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

: материалы временных коллективов / I. N. Tretyakova // Forest genetic improvement for environment and production: abstract collection of the Asia-Pacific symposium on forest genetic improvement (October 19-22, 1994, Beijing, China). - 1994. - С. 4-5

Держатели документа:
Институт леса им. В.Н. Сукаыева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

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Третьякова, Ираида Николаевна
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РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1

: материалы временных коллективов / L. I. Milyutin // Forest genetic improvement for environment and production: abstract collection of the Asia-Pacific symposium on forest genetic improvement (October 19-22, 1994, Beijing, China). - 1994. - С. 19

Держатели документа:
Институт леса им. В.Н. Сукаыева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

Доп.точки доступа:
Милютин, Леонид Иосифович
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РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1

: материалы временных коллективов / M. A. Shemberg // Forest genetic improvement for environment and production: abstract collection of the Asia-Pacific symposium on forest genetic improvement (October 19-22, 1994, Beijing, China). - 1994. - С. 19

Держатели документа:
Институт леса им. В.Н. Сукачева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

Доп.точки доступа:
Шемберг, Михаил Антонович
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РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1

: материалы временных коллективов / N. A. Kuzmina, V. N. Sukachev // Forest genetic improvement for environment and production: abstract collection of the Asia-Pacific symposium on forest genetic improvement (October 19-22, 1994, Beijing, China). - 1994. - С. 44

Держатели документа:
Институт леса им. В.Н. Сукачева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

Доп.точки доступа:
Sukachev, Vladimir Nikolayevich; Кузьмина, Нина Алексеевна
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РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1

: материалы временных коллективов / G. V. Kuznetsova // Forest genetic improvement for environment and production: abstract collection of the Asia-Pacific symposium on forest genetic improvement (October 19-22, 1994, Beijing, China). - 1994. - С. 45

Держатели документа:
Институт леса им. В.Н. Сукачева Сибирского отделения Российской академии наук : 660036, Красноярск, Академгородок, 50, стр., 28

Доп.точки доступа:
Кузнецова, Галина Васильевна
Имеются экземпляры в отделах:
РСФ (29.01.2008г. (1 экз.) - Б.ц.) - свободны 1

[Text] / Y. . Liu [et al.] // Chin. Sci. Bull. - 2004. - Vol. 49, Is. 4. - P405-409, DOI 10.1360/03wd0409. - Cited References: 16 . - 5. - ISSN 1001-6538РУБ Multidisciplinary Sciences

Аннотация: By analyzing statistical characteristics of five tree-ring standard chronologies, early-wood ring width (EWW), late-wood ring width (LWW), total ring width (TRW), minimum early-wood density (MinD), maximum late-wood density (MaxD) and, their climatic response respectively, we reconstructed the May to July precipitation using late-wood ring width (LWW) over the north Helan Mountain since A.D. 1726. The explained variance is 42% (R-adj(2) = 41%, F = 31.46, p < 0.000001). After 11-a moving average, the explained variance reaches 82% (F = 156.9, p < 0.05). On the decadal scale, the rainfall reconstruction of the northern Helan Mountain displays a quite similar variation pattern with that of the April to early July precipitation in Baiyinaobao, east of Inner Mongolia for the last 150 years. It may reflect the intensity variation of the East Asia Summer Monsoon front to a certain extent. Spectrum analysis shows 11-a and 22-a periodicities in the May to July precipitation reconstruction at the north Helan Mountain.

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Держатели документа:
Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China
Russian Acad Sci, Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Liu, Y...; Shi, J.F.; Shishov, V...; Vaganov, E...; Yang, Y.K.; Cai, Q.F.; Sun, J.Y.; Wang, L...; Djanseitov, I...

[Text] / W. E. WALLNER [et al.] // J. Econ. Entomol. - 1995. - Vol. 88, Is. 2. - P337-342. - Cited References: 31 . - 6. - ISSN 0022-0493РУБ Entomology

Аннотация: In field studies in the Russian Far East, five types of illuminating devices were evaluated for attracting adult gypsy moth, Lymantria dispar (L.), pink gypsy moth, L. mathura Moore, and nun moth, L. monacha (L.). Our objective was to determine if light from commercial lamps suited to out-of-doors floodlighting could be modified to reduce their attractiveness to moths without a reduction of illumination. During 17 nights of tests, fluorescent blacklight lamps captured significantly more adults than either phosphor mercury or high-pressure sodium lamps, Captures were slightly higher for phosphor mercury than high-pressure sodium lamps but both were unattractive to all three lymantriids after the addition of filters that blocked spectral emissions <480 nm. Daily temporal periodicity, based on adult captures at lights, resulted in distinct activity patterns for the three lymantriids. Peak activity for L. dispar was between 2300 and 0100 hours; for L. mathura, 0100-0300 hours; and 0300-0500 hours for L. monacha. Temporal activity patterns suggest that L. dispar and L. monacha possess nonoverlapping diel rhythms, whereas L. mathura overlaps broadly with both L. dispar and L. monacha.

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Держатели документа:
FORESTRY CANADA,PACIFIC FORESTRY CTR,VICTORIA,BC V8Z 1M5,CANADA
OSRAM SYLVANIA,SALEM,MA 01970
VN SUKACHEV INST FOREST,KRASNOYARSK 660036,RUSSIA
UNIV MASSACHUSETTS,DEPT ENTOMOL,AMHERST,MA 01003

Доп.точки доступа:
WALLNER, W.E.; HUMBLE, L.M.; LEVIN, R.E.; BARANCHIKOV, Y.N.; CARDE, R.T.

[Text] / N. I. Kirichenko, Y. N. Baranchikov, S. . Vidal // Agric. For. Entomol. - 2009. - Vol. 11, Is. 3. - P247-254, DOI 10.1111/j.1461-9563.2009.00437.x. - Cited References: 43. - We thank Mr Viktor Petrov, director of forest protection centre of the Republic of Tuva (Russia), for his assistance in collecting insects in the field, as well as Dr Vlad Pet'ko (VN Sukachev Institute of Forest, Siberian Branch of the Russian Academy of Sciences, Akademgorodok, Krasnoyarsk), Ms Natalia Chevichelova (Russia) and Ms Claudia Nordmann (Department of Crop Sciences, Entomological Section, Georg-August University, Germany) for their valuable help in the indoor experiments. We very much appreciate the comments of four anonymous reviewers and the editor on a previous draft, which substantially improved the manuscript. The work was funded by Deutscher Akademischer Austauschdienst, Germany (grant No. A/06/27352); and Krasnoyarsk Regional Scientific Fund, Russia (grant No. f16G025). . - 8. - ISSN 1461-9555РУБ Entomology

Аннотация: 1 The native range of the Siberian moth extends from the Pacific Ocean (Russian Far East, Japan and Northern Korea) across Siberia, Northern China and Mongolia to the Ural Mountains. At the beginning of the 21st Century, this species was documented west of the Ural Mountains in the Republic of Mari El, indicating range extension toward the west. 2 The Siberian moth has recently been suggested for regulation as a quarantine pest for European and Mediterranean Plant Protection Organization member countries. However, no specific report on European host plants for this pest has been published so far. 3 In the present study, larval host plant choice and performance was tested for the first time on coniferous tree species that are widely distributed and of commercial value in Europe. 4 Based on dual-choice tests on neonates and mortality, developmental duration and relative growth rates of the first- to sixth-instar larvae, we found European larch Larix decidua to be the most suitable host for the moth larvae, whereas European black pine Pinus nigra and Scots pine Pinus sylvestris were the poorest hosts. The remaining conifer species tested, European silver fir Abies alba, Nordmann fir Abies nordmanniana, and Norway spruce Picea abies, were intermediate host plants. Douglas-fir Pseudotsuga menziesii, originating from North America, was chosen by the larvae to the same extend as European larch, and was also highly suitable for larval development. 5 If the moth is introduced to European countries, it will become damaging in stands of European larch and Douglas-fir, mixed stands of fir and spruce; however, it will be less damaging in forests dominated by two-needle pines. 6 We predict that Dendrolimus superans sibiricus will be able to survive and develop on the main European coniferous tree species, including non-native coniferous tree species, resulting in severe damage to large areas of forests.

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[Vidal, Stefan] Univ Gottingen, Entomol Sect, Dept Crop Sci, D-37077 Gottingen, Germany
[Kirichenko, Natalia I.] Krasnoyarsk State Trade Econ Inst, Informat Technol & Math Modelling Dept, Krasnoyarsk 660075, Russia
[Baranchikov, Yuri N.] Russian Acad Sci, Siberian Branch, Dept Forest Zool, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia

Доп.точки доступа:
Kirichenko, N.I.; Baranchikov, Y.N.; Vidal, S...; Deutscher Akademischer Austauschdienst, Germany [A/06/27352]; Krasnoyarsk Regional Scientific Fund, Russia [f16G025]

/ R. H.A. Baker [et al.] // EPPO Bulletin. - 2009. - Vol. 39, Is. 1. - P87-93, DOI 10.1111/j.1365-2338.2009.02246.x . - ISSN 0250-8052
Аннотация: PRATIQUE is an EC-funded 7th Framework research project designed to address the major challenges for pest risk analysis (PRA) in Europe. It has three principal objectives: (a) to assemble the datasets required to construct PRAs valid for the whole of the EU, (b) to conduct multi-disciplinary research that enhances the techniques used in PRA and (c) to provide a decision support scheme for PRA that is efficient and user-friendly. The research will be undertaken by scientists from 13 institutes in the EU and one each from Australia and New Zealand with subcontractors from institutes in China and Russia. They will produce a structured inventory of PRA datasets for the EU and undertake targeted research to improve existing procedures and develop new methods for (a) the assessment of economic, environmental and social impacts, (b) summarising risk while taking account of uncertainty, (c) mapping endangered areas (d) pathway risk analysis and systems approaches and (e) guiding actions during emergencies caused by outbreaks of harmful organisms. The results will be tested and provided as protocols, decision support systems and computer programs with examples of best practice linked to a computerised European and Mediterranean Plant Protection Organization (EPPO) PRA scheme. В© 2009 OEPP/EPPO.

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Держатели документа:
Central Science Laboratory, Sand Hutton, York YO30 7BH, United Kingdom
Department of Environmental Agronomy, University of Padova, 16a Via Universita, Legnaro PD, 35020, Italy
Landbouw-Economisch Instituut (LEI) B.V., 19 Burgemeester Patijnlaan, The Hague, 2585 BE, Netherlands
CABI Europe-Switzerland, 1 Rue des Grillons, Delemont, 2800, Switzerland
Centre for Environmental Policy, Imperial College London, Silwood Park, Ascot SL5 7PY, United Kingdom
European and Mediterranean Plant Protection Organization, 1 rue le Notre, Paris, 75016, France
Julius Kuhn-Institut (JKI), Bundesforschungsinstitut fur Kulturpflanzen, Messeweg 11/12, Braunschweig, 38104, Germany
University of Fribourg, 6 Chemin de Musee, Fribourgm 1700, Switzerland
Cooperative Research Centre for National Plant Biosecurity, CSIRO Entomology, 120 Meiers Road, Indooroopilly, 4068, Australia
Bio-Protection Research Centre, Lincoln University, PO Box 84, Lincoln, Canterbury, New Zealand
Plant Protection Institute, 35 Panayot Volov, Kostinbrod, 2230, Bulgaria
Wageningen University, 1 Hollandseweg, Wageningen, 6706 KN, Netherlands
Centre de Cooperation Internationale en Recherche Agronomique Pour le Developpement, UMR PVBMT, Pole de Protection des Plantes, 7 chemin de I'IRAT, Saint Pierre, Reunion, 97410, France
Institute of Botany, Academy of Sciences of the Czech Republic, Zamek 1, Prhonice, CZ 25243, Czech Republic
Faculty of Science, Department of Ecology, Charles University, Prague, Czech Republic
Institut National de la Recherche Agronomique, UR633, Zoologie Forestierem Ardon, Avenue de la Pomme de Pin, Ardon, Olivet, 45166, France
Sukachev Institute of Forest, Siberian Branch, Russian Academy of Science, Krasnoyarsk, Russian Federation
State Key Laboratory of Integrated Management of Pest Insects and Rodents, Institute of Zoology, Chinese Academy of Sciences, Beijing, China

Доп.точки доступа:
Baker, R.H.A.; Battisti, A.; Bremmer, J.; Kenis, M.; Mumford, J.; Petter, F.; Schrader, G.; Bacher, S.; De Barro, P.; Hulme, P.E.; Karadjova, O.; Lansink, A.O.; Pruvost, O.; Pyek, P.; Roques, A.; Baranchikov, Y.; Sun, J.-H.

[Text] / Y. L. Liu [et al.] // J. Geophys. Res.-Atmos. - 2015. - Vol. 120, Is. 7. - P2647-2660, DOI 10.1002/2014JD022531. - Cited References:61. - This research is supported by the NASA Land Use and Land Cover Change program (NASA-NNX09AI26G, NN-H-04-Z-YS-005-N, and NNX09AM55G); the Department of Energy (DE-FG02-08ER64599); the National Science Foundation (NSF-1028291, NSF-0919331, and AGS 0847472); and the NSF Carbon and Water in the Earth Program (NSF-0630319). D.G.M. acknowledges financial support from The Netherlands Organisation for Scientific Research (NWO) Veni grant 863.14.004. We acknowledge the Global Runoff Data Centre for the provision of the gauge station data. Runoff data in Peterson et al. [2002] were obtained from the R-ArcticNet database. A special acknowledgment is made to Brigitte Mueller and Martin Hirschi for the provision of the LandFlux-EVAL data set. Eddy covariance measurements were obtained from http://www.asianflux.com and http://gaia.agraria.unitus.it/, and meteorological station measurements were taken from ECA&D and CMA. We also acknowledge the different institutes developing and distributing the forcing climate data: University of East Anglia, ECMWF, NASA, NCEP/NCAR, and Princeton University. For model input files, source codes, and results, contact Q.Z. . - ISSN 2169-897X. - ISSN 2169-8996РУБ Meteorology & Atmospheric Sciences

Аннотация: The ecosystems in Northern Eurasia (NE) play an important role in the global water cycle and the climate system. While evapotranspiration (ET) is a critical variable to understand this role, ET over this region remains largely unstudied. Using an improved version of the Terrestrial Ecosystem Model with five widely used forcing data sets, we examine the impact that uncertainties in climate forcing data have on the magnitude, variability, and dominant climatic drivers of ET for the period 1979-2008. Estimates of regional average ET vary in the range of 241.4-335.7mmyr(-1) depending on the choice of forcing data. This range corresponds to as much as 32% of the mean ET. Meanwhile, the spatial patterns of long-term average ET across NE are generally consistent for all forcing data sets. Our ET estimates in NE are largely affected by uncertainties in precipitation (P), air temperature (T), incoming shortwave radiation (R), and vapor pressure deficit (VPD). During the growing season, the correlations between ET and each forcing variable indicate that T is the dominant factor in the north and P in the south. Unsurprisingly, the uncertainties in climate forcing data propagate as well to estimates of the volume of water available for runoff (here defined as P-ET). While the Climate Research Unit data set is overall the best choice of forcing data in NE according to our assessment, the quality of these forcing data sets remains a major challenge to accurately quantify the regional water balance in NE. Key Points

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Держатели документа:
Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA.
Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA.
Vrije Univ Amsterdam, Dept Earth Sci, Amsterdam, Netherlands.
Univ Ghent, Lab Hydrol & Water Management, B-9000 Ghent, Belgium.
China Agr Univ, Coll Resources & Environm Sci, Beijing 100094, Peoples R China.
Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA.
Univ Calif Berkeley, Lawrence Berkeley Natl Lab, Div Earth Sci, Climate Sci Dept, Berkeley, CA 94720 USA.
Michigan State Univ, CGCEO Geog, E Lansing, MI 48824 USA.
Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk, Russia.
Russian Acad Sci, Inst Forest Sci, Lab Peatland Forestry & Ameliorat, Uspenskoye, Russia.

Доп.точки доступа:
Liu, Yaling; Zhuang, Qianlai; Miralles, Diego; Pan, Zhihua; Kicklighter, David; Zhu, Qing; He, Yujie; Chen, Jiquan; Tchebakova, Nadja; Sirin, Andrey; Niyogi, Dev; Melillo, Jerry; NASA [NASA-NNX09AI26G, NN-H-04-Z-YS-005-N, NNX09AM55G]; Department of Energy [DE-FG02-08ER64599]; National Science Foundation [NSF-1028291, NSF-0919331, AGS 0847472]; NSF [NSF-0630319]; Netherlands Organisation for Scientific Research (NWO) [863.14.004]

/ D. Ovchinnikov, L. Lyu, A. Kirdyanov // International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2015. - Vol. 2: 15th International Multidisciplinary Scientific Geoconference and EXPO, SGEM 2015 (18 June 2015 through 24 June 2015, ) Conference code: 153969, Is. 3. - P491-498 . -
Аннотация: Comparison of the long tree-ring series from different regions is important to understand low frequency climate variability over large regions, but it is difficult to identify common low frequency periodicity and their causes. A Hilbert-Huang transform method (HHT) was used to exam two regional temperature sensitive tree-ring width chronologies in the northern Siberia and Altai Mountains. Seven empirical modes were calculated for each tree-ring width chronology to represent high-, mid- and low-frequency signals. A low-frequency variability have identified the common 100-200-year long cycles for the regions. The cyclicity in tree radial growth is likely to be associated with solar periodicity (Gleissberg and Suess cycles). Thus, common decrease of tree-ring radial growth in the two regions around 1700 AD is possibly a result of reduced solar activity (Maunder minimum). The use of HHT method can provide the basis to extract low frequency in climate variability for remote regions to understand better global climate change. © SGEM2015 All Rights Reserved.

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Держатели документа:
Sukachev Institute of Forest, SB RAS, Krasnoyarsk, Russian Federation
Institute of Botany, CAS, Beijing, China

Доп.точки доступа:
Ovchinnikov, D.; Lyu, L.; Kirdyanov, A.

/ U. Buntgen [et al.] // Nat. Geosci. - 2016. - Vol. 9, Is. 3. - P231-236, DOI 10.1038/ngeo2652 . - ISSN 1752-0894
Аннотация: Climatic changes during the first half of the Common Era have been suggested to play a role in societal reorganizations in Europe and Asia. In particular, the sixth century coincides with rising and falling civilizations, pandemics, human migration and political turmoil. Our understanding of the magnitude and spatial extent as well as the possible causes and concurrences of climate change during this period is, however, still limited. Here we use tree-ring chronologies from the Russian Altai and European Alps to reconstruct summer temperatures over the past two millennia. We find an unprecedented, long-lasting and spatially synchronized cooling following a cluster of large volcanic eruptions in 536, 540 and 547 AD (ref.), which was probably sustained by ocean and sea-ice feedbacks, as well as a solar minimum. We thus identify the interval from 536 to about 660 AD as the Late Antique Little Ice Age. Spanning most of the Northern Hemisphere, we suggest that this cold phase be considered as an additional environmental factor contributing to the establishment of the Justinian plague, transformation of the eastern Roman Empire and collapse of the Sasanian Empire, movements out of the Asian steppe and Arabian Peninsula, spread of Slavic-speaking peoples and political upheavals in China. © 2016 Macmillan Publishers Limited. All rights reserved.

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Держатели документа:
Swiss Federal Research Institute WSL, Birmensdorf, Switzerland
Oeschger Centre for Climate Change Research, Bern, Switzerland
Global Change Research Centre AS CR, Brno, Czech Republic
Siberian Federal University, Krasnoyarsk, Russian Federation
Department of History, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Initiative for the Science of the Human Past (SoHP), Harvard University, Cambridge, MA, United States
Institute for Advanced Study, School of Historical Studies, Princeton, NJ, United States
Paul Scherrer Institute PSI, Villigen, Switzerland
Max Planck Institute for Meteorology, Hamburg, Germany
Institute for Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, Germany
Navarino Environmental Observatory, Messinia, Greece
Department of Geography, Johannes Gutenberg University, Mainz, Germany
University of Lausanne, Institute of Earth Surface Dynamics, Lausanne, Switzerland
Department of Linguistics and Information Sciences, University of Lausanne, Lausanne, Switzerland
Department of Geography, Justus Liebig University, Giessen, Germany
Laboratory for Ion Beam Physics, ETHZ, Zurich, Switzerland
Department of Forest Growth, Albert-Ludwigs University, Freiburg, Germany
VN Sukachev Institute of Forest SB RAS, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Buntgen, U.; Myglan, V. S.; Ljungqvist, F. C.; McCormick, M.; Di Cosmo, N.; Sigl, M.; Jungclaus, J.; Wagner, S.; Krusic, P. J.; Esper, J.; Kaplan, J. O.; De Vaan, M. A.C.; Luterbacher, J.; Wacker, L.; Tegel, W.; Kirdyanov, A. V.

[Text] / D. Ovchinnikov, L. X. Lyu, A. Kirdyanov // WATER RESOURCES, FOREST, MARINE AND OCEAN ECOSYSTEMS, SGEM 2015, VOL II : STEF92 TECHNOLOGY LTD, 2015. - 15th International Multidisciplinary Scientific Geoconference (SGEM) (JUN 18-24, 2015, Albena, BULGARIA). - P491-497. - (International Multidisciplinary Scientific GeoConference-SGEM). - Cited References:15 . -
Аннотация: Comparison of the long tree-ring series from different regions is important to understand low frequency climate variability over large regions, but it is difficult to identify common low frequency periodicity and their causes. A Hilbert-Huang transform method (HHT) was used to exam two regional temperature sensitive tree-ring width chronologies in the northern Siberia and Altai Mountains. Seven empirical modes were calculated for each tree-ring width chronology to represent high-, mid-and low-frequency signals. A low-frequency variability have identified the common 100-200-year long cycles for the regions. The cyclicity in tree radial growth is likely to be associated with solar periodicity (Gleissberg and Suess cycles). Thus, common decrease of tree-ring radial growth in the two regions around 1700 AD is possibly a result of reduced solar activity (Maunder minimum). The use of HHT method can provide the basis to extract low frequency in climate variability for remote regions to understand better global climate change.

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Держатели документа:
SB RAS, Sukachev Inst Forest, Krasnoyarsk, Russia.
Chinese Acad Sci, Inst Bot, Beijing, Peoples R China.

Доп.точки доступа:
Ovchinnikov, Dmitriy; Lyu, Lixin; Kirdyanov, Alexander

[Text] / J. Esper [et al.] // Quat. Sci. Rev. - 2016. - Vol. 145. - P134-151, DOI 10.1016/j.quascirev.2016.05.009. - Cited References:123. - We thank all the tree-ring data producers for sharing their chronologies and measurement series. Supported by the German Science Foundation, Grant 161/9-1. Lamont-Doherty Earth Observatory contribution number 8019. JL acknowledges the German Science Foundation project "Attribution of forced and internal Chinese climate variability in the Common Era". VM acknowledges grant RNF 15-14-30011. BY acknowledges the National Natural Science Foundation of China (Grant 41325008). . - ISSN 0277-3791РУБ Geography, Physical + Geosciences, Multidisciplinary

Аннотация: Tree-ring chronologies are widely used to reconstruct high-to low-frequency variations in growing season temperatures over centuries to millennia. The relevance of these timeseries in large-scale climate reconstructions is often determined by the strength of their correlation against instrumental temperature data. However, this single criterion ignores several important quantitative and qualitative characteristics of tree-ring chronologies. Those characteristics are (i) data homogeneity, (ii) sample replication, (iii) growth coherence, (iv) chronology development, and (v) climate signal including the correlation with instrumental data. Based on these 5 characteristics, a reconstruction-scoring scheme is proposed and applied to 39 published, millennial-length temperature reconstructions from Asia, Europe, North America, and the Southern Hemisphere. Results reveal no reconstruction scores highest in every category and each has their own strengths and weaknesses. Reconstructions that perform better overall include N-Scan and Finland from Europe, E-Canada from North America, Yamal and Dzhelo from Asia. Reconstructions performing less well include W-Himalaya and Karakorum from Asia, Tatra and S-Finland from Europe, and Great Basin from North America. By providing a comprehensive set of criteria to evaluate tree-ring chronologies we hope to improve the development of large-scale temperature reconstructions spanning the past millennium. All reconstructions and their corresponding scores are provided at www.blogs.uni-mainz.de/fb09climatology. (C) 2016 Elsevier Ltd. All rights reserved.

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Держатели документа:
Johannes Gutenberg Univ Mainz, Dept Geog, D-55099 Mainz, Germany.
Stockholm Univ, Dept Phys Geog, S-10691 Stockholm, Sweden.
Navarino Environm Observ, Messinia, Greece.
Stockholm Univ, Dept Hist, S-10691 Stockholm, Sweden.
Stockholm Univ, Bolin Ctr Climate Res, S-10691 Stockholm, Sweden.
Univ Giessen, Dept Geog, D-35390 Giessen, Germany.
Univ Giessen, Ctr Int Dev & Environm Res, D-35390 Giessen, Germany.
Univ Padua, Dipartimento Territorio & Sistemi AgroForestali, I-35020 Legnaro, Italy.
Lamont Doherty Earth Observ, Tree Ring Lab, Palisades, NY 10964 USA.
William Paterson Univ, Dept Environm Sci, Wayne, NJ 07470 USA.
RAS, SB, Inst Forest, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Lab Ecosyst Biogeochem, Krasnoyarsk 660041, Russia.
Siberian Fed Univ, Inst Humanities, Krasnoyarsk 660041, Russia.
Nat Resources Inst Finland Luke, Rovaniemi Unit, Rovaniemi, Finland.
Swiss Fed Res Inst WSL, CH-8903 Birmensdorf, Switzerland.
Univ Arizona, Tree Ring Res Lab, Tucson, AZ 85721 USA.
CONICET Mendoza, Inst Argentino Nivol Glaciol & Ciencias Ambiental, RA-5500 Mendoza, Argentina.
Chinese Acad Sci, Key Lab Desert & Desertificat, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China.

Доп.точки доступа:
Esper, Jan; Krusic, Paul J.; Ljungqvist, Fredrik C.; Luterbacher, Juerg; Carrer, Marco; Cook, E.d.; Davi, Nicole K.; Hartl-Meier, Claudia; Kirdyanov, Alexander; Konter, Oliver; Myglan, Vladimir; Timonen, Mauri; Treydte, Kerstin; Trouet, Valerie; Villalba, Ricardo; Yang, Bao; Buntgen, Ulf; German Science Foundation [161/9-1]; National Natural Science Foundation of China [41325008]; [RNF 15-14-30011]

/ A. Chen [et al.] // Agric. Ecosyst. Environ. - 2016. - Vol. 232. - P302-311, DOI 10.1016/j.agee.2016.08.018 . - ISSN 0167-8809
Аннотация: A decrease in C inputs from the return of crop residues to soil has occurred in many regions worldwide in recent years. The effects of this decline in C inputs could provide valuable information for assessing the long-term impact of litter C inputs on soil organic C (SOC) in rice paddy soils. The present study aimed to evaluate the response of rice paddy SOC accumulation to changes in actual C inputs in subtropical China, with emphasis on the response of C accumulation to declining C inputs. For this, we used a long-term field experiment on paddy soil in a rice-rice (Oryza sativa L.) cropping system running from 1990 to 2014. The four treatments were CK (control, no fertilizer), OM (organic matter application), NPK (N, P, and K fertilizer application), and NPKOM (NPK and organic matter application). Organic matter application for the OM and NPKOM treatments included rice straw and green manure that were left in the field after harvest and chopped, along with rice residues with stubbles and roots. In all treatments, C sequestration showed an increasing trend (from 0.207 to 0.880 g kg?1 yr?1) in the early and middle stages of the experiment (1990–2006) followed by a decreasing trend (from ?0.429 to ?0.064 g kg?1 yr?1) in the late stage (2007–2014). The trends were more pronounced for the OM and NPKOM treatments than for their CK and NPK counterparts. The changes in SOC stocks were consistent with changes in C inputs (p < 0.01). During the late stage, yield and litter inputs from crop residues and green manure decreased, quickly affecting SOC stock in paddy soils. This declining trend in annual rice yields was mainly caused by the decline in first rice yields, accounting for 42.3–91.5% of the decrease in annual C inputs. Insufficient P or N and K supply and unfavorable climatic factors (decreases in sunshine duration and both maximum and minimum temperatures) are possible reasons for the decline in first rice yields and green manure biomass in the late stage. Collectively, the results suggest that C stocks in high-productivity paddy soils respond very sensitively to a decline in C inputs. This raises the risk of loss of C stock in paddy soil if, in the long run, a large return of C to soil with crop residues or by other sources, e.g., green manure, cannot be achieved. © 2016 Elsevier B.V.

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Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of SciencesHunan, China
Department of Soil Science of Temperate Ecosystems, Department of Agricultural Soil Science, University of Gottingen, Gottingen, Germany
Institute of Soil Science, Leibniz Universitat Hannover, Hannover, Germany
VN Sukachev Institute of Forest, SB-RAS, Krasnoyarsk, Russian Federation

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Chen, A.; Xie, X.; Dorodnikov, M.; Wang, W.; Ge, T.; Shibistova, O.; Wei, W.; Guggenberger, G.

/ Z. Zhu [et al.] // Biogeosciences. - 2016. - Vol. 13, Is. 15. - P4481-4489, DOI 10.5194/bg-13-4481-2016 . - ISSN 1726-4170
Аннотация: The input of recently photosynthesized C has significant implications on soil organic C sequestration, and in paddy soils, both plants and soil microbes contribute to the overall C input. In the present study, we investigated the fate and priming effect of organic C from different sources by conducting a 300-day incubation study with four different 13C-labelled substrates: rice shoots (shoot-C), rice roots (root-C), rice rhizodeposits (rhizo-C), and microbe-assimilated C (micro-C). The efflux of both 13CO2 and 13CH4 indicated that the mineralization of C in shoot-C-, root-C-, rhizo-C-, and micro-C-treated soils rapidly increased at the beginning of the incubation and decreased gradually afterwards. The highest cumulative C mineralization was observed in root-C-treated soil (45.4%), followed by shoot-C- (31.9%), rhizo-C- (7.90%), and micro-C-treated (7.70%) soils, which corresponded with mean residence times of 39.5, 50.3, 66.2, and 195 days, respectively. Shoot and root addition increased C emission from native soil organic carbon (SOC), up to 11.4 and 2.3 times higher than that of the control soil by day 20, and decreased thereafter. Throughout the incubation period, the priming effect of shoot-C on CO2 and CH4 emission was strongly positive; however, root-C did not exhibit a significant positive priming effect. Although the total C contents of rhizo-C-(1.89%) and micro-C-treated soils (1.90%) were higher than those of untreated soil (1.81%), no significant differences in cumulative C emissions were observed. Given that about 0.3 and 0.1% of the cumulative C emission were derived from labelled rhizo-C and micro-C, we concluded that the soil organic C-derived emissions were lower in rhizo-C- and micro-C-treated soils than in untreated soil. This indicates that rhizodeposits and microbe-assimilated C could be used to reduce the mineralization of native SOC and to effectively improve soil C sequestration. The contrasting behaviour of the different photosynthesized C substrates suggests that recycling rice roots in paddies is more beneficial than recycling shoots and demonstrates the importance of increasing rhizodeposits and microbe-assimilated C in paddy soils via nutrient management. © 2016 Author(s).

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Key Laboratory of Agro-ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Hunan, China
Changsha Research Station for Agricultural and Environmental Monitoring, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Hunan, China
Institute of Soil Science, Leibniz Universitat Hannover, Hannover, Germany
VN Sukachev Institute of Forest, Siberian Branch, Russian Academy of Science, Krasnoyarsk, Russian Federation
College of Resources and Environment, Southwest University, Chongqing, China

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Zhu, Z.; Zeng, G.; Ge, T.; Hu, Y.; Tong, C.; Shibistova, O.; He, X.; Wang, J.; Guggenberger, G.; Wu, J.

/ A. V. Taynik [et al.] // Dendrochronologia. - 2016. - Vol. 39: Workshop on Current Status and the Potential of Tree-Ring Research in (JAN 20-21, 2015, Krasnoyarsk, RUSSIA). - P10-16, DOI 10.1016/j.dendro.2015.12.003. - Cited References:38 . - ISSN 1125-7865. - ISSN 1612-0051РУБ Plant Sciences + Forestry + Geography, Physical

Аннотация: Tree-ring research in the Altai-Sayan Mountains so far only considered a limited number of well replicated site chronologies. The dendroecological and palaeoclimatological potential and limitations of large parts of south-central Russia therefore remain rather unexplored. Here, we present a newly updated network of 13 larch (Larix sibirica Ldb.) tree-ring width (TRW) chronologies from mid to higher elevations along a nearly 1000 km west-to-east transect across the greater Altai-Sayan region. All data were sampled between 2009 and 2014. The corresponding site chronologies cover periods from 440 to 860 years. The highest TRW agreement is found between chronologies >= 2200 m asl, whereas the material from lower elevations reveals overall less synchronized interannual to longer-term growth variability. While fluctuations in average June July temperature predominantly contribute to the growth at higher elevations, arid air masses from Mongolia mainly affect TRW formation at lower elevations. Our results are indicative for the dendroclimatological potential of the Altai-Sayan Mountains, where both, variation in summer temperature and hydroclimate can be robustly reconstructed back in time. These findings are valid for a huge region in central Asia where reliable meteorological observations are spatially scarce and temporally restricted to the second half of the 20th century. The development of new high-resolution climate reconstruction over several centuries to millennia will further appear beneficial for timely endeavors at the interface of archaeology, climatology and history. (C) 2015 Elsevier GmbH. All rights reserved.

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Siberian Fed Univ, Krasnoyarsk 660041, Russia.
Sukachev Inst Forest SB RAS, Krasnoyarsk 660036, Russia.
Tuva State Univ, Kyzyl 667000, Republic Of Tuv, Russia.
Swiss Fed Res Inst WSL, Zurcherstr 111, CH-8903 Birmensdorf, Switzerland.

Доп.точки доступа:
Taynik, Anna V.; Barinov, Valentin V.; Oidupaa, Orlan Ch.; Myglan, Vladimir S.; Reinig, Frederick; Buntgen, Ulf

/ M. He [et al.] // Dendrochronologia. - 2017. - Vol. 42. - P31-41, DOI 10.1016/j.dendro.2017.01.002 . - ISSN 1125-7865
Аннотация: Response of climate warming on tree-ring formation has attracted much attention during recent years. However, most studies are based on statistical analysis, lacking understanding of tree-physiological processes, especially in the mountainous regions of the Tibetan Plateau (TP). Herein, we firstly use an updated new version of the tree-ring process-based Vaganov-Shashkin model (VS-oscilloscope) to simulate tree-ring formation and its relationships with climate factors during the past six decades. Our analyses covered 341 sampled trees growing within elevations ranging from 2750 to 4575 m a.s.l. at five sampling sites across the TP. Simulated tree-ring width series are significantly (p < 0.01) correlated with actual tree-ring width chronologies during their common interval periods. Starting dates of tree-ring formation are determined by temperature at all five sampling sites. After the initiation of tree stem cambial activity, soil moisture content has a significant effect on tree radial growth. Ending dates of cambial activity are driven by temperature over the whole study region. Simulated results indicate differences between wide and narrow tree-rings are mostly induced by soil moisture content, especially during the first half of the growing season, when effects from temperature variations are minor. Interestingly, we detected significantly (p < 0.001) increased relative growth rates due to higher soil moisture content after the year 1985 at the five sampling sites. However, the variability of mean relative growth rates due to temperature is negligible before and after that. Based on the successful application of VS-oscilloscope modeling on the high-elevation tree stands on the TP, our study provides a new perspective on tree radial growth process and their varying relationships to climate factors during the past six decades. © 2017 Elsevier GmbH

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Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China
Mathematical Methods and Information Technology Department, Siberian Federal University, L. Prushinskoi street, 2, Krasnoyarsk, Russian Federation
V.N Sukachev Institute of Forest SB RAS, Laboratory of Tree-Ring Structure, Krasnoyarsk, Russian Federation
Institute of Geography, University of Erlangen-Nurnberg, Erlangen, Germany

Доп.точки доступа:
He, M.; Shishov, V.; Kaparova, N.; Yang, B.; Brauning, A.; Grie?inger, J.

/ N. Kirichenko [et al.] // PLoS ONE. - 2017. - Vol. 12, Is. 2, DOI 10.1371/journal.pone.0171104 . - ISSN 1932-6203
Аннотация: Knowing the phylogeographic structure of invasive species is important for understanding the underlying processes of invasion. The micromoth Phyllonorycter issikii, whose larvae damage leaves of lime trees Tilia spp., was only known from East Asia. In the last three decades, it has been recorded in most of Europe, Western Russia and Siberia. We used the mitochondrial cytochrome c oxidase subunit I (COI) gene region to compare the genetic variability of P. issikii populations between these different regions. Additionally, we sequenced two nuclear genes (28S rRNA and Histone 3) and run morphometric analysis of male genitalia to probe for the existence of cryptic species. The analysis of COI data of 377 insect specimens collected in 16 countries across the Palearctic revealed the presence of two different lineages: P. issikii and a putative new cryptic Phyllonorycter species distributed in the Russian Far East and Japan. In P. issikii, we identified 31 haplotypes among which 23 were detected in the invaded area (Europe) and 10 were found in its putative native range in East Asia (Russian Far East, Japan, South Korea and China), with only two common haplotypes. The high number of haplotypes found in the invaded area suggest a possible scenario of multiple introductions. One haplotype H1 was dominant (119 individuals, 67.2%), not only throughout its expanding range in Europe and Siberia but, intriguingly, also in 96% of individuals originating from Japan. We detected eight unique haplotypes of P. issikii in East Asia. Five of them were exclusively found in the Russian Far East representing 95% of individuals from that area. The putative new cryptic Phyllonorycter species showed differences from P. issikii for the three studied genes. However, both species are morphologically undistinguishable. They occur in sympatry on the same host plants in Japan (Sendai) and the Russian Far East (Primorsky krai) without evidence of admixture. © 2017 Kirichenko et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

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Sukachev Institute of Forest SB RAS, Federal Research Center Krasnoyarsk Science Center SB RAS, Krasnoyarsk, Russian Federation
Siberian Federal University, Krasnoyarsk, Russian Federation
INRA, UR0633 Zoologie Forestiere, Orleans, France
Museo Civico di Storia Naturale, Verona, Italy
Department of Life and Environmental Sciences, Kyoto Prefectural University, Kyoto, Japan
UMR CBGP (INRA, CIRAD, IRD, SupAgro), Montpellier, France
Department of Biological Science and Biotechnology, Hannam University, Daejeon, South Korea
College of Life Sciences, Nankai University, Tianjin, China
Institut de Recherche sur la Biologie de l'Insecte, CNRS UMR 7261, Universite Francois-Rabelais de Tours, UFR Sciences et Techniques, Tours, France

Доп.точки доступа:
Kirichenko, N.; Triberti, P.; Ohshima, I.; Haran, J.; Byun, B. -K.; Li, H.; Augustin, S.; Roques, A.; Lopez-Vaamonde, C.

/ S. Guillet [et al.] // Nat. Geosci. - 2017. - Vol. 10, Is. 2. - P123-+, DOI 10.1038/NGEO2875. - Cited References:45. - S.G., C.C., M.S. and O.V.C. acknowledge support from the Era.Net RUSplus project ELVECS (SNF project number: IZRPZ0_164735). This study benefited from data gathered within the ANR CEPS GREENLAND project. V.S.M. received support from the Russian Science Foundation (project no. 15-14-30011). R. Hantemirov kindly provided a millennium-long chronology. The authors are grateful to W. S. Atwell and W. Wayne-Farris for discussions on historical sources from Japan as well as to M. Luisa Avila for her help with Muslim sources from Mediaeval Spain. S.G. and C.C. are very grateful to S. Finet, L. Fazan and P. Guerin for their help with R-scripts, translations and fruitful discussions, respectively. . - ISSN 1752-0894. - ISSN 1752-0908РУБ Geosciences, Multidisciplinary

Аннотация: The eruption of Samalas in Indonesia in 1257 ranks among the largest sulfur-rich eruptions of the Common Era with sulfur deposition in ice cores reaching twice the volume of the Tambora eruption in 1815. Sedimentological analyses of deposits confirm the exceptional size of the event, which had both an eruption magnitude and a volcanic explosivity index of 7. During the Samalas eruption, more than 40 km(3) of dense magma was expelled and the eruption column is estimated to have reached altitudes of 43 km. However, the climatic response to the Samalas event is debated since climate model simulations generally predict a stronger and more prolonged surface air cooling of Northern Hemisphere summers than inferred from tree-ring-based temperature reconstructions. Here, we draw on historical archives, ice-core data and tree-ring records to reconstruct the spatial and temporal climate response to the Samalas eruption. We find that 1258 and 1259 experienced some of the coldest Northern Hemisphere summers of the past millennium. However, cooling across the Northern Hemisphere was spatially heterogeneous. Western Europe, Siberia and Japan experienced strong cooling, coinciding with warmer-than-average conditions over Alaska and northern Canada. We suggest that in North America, volcanic radiative forcing was modulated by a positive phase of the El Nino-Southern Oscillation. Contemporary records attest to severe famines in England and Japan, but these began prior to the eruption. We conclude that the Samalas eruption aggravated existing crises, but did not trigger the famines.

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Univ Bern, Inst Geol Sci, Dendrolab Ch, Baltzerstr 1 3, CH-3012 Bern, Switzerland.
Univ Blaise Pascal, CNRS, UMR 6042, Geolab, 4 Rue Ledru, F-63057 Clermont Ferrand, France.
Univ Geneva, Inst Environm Sci, Climat Change & Climate Impacts, 66 Blvd Carl Vogt, CH-1205 Geneva, Switzerland.
Univ Geneva, Dept Earth Sci, Rue Maraichers 13, CH-1205 Geneva, Switzerland.
Univ Paris 06, Lab Oceanog & Climat Expt Approches Numer, 4 Pl Jussieu, F-75252 Paris 05, France.
Univ Paris 1 Pantheon Sorbonne, Lab Geog Phys, 1 Pl Aristide Briand, F-92195 Meudon, France.
Univ Reading, Dept Meteorol, NCAS Climate, Reading RG6 6BB, Berks, England.
UR ETNA Univ Grenoble Alpes, Irstea, 2 Rue Papeterie, F-38402 St Martin Dheres, France.
Univ Paris Saclay, Lab Sci Climat & Environm, Inst Pierre Simon Laplace, CEA,CNRS,UVSQ,UMR8212, F-91191 Gif Sur Yvette, France.
VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, RU-660041 Krasnoyarsk, Russia.
William Paterson Univ, Dept Environm Sci, Wayne, NJ 07470 USA.
Univ Arizona, Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA.
CNRS, UMR 7299, CCJ, Maison Mediterraneenne Sci Homme 5 Rue Chateau, F-13094 Aix En Provence, France.
Chinese Acad Sci, Inst Geog Sci & Nat Resources, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China.
Chinese Acad Sci, Ctr Excellence & Innovat Tibetan Plateau Earth Sy, Beijing 100101, Peoples R China.
Univ Western Ontario, Dept Geog, 1151 Richmond St, London, ON N6A 5C2, Canada.
Aix Marseille Univ, CNRS, IRD, Coll France,CEREGE,ECCOREV, F-13545 Aix En Provence, France.
Univ Cambridge, Dept Geog, Downing Pl, Cambridge CB2 3EN, England.

Доп.точки доступа:
Guillet, Sebastien; Corona, Christophe; Stoffel, Markus; Khodri, Myriam; Lavigne, Franck; Ortega, Pablo; Eckert, Nicolas; Sielenou, Pascal Dkengne; Daux, Valerie; Churakova, O. V.; Davi, Nicole; Edouard, Jean-Louis; Zhang, Yong; Luckman, Brian H.; Myglan, Vladimir S.; Guiot, Joel; Beniston, Martin; Masson-Delmotte, Valerie; Oppenheimer, Clive; Era.Net RUSplus project ELVECS (SNF) [IZRPZ0_164735]; Russian Science Foundation [15-14-30011]