Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

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Найдено документов в текущей БД: 24

    The Pool of Organic Carbon in the Soils of Russia
/ D. G. Schepaschenko [et al.] // Eurasian Soil Sci. - 2013. - Vol. 46, Is. 2. - P107-116, DOI 10.1134/S1064229313020129. - Cited References: 50 . - 10. - ISSN 1064-2293
РУБ Soil Science
Рубрики:
PASTURE
   FOREST

Кл.слова (ненормированные):
Organic matter -- soil cover -- information system -- soils of Russia

Аннотация: An automated information system making it possible to estimate spatial distribution of soil organic carbon pool with a high spatial resolution (1 km(2)) has been developed. According to the obtained estimates, the total pool of organic carbon in the 1-m-deep soil layer on the territory of Russia reaches 317.1 Pg; the average organic carbon density in this layer for the entire Russia constitutes 19.2 kg C/m(2). Of this amount, 14.4 Pg (or 0.90 kg C/m(2)) is stored in the litter horizon. The developed algorithm allows us to refine the results with the acquisition of new data on soils, vegetation, and the degree of their disturbance, which is particularly important in the changing world.

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Держатели документа:
[Schepaschenko, D. G.
Shvidenko, A. Z.] Int Inst Appl Syst Anal, A-2361 Laxenburg, Austria
[Schepaschenko, D. G.] Moscow State Forest Univ, Moscow 141005, Russia
[Mukhortova, L. V.
Shvidenko, A. Z.
Vedrova, E. F.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Schepaschenko, D.G.; Mukhortova, L.V.; Shvidenko, A.Z.; Vedrova, E.F.

    Impact of wildfire in Russia between 1998-2010 on ecosystems and the global carbon budget
[Text] / A. Z. Shvidenko [et al.] // Dokl. Earth Sci. - 2011. - Vol. 441, Is. 2. - P1678-1682, DOI 10.1134/S1028334X11120075. - Cited References: 15 . - 5. - ISSN 1028-334X
РУБ Geosciences, Multidisciplinary

Аннотация: Verified estimates of wildfire area and related carbon emissions in territories of Russia are reported for the period of 1998-2010. It is shown that the average burnt area is estimated to be at 8.23 million hectares per year (uncertainty +/- 9.0%, confidence interval 0.9), and carbon emissions-121 Tg C yr(-1) (+/- 23%), with a significant interannual variability of these indicators. A quantitative characteristic of fire emissions by species is reported. Forests are a source of three quarters of all carbon emissions caused by wildfires. A significant acceleration of fire regimes is expected during the 21st century as a result of climate change in the country.

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Держатели документа:
[Shvidenko, A. Z.
Shchepashchenko, D. G.
McCallum, I.
Lakyda, I. P.] Int Inst Appl Syst Anal, A-2361 Laxenburg, Austria
[Shchepashchenko, D. G.] Moscow State Forest Univ, Moscow 141005, Moscow Oblast, Russia
[Shvidenko, A. Z.
Vaganov, E. A.
Sukhinin, A. I.] Russian Acad Sci, Sukachev Inst Forest, Siberian Div, Krasnoyarsk 660036, Russia
[Vaganov, E. A.] Siberian Fed Univ, Krasnoyarsk 660041, Russia
[Maksyutov, Sh Sh] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan

Доп.точки доступа:
Shvidenko, A.Z.; Shchepashchenko, D.G.; Vaganov, E.A.; Sukhinin, A.I.; Maksyutov, S.S.; McCallum, I...; Lakyda, I.P.

    Application of the Methods of Thermal Analysis for the Assessment of Organic Matter in Postpyrogenic Soils
[Text] / O. A. Shapchenkova, Y. N. Krasnoshchekov, S. R. Loskutov // Eurasian Soil Sci. - 2011. - Vol. 44, Is. 6. - P677-685, DOI 10.1134/S1064229311060123. - Cited References: 12. - This stugy was supported by the Russian Foundation for Basic Research project no. 08-04-00027. . - 9. - ISSN 1064-2293
РУБ Soil Science

Аннотация: Experimental data on the effect of surface fires on the organic matter transformation in the gray-humus soils of pine forests were obtained in the southwestern part of the Baikal region. The application of methods of thermal analysis (such as differential scanning calorimetry and thermogravimetry) made it possible to obtain qualitative and quantitative information about the decomposition (oxidation) of the components of the soil organic matter upon their heating. It was found that the organic matter content in the soils subjected to fires of high intensity decreased by 1.9 times in comparison with the control. In the litter horizons of the undisturbed soils, thermolabile components (mostly, oligo- and polysaccharides) comprised 61% of the organic matter, and the portion of thermostable components (aromatic compounds) was 39%. A significant decrease in the content of thermolabile components and an increase in the content of thermostable components (up to 62%) were observed in the organic matter of the postpyrogenic forest litter as a result of the charcoal formation during the fire.

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Держатели документа:
[Shapchenkova, O. A.
Krasnoshchekov, Yu. N.
Loskutov, S. R.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Shapchenkova, O.A.; Krasnoshchekov, Y.N.; Loskutov, S.R.

    Ecosystems and climate interactions in the boreal zone of northern Eurasia
[Text] / N. N. Vygodskaya [et al.] // Environ. Res. Lett. - 2007. - Vol. 2, Is. 4. - Ст. 45033, DOI 10.1088/1748-9326/2/4/045033. - Cited References: 33 . - 7. - ISSN 1748-9326
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: The climate system and terrestrial ecosystems interact as they change. In northern Eurasia these interactions are especially strong, span all spatial and timescales, and thus have become the subject of an international program: the Northern Eurasia Earth Science Partnership Initiative (NEESPI). Without trying to cover all areas of these interactions, this paper introduces three examples of the principal micrometeorological, mesometeorological and subcontinental feedbacks that control climate-terrestrial ecosystem interactions in the boreal zone of northern Eurasia. Positive and negative feedbacks of forest paludification, of windthrow, and of climate-forced displacement of vegetation zones are presented. Moreover the interplay of different scale feedbacks, the multi-faceted nature of ecosystems-climate interactions and their potential to affect the global Earth system are shown. It is concluded that, without a synergetic modeling approach that integrates all major feedbacks and relationships between terrestrial ecosystems and climate, reliable projections of environmental change in northern Eurasia are impossible, which will also bring into question the accuracy of global change projections.

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Держатели документа:
[Vygodskaya, N. N.] Jan Kochanowski Univ Humanities & Sci, Inst Geog, Sventokshistkaya Acad Poland, PL-25406 Kielce, Poland
[Groisman, P. Ya] Natl Climat Ctr, Asheville, NC 28801 USA
[Tchebakova, N. M.
Parfenova, E. I.] VN Sukachev Inst Forest, Siberian Branch Russian Acad Sci, Krasnoyarsk 660036, Russia
[Kurbatova, J. A.] Russian Acad Sci, AN Severtsov Inst Ecol & Evolut, Moscow 119071, Russia
[Panfyorov, O.] Univ Gottingen, Inst Bioclimatol, D-37077 Gottingen, Germany
[Sogachev, A. F.] Univ Helsinki, Dept Phys Sci, FI-00014 Helsinki, Finland

Доп.точки доступа:
Vygodskaya, N.N.; Groisman, P.Y.; Tchebakova, N.M.; Kurbatova, J.A.; Panfyorov, O...; Parfenova, E.I.; Sogachev, A.F.

    Climatic responses of tree-ring widths of Larix gmelinii on contrasting north-facing and south-facing slopes in central Siberia
[Text] / J. . Kujansuu [et al.] // J. Wood Sci. - 2007. - Vol. 53: 55th Annual Meeting of the Japan-Wood-Research-Society (MAR, 2005, Kyoto, JAPAN), Is. 2. - P87-93, DOI 10.1007/s10086-006-0837-9. - Cited References: 19 . - 7. - ISSN 1435-0211
РУБ Forestry + Materials Science, Paper & Wood

Аннотация: An analysis was performed on the climatic responses of the radial growth of Larix gmelinii (Rupr.) Rupr. on contrasting north-facing and south-facing slopes in Tura, central Siberia. We developed chronologies of tree-ring width for four plots, designated as north-upper, northlower, south-upper, and south-lower. Both residual and standard chronologies of tree-ring widths exhibited a significant positive correlation with temperature from the end of May until early June in all four plots. The chronologies of ring width did not reveal any major difference in the response to temperature among the four plots. The standard chronologies of ring widths on the north-facing slope were negatively correlated with precipitation during the winter (October-April) and in early and mid-May, whereas the residual chronologies did not reveal clear relationships with precipitation during the winter and May. The significant correlation between ring width and temperature from the end of May until early June indicates that temperatures in springtime play a significant role in the radial growth of L. gmelinii. The negative correlations between standard chronologies of tree-ring width and precipitation in the winter and in May on the north-facing slope indicate that lowfrequency fluctuations in snowfall have negative effects on the radial growth. However, these effects vary and depend on the microscale topography.

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Держатели документа:
Shinshu Univ, Fac Agr, Dept Forest Sci, Nagano 3994598, Japan
Gifu Univ, United Grad Sch Agr Sci, Gifu 5011193, Japan
Hokkaido Univ, Fac Agr, Sapporo, Hokkaido 0600811, Japan
Russian Acad Sci, Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia
Kyushu Res Ctr, Forestry & Forest Prod Res Inst, Kumamoto 8600862, Japan
Forestry & Forest Prod Res Inst, Tsukuba, Ibaraki 3058687, Japan

Доп.точки доступа:
Kujansuu, J...; Yasue, K...; Koike, T...; Abaimov, A.P.; Kajimoto, T...; Takeda, T...; Tokumoto, M...; Matsuura, Y...

    Microbial characteristics of soils on a latitudinal transect in Siberia
[Text] / H. . Santruckova [et al.] // Glob. Change Biol. - 2003. - Vol. 9, Is. 7. - P1106-1117, DOI 10.1046/j.1365-2486.2003.00596.x. - Cited References: 47 . - 12. - ISSN 1354-1013
РУБ Biodiversity Conservation + Ecology + Environmental Sciences

Аннотация: Soil microbial properties were studied from localities on a transect along the Yenisei River, Central Siberia. The 1000 km-long transect, from 56degreesN to 68degreesN, passed through tundra, taiga and pine forest characteristic of Northern Russia. Soil microbial properties were characterized by dehydrogenase activity, microbial biomass, composition of microbial community (PLFAs), respiration rates, denitrification and N mineralization rates. Relationships between vegetation, latitude, soil quality (pH, texture), soil organic carbon (SOC) and the microbial properties were examined using multivariate analysis. In addition, the temperature responses of microbial growth (net growth rate) and activity (soil respiration rate) were tested by laboratory experiments. The major conclusions of the study are as follows: 1. Multivariate analysis of the data revealed significant differences in microbial activity. SOC clay content was positively related to clay content. Soil texture and SOC exhibited the dominant effect on soil microbial parameters, while the vegetation and climatic effects (expressed as a function of latitude) were weaker but still significant. The effect of vegetation cover is linked to SOC quality, which can control soil microbial activity. 2. When compared to fine-textured soils, coarse-textured soils have (i) proportionally more SOC bound in microbial biomass, which might result in higher susceptibility of SOC transformation to fluctuation of environmental factors, and (ii) low mineralization potential, but with a substantial part of the consumed C being transformed to microbial products. 3. The soil microbial community from the northernmost study region located within the permafrost zone appears to be adapted to cold conditions. As a result, microbial net growth rate became negative when temperature rose above 5 degreesC and C mineralization then exceeded C accumulation.

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Держатели документа:
AS CR, Inst Soil Biol, CZ-37005 Ceske Budejovice, Czech Republic
Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
Australian Natl Univ, Res Sch Biol Sci, Canberra, ACT 0200, Australia
Russian Acad Sci, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
Severtsovs Inst Ecol & Evolut Problems, Moscow 117071, Russia
Max Planck Inst Biogeochem, D-07701 Jena, Germany

Доп.точки доступа:
Santruckova, H...; Bird, M.I.; Kalaschnikov, Y.N.; Grund, M...; Elhottova, D...; Simek, M...; Grigoryev, S...; Gleixner, G...; Arneth, A...; Schulze, E.D.; Lloyd, J...

    Comparative ecosystem-atmosphere exchange of energy and mass in a European Russian and a central Siberian bog II. Interseasonal and interannual variability of CO2 fluxes
[Text] / A. . Arneth [et al.] // Tellus Ser. B-Chem. Phys. Meteorol. - 2002. - Vol. 54, Is. 5. - P514-530, DOI 10.1034/j.1600-0889.2002.01349.x. - Cited References: 53 . - 17. - ISSN 0280-6509
РУБ Meteorology & Atmospheric Sciences

Аннотация: Net ecosystem-atmosphere exchange of CO2 (NEE) was measured in two boreal bogs during the snow-free periods of 1998, 1999 and 2000. The two sites were located in European Russia (Fyodorovskoye), and in central Siberia (Zotino). Climate at both sites was generally continental but with more extreme summer-winter gradients in temperature at the more eastern site Zotino. The snow-free period in Fyodorovskoye exceeded the snow-free period at Zotino by several weeks. Marked seasonal and interannual differences in NEE were observed at both locations, with contrasting rates and patterns. Amongst the most important contrasts were: (1) Ecosystem respiration at a reference soil temperature was higher at Fyodorovskoye than at Zotino. (2) The diurnal amplitude of summer NEE was larger at Fyodorovskoye than at Zotino. (3) There was a modest tendency for maximum 24 h NEE during average rainfall years to be more negative at Zotino (-0.17 versus -0.15 mol m(-2) d(-1)), suggesting a higher productivity during the summer months. (4) Cumulative net uptake of CO2 during the snow-free period was strongly related to climatic differences between years. In Zotino the interannual variability in climate, and also in the CO2 balance during the snow-free period, was small. However, at Fyodorovskoye the bog was a significant carbon sink in one season and a substantial source for CO2-C in the next, which was below-average dry. Total snow-free uptake and annual estimates of net CO2-C uptake are discussed, including associated uncertainties.

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Держатели документа:
Max Planck Inst Biogeochem, D-07701 Jena, Germany
Max Planck Inst Meteorol, D-20146 Hamburg, Germany
Severtsov Inst Ecol & Evolut, Moscow, Russia
VN Sukachev Forest Inst, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Arneth, A...; Kurbatova, J...; Kolle, O...; Shibistova, O.B.; Lloyd, J...; Vygodskaya, N.N.; Schulze, E.D.

    Feasibility of estimating stem size distribution from measurement on the largest trees in even-aged pure stands
[Text] / A. . Osawa, A. P. Abaimov // Can. J. For. Res.-Rev. Can. Rech. For. - 2001. - Vol. 31, Is. 5. - P910-918, DOI 10.1139/cjfr-31-5-910. - Cited References: 23 . - 9. - ISSN 0045-5067
РУБ Forestry

Аннотация: Reconstruction of the size distribution of trees in stands provides critical information for assessing the effects of environmental changes on forests and for forest management. For furthering a method of such reconstruction, feasibility of estimating size distribution in stem volume from measurement of the largest trees was examined for even-aged pure stands of Pinus banksiana Lamb.and Larix gmelinii (Rupr.) Rupr. We tested what percentage of the largest trees should be included in obtaining a frequency distribution in stem volume that is not statistically different from the observed size distribution patterns. The -3/2 power, beta-type, and adjusted beta-type distribution functions were applied. Comparison of the observed stem frequencies and those estimated from measurement of the largest trees in a stand suggested that (i) the -3/2 power distribution, beta-type distribution, or adjusted beta-type distribution may be used for reconstruction of stem size variation in pure stands, if the overall size variation could be approximated by one of these functions; (ii) we can be at least 95% sure that the tree size pattern be expressed successfully with the -3/2 power distribution with tree samples of only the largest 20% in the stand, or with the beta-type distribution with the largest 30% in the stand; and (iii) the reliability decreases somewhat for the adjusted beta-type distribution. The second observation implies that reconstruction of the temporal changes in stand structure may be reliable up to the time when the stand density was about five times that of the trees used for fitting the -3/2 power distribution curve. Reliability may be warranted up to the stand density of about three times as the number of trees used for fitting the beta-type distribution. Other considerations and limitations are also discussed.

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Держатели документа:
Ryukoku Univ, Fac Intercultural Commun, Ohtsu, Shiga 5202194, Japan
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Osawa, A...; Abaimov, A.P.

    Foliar carbon isotope discrimination in Larix species and sympatric evergreen conifers: a global comparison
[Text] / B. D. Kloeppel [et al.] // Oecologia. - 1998. - Vol. 114, Is. 2. - P153-159, DOI 10.1007/s004420050431. - Cited References: 45 . - 7. - ISSN 0029-8549
РУБ Ecology

Аннотация: Larches (Larix spp.), deciduous conifers, occur in the northern hemisphere in cold-temperate and boreal climates - an environment normally thought to favor ever-green tree species. We compare foliar carbon isotope discrimination (Delta), instantaneous water use efficiency, total foliar nitrogen concentration, and specific leaf area (for a subset of sites) between Larix spp. and co-occurring evergreen conifers at 20 sites throughout the natural range of larches. Except for Larix occidentalis in the xeric Intermountain West, USA, Delta is significantly (P < 0.05) greater for larches than co-occurring evergreen conifers at 77% of the sites, suggesting that larches use water less efficiently. At elevations greater than 3000 m, the Delta of Lar ix-spp. and co-occurring conifers converge, suggesting that water is not the limiting resource. Foliar nitrogen concentration and specific leaf area are two ecophysiological characteristics that are positively correlated with high photosynthetic capacity. Foliar nitrogen concentration is significantly greater for larches than evergreen conifers at 88% of the sites and specific leaf area is approximately three times greater for larches than co-occurring conifers. Future studies should examine the potential effect that global warming may have on the distribution of larch forests because the water use efficiency of larches is commonly less than cooccurring evergreen conifers and the boreal and high-latitude environments are likely to experience the greatest climate warming.

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Держатели документа:
Univ Wisconsin, Dept Forest Ecol & Management, Madison, WI 53706 USA
Univ Wisconsin, Dept Chem, Madison, WI 53706 USA
Russian Acad Sci, Sukachev Forest Inst, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Kloeppel, B.D.; Gower, S.T.; Treichel, I.W.; Kharuk, S...

    Similar patterns of change in stemwood calcium concentration in red spruce and Siberian fir
[Text] / W. C. Shortle [et al.] // J. Biogeogr. - 1995. - Vol. 22: 1st Global Change and Terrestrial Ecosystems Science Conference (MAY 23-27, 1994, WOODS HOLE, MA), Is. 02.03.2013. - P467-473, DOI 10.2307/2845943. - Cited References: 11 . - 7. - ISSN 0305-0270
РУБ Ecology + Geography, Physical
Рубрики:
ACIDIC DEPOSITION
   TRENDS

   IMPACT

   FOREST

Кл.слова (ненормированные):
dendrochemistry -- forest decline -- environmental markers -- wood cations

Аннотация: Changes in stemwood calcium concentration ([Ca]) for the last 120 years occurred in a common pattern for two sample collections of red spruce (n=33 and 20) from the northeastern United States and for one sample collection of Siberian fir (n=20) from southcentral Siberia, Russia. The [Ca] was measured for wood formed during the periods 1871-90, 1891-1910, 1911-30, 1931-50, 1951-70 and 1971-90. For each core, the relative increase or decrease in [Ca] for adjacent periods of wood formation was recorded. The relative frequency of positive change in [Ca] for each period of wood formation was calculated for the three sample collections. Previous research indicated that under equilibrium conditions, [Ca] in stemwood tended to decrease in more recently formed wood, due to declining numbers of Ca binding sites. Consequently, we expected a low frequency of positive changes in [Ca] in successively formed wood. Consistent with expectation, the relative frequency of positive change from the preceding period to the periods 1891-1910, 1911-30, 1931-50, and 1971-90 were low. Contrary to expectation, the frequency of positive increases in [Ca] more than doubled in 1951-70 compared to 1931-50. The frequency of positive increases in the 1951-70 period relative to the preceding period was 48%, significantly greater than all other periods (P less than or equal to 0.01). The frequencies of positive increases for all other periods were not significantly different from each other (overall mean = 21%, SD = 7). This anomaly in the frequency of positive change in [Ca] in wood formed in 1951-70 relative to wood formed in 1931-50 indicated a perturbation in the ion exchange chemistry of stemwood in two widely separated parts of the northern coniferous forest. This anomaly could be due to external or internal factors. Changes in sap chemistry that affected stemwood chemistry could have been due to changes in the rooting zone. Such changes in rooting zone chemistry could result from the atmospheric deposition of ionic pollutants. Other external factors that could cause the observed anomaly include unusual climatic periods or environmental disturbances such as logging or fire. Internal factors that might produce an anomalously high frequency of positive change of [Ca] include heartwood formation, stemwood infection and a hypersensitive response of the tree against infection.

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Держатели документа:
US FOREST SERV,DURHAM,NH 03824
VV SUKACHEV FOREST INST,KRASNOYARSK 660036,RUSSIA

Доп.точки доступа:
Shortle, W.C.; Smith, K.T.; Minocha, R...; Alexeyev, V.A.

    Influence of climatypes of Scots pine on certain chemical and microbiological characteristics of soils
[Text] / N. B. Naumova [et al.] // Contemp. Probl. Ecol. - 2009. - Vol. 2, Is. 2. - P147-151, DOI 10.1134/S1995425509020106. - Cited References: 20. - The work was carried out with the financial support of the Integration projects of SB RAS no. 5.23 and no. 24, as well as the project "Biogeochemical Cycles in the Natural and Man-Made Landscape, Their Biospheric and Regional Meaning and Regulation," reg. no. 0120.0 406322. . - 5. - ISSN 1995-4255
РУБ Ecology

Аннотация: By using multivariate statistical analysis, the influence of Scots pine climatypes on a set of chemical and microbiological properties of soil, i.e., soil C/N, C(mic)/C(org), and C(mic)/N(mic), was revealed in a series of long-term (ca. 30 years) field experiments, which were carried out according to the same scheme under contrasting environmental and soil conditions of Siberian forestries.

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Держатели документа:
[Naumova, N. B.
Makarikova, R. P.] Russian Acad Sci, Siberian Branch, Inst Soil Sci & Agrochem, Novosibirsk 630099, Russia
[Tarakanov, V. V.] Russian Acad Sci, Siberian Branch, W Siberian Affiliat Sukachev Inst Forest, Novosibirsk 630082, Russia
[Kuz'mina, N. A.
Novikova, T. N.
Milyutin, L. I.] Russian Acad Sci, Siberian Branch, Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Naumova, N.B.; Makarikova, R.P.; Tarakanov, V.V.; Kuz'mina, N.A.; Novikova, T.N.; Milyutin, L.I.; SB RAS [5.23, 24]

    The Eurosiberian Transect: an introduction to the experimental region
[Text] / E. D. Schulze [et al.] // Tellus Ser. B-Chem. Phys. Meteorol. - 2002. - Vol. 54, Is. 5. - P421-428, DOI 10.1034/j.1600-0889.2002.01342.x. - Cited References: 27 . - 8. - ISSN 0280-6509
РУБ Meteorology & Atmospheric Sciences

Аннотация: An introduction is given to the geography of Russian forests and to the specific conditions of the study sites located along the 60degrees latitude east of Moscow (Fyedorovskoe) near the Ural Mountains (Syktivkar) and in Central Siberia near the Yennisei river (Zotino). The climatic conditions were similar at all three sites. The main ecological parameter that changes between European Russia and Siberia is the length of the growing season (230 d above 0 degreesC NE Moscow to 170 d above 0 degreesC in Central Siberia) and to a lesser extent precipitation (580 mm NE Moscow to 530 mm in Central Siberia). The experimental sites were generally similar to the regional conditions,. although the Tver region has less forest and more grassland than the central forest reserve, and the Komi region has slightly less wetland than the study area. The Krasnoyarsk region reaches from the arctic ocean to and central Asia and contains a significant proportion of non-forest land. The boreal forest of west and east Yennisei differs mainly with respect to wetlands, which cover almost half of the land area on the west bank. All sites are prone to disturbance. Heavy winds and drought or surplus water are the main disturbance factors in European Russia (a 15-20 yr cycle), and fire is the dominating disturbance factor in Siberia (220-375 yr for stand replacing fires).

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Держатели документа:
Max Planck Inst Biogeochem, D-07701 Jena, Germany
RAS, Severtsov Inst Ecol & Evolut, Moscow 1107071, Russia
Siberian RAS, Inst Forest, Krasnoyarsk 660036, Russia
Univ Tuscia, Dept Forest Scil & Environm, I-01100 Viterbo, Italy

Доп.точки доступа:
Schulze, E.D.; Vygodskaya, N.N.; Tchebakova, N.M.; Czimczik, C.I.; Kozlov, D.N.; Lloyd, J...; Mollicone, D...; Parfenova, E...; Sidorov, K.N.; Varlagin, A.V.; Wirth, C...

    Intra-annual variability of anatomical structure and delta C-13 values within tree rings of spruce and pine in alpine, temperate and boreal Europe
[Text] / E. A. Vaganov [et al.] // Oecologia. - 2009. - Vol. 161, Is. 4. - P729-745, DOI 10.1007/s00442-009-1421-y. - Cited References: 72. - This work was supported by Alexander von Humboldt (Research Award 2003 for E. Vaganov) and the Russian Foundation of Basic Research (RFBR-05-04-48069). We thank Alessandro Cescatti, Leonardo Montagnani, Stefano Minerbi and Claudio Mutinelli for providing the climate and nitrogen data for Renon, Sune Linder for dendrometer data, and Anders Lindroth for eddy flux data of the Flakaliden site. We thank Gerd Gleixner for discussion of this manuscript. We also like to thank Annett Boerner for the artwork and Jens Schumacher for advice on statistical analyses. . - 17. - ISSN 0029-8549
РУБ Ecology

Аннотация: Tree-ring width, wood density, anatomical structure and C-13/C-12 ratios expressed as delta C-13-values of whole wood of Picea abies were investigated for trees growing in closed canopy forest stands. Samples were collected from the alpine Renon site in North Italy, the lowland Hainich site in Central Germany and the boreal Flakaliden site in North Sweden. In addition, Pinus cembra was studied at the alpine site and Pinus sylvestris at the boreal site. The density profiles of tree rings were measured using the DENDRO-2003 densitometer, delta C-13 was measured using high-resolution laser-ablation-combustion-gas chromatography-infra-red mass spectrometry and anatomical characteristics of tree rings (tracheid diameter, cell-wall thickness, cell-wall area and cell-lumen area) were measured using an image analyzer. Based on long-term statistics, climatic variables, such as temperature, precipitation, solar radiation and vapor pressure deficit, explained < 20% of the variation in tree-ring width and wood density over consecutive years, while 29-58% of the variation in tree-ring width were explained by autocorrelation between tree rings. An intensive study of tree rings between 1999 and 2003 revealed that tree ring width and delta C-13-values of whole wood were significantly correlated with length of the growing season, net radiation and vapor pressure deficit. The delta C-13-values were not correlated with precipitation or temperature. A highly significant correlation was also found between delta C-13 of the early wood of one year and the late wood of the previous year, indicating a carry-over effect of the growing conditions of the previous season on current wood production. This latter effect may explain the high autocorrelation of long-term tree-ring statistics. The pattern, however, was complex, showing stepwise decreases as well as stepwise increases in the delta C-13 between late wood and early wood. The results are interpreted in the context of the biochemistry of wood formation and its linkage to storage products. It is clear that the relations between delta C-13 and tree-ring width and climate are multi-factorial in seasonal climates.

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Держатели документа:
[Schulze, Ernst-Detlef
Brand, Willi A.
Roscher, Christiane] Max Planck Inst Biogeochem, D-07701 Jena, Germany
[Vaganov, Eugene A.
Skomarkova, Marina V.] RAS, Inst Forest SB, Krasnoyarsk 660036, Russia
[Knohl, Alexander] ETH, Dept Plant Sci, CH-8092 Zurich, Switzerland

Доп.точки доступа:
Vaganov, E.A.; Schulze, E.D.; Skomarkova, M.V.; Knohl, A...; Brand, W.A.; Roscher, C...; Alexander von Humboldt; Russian Foundation of Basic Research [RFBR-05-04-48069]

    Influence of logging on the effects of wildfire in Siberia
[Text] / E. A. Kukavskaya [et al.] // Environ. Res. Lett. - 2013. - Vol. 8, Is. 4. - Ст. 45034, DOI 10.1088/1748-9326/8/4/045034. - Cited References: 43. - The authors gratefully acknowledge financial support for this research from the National Aeronautics and Space Administration (NASA), the Land Cover Land Use Change (LCLUC) Science Program, the Russian Foundation for Basic Research (grant No. 12-04-31258), and the Russian Academy of Sciences, Siberian Branch. The authors would like to thank the three anonymous reviewers for their helpful comments and useful suggestions. . - 11. - ISSN 1748-9326
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences
Рубрики:
FOREST
   COVER

   MODIS

   AREAS

Кл.слова (ненормированные):
light conifer stands -- Pinus -- Larix -- fire -- clear-cuts -- partial logging -- legal and illegal logging -- fuel consumption -- carbon emissions -- regeneration

Аннотация: The Russian boreal zone supports a huge terrestrial carbon pool. Moreover, it is a tremendous reservoir of wood products concentrated mainly in Siberia. The main natural disturbance in these forests is wildfire, which modifies the carbon budget and has potentially important climate feedbacks. In addition, both legal and illegal logging increase landscape complexity and affect burning conditions and fuel consumption. We investigated 100 individual sites with different histories of logging and fire on a total of 23 study areas in three different regions of Siberia to evaluate the impacts of fire and logging on fuel loads, carbon emissions, and tree regeneration in pine and larch forests. We found large variations of fire and logging effects among regions depending on growing conditions and type of logging activity. Logged areas in the Angara region had the highest surface and ground fuel loads (up to 135 t ha(-1)), mainly due to logging debris. This resulted in high carbon emissions where fires occurred on logged sites (up to 41 tC ha(-1)). The Shushenskoe/Minusinsk and Zabaikal regions are characterized by better slash removal and a smaller amount of carbon emitted to the atmosphere during fires. Illegal logging, which is widespread in the Zabaikal region, resulted in an increase in fire hazard and higher carbon emissions than legal logging. The highest fuel loads (on average 108 t ha(-1)) and carbon emissions (18-28 tC ha(-1)) in the Zabaikal region are on repeatedly burned unlogged sites where trees fell on the ground following the first fire event. Partial logging in the Shushenskoe/Minusinsk region has insufficient impact on stand density, tree mortality, and other forest conditions to substantially increase fire hazard or affect carbon stocks. Repeated fires on logged sites resulted in insufficient tree regeneration and transformation of forest to grasslands. We conclude that negative impacts of fire and logging on air quality, the carbon cycle, and ecosystem sustainability could be decreased by better slash removal in the Angara region, removal of trees killed by fire in the Zabaikal region, and tree planting after fires in drier conditions where natural regeneration is hampered by soil overheating and grass proliferation.

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Держатели документа:
[Kukavskaya, E. A.
Ivanova, G. A.
Zhila, S. V.] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia
[Buryak, L. V.
Kalenskaya, O. P.] Siberian State Technol Univ, Krasnoyarsk 660049, Russia
[Conard, S. G.] US Forest Serv, Rocky Mt Res Stn, Missoula, MT 59807 USA
[Conard, S. G.] George Mason Univ, Fairfax, VA 22030 USA
[McRae, D. J.] Canadian Forest Serv, Nat Resources Canada, Sault Ste Marie, ON P6A 2E5, Canada
ИЛ СО РАН

Доп.точки доступа:
Kukavskaya, E.A.; Buryak, L.V.; Ivanova, G.A.; Conard, S.G.; Kalenskaya, O.P.; Zhila, S.V.; McRae, D.J.; National Aeronautics and Space Administration (NASA); Land Cover Land Use Change (LCLUC) Science Program; Russian Foundation for Basic Research [12-04-31258]; Russian Academy of Sciences, Siberian Branch

    Biological activity of waste dump substrates in the eastern part of the Kansk-Achinsk coal field
[Text] / O. V. Trefilova, P. A. Oskorbin // Eurasian Soil Sci. - 2014. - Vol. 47, Is. 2. - P96-101, DOI 10.1134/S1064229314020112. - Cited References: 22 . - ISSN 1064-2293. - ISSN 1556-195X
РУБ Soil Science

Аннотация: The results of a field experiment for studying the seasonal dynamics of the CO2 (R-all) emitted from the overburden and enclosing rocks of a coal mine are presented as an integral index of their biological activity. The mean rate of the CO2 emission from the control substrate was 1.2 g C/m(2) per 24 h. The intensity of R-all for the variant with the application of mineral and complex fertilizers, along with a microbiological preparation, was higher by 28 and 34%, respectively. In the same variants, the R-all values little changed during the whole growing period. The measurements of the potential respiration of the rock mixture in the laboratory showed that a significant part of the CO2 flux was formed at the expense of carbon dioxide of abiotic origin. The values of the CO2 emission are concluded to be overestimated as compared to those for the real level of the biological activity of the substrates studied.

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Держатели документа:
[Trefilova, O. V.
Oskorbin, P. A.] Russian Acad Sci, Siberian Div, Sukachev Inst Forestry, Krasnoyarsk 660036, Russia
ИЛ СО РАН

Доп.точки доступа:
Trefilova, O.V.; Oskorbin, P.A.

    Biological sources of soil CO2 under Larix sibirica and Pinus sylvestris
[Text] / A. I. Matvienko, M. I. Makarov, O. V. Menyailo // Russ. J. Ecol. - 2014. - Vol. 45, Is. 3. - P174-180, DOI 10.1134/S1067413614030072. - Cited References: 15. - This study was supported by the Russian Foundation for Basic Research (project no. 10-04-92518-IK_a), the Siberian Branch of the Russian Academy of Sciences (project no. 122), and a CRDF grant no. RUG1-2979-KR-10. . - ISSN 1067-4136. - ISSN 1608-3334
РУБ Ecology

Аннотация: Mycorrhizal ingrowth collars were used to study the effect of tree species on the seasonal dynamics of carbon dioxide flux from three major sources of soil respiration: (1) plant roots, (2) mycorrhizal hyphae, and (3) microorganisms. Distinct seasonality in carbon transport to mycorrhizae was revealed, with its highest values being observed during the second half of the growing season. The annual amount of C transferred through mycorrhizae did not differ between the two tree species, and the contribution of mycorrhizae to soil surface CO2 emission was about 20%.

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Держатели документа:
[Matvienko, A. I.
Menyailo, O. V.] Russian Acad Sci, Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia
[Makarov, M. I.] Moscow MV Lomonosov State Univ, Moscow 119991, Russia
ИЛ СО РАН

Доп.точки доступа:
Matvienko, A.I.; Makarov, M.I.; Menyailo, O.V.; Russian Foundation for Basic Research [10-04-92518-IK_a]; Siberian Branch of the Russian Academy of Sciences [122]; CRDF [RUG1-2979-KR-10]

    Variability of ground CO2 concentration in the middle taiga subzone of the Yenisei region of Siberia
[Text] / A. V. Timokhina [et al.] // Russ. J. Ecol. - 2015. - Vol. 46, Is. 2. - P143-151, DOI 10.1134/S1067413615020125. - Cited References:30. - The study of daily variability of CO2 atmospheric concentration at ZOTTO station and seasonal distribution of COINF2/INF over Siberia in comparison with Canada and the North Atlantic was supported by the Russian Science Foundation, project no. 14-24-00113. . - ISSN 1067-4136. - ISSN 1608-3334
РУБ Ecology

Аннотация: The results of measurements of ground CO2 concentration in the middle taiga subzone of the Yenisei region of Siberia (the ZOTTO observatory) in 2009 to 2012 are presented. Specific features of CO2 variability over the altitude profile up to 301 m are accounted for by specific diurnal and seasonal features in the functioning of terrestrial ecosystems as well as by atmospheric processes. It has been shown that the significance of regional and global components increases with elevation, while the contribution of the underlying surface in the region of the observatory decreases. The observed gradient differences between CO2 concentrations recorded at the onset and at the end of the cold period are explained by seasonal changes in the height of the atmospheric boundary layer. Comparison of data obtained at the ZOTTO observatory and at monitoring stations in Canada and the North Atlantic has shown that general trends in the seasonal variability of CO2 are similar and that specific features of the processes under study are dependent on biogeographic characteristics of the study regions.

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Scopus

Держатели документа:
Russian Acad Sci, Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia.
Max Planck Inst Biogeochem, D-07745 Jena, Germany.
ИЛ СО РАН

Доп.точки доступа:
Timokhina, A.V.; Prokushkin, A.S.; Onuchin, A.A.; Panov, A.V.; Kofman, G.B.; Heimann, M.; Russian Science Foundation [14-24-00113]

    Climate-induced mortality of spruce stands in Belarus
[Text] / V. I. Kharuk [et al.] // Environ. Res. Lett. - 2015. - Vol. 12, Is. 12. - Ст. 125006, DOI 10.1088/1748-9326/10/12/125006. - Cited References:54. - The Russian Science Foundation (grant #14-24-00112) primarily supported this research. Additional support for K J Ranson by NASA's Terrestrial Ecology program is acknowledged. . - ISSN 1748-9326
РУБ Environmental Sciences + Meteorology & Atmospheric Sciences

Аннотация: The aim of this work is an analysis of the causes of spruce (Picea abies L.) decline and mortality in Belarus. The analysis was based on forest inventory and Landsat satellite (land cover classification, climate variables (air temperature, precipitation, evaporation, vapor pressure deficit, SPEI drought index)), and GRACE-derived soil moisture estimation (equivalent of water thickness anomalies, EWTA). We found a difference in spatial patterns between dead stands and all stands (i.e., before mortality). Dead stands were located preferentially on relief features with higher water stress risk (i.e., higher elevations, steeper slopes, south and southwestern exposure). Spruce mortality followed a series of repeated droughts between 1990 and 2010. Mortality was negatively correlated with air humidity (r = -0.52), and precipitation (r = -0.57), and positively correlated with the prior year vapor pressure deficit (r = 0.47), and drought increase (r = 0.57). Mortality increased with the increase in occurrence of spring frosts (r = 0.5), and decreased with an increase in winter cloud cover (r = -0.37). Spruce mortality was negatively correlated with snow water accumulation (r = -0.81) and previous year anomalies in water soil content (r = -0.8). Weakened by water stress, spruce stands were attacked by pests and phytopathogens. Overall, spruce mortality in Belarussian forests was caused by drought episodes and drought increase in synergy with pest and phytopathogen attacks. Vast Picea abies mortality in Belarus and adjacent areas of Russia and Eastern Europe is a result of low adaptation of that species to increased drought. This indicates the necessity of spruce replacement by drought-tolerant indigenous (e.g., Pinus sylvestris, Querqus robur) or introduced (e.g., Larix sp. or Pseudotsuga menzieslii) species to obtain sustainable forest growth management.

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Держатели документа:
VN Sukachev Inst Forest SB RAS, Krasnoyarsk, Russia.
Siberian Fed Univ, Krasnoyarsk, Russia.
Siberian State Aerosp Univ, Krasnoyarsk, Russia.
NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA.

Доп.точки доступа:
Kharuk, Viacheslav I.; Im, Sergei T.; Dvinskaya, Maria L.; Golukov, Alexei S.; Ranson, Kenneth J.; Russian Science Foundation [14-24-00112]; NASA's Terrestrial Ecology program

    The Effect of Postfire Temperature Anomalies on Seasonal Soil Thawing in the Permafrost Zone of Central Siberia Evaluated Using Remote Data
/ E. I. Ponomarev, T. V. Ponomareva // Contemp. Probl. Ecol. - 2018. - Vol. 11, Is. 4. - P420-427, DOI 10.1134/S1995425518040066. - Cited References:26. - This work was supported by the Russian Foundation for Basic Research, projects nos. 17-04-00589 and 18-05-00432; the Government of Krasnoyarsk krai and the Foundation for Research and Technology Support of Krasnoyarsk krai, project no. 17-41-240475. . - ISSN 1995-4255. - ISSN 1995-4263
РУБ Ecology
Рубрики:
FOREST
Кл.слова (ненормированные):
remote data -- temperature -- postfire areas -- permafrost zone -- larch -- forests -- seasonally thawed layer

Аннотация: This article contains data on the dynamics of thermal fields in postfire areas obtained using remote satellite imagery. It is found that postfire areas of the permafrost zone have a background thermal field in the range of 10.780-11.280 mu m, which is caused by changes in the parameters of the stand, the ground cover, and the litter. The average surface temperature of postfire areas in larch forests is characterized by increasing up to Delta T = 7.2 +/- 1.3A degrees D relative to the control values in summer, which is 20-40% higher than the temperature of the control undisturbed areas. Temperature anomalies last for more than 10 years under conditions of the natural restoration of the ground cover. It is found that the rate of recovery of temperature anomalies is 2.5 times lower than the dynamics of the NDVI vegetative index. It is numerically evaluated that temperature anomalies on the soil surface could lead to an increase in the thawing depth of the soil layer by up to 20% more than the average statistical rate.

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Держатели документа:
Russian Acad Sci, Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Krasnoyarsk 660041, Russia.

Доп.точки доступа:
Ponomarev, E. I.; Ponomareva, T. V.; Russian Foundation for Basic Research [17-04-00589, 18-05-00432]; Government of Krasnoyarsk krai; Foundation for Research and Technology Support of Krasnoyarsk krai [17-41-240475]

    Warming hiatus and evergreen conifers in Altay-Sayan Region, Siberia
/ V. I. Kharuk, S. T. Im, I. A. Petrov // J Mt. Sci. - 2018. - Vol. 15, Is. 12. - P2579-2589, DOI 10.1007/s11629-018-5071-6. - Cited References:44. - This research was supported by the Russian Foundation for Basic Research (grants #18-05- 00432). Dendrochronological analysis was supported by the Russian Science Foundation (17-74-10113). . - ISSN 1672-6316. - ISSN 1993-0321
РУБ Environmental Sciences

Аннотация: Warming hiatus occurred in the Altay-Sayan Mountain Region, Siberia in c. 1997-2014. We analyzed evergreen conifer (EGC) stands area (satellite data) and trees (Siberian pine, Pinus sibirica Du Tour, Siberian fir, Abies sibirica Ledeb.) growth increment (dendrochronology data) response to climate variables before and during the hiatus. During the hiatus, EGC area increased in the highlands (>1000 m) (+30%), whereas at low and middle elevations (<1000 m. a.s.l.) the EGC area decreased (-7%). The EGC area increase was observed on the rain-ward northwest slopes mainly. In highlands, EGC area increase mainly correlated with summer air temperature, whereas at low and middle elevations EGC area decrease correlated with drought index SPEI and vapor pressure deficit (VPD). EGC mortality (fir and Siberian pine) in lowland was caused by the synergy of water stress (inciting factor) and barkbeetle attacks (contributing factor). Tree growth increment (GI) dynamics differs with respect to elevation. At high elevation (1700 m) GI permanently increased since warming onset, whereas at the middle (900 m) and low elevations (450 m) GI increased until c. 1983 yr. with followed depression. That GI breakpoint occurred about a decade before hiatus onset. In spite of growth depression, during hiatus GI was higher than that in pre-warming period. At high elevation, GI positively responded to elevated June temperatures and negatively to moisture increase (precipitation, root zone moisture content, VPD, and SPEI). At low elevation GI negatively responded to June temperatures and positively to moisture increase. For both, low and high elevation, these patterns persisted throughout the study period (1967-2014). On the contrary, at middle elevations GI dependence on climate variables switch after breakpoint year (1983). Before breakpoint, June air temperature (positive correlation) and moisture (negative correlations) controlled GI. Further temperature increase leads GI depression and switched correlation signs to opposite (from positive to negative with temperature, and from negative to positive with moisture variables).

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Держатели документа:
Russian Acad Sci, Siberian Branch, Fed Sci Ctr, Sukachev Inst Forest, Academgorodok 50-28, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Svobodny Str 79, Krasnoyarsk 660041, Russia.
Reshetnev Siberian State Univ Sci & Technol, Krasnoyarsky Rabochy Str 31, Krasnoyarsk 660014, Russia.

Доп.точки доступа:
Kharuk, Viacheslav I.; Im, Sergei T.; Petrov, Il'ya A.; Russian Foundation for Basic Research [18-05- 00432]; Russian Science Foundation [17-74-10113]