2005
DOI: 10.1016/j.soilbio.2004.08.008
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Dissolved organic nitrogen uptake by plants—an important N uptake pathway?

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Cited by 516 publications
(338 citation statements)
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“…Experiments that directly apply amino acid solutions instead of a soil environment neglect the importance of microorganisms as competitors for these substances and as main decomposers. It has been shown that the results obtained under such conditions are distinctly different from those obtained in the field (Jones et al 2005) and hence cannot reveal the ecological significance of organic N acquisition. Second, classic 15 N-tracer studies alone, not in combination with 14 C or 13 C labels, cannot separate the uptake of intact amino acids from uptake of mineralized N. Recently, the acquisition of organic N as intact amino acids by plants has been demonstrated using dual-labelled ( 13 C and 15 N) amino acids (Nä sholm and Persson 2001;Miller and Cramer 2004;Jones et al 2005).…”
Section: Introductionmentioning
confidence: 80%
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“…Experiments that directly apply amino acid solutions instead of a soil environment neglect the importance of microorganisms as competitors for these substances and as main decomposers. It has been shown that the results obtained under such conditions are distinctly different from those obtained in the field (Jones et al 2005) and hence cannot reveal the ecological significance of organic N acquisition. Second, classic 15 N-tracer studies alone, not in combination with 14 C or 13 C labels, cannot separate the uptake of intact amino acids from uptake of mineralized N. Recently, the acquisition of organic N as intact amino acids by plants has been demonstrated using dual-labelled ( 13 C and 15 N) amino acids (Nä sholm and Persson 2001;Miller and Cramer 2004;Jones et al 2005).…”
Section: Introductionmentioning
confidence: 80%
“…Many plants in cold environments such as arctic (Chapin et al 1993;Kielland 1994;Schimel and Chapin 1996), boreal (Nä sholm et al 1998;Nä sholm and Persson 2001) and alpine ecosystems Raab et al 1996Raab et al , 1999Miller and Bowman 2003;Xu et al 2004) showed the capacities to take up organic N from soils in the form of low molecular-weight substances, mainly amino acids. Laboratory studies using Michaelis-Menten kinetics have estimated that amino acids may contribute 60% and between 10% and 82% to the annual N acquisition of E. vaginatum (Chapin et al 1993) and of 10 arctic tundra species (Kielland 1994), respectively, but the ecological significance of organic N to the total N uptake by plants has not been quantified under field conditions (Nä sholm and Persson 2001;Merilä et al 2002;Jones et al 2004Jones et al , 2005.…”
Section: Introductionmentioning
confidence: 99%
“…The rhizobacteria help to fix the atmospheric nitrogen in soil. The number of amino acid transporters have been identified in plants, which confirms that plants have require machinery for amino acids transport from soil into their roots [22]. However, soil bacteria induced amino acid changes were reported as scare.…”
Section: Phosphate Solubilizing Ability Of Bacterial Isolate Mj1212mentioning
confidence: 86%
“…The concentration of dissolved organic C, or more precisely water-extractable organic C, has been reported by a number of researchers as a parameter which consistently decreases during the decomposition process, and has therefore been related to the process of stabilization [123]. The conversion of solid organic matter into dissolved organic matter has been shown to be the rate limiting step to the supply of N [24,54] and is therefore, likely to influence C and N dynamics in soil [77]. For example, the addition of a labile fraction of SOM to soil did not affect gross N mineralization, but markedly increased immobilization [37].…”
Section: Transformation Of Carbon and Nitrogen During Decompositionmentioning
confidence: 99%