Kuzyakov, Yakov

[["dc.bibliographiccitation.artnumber","S1164556321000893"],["dc.bibliographiccitation.firstpage","103353"],["dc.bibliographiccitation.journal","European Journal of Soil Biology"],["dc.bibliographiccitation.volume","106"],["dc.contributor.author","Bilyera, Nataliya"],["dc.contributor.author","Dippold, Michaela A."],["dc.contributor.author","Bleicher, Jarrett"],["dc.contributor.author","Maranguit, Deejay"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.date.accessioned","2021-10-01T09:57:31Z"],["dc.date.available","2021-10-01T09:57:31Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1016/j.ejsobi.2021.103353"],["dc.identifier.pii","S1164556321000893"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/89856"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-469"],["dc.relation.issn","1164-5563"],["dc.relation.orgunit","Department für Nutzpflanzenwissenschaften"],["dc.title","Microbial tradeoffs in internal and external use of resources regulated by phosphorus and carbon availability"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","66"],["dc.bibliographiccitation.journal","Soil Biology and Biochemistry"],["dc.bibliographiccitation.lastpage","78"],["dc.bibliographiccitation.volume","128"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.contributor.author","Horwath, William R."],["dc.contributor.author","Dorodnikov, Maxim"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.date.accessioned","2020-12-10T15:21:24Z"],["dc.date.available","2020-12-10T15:21:24Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1016/j.soilbio.2018.10.005"],["dc.identifier.issn","0038-0717"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73012"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Review and synthesis of the effects of elevated atmospheric CO2 on soil processes: No changes in pools, but increased fluxes and accelerated cycles"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","156"],["dc.bibliographiccitation.journal","Soil Biology and Biochemistry"],["dc.bibliographiccitation.lastpage","167"],["dc.bibliographiccitation.volume","127"],["dc.contributor.author","Guber, Andrey"],["dc.contributor.author","Kravchenko, Alexandra"],["dc.contributor.author","Razavi, Bahar S."],["dc.contributor.author","Uteau, Daniel"],["dc.contributor.author","Peth, Stephan"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2020-12-10T15:21:24Z"],["dc.date.available","2020-12-10T15:21:24Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.soilbio.2018.09.030"],["dc.identifier.issn","0038-0717"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73010"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Quantitative soil zymography: Mechanisms, processes of substrate and enzyme diffusion in porous media"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","221"],["dc.bibliographiccitation.journal","Biomass and Bioenergy"],["dc.bibliographiccitation.lastpage","229"],["dc.bibliographiccitation.volume","45"],["dc.contributor.author","Chen, Ruirui"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Senbayram, Mehmet"],["dc.contributor.author","Blagodatsky, Sergey A."],["dc.contributor.author","Myachina, Olga"],["dc.contributor.author","Dittert, Klaus"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2018-11-07T09:05:19Z"],["dc.date.available","2018-11-07T09:05:19Z"],["dc.date.issued","2012"],["dc.description.abstract","The rapid development of biogas production will result in increased use of biogas residues as organic fertilizers. However, control of microbial activity by organic fertilizers remains a challenge for modern land use, especially with respect to mitigating greenhouse effects and increasing C sequestration in soil. To address this issue, we compared CO2 emissions, microbial growth and extracellular enzyme activities in agricultural soil amended with biogas residues (BGR) versus maize straw (MST). Over a 21 day incubation period, 6.4% of organic C added was mineralised and evolved as CO2 with BGR and 30% with MST. As shown by the substrate-induced growth respiration approach, BGR and MST significantly decreased the specific microbial growth rate (mu) and increased the microbial biomass C in the soil, indicating a clear shift in the microbial community to slower-growing microorganisms. Because of the reduced availability of C associated with the less labile C and more lignin in biogas residues, observed mu values and microbial biomass C were lower after BGR application than after MST application. After 21 days incubation, BGR had no effect on the activity of three extracellular enzymes: beta-glucosidase and cellobiohydrolase, both of which are involved in cellulose decomposition; and xylanase, which is involved in hemicellulose decomposition. In contrast, MST significantly increased the activity of these three enzymes. The application of biogas residues in short-term experiment leads to a 34% increase in soil C content and slower C turnover as compared to common maize residues. (c) 2012 Elsevier Ltd. All rights reserved."],["dc.identifier.doi","10.1016/j.biombioe.2012.06.014"],["dc.identifier.isi","000308384500024"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25289"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0961-9534"],["dc.title","Decomposition of biogas residues in soil and their effects on microbial growth kinetics and enzyme activities"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","61"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Functional Ecology"],["dc.bibliographiccitation.lastpage","70"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Tian, Jing"],["dc.contributor.author","He, Nianpeng"],["dc.contributor.author","Hale, Lauren"],["dc.contributor.author","Niu, Shuli"],["dc.contributor.author","Yu, Guirui"],["dc.contributor.author","Liu, Yuan"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.contributor.author","Gao, Qun"],["dc.contributor.author","Zhou, Jizhong"],["dc.contributor.editor","Classen, Aimee"],["dc.date.accessioned","2020-12-10T18:26:25Z"],["dc.date.available","2020-12-10T18:26:25Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1111/1365-2435.12952"],["dc.identifier.eissn","1365-2435"],["dc.identifier.issn","0269-8463"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76075"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Soil organic matter availability and climate drive latitudinal patterns in bacterial diversity from tropical to cold temperate forests"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","57"],["dc.bibliographiccitation.journal","European Journal of Soil Biology"],["dc.bibliographiccitation.lastpage","64"],["dc.bibliographiccitation.volume","66"],["dc.contributor.author","Tian, Jing"],["dc.contributor.author","McCormack, Luke"],["dc.contributor.author","Wang, J."],["dc.contributor.author","Guo, D. H."],["dc.contributor.author","Wang, Qiufeng"],["dc.contributor.author","Zhang, X."],["dc.contributor.author","Yu, G."],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2018-11-07T10:03:48Z"],["dc.date.available","2018-11-07T10:03:48Z"],["dc.date.issued","2015"],["dc.description.abstract","Patterns in the spatial distribution of soil microorganisms and the factors that determine them provide important information about the mechanisms regulating diversity and function of terrestrial ecosystems. The spatial heterogeneity of metabolic functional diversity of soil microorganisms was studied across a 30 x 40 m plot and at two soil depths (0-10 cm and 10-20 cm) in a natural, mixed broad-leaved Korean pine (Pinus koraiensis) forest soil in the Changbai Mountains. In addition, we assessed the importance of the quantity and quality (indicated by labile soil organic matter fractions) of soil organic matter in small-scale structuring of soil microbial metabolic functional diversity. Microbial metabolic functional diversity was characterized based on the Biolog profile. The results showed that metabolic activity exhibited moderate spatial dependence, while functional diversity had a much stronger spatial dependence. All soil organic matter fractions including total soil organic matter, dissolved organic matter, particulate organic matter explained 15-27% of the variance in microbial functional diversity in the two soil layers. Among all soil organic matter fractions, the labile dissolved organic carbon accounted for the largest amount of variation. Overall, the significant relationship between soil microorganisms and organic matter fractions allows for better understanding the ecological functions governing C cycling and microbial communities in forest ecosystems. (C) 2014 Elsevier Masson SAS. All rights reserved."],["dc.identifier.doi","10.1016/j.ejsobi.2014.12.001"],["dc.identifier.isi","000348243400008"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/38555"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier France-editions Scientifiques Medicales Elsevier"],["dc.relation.issn","1778-3615"],["dc.relation.issn","1164-5563"],["dc.title","Linkages between the soil organic matter fractions and the microbial metabolic functional diversity within a broad-leaved Korean pine forest"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2356"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Global Change Biology"],["dc.bibliographiccitation.lastpage","2367"],["dc.bibliographiccitation.volume","20"],["dc.contributor.author","Chen, Ruirui"],["dc.contributor.author","Senbayram, Mehmet"],["dc.contributor.author","Blagodatsky, Sergey A."],["dc.contributor.author","Myachina, Olga"],["dc.contributor.author","Dittert, Klaus"],["dc.contributor.author","Lin, Xiangui"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2018-11-07T09:38:28Z"],["dc.date.available","2018-11-07T09:38:28Z"],["dc.date.issued","2014"],["dc.description.abstract","The increasing input of anthropogenically derived nitrogen (N) to ecosystems raises a crucial question: how does available N modify the decomposer community and thus affects the mineralization of soil organic matter (SOM). Moreover, N input modifies the priming effect (PE), that is, the effect of fresh organics on the microbial decomposition of SOM. We studied the interactive effects of C and N on SOM mineralization (by natural C-13 labelling adding C-4-sucrose or C-4-maize straw to C-3-soil) in relation to microbial growth kinetics and to the activities of five hydrolytic enzymes. This encompasses the groups of parameters governing two mechanisms of priming effects -microbial N mining and stoichiometric decomposition theories. In sole C treatments, positive PE was accompanied by a decrease in specific microbial growth rates, confirming a greater contribution of K-strategists to the decomposition of native SOM. Sucrose addition with N significantly accelerated mineralization of native SOM, whereas mineral N added with plant residues accelerated decomposition of plant residues. This supports the microbial mining theory in terms of N limitation. Sucrose addition with N was accompanied by accelerated microbial growth, increased activities of beta-glucosidase and cellobiohydrolase, and decreased activities of xylanase and leucine amino peptidase. This indicated an increased contribution of r-strategists to the PE and to decomposition of cellulose but the decreased hemicellulolytic and proteolytic activities. Thus, the acceleration of the C cycle was primed by exogenous organic C and was controlled by N. This confirms the stoichiometric decomposition theory. Both K-and r-strategists were beneficial for priming effects, with an increasing contribution of K-selected species under N limitation. Thus, the priming phenomenon described in 'microbial N mining' theory can be ascribed to K-strategists. In contrast, 'stoichiometric decomposition' theory, that is, accelerated OM mineralization due to balanced microbial growth, is explained by domination of r-strategists."],["dc.identifier.doi","10.1111/gcb.12475"],["dc.identifier.isi","000337680700029"],["dc.identifier.pmid","24273056"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33072"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Wiley-blackwell"],["dc.relation.issn","1365-2486"],["dc.relation.issn","1354-1013"],["dc.title","Soil C and N availability determine the priming effect: microbial N mining and stoichiometric decomposition theories"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","523"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Biology and Fertility of Soils"],["dc.bibliographiccitation.lastpage","532"],["dc.bibliographiccitation.volume","53"],["dc.contributor.author","Tian, Jing"],["dc.contributor.author","Lou, Yilai"],["dc.contributor.author","Gao, Yang"],["dc.contributor.author","Fang, Huajun"],["dc.contributor.author","Liu, Shutang"],["dc.contributor.author","Xu, Minggang"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2018-11-07T10:22:21Z"],["dc.date.available","2018-11-07T10:22:21Z"],["dc.date.issued","2017"],["dc.description.abstract","The effects of organic and mineral fertilization on four soil organic matter (SOM) fractions (non-protected, physically protected, chemically protected, and biochemically protected) and microbial community composition were investigated by sampling soil of a 35-year-long fertilization experiment. The SOM fractions were investigated by combined physical and chemical approaches, while microbial community composition was determined by phospholipid fatty acid analysis (PLFA). Organic C (SOC) was primarily distributed within the microaggregate-protected particulate organic matter (iPOM) and the hydrolysable and non-hydrolysable silt-sized (H-Silt, NH-Silt) fractions, which accounted for 11.6-16.9, 23.4-28.9, and 25.4-30.6% of the total SOC content, respectively. The contributions of these \"slow\" fractions (iPOM, H-Silt, NH-Silt) to the increased SOC were 178-293, 118-209, and 85-109% higher after long-term sole manure or manure in combination with inorganic N fertilization compared with unfertilized soil (control). The combination of manure and mineral fertilizers increased the coarse and fine non-protected C (cPOM and fPOM) contents much more (34.1-60.7%) than did manure alone. PLFAs, bacteria, G (+) bacteria, and actinomycete abundances were the highest in soil with manure, followed by soil treated with manure combined with mineral N. The addition of inorganic and organic fertilization both altered the microbial community composition compared with the control. All SOM fractions contributed to 81.1% of the variance of the PLFAs-related microbial community composition by direct and indirect effects. The change in coarse unprotected particulate organic matter (cPOM) was the major factor affecting soil microbial community composition (p < 0.001). Our study indicates that physical, chemical, and biochemical protection mechanisms are important in maintaining high SOC level after the addition of manure. A close linkage between soil microbial community composition and cPOM suggests that C availability is an important factor for influencing microbial composition after long-term inorganic and organic fertilization."],["dc.identifier.doi","10.1007/s00374-017-1189-x"],["dc.identifier.isi","000403352800006"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42252"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Springer"],["dc.relation.issn","1432-0789"],["dc.relation.issn","0178-2762"],["dc.title","Response of soil organic matter fractions and composition of microbial community to long-term organic and mineral fertilization"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","287"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Biology and Fertility of Soils"],["dc.bibliographiccitation.lastpage","301"],["dc.bibliographiccitation.volume","53"],["dc.contributor.author","Shahbaz, Muhammad"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.contributor.author","Sanaullah, Muhammad"],["dc.contributor.author","Heitkamp, Felix"],["dc.contributor.author","Zelenev, Vladimir"],["dc.contributor.author","Kumar, Amit"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.date.accessioned","2018-11-07T10:25:41Z"],["dc.date.available","2018-11-07T10:25:41Z"],["dc.date.issued","2017"],["dc.description.abstract","Crop residue quality and quantity have contrasting effects on soil organic matter (SOM) decomposition, but the mechanisms explaining such priming effect (PE) are still elusive. To reveal the role of residue quality and quantity in SOM priming, we applied two rates (5.4-10.8 g kg(-1)) of C-13-labeled wheat residues (separately: leaves, stems, roots) to soil and incubated for 120 days. To distinguish PE mechanisms, labeled C was traced in CO2 efflux and in microbial biomass and enzyme activities (involved in C, N, and P cycles) were measured during the incubation period. Regardless of residue type, PE intensity declined with increasing C additions. Roots were least mineralized but caused up to 60% higher PE compared to leaves or stems. During intensive residue mineralization (first 2-3 weeks), the low or negative PE resulted from pool substitution. Thereafter (15-60 days), a large decline in microbial biomass along with increased enzyme activity suggested that microbial necromass served as SOM primer. Finally, incorporation of SOM-derived C into remaining microbial biomass corresponded to increased enzyme activity, which is indicative of SOM cometabolism. Both PE and enzyme activities were primarily correlated with residue-metabolizing soil microorganisms. A unifying model demonstrated that PE was a function of residue mineralization, with thresholds for strong PE increase of up to 20% root, 44% stem, and 51% leaf mineralization. Thus, root mineralization has the lowest threshold for a strong PE increase. Our study emphasizes the role of residue-feeding microorganisms as active players in the PE, which are mediated by quality and quantity of crop residue additions."],["dc.identifier.doi","10.1007/s00374-016-1174-9"],["dc.identifier.isi","000398708200004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42905"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Springer"],["dc.relation.issn","1432-0789"],["dc.relation.issn","0178-2762"],["dc.title","Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues: mechanisms and thresholds"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","270"],["dc.bibliographiccitation.journal","CATENA"],["dc.bibliographiccitation.lastpage","277"],["dc.bibliographiccitation.volume","162"],["dc.contributor.author","Yang, Fan"],["dc.contributor.author","Tian, Jing"],["dc.contributor.author","Meersmans, Jeroen"],["dc.contributor.author","Fang, Huajun"],["dc.contributor.author","Yang, Hao"],["dc.contributor.author","Lou, Yilai"],["dc.contributor.author","Li, Zhongfang"],["dc.contributor.author","Liu, Kailou"],["dc.contributor.author","Zhou, Yi"],["dc.contributor.author","Blagodatskaya, Evgenia"],["dc.contributor.author","Kuzyakov, Yakov"],["dc.date.accessioned","2020-12-10T14:22:51Z"],["dc.date.available","2020-12-10T14:22:51Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1016/j.catena.2017.11.004"],["dc.identifier.issn","0341-8162"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71760"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Functional soil organic matter fractions in response to long-term fertilization in upland and paddy systems in South China"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]