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-1 and 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.

Biogeochemical cycling in terrestrial ecosystems of the Caatinga Biome / Ciclagem biogeoquímica em ecossistemas terrestres do Bioma Caatinga

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.

Os ciclos biogeoquímicos de C, N, P e água, os impactos das mudanças do uso da terra nos estoques e fluxos destes elementos e como estas mudanças podem afetar a estrutura e o funcionamento da Caatinga foram revisados. Cerca da metade desse Bioma ainda é coberta por vegetação nativa secundária. Os solos são deficientes em nutrientes, principalmente N e P. A concentração média, na camada superficial (0-20 cm), de P total é 196 mg kg-1, e a de C é 9.3 g kg-1, correspondendo a estoques médios em torno de 23 Mg ha-1 de carbono. A biomassa aérea da vegetação varia entre 30 a 50 Mg ha-1, e a biomassa radicular entre 3 a 12 Mg ha-1. As produtividades e acumulações anuais de biomassa nos diferentes usos da terra variam de 1 a 7 Mg ha-1. A fixação biológica de N2 atmosférico é estimada em 3 a 11 kg N ha-1 ano-1 e 21 a 26 kg N ha-1 ano-1 em Caatinga madura e em regeneração, respectivamente. Os principais processos de perda de nutrientes e água são queimadas, erosão do solo, escoamento e colheita de cultivos e produtos animais. As mudanças climáticas projetadas indicam maiores temperaturas e menores precipitações. Considerando a alta variabilidade intrínseca, ações para aumentar a sustentabilidade deveriam melhorar a resiliência e a estabilidade dos ecossistemas. Sistemas de uso da terra baseados em espécies perenes, em contraposição a anuais, devem ser mais estáveis e resilientes, portanto mais adequados para enfrentar os potenciais aumentos na variabilidade climática. Estudos de longa duração para avaliar o potencial da biodiversidade nativa ou de exóticas adaptadas no delineamento de sistemas de uso sustentáveis deveriam ser encorajados.

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.

Os ciclos biogeoquímicos de C, N, P e água, os impactos das mudanças do uso da terra nos estoques e fluxos destes elementos e como estas mudanças podem afetar a estrutura e o funcionamento da Caatinga foram revisados. Cerca da metade desse Bioma ainda é coberta por vegetação nativa secundária. Os solos são deficientes em nutrientes, principalmente N e P. A concentração média, na camada superficial (0-20 cm), de P total é 196 mg kg-1, e a de C é 9.3 g kg-1, correspondendo a estoques médios em torno de 23 Mg ha-1 de carbono. A biomassa aérea da vegetação varia entre 30 a 50 Mg ha-1, e a biomassa radicular entre 3 a 12 Mg ha-1. As produtividades e acumulações anuais de biomassa nos diferentes usos da terra variam de 1 a 7 Mg ha-1. A fixação biológica de N2 atmosférico é estimada em 3 a 11 kg N ha-1 ano-1 e 21 a 26 kg N ha-1 ano-1 em Caatinga madura e em regeneração, respectivamente. Os principais processos de perda de nutrientes e água são queimadas, erosão do solo, escoamento e colheita de cultivos e produtos animais. As mudanças climáticas projetadas indicam maiores temperaturas e menores precipitações. Considerando a alta variabilidade intrínseca, ações para aumentar a sustentabilidade deveriam melhorar a resiliência e a estabilidade dos ecossistemas. Sistemas de uso da terra baseados em espécies perenes, em contraposição a anuais, devem ser mais estáveis e resilientes, portanto mais adequados para enfrentar os potenciais aumentos na variabilidade climática. Estudos de longa duração para avaliar o potencial da biodiversidade nativa ou de exóticas adaptadas no delineamento de sistemas de uso sustentáveis deveriam ser encorajados.

Pressure-induced formation of inactive triple-shelled rotavirus particles is associated with changes in the spike protein Vp4.

Rotaviruses are non-enveloped, triple-shelled particles that cause enteritis in animals and humans. The interactions among the different viral proteins located in the three concentric layers make the rotavirus particle an excellent model for physico-chemical and biological studies of viral assemblage. SA11-4S rotaviruses subjected to high pressure were inactivated by more than five log units. After pressure treatment, the particles were recovered with slight structural changes when compared to the control. Electron microscopy suggested subtle changes in the viral outer layer in some pressurised particles. Fluorescence spectroscopy showed that much more dramatic changes were produced by urea denaturation than by pressure. Based on the fluorescence spectrum, the genome resistance to ribonuclease, and the absence of changes in hydrodynamic properties, there was little or no disruption of the capsid under pressure. On the other hand, hemagglutination assays indicated that the main component affected by pressure was the spike protein VP4, thus accounting for changes in interaction with host cells and greatly reduced infectivity. The changes leading to inactivation did not cause removal of VP4 from the outer capsid, as verified by size-exclusion chromatography. Antibodies raised against pressurised material were as effective as antibodies raised against the intact virus, based on their neutralisation titre in plaque reduction assays, enzyme-linked immunosorbent assays and direct interaction with the particle, as measured by gel-filtration chromatography. Therefore, the new conformation of the pressurised particle did not result in loss of immunogenicity. We propose that pressure alters the receptor-binding protein VP4 by triggering changes similar to those produced when the virus interacts with target cells. As the changes in VP4 conformation caused by pressure occur prior to virus exposure to target cells, it leads to non-infectious particles and may lead to the exposure of previously occult epitopes, important for vaccine development.

Effects of hydrostatic pressure on the Leptospira interrogans: high immunogenicity of the pressure-inactivated serovar hardjo.

The Hardjoprajitno strain of Leptospira interrogans serovar hardjo was subjected to different hydrostatic pressures. Complete inactivation occurred when the leptospires were treated with 2 kbar for 60 min. Electron microscopy showed dislocation of the outer membrane, partial loss of the helical shape and extrusion of the axial filament from the cytoplasmic cylinder of the pressurized leptospires. When the pressure-treated leptospires were inoculated into rabbits they were highly immunogenic. The sera of these animals presented a titer of 2048 in the microscopic serum agglutination reaction. Fluorescence measurements indicated that the action of pressure on the leptospires might have resulted from perturbation on membrane protein components, permitting the binding of the fluorescent probe bis (8-anilinonaphthalene-1-sulfonate) (Bis-ANS). This is the first report of the use of hydrostatic pressure to inactivate pathogenic bacteria with the potential to lead to a vaccine.