Chronic nitrogen fertilization and carbon sequestration in grassland soils: evidence of a microbial enzyme link
File(s)
Author(s)
Type
Journal Article
Abstract
Chronic nitrogen (N) fertilization can greatly affect soil carbon (C) sequestration by altering biochemical interactions between plant detritus and soil microbes. In lignin-rich forest soils, chronic N additions tend to increase soil C content partly by decreasing the activity of lignin-degrading enzymes. In cellulose-rich grassland soils it is not clear whether cellulose-degrading enzymes are also inhibited by N additions and what consequences this might have on changes in soil C content. Here we address whether chronic N fertilization has affected (1) the C content of light versus heavier soil fractions, and (2) the activity of four extracellular enzymes including the C-acquiring enzyme β-1,4-glucosidase (BG; necessary for cellulose hydrolysis). We found that 19 years of chronic N-only addition to permanent grassland have significantly increased soil C sequestration in heavy but not in light soil density fractions, and this C accrual was associated with a significant increase (and not decrease) of BG activity. Chronic N fertilization may increase BG activity because greater N availability reduces root C:N ratios thus increasing microbial demand for C, which is met by C inputs from enhanced root C pools in N-only fertilized soils. However, BG activity and total root mass strongly decreased in high pH soils under the application of lime (i.e. CaCO3), which reduced the ability of these organo-mineral soils to gain more C per units of N added. Our study is the first to show a potential ‘enzyme link’ between (1) long-term additions of inorganic N to grassland soils, and (2) the greater C content of organo-mineral soil fractions. Our new hypothesis is that the ‘enzyme link’ occurs because (a) BG activity is stimulated by increased microbial C demand relative to N under chronic fertilization, and (b) increased BG activity causes more C from roots and from microbial metabolites to accumulate and stabilize into organo-mineral C fractions. We suggest that any combination of management practices that can influence the BG ‘enzyme link’ will have far reaching implications for long-term C sequestration in grassland soils.
Date Issued
2015-11-14
Date Acceptance
2015-10-31
Citation
Biogeochemistry, 2015, 126 (3), pp.301-313
ISSN
1573-515X
Publisher
Springer Verlag
Start Page
301
End Page
313
Journal / Book Title
Biogeochemistry
Volume
126
Issue
3
Copyright Statement
© The Author(s) 2015. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
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Subjects
Science & Technology
Life Sciences & Biomedicine
Physical Sciences
Environmental Sciences
Geosciences, Multidisciplinary
Environmental Sciences & Ecology
Geology
Extracellular enzyme activity
beta-1,4-Glucosidase
Fertilization
Liming
Soil carbon
sequestration
Root C:N ratio
ORGANIC-MATTER
N DEPOSITION
FOREST ECOSYSTEMS
NUTRIENT RELEASE
LITTER DECAY
DECOMPOSITION
RESPONSES
PHOSPHORUS
TURNOVER
DYNAMICS
Agronomy & Agriculture
0399 Other Chemical Sciences
0402 Geochemistry
Publication Status
Published