96th ESA Annual Meeting (August 7 -- 12, 2011)

PS 66-130 - Changes in soil C, N, and P storage following woody plant invasion of grassland

Thursday, August 11, 2011
Exhibit Hall 3, Austin Convention Center
Ilsa B. Kantola, Ecosystem Science and Management, Texas A&M University, College Station, TX, Thomas W. Boutton, Ecology and Conservation Biology, Texas A&M University, College Station, TX, Timothy R. Filley, Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN and C. Thomas Hallmark, Soil and Crop Sciences, Texas A&M University, College Station, TX
Background/Question/Methods

Many grass-dominated ecosystems around the world have experienced woody plant encroachment over the last century due to livestock grazing, fire suppression, and/or changes in climate and atmospheric chemistry.  In the Rio Grande Plains of Texas, subtropical thorn woodlands dominated by N-fixing tree legumes have largely replaced grasslands and altered the biogeochemistry of this region.  The purpose of this study was to assess the impact of this grassland-to-woodland transition on the size and distribution of soil C, N, and P pools across five landscape elements of a mesquite-invaded grassland.  Soil samples (0-10 cm) were collected in remnant grasslands and near the centers of woody plant clusters, groves, drainage woodlands, and playas ranging in age from 14 to 134 years in a subtropical savanna parkland in southern Texas.  Soil organic C and total N were measured by elemental analysis, and total P was measured by lithium fusion followed by phospho-molybdate colorimetry.  

Results/Conclusions

Concentrations of soil C, N, and P increased linearly in all wooded landscape elements with time following woody encroachment.  Mean soil organic C increased between 320 and 460% in wooded areas compared to remnant grasslands.   Similarly, soil total N increased 285-535% and total P increased 160-340% in wooded areas.  The most dramatic increases were observed in the lowland drainages and playas, while C, N, and P increased at slower rates in upland woody clusters and groves.   Woody plant invasion likely increases C and N pools in the soil through increased NPP and symbiotic N-fixation by legume species, respectively.  Soil P likely increases because the more deeply rooted woody plants are acquiring P from deep in the soil profile and transferring it into the upper portion of the profile via litterfall and root turnover.  Since N and P are generally the most limiting nutrients in terrestrial ecosystems, increased stores of these elements are likely to alter rates of microbial processes, plant-microbe and plant-plant interactions, and successional dynamics in this ecosystem.