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Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest

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Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest. / Brechet, Laetitia Magali; Le Dantec, Valérie ; Ponton, Stéphane et al.
In: Ecosystems, Vol. 20, No. 6, 09.2017, p. 1190-1204.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Brechet, LM, Le Dantec, V, Ponton, S, Goret, J-Y, Sayer, EJ, Bonal, D, Freycon, V, Roy, J & Epron, D 2017, 'Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest', Ecosystems, vol. 20, no. 6, pp. 1190-1204. https://doi.org/10.1007/s10021-016-0104-x

APA

Vancouver

Brechet LM, Le Dantec V, Ponton S, Goret J-Y, Sayer EJ, Bonal D et al. Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest. Ecosystems. 2017 Sept;20(6):1190-1204. Epub 2017 Jan 5. doi: 10.1007/s10021-016-0104-x

Author

Brechet, Laetitia Magali ; Le Dantec, Valérie ; Ponton, Stéphane et al. / Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest. In: Ecosystems. 2017 ; Vol. 20, No. 6. pp. 1190-1204.

Bibtex

@article{3035dce282f749ea915e8ad6c0360501,
title = "Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest",
abstract = "Heterotrophic soil respiration (SRH) alone can contribute up to 50% of total ecosystem respiration in tropical forests. Whereas the abiotic controls of SRH have been extensively studied, the influence of plant traits is less well characterised. We used field experiments and a modelling approach to test the relative influence of plant traits on SRH in lowland tropical forest in French Guiana. We measured leaf- and root litter traits for five common tree species and conducted a root decomposition experiment to evaluate the influence of root chemistry on decay rates. We measured SRH in trenched plots and used our field measurements to parameterize and test the Century model of soil C dynamics. Overall, the Century model performed well in simulating SRH, and species-specific root decomposition in Century corresponded well to decomposition rates measured in situ. Root litter characterized by low lignin-to-nitrogen ratios decomposed more rapidly than low-quality root litter during the first 6 months. Model runs over different time scales revealed that litter quality substantially influenced SRH on an annual time-scale by determining the rates of root- and leaf litter decomposition. However, litter mass had an overriding influence on SRH over the longer term in 20-year model runs. Synthesis Using simple plant trait data to parameterise the Century model, we were able to accurately simulate changes in SRH in a lowland tropical forest. Our results suggest that this approach could be used to predict changes in tropical soil C dynamics under global change scenarios by including data on changes in plant productivity and C inputs to the soil (for example litterfall and root turnover).",
keywords = "Century model, decomposition, leaf litter, fine roots, heterotrophic soil respiration, sensitivity analysis, soil carbon dynamics, plant traits",
author = "Brechet, {Laetitia Magali} and {Le Dantec}, Val{\'e}rie and St{\'e}phane Ponton and Jean-Yves Goret and Sayer, {Emma Jane} and Damien Bonal and Vincent Freycon and Jacques Roy and Daniel Epron",
note = "The final publication is available at Springer via http://dx.doi.org/10.1007/s10021-016-0104-x",
year = "2017",
month = sep,
doi = "10.1007/s10021-016-0104-x",
language = "English",
volume = "20",
pages = "1190--1204",
journal = "Ecosystems",
issn = "1432-9840",
publisher = "Springer New York LLC",
number = "6",

}

RIS

TY - JOUR

T1 - Short- and long-term influence of litter quality and quantity on simulated heterotrophic soil respiration in a lowland tropical forest

AU - Brechet, Laetitia Magali

AU - Le Dantec, Valérie

AU - Ponton, Stéphane

AU - Goret, Jean-Yves

AU - Sayer, Emma Jane

AU - Bonal, Damien

AU - Freycon, Vincent

AU - Roy, Jacques

AU - Epron, Daniel

N1 - The final publication is available at Springer via http://dx.doi.org/10.1007/s10021-016-0104-x

PY - 2017/9

Y1 - 2017/9

N2 - Heterotrophic soil respiration (SRH) alone can contribute up to 50% of total ecosystem respiration in tropical forests. Whereas the abiotic controls of SRH have been extensively studied, the influence of plant traits is less well characterised. We used field experiments and a modelling approach to test the relative influence of plant traits on SRH in lowland tropical forest in French Guiana. We measured leaf- and root litter traits for five common tree species and conducted a root decomposition experiment to evaluate the influence of root chemistry on decay rates. We measured SRH in trenched plots and used our field measurements to parameterize and test the Century model of soil C dynamics. Overall, the Century model performed well in simulating SRH, and species-specific root decomposition in Century corresponded well to decomposition rates measured in situ. Root litter characterized by low lignin-to-nitrogen ratios decomposed more rapidly than low-quality root litter during the first 6 months. Model runs over different time scales revealed that litter quality substantially influenced SRH on an annual time-scale by determining the rates of root- and leaf litter decomposition. However, litter mass had an overriding influence on SRH over the longer term in 20-year model runs. Synthesis Using simple plant trait data to parameterise the Century model, we were able to accurately simulate changes in SRH in a lowland tropical forest. Our results suggest that this approach could be used to predict changes in tropical soil C dynamics under global change scenarios by including data on changes in plant productivity and C inputs to the soil (for example litterfall and root turnover).

AB - Heterotrophic soil respiration (SRH) alone can contribute up to 50% of total ecosystem respiration in tropical forests. Whereas the abiotic controls of SRH have been extensively studied, the influence of plant traits is less well characterised. We used field experiments and a modelling approach to test the relative influence of plant traits on SRH in lowland tropical forest in French Guiana. We measured leaf- and root litter traits for five common tree species and conducted a root decomposition experiment to evaluate the influence of root chemistry on decay rates. We measured SRH in trenched plots and used our field measurements to parameterize and test the Century model of soil C dynamics. Overall, the Century model performed well in simulating SRH, and species-specific root decomposition in Century corresponded well to decomposition rates measured in situ. Root litter characterized by low lignin-to-nitrogen ratios decomposed more rapidly than low-quality root litter during the first 6 months. Model runs over different time scales revealed that litter quality substantially influenced SRH on an annual time-scale by determining the rates of root- and leaf litter decomposition. However, litter mass had an overriding influence on SRH over the longer term in 20-year model runs. Synthesis Using simple plant trait data to parameterise the Century model, we were able to accurately simulate changes in SRH in a lowland tropical forest. Our results suggest that this approach could be used to predict changes in tropical soil C dynamics under global change scenarios by including data on changes in plant productivity and C inputs to the soil (for example litterfall and root turnover).

KW - Century model

KW - decomposition

KW - leaf litter

KW - fine roots

KW - heterotrophic soil respiration

KW - sensitivity analysis

KW - soil carbon dynamics

KW - plant traits

U2 - 10.1007/s10021-016-0104-x

DO - 10.1007/s10021-016-0104-x

M3 - Journal article

VL - 20

SP - 1190

EP - 1204

JO - Ecosystems

JF - Ecosystems

SN - 1432-9840

IS - 6

ER -