2010
DOI: 10.1007/s10021-010-9320-y
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N:P Ratio and the Nature of Nutrient Limitation in Calluna-Dominated Heathlands

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Cited by 71 publications
(45 citation statements)
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“…Probably due to the chronic high deposition of nitrogen from the atmosphere, there has been a change in the former fluctuation of the cover of the grass to a more stable situation where D. flexuosa, and lately also Molinia caerulea, are often the dominating species in nutrient-poor inland ecosystems such as wet and dry heath. The same scenario has been observed in a number of western European countries (Bobbink et al 2003) and (von Oheimb et al 2010).…”
Section: Introductionsupporting
confidence: 79%
“…Probably due to the chronic high deposition of nitrogen from the atmosphere, there has been a change in the former fluctuation of the cover of the grass to a more stable situation where D. flexuosa, and lately also Molinia caerulea, are often the dominating species in nutrient-poor inland ecosystems such as wet and dry heath. The same scenario has been observed in a number of western European countries (Bobbink et al 2003) and (von Oheimb et al 2010).…”
Section: Introductionsupporting
confidence: 79%
“…These results agree with other recent studies that have found co-limitation to occur in temperate (Niinemets and Kalevi, 2005;Vadeboncoeur, 2010) and tropical (Wullaert et al, 2010) ecosystems. P-limitation or co-limitation in temperate systems might occur because: (1) until recently P limitations have not been investigated as rigorously as N limitations in the temperate systems (Vadeboncoeur, 2010), and (2) increased N deposition and its physiological consequences are shifting the nature and extent of nutrient limitations (Von Oheimb et al, 2010). Similarly, some tropical forests have been found to have N-limitation due to substrate age and type that does not fit the norm for tropical systems (Domingues et al, 2010).…”
Section: Trends In Rr N and Rr P Across Climatic Gradients And Ecosysmentioning
confidence: 99%
“…Numerous studies have suggested that biomass N : P ratios of less than 14 (mass basis) indicate N limitation, and that ratios greater than 16 indicate P limitation in terrestrial plants (Koerselman and Meuleman, 1996;Aerts and Champin, 2000). On the basis of a meta-analysis, Güsewell (2004) suggested that the N : P ratio indicating N limitation was lowered to 10 and the limit for P limitation was raised to 20; for ratios between 10 and 20, plant growth may be co-limited by N and P. However, several studies have suggested that speciesspecific leaf N : P ratios do not reflect the type of nutrient limitation at the local scale (von Oheimb et al, 2010). 15 N fractionation due to discrimination against the isotopically heavier 15 N substrates can occur during N uptake and assimilation by plant tissues (e.g., enzymatic NH 4 or NO À 3 assimilation; Evans, 2001).…”
Section: Introductionmentioning
confidence: 97%