Root‐associated fungi and acquisitive root traits facilitate permafrost nitrogen uptake from long‐term experimentally warmed tundra

Author:

Hewitt Rebecca E.12ORCID,DeVan M. Rae3ORCID,Taylor D. Lee3ORCID,Mack Michelle C.1ORCID

Affiliation:

1. Center for Ecosystem Science and Society Northern Arizona University PO Box 5620 Flagstaff AZ 86011 USA

2. Department of Environmental Studies Amherst College Amherst MA 01002 USA

3. Department of Biology University of New Mexico MSC03 2020 Albuquerque NM 87131 USA

Abstract

Summary Root‐associated fungi (RAF) and root traits regulate plant acquisition of nitrogen (N), which is limiting to growth in Arctic ecosystems. With anthropogenic warming, a new N source from thawing permafrost has the potential to change vegetation composition and increase productivity, influencing climate feedbacks. Yet, the impact of warming on tundra plant root traits, RAF, and access to permafrost N is uncertain. We investigated the relationships between RAF, species‐specific root traits, and uptake of N from the permafrost boundary by tundra plants experimentally warmed for nearly three decades at Toolik Lake, Alaska. Warming increased acquisitive root traits of nonmycorrhizal and mycorrhizal plants. RAF community composition of ericoid (ERM) but not ectomycorrhizal (ECM) shrubs was impacted by warming and correlated with root traits. RAF taxa in the dark septate endophyte, ERM, and ECM guilds strongly correlated with permafrost N uptake for ECM and ERM shrubs. Overall, a greater proportion of variation in permafrost N uptake was related to root traits than RAF. Our findings suggest that warming Arctic ecosystems will result in interactions between roots, RAF, and newly thawed permafrost that may strongly impact feedbacks to the climate system through mechanisms of carbon and N cycling.

Funder

Directorate for Biological Sciences

Publisher

Wiley

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