Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues: mechanisms and thresholds.

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Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues : mechanisms and thresholds. / Shahbaz, Muhammad; Kuzyakov, Yakov; Sanaullah, Muhammad et al.

In: Biology and Fertility of Soils, Vol. 53, No. 3, 01.04.2017, p. 287-301.

Research output: Journal contributionsJournal articlesResearchpeer-review

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Shahbaz M, Kuzyakov Y, Sanaullah M, Heitkamp F, Zelenev V, Kumar A et al. Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues: mechanisms and thresholds. Biology and Fertility of Soils. 2017 Apr 1;53(3):287-301. doi: 10.1007/s00374-016-1174-9

Bibtex

@article{f6829e3640314bc183ecade6eeb2ed82,
title = "Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues: mechanisms and thresholds.",
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 13C-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.",
keywords = "13C-labeled crop residues, Enzyme activities, Litter quality, Microbial necromass, Priming effect, Soil organic matter, Ecosystems Research",
author = "Muhammad Shahbaz and Yakov Kuzyakov and Muhammad Sanaullah and Felix Heitkamp and Vladimir Zelenev and Amit Kumar and Evgenia Blagodatskaya",
year = "2017",
month = apr,
day = "1",
doi = "10.1007/s00374-016-1174-9",
language = "English",
volume = "53",
pages = "287--301",
journal = "Biology and Fertility of Soils",
issn = "0178-2762",
publisher = "Springer",
number = "3",

}

RIS

TY - JOUR

T1 - Microbial decomposition of soil organic matter is mediated by quality and quantity of crop residues

T2 - mechanisms and thresholds.

AU - Shahbaz, Muhammad

AU - Kuzyakov, Yakov

AU - Sanaullah, Muhammad

AU - Heitkamp, Felix

AU - Zelenev, Vladimir

AU - Kumar, Amit

AU - Blagodatskaya, Evgenia

PY - 2017/4/1

Y1 - 2017/4/1

N2 - 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 13C-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.

AB - 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 13C-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.

KW - 13C-labeled crop residues

KW - Enzyme activities

KW - Litter quality

KW - Microbial necromass

KW - Priming effect

KW - Soil organic matter

KW - Ecosystems Research

U2 - 10.1007/s00374-016-1174-9

DO - 10.1007/s00374-016-1174-9

M3 - Journal articles

VL - 53

SP - 287

EP - 301

JO - Biology and Fertility of Soils

JF - Biology and Fertility of Soils

SN - 0178-2762

IS - 3

ER -