Soil Microbes in Ecological Restoration
By restoration scientists Elizabeth Bach, Jonathan Bauer, and Liz Koziol
Increasingly, ecological restoration goals include belowground ecosystem services including reducing soil erosion, retaining soil nutrients, restoring plant-soil feedbacks, and potentially storing carbon to reduce CO2 concentrations in the atmosphere. Soil organisms are involved in providing all these services, as such, interest in soil communities is booming in the restoration community.
Within the tallgrass prairies of the Midwest and Great Lakes region, there has been exciting progress made in this area of research, with scientists advancing our foundational knowledge of soil ecology, gaining insights into how soil microbial communities respond to ecological management, and developing techniques for the reintroduction of soil microbial communities to restoration sites. At the 2016 meeting of the SER MWGL, we organized a symposium featuring early and mid-career scientists actively contributing to this rapidly developing field. The symposium featured Dr. Kathryn Docherty (Western Michigan University), Dr. Sara Baer (Southern Illinois University Carbondale), Dr. Elizabeth Bach (Illinois Natural History Survey), Dr. Jonathan Bauer (Indiana University), and Liz Koziol (Indiana University).
Kathryn Docherty kicked-off the symposium sharing her research focused on the function of soil microbial communities and their recovery in restored tallgrass prairie.
Even 65 years after restoration, prairie soil microbes stored less carbon, released more CO2 than in remnants –@DrDocherty #sermwgl2016
— Dr. Anna Groves (@annamgroves) April 1, 2016
This is an important finding for two reasons. First, it emphasizes the importance of protecting the limited native prairie left in order to keep soil carbon out of the atmosphere. Second, microbial recovery may take much longer than aboveground recovery. However, it might be possible to restore soil communities and their effects on the soil. Docherty found that inoculation with microbes from remnant prairies and planting of diverse plant communities can stabilize microbe-driven carbon cycling.
Sara Baer built on these conclusions with a cross-continental dataset. Her work from restored grasslands in Nebraska, Illinois, Kansas, and the Free State, South Africa show that abiotic soil factors, like soil texture, play an important role in recovery of microbially-mediated soil functions like carbon and nitrogen storage. Even when aboveground plant community recovery was similar, belowground communities did not recover on similar trajectories. This provides another key insight, that soil type may be an important consideration when prioritizing sites for ecological restoration to meet goals focused on belowground ecosystem services.
#MWGLSER2016 Microbes, not just roots, increase soil C in restored prairie @SoilOrgMatters
— Elizabeth Bach (@SoilOrgMatters) April 1, 2016
Elizabeth Bach focused on soil fungal community recovery in restored and remnant prairies across Illinois. Supporting the conclusions of Docherty and Baer, Bach found distinct fungal communities in restorations compared with remnants, and this pattern was consistent on different soil types at multiple locations. In addition, microbial activity varied within the growing season, and these seasonal patterns were also similar across soil types and in remnants and restorations, although overall activity was greater on silty loam soils. These data are very important to restoration practices because they suggest some microbial recovery patterns are consistent across sites.
Jonathan Bauer dove deeper into soil fungal community relationships, sharing his work using fungi to facilitate the establishment of “late-successional” prairie plants:
It's the late successional plants that are the most benefitted by AMF associations in restoration says @JonathanTBauer #sermwgl2016
— Dr. Anna Groves (@annamgroves) April 1, 2016
Bauer’s work shows that fungi, particularly arbuscular mycorrhizal fungi that form mutualistic associations with plants, are important to the establishment and success of many desired plant species with high floristic quality in prairie restoration. Bauer showed that early successional species, many of which have low floristic quality, are most likely to establish in a restoration and are less mycorrhizal, such as Ambrosia artemesiifolia and Rudbeckia hirta. In contrast, plants that are late successional plants and of high floristic quality tend to be both very responsive to soil fungi and are less likely to establish from seed in a restoration, such as Amorpha canescens and Veronicastrum virginicum.
AMF dependent plants difficult to restore. Koziol up next, reporting on restoration of AMF symbiosis #SERMWGL2016 pic.twitter.com/u2tsbaLHUP
— Jonathan Bauer (@JonathanTBauer) April 1, 2016
Liz Koziol rounded out the symposium sharing her exciting work using inoculations of soil microbial communities to improve late successional establishment in tallgrass prairie restoration.
AM fungi double the seed recruitment of late successional species – Koziol #sermwgl2016
— Jonathan Bauer (@JonathanTBauer) April 1, 2016
#MWGLSER2016 Koziol: AM fungi reduced non-desirable biomass by 50%
— Elizabeth Bach (@SoilOrgMatters) April 1, 2016
Koziol demonstrated that adding prairie microbial inocula, specifically arbuscular mycorrhizal fungi acquired from remnant prairie soils, can be effective at improving the establishment of high quality prairie plant communities from seed plantings. Liz found that the particular composition of arbuscular fungal species at a restoration site can have dramatic effects on the plant species that establish there, as some fungi promote weeds while other promote desirable species. Liz cautioned against many commercially propagated inocula sources, where origin and quality of the fungi is unknown. Instead, Koziol suggested that adding a diverse AM fungal inocula from an undisturbed reference site more quickly facilitates late successional prairie establishment.
The symposium ended with open questions for all speakers from the audience. The engaging discussion included questions about how restoration practitioners can incorporate new belowground knowledge and measure success of belowground recovery. Here’s what the panelists suggested:
- Baer: easiest, quickest single measure of belowground recovery is soil bulk density, essentially the density of a known volume of soil. Soil density covaries with microbial communities and functioning
- Docherty: get roots in the ground, establishing plants is key to microbial recovery, although belowground recovery will be much slower
- Bach: feed the microbes to feed the full ecosystem, more roots and inputs to microbes will increase belowground functioning and feed the aboveground community
- Koziol: consider inoculations, but source is very important. Consider fungal/microbial nurseries that produce native and locally adapted microbial inocula, just like plant nurseries
- Bauer: target to site goals, different goals may require different actions, if goal is establishing a late-successional plant community, invest lots in AMF mutualisms
Relevant additional reading on the topic of soil microbes in restored environments:
- Bach, Elizabeth M., et al. “Soil texture affects soil microbial and structural recovery during grassland restoration.” Soil Biology and Biochemistry 42.12 (2010): 2182-2191.
- Bach, Elizabeth M., & Hofmockel, K.S. “Coupled Carbon and Nitrogen Inputs Increase Microbial Biomass and Activity in Prairie Bioenergy Systems” Ecosystems 18.3(2015): 417-427
- Baer, Sara G., et al. “Belowground ecosystem recovery during grassland restoration: South African Highveld compared to US tallgrass prairie.” Ecosystems 18.3 (2015): 390-403.
- Baer, S. G., et al. “Changes in ecosystem structure and function along a chronosequence of restored grasslands.” Ecological Applications 12.6 (2002): 1688-1701.
- Baer, S. G., C. K. Meyer, E. M. Bach, R. P. Klopf, and J. Six. 2010. Contrasting ecosystem recovery on two soil textures: implications for carbon mitigation and grassland conservation. Ecosphere 1(1):art5
- Bauer, Jonathan T., Keenan ML Mack, and James D. Bever. 2015. Plant-soil feedbacks as drivers of succession: evidence from remnant and restored tallgrass prairies. Ecosphere 6.9 art158.
- Docherty, Kathryn M. & Gutknecht. “The role of environmental microorganisms in ecosystem responses to global change: Current state of research and future outlooks.” Biogeochemistry 109 (2012):1-6
- Docherty, Kathryn M. et al. “Key Edaphic Properties Largely Explain Temporal and Geographic Variation in Soil Microbial Communities across Four Biomes” PLoS One 10 (2015): e0135352. doi:10.1371/journal.pone.0135352
- Koziol, Liz, and James D. Bever. “Mycorrhizal response trades off with plant growth rate and increases with plant successional status.” Ecology 96.7 (2015): 1768-1774.
- Maltz, M. R. and Treseder, K. K. (2015), Sources of inocula influence mycorrhizal colonization of plants in restoration projects: a meta-analysis. Restoration Ecology, 23: 625–634. doi: 10.1111/rec.12231
- Middleton, E. L., S. Richardson, L. Koziol, C. E. Palmer, Z. Yermakov, J. A. Henning, P. A. Schultz, and J. D. Bever. 2015. Locally adapted arbuscular mycorrhizal fungi improve vigor and resistance to herbivory of native prairie plant species. Ecosphere 6(12):276. http://dx.doi.org/10.1890/ES15-00152.1