Abstract

ABSTRACTOngoing responses to climate change in arctic-alpine ecosystems, including the increasing dominance of deciduous shrubs, involve major shifts in plant functional group composition. Because rates of photosynthesis and respiration and their responses to temperature may vary among plant functional groups, a better understanding of their contributions to carbon fluxes will help improve predictions of how ecosystem changes will affect carbon source-sink relations in globally important tundra regions. We used a sequential harvest method to estimate growing season functional group contributions to net ecosystem exchange (NEE), ecosystem respiration (ER), and gross photosynthesis (GP) in alpine heath-, meadow-, and Salix-dominated shrub communities. We also partitioned ER into aboveground and belowground components in all three communities. Belowground efflux was the dominant component of ER in the heath and meadow communities (63 percent and 88 percent of ER, respectively) but contributed only approximately 40 percent of ER in the shrub community. The dominant functional group in each community contributed most to aboveground exchanges. Estimates for cryptogams were uncertain, but indicated a minor role for bryophytes and lichens in overall exchange. The results of our novel method of partitioning gas-exchange measurements suggest strong differences in the relative proportions of soil versus aboveground respiration and in the contributions of different functional groups in the net carbon exchange of three important arctic-alpine community types, with implications for changes in carbon dynamics as these systems respond to environmental change.

Highlights

  • Climate change is expected to result in changes in functional group composition in terrestrial ecosystems (Condit, Hubbell, and Foster 1996; Diaz and Cabido 1997)

  • We focused on the following questions: (1) What are the relative contributions of belowground and aboveground biotic processes to ecosystem respiration in arctic-alpine plant communities? and (2) What are the relative contributions of the major functional groups, including cryptogams, to ER, net ecosystem exchange (NEE), and gross photosynthesis (GP) in these communities? In addition, we discuss how changes in functional group composition may affect C source-sink activity as arctic-alpine ecosystems respond to environmental change with an increased abundance of deciduous shrubs

  • The adjusted data suggest that gross photosynthesis and net exchange in the meadow may be intermediate—lower than in the shrub community and higher than in the heath community

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Summary

Introduction

Climate change is expected to result in changes in functional group composition in terrestrial ecosystems (Condit, Hubbell, and Foster 1996; Diaz and Cabido 1997). In arctic regions, where warming has been greatest, shrub cover is expanding at the expense of other functional groups (Myers-Smith et al 2011) These changes may be accompanied by changes in ecosystem processes, including nutrient cycling and carbon (C) fluxes and storage (Sørensen et al 2018b), as well as effects on energy balance via boundary layer, sensible heat exchange, albedo, and snow cover, which may feed back on global temperature and precipitation patterns (Dormann and Woodin 2002; Cornelissen et al 2007; De Deyn, Cornelissen, and Bardgett 2008; Chapin et al 2009; Wookey et al 2009). Shifts in the balance between C uptake and respiration in these systems could result in a strong positive feedback on global warming, and there is evidence that this is already

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