Abstract

AbstractMany soils are deep, yet soil below 20 cm remains largely unexplored. Exotic plants can have shallower roots than native species, so their impact on microorganisms is anticipated to change with depth. Using environmental DNA and extracellular enzymatic activities, we studied fungal and bacterial community composition, diversity, function, and co‐occurrence networks between native and exotic grasslands at soil depths up to 1 m. We hypothesized (1) the composition and network structure of both fungal and bacterial communities will change with increasing depth, and diversity and enzymatic function will decrease; (2) microbial enzymatic function and network connectedness will be lower in exotic grasslands; and (3) irrigation will alter microbial networks, increasing the overall connectedness. Microbial diversity decreased with depth, and community composition was distinctly different between shallow and deeper soil depths with higher numbers of unknown taxa in lower soil depths. Fungal communities differed between native and exotic plant communities. Microbial community networks were strongly shaped by biotic and abiotic factors concurrently and were the only microbial measurement affected by irrigation. In general, fungal communities were more connected in native plant communities than exotic, especially below 10 cm. Fungal networks were also more connected at lower soil depths albeit with fewer nodes. Bacterial communities demonstrated higher complexity, and greater connectedness and nodes, at lower soil depths for native plant communities. Exotic plant communities’ bacterial network connectedness altered at lower soil depths dependent on irrigation treatments. Microbial extracellular enzyme activity for carbon cycling enzymes significantly declined with soil depth, but enzymes associated with nitrogen and phosphorus cycling continued to have similar activities up to 1 m deep. Our results indicate that native and exotic grasslands have significantly different fungal communities in depths up to 1 m and that both fungal and bacterial networks are strongly shaped jointly by plant communities and abiotic factors. Soil depth is independently a major determinant of both fungal and bacterial community structures, functions, and co‐occurrence networks and demonstrates further the importance of including soil itself when investigating plant–microbe interactions.

Highlights

  • Exotic plant species are increasing in abundance, often forming novel ecosystems with species that lack an evolutionary history (Hobbs et al 2006, 2013, Wilsey et al 2009, Cook-Patton et al 2011)

  • We hypothesized (1) the composition and network structure of both fungal and bacterial communities will change with increasing depth, and diversity and enzymatic function will decrease; (2) microbial enzymatic function and network connectedness will be lower in exotic grasslands; and (3) irrigation will alter microbial networks, increasing the overall connectedness

  • As we found previously (Checinska-Sielaff et al 2018), fungal communities were more strongly impacted by the plant community treatment than bacterial communities, demonstrating that novel grassland ecosystems have altered soil fungal communities compared with the native grasslands that they replaced

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Summary

Introduction

Exotic plant species are increasing in abundance, often forming novel ecosystems with species that lack an evolutionary history (Hobbs et al 2006, 2013, Wilsey et al 2009, Cook-Patton et al 2011). A shift from native to exotic plant species could have large and longlasting impacts on soil microorganisms and elemental cycling by altering substrate inputs (Seastedt et al 2008, Pries et al 2018). These differences could be exacerbated if native and exotic plant species respond differently to climatic events, including extreme rainfall or drought events, due to their different rooting depths (Singh et al 1998, Heisler-White et al 2009, Hodge 2009, Maestre et al 2012, Hoover et al 2015, Bernardo et al 2016). Interactions between plants and microbes deeper in the soil profile may contribute to C accumulation, resulting in over two-thirds of soil C occurring below 30 cm (Balesdent et al 2018), as evidenced in the large pool (~2000 Pg) of organic C in the top 1 m of Earth’s soil (Janzen 2005)

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