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 nutrient...

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Main Authors: RSC Menezes, EVSB Sampaio, V Giongo, AM Pérez-Marin
Format: Article
Language:English
Published: Instituto Internacional de Ecologia
Series:Brazilian Journal of Biology
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842012000400004&lng=en&tlng=en
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spelling doaj-4773f3fb8aaa45f8a7154795387f91e02020-11-24T22:26:45ZengInstituto Internacional de EcologiaBrazilian Journal of Biology1678-4375723 suppl64365310.1590/S1519-69842012000400004S1519-69842012000400004Biogeochemical cycling in terrestrial ecosystems of the Caatinga BiomeRSC Menezes0EVSB Sampaio1V Giongo2AM Pérez-Marin3Universidade Federal de PernambucoEmbrapaEmbrapaMinistério da Ciência, Tecnologia e InovaçãoThe 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.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842012000400004&lng=en&tlng=entropical dry forestnutrient fluxescarbonnitrogenphosphorus
collection DOAJ
language English
format Article
sources DOAJ
author RSC Menezes
EVSB Sampaio
V Giongo
AM Pérez-Marin
spellingShingle RSC Menezes
EVSB Sampaio
V Giongo
AM Pérez-Marin
Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome
Brazilian Journal of Biology
tropical dry forest
nutrient fluxes
carbon
nitrogen
phosphorus
author_facet RSC Menezes
EVSB Sampaio
V Giongo
AM Pérez-Marin
author_sort RSC Menezes
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
publisher Instituto Internacional de Ecologia
series Brazilian Journal of Biology
issn 1678-4375
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.
topic tropical dry forest
nutrient fluxes
carbon
nitrogen
phosphorus
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S1519-69842012000400004&lng=en&tlng=en
work_keys_str_mv AT rscmenezes biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT evsbsampaio biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT vgiongo biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
AT amperezmarin biogeochemicalcyclinginterrestrialecosystemsofthecaatingabiome
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