Origin of volatile organic compound emissions from subarctic tundra under global warming

© 2020 The Authors. Global Change Biology published by John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 26(2020), 3 vom: 18. März, Seite 1908-1925
1. Verfasser: Ghirardo, Andrea (VerfasserIn)
Weitere Verfasser: Lindstein, Frida, Koch, Kerstin, Buegger, Franz, Schloter, Michael, Albert, Andreas, Michelsen, Anders, Winkler, J Barbro, Schnitzler, Jörg-Peter, Rinnan, Riikka
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2020
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article Research Support, Non-U.S. Gov't 13CO2 Arctic climate change de novo biosynthesis global warming net ecosystem exchange subarctic heath terpene mehr... tundra volatile organic compound Volatile Organic Compounds
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520 |a Warming occurs in the Arctic twice as fast as the global average, which in turn leads to a large enhancement in terpenoid emissions from vegetation. Volatile terpenoids are the main class of biogenic volatile organic compounds (VOCs) that play crucial roles in atmospheric chemistry and climate. However, the biochemical mechanisms behind the temperature-dependent increase in VOC emissions from subarctic ecosystems are largely unexplored. Using 13 CO2 -labeling, we studied the origin of VOCs and the carbon (C) allocation under global warming in the soil-plant-atmosphere system of contrasting subarctic heath tundra vegetation communities characterized by dwarf shrubs of the genera Salix or Betula. The projected temperature rise of the subarctic summer by 5°C was realistically simulated in sophisticated climate chambers. VOC emissions strongly depended on the plant species composition of the heath tundra. Warming caused increased VOC emissions and significant changes in the pattern of volatiles toward more reactive hydrocarbons. The 13 C was incorporated to varying degrees in different monoterpene and sesquiterpene isomers. We found that de novo monoterpene biosynthesis contributed to 40%-44% (Salix) and 60%-68% (Betula) of total monoterpene emissions under the current climate, and that warming increased the contribution to 50%-58% (Salix) and 87%-95% (Betula). Analyses of above- and belowground 12/13 C showed shifts of C allocation in the plant-soil systems and negative effects of warming on C sequestration by lowering net ecosystem exchange of CO2 and increasing C loss as VOCs. This comprehensive analysis provides the scientific basis for mechanistically understanding the processes controlling terpenoid emissions, required for modeling VOC emissions from terrestrial ecosystems and predicting the future chemistry of the arctic atmosphere. By changing the chemical composition and loads of VOCs into the atmosphere, the current data indicate that global warming in the Arctic may have implications for regional and global climate and for the delicate tundra ecosystems 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a 13CO2 
650 4 |a Arctic 
650 4 |a climate change 
650 4 |a de novo biosynthesis 
650 4 |a global warming 
650 4 |a net ecosystem exchange 
650 4 |a subarctic heath 
650 4 |a terpene 
650 4 |a tundra 
650 4 |a volatile organic compound 
650 7 |a Volatile Organic Compounds  |2 NLM 
700 1 |a Lindstein, Frida  |e verfasserin  |4 aut 
700 1 |a Koch, Kerstin  |e verfasserin  |4 aut 
700 1 |a Buegger, Franz  |e verfasserin  |4 aut 
700 1 |a Schloter, Michael  |e verfasserin  |4 aut 
700 1 |a Albert, Andreas  |e verfasserin  |4 aut 
700 1 |a Michelsen, Anders  |e verfasserin  |4 aut 
700 1 |a Winkler, J Barbro  |e verfasserin  |4 aut 
700 1 |a Schnitzler, Jörg-Peter  |e verfasserin  |4 aut 
700 1 |a Rinnan, Riikka  |e verfasserin  |4 aut 
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773 1 8 |g volume:26  |g year:2020  |g number:3  |g day:18  |g month:03  |g pages:1908-1925 
856 4 0 |u http://dx.doi.org/10.1111/gcb.14935  |3 Volltext 
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