Figures
Abstract
Most manipulation experiments simulating global change in tundra were short-term or did not measure plant growth directly. Here, we assessed the growth of three shrubs (Cassiope tetragona, Empetrum hermaphroditum and Betula nana) at a subarctic heath in Abisko (Northern Sweden) after 22 years of warming (passive greenhouses), fertilisation (nutrients addition) and shading (hessian fabric), and compare this to observations from the first decade of treatment. We assessed the growth rate of current-year leaves and apical stem (primary growth) and cambial growth (secondary growth), and integrated growth rates with morphological measurements and species coverage. Primary- and total growth of Cassiope and Empetrum were unaffected by manipulations, whereas growth was substantially reduced under fertilisation and shading (but not warming) for Betula. Overall, shrub height and length tended to increase under fertilisation and warming, whereas branching increased mostly in shaded Cassiope. Morphological changes were coupled to increased secondary growth under fertilisation. The species coverage showed a remarkable increase in graminoids in fertilised plots. Shrub response to fertilisation was positive in the short-term but changed over time, likely because of an increased competition with graminoids. More erected postures and large, canopies (requiring enhanced secondary growth for stem reinforcement) likely compensated for the increased light competition in Empetrum and Cassiope but did not avoid growth reduction in the shade intolerant Betula. The impact of warming and shading on shrub growth was more conservative. The lack of growth enhancement under warming suggests the absence of long-term acclimation for processes limiting biomass production. The lack of negative effects of shading on Cassiope was linked to morphological changes increasing the photosynthetic surface. Overall, tundra shrubs showed developmental plasticity over the longer term. However, such plasticity was associated clearly with growth rate trends only in fertilised plots.
Citation: Campioli M, Leblans N, Michelsen A (2012) Twenty-Two Years of Warming, Fertilisation and Shading of Subarctic Heath Shrubs Promote Secondary Growth and Plasticity but Not Primary Growth. PLoS ONE 7(4): e34842. https://doi.org/10.1371/journal.pone.0034842
Editor: Bente Jessen Graae, Norwegian University of Science and Technology, Norway
Received: September 19, 2011; Accepted: March 8, 2012; Published: April 12, 2012
Copyright: © 2012 Campioli et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This work was supported by Methusalem funding (Research Center of Excellence ‘Eco’, University of Antwerp) and by the Danish Council for Independent Research | Natural Sciences. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Introduction
The Arctic is the region which will likely experience the most pronounced alteration in climate and environment due to global change [1]. As arctic ecosystems are very sensitive to changes in environmental conditions and store a significant amount (12%) of the global soil carbon (C), extensive research efforts have been made in the last three decades to understand the future feedback of arctic ecosystems to the greenhouse effect and global climate [1]–[3]. In particular, manipulation experiments have been set up to mimic the expected changes in arctic climate and their impact on ecosystems [4]–[6]. Many experiments have focused on the effect of warming during the growing season, of crucial importance for the arctic plant communities adapted to a short and cool summer [7]. Focus has been on plant growth, which (i) can be considered as a surrogate for plant fitness and as such a crucial process for plant subsistence and development, (ii) represents the amount of C taken up annually by the vegetation, and (iii) determines, through the process of C allocation to plant organs with different life-spans and decomposition rates, the C release by the ecosystem in the long-term [8].
The impact of warming on plant growth can be direct or indirect. The direct effect of warming has been mimicked by enhancing air and soil temperature, e.g. with open top chambers [9], [10]. Indirect effects of warming are manifold [11], [12]. However, the increase in nutrient availability through enhanced net mineralization is thought to be one of the most important indirect effects of warming for arctic plant communities, which are commonly nutrient limited [13], [14]. This indirect effect of warming has been mimicked by adding fertilisers during the growing season [15], under ambient or enhanced temperature. A second indirect effect (particularly important in the Subarctic and Low Arctic), is the potential increase in competition due to tree-line advancement and shrub expansion [16]–[18]. Such impact has been mimicked by shading [9], [10]. In the Subarctic and Low Arctic, manipulative experiments have shown that fertilisation has a strong effect on the growth of deciduous species in tussock tundra, and of all vascular species (and particularly graminoids) in heath tundra, whereas warming and shading have small or non significant effects [5], [11]. However, these findings rely mainly on studies not longer than a decade.
In this study, we aimed to broaden the current knowledge on the long-term impact of warming, fertilisation and shading in subarctic ecosystems by assessing the long-term responses in growth of the widespread dwarf-shrubs Cassiope tetragona (L.) D. Don., Empetrum hermaphroditum Hagerup and the low shrub Betula nana L., at a tree-line heath in Northern Sweden after 22 years of manipulation. The experiment is unique as we are not aware of similar well-replicated experiments of such duration in the Subarctic and Low Arctic. Furthermore, the experimental site is particularly suited for this analysis as it was intensively investigated in the first decade of manipulation, providing reports on the shorter term responses of shrub growth to manipulations. In the first decade of manipulation, warming yielded a modest positive response in the growth of Cassiope and no response in Empetrum and Betula, fertilisation led to a positive response in Cassiope and particularly in Empetrum but not in Betula, whereas shading gave a negative response, strong for Betula and modest for Cassiope and Empetrum [5], [13], [19], [20], [21]. After more than two decades of treatment, we expected the growth responses of arctic shrubs to differ from the short-term responses for three reasons. First, the steady changes in community composition, favouring graminoids, which were observed in fertilized plots in the short-term [22], and the competition for light that graminoids exert on prostrate shrubs [5], are likely to negatively affect the shrub growth over the longer term. Second, the mechanisms that buffered the negative effect of shading in the first years of treatment (e.g. usage of stored resources, short-term acclimations) [19], [21], were expected to weaken over the longer term, in particular for the less shade tolerant species such as Betula and Cassiope. Third, the rate of physiological processes that counterbalanced the positive effect of warming on gross photosynthesis over the shorter term (e.g. respiration, tissue turnover) [9], [11] was expected to decrease because of long-term acclimation [9], [23].
The stem secondary growth of shrubs (cambial growth or increase in stem diameter) accounts for a significant portion of aboveground net primary production in tundra ecosystems (e.g. up to ∼50% at species level (Salix pulchra [24]) and ∼20% at plant community level (subarctic heath [25])) and it is sensitive to environmental perturbations [26]. Nevertheless, secondary growth is seldom investigated. The physiological function of secondary growth differs from the one of primary growth. In fact, whereas primary growth assures light interception and photosynthetic uptake, secondary growth sustains the C uptake (e.g. by producing new conduits for water and sugar transport) but also provides the essential mechanical support to the canopy [26]. In a recent study on the growth of arctic shrubs, Campioli et al. [27] found that changes in primary and secondary growth between sites with different environmental conditions were not proportional.
In detail, we tested two hypotheses. Hypothesis 1. The growth responses of arctic shrubs to long-term environmental manipulations differ from the short-term growth responses. Over the longer term, warming was expected to have a more positive effect, fertilisation a less positive effect (or even a negative effect) and shading a more negative effect. Hypothesis 2. The responses of primary and secondary growth to environmental manipulations differ according to the concurrent morphological changes. If the manipulations promoted morphological changes implying enhanced mechanical support for the shrub stem (e.g. increase in shrub height or branching), the response of the secondary growth is expected to differ from the response of the primary growth. On the other hand, if the morphology of the shrub was not altered by the manipulations, primary and secondary growth are expected to present similar response patterns.
Results
Growth rates
The long-term environmental manipulations did not affect the total growth of Cassiope and Empetrum (Fig. 1a,b; Table 1). By contrast, the secondary growth increased under fertilisation for both species (Fig. 1a,b; Table 1). The total growth of Betula was significantly reduced (by a factor 2.0–2.4) under shading and fertilisation (Fig. 1c; Table 1). For Betula, the primary growth presented significant trends similar as for the total growth, whereas the secondary growth increased under fertilisation (Fig. 1c; Table 1).
Growth rate (bars: total aboveground vegetative growth, indicated as ‘total’; white stacks: primary growth i.e. leaves plus apical stem, indicated as ‘prim.’; grey stacks: secondary growth i.e. stem diameter increment, indicated as ‘sec.’; mean+1SE; n = 5–6) of the shrubs Cassiope tetragona, Empetrum hermaphroditum and Betula nana in a subarctic heath in Abisko (Northern Sweden) subjected to 22 years of environmental manipulation: shading (S), warming (W), fertilisation (F), combined warming plus fertilisation (WF). The control is indicated by C. The environmental factors significantly affecting growth are reported on the top left corner of each panel (shad: shading; fert: fertilisation) with the symbols + and − indicating the direction of the response, positive and negative, respectively. Note the different scale between y-axes of panel A and panel B,C.
Samples from the control treatment showed that the total growth rate was largest for Betula (∼130% year−1), intermediate for Empetrum (∼110% year−1) and lowest for Cassiope (∼70% year−1), and that the primary growth represented 80–85% of the total growth for each species (Fig. 1a,b,c). Leaf production accounted for the large majority of primary growth: 85% for Cassiope and Empetrum and 98% for Betula.
Shrub height and length
Shrub height was positively affected by warming for each species and by fertilisation for Empetrum and Betula (Fig. 2a,b,c; Table 1). Increase in height was of particular relevance in the warming plus fertilisation treatment (WF), where shrubs were 2–3 times taller than in the control (Fig. 2a,b,c). Shading had no effect on shrub height (Fig. 2a,b,c; Table 1). The impact of the environmental manipulations on shrub length was similar to the impact on shrub height (Fig. 2g,h,i). In contrast to shrub height, shrub length of Cassiope was positively affected by shading (Fig. 2g; Table 1) which relates to a significant increase in the number and length of the branches (see below).
Values (mean+1SE; n = 5–6) of shrub height (left panels), apical increment (central panels) and shrub length (right panel) of three subarctic heath shrubs (Cassiope tetragona, Empetrum hermaphroditum and Betula nana) in Abisko (Northern Sweden) subjected to 22 years of environmental manipulation (shading S, warming W, fertilisation F, combined warming plus fertilisation WF) against the control (C). The environmental factors significantly affecting growth are reported on the upper part of each panel (shad: shading; warm: warming; fert: fertilisation, and warm×fert: warming×fertilisation) with the symbols + and − indicating the direction of the response (positive and negative, respectively).
Branch number, branch length and apical increment
Shading exerted mainly a positive impact on the number and length of the youngest branches, particularly for Cassiope (Fig. 3a,d). Fertilisation had mainly a negative impact on the number and length of old branches of Empetrum and, particularly, Cassiope and a positive impact on the length of the youngest branches (up to 3 year-old) of all species (Fig. 3). The impact of warming was minor and affecting only Cassiope and Empetrum, with reduced branch numbers in few old cohorts and increased branch length in few young cohorts (Fig. 3a,b,d,e). The F and p values of the ANOVA analyses are reported in Table S1.
Number and length of the branches vs. branch age (means+1SE; n = 5–6) of the shrubs Cassiope tetragona, Empetrum hermaphroditum and Betula nana at a subarctic heath in Abisko (Northern Sweden) after 22 years of environmental manipulation. Text on the top left indicates the environmental factors with a significant impact (shad: shading; warm: warming; fert: fertilisation, and warm×fert: warming×fertilisation), their direction (+: positive, −: negative) and the age of the branches affected. Note the different scale between y-axes of panel A,B,D,E and panel C,F.
The apical increment of Cassiope was positively affected by shading and warming, whereas the apical increment of Empetrum and Betula was positively affected by fertilisation (Fig. 2d,e,f; Table 1). Overall, the number of branches was similar for Cassiope and Empetrum but much lower (a factor of 2–4) for Betula (Fig. 3a,b,c). Cassiope and Empetrum presented branch length larger than Betula for young cohorts but similar branch length for older cohorts (Fig. 3d,e,f).
Species coverage
Fertilisation had a positive impact on the coverage of graminoids and Empetrum and negative on the coverage of Cassiope, whereas warming had a positive effect on Betula (Fig. 4; Table 2). Overall, the total vascular cover was positively affected by warming and fertilisation and negatively affected by shading (Fig. 4; Table 2). Graminoids increased by a factor of 6 in the WF treatment (Fig. 4).
Coverage (mean+1SE; n = 6) of the shrubs Cassiope tetragona, Empetrum hermaphroditum and Betula nana, the graminoids (gram.) and of the total vascular species (total vasc.) at a subarctic heath in Abisko (Northern Sweden) after 22 years of environmental manipulation: shading (S), warming (W), fertilisation (F), combined warming plus fertilisation (WF). Text on the top left indicates the environmental factors with a significant impact on coverage (shad: shading; warm: warming; fert: fertilisation, and warm×fert: warming×fertilisation) and their direction (+: positive, −: negative).
Discussion
Our expectations were only partially confirmed, with differences among treatments and species. Both hypotheses were overall valid under fertilisation but not under warming. For shading, the expectations were confirmed for Empetrum and Betula only partially and were not confirmed for Cassiope. Besides the growth patterns, the study showed that the investigated shrubs developed a significant plasticity over the longer term.
Hypothesis 1: growth responses change over the longer term
Fertilisation.
As expected, the effect of fertilisation became less favourable over the longer term for each species. The effect of fertilisation on Empetrum and Cassiope changed from positive to non-significant (Table 3). This reveals that the positive effect of nutrient addition on the growth of evergreen dwarf-shrubs was transient at our experiment because of the concomitant positive effect of fertilisation on graminoids. A progressive shrub decline concurrent to an increase in graminoids has previously been observed in other subarctic and low arctic fertilised heaths [28], [29]. Furthermore, the growth of evergreen dwarf-shrubs degenerated in tussock tundra after 3 and 9 years of fertilisation because of the progressive increase in competition with Betula [9]. However, our study is the first to show that after more than two decades of treatment, aboveground growth of evergreen dwarf-shrubs is not suppressed and ancillary positive growth impacts are still recorded (e.g. increase in Empetrum coverage, Fig. 4). This is likely due to the shade tolerance of Cassiope and Empetrum and to morphological plasticity (see below). Betula showed a different dynamics as the effect of fertilisation changed from non-significant to strongly negative (i.e. halving of the growth rate). Despite an important plastic response (see below), Betula was suppressed over the longer term because the competition with graminoids was particularly severe for this species characterized by low shade tolerance. However, Betula might suffer competition (or other growth limitations) even in control conditions at our site and fertilisation likely exacerbates a natural constrained growth. This is supported by comparing the growth of Betula at the experimental site with the growth of Betula at other heath sites [27] and by the fact that the growth of fertilised Betula was stimulated after 8 years of treatment in a more open tundra heath despite an even larger increase in graminoids abundance [28].
Shading.
Despite some acclimation to shade (e.g. increased leaf nitrogen and chlorophyll [21]), the growth of Cassiope and Empetrum showed some negative responses in the first 10 years of shading treatment (Table 3). Over the longer term, contrary to our expectations, negative effects disappeared as the response of the growth rate of Cassiope and Empetrum to shade was non-significant. Cassiope was expected to have a limited shade tolerance as it does not grow in shaded habitats [19]. However, Cassiope likely compensated the negative effect of shading by substantial changes in allocation pattern. While maintaining the same growth rate (and thus biomass production), shaded Cassiope ramets increased greatly in branch numbers and branch length (Fig. 3a,d), hence increasing photosynthesising surface and light interception. Empetrum is likely to be shade tolerant (it grows in the understory of taller tundra shrubs and boreal forests [21]) and only very minor changes in morphology were observed over the longer term. On the other hand, the response of Betula to shading confirmed our expectations for this species. The reduction of aboveground growth of shaded Betula was one of the most significant responses recorded in our study and it was related to a strong reduction in leaf production. This confirms that the negative response of Betula leaves observed earlier at the same plots was not transient (Table 3). On the other hand, the observed continuous growth decline was not associated with alteration in Betula cover (Fig. 4). Despite the well known low tolerance of Betula to shade [30], [31], some compensatory processes might have played a role over the longer term and avoided complete suppression. For instance, shaded Betula might have partially benefitted from a reduction in total vascular cover (Fig. 4) or from a reduction in the stem turnover, which is stimulated in shaded Betula [9] and is perhaps responsible for the transient reduction in stem biomass recorded earlier in our plots (Table 3).
Warming.
Contrary to our expectations, the effect of warming on aboveground growth was non-significant after 22 years of treatment. Despite the consensus on the positive direct effect of warming on the growth of arctic plants, our findings suggest that physiological processes limiting net biomass production (e.g. respiration, stem turnover; [9], [11]) do not acclimate over the longer term. Alternatively, other factors might limit growth under long-term warming [11]. For instance, nutrient limitation might be important in our warmed plots due to increased vascular cover and competition (Fig. 4). On the other hand, heat stress might occur on warmed plants during warm summer days [11], as observed for Ledum palustre in the Low Arctic [9] and in Salix arctica in the Mid Arctic [32]. Empetrum is likely to be particularly sensitive to heat stress as it was favoured by warming level of 2.5°C and not by warming level of 4°C at our site after 6 years of treatment [20]. Our results indicate thus that the positive effect of warming on Cassiope recorded after 5 years of treatment was transient (Table 3). Transient positive responses to warming have been observed in other short-term tundra warming experiments and associated with temporary increases in mineralization or use of stored resources [11].
Hypothesis 2: responses of primary and secondary growth differ according to morphology
Fertilisation.
Fertilised ramets of the three species showed a similar pattern with non-significant variation or decrease in primary growth and increase in secondary growth (Fig. 1). For Empetrum and Betula, this pattern was accompanied by a significant increase in shrub height, total shrub length and length of the youngest branches. For these two species our expectations were therefore confirmed. In presence of a lush graminoid canopy, Empetrum and Betula (procumbent at the site) grew more vertically and explored more lateral space. A more erected and large posture requires more resources to reinforce the stem mechanical strength, implying enhanced secondary growth. This typical morphological plastic reaction prevented these shrubs from being completely confined in the shaded understory. For Empetrum, such response likely avoided reduction in the aboveground growth. For Betula, such plastic reaction was likely not enough to maintain the same C assimilation as in the control, resulting in fewer resources available for primary growth and in an overall growth reduction. Cassiope is likely to have a similar pattern as for Empetrum but less marked. In fact, for Cassiope, the significant increase in secondary growth was coupled to a non-significant increase in shrub height (p = 0.11) (Table 1).
Shading.
Our expectations were confirmed for Empetrum, whose growth pattern and morphology were both unaffected by shading. For Betula, we did not expect uncoupling in the response of primary and secondary growth as the morphology of Betula did not change in shaded plots. However, the prolonged light attenuation significantly decreased Betula leaf production, impairing the relationship between primary and secondary growth. Cassiope showed a less clear pattern with no increase in secondary growth and substantial increase in total length and branching. However, the fact that the shaded Cassiope ramets had low stature (Fig. 2b) probably resulted in procumbent Cassiope branches laid on the moss mat, thus requiring less mechanical support from the stem.
Warming.
Warmed ramets showed unaffected primary and secondary growth but increased shrub height and (for Cassiope and Empetrum) increased shrub length and branch length of the youngest branches. This was unexpected. It is possible that the morphological changes under warming were the result of an overall improved (micro)environment rather than the result of the competition for light as in the fertilised plots. Such supposition is coherent with the species coverage results, which showed no negative impact of warming, increase in total vascular cover and no impact on graminoids (Fig. 4).
Overall.
Previous short term (<10 years) studies on tundra concluded that evergreen dwarf-shrubs have low developmental plasticity, conservative secondary growth and tend to become subcanopy species [9], [26], [33]. Our study reveals that evergreen dwarf-shrubs can show opposite dynamics over the longer term and posses an overall important plasticity. As acclimation normally occurs through formation of new tissue, it is indeed plausible that slow growing species need long time to acclimate [9], [34]. Furthermore, our study showed that apical increment presented a different response than primary growth for each treatment and species. This because length increment does not necessarily correlate to biomass increment in arctic shrubs [25], [27]. Such uncoupling calls for caution when inferring growth responses of tundra shrub to environmental manipulations from apical increment only.
Materials and Methods
Experimental set up
Study site.
The study took place at a tree-line heath on sloping terrain (20–30%) at 450 m a.s.l. at Abisko (68°21′N, 18°49′E), in Northern Sweden. The region has a subarctic montane climate, with mean annual temperature and precipitation of −1.0°C and 304 mm, respectively, and the growing season lasting from early-mid June until late August-early September [25], [35]. The site is an evergreen dwarf-shrub community dominated by Cassiope tetragona and by the co-dominant Empetrum hermaphroditum. Betula nana is one of the most common deciduous shrubs. Graminoids and forbs are also present, as well as nonvascular plants which form a continuous mat [20]. Bedrock consists of base-rich mica schists [19]. The soil has pH of 7.1 (typical for ecosystems with similar bedrock and topography in the region [36]), an organic layer of about 15 cm and is well drained [25], [37], [38]. No specific permits were required for the described field studies, as the location is not privately-owned and not protected and the field studies did not involve endangered or protected species.
Environmental manipulations.
The experiment started in 1989 in an area of about 400 m2. It consisted of eight treatments replicated in six blocks: control, low warming, high warming, shading, fertilisation, fertilisation plus low warming, fertilisation plus high warming and fertilisation plus shading [13]. In this study, we investigated five key treatments: shading (S), high warming (W), fertilisation (F), fertilisation plus high warming (WF) and control (C). Temperature was enhanced by small (1.2×1.2 m, 50 cm high) dome-shaped open top greenhouses of polyethylene film (0.05 mm) supported by PVC tubes. Greenhouses were in place every year from early June (just after snowmelt) until end of August-early September (leaf fall) enhancing the summer air and soil temperature by 3.9°C and 1.2°–1.8°C, respectively. The greenhouses did not provoke critical side effects on plant growth because: (1) they caused only minor and non-significant reduction in relative soil water content (<6%) as the sloping terrain permitted lateral water movement [19], [21]; (2) they did not change significantly the air humidity (<3%); (3) they only led to a 9% reduction in photosynthetically active radiation [19], [21]; (4) they did not affect the snow cover as they were not in place in winter and (5) their sheltering effect had a minor impact on shrub morphology as in tundra heath the effect of wind exposure on the shrub structure is much more relevant in winter [7], [39]. Furthermore, the greenhouses (resting on the shrub canopy and opened at the top) do not impact the presence of small herbivores (e.g. insects, rodents). Reindeer grazing and moose browsing is generally limited to periods out of the growing season (e.g. reindeers normally do not stay at the tree-line during summer) and are not affected by our manipulative experiment, which is in place only between June and August. The shading was obtained with hessian (jute) fabric, arranged in the same way and in the same period as the polyethylene film of the greenhouses. Hessian fabric reduced the light by 64% without significant effect on air humidity and temperature [19], [21]. Fertilisation (10.0 g m−2 N, 2.6 g m−2 P and 9.0 g m−2 K, in the form of NH4NO3, KH2PO4 and KCl) occurred once per year after snow melt in June (except in 1998, half amount, and in 1993 and 2001, not applied). The dose of N applied was considered similar in magnitude to potential N release from the soil of tundra ecosystems under global change scenario [15].
Sampling and processing of shrub ramets.
Sampling took place in mid-late August 2010, after 22 years of experimental manipulation. Individual ramets (i.e. aboveground stem with all lateral branches) of Cassiope and Empetrum (two ramets) and Betula (one ramet) were collected for each block and treatment (n = 6). However, for Betula, only five replicates were considered in the analysis as most of the ramets of one block were too young or too damaged (i.e. broken stem or branches) to be analyzed. The ramets were sampled in the central part of the experimental plots. This assured that biases due to sampling of ramets supporting biomass outside of the plot or ramets grown into the plots after the treatment began were minor because (i) the colonization rate of these slow growth ericaceous plants is inherently low [19], (ii) the shrub frequency in the area surrounding the plots has been reduced by trampling [40] and (iii) woody functional type as evergreen and multiple-flush deciduous have a high degree of ‘shoot autonomy’ [41], meaning that relocation of assimilates among ramets is limited.
Stem and branches were divided into segment cohorts of the same age. This was done by counting the apical bud scars for Empetrum [24], the stem sections with smaller leaves for Cassiope [42] and the annual growth rings in thin stem/branch cross-sections after staining with 0.5% phloroglucinol in 10% HCl for Betula [26]. Each stem/branch segment cohort was dried at 70°C for 48 hours and leaves were detached. The number of stem/branch segments of each cohort, their aggregated length and dry weight were recorded [24] as well as the weight of the current-year leaves. Ramets of Empetrum and Betula were 5–7 year-old. Ramets of Cassiope were 10–12 year-old.
Measurement of growth variables
Growth of shrubs was assessed with comparable but refined methods to the ones used to characterize growth responses in the first decade of manipulation, as the latter were too invasive to be repeated (e.g. standing biomass harvest) or had limitations (e.g. lack of assessment of secondary growth and branching pattern). In the current study, shrub growth was determined as primary growth (leaf and apical stem production) and secondary growth, both expressed as percentage of old stem biomass [24], [26], [27], [43], [44]. Data on growth rate were complemented by several measurements of shrub morphology (e.g. shrub height, number and length of branches, total length of stem and branches) and of species coverage. Growth rates were used to evaluate the long-term impact of the environmental manipulations on shrub growth because they provide a direct estimation of plant biomass production. Morphological characteristics were compared to the growth rate estimates to better understand the response pattern of the primary- and secondary growth. The species coverage was used to indirectly infer species abundance. A summary of the growth variables measured, the plant organ and organ age considered and the way the results are expressed (e.g. relative or absolute values, values per plot or per ramet) is reported in Table 4.
Growth rates.
We assessed the annual rate of the aboveground vegetative growth as primary-, secondary- and total growth. We determined primary growth rate (% year−1) for each ramet as the production of current year's apical biomass (leaves and stem) as a percentage of old standing stem biomass [27]. The data needed to calculate the primary growth were directly available from the harvested material (see above). The stem secondary growth was expressed in the same way but the current-year secondary growth was not directly available from the harvested material. Instead, we derived that following the model of Bret-Harte et al. [26] (see key equations below) who assumed that (i) a stem/branch segment is cylindrical, (ii) the annual increment in stem/branch radius does not vary with the age of the stem/branch segments in the aboveground portion of the ramet, and (iii) the annual increment in stem/branch radius changes under manipulated environmental conditions. For the study species, the performance of the model of Bret-Harte et al. [26] was very good, with average slopes of the regression modelled vs. measured standing stem biomass M of 0.90–1.1 and r2>0.94 [45]. The total growth rate was calculated as the sum of the primary and secondary growth rate.
The calculation of the secondary growth of individual ramets at yearly basis is summarized in four steps (for details see [26]). (i) The mass (m) of a stem/branch segment cohort of a given age n (in years) of an individual ramet is estimated as:(1)where l is the length of the stem/branch segment cohort, c equals (m/l)1/2 of the current-year stem and α the slope of a linear relationship (m/l)1/2 vs. n. (ii) The annual mass increment due to secondary growth (Δm) of a stem/branch segment cohort equals:
(2)(iii) The mass (M) of an individual ramet is calculated as the sum of m for all the segment cohort age classes and the annual mass increment due to secondary growth (ΔM) as the sum of Δm for all the segment cohort age classes. (iv) The annual stem secondary growth rate equals ΔM/M.
Shrub height and length.
The height of nine randomly selected shoots of Cassiope, Empetrum and Betula was measured in two 25×50 cm rectangulars within the central area of each plot in mid-late August 2010 and averaged for each plot (n = 6). The height was measured with a ruler as the perpendicular height from shoot apex to ground. Shrub length refers to the total length of stem and branches of each ramet of Cassiope, Empetrum and Betula sampled for the determination of the growth rate (see above).
Branch number, branch length and apical increment.
Branch number and branch length of each ramet of Cassiope, Empetrum and Betula were derived separately for each age class composing the ramet (in years) from the ramets sampled for the determination of the growth rate (see above). Branch length refers to the total aggregated length for a given branch age class. The length of the current year's branches is defined as apical increment. As young stem and young branches are difficult to differentiate for the clonal species investigated, all woody segments of a given age class were considered as branches in these assessments.
Species coverage.
Species coverage was measured in mid-late August 2010 with the pin-point method in the same two rectangulars (25×50 cm) per plot investigated for shrub height. A pin was passed vertically at 100 points (5 cm spaced) and all matter touched by the pin was recorded as a hit [46]. Vascular vegetation was recorded at species level, nonvascular vegetation was lumped in bryophytes and lichens, whereas attached or unattached dead tissue was recorded as litter. In this study, we present coverage data for the model shrub species Cassiope, Empetrum and Betula, for the lumped graminoids group and for the total vascular plant cover.
Statistics
The impact of manipulated environmental factors (warming, fertilisation, shading) was assessed with analysis of variance. Due to the incomplete factorial design, the analysis was conducted separately for (i) shading and (ii) warming and fertilisation [13]. The response to shading was tested with a one-way ANOVA, whereas the response to warming and fertilisation with a two-way ANOVA with interaction between warming and fertilisation. The block factor was not considered because preliminary analyses showed that it had no effect on the dependent variables. If prerequisites for analysis of variances (normality, checked with Shapiro test, and homoscedasticity, checked with Bartlett test) were not met, we performed a Kruskal-Wallis test instead of one-way ANOVA or repeated the same analysis after transformation (logx and in few cases x1/2 or x−1) for two-way ANOVA, as no standard non-parametric test fitted our design and transformed data fulfilled the ANOVA prerequisites. Transformation was needed for: (i) growth rates of Cassiope and Empetrum, (ii) total height of each species, (iii) total length and apical increment of Cassiope and Empetrum, (iv) coverage of Cassiope, Betula and graminoids, and (v) datasets on branch number and branch length (see details in Table S1).
Dependent variables tested with the ANOVA analysis were growth rates (primary, secondary and total), shrub height, shrub length, species coverage, apical increment, branch number and length. Primary and secondary growth were tested separately as they proved to be uncorrelated (tested with Pearson's correlation) for any treatment and species. If more within-plot measures of the dependent variable were available per plot (e.g. for growth rates of Cassiope and Empetrum), a nested level was added to the ANOVAs. Treatment effects on branch number and length were tested separately for each species and age class, except for 7 year-old branches of Empetrum and Betula which were not analyzed because of the few replicates available. All analyses were performed in R version 2.12.2 (R Development Core Team 2011).
Supporting Information
Table S1.
Results of ANOVAs (F and P values) on the number and length of branches of cohort of the same age (up to 12 year-old) of the shrubs Cassiope tetragona, Empetrum hermaphroditum and Betula nana at a subarctic heath in Abisko (Northern Sweden) after 22 years of environmental manipulation.
https://doi.org/10.1371/journal.pone.0034842.s001
(DOC)
Acknowledgments
Special thanks are due to the Abisko Scientific Research Station for the logistic support.
Author Contributions
Conceived and designed the experiments: MC AM. Performed the experiments: MC NL AM. Analyzed the data: MC NL. Contributed reagents/materials/analysis tools: MC AM. Wrote the paper: MC NL AM.
References
- 1.
Solomon S, Qin D, Manning M, Chen Z, Marquis M, et al., editors. IPCC (2007) Climate change 2007: the physical science basis. Contribution of Working Group I to the fourth assessment report of the Intergovernmental Panel on Climate Change. Cambridge and New York: Cambridge University Press.
- 2. Callaghan TV, Bjorn LO, Chernov Y, Chapin T, Christensen TR, et al. (2004) Effects on the function of arctic ecosystems in the short- and long-term perspectives. Ambio 33: 448–458.
- 3. Callaghan TV, Bjorn LO, Chernov Y, Chapin T, Christensen TR, et al. (2004) Effects of changes in climate on landscape and regional processes, and feedbacks to the climate system. Ambio 33: 459–468.
- 4. Arft AM, Walker MD, Gurevitch J, Alatalo JM, Bret-Harte MS, et al. (1999) Responses of tundra plants to experimental warming: Meta-analysis of the international tundra experiment. Ecol Monog 69: 491–511.
- 5. van Wijk MT, Clemmensen KE, Shaver GR, Williams M, Callaghan TV, et al. (2004) Long-term ecosystem level experiments at Toolik Lake, Alaska, and at Abisko, Northern Sweden: generalizations and differences in ecosystem and plant type responses to global change. Global Change Biol 10: 105–123.
- 6. Wookey PA (2008) Experimental approaches to predicting the future of tundra plant communities. Plant Ecol Divers 1: 299–307.
- 7. Sonesson M, Callaghan TV (1991) Strategies of survival in plants of the Fennoscandian tundra. Arctic 44: 95–105.
- 8. Trumbore S (2006) Carbon respired by terrestrial ecosystems - recent progress and challenges. Global Change Biol 12: 141–153.
- 9. Chapin FS, Shaver GR (1996) Physiological and growth responses of arctic plants to a field experiment simulating climatic change. Ecology 77: 822–840.
- 10. Jonasson S, Michelsen A, Schmidt IK (1999) Coupling of nutrient cycling and carbon dynamics in the Arctic, integration of soil microbial and plant processes. Appl Soil Ecol 11: 135–146.
- 11. Callaghan TV, Bjorn LO, Chernov Y, Chapin T, Christensen TR, et al. (2004) Responses to projected changes in climate and UV-B at the species level. Ambio 33: 418–435.
- 12. Callaghan TV, Bjorn LO, Chernov Y, Chapin T, Christensen TR, et al. (2004) Effects on the structure of arctic ecosystems in the short- and long-term perspectives. Ambio 33: 436–447.
- 13. Jonasson S, Michelsen A, Schmidt IK, Nielsen EV (1999) Responses in microbes and plants to changed temperature, nutrient, and light regimes in the arctic. Ecology 80: 1828–1843.
- 14.
Shaver GR, Jonasson S (2001) Productivity of arctic ecosystems. In: Roy J, Saugier B, Mooney HA, editors. Terrestrial global productivity. San Diego: Academic Press. pp. 189–209.
- 15. Mack MC, Schuur EAG, Bret-Harte MS, Shaver GR, Chapin FS (2004) Ecosystem carbon storage in arctic tundra reduced by long-term nutrient fertilisation. Nature 431: 440–443.
- 16. Tape K, Sturm M, Racine C (2006) The evidence for shrub expansion in Northern Alaska and the Pan-Arctic. Global Change Biol 12: 686–702.
- 17. Forbes BC, Macias Fauria M, Zetterberg P (2010) Russian Arctic warming and ‘greening’ are closely tracked by tundra shrub willows. Global Change Biol 16: 1542–1554.
- 18. Hallinger M, Manthey M, Wilmking M (2010) Establishing a missing link: warm summers and winter snow cover promote shrub expansion into alpine tundra in Scandinavia. New Phytol 186: 890–899.
- 19. Havström M, Callaghan TV, Jonasson S (1993) Differential growth-responses of Cassiope tetragona, an arctic dwarf shrub, to environmental perturbations among three contrasting High sites and Sub-Arctic sites. Oikos 66: 389–402.
- 20. Graglia E, Jonasson S, Michelsen A, Schmidt IK (1997) Effects of shading, nutrient application and warming on leaf growth and shoot densities of dwarf shrubs in two arctic-alpine plant communities. Ecoscience 4: 191–198.
- 21. Michelsen A, Jonasson S, Sleep D, Havström M, Callaghan TV (1996) Shoot biomass, δ13C, nitrogen and chlorophyll responses of two arctic dwarf shrubs to in situ shading, nutrient application and warming simulating climatic change. Oecologia 105: 1–12.
- 22. Graglia E, Jonasson S, Michelsen A, Schmidt IK, Havstrom M, et al. (2001) Effects of environmental perturbations on abundance of subarctic plants after three, seven and ten years of treatments. Ecography 24: 5–12.
- 23. Atkin OK, Tjoelker MG (2003) Thermal acclimation and the dynamic response of plant respiration to temperature. Trends plant sci 8: 343–351.
- 24. Shaver GR (1986) Woody stem production in Alaskan tundra shrubs. Ecology 67: 660–669.
- 25. Campioli M, Michelsen A, Demey A, Vermeulen A, Samson R, et al. (2009) Net primary production and carbon stocks for subarctic mesic-dry tundras with contrasting microtopography, altitude, and dominant species. Ecosystems 12: 760–776.
- 26. Bret-Harte MS, Shaver GR, Chapin FS (2002) Primary and secondary stem growth in arctic shrubs: implications for community response to environmental change. J Ecol 90: 251–267.
- 27. Campioli M, Leblans N, Michelsen A (2012) Stem secondary growth of tundra shrubs: impact of environmental factors and relationships with apical growth. Arc Antarc Alp Res 44: 16–25.
- 28. Gough L, Wookey PA, Shaver GR (2002) Dry heath arctic tundra responses to long-term nutrient and light manipulation. Arc Antarc Alp Res 34: 211–218.
- 29. Richardson SJ, Press MC, Parsons AN, Hartley SE (2002) How do nutrients and warming impact on plant communities and their insect herbivores? A 9-year study from a sub-arctic heath. J Ecol 90: 544–556.
- 30. DeGroot WJ, Thomas PA, Wein RW (1997) Betula nana L and Betula glandulosa Michx. J Ecol 85: 241–264.
- 31. Niinemets U, Portsmuth A, Truus L (2002) Leaf structural and photosynthetic characteristics, and biomass allocation to foliage in relation to foliar nitrogen content and tree size in three Betula species. Ann Bot-London 89: 191–204.
- 32. Marchand FL, Kockelbergh F, van de Vijver B, Beyens L, Nijs I (2006) Are heat and cold resistance of arctic species affected by successive extreme temperature events? New Phytol 170: 291–300.
- 33. Parsons AN, Welker JM, Wookey PA, Press MC, Callaghan TV, et al. (1994) Growth responses of four sub-arctic dwarf-shrubs to simulated environmental change. J Ecol 82: 307–318.
- 34. Berry J, Björkman O (1980) Photosynthetic response and adaptation to temperature in higher plants. Annual Review of Plant Physiology and Plant Molecular Biology 31: 491–543.
- 35. Campioli M, Michelsen A, Samson R, Lemeur R (2009) Seasonal variability of leaf area index and foliar nitrogen in contrasting dry-mesic tundras. Botany 87: 431–442.
- 36. Arnesen G, Beck PSA, Engelskjon T (2007) Soil acidity, content of carbonates, and available phosphorus are the soil factors best correlated with alpine vegetation: Evidence from Troms, North Norway. Arc Antarc Alp Res 39: 189–199.
- 37. Schmidt IK, Jonasson S, Shaver GR, Michelsen A, Nordin A (2002) Mineralization and distribution of nutrients in plants and microbes in four arctic ecosystems: responses to warming. Plant Soil 242: 93–106.
- 38. Ruess L, Michelsen A, Schmidt IK, Jonasson S (1999) Simulated climate change affecting microorganisms, nematode density and biodiversity in subarctic soils. Plant Soil 212: 63–73.
- 39. Callaghan TV, Bjorn LO, Chernov Y, Chapin T, Christensen TR, et al. (2004) Biodiversity, distributions and adaptations of arctic species in the context of environmental change. Ambio 33: 404–417.
- 40. Tybirk K, Nilsson MC, Michelson A, Kristensen HL, Shevtsova A, et al. (2000) Nordic Empetrum dominated ecosystems: Function and susceptibility to environmental changes. Ambio 29: 90–97.
- 41. Sprugel DG, Hinckley TM, Schaap W (1991) The theory and the practice of branch autonomy. Annual Review of Ecology and Systematics 22: 309–334.
- 42. Callaghan TV, Carlsson BA, Tyler NJC (1989) Historical records of climate-related growth in Cassiope tetragona from the Arctic. J Ecol 77: 823–837.
- 43. Shaver GR, Chapin FS (1991) Production - biomass relationships and element cycling in contrasting arctic vegetation types. Ecol Monogr 61: 1–31.
- 44. Shaver GR, Laundre JA, Giblin AE, Nadelhoffer KJ (1996) Changes in live plant biomass, primary production and species composition along a riverside toposequence in Arctic Alaska, USA. Arc Antarc Alp Res 28: 363–379.
- 45.
Leblans N (2011) Environmental drivers and expected impacts of climate change on the secondary growth of woody shrubs in arctic ecosystems (MS thesis in Dutch). Wilrijk: University of Antwerp.
- 46. Press MC, Potter JA, Burke MJW, Callaghan TV, Lee JA (1998) Responses of a subarctic dwarf shrub heath community to simulated environmental change. J Ecol 86: 315–327.