Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient
Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an ex...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Vallano, Dena M. [verfasserIn] Sparks, Jed P. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2012 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Oecologia - Berlin : Springer, 1968, 172(2012), 1 vom: 16. Okt., Seite 47-58 |
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| Übergeordnetes Werk: |
volume:172 ; year:2012 ; number:1 ; day:16 ; month:10 ; pages:47-58 |
| Links: |
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| DOI / URN: |
10.1007/s00442-012-2489-3 |
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| Katalog-ID: |
SPR006087299 |
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| 520 | |a Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. | ||
| 650 | 4 | |a Nitrogen isotope composition |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Foliar uptake |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Nitrogen cycling |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Reactive nitrogen |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Temperate forest |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Sparks, Jed P. |e verfasserin |4 aut | |
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10.1007/s00442-012-2489-3 doi (DE-627)SPR006087299 (SPR)s00442-012-2489-3-e DE-627 ger DE-627 rakwb eng 590 333.7 ASE 42.90 bkl Vallano, Dena M. verfasserin aut Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 Sparks, Jed P. verfasserin aut Enthalten in Oecologia Berlin : Springer, 1968 172(2012), 1 vom: 16. Okt., Seite 47-58 (DE-627)25462975X (DE-600)1462019-4 1432-1939 nnns volume:172 year:2012 number:1 day:16 month:10 pages:47-58 https://dx.doi.org/10.1007/s00442-012-2489-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2939 GBV_ILN_2946 GBV_ILN_2949 GBV_ILN_2951 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4393 GBV_ILN_4700 42.90 ASE AR 172 2012 1 16 10 47-58 |
| spelling |
10.1007/s00442-012-2489-3 doi (DE-627)SPR006087299 (SPR)s00442-012-2489-3-e DE-627 ger DE-627 rakwb eng 590 333.7 ASE 42.90 bkl Vallano, Dena M. verfasserin aut Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 Sparks, Jed P. verfasserin aut Enthalten in Oecologia Berlin : Springer, 1968 172(2012), 1 vom: 16. Okt., Seite 47-58 (DE-627)25462975X (DE-600)1462019-4 1432-1939 nnns volume:172 year:2012 number:1 day:16 month:10 pages:47-58 https://dx.doi.org/10.1007/s00442-012-2489-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2939 GBV_ILN_2946 GBV_ILN_2949 GBV_ILN_2951 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4393 GBV_ILN_4700 42.90 ASE AR 172 2012 1 16 10 47-58 |
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10.1007/s00442-012-2489-3 doi (DE-627)SPR006087299 (SPR)s00442-012-2489-3-e DE-627 ger DE-627 rakwb eng 590 333.7 ASE 42.90 bkl Vallano, Dena M. verfasserin aut Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 Sparks, Jed P. verfasserin aut Enthalten in Oecologia Berlin : Springer, 1968 172(2012), 1 vom: 16. Okt., Seite 47-58 (DE-627)25462975X (DE-600)1462019-4 1432-1939 nnns volume:172 year:2012 number:1 day:16 month:10 pages:47-58 https://dx.doi.org/10.1007/s00442-012-2489-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2939 GBV_ILN_2946 GBV_ILN_2949 GBV_ILN_2951 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4393 GBV_ILN_4700 42.90 ASE AR 172 2012 1 16 10 47-58 |
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10.1007/s00442-012-2489-3 doi (DE-627)SPR006087299 (SPR)s00442-012-2489-3-e DE-627 ger DE-627 rakwb eng 590 333.7 ASE 42.90 bkl Vallano, Dena M. verfasserin aut Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 Sparks, Jed P. verfasserin aut Enthalten in Oecologia Berlin : Springer, 1968 172(2012), 1 vom: 16. Okt., Seite 47-58 (DE-627)25462975X (DE-600)1462019-4 1432-1939 nnns volume:172 year:2012 number:1 day:16 month:10 pages:47-58 https://dx.doi.org/10.1007/s00442-012-2489-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2939 GBV_ILN_2946 GBV_ILN_2949 GBV_ILN_2951 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4393 GBV_ILN_4700 42.90 ASE AR 172 2012 1 16 10 47-58 |
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10.1007/s00442-012-2489-3 doi (DE-627)SPR006087299 (SPR)s00442-012-2489-3-e DE-627 ger DE-627 rakwb eng 590 333.7 ASE 42.90 bkl Vallano, Dena M. verfasserin aut Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient 2012 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 Sparks, Jed P. verfasserin aut Enthalten in Oecologia Berlin : Springer, 1968 172(2012), 1 vom: 16. Okt., Seite 47-58 (DE-627)25462975X (DE-600)1462019-4 1432-1939 nnns volume:172 year:2012 number:1 day:16 month:10 pages:47-58 https://dx.doi.org/10.1007/s00442-012-2489-3 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_266 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_374 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2939 GBV_ILN_2946 GBV_ILN_2949 GBV_ILN_2951 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4393 GBV_ILN_4700 42.90 ASE AR 172 2012 1 16 10 47-58 |
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English |
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Enthalten in Oecologia 172(2012), 1 vom: 16. Okt., Seite 47-58 volume:172 year:2012 number:1 day:16 month:10 pages:47-58 |
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Enthalten in Oecologia 172(2012), 1 vom: 16. Okt., Seite 47-58 volume:172 year:2012 number:1 day:16 month:10 pages:47-58 |
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Nitrogen isotope composition Foliar uptake Nitrogen cycling Reactive nitrogen Temperate forest |
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Oecologia |
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Vallano, Dena M. @@aut@@ Sparks, Jed P. @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR006087299</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230519174211.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201002s2012 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00442-012-2489-3</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR006087299</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00442-012-2489-3-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">590</subfield><subfield code="a">333.7</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">42.90</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Vallano, Dena M.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2012</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nitrogen isotope composition</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Foliar uptake</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nitrogen cycling</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Reactive nitrogen</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Temperate forest</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sparks, Jed P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Oecologia</subfield><subfield code="d">Berlin : Springer, 1968</subfield><subfield code="g">172(2012), 1 vom: 16. 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|
| author |
Vallano, Dena M. |
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Vallano, Dena M. ddc 590 bkl 42.90 misc Nitrogen isotope composition misc Foliar uptake misc Nitrogen cycling misc Reactive nitrogen misc Temperate forest Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
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Vallano, Dena M. |
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590 333.7 ASE 42.90 bkl Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient Nitrogen isotope composition (dpeaa)DE-He213 Foliar uptake (dpeaa)DE-He213 Nitrogen cycling (dpeaa)DE-He213 Reactive nitrogen (dpeaa)DE-He213 Temperate forest (dpeaa)DE-He213 |
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ddc 590 bkl 42.90 misc Nitrogen isotope composition misc Foliar uptake misc Nitrogen cycling misc Reactive nitrogen misc Temperate forest |
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ddc 590 bkl 42.90 misc Nitrogen isotope composition misc Foliar uptake misc Nitrogen cycling misc Reactive nitrogen misc Temperate forest |
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ddc 590 bkl 42.90 misc Nitrogen isotope composition misc Foliar uptake misc Nitrogen cycling misc Reactive nitrogen misc Temperate forest |
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Elektronische Aufsätze Aufsätze Elektronische Ressource |
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Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
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Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
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Vallano, Dena M. |
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Oecologia |
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Vallano, Dena M. Sparks, Jed P. |
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Vallano, Dena M. |
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10.1007/s00442-012-2489-3 |
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foliar $ δ^{15} $n is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
| title_auth |
Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
| abstract |
Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. |
| abstractGer |
Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. |
| abstract_unstemmed |
Abstract Foliar nitrogen isotope ($ δ^{15} $N) composition patterns have been linked to soil N, mycorrhizal fractionation, and within-plant fractionations. However, few studies have examined the potential importance of the direct foliar uptake of gaseous reactive N on foliar $ δ^{15} $N. Using an experimental set-up in which the rate of mycorrhizal infection was reduced using a fungicide, we examined the influence of mycorrhizae on foliar $ δ^{15} $N in potted red maple (Acer rubrum) seedlings along a regional N deposition gradient in New York State. Mycorrhizal associations altered foliar $ δ^{15} $N values in red maple seedlings from 0.06 to 0.74 ‰ across sites. At the same sites, we explored the predictive roles of direct foliar N uptake, soil $ δ^{15} $N, and mycorrhizae on foliar $ δ^{15} $N in adult stands of A. rubrum, American beech (Fagus grandifolia), black birch (Betula lenta), and red oak (Quercus rubra). Multiple regression analysis indicated that ambient atmospheric nitrogen dioxide ($ NO_{2} $) concentration explained 0, 69, 23, and 45 % of the variation in foliar $ δ^{15} $N in American beech, red maple, red oak, and black birch, respectively, after accounting for the influence of soil $ δ^{15} $N. There was no correlation between foliar $ δ^{13} $C and foliar %N with increasing atmospheric $ NO_{2} $ concentration in most species. Our findings suggest that total canopy uptake, and likely direct foliar N uptake, of pollution-derived atmospheric N deposition may significantly impact foliar $ δ^{15} $N in several dominant species occurring in temperate forest ecosystems. |
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Foliar $ δ^{15} $N is affected by foliar nitrogen uptake, soil nitrogen, and mycorrhizae along a nitrogen deposition gradient |
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| score |
7.397691 |