Range shifts in a foundation sedge potentially induce large Arctic ecosystem carbon losses and gains

Abstract Foundation species have disproportionately large impacts on ecosystem structure and function. As a result, future changes to their distribution may be important determinants of ecosystem carbon (C) cycling in a warmer world. We assessed the role of a foundation tussock sedge ( Eriophorum va...

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Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Curasi, Salvatore R, Fetcher, Ned, Hewitt, Rebecca E, Lafleur, Peter M, Loranty, Michael M, Mack, Michelle C, May, Jeremy L, Myers-Smith, Isla H, Natali, Susan M, Oberbauer, Steven F, Parker, Thomas C, Sonnentag, Oliver, Vargas Zesati, Sergio A, Wullschleger, Stan D, Rocha, Adrian V
Other Authors: Natural Environment Research Council, National Geographic, National Science Foundation
Format: Article in Journal/Newspaper
Language:unknown
Published: IOP Publishing 2022
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Online Access:http://dx.doi.org/10.1088/1748-9326/ac6005
https://iopscience.iop.org/article/10.1088/1748-9326/ac6005
https://iopscience.iop.org/article/10.1088/1748-9326/ac6005/pdf
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Summary:Abstract Foundation species have disproportionately large impacts on ecosystem structure and function. As a result, future changes to their distribution may be important determinants of ecosystem carbon (C) cycling in a warmer world. We assessed the role of a foundation tussock sedge ( Eriophorum vaginatum ) as a climatically vulnerable C stock using field data, a machine learning ecological niche model, and an ensemble of terrestrial biosphere models (TBMs). Field data indicated that tussock density has decreased by ∼0.97 tussocks per m 2 over the past ∼38 years on Alaska’s North Slope from ∼1981 to 2019. This declining trend is concerning because tussocks are a large Arctic C stock, which enhances soil organic layer C stocks by 6.9% on average and represents 745 Tg C across our study area. By 2100, we project that changes in tussock density may decrease the tussock C stock by 41% in regions where tussocks are currently abundant (e.g. −0.8 tussocks per m 2 and −85 Tg C on the North Slope) and may increase the tussock C stock by 46% in regions where tussocks are currently scarce (e.g. +0.9 tussocks per m 2 and +81 Tg C on Victoria Island). These climate-induced changes to the tussock C stock were comparable to, but sometimes opposite in sign, to vegetation C stock changes predicted by an ensemble of TBMs. Our results illustrate the important role of tussocks as a foundation species in determining future Arctic C stocks and highlight the need for better representation of this species in TBMs.