Folia Geobotanica

, Volume 50, Issue 3, pp 175–184 | Cite as

Landforms and soil attributes determine the vegetation structure in the Brazilian semiarid

  • Daniel M. Arruda
  • Carlos E. G. R. Schaefer
  • Guilherme R. Corrêa
  • Priscyla M. S. Rodrigues
  • Reinaldo Duque-Brasil
  • Walnir G. Ferreira-JR
  • Ary T. Oliveira-Filho
Article

Abstract

The semiarid region of Brazil consists of a great variety of landscapes, soils and vegetation forms, with complex interrelations. In order to better understand this interplay, we posed two questions: Are there greater pedological similarities among the different landforms of the same catena or among the same landforms from different catenas? Which soil attributes could be the most important to segregate communities of plants? We sampled soils and vegetation on different landforms in four different catenas and performed NMS (non-metric multidimensional scaling) and ANOVA (analysis of variance) to address the first question; also, we carried another NMS following GLM (general linear model regression) to answer the second question. The first NMS indicated the existence of a fertility gradient, grouping communities in relation to similar landforms, confirmed by ANOVA. The second NMS indicated the same gradient whereas the GLM showed that is controlled by aluminum saturation, sodium saturation, phosphorous and sand content. One extreme of the gradient has uplands associated with cerrado vegetation forms whereas the other extreme slopes were associated with dry forests. The lowlands associated with dry forest represent the central position of the fertility gradient. In general, soils at similar landforms showed greater pedological similarity, and their physico-chemical attributes determined the formation and structure of vegetation. This similarity across the same landform refers to the comparable soil formation at each landform and soil age at landscape scale. The characteristics of the vegetation and soils in the Brazilian southern semiarid region indicated a previously wetter climate, during which deep weathered latosols (oxisols) were formed and remain as relics in the present semiarid.

Keywords

cerrado climate transition gradient of vegetation seasonally dry tropical forest semiarid geomorphology vegetation-soil relationship 

Notes

Acknowledgements

Authors thank the FAPEMIG Foundation (Fundação de Amparo à Pesquisa de Minas Gerais) and the State Secretary of Science and Technology (SECTES-MG) for financing this project. We are grateful for Andreza Neri, Rubens Santos and Rúbia Fonseca for suggestions to the first version of rhw manuscript; Luiz Magnago for his suggestions and statistical support; Marcio Batista, Davi Gjorup, Bruno Vasconcelos and Vitor Moura for rich discussions during field work and Rubens Santos for identification of the botanical material. We also thank both anonymous reviewers, who provide valuable comments on earlier version of this paper.

Supplementary material

12224_2015_9221_MOESM1_ESM.docx (14 kb)
ESM 1 (DOCX 14 kb)

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Copyright information

© Institute of Botany, Academy of Sciences of the Czech Republic 2015

Authors and Affiliations

  • Daniel M. Arruda
    • 1
  • Carlos E. G. R. Schaefer
    • 2
  • Guilherme R. Corrêa
    • 3
  • Priscyla M. S. Rodrigues
    • 1
  • Reinaldo Duque-Brasil
    • 4
  • Walnir G. Ferreira-JR
    • 5
  • Ary T. Oliveira-Filho
    • 6
  1. 1.Departamento de Biologia VegetalUniversidade Federal de ViçosaViçosaBrasil
  2. 2.Departamento de SolosUniversidade Federal de ViçosaViçosaBrasil
  3. 3.Universidade Federal de UberlândiaUberlândiaBrasil
  4. 4.Universidade Federal de Juiz de ForaGovernador ValadaresBrasil
  5. 5.Instituição Federal de Educação, Ciência e Tecnologia do Sul de MinasMachadoBrasil
  6. 6.Departamento de BotânicaUniversidade Federal de Minas GeraisBelo HorizonteBrasil

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