Contribution of plant photosynthate to soil respiration and dissolved organic carbon in a naturally recolonising cutover peatland

Lancaster Environment Centre

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https://doi.org/10.1016/j.soilbio.2008.01.016
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Keywords

(13)C, Calluna vulgaris, CO(2) efflux, cutover peatland, DOC, Eriophorum angustifolium, Eriophorum vaginatum, in situ, pulse labelling, microbial biomass, restoration

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Contribution of plant photosynthate to soil respiration and dissolved organic carbon in a naturally recolonising cutover peatland. / Trinder, Clare J.; Artz, Rebekka R. E.; Johnson, David.
In: Soil Biology and Biochemistry, Vol. 40, No. 7, 31.07.2008, p. 1622-1628.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Bibtex

@article{510d417d6103424aae1d36c535a5053f,

title = "Contribution of plant photosynthate to soil respiration and dissolved organic carbon in a naturally recolonising cutover peatland",

abstract = "The aim of this study was to investigate how three vascular plant species (Calluna vulgaris, Eriophorum angustifolium and Eriophorum vaginatum) colonising an abandoned cutover peatland affect fluxes of recent photosynthate to dissolved organic carbon (DOC), soil and plant respiration and shoot biomass. We used in situ 13CO2 pulse labelling to trace carbon (C) throughout a 65 day pulse chase period. Between 16 and 35% of the pulse of 13C remained in shoot biomass after 65 days with significant differences between C. vulgaris and E. angustifolium (P = 0.009) and between C. vulgaris and E. vaginatum (P = 0.04). A maximum of 29% was detected in DOC beneath labelled plants and losses of 13C from peat respiration never exceeded 0.16% of the original pulse, showing that little newly fixed C was allocated to this pool. There were no significant differences between the different plant species with respect to 13C recovered from DOC or via peat respiration. More C was lost via shoot respiration; although amounts varied between the three plant species, with 4.94–27.33% of the 13C pulse respired by the end of the experiment. Significant differences in 13C recovered from shoot respiration were found between C. vulgaris and E. angustifolium (P = 0.001) and between E. angustifolium and E. vaginatum (P = 0.032). Analysis of δ13C of microbial biomass indicated that recently assimilated C was allocated to this pool within 1 day of pulse labelling but there were no significant differences in the 13C enrichment of the microbial biomass associated with the different plant species. The data suggest that peat respiration represents a small flux of recent assimilate compared to other fluxes and pools and that different vascular plant species show considerable variation in the quantities and dynamics of C allocated to DOC.",

keywords = "(13)C, Calluna vulgaris, CO(2) efflux, cutover peatland, DOC, Eriophorum angustifolium, Eriophorum vaginatum, in situ, pulse labelling, microbial biomass, restoration",

author = "Trinder, {Clare J.} and Artz, {Rebekka R. E.} and David Johnson",

year = "2008",

month = jul,

day = "31",

doi = "10.1016/j.soilbio.2008.01.016",

language = "English",

volume = "40",

pages = "1622--1628",

journal = "Soil Biology and Biochemistry",

issn = "0038-0717",

publisher = "Elsevier Ltd",

number = "7",

}

RIS

TY - JOUR

T1 - Contribution of plant photosynthate to soil respiration and dissolved organic carbon in a naturally recolonising cutover peatland

AU - Trinder, Clare J.

AU - Artz, Rebekka R. E.

AU - Johnson, David

PY - 2008/7/31

Y1 - 2008/7/31

N2 - The aim of this study was to investigate how three vascular plant species (Calluna vulgaris, Eriophorum angustifolium and Eriophorum vaginatum) colonising an abandoned cutover peatland affect fluxes of recent photosynthate to dissolved organic carbon (DOC), soil and plant respiration and shoot biomass. We used in situ 13CO2 pulse labelling to trace carbon (C) throughout a 65 day pulse chase period. Between 16 and 35% of the pulse of 13C remained in shoot biomass after 65 days with significant differences between C. vulgaris and E. angustifolium (P = 0.009) and between C. vulgaris and E. vaginatum (P = 0.04). A maximum of 29% was detected in DOC beneath labelled plants and losses of 13C from peat respiration never exceeded 0.16% of the original pulse, showing that little newly fixed C was allocated to this pool. There were no significant differences between the different plant species with respect to 13C recovered from DOC or via peat respiration. More C was lost via shoot respiration; although amounts varied between the three plant species, with 4.94–27.33% of the 13C pulse respired by the end of the experiment. Significant differences in 13C recovered from shoot respiration were found between C. vulgaris and E. angustifolium (P = 0.001) and between E. angustifolium and E. vaginatum (P = 0.032). Analysis of δ13C of microbial biomass indicated that recently assimilated C was allocated to this pool within 1 day of pulse labelling but there were no significant differences in the 13C enrichment of the microbial biomass associated with the different plant species. The data suggest that peat respiration represents a small flux of recent assimilate compared to other fluxes and pools and that different vascular plant species show considerable variation in the quantities and dynamics of C allocated to DOC.

AB - The aim of this study was to investigate how three vascular plant species (Calluna vulgaris, Eriophorum angustifolium and Eriophorum vaginatum) colonising an abandoned cutover peatland affect fluxes of recent photosynthate to dissolved organic carbon (DOC), soil and plant respiration and shoot biomass. We used in situ 13CO2 pulse labelling to trace carbon (C) throughout a 65 day pulse chase period. Between 16 and 35% of the pulse of 13C remained in shoot biomass after 65 days with significant differences between C. vulgaris and E. angustifolium (P = 0.009) and between C. vulgaris and E. vaginatum (P = 0.04). A maximum of 29% was detected in DOC beneath labelled plants and losses of 13C from peat respiration never exceeded 0.16% of the original pulse, showing that little newly fixed C was allocated to this pool. There were no significant differences between the different plant species with respect to 13C recovered from DOC or via peat respiration. More C was lost via shoot respiration; although amounts varied between the three plant species, with 4.94–27.33% of the 13C pulse respired by the end of the experiment. Significant differences in 13C recovered from shoot respiration were found between C. vulgaris and E. angustifolium (P = 0.001) and between E. angustifolium and E. vaginatum (P = 0.032). Analysis of δ13C of microbial biomass indicated that recently assimilated C was allocated to this pool within 1 day of pulse labelling but there were no significant differences in the 13C enrichment of the microbial biomass associated with the different plant species. The data suggest that peat respiration represents a small flux of recent assimilate compared to other fluxes and pools and that different vascular plant species show considerable variation in the quantities and dynamics of C allocated to DOC.

KW - (13)C

KW - Calluna vulgaris, CO(2) efflux

KW - cutover peatland

KW - DOC

KW - Eriophorum angustifolium

KW - Eriophorum vaginatum

KW - in situ

KW - pulse labelling

KW - microbial biomass

KW - restoration

U2 - 10.1016/j.soilbio.2008.01.016

DO - 10.1016/j.soilbio.2008.01.016

M3 - Journal article

VL - 40

SP - 1622

EP - 1628

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

SN - 0038-0717

IS - 7

ER -

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