Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.

The biogeochemical cycles of C, N, P and water, the impacts of land use in the stocks and flows of these elements and how they can affect the structure and functioning of Caatinga were reviewed. About half of this biome is still covered by native secondary vegetation. Soils are deficient in nutrients, especially N and P. Average concentrations of total soil P and C in the top layer (0-20 cm) are 196 mg kg?1 and 9.3 g kg?1, corresponding to C stocks around 23 Mg ha?1. Aboveground biomass of native vegetation varies from 30 to 50 Mg ha?1, and average root biomass from 3 to 12 Mg ha?1. Average annual productivities and biomass accumulation in different land use systems vary from 1 to 7 Mg ha?1 year?1. Biological atmospheric N2 fixation is estimated to vary from 3 to 11 kg N ha?1 year?1and 21 to 26 kg N ha?1 year?1 in mature and secondary Caatinga, respectively. The main processes responsible for nutrient and water losses are fire, soil erosion, runoff and harvest of crops and animal products. Projected climate changes in the future point to higher temperatures and rainfall decreases. In face of the high intrinsic variability, actions to increase sustainability should improve resilience and stability of the ecosystems. Land use systems based on perennial species, as opposed to annual species, may be more stable and resilient, thus more adequate to face future potential increases in climate variability. Long-term studies to investigate the potential of the native biodiversity or adapted exotic species to design sustainable land use systems should be encouraged.

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Main Authors: MENEZES, R. S. C., SAMPAIO, E. V. S. B., GIONGO, V., PÉREZ-MARIN, A. M.
Other Authors: UFPE; VANDERLISE GIONGO, CPATSA; Instituto Nacional do Semiárido.
Format: Artigo de periódico biblioteca
Language:pt_BR
por
Published: 2013-01-02
Subjects:Floresta seca tropical, Fluxo de nutrientes, Bioma Caatinga, Natural resource., Caatinga, Biodiversidade, Recurso natural, Carbono, Fósforo, Nitrogênio.,
Online Access:http://www.alice.cnptia.embrapa.br/alice/handle/doc/943753
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spelling dig-alice-doc-9437532017-08-16T00:18:13Z Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome. MENEZES, R. S. C. SAMPAIO, E. V. S. B. GIONGO, V. PÉREZ-MARIN, A. M. UFPE; VANDERLISE GIONGO, CPATSA; Instituto Nacional do Semiárido. Floresta seca tropical Fluxo de nutrientes Bioma Caatinga Natural resource. Caatinga Biodiversidade Recurso natural Carbono Fósforo Nitrogênio. The biogeochemical cycles of C, N, P and water, the impacts of land use in the stocks and flows of these elements and how they can affect the structure and functioning of Caatinga were reviewed. About half of this biome is still covered by native secondary vegetation. Soils are deficient in nutrients, especially N and P. Average concentrations of total soil P and C in the top layer (0-20 cm) are 196 mg kg?1 and 9.3 g kg?1, corresponding to C stocks around 23 Mg ha?1. Aboveground biomass of native vegetation varies from 30 to 50 Mg ha?1, and average root biomass from 3 to 12 Mg ha?1. Average annual productivities and biomass accumulation in different land use systems vary from 1 to 7 Mg ha?1 year?1. Biological atmospheric N2 fixation is estimated to vary from 3 to 11 kg N ha?1 year?1and 21 to 26 kg N ha?1 year?1 in mature and secondary Caatinga, respectively. The main processes responsible for nutrient and water losses are fire, soil erosion, runoff and harvest of crops and animal products. Projected climate changes in the future point to higher temperatures and rainfall decreases. In face of the high intrinsic variability, actions to increase sustainability should improve resilience and stability of the ecosystems. Land use systems based on perennial species, as opposed to annual species, may be more stable and resilient, thus more adequate to face future potential increases in climate variability. Long-term studies to investigate the potential of the native biodiversity or adapted exotic species to design sustainable land use systems should be encouraged. Suplemento 3. 2013-01-02T11:11:11Z 2013-01-02T11:11:11Z 2013-01-02 2012 2013-02-07T11:11:11Z Artigo de periódico Brazilian Journal of Biology, São Carlos, v. 72, n. 3, p. 643-653, 2012. http://www.alice.cnptia.embrapa.br/alice/handle/doc/943753 pt_BR por openAccess
institution EMBRAPA
collection DSpace
country Brasil
countrycode BR
component Bibliográfico
access En linea
databasecode dig-alice
tag biblioteca
region America del Sur
libraryname Sistema de bibliotecas de EMBRAPA
language pt_BR
por
topic Floresta seca tropical
Fluxo de nutrientes
Bioma Caatinga
Natural resource.
Caatinga
Biodiversidade
Recurso natural
Carbono
Fósforo
Nitrogênio.
Floresta seca tropical
Fluxo de nutrientes
Bioma Caatinga
Natural resource.
Caatinga
Biodiversidade
Recurso natural
Carbono
Fósforo
Nitrogênio.
spellingShingle Floresta seca tropical
Fluxo de nutrientes
Bioma Caatinga
Natural resource.
Caatinga
Biodiversidade
Recurso natural
Carbono
Fósforo
Nitrogênio.
Floresta seca tropical
Fluxo de nutrientes
Bioma Caatinga
Natural resource.
Caatinga
Biodiversidade
Recurso natural
Carbono
Fósforo
Nitrogênio.
MENEZES, R. S. C.
SAMPAIO, E. V. S. B.
GIONGO, V.
PÉREZ-MARIN, A. M.
Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
description The biogeochemical cycles of C, N, P and water, the impacts of land use in the stocks and flows of these elements and how they can affect the structure and functioning of Caatinga were reviewed. About half of this biome is still covered by native secondary vegetation. Soils are deficient in nutrients, especially N and P. Average concentrations of total soil P and C in the top layer (0-20 cm) are 196 mg kg?1 and 9.3 g kg?1, corresponding to C stocks around 23 Mg ha?1. Aboveground biomass of native vegetation varies from 30 to 50 Mg ha?1, and average root biomass from 3 to 12 Mg ha?1. Average annual productivities and biomass accumulation in different land use systems vary from 1 to 7 Mg ha?1 year?1. Biological atmospheric N2 fixation is estimated to vary from 3 to 11 kg N ha?1 year?1and 21 to 26 kg N ha?1 year?1 in mature and secondary Caatinga, respectively. The main processes responsible for nutrient and water losses are fire, soil erosion, runoff and harvest of crops and animal products. Projected climate changes in the future point to higher temperatures and rainfall decreases. In face of the high intrinsic variability, actions to increase sustainability should improve resilience and stability of the ecosystems. Land use systems based on perennial species, as opposed to annual species, may be more stable and resilient, thus more adequate to face future potential increases in climate variability. Long-term studies to investigate the potential of the native biodiversity or adapted exotic species to design sustainable land use systems should be encouraged.
author2 UFPE; VANDERLISE GIONGO, CPATSA; Instituto Nacional do Semiárido.
author_facet UFPE; VANDERLISE GIONGO, CPATSA; Instituto Nacional do Semiárido.
MENEZES, R. S. C.
SAMPAIO, E. V. S. B.
GIONGO, V.
PÉREZ-MARIN, A. M.
format Artigo de periódico
topic_facet Floresta seca tropical
Fluxo de nutrientes
Bioma Caatinga
Natural resource.
Caatinga
Biodiversidade
Recurso natural
Carbono
Fósforo
Nitrogênio.
author MENEZES, R. S. C.
SAMPAIO, E. V. S. B.
GIONGO, V.
PÉREZ-MARIN, A. M.
author_sort MENEZES, R. S. C.
title Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
title_short Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
title_full Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
title_fullStr Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
title_full_unstemmed Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome.
title_sort biogeochemical cycling in terrestrial ecosystems of the caatinga biome.
publishDate 2013-01-02
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/943753
work_keys_str_mv AT menezesrsc biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT sampaioevsb biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT giongov biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT perezmarinam biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
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