title: Ectomycorrhizal communities of ponderosa pine and lodgepole pine in the south-central Oregon pumice zone.
abstract: Forest ecosystems of the Pacific Northwest of the USA are changing as a result of climate change. Specifically, rise of global temperatures, decline of winter precipitation, earlier loss of snowpack, and increased summer drought are altering the range of Pinus contorta. Simultaneously, flux in environmental conditions within the historic P. contorta range may facilitate the encroachment of P. ponderosa into P. contorta territory. Furthermore, successful pine species migration may be constrained by the distribution or co-migration of ectomycorrhizal fungi (EMF). Knowledge of the linkages among soil fungal diversity, community structure, and environmental factors is critical to understanding the organization and stability of pine ecosystems. The objectives of this study were to establish a foundational knowledge of the EMF communities of P. ponderosa and P. contorta in the Deschutes National Forest, OR, USA, and to examine soil characteristics associated with community composition. We examined EMF root tips of P. ponderosa and P. contorta in soil cores and conducted soil chemistry analysis for P. ponderosa cores. Results indicate that Cenococcum geophilum, Rhizopogon salebrosus, and Inocybe flocculosa were dominant in both P. contorta and P. ponderosa soil cores. Rhizopogon spp. were ubiquitous in P. ponderosa cores. There was no significant difference in the species composition of EMF communities of P. ponderosa and P. contorta. Ordination analysis of P. ponderosa soils suggested that soil pH, plant-available phosphorus (Bray), total phosphorus (P), carbon (C), mineralizable nitrogen (N), ammonium (NH4), and nitrate (NO3) are driving EMF community composition in P. ponderosa stands. We found a significant linear relationship between EMF species richness and mineralizable N. In conclusion, P. ponderosa and P. contorta, within the Deschutes National Forest, share the same dominant EMF species, which implies that P. ponderosa may be able to successfully establish within the historic P. contorta range and dominant EMF assemblages may be conserved.
authors.affiliation: Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR, 97331, USA.|Department of Biology, Boston University, 5 Cummington Mall, Boston, MA, 02215, USA.
authors.forename: Maria O
authors.initials: MO
authors.lastname: Garcia
authors.affiliation: US Department of Agriculture, Forest Service, Pacific Northwest Research Station, Forestry Sciences Laboratory, 3200 Jefferson Way, Corvallis, OR, 97331, USA. jsmith01@fs.fed.us.
authors.forename: Jane E
authors.initials: JE
authors.lastname: Smith
authors.affiliation: Department of Forest Ecosystems and Society, Oregon State University, Corvallis, OR, 97331, USA.
authors.forename: Daniel L
authors.initials: DL
authors.lastname: Luoma
authors.affiliation: Biology Department, Institute for Biodiversity, Resilience and Ecosystem Services, University of British Columbia, Okanagan campus, Kelowna, British Columbia, V1V 1V7, Canada.
authors.forename: Melanie D
authors.initials: MD
authors.lastname: Jones
mesh_terms: D057231:Climate Change; D017753:Ecosystem; D005658:Fungi / Q000145:classification / Q000235:genetics / Q000302:isolation & purification*; D038821:Mycorrhizae / Q000145:classification / Q000235:genetics / Q000302:isolation & purification*; D009922:Oregon; D028223:Pinus / Q000382:microbiology*; D041604:Pinus ponderosa / Q000382:microbiology*; D012621:Seasons
keywords: Climate change; Ectomycorrhizal communities; Pine species migration; Pinus contorta; Pinus ponderosa