Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/31227
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Plant carbon allocation drives turnover of old soil organic matter in permafrost tundra soils
Author(s): Street, Lorna E
Garnett, Mark H
Subke, Jens-Arne
Wookey, Philip A
Baxter, Robert
Dean, Joshua F
Contact Email: p.a.wookey@stir.ac.uk
Keywords: radiocarbon
arctic
priming
root
rhizosphere
shrub
vegetation change
mycorrhiza
isotopes
belowground
Issue Date: Aug-2020
Citation: Street LE, Garnett MH, Subke J, Wookey PA, Baxter R & Dean JF (2020) Plant carbon allocation drives turnover of old soil organic matter in permafrost tundra soils. Global Change Biology, 26 (8), pp. 4559-4571. https://doi.org/10.1111/gcb.15134
Abstract: Carbon cycle feedbacks from permafrost ecosystems are expected to accelerate global climate change. Shifts in vegetation productivity and composition in permafrost regions could influence soil organic carbon (SOC) turnover rates via rhizosphere (root zone) priming effects (RPEs), but these processes are not currently accounted for in model predictions. We use a radiocarbon (bomb-14C) approach to test for RPEs in two Arctic tall shrubs,alder (Alnus viridis (Chaix) DC) and birch (Betula glandulosa Michx.)), and in ericaceous heath tundra vegetation. We compare surface CO2 efflux rates and 14C content between intact vegetation and plots in which belowground allocation of recent photosynthate was prevented by trenching and removal of aboveground biomass. We show, for the first time, that recent photosynthate drives mineralization of older (> 50 years old) SOC under birch shrubs and ericaceous heath tundra. By contrast, we find no evidence of RPEs in soils under alder. This is the first direct evidence from permafrost systems that vegetation influences SOC turnover through belowground C allocation. The vulnerability of SOC to decomposition in permafrost systems may therefore be directly linked to vegetation change, such that expansion of birch shrubs across the Arctic could increase decomposition of older SOC. Our results suggest that carbon cycle models that don’t include RPEs risk underestimating the carbon cycle feedbacks associated with changing conditions in tundra regions.
DOI Link: 10.1111/gcb.15134
Rights: © 2020 The Authors. Global Change Biology published by John Wiley & Sons Ltd This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
Licence URL(s): http://creativecommons.org/licenses/by/4.0/

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