Do evergreen and deciduous trees have different effects on net N mineralization in soil?
Evergreen and deciduous plants are widely expected to have different impacts on soil nitrogen (N) availability because of differences in leaf litter chemistry and ensuing effects on net N mineralization (N min ). We evaluated this hypothesis by compiling published data on net N min rates beneath co-...
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Veröffentlicht in: | Ecology (Durham) 2012-06, Vol.93 (6), p.1463-1472 |
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Sprache: | eng |
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Zusammenfassung: | Evergreen and deciduous plants are widely expected to have different impacts on soil nitrogen (N) availability because of differences in leaf litter chemistry and ensuing effects on net N mineralization (N
min
). We evaluated this hypothesis by compiling published data on net N
min
rates beneath co-occurring stands of evergreen and deciduous trees. The compiled data included 35 sets of co-occurring stands in temperate and boreal forests. Evergreen and deciduous stands did not have consistently divergent effects on net N
min
rates; net N
min
beneath deciduous trees was higher when comparing natural stands (19 contrasts), but equivalent to evergreens in plantations (16 contrasts). We also compared net N
min
rates beneath pairs of co-occurring genera. Most pairs of genera did not differ consistently, i.e., tree species from one genus had higher net N
min
at some sites and lower net N
min
at other sites. Moreover, several common deciduous genera (
Acer
,
Betula
,
Populus
) and deciduous
Quercus
spp. did not typically have higher net N
min
rates than common evergreen genera (
Pinus
,
Picea
). There are several reasons why tree effects on net N
min
are poorly predicted by leaf habit and phylogeny. For example, the amount of N mineralized from decomposing leaves might be less than the amount of N mineralized from organic matter pools that are less affected by leaf litter traits, such as dead roots and soil organic matter. Also, effects of plant traits and plant groups on net N
min
probably depend on site-specific factors such as stand age and soil type. |
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ISSN: | 0012-9658 1939-9170 |
DOI: | 10.1890/11-1906.1 |