Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios

By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C...

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Veröffentlicht in:Biogeochemistry 2021-06, Vol.154 (2), p.405-426
Hauptverfasser: Martinelli, L. A., Nardoto, G. B., Soltangheisi, A., Reis, C. R. G., Abdalla-Filho, A. L., Camargo, P. B., Domingues, T. F., Faria, D., Figueira, A. M., Gomes, T. F., Lins, S. R. M., Mardegan, S. F., Mariano, E., Miatto, R. C., Moraes, R., Moreira, M. Z., Oliveira, R. S., Ometto, J. P. H. B., Santos, F. L. S., Sena-Souza, J., Silva, D. M. L., Silva, J. C. S. S., Vieira, S. A.
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container_end_page 426
container_issue 2
container_start_page 405
container_title Biogeochemistry
container_volume 154
creator Martinelli, L. A.
Nardoto, G. B.
Soltangheisi, A.
Reis, C. R. G.
Abdalla-Filho, A. L.
Camargo, P. B.
Domingues, T. F.
Faria, D.
Figueira, A. M.
Gomes, T. F.
Lins, S. R. M.
Mardegan, S. F.
Mariano, E.
Miatto, R. C.
Moraes, R.
Moreira, M. Z.
Oliveira, R. S.
Ometto, J. P. H. B.
Santos, F. L. S.
Sena-Souza, J.
Silva, D. M. L.
Silva, J. C. S. S.
Vieira, S. A.
description By analyzing 6,480 tree leaf samples from 57 sites within Brazilian biomes, we considered whether vegetation types in terrestrial ecosystems reflect biogeochemical diversity and whether they fit into a leaf economics spectrum (LES). To achieve this, we investigated the relations among leaf carbon (C) and nitrogen (N) concentrations, their isotope natural abundance and C:N ratio. In addition, we tested their correlations with mean annual temperature (MAT) and precipitation (MAP), as climatic factors. We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. Finally, we expect our findings to contribute to a better understanding of the tropics in global climate models.
doi_str_mv 10.1007/s10533-020-00714-2
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A. ; Nardoto, G. B. ; Soltangheisi, A. ; Reis, C. R. G. ; Abdalla-Filho, A. L. ; Camargo, P. B. ; Domingues, T. F. ; Faria, D. ; Figueira, A. M. ; Gomes, T. F. ; Lins, S. R. M. ; Mardegan, S. F. ; Mariano, E. ; Miatto, R. C. ; Moraes, R. ; Moreira, M. Z. ; Oliveira, R. S. ; Ometto, J. P. H. B. ; Santos, F. L. S. ; Sena-Souza, J. ; Silva, D. M. L. ; Silva, J. C. S. S. ; Vieira, S. A.</creator><creatorcontrib>Martinelli, L. A. ; Nardoto, G. B. ; Soltangheisi, A. ; Reis, C. R. G. ; Abdalla-Filho, A. L. ; Camargo, P. B. ; Domingues, T. F. ; Faria, D. ; Figueira, A. M. ; Gomes, T. F. ; Lins, S. R. M. ; Mardegan, S. F. ; Mariano, E. ; Miatto, R. C. ; Moraes, R. ; Moreira, M. Z. ; Oliveira, R. S. ; Ometto, J. P. H. B. ; Santos, F. L. S. ; Sena-Souza, J. ; Silva, D. M. L. ; Silva, J. C. S. S. ; Vieira, S. 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We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. 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We found consistent differences in the C and N concentrations and their isotopic composition among the vegetation types. MAP is the main climatic driver of changes in N, C:N ratio, δ¹⁵N, and δ¹³C, correlating negatively with N and positively with C:N ratio. These relations show that these biomes follow an LES. The Caatinga had the highest δ¹⁵N values, suggesting that N residence time in soil is longer due to low leaching and plant uptake. We observed that MAP is not the only factor influencing δ¹³C values in different biomes; instead canopy effect probably explains the highest values observed in the Cerrado. Our results reinforce earlier findings that life diversity in the tropics reflects biogeochemistry diversity and leaf δ¹⁵N opens the possibility for investigating plant trade-offs dictated by the LES. 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subjects Annual precipitation
Biogeochemistry
Biogeosciences
Carbon
Climate models
Earth and Environmental Science
Earth Sciences
Ecological function
Economics
Ecosystems
Environmental Chemistry
Global climate
Global climate models
Herbivores
Isotope ratios
Leaching
Leaves
Life Sciences
Nitrogen
ORIGINAL PAPERS
Plant cover
Residence time
Stable isotopes
Terrestrial ecosystems
Tropical environments
Uptake
Vegetation
title Determining ecosystem functioning in Brazilian biomes through foliar carbon and nitrogen concentrations and stable isotope ratios
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