Nutrient cycling responses to fire frequency in the Kruger National Park (South Africa) indicated by stable isotopes

J.N. ARANIBAR; S. A. MACKO; I. C. ANDERSON; A. POTGIETER; R. SOWRY; H.H. SHUGART

ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES

Taylor and Francis healthsciences

Lugar: Alemania; Año: 2003 vol. 39 p. 141 - 158

1025-6016

Fires, which are an intrinsic feature of southern African ecosystems, produce biogenic and pyrogenic losses of nitrogen (N) from plants and soils. Because of the long history of fires in these savannas, it was hypothesized that N2 fixation by legumes balances the N losses caused by fires. In this study, the N2 fixation activity of woody legumes was estimated by analyzing foliar d15N and proportional basal area of N2 fixing species along experimental fire gradients in the Kruger National Park (South Africa). In addition, soil carbon (C) and N pools, foliar phosphorus (P) and gross N mineralization and nitrification rates were measured, to indicate the effects of fires on nutrient stocks and the possible N cycling processes modified by fires. Although observations of increased soil C=N and mineralization rates in frequently burned plots support previous reports of N losses caused by fires, soil %N did not decrease with increasing fire frequency (except in 1 plot), suggesting that N losses are replenished in burned areas. However, relative abundance and N2 fixation of woody legumes decreased with fire frequency in two of the three fire gradients analyzed, suggesting that woody legume N2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.2 fixation by legumes balances the N losses caused by fires. In this study, the N2 fixation activity of woody legumes was estimated by analyzing foliar d15N and proportional basal area of N2 fixing species along experimental fire gradients in the Kruger National Park (South Africa). In addition, soil carbon (C) and N pools, foliar phosphorus (P) and gross N mineralization and nitrification rates were measured, to indicate the effects of fires on nutrient stocks and the possible N cycling processes modified by fires. Although observations of increased soil C=N and mineralization rates in frequently burned plots support previous reports of N losses caused by fires, soil %N did not decrease with increasing fire frequency (except in 1 plot), suggesting that N losses are replenished in burned areas. However, relative abundance and N2 fixation of woody legumes decreased with fire frequency in two of the three fire gradients analyzed, suggesting that woody legume N2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.d15N and proportional basal area of N2 fixing species along experimental fire gradients in the Kruger National Park (South Africa). In addition, soil carbon (C) and N pools, foliar phosphorus (P) and gross N mineralization and nitrification rates were measured, to indicate the effects of fires on nutrient stocks and the possible N cycling processes modified by fires. Although observations of increased soil C=N and mineralization rates in frequently burned plots support previous reports of N losses caused by fires, soil %N did not decrease with increasing fire frequency (except in 1 plot), suggesting that N losses are replenished in burned areas. However, relative abundance and N2 fixation of woody legumes decreased with fire frequency in two of the three fire gradients analyzed, suggesting that woody legume N2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.=N and mineralization rates in frequently burned plots support previous reports of N losses caused by fires, soil %N did not decrease with increasing fire frequency (except in 1 plot), suggesting that N losses are replenished in burned areas. However, relative abundance and N2 fixation of woody legumes decreased with fire frequency in two of the three fire gradients analyzed, suggesting that woody legume N2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.2 fixation of woody legumes decreased with fire frequency in two of the three fire gradients analyzed, suggesting that woody legume N2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.2 fixation is not the mechanism that balances N losses. The relatively constant %N along fire gradients suggests that these ecosystems have other mechanisms to balance the N lost by fires, which could include inputs by atmospheric deposition and N2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.2 fixation by forbs, grasses and soil cyanobacteria. Soil isotopic signatures have been previously used to infer patterns of fire history. However, the lack of a relationship between soil d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.d15N and fire frequency found in this study indicates that the effects of fires on ecosystem d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.d15N are unpredictable. Similar soil d15N along fire gradients may reflect the contrasting effects of increased N gaseous emissions (which increases d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.d15N) and N2 fixation other than that associated with woody legumes (which lowers d15N) on isotopic signatures.d15N) on isotopic signatures.