Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest

Soils of tropical forests are important to the global budgets of greenhouse gases. The Brazilian Atlantic Forest is the second largest tropical moist forest area of South America, after the vast Amazonian domain. This study aimed to investigate the emissions of nitrous oxide (N<sub>2&a...

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Main Authors: E. Sousa Neto, J. B. Carmo, M. Keller, S. C. Martins, L. F. Alves, S. A. Vieira, M. C. Piccolo, P. Camargo, H. T. Z. Couto, C. A. Joly, L. A. Martinelli
Format: Article
Language:English
Published: Copernicus Publications 2011-03-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/8/733/2011/bg-8-733-2011.pdf
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author E. Sousa Neto
J. B. Carmo
M. Keller
S. C. Martins
L. F. Alves
S. A. Vieira
M. C. Piccolo
P. Camargo
H. T. Z. Couto
C. A. Joly
L. A. Martinelli
author_facet E. Sousa Neto
J. B. Carmo
M. Keller
S. C. Martins
L. F. Alves
S. A. Vieira
M. C. Piccolo
P. Camargo
H. T. Z. Couto
C. A. Joly
L. A. Martinelli
author_sort E. Sousa Neto
collection DOAJ
description Soils of tropical forests are important to the global budgets of greenhouse gases. The Brazilian Atlantic Forest is the second largest tropical moist forest area of South America, after the vast Amazonian domain. This study aimed to investigate the emissions of nitrous oxide (N<sub>2</sub>O), carbon dioxide (CO<sub>2</sub>) and methane (CH<sub>4</sub>) fluxes along an altitudinal transect and the relation between these fluxes and other climatic, edaphic and biological variables (temperature, fine roots, litterfall, and soil moisture). Annual means of N<sub>2</sub>O flux were 3.9 (± 0.4), 1.0 (± 0.1), and 0.9 (± 0.2) ng N cm<sup>−2</sup> h<sup>−1</sup> at altitudes 100, 400, and 1000 m, respectively. On an annual basis, soils consumed CH<sub>4</sub> at all altitudes with annual means of −1.0 (± 0.2), −1.8 (± 0.3), and −1.6 (± 0.1) mg m<sup>−2</sup> d<sup>−1</sup> at 100 m, 400 m and 1000 m, respectively. Estimated mean annual fluxes of CO<sub>2</sub> were 3.5, 3.6, and 3.4 μmol m<sup>−2</sup> s<sup>−1</sup> at altitudes 100, 400 and 1000 m, respectively. N<sub>2</sub>O fluxes were significantly influenced by soil moisture and temperature. Soil-atmosphere exchange of CH<sub>4</sub> responded to changes in soil moisture. Carbon dioxide emissions were strongly influenced by soil temperature. While the temperature gradient observed at our sites is only an imperfect proxy for climatic warming, our results suggest that an increase in air and soil temperatures may result in increases in decomposition rates and gross inorganic nitrogen fluxes that could support consequent increases in soil N<sub>2</sub>O and CO<sub>2</sub> emissions and soil CH<sub>4</sub> consumption.
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spelling doaj.art-3c1daaeeef0a4661a87f88040c4fa4cd2022-12-21T23:45:51ZengCopernicus PublicationsBiogeosciences1726-41701726-41892011-03-018373374210.5194/bg-8-733-2011Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forestE. Sousa NetoJ. B. CarmoM. KellerS. C. MartinsL. F. AlvesS. A. VieiraM. C. PiccoloP. CamargoH. T. Z. CoutoC. A. JolyL. A. MartinelliSoils of tropical forests are important to the global budgets of greenhouse gases. The Brazilian Atlantic Forest is the second largest tropical moist forest area of South America, after the vast Amazonian domain. This study aimed to investigate the emissions of nitrous oxide (N<sub>2</sub>O), carbon dioxide (CO<sub>2</sub>) and methane (CH<sub>4</sub>) fluxes along an altitudinal transect and the relation between these fluxes and other climatic, edaphic and biological variables (temperature, fine roots, litterfall, and soil moisture). Annual means of N<sub>2</sub>O flux were 3.9 (± 0.4), 1.0 (± 0.1), and 0.9 (± 0.2) ng N cm<sup>−2</sup> h<sup>−1</sup> at altitudes 100, 400, and 1000 m, respectively. On an annual basis, soils consumed CH<sub>4</sub> at all altitudes with annual means of −1.0 (± 0.2), −1.8 (± 0.3), and −1.6 (± 0.1) mg m<sup>−2</sup> d<sup>−1</sup> at 100 m, 400 m and 1000 m, respectively. Estimated mean annual fluxes of CO<sub>2</sub> were 3.5, 3.6, and 3.4 μmol m<sup>−2</sup> s<sup>−1</sup> at altitudes 100, 400 and 1000 m, respectively. N<sub>2</sub>O fluxes were significantly influenced by soil moisture and temperature. Soil-atmosphere exchange of CH<sub>4</sub> responded to changes in soil moisture. Carbon dioxide emissions were strongly influenced by soil temperature. While the temperature gradient observed at our sites is only an imperfect proxy for climatic warming, our results suggest that an increase in air and soil temperatures may result in increases in decomposition rates and gross inorganic nitrogen fluxes that could support consequent increases in soil N<sub>2</sub>O and CO<sub>2</sub> emissions and soil CH<sub>4</sub> consumption.http://www.biogeosciences.net/8/733/2011/bg-8-733-2011.pdf
spellingShingle E. Sousa Neto
J. B. Carmo
M. Keller
S. C. Martins
L. F. Alves
S. A. Vieira
M. C. Piccolo
P. Camargo
H. T. Z. Couto
C. A. Joly
L. A. Martinelli
Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
Biogeosciences
title Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
title_full Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
title_fullStr Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
title_full_unstemmed Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
title_short Soil-atmosphere exchange of nitrous oxide, methane and carbon dioxide in a gradient of elevation in the coastal Brazilian Atlantic forest
title_sort soil atmosphere exchange of nitrous oxide methane and carbon dioxide in a gradient of elevation in the coastal brazilian atlantic forest
url http://www.biogeosciences.net/8/733/2011/bg-8-733-2011.pdf
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