4.7 Article

Spatial heterogeneity of subsurface soil texture drives landscape-scale patterns of woody patches in a subtropical savanna

Journal

LANDSCAPE ECOLOGY
Volume 32, Issue 4, Pages 915-929

Publisher

SPRINGER
DOI: 10.1007/s10980-017-0496-9

Keywords

Spatial heterogeneity; Subsurface soil texture; Non-argillic inclusions; Argillic horizon; Woody patches; Landscape evolution; Subtropical savanna

Funding

  1. Sid Kyle Graduate Merit Assistantship from Department of Ecosystem Science and Management, Texas AM University
  2. NSF Doctoral Dissertation Improvement Grant [DEB/DDIG-1600790]
  3. Howard McCarley Student Research Award from the Southwestern Association of Naturalist
  4. Exploration Fund Grant from the Explorers Club
  5. USDA/NIFA Hatch Project [1003961]
  6. Direct For Biological Sciences
  7. Division Of Environmental Biology [1600790] Funding Source: National Science Foundation

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Context In the Rio Grande Plains of southern Texas, subtropical savanna vegetation is characterized by a two-phase pattern consisting of discrete woody patches embedded within a C-4 grassland matrix. Prior trench transect studies have suggested that, on upland portions of the landscape, large woody patches (groves) occur on non-argillic inclusions, while small woody patches (clusters) are dispersed among herbaceous vegetation where the argillic horizon is present. Objective To test whether spatial heterogeneity of subsurface soil texture drives the landscape-scale pattern of woody patches in this subtropical savanna. Methods Landscape-scale spatial patterns of soil texture were quantified by taking spatially-specific soil samples to a depth of 1.2 m in a 160 m x 100 m plot. Kriged maps of soil texture were developed, and the locations of non-argillic inclusions were mapped. Results Visual comparison of kriged maps of soil texture to a high resolution aerial photograph of the study area revealed that groves were present exclusively where the non-argillic inclusions were present. This clear visual relationship was further supported by positive correlations between soil sand concentration in the lower soil layers and total fine root biomass which mapped the locations of groves. Conclusions Subsurface non-argillic inclusions may favor the establishment and persistence of groves by enabling root penetration deeper into the profile, providing greater access to water and nutrients that are less accessible on those portions of the landscape where the argillic horizon is present, thereby regulating the distribution of grove vegetation and structuring the evolution of this landscape.

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