Successional changes in soil nitrogen availability, non-symbiotic nitrogen fixation and carbon/nitrogen ratios in southern Chilean forest ecosystems
dc.contributor.author | Pérez, CA | |
dc.contributor.author | Carmona, MR | |
dc.contributor.author | Aravena, JC | |
dc.contributor.author | Armesto, JJ | |
dc.date.accessioned | 2025-01-21T01:07:45Z | |
dc.date.available | 2025-01-21T01:07:45Z | |
dc.date.issued | 2004 | |
dc.description.abstract | Vast areas of southern Chile are now covered by second-growth forests because of fire and logging. To study successional patterns after moderate-intensity, anthropogenic fire disturbance, we assessed differences in soil properties and N fluxes across a chronosequence of seven successional stands (2-130 years old). We examined current predictions of successional theory concerning changes in the N cycle in forest ecosystems. Seasonal fluctuations of net N mineralization (N-min) in surface soil and N availability (N-a; N-a=NH4+-N+NO3--N) in upper and deep soil horizons were positively correlated with monthly precipitation. In accordance with theoretical predictions, stand age was positively, but weakly related to both N-a (r(2)=0.282, P<0.001) and total N (N-tot; r(2)=0.192, P<0.01), and negatively related to soil C/N ratios (r(2)=0.187, P<0.01) in surface soils. A weak linear increase in soil N-min (upper plus deep soil horizons) was found across the chronosequence (r(2)=0.124, P<0.022). N-min occurred at modest rates in early successional stands, suggesting that soil disturbance did not impair microbial processes. The relationship between N fixation (N-fix) in the litter layer and stand age best fitted a quadratic model (r(2)=0.228, P<0.01). In contrast to documented successional trends for most temperate, tropical and Mediterranean forests, non-symbiotic N-fix in the litter layer is a steady N input to unpolluted southern temperate forests during mid and late succession, which may compensate for hydrological losses of organic N from old-growth ecosystems. | |
dc.fuente.origen | WOS | |
dc.identifier.doi | 10.1007/s00442-004-1627-y | |
dc.identifier.eissn | 1432-1939 | |
dc.identifier.issn | 0029-8549 | |
dc.identifier.uri | https://doi.org/10.1007/s00442-004-1627-y | |
dc.identifier.uri | https://repositorio.uc.cl/handle/11534/96375 | |
dc.identifier.wosid | WOS:000223266500010 | |
dc.issue.numero | 4 | |
dc.language.iso | en | |
dc.pagina.final | 625 | |
dc.pagina.inicio | 617 | |
dc.revista | Oecologia | |
dc.rights | acceso restringido | |
dc.subject | nitrogen cycle | |
dc.subject | net nitrogen mineralization | |
dc.subject | southern temperate forests | |
dc.subject | secondary succession | |
dc.subject.ods | 02 Zero Hunger | |
dc.subject.ods | 13 Climate Action | |
dc.subject.ods | 15 Life on Land | |
dc.subject.ods | 14 Life Below Water | |
dc.subject.odspa | 02 Hambre cero | |
dc.subject.odspa | 13 Acción por el clima | |
dc.subject.odspa | 15 Vida de ecosistemas terrestres | |
dc.subject.odspa | 14 Vida submarina | |
dc.title | Successional changes in soil nitrogen availability, non-symbiotic nitrogen fixation and carbon/nitrogen ratios in southern Chilean forest ecosystems | |
dc.type | artículo | |
dc.volumen | 140 | |
sipa.index | WOS | |
sipa.trazabilidad | WOS;2025-01-12 |