1. Nonlinear Growth and Physiological Responses of White Spruce at North American Arctic Treeline.
- Author
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Lévesque, Mathieu, Andreu‐Hayles, Laia, D'Arrigo, Rosanne, Oelkers, Rose, and Buckley, Brendan M.
- Subjects
WHITE spruce ,TIMBERLINE ,ATMOSPHERIC carbon dioxide ,SEA ice ,WATER efficiency ,SPRUCE - Abstract
Much is still unknown about the growth and physiological responses of trees to global change at the northern treeline. We combined tree‐ring width data with century‐long stable carbon and oxygen isotope records to investigate growth and physiological responses of white spruce at two treeline sites in the Canadian Arctic to concurrent increases in temperature, atmospheric CO2 concentration (ca), and decline in sea ice extent over the past century. The tree‐ring records were assessed during three periods with contrasting climatic conditions: (a) the early 20th century warming, (b) the 1940–1970 cooling period, and (c) the anthropogenic late 20th century warming period. We found opposing growth trends between the two sites, but similar carbon isotope discrimination (Δ13C) and intrinsic water‐use efficiency (iWUE) trajectories. While tree growth (defined as basal area increment) increased at the site nearer to the Arctic Ocean during the 20th century following the rise in temperature and sea ice loss, growth declined after 1950 at the more interior site. At both sites, Δ13C slightly increased over these periods. However, trees showed a nonlinear response to increased ca, shifting after 1970 from a passive stomatal response (i.e., no changes in iWUE) to an active response (i.e., a moderate ∼12% increase in iWUE). Further, our isotope‐based findings do not support the idea that temperature‐induced drought stress caused the divergent growth trends at our treeline sites. This study thus highlights nonlinear and complex physiological and growth adjustments to concomitant changes in temperature, sea ice extent, and ca over the last century at the northern treeline. Plain Language Summary: In the last decades, Arctic ecosystems have experienced unprecedented warmer temperatures, higher atmospheric carbon dioxide concentrations, and a decline in sea ice extent. However, it is still unknown how these changes in environmental factors have impacted tree populations at their northern distribution limits. Here, we examine how the growth and water‐use efficiency of white spruce trees have changed over the last century in response to warmer temperatures, higher carbon dioxide concentrations, and sea ice decline at two treeline sites in the Canadian Arctic. We found that tree growth increased at the site nearer to the Arctic Ocean during the 20th century following the rise in temperature and sea ice loss, while growth declined after 1950 at the more interior site. At both sites, the water‐use efficiency of trees was stable until 1970. Following the rapid temperature and carbon dioxide increase since the 1970s, trees have become more efficient in using water. The contrasting growth trends found at our study sites highlight complex growth and physiological adjustments of white spruce trees to rapid and simultaneous changes in temperature, sea ice extent, and carbon dioxide concentrations in the Arctic. Key Points: Complex growth and physiological responses of white spruce trees to changes in temperature and sea ice extent inferred from stable isotopesWhite spruce radial growth at Arctic latitudinal treeline decreased at an interior site and increased at a site closer to the Arctic OceanWhite spruce shifted from a passive to an active water‐use efficiency response to rising CO2 concentration over the 20th century [ABSTRACT FROM AUTHOR]
- Published
- 2023
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