<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">AJPS</journal-id><journal-title-group><journal-title>American Journal of Plant Sciences</journal-title></journal-title-group><issn pub-type="epub">2158-2742</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/ajps.2013.43A094</article-id><article-id pub-id-type="publisher-id">AJPS-29518</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Biomedical&amp;Life Sciences</subject></subj-group></article-categories><title-group><article-title>
 
 
  Lichen-Spruce Woodland Early Indicators of Ecological Resilience Following Silvicultural Disturbances in Qu&#233;bec’s Closed-Crown Forest Zone
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>steban</surname><given-names>Gonzalez</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>François</surname><given-names>Hébert</given-names></name><xref ref-type="aff" rid="aff2"><sup>2</sup></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jean-François</surname><given-names>Boucher</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pascal</surname><given-names>Sirois</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Daniel</surname><given-names>Lord</given-names></name><xref ref-type="aff" rid="aff1"><sup>1</sup></xref></contrib></contrib-group><aff id="aff2"><addr-line>Direction de la Recherche Forestière, Ministère des Ressources Naturelles, Québec, Canada.</addr-line></aff><aff id="aff1"><addr-line>Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Saguenay, Canada</addr-line></aff><author-notes><corresp id="cor1">* E-mail:<email>francois.hebert@mrn.gouv.qc.ca(FH)</email>;</corresp></author-notes><pub-date pub-type="epub"><day>29</day><month>03</month><year>2013</year></pub-date><volume>04</volume><issue>03</issue><fpage>749</fpage><lpage>765</lpage><history><date date-type="received"><day>January</day>	<month>6th,</month>	<year>2013</year></date><date date-type="rev-recd"><day>February</day>	<month>18th,</month>	<year>2013</year>	</date><date date-type="accepted"><day>February</day>	<month>24th,</month>	<year>2013</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
   Lichen woodlands (LW) located in the closed-crown boreal forest are not a successional stage moving towards a closed black spruce feathermoss stand (FM), but an alternative stable state, due to their previous forest history, and the occurrence of LWs located nearby closed-crown FM stands. Therefore, afforestation in those LWs through site preparation and plantation could shift back LW into FM stands. We implemented an experimental design with different combinations of silvicultural treatments in both site types (LW, FM). We monitored the evolution of plant diversity and the physiology of three bio-indicators (Picea mariana, Kalmia angustifolia, Rhododendron groenlandicum) in different microsites created by the silvicultural treatments. The return to the initial composition was noticed only two years after treatments, especially in the LW stands, thus indicating a higher level of early ecosystem resilience in LWs compared to FM stands. Mean species cover, especially in the FM stands, decreased the most in the skid trails created by logging, probably due to a lack of acclimation of bryophytes to open stand conditions. Conversely, ericaceous shrubs and lichens found in the LWs were already acclimated to open stand conditions, which give to LWs a restructuring advantage compared to FM plant communities after silvicultural treatments. Overall, FM and LW short-term resilience was similar, indicating equally efficient ecosystem reorganization in both stands. The comparable early resilience in managed LW and FM stands, in terms of plant biodiversity, contradicts the presumed fragility of LW stands, especially in this case where LWs are assumed to be an alternative stable state created by compound disturbances. Silvicultural treatments maintained the functional group diversity in LWs, a key element for ecosystem resilience. Therefore, this study support the idea that plantation following site preparation in LWs could be a valuable management strategy to reach several objectives, such as increasing forest carbon sinks.
     
 
</p></abstract><kwd-group><kwd>Afforestation; Black Spruce; Kalmia angustifolia; Rhododendron groenlandicum; Logging; Picea mariana; Vegetation Recovery; Scarification; Silviculture</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction</title><p>Historically, the resilience of ecosystems mainly drew the attention of theoretical ecologists [<xref ref-type="bibr" rid="scirp.29518-ref1">1</xref>]. However, as stressors like forest management and climate change have become increasingly recognized as potential threats to biodiversity, the interest of forest ecologists and managers in ecosystem resilience is now growing substantially [<xref ref-type="bibr" rid="scirp.29518-ref2">2</xref>]. The traditional concept of resilience refers to the stability of an ecosystem near its equilibrium steady-state and its capacity to return to this steady-state following disturbance. This view of resilience is termed engineering resilience [<xref ref-type="bibr" rid="scirp.29518-ref3">3</xref>] and is only theoretically relevant in disturbance-driven ecosystems where the “equilibrium state” is rarely reached [4-6]. A more contemporary definition of resilience, ecological resilience, refers to the amount of disturbance that an ecosystem can endure before it modifies its organizing processes and restructures to an alternative state [1,6-7].</p><p>An alternative stable state is an ecosystem that can persist (i.e., pass through one or several turnovers) under the same environmental and climatic conditions as another different ecosystem type, and is generally characterized by system state variables like species diversity, abundance, and composition. The shift to an alternative stable state occurs if a threshold limit of the biotic mechanisms ensuring ecosystem resilience is exceeded by the severity and/or frequency of disturbances [5,6]. Fire is involved in many cases of alternative stable states in various vegetation systems around the world [<xref ref-type="bibr" rid="scirp.29518-ref5">5</xref>]. In the boreal forest, studies showed evidence of the phenomenon where fire is the main disturbing event [4,6].</p><p>Black spruce (Picea mariana [Mill.] B.S.P.) feathermoss (FM) stands are common in the closed-crown forest zone of the North American boreal forest, which extends from Alaska to Newfoundland [4,8]. Successful black spruce regeneration after wildfire, the main stand-replacement driver of those stands, depends on seed bank quality (seed number and viability) and fire severity [9,10]. However, regeneration may be unsuccessful in the following circumstances: a spruce budworm (Choristoneura fumiferana [Clem.]) outbreak shortly followed by a wildfire, or two back to back fire events, therefore compromising post fire seed production-related regeneration, and favouring competing vegetation encroachment by ericaceous shrubs and lichens [11-13]. This leads to the formation of an open lichen-spruce woodlands (LWs) scattered within the closed-crown forest zone [<xref ref-type="bibr" rid="scirp.29518-ref4">4</xref>]. Between 1950 and 2002, a 9% increase in LWs has been documented in Eastern Canada [<xref ref-type="bibr" rid="scirp.29518-ref10">10</xref>].</p><p>It has been concluded that LWs, within the closecrown boreal forest, are not a successional stage moving towards a closed FM forest, but rather an alternative stable state, because of their previous moss forest history, and the occurrence of adjacent LWs and closed-crown FM stands [4,6]. A natural shift from LW to a closed-crown FM forest is theoretically possible with a sufficient and healthy seed bank, and a wildfire intense enough to remove the lichen mat [<xref ref-type="bibr" rid="scirp.29518-ref14">14</xref>]. However, historical records have so far failed to demonstrate this possibility [<xref ref-type="bibr" rid="scirp.29518-ref6">6</xref>].</p><p>Silviculture could promote LWs shift to closed-crown FM stands, in particular where past presence of the latter is demonstrated or where biophysical conditions to this forest conversion are assembled [<xref ref-type="bibr" rid="scirp.29518-ref15">15</xref>]. This human-induced conversion of open to closed-crown stands can help realize at least two goals: restore the historical tree density in the boreal forest zone [4,6,10,16], and contribute to climate change mitigation through the afforestation of non-forest areas [17-19]. Afforestation efforts in the boreal zone, where manageable open woodlands such as LWs are theoretically abundant in both North America and Russia [19,20], could represent an eventual significant mitigation measures, especially because land use change in boreal territories generates very few conflicts with other human activities, thanks to the uninhabited—and unsuitable for cultivation—nature of the boreal forest [17,19]. However, very few field validations of the support capacity of LWs (and boreal open woodlands in general) to afforestation presently exist, so that this theoretical mitigation potential can get closer to a field-supported feasibility.</p><p>Actually, information is scarce about the effects of logging or site preparation practices on LWs productivity and resilience. H&#233;bert et al. [<xref ref-type="bibr" rid="scirp.29518-ref21">21</xref>] showed that scarification improved water relations and growth of black spruce and jack pine (Pinus banksiana Lamb.) planted seedlings, during the establishment phase, close to levels encountered in seedlings planted on FM stands with a higher intensity of site disturbance (logging + scarification). However, the effect of different intensities of silvicultural disturbances on stand ecological resilience still needs to be addressed to assess the capacity of LWs to support afforestation. Biodiversity can enhance ecosystem resilience, and ecosystem shifts are common where human actions are eroding biological diversity [<xref ref-type="bibr" rid="scirp.29518-ref22">22</xref>]. In many habitats, understory vegetation comprises the vast majority of plant biodiversity and contributes to a wide variety of ecosystem functions [<xref ref-type="bibr" rid="scirp.29518-ref23">23</xref>]. Silviculture affects biodiversity through changes of species composition and abundance, which in turn modifies plant biodiversity [<xref ref-type="bibr" rid="scirp.29518-ref24">24</xref>]. Silviculture also influences species physiology, which can be used as a plant productivity indicator [21,25,26]. Therefore, one could use both plant biodiversity, through measurement of vegetation recovery, and productivity of key species, through measurement of plant traits, to compare the ecological resilience of contrasting ecosystems after disturbance, such as LWs and FM stands after silvicultural treatments [<xref ref-type="bibr" rid="scirp.29518-ref21">21</xref>].</p><p>The objectives of this study were therefore (1) to test and compare the effect of various levels of silvicultural treatments on plant biodiversity and physiology of key species in afforested LWs and reforested closed crown FM stands, two co-existing but contrasting stand types and, (2) to assess and compare the effect of silvicultural treatment intensity on plant biodiversity and physiology of key species in afforested LWs and reforested closed-crown FM stands. A field-based experimental design was implemented with different combinations of silvicultural treatments (logging and scarification) in each site type. We then monitored the evolution of plant diversity and the physiology of three bioindicators (Picea mariana, Kalmia angustifolia, Rhododendron groenlandicum) in different microsites created by the silvicultural treatments, during the establishment phase.</p></sec><sec id="s2"><title>2. Material and Methods</title><sec id="s2_1"><title>2.1. Site Description</title><p>A total of six experimental sites were established in the northeastern North American boreal forest. Four sites were located at the border between the balsam fir/white birch (South) and black spruce/feathermoss (North) bioclimatic domains (49˚42'579''N, 71˚20'512''W), and two in the spruce/feathermoss domain (50˚17'822''N, 72˚02'664''W) [<xref ref-type="bibr" rid="scirp.29518-ref27">27</xref>]. Mean annual temperature for this region between 1971-2000 was 0˚C (&#177; 1.3) with a mean annual precipitation of 961.3 mm (33% as snow) [<xref ref-type="bibr" rid="scirp.29518-ref28">28</xref>]. Soils were humo-ferric podzols (Humods Spodosols) located on a coarse till glacial deposit (&gt;1 m), with a mor humus (depth between 5 and 33 cm), and sandy loam texture (&lt;1 m), except for one site that was established on a fluvioglacial outwash.</p><p>Each site included a lichen-spruce open woodland stand (LW) adjacent to a closed crown black sprucefeathermoss stand (FM), both with similar slope, aspect, soil drainage, tree dominant height, and age since fire (between 70 - 90 years). The LW had a crown cover of less than 25% and FM crown cover was between 60% and 80%. For each stand type, the overstory was dominated by black spruce (BS), associated with jack pine, white birch (Betula papyrifera Marsh.), and trembling aspen (Populus tremuloides Michx.). The understory included ericaceous shrubs like Kalmia angustifolia L. (KA), Rhododendron groenlandicum (Oeder) Kron &amp; Judd (RG), Vaccinium angustifolium Ait., Vaccinium myrtilloides Michx., and Gaultheria hispidula L. M&#252;hl. [<xref ref-type="bibr" rid="scirp.29518-ref21">21</xref>].</p></sec><sec id="s2_2"><title>2.2. Experimental Design</title><p>The experimental design was a six-block factorial, each of the six sites corresponding to one experimental block (statistical replication). Each experimental block included a 2 ha LW stand adjacent to a 2 ha FM stand. The stands were logged and scarified in summer 2005. Careful logging around advance growth (CLAAG) was used as the harvesting method [<xref ref-type="bibr" rid="scirp.29518-ref26">26</xref>]. In every block, a supplementary 1 ha strip of each stand type was kept free of any silvicultural treatment to serve as a control. Every harvested stand (main plot) was then divided randomly in two sub-plots of 1.2 and 0.8 ha. The 0.8 ha sub-plot was scarified with a hydraulic TTS disk scarifier.</p><p>Five microsite types were classified on the basis of site disturbance intensity induced by silvicultural treatments. The microsite categories were (from the lowest to highest level of disturbance): non perturbed (NP), logging strips in the non-scarified plots (S0<sub>LS</sub>), skid trails in the nonscarified plots (S0<sub>ST</sub>), non-disturbed strips in the scarified plots (S1<sub>NS</sub>), and scarification furrows (S1<sub>SF</sub>). Three 4 m<sup>2</sup> sampling plots were randomly assigned to each microsite type, for a total of 30 sampling plots per experimental block. One set of measurements was made before silvicultural treatments for every stand type (LW, FM) &#215; treatment (NP, S0, S1) combination, using three representative 4 m<sup>2</sup> sampling plots per pre-identified combination area.</p><p>For vegetation cover and biodiversity indexes, stand type (LW or FM) was considered as the main plot, microsites in the silvicultural treatments as the sub-plot, and sampling time as the sub sub-plot. Due to a limited daily time frame available for physiological measurements, the main plot was the sampling time with stand type as the sub-plot and silvicultural treatments as the sub sub-plot.</p></sec><sec id="s2_3"><title>2.3. Vegetation Cover and Diversity Measurements</title><p>An exhaustive vegetation inventory was performed in each 4 m<sup>2</sup> sampling plot for the shrub (height &lt; 1 m), herbaceous, and moss layers. After adequate species identification, % cover of each taxon was evaluated visually. Vegetation cover was monitored during four measurement periods: just before silvicultural treatments in 2005 (day 0), after silvicultural treatments in 2005 (day 110), 2006 (day 501), and 2007 (day 801)—the term “day” used hereinafter corresponds to the average day of each measurement period. The vegetation surveys were performed by the same observer within each individual experimental block. Taxa count and abundance served for biodiversity index calculations. Selected indexes were: total vegetation cover (N in %), species richness (S), Pielou’s index of non-randomness (J’), and the Shannon-Wiener diversity index (H’) [<xref ref-type="bibr" rid="scirp.29518-ref29">29</xref>].</p></sec><sec id="s2_4"><title>2.4. Physiological Measurements</title><p>Black spruce (BS), Kalmia (KA), and Rhododendron (RG) were chosen as bio-indicators of plant resilience in response to disturbance from silvicultural practices. Net photosynthesis (A) was measured on current year needles of an excised shoot of one black spruce layer (&lt;1 m in height), and on current foliage of one excised Kalmia stem selected randomly in each experimental unit (S0, S1 and NP). A was measured on day 0, 110, 501, and 801. Excised shoots were placed in a sealed bag containing a wet sponge, and maintained in ambient light before measurements within 15 min following excision. Data were collected on sunny or partly cloudy days. Measurements were carried out with a LI-6400 portable photosynthesis system (LI-COR, Inc. Lincoln, NE, USA) equipped with a 0.25 L conifer chamber cuvette. A halogen lamp was placed at 30 cm above the cuvette to provide saturating light conditions when necessary (&gt;1200 &#181;mol photons m<sup>−2</sup>&#183;s<sup>−1</sup>). Ambient CO<sub>2</sub> was fixed at 400 ppm and the block temperature was set at 25˚C. Net photosynthesis was measured between 11:00 and 15:00 eastern saving time. Sampling on day 0 differed slightly from post disturbance measurements, with two black spruce and two Kalmia samples measured for each stand type (LW and FM) in every block for a total of eight samples per block (48 total). For every post disturbance sampling period, two samples per experimental unit (S0, S1 and NP), per species (black spruce and Kalmia), and per stand type (LW and FM) were collected for a total of 24 samples per block (144 total). Random sampling was done one species at a time and within a short interval for all experimental units of every block, to minimize the impact of time on treatments and/or stand types within a block.</p><p>A sub-sample of ten black spruce needles, selected for A, was stored in a freezer until foliar area determination, following the methodology described in H&#233;bert et al. [<xref ref-type="bibr" rid="scirp.29518-ref21">21</xref>]. For Kalmia, two leaves, which served for A determination, were scanned on a flatbed scanner, and leaf area was determined by software analysis (ImageJ, National Institute of Mental Health, Bethesda, MD, USA). Needles and leaves were then dried at 65˚C for 48 hours to calculate leaf mass per unit of area (LMA). We obtained one LMA measurement per sampling date and per experimental unit (S0-S1-NP); LMA was used to estimate foliar area of black spruce and Kalmia enclosed in the cuvette.</p><p>After each A measurement, two sub-samples of black spruce, Kalmia, and Rhododendron foliage were collected in each experimental unit and pooled to measure foliar nutrient concentrations (N, P, K, Ca, Mg). Each sample was dried at 65˚C for 48 hours and ground to a 40-mesh size prior to analyses. Total Kjeldahl N (TKN) was analyzed colorimetrically by spectrophotometry (Quickchem 8000, Lachat Instruments, Loveland, CO, USA), preceded by a H<sub>2</sub>SO<sub>4</sub>-Se-K<sub>2</sub>SO<sub>4</sub> digestion [<xref ref-type="bibr" rid="scirp.29518-ref30">30</xref>]. P, K, Ca, Mg were extracted with a Mehlich III solution and measured by inductively coupled plasma analysis ICAP- 61E (Inductively Coupled Argon Plasma-Optical Emission Spectrometry, Thermo Fisher Scientific, Waltham, MA, USA).</p></sec><sec id="s2_5"><title>2.5. Statistical Analyses</title><p>Mean vegetation cover of bio-indicators (BS, KA, RG), and biodiversity indexes (N, S, J’, and H’) were submitted to a repeated analysis of variance (ANOVAR) [<xref ref-type="bibr" rid="scirp.29518-ref31">31</xref>]. Three covariance matrixes (unstructured (UN), Compound Symmetry (CS), and Huynh-Feldt (HF)) were tested and the best choice was based on Akaike (AIC) and Schwarz (BIC) estimation parameters [<xref ref-type="bibr" rid="scirp.29518-ref32">32</xref>]. A priori contrasts were used when interactions were considered significant. The contrasts were aimed to see if stand types differed over time and between microsites. ANOVAR was performed with the MIXED procedure in the SAS software (SAS Institute Inc., Cary, NC, USA).</p><p>An ANOVA was used for physiological variables and was executed with the REML procedure in the JMP 7.0 software (SAS Institute Inc., Cary, NC, USA). Normality and homoscedasticity of variance were verified for all data by examining visual distribution of the data and by analysis of residues [<xref ref-type="bibr" rid="scirp.29518-ref33">33</xref>]. The natural logarithmic (ln(x + 1)) was applied when necessary, and untransformed data were presented. A significance level of 0.05 was used for statistical analyses.</p><p>Multivariate analyses were used to find vegetation differences between stand types and their variation in time. A Bray-Curtis similarity matrix was produced through a fourth-root data transformation [<xref ref-type="bibr" rid="scirp.29518-ref34">34</xref>]. This transformation down-weighted the importance of very abundant species and took rare species into account [<xref ref-type="bibr" rid="scirp.29518-ref29">29</xref>]. Species assemblages by non-metric multidimensional scaling (nMDS) were formed from the dissimilarity matrix. Dissimilarity is a function of distance between groups; the most different groups having a higher distance between each other. MDS representation precision was quantified by Kruskal stress values [<xref ref-type="bibr" rid="scirp.29518-ref31">31</xref>]; a low value indicating a more precise bi-dimensional representation, and a value higher than 0.3 representing a random representation [<xref ref-type="bibr" rid="scirp.29518-ref29">29</xref>]. All MDS matrices were produced with the PRIMER software 5.2.2 (PRIMER-E Ltd., Lutton, UK). No significance threshold was set for the dissimilarity matrices.</p></sec></sec><sec id="s3"><title>3. Results</title><sec id="s3_1"><title>3.1. Mean Vegetation Cover: Bio-Indicators</title><p>For black spruce (BS), we found a significant interaction between site type and time (<xref ref-type="table" rid="table1">Table 1</xref>). BS cover was significantly higher in the FM compared to LW before silvicultural treatment and decreased afterwards to a level similar to LW (<xref ref-type="fig" rid="fig1">Figure 1</xref>(a)). For Rhododendron (RG) mean cover, the interaction between site type and microsite was significant (<xref ref-type="table" rid="table1">Table 1</xref>). RG cover in S0<sub>LS</sub> was higher in the open lichen woodlands (LW) (<xref ref-type="fig" rid="fig1">Figure 1</xref>(c)). For Kalmia (KA) and RG, cover in the S0<sub>LS</sub> was around 0.3% on day 110 and rose to 1% on day 501. After that, KA cover was similar in all microsites and RG cover was still the highest for S0<sub>LS</sub> (Figures 1(b) and (d)).</p></sec><sec id="s3_2"><title>3.2. Species Assembly</title><p>Non-metric multidimensional scaling (nMDS) exhibited two distinct data groups. The first group was composed of LW data points and was located in the upper part of the frame, and the second was located in the lower part of the frame, and mainly consisted of FM data points (<xref ref-type="fig" rid="fig2">Figure 2</xref>(a)). Stand type response varied over time: a high variation was observed in the LWs between day 0 and 110. This variation decreased between day 501 and 801, data points converging back to day 0 values (Figure</p><p><xref ref-type="table" rid="table1">Table 1</xref>. Summary of ANOVA results for species mean cover (%) of regenerating black spruce layers and ericaceous shrubs submitted to various silvicultural treatments in lichen-spruce woodlands and black spruce-feathermoss stands. BS = Black spruce, KA = Kalmia angustifolia, RG = Rhododendron groenlandicum, LW = lichen-spruce woodland, FM = black spruce-feathermoss stand, NP = non perturbed, S0<sub>LS</sub> = logging strips in the non-scarified plots, S0<sub>ST</sub> = skid trails in the non-scarified plots, S1<sub>NS</sub> = non-disturbed strips in the scarified plots, S1<sub>SF</sub> = scarification furrows.</p><p><img src="11-2600665\6d7e4932-8c34-49a9-9097-1bf730961b9f.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom. <sup>*</sup>Ln-transformed data.</p><p>2(b)). This trend was less apparent for FM stands, where distances between day 110, 501, and 801 were more homogenous (<xref ref-type="fig" rid="fig2">Figure 2</xref>(c)).</p></sec><sec id="s3_3"><title>3.3. Biodiversity Indexes</title><p>The ANOVA revealed a significant triple interaction between site type, microsite, and time for total mean cover (N) (<xref ref-type="table" rid="table2">Table 2</xref>). Contrasts showed a difference in N between LWs and FMs on day 801 for S0<sub>LS</sub>, S0<sub>ST</sub>, and S1<sub>SF</sub> (<xref ref-type="table" rid="table2">Table 2</xref>, <xref ref-type="fig" rid="fig3">Figure 3</xref>(a)). For species richness (S) and Pielou’s evenness (J’), we found a significant interaction between site type and time (<xref ref-type="table" rid="table2">Table 2</xref>). Species richness (S) was higher in FM stands and the initial gap between stand types decreased after silvicultural treatments (<xref ref-type="fig" rid="fig3">Figure 3</xref>(b)). Otherwise, S increase in LWs between day 0 and 110 was around 132%, but an inverse trend was noted between day 501 and 801 (<xref ref-type="fig" rid="fig3">Figure 3</xref>(b)). The S0<sub>ST</sub> microsite had the lowest species richness, regardless of stand type and for all three sampling dates after silvicultural treatments (<xref ref-type="fig" rid="fig3">Figure 3</xref>(c)). For J’, stand type &#215; microsite interaction showed an advantage in favour of FM stands in S0<sub>ST</sub> and S1<sub>SF</sub> (<xref ref-type="table" rid="table2">Table 2</xref>, <xref ref-type="fig" rid="fig3">Figure 3</xref>(d)). Throughout the study, J’ variation showed similar trends between stand types (<xref ref-type="fig" rid="fig3">Figure 3</xref>(e)).</p></sec><sec id="s3_4"><title>3.4. Physiological Variables</title><p>For BS, foliar N and P foliar concentrations were significantly higher in the S0 and S1 treatments and the differences were constant throughout days 110, 501, and 801 (<xref ref-type="table" rid="table3">Table 3</xref>, <xref ref-type="fig" rid="fig4">Figure 4</xref>(a) and (b)). Foliar P and Mg concentrations were significantly higher in FM stands compared to LWs (P: LW = 1.15 g&#183;kg<sup>−1</sup> &#177; 0.40, FM =</p><p>1.29 g&#183;kg<sup>−1</sup> &#177; 0.46; Mg:LW = 0.85 g&#183;kg<sup>−1</sup> &#177; 0.11, FM = 0.93 g&#183;kg<sup>−1</sup> &#177; 0.19). However, silvicultural treatment application decreased the difference between stand types for K (<xref ref-type="table" rid="table3">Table 3</xref>, <xref ref-type="fig" rid="fig4">Figure 4</xref>(c)).</p><p>Kalmia foliar N concentrations were ≈10% higher in FM stands, regardless of the silvicultural treatment (<xref ref-type="table" rid="table4">Table 4</xref>, <xref ref-type="fig" rid="fig5">Figure 5</xref>(a)). Foliar P concentrations increased over the years, with slightly higher concentrations in the scarified plots after 801 days (<xref ref-type="fig" rid="fig5">Figure 5</xref>(b)); the same trend was also found for KA foliar K in the FM stands (<xref ref-type="fig" rid="fig5">Figure 5</xref>(c)). On the other hand, we noticed a slight decrease in foliar Ca concentrations over time (<xref ref-type="fig" rid="fig5">Figure 5</xref>(d)). Finally, Mg foliar concentrations increased over time, but only in NP (<xref ref-type="fig" rid="fig5">Figure 5</xref>(e)). Similar results were found for RG (<xref ref-type="table" rid="table5">Table 5</xref>, results not shown).</p><p>For BS in LWs, photosynthetic rates had increased by day 501, but no difference was found at the end of the experiment (<xref ref-type="table" rid="table6">Table 6</xref>, <xref ref-type="fig" rid="fig6">Figure 6</xref>(a)). In the FM stands, the increase on day 501 in the S1 treatment was still noticed for BS (<xref ref-type="table" rid="table6">Table 6</xref>, <xref ref-type="fig" rid="fig6">Figure 6</xref>(a)). For KA, photosynthetic rates in all treatments had increased significantly by day 501, and decreased slightly at the end of the experiment in the LWs (<xref ref-type="fig" rid="fig6">Figure 6</xref>(b)). The same trend was measured in FM stands, but KA photosynthetic rates in the S0 microsite increased from day 501 (<xref ref-type="fig" rid="fig6">Figure 6</xref>(b)). Leaf mass per unit area for KA differed only in the S1 treatment, with a higher value in the LWs (<xref ref-type="fig" rid="fig6">Figure 6</xref>(c)). Lastly, we found a significant positive relation between photosynthesis and LMA for KA (R<sup>2</sup>adj. = 0.46, P &lt; 0.001).</p></sec></sec><sec id="s4"><title>4. Discussion</title><sec id="s4_1"><title>4.1. Plant Community Response to Silvicultural Treatments</title><p>The decline in black spruce cover in the black sprucefeathermoss (FM) stands coupled with a slight increase in black spruce cover in the lichen-spruce woodlands (LW) indicates that silvicultural treatments induced a more adverse short-term effect in the FM stands. On the other hand, the degree of cover change for Kalmia, with</p><p><xref ref-type="table" rid="table2">Table 2</xref>. Summary of ANOVA results for total mean cover (N), species richness (S), Pielou’s index (J’), and Shannon-Wiener index (H’). Refer to <xref ref-type="table" rid="table1">Table 1</xref> for abbreviations.</p><p><img src="11-2600665\a7bac410-06d0-49de-a62b-279b0037d657.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom.</p><p><xref ref-type="table" rid="table3">Table 3</xref>. Summary of ANOVA results for black spruce foliar nutrient concentrations. LW = lichen spruce woodlands, FM = black spruce-feathermoss stand, NP = non perturbed, S0 = harvested, S1 = harvested + scarified.</p><p><img src="11-2600665\feaafeac-cee5-4a92-a19d-eadefe564c64.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom. <sup>*</sup>Ln-transformed data.</p><p><xref ref-type="table" rid="table4">Table 4</xref>. Summary of ANOVA results for Kalmia angustifolia foliar nutrient concentrations. Refer to <xref ref-type="table" rid="table3">Table 3</xref> for abbreviations.</p><p><img src="11-2600665\a9249a31-c0a3-436f-af22-42b9b0b6bcca.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom. <sup>*</sup>Ln-transformed data.</p><p><xref ref-type="table" rid="table5">Table 5</xref>. Summary of ANOVA results for Rhododendron groenlandicum foliar nutrient concentrations. Refer to <xref ref-type="table" rid="table3">Table 3</xref> for abbreviations.</p><p><img src="11-2600665\43ca29df-b793-4008-b35e-7f1fc4893612.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom. *Ln-transformed data.</p><p>respect to the silvicultural treatment applied, was similar between stand types. Two years following treatments, the highest decrease had happened in the most intensely disturbed microsites, especially in the scarified ones. Scarification is well known to reduce Kalmia cover in black spruce plantations by producing barriers against rhizome extension: Kalmia underground organs are located at the interface of the organic horizon and mineral layer instead of in the mineral soil [<xref ref-type="bibr" rid="scirp.29518-ref35">35</xref>]. However, absolute cover values between site types and microsites were similar, with relatively low mean cover measured overall.</p><p>Haeussler et al. [<xref ref-type="bibr" rid="scirp.29518-ref36">36</xref>] stated that there are three ways to reduce biological diversity through forest management: 1) by the displacement of indigenous species in favour of non-native species, 2) by diminishing forest overstory and understory diversity at the stand scale, and 3) by inducing changes in species composition that lead to a decreased spatial heterogeneity. Our results clearly showed that silvicultural treatments did not reduce plant diversity in either stand type based on those criteria. We admit that MDS analyses revealed variations in plant diversity for both stand types. However, the return to the initial composition was noticed only two years after treatments, especially in the LWs, thus indicating a higher level ecosystem resilience in LW.</p><p>Besides the plant bio-indicators selected, our results outlined a difference between responses of the plant community in LW and FM stands to logging and site preparations. Total mean cover of all species decreased drastically after logging in the skid trails, especially in the FM stands. Also, mean cover in LWs was higher at the end of the experiment. Skid trails are the microsites most affected by silviculture in terms of vegetation composition [37,38]. The higher decrease in total plant cover in the FM skid trails is due to a lack of acclimation by bryophyte species, which are more abundant in FM stands, an abrupt increase in light availability due to logging, and higher water stress [39-41]. Conversely, ericaceous shrubs and lichens found in the LWs are already acclimated to open stand conditions, which gave LWs a restructuring advantage over FM plant communities after silvicultural treatments. An increase in specific richness</p><p><xref ref-type="table" rid="table6">Table 6</xref>. Summary of ANOVA results for black spruce (BS) and Kalmia angustifolia (KA) photosynthesis (A) and leaf mass per unit of area (LMA). Refer to <xref ref-type="table" rid="table3">Table 3</xref> for abbreviations.</p><p><img src="11-2600665\218b9ffe-1e23-4503-bafa-a2c4b473abc7.jpg" /></p><p>Note: Bold indicates significance (P &lt; 0.05). ndf = numerator degrees of freedom. <sup>*</sup>Ln-transformed data.</p><p>after logging in the LWs, followed by a short-term return to the initial richness after treatments, was also found by Robert &amp; Zhu [<xref ref-type="bibr" rid="scirp.29518-ref24">24</xref>] in mixedwood stands. MDS analysis suggests a faster return of the initial species composition in the LWs, despite the higher early variation in species composition, compared to the FM stands. The general decrease of mean cover after two years in both stand types can also be explained by allelopathy and other negative interferences caused by the presence of ericaceous shrubs, which could inhibit the establishment of plant species and decrease site productivity [25,42,43].</p><p>Contrary to Mallik [<xref ref-type="bibr" rid="scirp.29518-ref44">44</xref>], Kalmia cover was not related to community species diversity, as expressed by the Shannon-Wiener index (H’) that was similar between stand types and silvicultural treatments. However, this index may not be adequate to evaluate the response to disturbance [<xref ref-type="bibr" rid="scirp.29518-ref24">24</xref>], because plant species reorganization at ecosystem level is more related to functional groups, rather than individual species that exert a direct control on the species composition [41,43]. Therefore, silvicultural treatments did not affect the stand plant cover composition, and H’ was not related to site productivity. Finally, Pielou’s index revealed a higher variation among microsites in the FM, further supporting that FM vegetation is more affected by silvicultural treatments.</p><p>Even if slight differences in plant community response to silvicultural treatments were found between stand types, we argue that FM and LW short-term resilience is similar, indicating equally efficient ecosystem reorganization in both types of stand. In direct response to one of the initial questions of this study, the FM and LW vegetation communities did not change after silvicultural treatments. Therefore, the LW ecosystem resilience observed is not showing a lack of tolerance to anthropogenic disturbances, at least on the short-term basis.</p></sec><sec id="s4_2"><title>4.2. Plant Physiological Response to Silvicultural Treatments</title><p>The lower pre-disturbance values for bio-indicators traits in LWs were expected. The lower foliar nutrient concentrations in the LWs, especially for black spruce nitrogen, can be related to the higher density of ericaceous shrubs, which negatively influence nutrient absorption [44-46]. H&#233;bert et al. [<xref ref-type="bibr" rid="scirp.29518-ref25">25</xref>] also showed that the presence of ericaceous shrubs not only decreased N available in the mineral soil, but also negatively affected black spruce advanced regeneration physiology ten years after logging. Conversely, the higher foliar nitrogen concentration in both ericaceous shrub species in the FM stands can result from a higher N pool in the FM organic and mineral horizon, Kalmia and Rhododendron being able to assimilate organic forms of nitrogen [47,48]. Furthermore, the short-term acclimation of Kalmia leaves in the FM skid trails, revealed by higher LMA and photosynthesis values, can explain the higher foliar N found in FM stands. By comparison, the absence of difference for LMA and photosynthesis after disturbance indicates that leaves in LWs were already acclimated to high light availability.</p><p>A plant response showing a partial reversion in stand productivity in LWs was also perceptible from the early (one year after treatment) leaf-level photosynthesis response to treatments for both black spruce regeneration and Kalmia shrubs. However, this response was mitigated after two years for black spruce, suggesting a possible trade-off mechanism where the increased site productivity also led to higher plant competition, especially where ericaceous species dominate [<xref ref-type="bibr" rid="scirp.29518-ref49">49</xref>]. Both leaf-level photosynthesis and LMA responses to treatments were more sustained in Kalmia two years after treatments than in black spruce, as observed in Rhododendron dominated stands [<xref ref-type="bibr" rid="scirp.29518-ref26">26</xref>].</p></sec><sec id="s4_3"><title>4.3. Management Implications</title><p>LWs have traditionally been considered as fragile ecosystems that could not support sustained tree growth [50-53]. The evidence for this was partly based on LWs located in the unproductive Taiga zone [<xref ref-type="bibr" rid="scirp.29518-ref27">27</xref>] where LWs are commonly found, and which result from a limited postfire tree regeneration caused by an unfavourable climate [<xref ref-type="bibr" rid="scirp.29518-ref4">4</xref>]. The LWs of our study are located in the productive closed-crown forest zone, where scattered LWs are adjacent to prevailing FM stands sharing similar site conditions (soil deposits, drainage, etc.) [6,10]. However, H&#233;bert et al. [<xref ref-type="bibr" rid="scirp.29518-ref21">21</xref>] showed the importance of site preparation for improving seedling growth and water relations in LWs. Leaf traits of bio-indicators and plant community responses suggest a potential for silvicultural treatments to increase site productivity in LWs, but additional work is needed to scale these results up to site-level metrics of productivity.</p><p>The comparable early resilience in managed LWs and FM stands, in terms of plant biodiversity, contradicts the presumed fragility of LW stands, especially in this case where LWs are assumed to be an alternative stable state created by compound disturbances [6,10]. Silvicultural treatments maintained the functional group diversity in LWs, a key element for ecosystem resilience [<xref ref-type="bibr" rid="scirp.29518-ref54">54</xref>]. Since fragility cannot be quantified [<xref ref-type="bibr" rid="scirp.29518-ref55">55</xref>], this term should be avoided in managed LWs, unless the protection of wild animals is the ultimate goal (e.g. the woodland caribou, Rangifer tarandus caribou, [52,56]).</p><p>Considering that LWs in the closed-crown boreal forest are an alternative stable state, forest management that could favour an increase in both natural and artificial black spruce regeneration needs to be scrutinized. On a landscape basis, Girard et al. [<xref ref-type="bibr" rid="scirp.29518-ref10">10</xref>] noticed a recent increase in the creation rate of LWs within Qu&#233;bec’s closed crown boreal forest. Those LWs were created by a succession of disturbance events, like wildfires, spruce budworm epidemics, but also by logging, resulting in a decreased resilience of the spruce-feathermoss bioclimatic domain, since no evidence of a natural shift of LWs back to FM stands has been found [6,14]. The results of this study support the idea that plantation following site preparations in LWs could be considered a valuable management strategy, at least based on the early site resilience response to silvicultural treatments. Moreover, adequate silvicultural strategies may maintain the resilience of desired states and transform the undesirable states [<xref ref-type="bibr" rid="scirp.29518-ref57">57</xref>]. The afforestation of boreal open woodlands such as LWs is also interesting when considering the greenhouse gas mitigation potential it represents in both North America and Russia [18-20], in spite of possible limitations that also need to be addressed [53,58] in addition to the need for long-term evaluation of the site resilience to disturbance and plantation productivity.</p></sec></sec><sec id="s5"><title>5. Acknowledgements</title><p>This research was funded by a Fonds de Recherche pour la Nature et des Technologies du Gouvernement du Qu&#233;bec (FQRNT) grant to D. Lord, and the Carbone bor&#233;al project. We thank Virginie Blais, Solveil Bourque, Pierre-Luc Gaudreault, Silvie Paquette, Marc Tremblay and Pascal Tremblay for their field assistance.</p></sec><sec id="s6"><title>REFERENCES</title></sec><sec id="s7"><title>NOTES</title></sec></body><back><ref-list><title>References</title><ref id="scirp.29518-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">E. H. Hamilton and S. Haeussler, “Modeling Stability and Resilience after Slashburning across a Sub-Boreal to Subalpine Forest Gradient in British Columbia,” Canadian Journal of Forest Research, Vol. 38, No. 2, 2008, pp. 304-316. doi:10.1139/X07-098</mixed-citation></ref><ref id="scirp.29518-ref2"><label>2</label><mixed-citation publication-type="other" xlink:type="simple">M. D. Morecroft, H. Q. P. Crick, S. J. Duffield and N. A. 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