2012
DOI: 10.1007/s11258-012-0034-4
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Moss-specific changes in nitrogen fixation following two decades of warming, shading, and fertilizer addition

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Cited by 59 publications
(58 citation statements)
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“…2). As in other subarctic heaths, grasses, and forbs had low cover and did not respond significantly, even after two decades of warming (Sorensen et al 2012). These responses are consistent with a global assessment of experimental climate warming on tundra vegetation, which has shown that shrubs increase with warming only where ambient temperature is highest, i.e., in the Subarctic and Low Arctic, whereas graminoids increase primarily in high arctic sites (Elmendorf et al 2012).…”
Section: Plant Functional Types Nutrient Availability and Responsivsupporting
confidence: 83%
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“…2). As in other subarctic heaths, grasses, and forbs had low cover and did not respond significantly, even after two decades of warming (Sorensen et al 2012). These responses are consistent with a global assessment of experimental climate warming on tundra vegetation, which has shown that shrubs increase with warming only where ambient temperature is highest, i.e., in the Subarctic and Low Arctic, whereas graminoids increase primarily in high arctic sites (Elmendorf et al 2012).…”
Section: Plant Functional Types Nutrient Availability and Responsivsupporting
confidence: 83%
“…3), probably due to the relatively high P content in birch litter (Sorensen and Michelsen 2011), the very high nutrient input with NPK fertilizer strongly reduced N 2 fixation at the mesic heath (Fig. 3) (Sorensen et al 2012). If N input increases due to deposition, N 2 fixation is likely to decrease.…”
Section: Nitrogen Cycling In Strongly N-limited Ecosystemsmentioning
confidence: 96%
“…This warming is likely to have a positive effect on forest floor cyanobacteria growth and N fixation as long as temperatures remain within or below the enzymatic optimum temperature for N fixation (between 20 • C and 30 • C) [14]. With that said, increases in temperature might have a negative effect on moss host plants that could reduce forest-wide densities of N fixing cyanobacteria [11,30,31], thus extrapolating the stimulatory effects of increased temperature and CO 2 on forest floor, moss-associated cyanobacterial N fixation to the forest level is difficult [32]. Another reason for this is because the fate of the N fixed by terrestrial cyanobacteria is still unclear.…”
Section: Discussionmentioning
confidence: 99%
“…(2,30) 9.77 <0.001 CO 2 × temperature (2,30) 4.71 0.017 time (6,180) 53.83 <0.001 time × CO 2 (6,180) 1.41 0.204 time × temperature (12,180) 30.95 <0.001 time × CO 2 × temperature (12,180) 2.34 0.008…”
Section: Experiments 2: N Fixation Under Elevated Warming and Atmosphementioning
confidence: 99%
“…In temperate and subtropical regions, nutrient enrichment tends to increase algal growth and alter species composition (Goldsborough and Robinson 1996), with consequences for ecosystem function (Richardson 2010). Similar information is not available for algae in northern peatlands, where nutrient levels are typically low (Sorensen et al 2012) and elevated nutrient levels are likely to coincide with warmer temperatures. Since many of the enzymatic reactions involved in photosynthesis are temperature-dependent (Davison 1991), warmer temperatures may enhance the influence of elevated nutrient levels on algal production in northern ecosystems where low mean annual temperatures tend to constrain metabolic activity (Rosa et al 2013).…”
Section: Introductionmentioning
confidence: 99%