SOILS AND GEOENVIRONMENTS OF THE NATIONAL PARK OF VIRUÁ AND SURROUNDING, RORAIMA: INTEGRATED VISION OF THE LANDSCAPE AND ENVIRONMENTAL SERVICE

• Autor(a) principal: Mendonça, Bruno Araujo Furtado de
• Data de Publicação: 2013
• Outros Autores: Fernandes Filho, Elpídio Inácio, Schaefer, Carlos Ernesto Gonçalves Reynaud, Simas, Felipe Nogueira Bello, Vale Junior, José Frutuoso do, Lisboa, Beatriz de Aquino Ribeiro, Mendonça, Júlia Gaio Furtado de
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Ciência Florestal (Online)
• Texto Completo: https://periodicos.ufsm.br/cienciaflorestal/article/view/9287
• topic: Campinaranas; Amazon; sandy soils; carbon stocks; campinaranas; Amazônia; solos arenosos; estoque de carbono

http://dx.doi.org/10.5902/198050989287The Viruá National Park (PARNA Viruá) occupies 227.011ha, in the region of the low ‘Branco’ river, in Roraima state. This area includes an extensive mosaic of complex seasonally flooded forested and non-forested environments. The present work had as general objective to characterize the pedology aspects and the geo-environmental units of the Park and surroundings, in an integrated vision of the landscape and, additionally, estimate the carbon stocks in the soils and geo-environments. We described and collected 29 soil profiles in the main vegetation types of Campinaranas and Forests of PARNA Viruá and surroundings. The main soil classes are: Espodossolo Humilúvico, Neossolo Quartzarênico, Neossolo Flúvico, Neossolo Litólicos, Latossolo Vermelho-Amarelo, Latossolo Vermelho, Cambissolo Háplico, Cambissolo Flúvico, Gleissolo Háplico and Plintossolo Háplico. The soils present spatial distribution marked by abrupt limits and close association with the vegetation type. We identified three pedo-environments: (1) sandy soils of the Campinaranas; (2) soils associated with the inselbergs and adjacencies; and (3) alluvial soils. We mapped and described 18 geoenvironmental units in PARNA Viruá National Park. The main geo-environments are: i) Sandy plains and Paleodunes with grassy and arborous Campinarana on ‘Neossolos Quartzarênicos hidromórficos’ and ‘Espodossolos’; and Floodplains and; ii) Terraces with Igapó Forest on sandy hydromorphic soils, occupying 24.6% and 20.1% of the studied area, respectively. In terms of total soil carbon stocks, the geo-environments of the sandy complexes of Campinaranas and associations stand out, with 9450.9 Gg C. The great extension and representativeness of the sandy areas of Campinaranas characterize PARNA Viruá PArk as an important conservation unit for protection Amazonian sandy soil systems. The areas under the domain of ‘Espodossolos’ possess the largest stocks of organic carbon and the sandy areas of Campinaranas and associations represent the most relevant geo-environment in terms of environmental services and conservation of carbon in the soils.