Diverse Mycorrhizal Associations Enhance Terrestrial C Storage in a Global Model

Sulman, Benjamin N.; Shevliakova, Elena; Brzostek, Edward R.; Kivlin, Stephanie N.; Malyshev, Sergey; Menge, Duncan N. L.; Zhang, Xin

doi:10.1029/2018GB005973

Diverse Mycorrhizal Associations Enhance Terrestrial C Storage in a Global Model

Journal Article · Sat Mar 23 00:00:00 EDT 2019 · Global Biogeochemical Cycles

DOI:https://doi.org/10.1029/2018GB005973· OSTI ID:1511936

^[1]; Shevliakova, Elena ^[2]; ^[3]; Kivlin, Stephanie N. ^[4]; ^[5]; ^[6]; ^[7]

Princeton Univ., NJ (United States); Univ. of California, Merced, CA (United States); Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
NOAA Geophysical Fluid Dynamics Lab., Princeton, NJ (United States)
West Virginia Univ., Morgantown, WV (United States)
Univ. of Tennessee, Knoxville, TN (United States)
NOAA Geophysical Fluid Dynamics Lab., Princeton, NJ (United States); Princeton Univ., NJ (United States)
Columbia Univ., New York, NY (United States)
Princeton Univ., NJ (United States); Univ. of Maryland, Frostburg, MD (United States)

Accurate projections of the terrestrial carbon (C) sink are critical to understanding the future global C cycle and setting CO₂ emission reduction goals. Current earth system models (ESMs) and dynamic global vegetation models (DGVMs) with coupled carbon-nitrogen cycles project that future terrestrial C sequestration will be limited by nitrogen (N) availability, but the magnitude of N limitation remains a critical uncertainty. Plants use multiple symbiotic nutrient acquisition strategies to mitigate N limitation, but current DGVMs omit these mechanisms. Fully coupling N-acquiring plant-microbe symbioses to soil organic matter (SOM) cycling within a DGVM for the first time, we demonstrate that increases in N acquisition via SOM decomposition and atmospheric N₂ fixation could support long-term enhancement of terrestrial C sequestration at global scales under elevated CO₂. The model reproduced elevated CO2 responses from two experiments (Duke and Oak Ridge) representing contrasting N acquisition strategies. N release from enhanced SOM decomposition supported vegetation growth at Duke, while inorganic N depletion limited growth at Oak Ridge. Global simulations reproduced spatial patterns of N-acquiring symbioses from a novel niche-based map of mycorrhizal fungi. Under a 100-ppm increase in CO2 concentrations, shifts in N acquisition pathways facilitated 200 Pg C of terrestrial C sequestration over 100 years compared to 50 Pg C for a scenario with static N acquisition pathways. Our results imply that N acquisition strategies are important determinants of terrestrial C sequestration potential under elevated CO₂ and that nitrogen-enabled DGVMs that omit symbiotic N acquisition may underestimate future terrestrial C uptake.

View Accepted Manuscript (DOE)

Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: USDOE; USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)

Grant/Contract Number:: AC05-00OR22725; SC0016188

OSTI ID:: 1511936

Alternate ID(s):: OSTI ID: 1507473

Journal Information:: Global Biogeochemical Cycles, Journal Name: Global Biogeochemical Cycles Journal Issue: 4 Vol. 33; ISSN 0886-6236

Publisher:: American Geophysical Union (AGU)Copyright Statement

Country of Publication:: United States

Language:: English

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