4.7 Article

Plant removal across an elevational gradient marginally reduces rates, substantially reduces variation in mineralization

Journal

ECOLOGY
Volume 103, Issue 1, Pages -

Publisher

WILEY
DOI: 10.1002/ecy.3546

Keywords

biodiversity loss; carbon mineralization; elevational gradient; nitrogen mineralization; plant removal; plant-soil linkages

Categories

Funding

  1. Semper Ardens grant from the Carlsbergfondet
  2. Catalyst Grant from the Gund Institute for Environment at the University of Vermont
  3. NSF [MRI-0821369]
  4. DOE
  5. National Science Foundation Graduate Research Fellowship Program [NSF-16-588]

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The study examined the impact of plant species loss on belowground function in ecosystems with different climatic conditions and soil properties. The results showed that plant removal decreased the variation in potential nitrogen mineralization rates and marginally reduced the magnitude of nitrogen mineralization rates, while carbon mineralization rates were sensitive to climatic and soil differences. Plant removal had little impact on soil enzyme activity.
The loss of aboveground plant diversity alters belowground ecosystem function; yet, the mechanisms underpinning this relationship and the degree to which plant community structure and climate mediate the effects of plant species loss remain unclear. Here, we explored how plant species loss through experimental removal shaped belowground function in ecosystems characterized by different climatic regimes and edaphic properties. We measured plant community composition as well as potential carbon (C) and nitrogen (N) mineralization and microbial extracellular enzyme activity in soils collected from four unique plant removal experiments located along an elevational gradient in Colorado, USA. We found that, regardless of the identity of the removed species or the climate at each site, plant removal decreased the absolute variation in potential N mineralization rates and marginally reduced the magnitude of N mineralization rates. While plant species removal also marginally reduced C mineralization rates, C mineralization, unlike N mineralization, displayed sensitivity to the climatic and edaphic differences among sites, where C mineralization was greatest at the high elevation site that receives the most precipitation annually and contains the largest soil total C pool. Plant removal had little impact on soil enzyme activity. Removal effects were not contingent on the amount of biomass removed annually, and shifts in mineralization rates occurred despite only marginal shifts in plant community structure following plant species removal. Our results present a surprisingly simple and consistent pattern of belowground response to the loss of dominant plant species across an elevational gradient with different climatic and edaphic properties, suggesting a common response of belowground ecosystem function to plant species loss regardless of which plant species are lost or the broader climatic context.

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