2013
DOI: 10.1016/j.soilbio.2012.10.027
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N-driven changes in a plant community affect leaf-litter traits and may delay organic matter decomposition in a Mediterranean maquis

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Cited by 31 publications
(21 citation statements)
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“…However, Perakis et al [63] found that the positive effect of N addition on decomposition only appeared in the early stage (0.67 year), the negative effect appeared after 3-year decomposition (mass remaining was 54.6% in the control plots and 62.2% in the N-addition plots). In addition, many other studies also proved that N addition (N deposition) inhibited litter decomposition in the later stage or soil organic matter decomposition [66,75]. One possible reason for this result is that the added-N combined with lignin and phenolic matter to form more recalcitrant materials to start the first stage of humification earlier [34,76].…”
Section: Altered Litter and Forest Substrates Chemical Qualitiesmentioning
confidence: 97%
“…However, Perakis et al [63] found that the positive effect of N addition on decomposition only appeared in the early stage (0.67 year), the negative effect appeared after 3-year decomposition (mass remaining was 54.6% in the control plots and 62.2% in the N-addition plots). In addition, many other studies also proved that N addition (N deposition) inhibited litter decomposition in the later stage or soil organic matter decomposition [66,75]. One possible reason for this result is that the added-N combined with lignin and phenolic matter to form more recalcitrant materials to start the first stage of humification earlier [34,76].…”
Section: Altered Litter and Forest Substrates Chemical Qualitiesmentioning
confidence: 97%
“…Dias et al. () found that N‐driven changes in plant communities influence leaf‐litter traits, and may alter the process of SOM decomposition. Therefore, changes in plant communities and the N:C ratios of new SOM inputs are expected to influence SOM stability and storage (Drake et al.…”
Section: Discussionmentioning
confidence: 99%
“…However, NO 3 − leaching can occur much later than many diversity and internal N cycle changes [8]. On the other hand, and in contrast to observations of several studies [52], high N (80AN) addition does appear to have increased soil organic matter, most likely reflecting a decrease in decomposition [53]. This is of particular importance for Mediterranean Basin soils due to their naturally low organic matter concentration and hence higher susceptibility to erosion and desertification [54].…”
Section: Discussionmentioning
confidence: 99%