Above- and belowground linkages shape responses of mountain vegetation to climate change
Abstract
Upward shifts of mountain vegetation lag behind rates of climate warming, partly related to interconnected changes belowground. Here, we unravel above- and belowground linkages by drawing insights from short-term experimental manipulations and elevation gradient studies. Soils will likely gain carbon in early successional ecosystems, while losing carbon as forest expands upward, and the slow, high-elevation soil development will constrain warming-induced vegetation shifts. Current approaches fail to predict the pace of these changes and how much they will be modified by interactions among plants and soil biota. Integrating mountain soils and their biota into monitoring programs, combined with innovative comparative and experimental approaches, will be crucial to overcome the paucity of belowground data and to better understand mountain ecosystem dynamics and their feedbacks to climate.
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Science
Volume 365 | Issue 6458
13 September 2019
13 September 2019
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Copyright © 2019, American Association for the Advancement of Science.
This is an article distributed under the terms of the Science Journals Default License.
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Published in print: 13 September 2019
Acknowledgments
We thank T. Walker for critical comments on the manuscript and the Stillberg team and P. Moiseev for their long-term support in treeline research. Funding: F.H. received funding from the Swiss National Science Foundation (grant no. 171171); K.G. was supported by funding from the Swiss National Science Foundation (grant no. PZ00P2_174047); and J.M.A. received funding from the European Union’s Horizon 2020 research and innovation program (grant no. 678841) and from the Swiss National Science Foundation (grant no. 31003A_176044). Competing interests: The authors declare no competing interests.
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Funding Information
H2020 European Research Council: 678841
Swiss National Science Foundation: PZ00P2_174047
Swiss National Science Foundation: 31003A_176044
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