Assessing turnover of microbial biomass phosphorus: Combination of an isotopic dilution method with a mass balance model

Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink (immobilization) of phosphate ions (iP). To assess the role of the microbial P pools, both the dynamics (i.e. the turnover) and the size of the microbi...

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Vydáno v:	Soil biology & biochemistry Ročník 42; číslo 12; s. 2231 - 2240
Hlavní autoři:	Achat, David L., Morel, Christian, Bakker, Mark R., Augusto, Laurent, Pellerin, Sylvain, Gallet-Budynek, Anne, Gonzalez, Maya
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Amsterdam Elsevier Ltd 01.12.2010 Elsevier
Témata:	Agricultural sciences Agronomy. Soil science and plant productions Biochemistry and biology biogeochemical cycles Biological and medical sciences Chemical, physicochemical, biochemical and biological properties Forest ecosystem forest soils forest trees France Fundamental and applied biological sciences. Psychology immobilization in soil Isotopic dilution method Life Sciences Mass balance model Microbial biomass Microbiology mineralization nutrient availability nutrient uptake P availability P cycling phosphates Phosphorus Physics, chemistry, biochemistry and biology of agricultural and forest soils plant nutrition simulation models soil microorganisms soil organic matter Soil science Soil study temperate forests temporal variation Turnover France P cycling Isotopic dilution method P availability Forest ecosystem Turnover Phosphorus Microbial biomass Mass balance model Forests Forest zone Available nutrient Isotope dilution Modeling Ecosystem Soil science Material balance PHOSPHORUS MICROBIAL BIOMASS MASS BALANCE MODEL TURNOVER P AVAILABILITY FOREST ECOSYSTEM ISOTOPIC DILUTION METHOD P CYCLING
ISSN:	0038-0717, 1879-3428
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Abstract	Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink (immobilization) of phosphate ions (iP). To assess the role of the microbial P pools, both the dynamics (i.e. the turnover) and the size of the microbial P pools were studied in forest soils. Combining an isotopic dilution method with a modelling approach, we showed the existence of two pools of microbial P with different dynamics and therefore of different importance in soil P availability and cycling. In particular, we showed that the largest pool of microbial P (80%) had a fast turnover (nine days). Microbial P increased with an increase in soil organic matter and represented up to 53% of total P in contrasting forest soils. By combining these results with the turnover times of microbial P obtained in the modelling study, we evaluated that 8.5–17.3 kg P ha −1 of microbial P could turn over in a few days. This suggests that microbial biomass P is a potentially significant source of available iP, and that micro-organisms can play a major role in P cycling in the forest studied here. However, microbial biomass can also be in competition with the trees since most of the remineralized P could be immobilized again in the microbial turnover.
AbstractList	Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink (immobilization) of phosphate ions (iP). To assess the role of the microbial P pools, both the dynamics (i.e. the turnover) and the size of the microbial P pools were studied in forest soils. Combining an isotopic dilution method with a modelling approach, we showed the existence of two pools of microbial P with different dynamics and therefore of different importance in soil P availability and cycling. In particular, we showed that the largest pool of microbial P (80%) had a fast turnover (nine days). Microbial P increased with an increase in soil organic matter and represented up to 53% of total P in contrasting forest soils. By combining these results with the turnover times of microbial P obtained in the modelling study, we evaluated that 8.5–17.3 kg P ha−1 of microbial P could turn over in a few days. This suggests that microbial biomass P is a potentially significant source of available iP, and that micro-organisms can play a major role in P cycling in the forest studied here. However, microbial biomass can also be in competition with the trees since most of the remineralized P could be immobilized again in the microbial turnover. Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink (immobilization) of phosphate ions (iP). To assess the role of the microbial P pools, both the dynamics (i.e. the turnover) and the size of the microbial P pools were studied in forest soils. Combining an isotopic dilution method with a modelling approach, we showed the existence of two pools of microbial P with different dynamics and therefore of different importance in soil P availability and cycling. In particular, we showed that the largest pool of microbial P (80%) had a fast turnover (nine days). Microbial P increased with an increase in soil organic matter and represented up to 53% of total P in contrasting forest soils. By combining these results with the turnover times of microbial P obtained in the modelling study, we evaluated that 8.5-17.3 kg P ha super(-1) of microbial P could turn over in a few days. This suggests that microbial biomass P is a potentially significant source of available iP, and that micro-organisms can play a major role in P cycling in the forest studied here. However, microbial biomass can also be in competition with the trees since most of the remineralized P could be immobilized again in the microbial turnover. Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink (immobilization) of phosphate ions (iP). To assess the role of the microbial P pools, both the dynamics (i.e. the turnover) and the size of the microbial P pools were studied in forest soils. Combining an isotopic dilution method with a modelling approach, we showed the existence of two pools of microbial P with different dynamics and therefore of different importance in soil P availability and cycling. In particular, we showed that the largest pool of microbial P (80%) had a fast turnover (nine days). Microbial P increased with an increase in soil organic matter and represented up to 53% of total P in contrasting forest soils. By combining these results with the turnover times of microbial P obtained in the modelling study, we evaluated that 8.5–17.3 kg P ha −1 of microbial P could turn over in a few days. This suggests that microbial biomass P is a potentially significant source of available iP, and that micro-organisms can play a major role in P cycling in the forest studied here. However, microbial biomass can also be in competition with the trees since most of the remineralized P could be immobilized again in the microbial turnover.
Author	Gallet-Budynek, Anne Pellerin, Sylvain Morel, Christian Gonzalez, Maya Achat, David L. Augusto, Laurent Bakker, Mark R.
Author_xml	– sequence: 1 givenname: David L. surname: Achat fullname: Achat, David L. email: dachat@bordeaux.inra.fr organization: ENITA de Bordeaux, UMR 1220 TCEM (INRA-ENITAB), 1 cours du Général de Gaulle, F-33175, France – sequence: 2 givenname: Christian surname: Morel fullname: Morel, Christian organization: INRA, UMR 1220 TCEM (INRA-ENITAB), 71 avenue E Bourlaux, F-33883 Villenave d’Ornon, France – sequence: 3 givenname: Mark R. surname: Bakker fullname: Bakker, Mark R. organization: ENITA de Bordeaux, UMR 1220 TCEM (INRA-ENITAB), 1 cours du Général de Gaulle, F-33175, France – sequence: 4 givenname: Laurent surname: Augusto fullname: Augusto, Laurent organization: INRA, UMR 1220 TCEM (INRA-ENITAB), 71 avenue E Bourlaux, F-33883 Villenave d’Ornon, France – sequence: 5 givenname: Sylvain surname: Pellerin fullname: Pellerin, Sylvain organization: INRA, UMR 1220 TCEM (INRA-ENITAB), 71 avenue E Bourlaux, F-33883 Villenave d’Ornon, France – sequence: 6 givenname: Anne surname: Gallet-Budynek fullname: Gallet-Budynek, Anne organization: INRA, UMR 1220 TCEM (INRA-ENITAB), 71 avenue E Bourlaux, F-33883 Villenave d’Ornon, France – sequence: 7 givenname: Maya surname: Gonzalez fullname: Gonzalez, Maya organization: ENITA de Bordeaux, UMR 1220 TCEM (INRA-ENITAB), 1 cours du Général de Gaulle, F-33175, France
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Keywords	P cycling Isotopic dilution method P availability Forest ecosystem Turnover Phosphorus Microbial biomass Mass balance model Forests Forest zone Available nutrient Isotope dilution Modeling Ecosystem Soil science Material balance PHOSPHORUS MICROBIAL BIOMASS MASS BALANCE MODEL TURNOVER P AVAILABILITY FOREST ECOSYSTEM ISOTOPIC DILUTION METHOD P CYCLING
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Snippet	Microbial biomass phosphorus (P) can play an important role in P cycling and availability to plants by acting as a source (remineralization) or sink...
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SubjectTerms	Agricultural sciences Agronomy. Soil science and plant productions Biochemistry and biology biogeochemical cycles Biological and medical sciences Chemical, physicochemical, biochemical and biological properties Forest ecosystem forest soils forest trees France Fundamental and applied biological sciences. Psychology immobilization in soil Isotopic dilution method Life Sciences Mass balance model Microbial biomass Microbiology mineralization nutrient availability nutrient uptake P availability P cycling phosphates Phosphorus Physics, chemistry, biochemistry and biology of agricultural and forest soils plant nutrition simulation models soil microorganisms soil organic matter Soil science Soil study temperate forests temporal variation Turnover
Title	Assessing turnover of microbial biomass phosphorus: Combination of an isotopic dilution method with a mass balance model
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