Phosphorus rather than nitrogen enhances CO 2 emissions in tropical forest soils: Evidence from a laboratory incubation study
Abstract Ecosystem functional responses such as soil CO 2 emissions are constrained by microclimate, available carbon (C) substrates and their effects upon microbial activity. In tropical forests, phosphorus (P) is often considered as a limiting factor for plant growth, but it is still not clear whe...
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Published in | European journal of soil science Vol. 71; no. 3; pp. 495 - 510 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
01.05.2020
|
Online Access | Get full text |
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Summary: | Abstract
Ecosystem functional responses such as soil CO
2
emissions are constrained by microclimate, available carbon (C) substrates and their effects upon microbial activity. In tropical forests, phosphorus (P) is often considered as a limiting factor for plant growth, but it is still not clear whether P constrains microbial CO
2
emissions from soils. In this study, we incubated seven tropical forest soils from Brazil and Puerto Rico with different nutrient addition treatments (no addition, Control; C, nitrogen (N) or P addition only; and combined C, N and P addition (CNP)). Cumulative soil CO
2
emissions were fit with a Gompertz model to estimate potential maximum cumulative soil CO
2
emission (
C
m
) and the rate of change of soil C decomposition (
k
). Quantitative polymerase chain reaction (qPCR) was conducted to quantify microbial biomass as bacteria and fungi. Results showed that P addition alone or in combination with C and N enhanced
C
m
, whereas N addition usually reduced
C
m
, and neither N nor P affected microbial biomass. Additions of CNP enhanced
k
, increased microbial abundances and altered fungal to bacterial ratios towards higher fungal abundance. Additions of CNP, however, tended to reduce
C
m
for most soils when compared to C additions alone, suggesting that microbial growth associated with nutrient additions may have occurred at the expense of C decomposition. Overall, this study demonstrates that soil CO
2
emission is more limited by P than N in tropical forest soils and those effects were stronger in soils low in P.
Highlights
A laboratory incubation study was conducted with nitrogen, phosphorus or carbon addition to tropical forest soils. Soil CO
2
emission was fitted with a Gompertz model and soil microbial abundance was quantified using qPCR. Phosphorus addition increased model parameters
C
m
and soil CO
2
emission, particularly in the Puerto Rico soils. Soil CO
2
emission was more limited by phosphorus than nitrogen in tropical forest soils. |
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ISSN: | 1351-0754 1365-2389 |
DOI: | 10.1111/ejss.12885 |