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Mycorrhizal associations of temperate forest seedlings mediate rhizodeposition, but not soil carbon storage, under elevated nitrogen availability

Journal Article · · Global Change Biology
DOI:https://doi.org/10.1111/gcb.17446· OSTI ID:2426976
 [1];  [2];  [3];  [4];  [2];  [2];  [2];  [2]
  1. Department of Biological Sciences Dartmouth College Hanover New Hampshire USA, Forest Ecosystems and Society, College of Forestry Oregon State University Corvallis Oregon USA
  2. Department of Biological Sciences Dartmouth College Hanover New Hampshire USA
  3. Department of Plant Pathology University of Wisconsin‐Madison Madison Wisconsin USA
  4. Odum School of Ecology University of Georgia Athens Georgia USA
Abstract

Tree‐mycorrhizal associations are associated with patterns in nitrogen (N) availability and soil organic matter storage; however, we still lack a mechanistic understanding of what tree and fungal traits drive these patterns and how they will respond to global changes in soil N availability. To address this knowledge gap, we investigated how arbuscular mycorrhizal (AM)‐ and ectomycorrhizal (EcM)‐associated seedlings alter rhizodeposition in response to increased seedling inorganic N acquisition. We grew four species each of EcM and AM seedlings from forests of the eastern United States in a continuously 13 C‐labeled atmosphere within an environmentally controlled chamber and subjected to three levels of 15 N‐labeled fertilizer. We traced seedling 15 N uptake from, and 13 C‐labeled inputs (net rhizodeposition) into, root‐excluded or ‐included soil over a 5‐month growing season. N uptake by seedlings was positively related to rhizodeposition for EcM‐ but not AM‐associated seedlings in root‐included soils. Despite this contrast in rhizodeposition, there was no difference in soil C storage between mycorrhizal types over the course of the experiment. Instead root‐inclusive soils lost C, while root‐exclusive soils gained C. Our findings suggest that mycorrhizal associations mediate tree belowground C investment in response to inorganic N availability, but these differences do not affect C storage. Continued soil warming and N deposition under global change will increase soil inorganic N availability and our seedling results indicate this could lead to greater belowground C investment by EcM‐associated trees. This potential for less efficient N uptake by EcM‐trees could contribute to AM‐tree success and a shift toward more AM‐dominated temperate forests.

Sponsoring Organization:
USDOE
Grant/Contract Number:
SC0020228
OSTI ID:
2426976
Alternate ID(s):
OSTI ID: 2579895
Journal Information:
Global Change Biology, Journal Name: Global Change Biology Journal Issue: 8 Vol. 30; ISSN 1354-1013
Publisher:
Wiley-BlackwellCopyright Statement
Country of Publication:
United Kingdom
Language:
English

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