The Balance of Coexistence in Alpine Tundra
We are exploring how feedbacks between plant species and ecosystem
processes can enhance community diversity and stability in moist meadow
alpine tundra. In this system, two functionally different plant species
are able to coexist due to their impacts on nitrogen cycling: net N
mineralization and nitrification rates are four times greater in areas
dominated by Deschampsia caespitosa than areas dominated by Acomastylis
rossii. This species-driven variation occurs within meters and is
as great as the variability across different communities in the tundra.
Deschampsia, directly through rapid N uptake, and Acomastylis,
indirectly through microbial N immobilization of its litter, exert
strong and often equivalent competitive effects (Suding et al.
2004; Suding
et al. 2006).
Because we
anticipate that many alpine species exert strong feedbacks through the
soil microbial community, we are initiating an investigation
of a broader range of species, specifically focusing on species effects
on microbial processes and whether these effects are related to N-form
preferences (inorganic, organic N) of the species and their
competitors. Plant utilization of different forms of nitrogen and
litter inputs of secondary carbon compounds can substantially influence
community and ecosystem dynamics. While both are driven by N
availability and microbial processes, they rarely have been considered
as joint factors contributing to strong biotic feedbacks . We are
exploring these linkages to understand when plant species create such
feedbacks, how these contribute to diversity patterns, and how abiotic
and biotic control varies across the alpine tundra.
- Funded by the Andrew Mellon Foundation (proposal) and NSF Long-term Ecological Research (Niwot Ridge)
- People involved: Isabel Ashton, Marko Spasojevic, Jane Smith, Warren Sconiers
- Related Projects: Woody shrub invasion (Isabel Ashton), Hemiparasites (Marko Spasojevic)
- Recent Presentations: Isabel's ESA 2007 talk (pdf)
We are also investigating how increased nitrogen availability
from
atmospheric deposition may shift species interactions and ecosystem
processes, particularly in the presence of strong plant-soil feedbacks.
This work is based at Niwot Ridge as part of the Long-term Ecological
Research (LTER) project. At larger scales, I lead a synthesis effort
across nine LTER sites to investigate functional responses to nitrogen
inputs across many ecosystems in temperate North America (Suding et al. 2005;
Pennings
et al. 2005; Clark
et al. 2007)
Collaborators: Scott Collins (UNM), Steve Pennings (UH), Chris Clark (UMinn), Elsa Cleland (NCEAS), Laura Gough (UTA), Jim Grace (USGS), Joe Fargione (UNM), Kay Gross (MSU), Daniel Milchunas (CSU). Funded by Niwot Ridge LTER and LTER Network Office.