Received: 05.06.2023 Revised: 22.06.2023 Accepted: 23.06.2023  &#46;&#46;&#46;]]></description>
										<content:encoded><![CDATA[<p><a style="color: #000000;" href="http://jfsi.ru/wp-content/uploads/2024/01/6-3-2023-Podolskaia.pdf"><img loading="lazy" class="size-full wp-image-1122 alignright" src="http://jfsi.ru/wp-content/uploads/2018/10/pdf.png" alt="" width="32" height="32" /></a></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong> E. </strong></span><strong style="font-family: 'times new roman', times, serif;">S. Podolskaia</strong></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Center for Forest Ecology and Productivity of the Russian Academy of Sciences </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Profsoyuznaya st. 84/32 bldg. 14, </em><em>Moscow,</em><em> 117997</em><em>,</em><em> Russian Federation</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">E-mail: podols_kate@mail.ru</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Received: 05.06.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Revised: 22.06.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Accepted: 23.06.2023</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Paper describes machine learning (ML) methods and tools for transport modeling to access forest fires and forest resources by ground means for the regions in Russia. Forestry transport accessibility is a subject to be studied and improved. ML methods play an important role in change detection and automated data collection for the transport infrastructure. We have analyzed recent scientific publications of two systems, namely Russian electronic library “CyberLeninka” and European network for researchers ResearchGate. It should be noted that as of autumn 2023 the number of papers on the ML forestry transport modeling in these systems is small. Plugins from Open Source QGIS’s repository were studied. Some possible increase in the number of ML plugins from researchers and students could be expected, individual developers and small groups show their interest in the topic. ML prospects for ground transport modeling in the forestry have not yet been sufficiently studied.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Key words:</em></strong><em> machine learning, Open Source, GIS, forestry, transport modeling</em></span></p>
<p>&nbsp;</p>
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<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Mihov O. M., Shatalova N. V., Borodina O. V., Vasil&#8217;ev Ju. I., Primenenie tehnologij mashinnogo obuchenija dlja Drone Network v logistike i portovoj dejatel&#8217;nosti Rossii (Application of machine learning technologies for Drone Network in logistics and port activities in Russia), <em>Morskie intellektual&#8217;nye tehnologii, </em>2021, No 4, Vol. 1, pp. 149–157.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><em>Narykova A. N., Plotnikova A. S., Podgotovka prediktorov dlja modelirovanija klimatoregulirujushhih jekosistemnyh uslug lesov na regional&#8217;nom urovne s pomoshh&#8217;ju Google Earth Engine (Preparation of predictors for modeling climate-regulating forest ecosystems services </em><em>at regional level using Google Earth Engine), </em><em>Nauchnye osnovy ustojchivogo upravlenija lesami: Materialy Vserossijskoj nauchnoj konferencii s mezhdunarodnym uchastiem, posvjashhennoj 30-letiju </em><em>CEPF RAS</em><em>. M.: CEPF RAS, 2022, pp. 182</em>–<em>184.</em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><em>Plotnikova A. S., Savin M. S., Lukina N. V., Teben&#8217;kova D. N., Kolycheva A. A., Chumachenko S. I., Shanin V. N., Kartografirovanie klimatoregulirujushhih jekosistemnyh uslug lesov na lokal&#8217;nom urovne (Mapping of forest climate-regulating ecosystem services at local level), </em><em>Nauchnye osnovy ustojchivogo upravlenija lesami: Materialy Vserossijskoj nauchnoj konferencii s mezhdunarodnym uchastiem, posvjashhennoj 30-letiju CEPF RAS.</em><em> M.: CEPF RAS, 2022, pp. 190</em>–<em>192.</em></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Podolskaia E. S., Obzor opyta reshenija zadach transportnogo modelirovanija v lesnom hozjajstve (Review of experience in solving transport modeling problems in the forestry), <em>Voprosy lesnoj nauki,</em> 2021, Vol. 4, No 4, pp. 1–32, DOI: 10.31509/2658-607x-2021-44-92.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Podolskaia E. S., <em>Ispol&#8217;zovanie dannyh distancionnogo zondirovanija Zemli iz kosmosa dlja raspoznavanija izobrazhenija dorog v lesnom hozjajstve (Using Earth remote sensing data from space for road image recognition in the forestry</em>), <em>Voprosy lesnoj nauki,</em> 2022, Vol. 5, No 4, pp. 1–21, DOI 10.31509/2658-607x-202252-115</span></p>
<p><span style="font-family: 'times new roman', times, serif;">Podolskaia E. S., Ershov D. V., Kovganko K. A., Infrastrukturnoe zonirovanie territorii dlja opredelenija svjazej s lesnymi pozharami (na primere Krasnojarskogo kraja, Rossija), (Infrastructure zoning of the territory for determination of links with forest fires (on the example of Krasnoyarsk Territory, Russia), <em>Forests of Russia: politics, industry, science, education: Materials of the VIII All-Russian Scientific and Technical Conference, </em>May 24–26, 2023, St. Petersburg, St. Petersburg State Forest Technical University named after S. M. Kirov, 2023, pp. 330–333.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Shyhaliev R. G., Issledovanie sovremennogo sostojanija primenenija mashinnogo obuchenija v neftegazovoj otrasli (A study of current state of machine learning application in the oil and gas industry), <em>İnformasiya texnologiyaları problemləri,</em> 2020, No 2, pp. 52–60. DOI: 10.25045/jpit.v11.i2.05</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">Snytkina D. A., <em>Primenenie metodov mashinnogo obuchenija pri ocenke i kartografirovanii prirodnyh resursov</em> (Application of machine learning methods to assess and mapping of natural resources): Magisterskaja VKR (spec. 05.04.03), Sankt-Peterburg: SPbGU, 2020, 92 p.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">CP-04-Artificial intelligence tools and platforms for GIS, 2023, URL: https://kurl.ru/TtgVM (2023, 10 August).</span></p>
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		<title>FORESTRY MONOPOLIZATION: A STEP FORWARD OR A STEP BACK?</title>
		<link>https://jfsi.ru/en/6-3-2023-gagarin/</link>
		
		<dc:creator><![CDATA[lena]]></dc:creator>
		<pubDate>Tue, 16 Jan 2024 14:05:33 +0000</pubDate>
				<category><![CDATA[№3 2023]]></category>
		<guid isPermaLink="false">https://jfsi.ru/?p=6160</guid>

					<description><![CDATA[Yu. N. Gagarin Center for Forest Ecology and Productivity of the Russian Academy of Sciences Profsoyuznaya st. 84/32 bldg. 14, Moscow 117997, Russian Federation   E-mail: j.gagarin@list.ru Received: 05.06.2023 Revised: 22.06.2023 Accepted: 23.06.2023 The&#46;&#46;&#46;]]></description>
										<content:encoded><![CDATA[<p><a style="color: #000000;" href="http://jfsi.ru/wp-content/uploads/2024/01/6-3-2023-Gagarin.pdf"><img loading="lazy" class="size-full wp-image-1122 alignright" src="http://jfsi.ru/wp-content/uploads/2018/10/pdf.png" alt="" width="32" height="32" /></a></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>Y</strong><strong>u</strong><strong>. N. Gagarin</strong></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Center for Forest Ecology and Productivity of the Russian Academy of Sciences </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em>Profsoyuznaya st. 84/32 bldg. 14, </em><em>Moscow 117997</em><em>,</em><em> Russian Federation</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><em> </em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">E-mail: j.gagarin@list.ru</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Received: 05.06.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Revised: 22.06.2023</span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;">Accepted: 23.06.2023</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;">The article contains a summary of the first results of the forest management reform conducted in accordance with the Federal Law “On Amendments to the Forestry Code of the Russian Federation” and Articles 14 and 16 of the Federal Law “On General Principles of Implementation of Local Self-Government in the Russian Federation” dated 02 July 2021 No 304-FZ. The scope of application of said law covers changes in the procedure for forest management activities, the establishment of qualification requirements and the procedure for certifying forest management experts, as well as the planning of forest management with reference to the existing and planned development of forests and areas of such development. The article includes a review of recent activities and stages of the forest management reform, an assessment of the impact of the monopoly state of forest management on the quantities and prices of the forest taxation services market, as well as the quality of forest management activities. The article also includes discussion on the aspects of state planning in the field of forest use, conservation, protection and reproduction, taking into consideration the forest planning documentation being granted the status of a binding regulatory document. The article covers the materials of the parliamentary hearings titled “Forest Management: Current Problems and Trends”, held in the Federation Council on 25 April 2023. It includes considerations on potential improvement of legal regulation in the field of forest management.</span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em> </em></strong></span></p>
<p style="text-align: justify;"><span style="font-family: 'times new roman', times, serif;"><strong><em>Key words:</em></strong><em> forestry legislation, forest management reform, service market, monopoly, administrative regulation, forest management regulations of forestry, forest development project, forest use declaration</em></span></p>
<p style="text-align: center;"><span style="font-family: 'times new roman', times, serif;"><strong>REFERENCES</strong></span></p>
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