Please use this identifier to cite or link to this item: http://www.repositorio.ufop.br/handle/123456789/8282
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dc.contributor.authorMessias, Maria Cristina Teixeira Braga-
dc.contributor.authorLeite, Mariangela Garcia Praça-
dc.contributor.authorMeira Neto, João Augusto Alves-
dc.contributor.authorKozovits, Alessandra Rodrigues-
dc.contributor.authorTavares, Ricardo-
dc.date.accessioned2017-07-20T13:20:44Z-
dc.date.available2017-07-20T13:20:44Z-
dc.date.issued2013-
dc.identifier.citationMESSIAS, M. C. T. B. et al. Soil-vegetation relationship in quartzitic and ferruginous Brazilian rocky outcrops. Folia Geobotanica Pruhonice, v. 48, p. 509–521 , 2013. Disponível em: <https://link.springer.com/article/10.1007/s12224-013-9154-4>. Acesso em: 20 de jun. 2017.pt_BR
dc.identifier.issn18749348-
dc.identifier.urihttp://www.repositorio.ufop.br/handle/123456789/8282-
dc.description.abstractCampo rupestre is a kind of Brazilian rocky outcrop with high biodiversity and many endemic and threatened species. It occurs mainly in the Espinhaço Range in a contact region between Cerrado and/or Caatinga and Atlantic Forest. The Espinhaço Range is recognized as a region with the highest floristic diversity in South America and with many endemic species, most of which are associated with rocky outcrop environments. These, among other peculiarities, recently granted the Espinhaço Range the status of Biosphere Reserve. The relationship between soil and vegetation was studied in campo rupestre areas with quartzite and itabirite rocks. Three habitats in both lithologies were defined by geomorphology as: 1. Slopes with grasslands; 2. Plateaus with grasslands and 3. Valleys with woody savannas. In each lithology, 30 plots (10 × 10 m), 10 in each habitat, were defined. The species and their respective coverage were recorded and soil was sampled to perform chemical and physical analyses. The analyzed soils were similar in being sandy, acidic and with low fertility. Nevertheless, they exhibited differences in chemical and physical properties. Altogether there were 272 species, belonging to 70 families. The canonical correspondence analysis of soil variables and species coverage showed a clear segregation of lithological sites due mainly to the exchangeable content of Ca, Cu, Mg, Mn and S; soil particle size – central tendency and sorting; and the percentage of silt, fine soil and bare rocks. A strong correlation between plant species coverage and soil properties was also found.pt_BR
dc.language.isoen_USpt_BR
dc.rightsrestritopt_BR
dc.subjectFerruginous campos rupestrespt_BR
dc.subjectMetalliferous soilpt_BR
dc.subjectPlant-soil relationshipspt_BR
dc.subjectRocky outcrop vegetationpt_BR
dc.titleSoil-vegetation relationship in quartzitic and ferruginous Brazilian rocky outcrops.pt_BR
dc.typeArtigo publicado em periodicopt_BR
dc.identifier.uri2https://link.springer.com/article/10.1007/s12224-013-9154-4pt_BR
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