Belowground impacts of alpine woody encroachment are determined by plant traits, local climate, and soil conditions

Courtney G. Collins, Marko J. Spasojevic, Concepción L. Alados, Emma L. Aronson, Juan C. Benavides, Nicoletta Cannone, Chatrina Caviezel, Oriol Grau, Hui Guo, Gaku Kudo, Nikolas J. Kuhn, Jana Müllerová, Michala L. Phillips, Nuttapon Pombubpa, Frédérique Reverchon, Hannah B. Shulman, Jason E. Stajich, Alexia Stokes, Sören E. Weber, Jeffrey M. Diez

Research output: Contribution to journalArticlepeer-review

32 Scopus citations

Abstract

Global climate and land use change are causing woody plant encroachment in arctic, alpine, and arid/semi-arid ecosystems around the world, yet our understanding of the belowground impacts of this phenomenon is limited. We conducted a globally distributed field study of 13 alpine sites across four continents undergoing woody plant encroachment and sampled soils from both woody encroached and nearby herbaceous plant community types. We found that woody plant encroachment influenced soil microbial richness and community composition across sites based on multiple factors including woody plant traits, site level climate, and abiotic soil conditions. In particular, root symbiont type was a key determinant of belowground effects, as Nitrogen-fixing woody plants had higher soil fungal richness, while Ecto/Ericoid mycorrhizal species had higher soil bacterial richness and symbiont types had distinct soil microbial community composition. Woody plant leaf traits indirectly influenced soil microbes through their impact on soil abiotic conditions, primarily soil pH and C:N ratios. Finally, site-level climate affected the overall magnitude and direction of woody plant influence, as soil fungal and bacterial richness were either higher or lower in woody encroached versus herbaceous soils depending on mean annual temperature and precipitation. All together, these results document global impacts of woody plant encroachment on soil microbial communities, but highlight that multiple biotic and abiotic pathways must be considered to scale up globally from site- and species-level patterns. Considering both the aboveground and belowground effects of woody encroachment will be critical to predict future changes in alpine ecosystem structure and function and subsequent feedbacks to the global climate system.

Original languageEnglish
Pages (from-to)7112-7127
Number of pages16
JournalGlobal Change Biology
Volume26
Issue number12
DOIs
StatePublished - Dec 2020
Externally publishedYes

Funding

This research was funded by an NSF Doctoral Dissertation Improvement Grant (DDIG) (Award No. (FAIN): DEB-1701979) awarded to C.G.C. and J.M.D. C.G.C. was also supported by a UC President's Dissertation Year Fellowship and a UCR Graduate Dean's Dissertation Research Grant. M.J.S. was supported by the Niwot Ridge LTER (NSF DEB-1637686). A.S. and F.R. were supported by the French and Mexican governments (ECOPICS project, ANR–16-CE03-0009 and CONACYT–2 73659). J.M. was supported by a long-term research development project RVO 67985939 (The Czech Academy of Sciences) and Fulbright Grant. C.L.A. was supported by the Ministerio de Economía y Competitividad-MINECO Project Nº: CGL2016-80783-R. O.G. was supported by the ERC Synergy project, SyG-2013-610028 IMBALANCE-P and an INTERACT grant agreement No: 730938 EU-H2020. J.E.S. is a CIFAR Fellow in the program Fungal Kingdom: Threats and Opportunities and supported by United States Department of Agriculture—National Institute of Food and Agriculture Hatch project CA-R-PPA-5062-H. N.P. was supported by a Royal Thai Government Fellowship. J.C.B. acknowledges the support of Javeriana University. We thank Maximillien Osbourne-Thacker, Amulya Kunduru, and Chloe Hull for assistance with processing soil samples and molecular sequencing prep. We thank the following for assistance with site selection, plant identification, and soil sampling: Nevados National Park in Colombia and its staff, Katrin Sieron, Marco Morales, Leonor Jiménez, Daniel Hernández, Fabien Anthelme, Luis Merino-Martin, and Miguel Castillo. This research was funded by an NSF Doctoral Dissertation Improvement Grant (DDIG) (Award No. (FAIN): DEB‐1701979) awarded to C.G.C. and J.M.D. C.G.C. was also supported by a UC President's Dissertation Year Fellowship and a UCR Graduate Dean's Dissertation Research Grant. M.J.S. was supported by the Niwot Ridge LTER (NSF DEB‐1637686). A.S. and F.R. were supported by the French and Mexican governments (ECOPICS project, ANR–16‐CE03‐0009 and CONACYT–2 73659). J.M. was supported by a long‐term research development project RVO 67985939 (The Czech Academy of Sciences) and Fulbright Grant. C.L.A. was supported by the Ministerio de Economía y Competitividad‐MINECO Project Nº: CGL2016‐80783‐R. O.G. was supported by the ERC Synergy project, SyG‐2013‐610028 IMBALANCE‐P and an INTERACT grant agreement No: 730938 EU‐H2020. J.E.S. is a CIFAR Fellow in the program Fungal Kingdom: Threats and Opportunities and supported by United States Department of Agriculture—National Institute of Food and Agriculture Hatch project CA‐R‐PPA‐5062‐H. N.P. was supported by a Royal Thai Government Fellowship. J.C.B. acknowledges the support of Javeriana University. We thank Maximillien Osbourne‐Thacker, Amulya Kunduru, and Chloe Hull for assistance with processing soil samples and molecular sequencing prep. We thank the following for assistance with site selection, plant identification, and soil sampling: Nevados National Park in Colombia and its staff, Katrin Sieron, Marco Morales, Leonor Jiménez, Daniel Hernández, Fabien Anthelme, Luis Merino‐Martin, and Miguel Castillo.

Keywords

  • alpine
  • global change
  • leaf traits
  • plant–soil interactions
  • soil microbes
  • woody encroachment

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