RESUMO

This research identified arbuscular mycorrhizal fungi (AMF) in rhizosphere soil of grapevines with Grapevine Death and Decline symptoms (GDD) or asymptomatic healthy (H) plants, and characterized the relationship of AMF communities with soil chemical attributes. The AMF spore number ranged from 287 to 432 spores 50 cm-³ in soil with GDD plants, and from 357 to 464 spores 50 cm-³ in H plants, with no differences among vineyards or between GDD and H plants within each vineyard. We detected 42 species and 17 genera, and most taxa belonged to Acaulosporaceae or Glomeraceae. Claroideoglomus etunicatum, Funneliformis mosseae, and Archaeospora trappei were the most frequent species in all vineyards. Soil chemical attributes were not determinant for the occurrence of most fungal species; although, Entrophospora infrequens, Diversispora sp1 and Diversispora sp2 were associated with a vineyard having high soil copper. Vineyards harbor highly diverse AMF communities, which are determined by location.

Este trabalho teve como objetivo identificar fungos micorrízicos arbusculares (FMA) em solo rizosférico de videiras com sintomas de declínio e morte da videira (D) e em plantas saudáveis (S), e caracterizar a relação das comunidades de FMA com atributos químicos do solo. O número de esporos de FMA variou de 287 a 432 esporos 50 cm-³ em solo em plantas D, e de 357 a 464 esporos 50 cm-³ em plantas S, sem diferenças entre vinhedos ou entre plantas D e S dentro de cada vinhedo. Detectamos 42 espécies e 17 gêneros, sendo que a maioria dos táxons pertencia a Acaulosporaceae ou Glomeraceae. Claroideoglomus etunicatum, Funneliformis mosseae e Archaeospora trappei foram as espécies mais frequentes em todos os vinhedos. Os atributos químicos do solo não foram determinantes para a ocorrência da maioria das espécies de fungos, embora Entrophospora infrequens, Diversispora sp1 e Diversispora sp2 estivessem associados a um vinhedo com alto teor de cobre do solo. Os vinhedos abrigam comunidades FMA altamente diversificadas, que são determinadas pela localização.

Assuntos

RESUMO

Soil microorganisms play crucial roles in ecosystem functioning, and the central goal in microbial ecology studies is to elucidate which factors shape community structure. A better understanding of the relationship between microbial diversity, functions and environmental parameters would increase our ability to set conservation priorities. Here, the bacterial and archaeal community structure in Atlantic Forest, restinga and mangrove soils was described and compared based on shotgun metagenomics. We hypothesized that each distinct site would harbor a distinct taxonomic and functional soil community, which is influenced by environmental parameters. Our data showed that the microbiome is shaped by soil properties, with pH, base saturation, boron and iron content significantly correlated to overall community structure. When data of specific phyla were correlated to specific soil properties, we demonstrated that parameters such as boron, copper, sulfur, potassium and aluminum presented significant correlation with the most number of bacterial groups. Mangrove soil was the most distinct site and presented the highest taxonomic and functional diversity in comparison with forest and restinga soils. From the total 34 microbial phyla identified, 14 were overrepresented in mangrove soils, including several archaeal groups. Mangrove soils hosted a high abundance of sequences related to replication, survival and adaptation; forest soils included high numbers of sequences related to the metabolism of nutrients and other composts; while restinga soils included abundant genes related to the metabolism of carbohydrates. Overall, our finds show that the microbial community structure and functional potential were clearly different across the environmental gradient, followed by functional adaptation and both were related to the soil properties.

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RESUMO

In this study, we hypothesized that the life history traits of Leiothrix spiralis and L. vivipara would be linked to soil factors of the rupestrian grasslands and that rosette size would be influenced by soil moisture. Soil analyses were performed from five populations of L. spiralis and four populations of L. vivipara. In each area, three replicates were employed in 19 areas of occurrence of Leiothrix species, and we quantified the life history attributes. The microhabitats of these species show low favorability regarding to soil factors. During the dry season, their rosettes decreased in diameter due the loss of its most outlying leaves. The absence of seedlings indicated the low fecundity of both species. However, both species showed rapid population growth by pseudovivipary. Both L. spiralis and L. vivipara exhibit a kind of parental care that was quantified by the presence of connections between parental-rosettes and ramets. The findings of the present study show that the life history traits are linked to soil factors.(AU)

Neste estudo, testamos a hipótese de que os traços da história de vida de Leiothrix spiralis e L.vivipara estariam ligados a fatores do solo dos campos rupestres, e que o tamanho de roseta seria influenciado pela umidade do solo. As análises de solo foram realizadas a partir de cinco populações de L. spiralis e quatro populações de L. vivipara. Em cada área, três repetições foram empregadas em 19 áreas de ocorrência das espécies de Leiothrix, e quantificamos os atributos de história de vida. Os microhabitats destas espécies apresentam baixa “favorabilidade” em relação aos fatores de solo. Durante a estação seca, as rosetas diminuíram de diâmetro devido à perda de suas folhas mais periféricas. A ausência de plântulas indicou a baixa fecundidade de ambas as espécies. No entanto, ambas as espécies apresentaram crescimento rápido da população por pseudoviviparidade. Tanto L. spiralis quanto L. vivipara exibem um tipo de cuidado parental que foi quantificada pela presença de conexões entre rosetas parentais e rametes. Os resultados do presente estudo mostram que os traços da história de vida estão ligados aos fatores do solo.(AU)

Assuntos

RESUMO

In this study, we hypothesized that the life history traits of Leiothrix spiralis and L. vivipara would be linked to soil factors of the rupestrian grasslands and that rosette size would be influenced by soil moisture. Soil analyses were performed from five populations of L. spiralis and four populations of L. vivipara. In each area, three replicates were employed in 19 areas of occurrence of Leiothrix species, and we quantified the life history attributes. The microhabitats of these species show low favorability regarding to soil factors. During the dry season, their rosettes decreased in diameter due the loss of its most outlying leaves. The absence of seedlings indicated the low fecundity of both species. However, both species showed rapid population growth by pseudovivipary. Both L. spiralis and L. vivipara exhibit a kind of parental care that was quantified by the presence of connections between parental-rosettes and ramets. The findings of the present study show that the life history traits are linked to soil factors.

Neste estudo, testamos a hipótese de que os traços da história de vida de Leiothrix spiralis e L.vivipara estariam ligados a fatores do solo dos campos rupestres, e que o tamanho de roseta seria influenciado pela umidade do solo. As análises de solo foram realizadas a partir de cinco populações de L. spiralis e quatro populações de L. vivipara. Em cada área, três repetições foram empregadas em 19 áreas de ocorrência das espécies de Leiothrix, e quantificamos os atributos de história de vida. Os microhabitats destas espécies apresentam baixa “favorabilidade” em relação aos fatores de solo. Durante a estação seca, as rosetas diminuíram de diâmetro devido à perda de suas folhas mais periféricas. A ausência de plântulas indicou a baixa fecundidade de ambas as espécies. No entanto, ambas as espécies apresentaram crescimento rápido da população por pseudoviviparidade. Tanto L. spiralis quanto L. vivipara exibem um tipo de cuidado parental que foi quantificada pela presença de conexões entre rosetas parentais e rametes. Os resultados do presente estudo mostram que os traços da história de vida estão ligados aos fatores do solo.

Assuntos