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

[Text] / B. . Wild [et al.] // Soil Biol. Biochem. - 2014. - Vol. 75. - P143-151, DOI 10.1016/j.soilbio.2014.04.014. - Cited References: 47. - This study was funded by the Austrian Science Fund (FWF) as part of the International Program CryoCARB (Long-term Carbon Storage in Cryoturbated Arctic Soils; FWF - I370-B17). . - ISSN 0038-0717РУБ Soil Science

Аннотация: Rising temperatures in the Arctic can affect soil organic matter (SOM) decomposition directly and indirectly, by increasing plant primary production and thus the allocation of plant-derived organic compounds into the soil. Such compounds, for example root exudates or decaying fine roots, are easily available for microorganisms, and can alter the decomposition of older SUM ("priming effect"). We here report on a SUM priming experiment in the active layer of a permafrost soil from the central Siberian Arctic, comparing responses of organic topsoil, mineral subsoil, and cryoturbated subsoil material (i.e., poorly decomposed topsoil material subducted into the subsoil by freeze-thaw processes) to additions of C-13-labeled glucose, cellulose, a mixture of amino acids, and protein (added at levels corresponding to approximately 1% of soil organic carbon). SUM decomposition in the topsoil was barely affected by higher availability of organic compounds, whereas SUM decomposition in both subsoil horizons responded strongly. In the mineral subsoil, SUM decomposition increased by a factor of two to three after any substrate addition (glucose, cellulose, amino acids, protein), suggesting that the microbial decomposer community was limited in energy to break down more complex components of SOM. In the cryoturbated horizon, SUM decomposition increased by a factor of two after addition of amino acids or protein, but was not significantly affected by glucose or cellulose, indicating nitrogen rather than energy limitation. Since the stimulation of SUM decomposition in cryoturbated material was not connected to microbial growth or to a change in microbial community composition, the additional nitrogen was likely invested in the production of extracellular enzymes required for SUM decomposition. Our findings provide a first mechanistic understanding of priming in permafrost soils and suggest that an increase in the availability of organic carbon or nitrogen, e.g., by increased plant productivity, can change the decomposition of SUM stored in deeper layers of permafrost soils, with possible repercussions on the global climate. (C) 2014 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/3.0/).

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Держатели документа:
[Wild, Birgit
Schnecker, Joerg
Watzka, Margarete
Richter, Andreas] Univ Vienna, Dept Microbiol & Ecosyst Sci, Div Terr Ecosyst Res, Vienna, Austria
[Wild, Birgit
Schnecker, Joerg
Alves, Ricardo J. Eloy
Gittel, Antje
Urich, Tim
Richter, Andreas] Austrian Polar Res Inst, Vienna, Austria
[Alves, Ricardo J. Eloy
Urich, Tim] Univ Vienna, Dept Ecogen & Syst Biol, Div Archaea Biol & Ecogen, Vienna, Austria
[Barsukov, Pavel
Shibistova, Olga] Russian Acad Sci, Siberian Branch, Inst Soil Sci & Agrochem, Novosibirsk, Russia
[Barta, Jiri
Capek, Petr
Santruckova, Hana] Univ South Bohemia, Dept Ecosyst Biol, Ceske Budejovice, Czech Republic
[Gentsch, Norman
Guggenberger, Georg
Mikutta, Robert
Shibistova, Olga] Leibniz Univ Hannover, Inst Soil Sci, D-30167 Hannover, Germany
[Gittel, Antje] Univ Bergen, Ctr Geobiol, Dept Biol, Bergen, Norway
[Lashchinskiy, Nikolay] Russian Acad Sci, Siberian Branch, Cent Siberian Bot Garden, Novosibirsk, Russia
[Shibistova, Olga
Zrazhevskaya, Galina] Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia
ИЛ СО РАН

Доп.точки доступа:
Wild, B...; Schnecker, J...; Alves, RJE; Barsukov, P...; Barta, J...; Capek, P...; Gentsch, N...; Gittel, A...; Guggenberger, G...; Lashchinskiy, N...; Mikutta, R...; Rusalimova, O...; Santruckova, H...; Shibistova, O...; Urich, T...; Watzka, M...; Zrazhevskaya, G...; Richter, A...; Austrian Science Fund (FWF) as part of the International Program CryoCARB [FWF - I370-B17]

/ P. Capek [et al.] // Soil Biol. Biochem. - 2015. - Vol. 90. - P19-29, DOI 10.1016/j.soilbio.2015.07.013 . - ISSN 0038-0717
Аннотация: Arctic permafrost soils contain large stocks of organic carbon (OC). Extensive cryogenic processes in these soils cause subduction of a significant part of OC-rich topsoil down into mineral soil through the process of cryoturbation. Currently, one-fourth of total permafrost OC is stored in subducted organic horizons. Predicted climate change is believed to reduce the amount of OC in permafrost soils as rising temperatures will increase decomposition of OC by soil microorganisms. To estimate the sensitivity of OC decomposition to soil temperature and oxygen levels we performed a 4-month incubation experiment in which we manipulated temperature (4-20 °C) and oxygen level of topsoil organic, subducted organic and mineral soil horizons. Carbon loss (CLOSS) was monitored and its potential biotic and abiotic drivers, including concentrations of available nutrients, microbial activity, biomass and stoichiometry, and extracellular oxidative and hydrolytic enzyme pools, were measured. We found that independently of the incubation temperature, CLOSS from subducted organic and mineral soil horizons was one to two orders of magnitude lower than in the organic topsoil horizon, both under aerobic and anaerobic conditions. This corresponds to the microbial biomass being lower by one to two orders of magnitude. We argue that enzymatic degradation of autochthonous subducted OC does not provide sufficient amounts of carbon and nutrients to sustain greater microbial biomass. The resident microbial biomass relies on allochthonous fluxes of nutrients, enzymes and carbon from the OC-rich topsoil. This results in a "negative priming effect", which protects autochthonous subducted OC from decomposition at present. The vulnerability of subducted organic carbon in cryoturbated arctic soils under future climate conditions will largely depend on the amount of allochthonous carbon and nutrient fluxes from the topsoil. © 2015 Elsevier Ltd.

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Держатели документа:
University of South Bohemia, Department of Ecosystems Biology, Branisovska 31, Ceske Budejovice, Czech Republic
Institute of Systematic Botany and Ecology, University of Ulm, Albert-Einstein-Allee 11, Ulm, Germany
University of Vienna, Department of Microbiology and Ecosystem Research, Division of Terrestrial Ecosystem Research, Althanstrasse 14, Vienna, Austria
Austrian Polar Research Institute, Althanstrasse 14, Vienna, Austria
University of Gothenburg, Department of Earth Sciences, Guldhedsgatan 5A, Gothenburg, Sweden
University of New Hampshire, Department of Natural Resources and the Environment, Durham, NH, United States
University of Vienna, Department of Ecogenomics and Systems Biology, Division of Archaea Biology and Ecogenomics, Vienna, Austria
Leibniz Universitat Hannover, Institute of Soil Science, Herrenhauser Strasse 2, Hannover, Germany
Martin-Luther-University Halle-Wittenberg, Soil Sciences, Halle, Germany
University of Stockholm, Department of Physical Geography, Stockholm, Sweden
Central Siberian Botanical Garden, Siberian Branch of the Russian Academy of Sciences, St. Zolotodolinskaya 101, Novosibirsk, Russian Federation
University of Bergen, Department of Biology, Centre for Geobiology, Thormohlensgate 53B, Bergen, Norway
Center for Geomicrobiology, Department of Bioscience, Ny Munkegade 114, Aarhus C, Denmark
VN Sukachev, Institute of Forest, Siberian Branch of the Russian Academy of Sciences, Akademgorodok, Krasnoyarsk, Russian Federation
University of Greifswald, Institute for Microbiology, Greifswald, Germany

Доп.точки доступа:
Capek, P.; Diakova, K.; Dickopp, J.-E.; Barta, J.; Wild, B.; Schnecker, J.; Alves, R.J.E.; Aiglsdorfer, S.; Guggenberger, G.; Gentsch, N.; Hugelius, G.; Lashchinsky, N.; Gittel, A.; Schleper, C.; Mikutta, R.; Palmtag, J.; Shibistova, O.; Urich, .; Richter, A.; Santruckova, H.

[Text] / B. Wild [et al.] // Sci Rep. - 2016. - Vol. 6. - Ст. 25607, DOI 10.1038/srep25607. - Cited References:52. - This study is part of the CryoCARB project (Long-term Carbon Storage in Cryoturbated Arctic Soils), and co-funded by the Austrian Science Fund (FWF): I370-B17, the German Federal Ministry of Education and Research (03F0616A), the Czech Ministry of Education, Youth and Sports (MSM 7E10073 - CryoCARB), the Russian Ministry of Education and Science (No. 14.25.31.0031), the Swedish Research Council (824-2009-77357), and the Norwegian Research Fund (NFR): NFR-200411. . - ISSN 2045-2322РУБ Multidisciplinary Sciences

Аннотация: Arctic ecosystems are warming rapidly, which is expected to promote soil organic matter (SOM) decomposition. In addition to the direct warming effect, decomposition can also be indirectly stimulated via increased plant productivity and plant-soil C allocation, and this so called "priming effect" might significantly alter the ecosystem C balance. In this study, we provide first mechanistic insights into the susceptibility of SOM decomposition in arctic permafrost soils to priming. By comparing 119 soils from four locations across the Siberian Arctic that cover all horizons of active layer and upper permafrost, we found that an increased availability of plant-derived organic C particularly stimulated decomposition in subsoil horizons where most of the arctic soil carbon is located. Considering the 1,035 Pg of arctic soil carbon, such an additional stimulation of decomposition beyond the direct temperature effect can accelerate net ecosystem C losses, and amplify the positive feedback to global warming.

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Держатели документа:
Univ Vienna, Dept Microbiol & Ecosyst Sci, Vienna, Austria.
Austrian Polar Res Inst, Vienna, Austria.
Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden.
Leibniz Univ Hannover, Inst Soil Sci, D-30167 Hannover, Germany.
Univ South Bohemia, Dept Ecosyst Biol, Ceske Budejovice, Czech Republic.
Univ Vienna, Dept Ecogen & Syst Biol, Vienna, Austria.
Univ Bergen, Dept Biol, Ctr Geobiol, Bergen, Norway.
Ctr Geomicrobiol, Dept Biosci, Aarhus, Denmark.
Stockholm Univ, Dept Phys Geog, S-10691 Stockholm, Sweden.
Russian Acad Sci, Siberian Branch, Cent Siberian Bot Garden, Novosibirsk, Russia.
Univ Halle Wittenberg, Soil Sci & Soil Protect, D-06108 Halle, Saale, Germany.
Univ New Hampshire, Dept Nat Resources & Environm, Durham, NH 03824 USA.
Russian Acad Sci, Siberian Branch, VN Sukachev Inst Forest, Krasnoyarsk, Russia.
Univ Lancaster, Lancaster Environm Ctr, Lancaster, England.
Ernst Moritz Arndt Univ Greifswald, Inst Microbiol, Greifswald, Germany.

Доп.точки доступа:
Wild, Birgit; Gentsch, Norman; Capek, Petr; Diakova, Katerina; Alves, Ricardo J. Eloy; Barta, Jiri; Gittel, Antje; Hugelius, Gustaf; Knoltsch, Anna; Kuhry, Peter; Lashchinskiy, Nikolay; Mikutta, Robert; Palmtag, Juri; Schleper, Christa; Schnecker, Joerg; Shibistova, Olga; Takriti, Mounir; Torsvik, Vigdis L.; Urich, Tim; Watzka, Margarete; Santruckova, Hana; Guggenberger, Georg; Richter, Andreas; CryoCARB project (Long-term Carbon Storage in Cryoturbated Arctic Soils); Austrian Science Fund (FWF) [I370-B17]; German Federal Ministry of Education and Research [03F0616A]; Czech Ministry of Education, Youth and Sports (MSM) [7E10073]; Russian Ministry of Education and Science [14.25.31.0031]; Swedish Research Council [824-2009-77357]; Norwegian Research Fund (NFR) [NFR-200411]

/ 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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Держатели документа:
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

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

/ Z. Zhu [et al.] // Soil Biol. Biochem. - 2018. - Vol. 121. - P67-76, DOI 10.1016/j.soilbio.2018.03.003 . - ISSN 0038-0717
Аннотация: Nitrogen (N) and phosphorus (P) availability plays a crucial role in carbon (C) cycling in terrestrial ecosystems. However, the C:N:P stoichiometric regulation of microbial mineralization of plant residues and its impact on the soil priming effect (PE), measured as CO2 and CH4 emission, in paddy soils remain unclear. In this study, the effect of soil C:N:P stoichiometry (regulated by the application of N and P fertilizers) on the mineralization of 13C-labelled rice straw and the subsequent PE was investigated in a 100-day incubation experiment in flooded paddy soil. N and P additions increased straw mineralization by approximately 25% and 10%, respectively. Additions of both N and P led to higher CO2 efflux, but lower CH4 emission. With an increase in the ratios of DOC:NH4 +-N, DOC:Olsen P, and microbial biomass C:N, 13CO2 efflux increased exponentially to a maximum. Compared with sole straw addition, exclusive N addition led to a weaker PE for CO2 emission, whereas exclusive P addition induced a stronger PE for CO2 emission. In contrast, CH4 emitted from native soil organic matter (SOM) was reduced by 7.4% and 46.1% following P and NP application, respectively. Structural equation models suggest that available N had dominant and direct positive effects, whereas microbial biomass stoichiometry mainly exerted negative indirect effects on PE. The stoichiometry of soil enzyme activity directly down-regulated CH4 emission from SOM. Microbes obviously regulate soil C turnover via stoichiometric flexibility to maintain an elemental stoichiometric balance between resources and microbial requirements. The addition of straw in combination with N and P fertilization in paddy soils could therefore meet microbial stoichiometric requirements and regulate microbial activity and extracellular enzyme production, resulting in co-metabolism of fresh C and native SOM. © 2018 Elsevier Ltd

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Держатели документа:
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 and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, China
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
Institute of Soil Science, Leibniz Universitat Hannover, Hannover, Germany
VN Sukachev Institute of Forest, SB-RAS, Krasnoyarsk, Russian Federation

Доп.точки доступа:
Zhu, Z.; Ge, T.; Luo, Y.; Liu, S.; Xu, X.; Tong, C.; Shibistova, O.; Guggenberger, G.; Wu, J.

/ Y. H. Liu [et al.] // Appl. Soil Ecol. - 2018. - Vol. 127. - P51-57, DOI 10.1016/j.apsoil.2018.02.012. - Cited References:53. - This study was financially supported by the National Key Research and Development program (2016YFD0300902), the National Natural Science Foundation of China (41522107; 41671253; 31470629), Chinese Academy of Sciences President's International Fellowship Initiative to Georg Guggenberger (2018VCA0031) and Youth Innovation Team Project of ISA, CAS (2017QNCXTD_GTD). We also thank to Public Service Technology Center, Institute of Subtropical Agriculture, Chinese Academy of Sciences for the technique support and Jiangxi Normal University domestic (abroad) visit programs funded support. . - ISSN 0929-1393. - ISSN 1873-0272РУБ Soil Science

Аннотация: Paddy soils have experienced intensive fertilization in recent decades. However, our understanding of the effects of fertilization on the carbon (C) cycle remains incomplete. In the present study, we investigated soil organic matter (SOM) decomposition in a 60-day incubation in response to N, P, K, Ca, and S addition to nutrient-limited paddy soil at three low and three high concentrations. High levels of nutrient addition decreased CO2 emission, qCO(2), and microbial biomass. CO2 emissions increased (12-17%) owing to low levels of nutrient addition, whereas it decreased (3-21%) in response to high levels of nutrient addition. Microbial biomass and nutrient turnover rates increased after low levels of nutrient addition. Positive priming effect occurs under nutrient-limited conditions owing to the stimulation of microbial biomass production after low amount of exogenous nutrient input. In contrast, high levels of nutrient addition decreased microbial biomass and net N mineralization. This high N, P, K, Ca, and S addition could satisfy the needs of microbial growth, thereby decreasing the dependency of the organisms on the original nutrients from SOM decomposition. Therefore, negative priming was observed after high-level nutrient addition. In conclusion, intensive fertilization (with N, P, K, Ca, and S) reduces SOM decomposition through increased microbial turnover in paddy soils, which might positively affect C sequestration.

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Jiangxi Normal Univ, Coll Life Sci, Nanchang 330022, Jiangxi, Peoples R China.
Chinese Acad Sci, Key Lab Agroecol Proc Subtrop Reg, Inst Subtrop Agr, Beijing 410125, Hunan, Peoples R China.
Chinese Acad Sci, Changsha Res Stn Agr & Environm Monitoring, Inst Subtrop Agr, Beijing 410125, Hunan, Peoples R China.
Univ Goettingen, Dept Agr Soil Sci, Dept Soil Sci Temperate Ecosyst, D-37077 Gottingen, Germany.
Cent South Univ Forestry & Technol, Coll Environm Sci & Engn, Changsha 410004, Hunan, Peoples R China.
Leibniz Univ Hannover, Inst Soil Sci, D-30419 Hannover, Germany.
SB RAS, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Liu, Yuhuai; Zang, Huadong; Ge, Tida; Bai, Jing; Lu, Shunbao; Zhou, Ping; Peng, Peiqing; Shibistova, Olga; Zhu, Zhenke; Wu, Jinshui; Guggenberger, Georg; National Key Research and Development program [2016YFD0300902]; National Natural Science Foundation of China [41522107, 41671253, 31470629]; Chinese Academy of Sciences President's International Fellowship Initiative [2018VCA0031]; Youth Innovation Team Project of ISA, CAS [2017QNCXTD_GTD]; Jiangxi Normal University domestic (abroad) visit programs

/ J. Cui, Z. Zhu, X. Xu [et al.] // Soil Biol. Biochem. - 2020. - Vol. 142. - Ст. 107720, DOI 10.1016/j.soilbio.2020.107720 . - ISSN 0038-0717
Аннотация: The impact of increasing amounts of labile C input on priming effects (PE) on soil organic matter (SOM) mineralization remains unclear, particularly under anoxic conditions and under high C input common in microbial hotspots. PE and their mechanisms were investigated by a 60-day incubation of three flooded paddy soils amended with13C-labeled glucose equivalent to 50–500% of microbial biomass C (MBC). PE (14–55% of unamended soil) peaked at moderate glucose addition rates (i.e., 50–300% of MBC). Glucose addition above 300% of MBC suppressed SOM mineralization but intensified microbial N acquisition, which contradicted the common PE mechanism of accelerating SOM decomposition for N-supply (frequently termed as “N mining”). Particularly at glucose input rate higher than 3 g kg?1 (i.e., 300–500% of MBC), mineral N content dropped on day 2 close to zero (1.1–2.5 mg N kg?1) because of microbial N immobilization. To cope with the N limitation, microorganisms greatly increased N-acetyl glucosaminidase and leucine aminopeptidase activities, while SOM decomposition decreased. Several discrete peaks of glucose-derived CO2 (contributing >80% to total CO2) were observed between days 13–30 under high glucose input (300–500% of MBC), concurrently with CH4 peaks. Such CO2 dynamics was distinct from the common exponential decay pattern, implicating the recycling and mineralization of 13C-enriched microbial necromass driven by glucose addition. Therefore, N recycling from necromass was hypothesized as a major mechanism to alleviate microbial N deficiency without SOM priming under excess labile C input. Compound-specific 13C-PLFA confirmed the redistribution of glucose-derived C among microbial groups, i.e., necromass recycling. Following glucose input, more than 4/5 of total 13C-PLFA was in the gram-negative and some non-specific bacteria, suggesting these microorganisms as r-strategists capable of rapidly utilizing the most labile C. However, their 13C-PLFA content decreased by 70% after 60 days, probably as a result of death of these r-strategists. On the contrary, the 13C-PLFA in gram-positive bacteria, actinomycetes and fungi (K-strategists) was initially minimal but increased by 0.5–5 folds between days 2 and 60. Consequently, the necromass of dead r-strategists provided a high-quality C–N source to the K-strategists. We conclude that under severe C excess, N recycling from necromass is a much more efficient microbial strategy to cover the acute N demand than N acquisition from the recalcitrant SOM. © 2020 Elsevier Ltd

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Держатели документа:
Key Laboratory of Agro-ecological Processes in Subtropical Region & Changsha Research Station for Agricultural and Environmental Monitoring, Institute of Subtropical Agriculture, Chinese Academy of Sciences, Hunan, 410125, China
State Key Laboratory of Organic Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Gongdong, 510640, China
Jiangsu Provincial Key Laboratory for Bioresources of Coastal Saline Soils, Jiangsu Coastal Biological Agriculture Synthetic Innovation Center, Yancheng Teachers' University, Yancheng, 224002, China
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China
School of Environment, Natural Resources & Geography, Bangor University, Gwynedd, LL57 2UW, United Kingdom
Department of Agricultural Soil Science, Department of Soil Science of Temperate Ecosystems, University of G?ttingen, G?ttingen, Germany
Institute of Environmental Sciences, Kazan Federal University, Kazan, 420049, Russian Federation
Agro-Technological Institute, RUDN University, Moscow, 117198, Russian Federation
Departamento de Ciencias Quimicas y Recursos Naturales, Universidad de La Frontera, Temuco, Chile
VN Sukachev Institute of Forest, SB-RAS, Krasnoyarsk, 660036, Russian Federation

Доп.точки доступа:
Cui, J.; Zhu, Z.; Xu, X.; Liu, S.; Jones, D. L.; Kuzyakov, Y.; Shibistova, O.; Wu, J.; Ge, T.

/ J. Cui, Z. K. Zhu, X. L. Xu [et al.] // Soil Biol. Biochem. - 2020. - Vol. 142. - Ст. 107720, DOI 10.1016/j.soilbio.2020.107720. - Cited References:80. - The study was supported by the National Key Research and Development Program of China (2017YFD0800104), the National Natural Science Foundation of China (41430860, 41771337, 41977093 and 31872695), State Key Laboratory of Organic Geochemistry, GIGCAS (SKLOG-201728), Hunan Province Base for Scientific and Technological Innovation Cooperation (2018WK4012), the Youth Innovation Team Project of Institute of Subtropical Agriculture, Chinese Academy of Sciences (2017QNCXTD_GTD), NSFC-RFBR joint project (N 19-54-53026) and Innovation Groups of National Natural Science Foundation of Hunan Province (2019JJ10003). We thank the Public Service Technology Center, Institute of Subtropical Agriculture, Chinese Academy of Sciences for technical assistance. The publication was supported by the Government Program of Competitive Growth of Kazan Federal University and with the support of the "RUDN University program 5-100." . - ISSN 0038-0717РУБ Soil Science

Аннотация: The impact of increasing amounts of labile C input on priming effects (PE) on soil organic matter (SOM) mineralization remains unclear, particularly under anoxic conditions and under high C input common in microbial hotspots. PE and their mechanisms were investigated by a 60-day incubation of three flooded paddy soils amended with(13)C-labeled glucose equivalent to 50-500% of microbial biomass C (MBC). PE (14-55% of unamended soil) peaked at moderate glucose addition rates (i.e., 50-300% of MBC). Glucose addition above 300% of MBC suppressed SOM mineralization but intensified microbial N acquisition, which contradicted the common PE mechanism of accelerating SOM decomposition for N-supply (frequently termed as "N mining"). Particularly at glucose input rate higher than 3 g kg(-1) (i.e., 300-500% of MBC), mineral N content dropped on day 2 close to zero (1.1-2.5 mg N kg(-1)) because of microbial N immobilization. To cope with the N limitation, microorganisms greatly increased N-acetyl glucosaminidase and leucine aminopeptidase activities, while SOM decomposition decreased. Several discrete peaks of glucose-derived CO2 (contributing >80% to total CO2) were observed between days 13-30 under high glucose input (300-500% of MBC), concurrently with CH4 peaks. Such CO2 dynamics was distinct from the common exponential decay pattern, implicating the recycling and mineralization of C-13-enriched microbial necromass driven by glucose addition. Therefore, N recycling from necromass was hypothesized as a major mechanism to alleviate microbial N deficiency without SOM priming under excess labile C input. Compound-specific C-13-PLFA confirmed the redistribution of glucose-derived C among microbial groups, i.e., necromass recycling. Following glucose input, more than 4/5 of total C-13-PLFA was in the gram-negative and some non-specific bacteria, suggesting these microorganisms as r-strategists capable of rapidly utilizing the most labile C. However, their C-13-PLFA content decreased by 70% after 60 days, probably as a result of death of these r-strategists. On the contrary, the C-13-PLFA in gram-positive bacteria, actinomycetes and fungi (K-strategists) was initially minimal but increased by 0.5-5 folds between days 2 and 60. Consequently, the necromass of dead r-strategists provided a high-quality C-N source to the K-strategists. We conclude that under severe C excess, N recycling from necromass is a much more efficient microbial strategy to cover the acute N demand than N acquisition from the recalcitrant SOM.

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Держатели документа:
Chinese Acad Sci, Inst Subtrop Agr, Key Lab Agroecol Proc Subtrop Reg, Changsha 410125, Hunan, Peoples R China.
Chinese Acad Sci, Inst Subtrop Agr, Changsha Res Stn Agr & Environm Monitoring, Changsha 410125, Hunan, Peoples R China.
Chinese Acad Sci, State Key Lab Organ Geochem, Guangzhou Inst Geochem, Gongdong 510640, Peoples R China.
Yancheng Teachers Univ, Jiangsu Prov Key Lab Bioresources Coastal Saline, Jiangsu Coastal Biol Agr Synthet Innovat Ctr, Yancheng 224002, Peoples R China.
Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China.
Bangor Univ, Sch Environm Nat Resources & Geog, Bangor LL57 2UW, Gwynedd, Wales.
Univ Gottingen, Dept Agr Soil Sci, Dept Soil Sci Temperate Ecosyst, Gottingen, Germany.
Kazan Fed Univ, Inst Environm Sci, Kazan 420049, Russia.
RUDN Univ, Agrotechnol Inst, Moscow 117198, Russia.
Univ La Frontera, Dept Ciencias Quim & Recursos Nat, Temuco, Chile.
RAS, SB, VN Sukachev Inst Forest, Krasnoyarsk 660036, Russia.

Доп.точки доступа:
Cui, Jun; Zhu, Zhenke; Xu, Xingliang; Liu, Shoulong; Jones, Davey L.; Kuzyakov, Yakov; Shibistova, Olga; Wu, Jinshui; Ge, Tida; National Key Research and Development Program of China [2017YFD0800104]; National Natural Science Foundation of ChinaNational Natural Science Foundation of China [41430860, 41771337, 41977093, 31872695]; State Key Laboratory of Organic Geochemistry, GIGCAS [SKLOG-201728]; Hunan Province Base for Scientific and Technological Innovation Cooperation [2018WK4012]; Youth Innovation Team Project of Institute of Subtropical Agriculture, Chinese Academy of Sciences [2017QNCXTD_GTD]; NSFC-RFBR joint project [N 19-54-53026]; Innovation Groups of National Natural Science Foundation of Hunan Province [2019JJ10003]; Government Program of Competitive Growth of Kazan Federal University; RUDN University program 5-100

/ F. Keuper, B. Wild, M. Kummu [et al.] // Nat. Geosci. - 2020, DOI 10.1038/s41561-020-0607-0 . - Article in press. - ISSN 1752-0894
Аннотация: As global temperatures continue to rise, a key uncertainty of climate projections is the microbial decomposition of vast organic carbon stocks in thawing permafrost soils. Decomposition rates can accelerate up to fourfold in the presence of plant roots, and this mechanism—termed the rhizosphere priming effect—may be especially relevant to thawing permafrost soils as rising temperatures also stimulate plant productivity in the Arctic. However, priming is currently not explicitly included in any model projections of future carbon losses from the permafrost area. Here, we combine high-resolution spatial and depth-resolved datasets of key plant and permafrost properties with empirical relationships of priming effects from living plants on microbial respiration. We show that rhizosphere priming amplifies overall soil respiration in permafrost-affected ecosystems by ~12%, which translates to a priming-induced absolute loss of ~40 Pg soil carbon from the northern permafrost area by 2100. Our findings highlight the need to include fine-scale ecological interactions in order to accurately predict large-scale greenhouse gas emissions, and suggest even tighter restrictions on the estimated 200 Pg anthropogenic carbon emission budget to keep global warming below 1.5 °C. © 2020, The Author(s), under exclusive licence to Springer Nature Limited.

Scopus

Держатели документа:
BioEcoAgro Joint Research Unit, INRAE, Barenton-Bugny, France
Climate Impacts Research Centre, Department of Ecology and Environmental Science, Umea University, Abisko, Sweden
Department of Environmental Science, Stockholm University, Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden
Water and Development Research Group, Aalto University, Espoo, Finland
Institute of Soil Science, Department of Earth Sciences, Universitat Hamburg, Hamburg, Germany
Center for Earth System Research and Sustainability, Universitat Hamburg, Hamburg, Germany
Experimental Plant Ecology, Institute of Botany and Landscape Ecology, Greifswald University, Greifswald, Germany
VetAgro Sup, UMR Ecosysteme Prairial, INRAE, Clermont Ferrand, France
Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Lausanne, Switzerland
Institute of Soil Science, Leibniz Universitat Hannover, Hannover, Germany
V. N. Sukachev Institute of Forest SB-RAS, Krasnoyarsk, Russian Federation
Department of Physical Geography, Stockholm University, Stockholm, Sweden
Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States
Department of Soil and Environment, Swedish University of Agricultural Sciences, Uppsala, Sweden
Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
International Institute for Applied Systems Analysis, Laxenburg, Austria
Department of Environmental Sciences and Engineering, Government College University Faisalabad, Faisalabad, Pakistan
Systems Ecology, Department of Ecological Sciences, Vrije Universiteit Amsterdam, Amsterdam, Netherlands

Доп.точки доступа:
Keuper, F.; Wild, B.; Kummu, M.; Beer, C.; Blume-Werry, G.; Fontaine, S.; Gavazov, K.; Gentsch, N.; Guggenberger, G.; Hugelius, G.; Jalava, M.; Koven, C.; Krab, E. J.; Kuhry, P.; Monteux, S.; Richter, A.; Shahzad, T.; Weedon, J. T.; Dorrepaal, E.

/ F. Keuper, B. Wild, M. Kummu [et al.] // Nat. Geosci. - 2020, DOI 10.1038/s41561-020-0607-0. - Cited References:76. - We thank P. Thornton, F. Dijkstra, Y. Carrillo and R. E. Hewitt for providing additional information on published data. Figure 1a-c is courtesy of R. Miedema (IN Produktie, Amsterdam). This study was supported by funding from: the Swedish Research Council (VR) (grant number 621-2011-5444), Formas (grant number 214-2011-788) and the Knut and Alice Wallenberg Foundation (grant number KAW 2012.0152) (all awarded to E.D.); Academy of Finland-funded projects SCART (grant number 267463) and WASCO (grant number 305471), Emil Aaltonen Foundation-funded project `eat-less-water', the European Research Council under the European Union's Horizon 2020 Research and Innovation Programme (grant agreement number 819202), and Maa-ja vesitekniikan tuki ry (all awarded to M.K.); the JPI Climate Project COUP-Austria (BMWFW-6.020/0008) (awarded to A.R.); two projects funded by the Swedish Research Council, the EU JPI Climate COUP project (E0689701) and the Project INCA (E0641701)-Marie Sklodowska-Curie Actions cofund (600398) (awarded to G.H.); the Deutsche Forschungsgemeinschaft (BE 6485/1-1) (to C.B.); and the US DOE BER RGMA programme through the RUBISCO SFA and ECRP projects (to C. K.). . - Article in press. - ISSN 1752-0894. - ISSN 1752-0908РУБ Geosciences, Multidisciplinary

Аннотация: As global temperatures continue to rise, a key uncertainty of climate projections is the microbial decomposition of vast organic carbon stocks in thawing permafrost soils. Decomposition rates can accelerate up to fourfold in the presence of plant roots, and this mechanism-termed the rhizosphere priming effect-may be especially relevant to thawing permafrost soils as rising temperatures also stimulate plant productivity in the Arctic. However, priming is currently not explicitly included in any model projections of future carbon losses from the permafrost area. Here, we combine high-resolution spatial and depth-resolved datasets of key plant and permafrost properties with empirical relationships of priming effects from living plants on microbial respiration. We show that rhizosphere priming amplifies overall soil respiration in permafrost-affected ecosystems by similar to 12%, which translates to a priming-induced absolute loss of similar to 40 Pg soil carbon from the northern permafrost area by 2100. Our findings highlight the need to include fine-scale ecological interactions in order to accurately predict large-scale greenhouse gas emissions, and suggest even tighter restrictions on the estimated 200 Pg anthropogenic carbon emission budget to keep global warming below 1.5 degrees C.

WOS

Держатели документа:
INRAE, BioEcoAgro Joint Res Unit, Barenton Bugny, France.
Umea Univ, Climate Impacts Res Ctr, Dept Ecol & Environm Sci, Abisko, Sweden.
Stockholm Univ, Dept Environm Sci, Stockholm, Sweden.
Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden.
Univ Gothenburg, Dept Earth Sci, Gothenburg, Sweden.
Aalto Univ, Water & Dev Res Grp, Espoo, Finland.
Univ Hamburg, Inst Soil Sci, Dept Earth Sci, Hamburg, Germany.
Univ Hamburg, Ctr Earth Syst Res & Sustainabil, Hamburg, Germany.
Greifswald Univ, Inst Bot & Landscape Ecol, Expt Plant Ecol, Greifswald, Germany.
INRAE, UMR Ecosyst Prairial, VetAgro Sup, Clermont Ferrand, France.
Swiss Fed Inst Forest Snow & Landscape Res WSL, Lausanne, Switzerland.
Leibniz Univ Hannover, Inst Soil Sci, Hannover, Germany.
VN Sukachev Inst Forest SB RAS, Krasnoyarsk, Russia.
Stockholm Univ, Dept Phys Geog, Stockholm, Sweden.
Lawrence Berkeley Natl Lab, Climate & Ecosyst Sci Div, Berkeley, CA USA.
Swedish Univ Agr Sci, Dept Soil & Environm, Uppsala, Sweden.
Univ Vienna, Ctr Microbiol & Environm Syst Sci, Vienna, Austria.
Int Inst Appl Syst Anal, Laxenburg, Austria.
Govt Coll Univ Faisalabad, Dept Environm Sci & Engn, Faisalabad, Pakistan.
Vrije Univ Amsterdam, Dept Ecol Sci, Syst Ecol, Amsterdam, Netherlands.

Доп.точки доступа:
Keuper, Frida; Wild, Birgit; Kummu, Matti; Beer, Christian; Blume-Werry, Gesche; Fontaine, Sebastien; Gavazov, Konstantin; Gentsch, Norman; Guggenberger, Georg; Hugelius, Gustaf; Jalava, Mika; Koven, Charles; Krab, Eveline J.; Kuhry, Peter; Monteux, Sylvain; Richter, Andreas; Shahzad, Tanvir; Weedon, James T.; Dorrepaal, Ellen; Swedish Research Council (VR)Swedish Research Council [621-2011-5444]; FormasSwedish Research Council Formas [214-2011-788]; Knut and Alice Wallenberg FoundationKnut & Alice Wallenberg Foundation [KAW 2012.0152]; Academy of FinlandAcademy of Finland [267463, 305471]; Emil Aaltonen Foundation; European Research Council under the European Union's Horizon 2020 Research and Innovation ProgrammeEuropean Research Council (ERC) [819202]; Maa-ja vesitekniikan tuki ry; JPI Climate Project COUP-Austria [BMWFW-6.020/0008]; Swedish Research CouncilSwedish Research Council; EU JPI Climate COUP project [E0689701]; Project INCA-Marie Sklodowska-Curie Actions cofund [E0641701, 600398]; Deutsche ForschungsgemeinschaftGerman Research Foundation (DFG) [BE 6485/1-1]; US DOE BER RGMA programme through the RUBISCO SFA projectUnited States Department of Energy (DOE); US DOE BER RGMA programme through ECRP projectUnited States Department of Energy (DOE)