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Title: High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland

Abstract

Societal Impact Statement Mycorrhizal fungi enable plants to thrive in the cold, waterlogged, organic soils of boreal peatlands and, with saprotrophic fungi, largely contribute to the sequestration of atmospheric carbon in peat. Hence, fungi support the contribution of peatlands to global climate regulation, on which society depends. Here we used high‐resolution minirhizotrons for an unprecedented glimpse of the belowground world of a forested bog and highlighted linkages between environmental change and the abundance, dynamics, and morphology of vascular plant fine roots and fungal mycelium. These changes may have implications for peat carbon accumulation on the boreal landscape. Summary Minirhizotron technology has rarely been deployed in peatlands which has limited our understanding of root‐fungal dynamics in one of planet's most carbon‐dense ecosystems. We used novel, high‐resolution minirhizotrons in a forested bog to explore temporal variation in the abundance and growth of plant fine roots and fungal mycelium with changes in peat temperature and moisture. We utilized the framework of the Spruce and Peatland Responses Under Changing Environments experiment and focused on two minirhizotron tubes installed at the coldest (+0, elevated CO 2 ) and warmest (+9°C, elevated CO 2 ) ends of the experimental temperature gradient, respectively. We found that inmore » warmer and drier peat, ericaceous shrub roots and ectomycorrhizal fungal rhizomorphs were more abundant, and the growth of rhizomorphs and sporocarps was greater. In turn, fine roots of trees, ectomycorrhizas, and dark‐colored fungal hyphae were more abundant in colder, wetter peat. Ultimately, the belowground active season for both plant roots and fungi was extended by 62 days at the warmest compared to the coldest end of the gradient, with implications for belowground carbon, water, and nutrient fluxes. High‐resolution minirhizotrons in peatlands provided an unprecedented view of ericaceous shrub and tree fine roots and their mycorrhizal fungal partners in situ. Therefore, this technology advanced our understanding of linkages between environmental change and the abundance, morphology, and dynamics of vascular plant fine roots and fungal mycelium.« less

Authors:
ORCiD logo [1];  [1]; ORCiD logo [2]; ORCiD logo [3];  [1]; ORCiD logo [3]; ORCiD logo [1]; ORCiD logo [1]
  1. Climate Change Science Institute and Environmental Sciences Division Oak Ridge National Laboratory Oak Ridge TN USA
  2. Department of Plant and Microbial Biology University of Minnesota St. Paul MN USA
  3. Department of Microbiology and Plant Pathology Center for Conservation Biology University of California‐Riverside Riverside CA USA
Publication Date:
Research Org.:
Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
OSTI Identifier:
1730983
Alternate Identifier(s):
OSTI ID: 1735437; OSTI ID: 1786620
Grant/Contract Number:  
AC05-00OR22725
Resource Type:
Published Article
Journal Name:
Plants, People, Planet
Additional Journal Information:
Journal Name: Plants, People, Planet; Journal ID: ISSN 2572-2611
Publisher:
New Phytologist Trust - Wiley
Country of Publication:
United States
Language:
English
Subject:
59 BASIC BIOLOGICAL SCIENCES; dynamics; fine roots; minirhizotron; mycorrhizal fungi; peatland; phenology; warming

Citation Formats

Defrenne, Camille E., Childs, Joanne, Fernandez, Christopher W., Taggart, Michael, Nettles, W. Robert, Allen, Michael F., Hanson, Paul J., and Iversen, Colleen M. High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland. United States: N. p., 2020. Web. doi:10.1002/ppp3.10172.
Defrenne, Camille E., Childs, Joanne, Fernandez, Christopher W., Taggart, Michael, Nettles, W. Robert, Allen, Michael F., Hanson, Paul J., & Iversen, Colleen M. High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland. United States. https://doi.org/10.1002/ppp3.10172
Defrenne, Camille E., Childs, Joanne, Fernandez, Christopher W., Taggart, Michael, Nettles, W. Robert, Allen, Michael F., Hanson, Paul J., and Iversen, Colleen M. Thu . "High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland". United States. https://doi.org/10.1002/ppp3.10172.
@article{osti_1730983,
title = {High‐resolution minirhizotrons advance our understanding of root‐fungal dynamics in an experimentally warmed peatland},
author = {Defrenne, Camille E. and Childs, Joanne and Fernandez, Christopher W. and Taggart, Michael and Nettles, W. Robert and Allen, Michael F. and Hanson, Paul J. and Iversen, Colleen M.},
abstractNote = {Societal Impact Statement Mycorrhizal fungi enable plants to thrive in the cold, waterlogged, organic soils of boreal peatlands and, with saprotrophic fungi, largely contribute to the sequestration of atmospheric carbon in peat. Hence, fungi support the contribution of peatlands to global climate regulation, on which society depends. Here we used high‐resolution minirhizotrons for an unprecedented glimpse of the belowground world of a forested bog and highlighted linkages between environmental change and the abundance, dynamics, and morphology of vascular plant fine roots and fungal mycelium. These changes may have implications for peat carbon accumulation on the boreal landscape. Summary Minirhizotron technology has rarely been deployed in peatlands which has limited our understanding of root‐fungal dynamics in one of planet's most carbon‐dense ecosystems. We used novel, high‐resolution minirhizotrons in a forested bog to explore temporal variation in the abundance and growth of plant fine roots and fungal mycelium with changes in peat temperature and moisture. We utilized the framework of the Spruce and Peatland Responses Under Changing Environments experiment and focused on two minirhizotron tubes installed at the coldest (+0, elevated CO 2 ) and warmest (+9°C, elevated CO 2 ) ends of the experimental temperature gradient, respectively. We found that in warmer and drier peat, ericaceous shrub roots and ectomycorrhizal fungal rhizomorphs were more abundant, and the growth of rhizomorphs and sporocarps was greater. In turn, fine roots of trees, ectomycorrhizas, and dark‐colored fungal hyphae were more abundant in colder, wetter peat. Ultimately, the belowground active season for both plant roots and fungi was extended by 62 days at the warmest compared to the coldest end of the gradient, with implications for belowground carbon, water, and nutrient fluxes. High‐resolution minirhizotrons in peatlands provided an unprecedented view of ericaceous shrub and tree fine roots and their mycorrhizal fungal partners in situ. Therefore, this technology advanced our understanding of linkages between environmental change and the abundance, morphology, and dynamics of vascular plant fine roots and fungal mycelium.},
doi = {10.1002/ppp3.10172},
journal = {Plants, People, Planet},
number = ,
volume = ,
place = {United States},
year = {Thu Dec 03 00:00:00 EST 2020},
month = {Thu Dec 03 00:00:00 EST 2020}
}

Journal Article:
Free Publicly Available Full Text
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https://doi.org/10.1002/ppp3.10172

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