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. 2011 Jul 1;1(2):151–159. doi: 10.1534/g3.111.000372

Genetic Variation in the Chemical Components of Eucalyptus globulus Wood

Desmond J Stackpole *,, René E Vaillancourt *, Ana Alves , José Rodrigues , Brad M Potts *,1
Editor: Brenda J Andrews
PMCID: PMC3276126  PMID: 22384327

Abstract

Despite the ecological and economic importance of lignin and other wood chemical components, there are few studies of the natural genetic variation that exists within plant species and its adaptive significance. We used models developed from near infra-red spectroscopy to study natural genetic variation in lignin content and monomer composition (syringyl-to-guaiacyl ratio [S/G]) as well as cellulose and extractives content, using a 16-year-old field trial of an Australian tree species, Eucalyptus globulus. We sampled 2163 progenies of 467 native trees from throughout the native geographic range of the species. The narrow-sense heritability of wood chemical traits (0.25–0.44) was higher than that of growth (0.15), but less than wood density (0.51). All wood chemical traits exhibited significant broad-scale genetic differentiation (QST = 0.34–0.43) across the species range. This differentiation exceeded that detected with putatively neutral microsatellite markers (FST = 0.09), arguing that diversifying selection has shaped population differentiation in wood chemistry. There were significant genetic correlations among these wood chemical traits at the population and additive genetic levels. However, population differentiation in the S/G ratio of lignin in particular was positively correlated with latitude (R2 = 76%), which may be driven by either adaptation to climate or associated biotic factors.

Keywords: tree improvement, wood chemicals, adaptation, lignin, cellulose, extractives, syringyl, guaiacyl


Forests occupy 30% of the world’s terrestrial surface (FAO 2007) and are key terrestrial carbon stores, much of which is from wood (Sedjo 1993). Wood derived from natural and planted forests is also the basis of renewable energy and industrial production systems for products such as timber and pulp, worth more than $327 billion US in annual trade (FAO 2007). Wood is the fibrous material in the trunk of trees under the bark, which is composed of a complex mix of plant polymers. The most important quantitatively is cellulose, followed by lignin, hemicelluloses, and then extractives (Walker 2006). Cellulose fibers are deposited on cell walls along with lignin during the process of wood formation as cells expand following differentiation at the cambium (Walker 2006). Cellulose gives strength to the cell walls (Turner and Somerville 1997). Lignin supports the cellulose fibers, provides the hydrophobic surfaces in vessels essential for water conduction (Plomion et al. 2001), and also has roles in defense against wood eaters and pathogens (Coleman et al. 2008; Salmore and Hunter 2001).

The evolution of lignin biosynthesis has been fundamental to the adaptation to the terrestrial environment (Weng and Chapple 2010), and the proportion of lignin in wood varies markedly between species (15%–36%) (Zobel and Van Buijtenen 1989). Lignin is constructed of three monolignol monomers, hydroxyphenyl (H), guaiacyl (G), and syringyl (S), with the proportion and location of the different monomers varying between and within species (Anterola and Lewis 2002). These monomers are synthesized in the cytoplasm, but lignin is formed when they are polymerized at the site of deposition (Lewis and Yamamoto 1990). The presence of methoxyl groups attached to the benzene ring of the lignin monomer increases the reactivity of the lignin to natural or artificial delignification agents (Pinto et al. 2002). As S has two methoxyl groups attached to the benzene ring, it has higher reactivity than G, which has only one methoxyl group. H is the least reactive having no methoxyl groups. Gymnosperm lignin is almost entirely composed of G with only a minor proportion of H and S (Alves et al. 2006; Campbell and Sederoff 1996; Godoy et al. 2007; Walker 2006), while woody angiosperms have H in trace amounts (Rencoret et al. 2008). In woody angiosperms, the ratio of S to G monomers (S/G) varies between species, provenance, and also between cell type within a tree (Pinto et al. 2002; Rodrigues et al. 1999; Rodrigues et al. 2001). Wood also contains extractives, a diverse group of nonstructural compounds that are mainly involved in chemical and physical defenses of living and dead wood (Boddy 2001). Extractives are present in sapwood, but preferentially deposited in the heartwood (Taylor et al. 2002). Resin acids predominate in the extractives of conifer heartwood, whereas a wide range of compounds occur in angiosperms, although in any one species the range is reduced (Gutierrez et al. 1999).

Planted forests comprise an increasing proportion of the world’s forests and now provide nearly half of the global wood production (FAO 2007). Short-rotation tree crops such as eucalypt plantations, are the feed stocks not only of the pulp and paper industry (Clarke 2009; Cotterill and Brolin 1997; Paues 1999), but are also seen as the basis of new industries replacing the use of fossil hydrocarbons for energy and industrial organic chemicals (Bozell 2010). In the case of pulp production, the strongest and highest quality pulp is produced by chemical delignification using powerful bases (the kraft process) leaving the cellulose fibers relatively undamaged for reconstitution as paper (Clarke 2009). Angiosperm wood with high S/G tends to be easier to delignify as per unit weight of dry wood it consumes less chemical and energy and produces higher pulp yield (Rencoret et al. 2007). Extractives may interfere with the efficiency of delignifying chemicals (Wallis et al. 1996) and also have adverse effects on the pulping process as they accumulate in industrial conduits which are costly to clean (Hillis and Sumimoto 1989).

Breeding objectives for biomass crops intended for delignification could conceivably include reduced total lignin content or increased S/G (Bose et al. 2009). Conversely, other processes or products might require higher lignin content or lower S/G (Clarke 2009). Similarly, adaptation of the tree to abiotic or biotic environmental stresses may be impacted by changes in lignin content or composition, and processing objectives may or may not be aligned with requirements for plantations to be adapted to current or future environments. The extent to which breeders can directly or indirectly change wood chemical composition through selection will depend upon its quantitative genetic architecture, including the levels of additive genetic variation in the population, its heritability, and correlations between chemical components and other traits (Falconer and Mackay 1996). However, despite the economic and ecological importance of lignin and other wood chemicals, as well as decades of biotechnological research on specific genotypes (Coleman et al. 2008; Weng and Chapple 2010), the basic quantitative genetic architecture of these traits across the gene pool of any woody angiosperm species is poorly known. This has been mainly due to the high cost of measuring lignin, which has prevented the acquisition of the large sample sizes required to obtain robust and accurate genetic parameter estimates (Falconer and Mackay 1996). Quantification of wood chemical constituents is notoriously difficult, and the different methods used all have limitations (Anterola and Lewis 2002; Hatfield and Fukushima 2005). However, rapid and inexpensive near-infrared (NIR) reflectance chemometric methods have been developed that allow the prediction of chemical composition from NIR spectra (Schimleck et al. 2000; Workman 1992). NIR has been applied to large-scale studies of conifer species to estimate genetic parameters for lignin content and quality (Da Silva Perez et al. 2007), but has not been applied in large-scale studies of the genetic architecture of woody angiosperms.

In this study, a large base population trial of open-pollinated Eucalyptus globulus was used to study the quantitative genetic architecture of wood chemical components (lignin, S/G, extractives, and cellulose) and their genetic correlation with traits under artificial selection (growth, wood density, and pulp yield; Stackpole et al. 2010b). Having studied the geographic variation in the wood chemicals across the geographic range of the species, we provide evidence that there is a signature of natural selection acting on these traits and discuss the potential drivers of genetic divergence.

Materials and Methods

Study system

Eucalyptus globulus Labill. (tasmanian blue gum sensu Brooker (2000), otherwise known as E. globulus ssp. globulus, Kirkpatrick,) is the main hardwood species grown in temperate Mediterranean climates across the globe (Potts et al. 2004). In its native range in south eastern Australia (Figure 1), it is often a dominant of coastal forests that typically grows 15 to 60 m tall (Williams and Potts 1996). The species is genetically diverse with geographic races showing broad-scale differences in numerous quantitative traits (Dutkowski and Potts 1999), many of which are presumably adaptive (e.g., frost tolerance; Tibbits et al. 2006; drought tolerance, Dutkowski 1995; Toro et al. 1998). Microsatellite analysis shows that contiguous races are more similar to one another than distant ones (Steane et al. 2006). E. globulus has a mixed mating system, and its open-pollinated seed contains between 65%–89% outcrossed progenies in different populations (Mimura et al. 2009). In addition, biparental inbreeding affects between 4% and 11% of the progenies (Mimura et al. 2009). All Eucalyptus species, including E. globulus, are believed to have the same chromosome number (2n = 22) (Oudjehih and Bentouati 2006).

Figure 1 .

Figure 1 

Geographic distribution of subrace means for syringyl/guaiacyl ratio (S/G), Klason lignin, extractives and cellulose content in Eucalyptus globulus grown in a common environment field trial. The larger the circle or triangle, the more the subrace mean deviates above or below the mid range value. Subrace codes are as follows: TP - Tasman Peninsula; SET - South-eastern Tasmania; INET - Inland North-eastern Tasmania; ST - Southern Tasmania; SF - Southern Furneaux; StH - St Helens; FI - Flinders Island; KI - King Island; GF - Gippsland Foothills; NET - North-eastern Tasmania; StF - Strzelecki Foothills; WOt -Western Otways; CP - Cape Patton; EOt - Eastern Otways; FWOt - Far West Otways; StrR - Strzelecki Ranges; GCP - Gippsland Coastal Plain.

The study was based on a Gunns Ltd family trial of E. globulus planted in 1989 at Latrobe in northern Tasmania (41° 16’ S, 146° 27’ E). The 570 families used in the trial were from single-tree, open-pollinated seed lots collected from a range-wide base population sampling of E. globulus. These families have been assigned to a geographic hierarchy of races, subraces and localities by Dutkowski and Potts (1999). This study focused on variation at the subrace and family levels, consistent with previous studies of this trial (Stackpole et al. 2010a,b). The trial design was a resolvable incomplete block design (Patterson and Williams 1976). The trial had five replicates, each divided into 24 incomplete blocks, each of which contained 24 families planted in two-tree plots. The trees that were alive in the trial at age 16 years were measured for diameter at breast height over bark at 1.3 m above ground level (DBH). Of these, a sample of 2163 trees was selected for wood property sampling, omitting four minor subraces (Wilson’s Promontory Lighthouse, Mount Dromedary, Recherche Bay and Western Tasmania) (see Dutkowski and Potts 1999). Four or five individual trees were sampled from each of the 467 families that had four or more suitable candidate trees (alive and more than 10.0 cm in DBH) in the trial. In 452 families, one tree per replicate was sampled while in 12 families only two to three replicates were sampled. The number of families per subrace averaged 27, and ranged from 3 to 107 (see supporting information). Further sampling details are given in Stackpole et al. (2010a,b).

Measurement of wood properties

Cambium to cambium wood cores were removed at 1.1 m above ground level. Each core was cut in half longitudinally and one half used to measure wood density (see Stackpole et al. 2010a) and the other half air-dried for predicting wood chemical composition (see Stackpole et al. 2010b). We used NIR spectroscopy to estimate wood chemical components as this is the only practical method for measuring the large number of samples required for detailed quantitative genetic analyses. NIR is widely used in assaying wood chemical composition in trees (Tsuchikawa 2007), including eucalypts (Schimleck et al. 2000; Raymond and Schimleck 2002). The air-dried wood was ground to pass through a 1-mm screen, and NIR spectra collected using a Bruker Optics Co. MPA (see supporting information). NIR models detailed in the supporting information were used to obtain predictions of S/G (coefficient of determination, R2 = 58.3), Klason lignin (R2 = 66.3), and extractives (R2 = 78.2%) for the 2163 trees. Validation of predictions was undertaken using chemical assays from 45 samples independent from those used to develop the model (S/G R2 = 47.0%, Klason lignin R2 = 60.0%, and extractives R2 = 83.3%). Because of the low phenotypic R2 for S/G, the genetic correlations were calculated between the NIR predictions and the 180 samples measured directly using pyrolysis, and a very high correlation was found (ra = 0.99). This means that with the averaging which occurs across families, there is a marked increase in the reliability of the NIR predictions at the genetic level over that at the individual phenotypic level (see supporting information for a more detailed explanation). Cellulose content (validation R2 = 85.0%) and pulp yield (validation R2 = 82.0%) for the same trees was obtained in a similar manner (see Stackpole et al. 2010b). Depending upon trait, the number of individuals for which wood property data were available ranged from 2140 to 2163 due to missing values (Table 1).

Table 1 . Genetic parameters for wood chemical traits in Eucalyptus globulus.

Trait n Mean Fsubrace Va (SE)a CVs CVa h2op (SE) QST (SE) P (QST >FST) Regression of Trait on Latitude
β Significance R2 (%)
S/G 2149 1.97 15.8*** 0.002 (0.0003) 4.05 2.55 0.44 (0.056) 0.34 (0.091) *** 0.040 *** 76
Klason lignin 2158 20.5 25.2*** 0.094 (0.019) 2.54 1.50 0.27 (0.052) 0.37 (0.101) *** −0.117 NS 16
Celluloseb 2154 43.4 32.4*** 0.325 (0.048) 2.12 1.31 0.42 (0.056) 0.34 (0.092) *** 0.290 * 30
Extractives 2140 4.76 28.9*** 0.113 (0.026) 13.7 7.08 0.25 (0.052) 0.44 (0.108) *** −0.199 * 28
Diameterb 3383 17.3 2.4** 1.535 (0.318) 3.35 7.16 0.15 (0.031) 0.04 (0.026) NS 0.057 NS 2
Densityb 2145 539 16.4*** 220.2 (28.2) 3.03 2.75 0.51 (0.058) 0.20 (0.066) ** −6.560 ** 49
Pulp yieldb 2163 53.2 35.5*** 0.399 (0.061) 2.05 1.19 0.39 (0.055) 0.37 (0.096) *** 0.400 ** 41

Included are the number of samples (n); grand mean for each trait; Fsubrace value and significance for the difference between subraces; additive genetic variation component (Va) and its standard error (SE); coefficients of variation at the subrace (CVs) and additive genetic (CVa) level; narrow-sense heritability (h2op); quantitative divergence between subraces (QST) and probability (P) that QST > FST of Steane et al. (2006); and the slope (β), significance, and coefficient of determination (R2) for the regression of subrace means on subrace latitude.

a

All variance components (Va) are significant at P < 0.001.

b

These traits are from Stackpole et al. (2010a)

Statistical analyses

Following the approach described in Stackpole et al. (2010b), a mixed model was fitted to the data from all the races used in the study. Replicate was fitted as a fixed effect, incomplete block and family within-subrace terms fitted as random effects, and subrace fitted as a fixed effect except in the bivariate analyses used to estimate subrace and family correlations. Univariate and bivariate models were fitted with ASReml (Gilmour et al. 2001). The effect of the wood chemical traits on survival were tested through calculation of the genetic correlation between the wood chemical and the whole trial survival data (0 = dead, 1 = alive) at age 16 years following the approach of Chambers et al. (1996). In addition to the analyses and tests described in Stackpole et al. (2010a,b), quantitative genetic divergence between subraces was also assessed using QST; which was calculated following Latta (1998) and Yang et al. (1996) as:

QST=σsubrace2/(σsubrace2+2σadd(subrace)2)

where σ2subrace is the restricted maximum likelihood estimate of the between subrace variance component, and σ2add(subrace) is the estimate of the pooled within-subrace additive genetic variance. σ2add(subrace) was calculated from the family within subrace variance component, σ2family(subrace) (Stackpole et al. 2010b) using a coefficient of relatedness (r) of 0.4 for the open-pollinated families. Narrow-sense heritabilities (h2op), the coefficient of additive genetic variance (CVa), the coefficient of subrace genetic variance (CVs), subrace genetic correlations, and additive within subrace genetic correlations were calculated as detailed in Stackpole et al. (2010b). It should be noted that we expect that the genetic parameters for the chemical traits are likely to be underestimated as the error of NIR prediction is essentially included in the error variance and this would decrease heritability.

The standard errors of QST and h2op were calculated with ASReml using an expanded Taylor series (Gilmour et al. 2001). For each trait a one-tailed likelihood ratio test was used to test whether QST was greater than the FST derived from putatively neutral microsatellite markers. QST is the quantitative genetic equivalent to the molecular measure of population divergence FST. If FST is measured using selectively neutral markers, then FST is the measure of the genetic differentiation among populations due to random drift or mutation (Latta 1998). If QST is significantly higher than FST, then this is evidence for diversifying natural selection acting on the quantitative trait (Latta 1998; Steane et al. 2006). The FST estimates used for this comparison were based on the average racial divergence in eight microsatellite loci as published by Steane et al. (2006) (FST = 0.09). We also tested against the highest FST reported for a single microsatellite locus in this species (FST = 0.158; Astorga et al. 2004) and obtained identical results but at the 0.05 level of significance.

Correlations were derived from bivariate analyses as the multivariate models with more than two traits did not converge. The difference of the subrace and additive genetic correlations from zero was tested using two-tailed log likelihood tests. The subrace means of each trait were regressed against their latitude of origin. Locality means of extractives and Klason lignin content were also regressed against wood decay reported in Poke et al. (2006) and Hamilton et al. (2007) which were in common with the present study.

Results

Genetic variation within subraces

Highly significant (P < 0.001) levels of additive genetic variation were evident within subraces for all traits assessed (LRT of σ2family(subrace); Table 1). Diameter had the lowest h2op (0.15 ± 0.03) and density the highest (0.51 ± 0.06), with the wood chemical traits all intermediate. The h2op of the four wood chemical traits (S/G, Klason lignin, extractives and cellulose) ranged from 0.25 to 0.44, and averaged 0.34. S/G had the highest estimate (0.44 ± 0.06) among these wood chemical traits. Despite their relatively high heritabilities, the coefficient of additive genetic variation within subraces (CVa) for the chemical and physical wood property traits were low when compared with diameter, except for extractives (Table 1). While the h2op of pulp yield was intermediate, it had the lowest CVa of all traits assessed.

Within subraces, there were strong additive genetic correlations among the wood chemical traits. Genetic variation in Klason lignin was negatively correlated with cellulose (ra = −0.90 ± 0.04) (Table 2), weakly negatively correlated with S/G (ra = −0.31 ± 0.11), and positively correlated with extractives (ra = 0.62 ± 0.10). The S/G was negatively genetically correlated with extractives (ra = −0.59 ± 0.10). The additive genetic correlations of chemical traits with growth were statistically significant (P < 0.05) but were generally low. Faster growing trees (larger diameter) had less lignin (ra = −0.38 ± 0.15), higher S/G (ra = 0.33 ± 0.124), and higher cellulose (ra = 0.45 ± 0.12) than slower growing trees. No significant correlation between survival and wood chemical traits was detected at either the additive genetic or subrace levels (data not shown). Additive genetic variation in density was weakly negatively correlated with that of Klason lignin (ra = −0.23 ± 0.11) and S/G (ra = −0.28 ± 0.09). Pulp yield was strongly positively correlated with cellulose (ra = 0.91 ± 0.02) and strongly negatively correlated with Klason lignin (ra = −0.92 ± 0.04). Higher pulp yield was moderately associated with higher S/G (ra = 0.47 ± 0.08), faster growth (diameter, ra = 0.53 ± 0.12) and lower extractives (ra = −0.61 ± 0.09).

Table 2 . Correlations among traits in Eucalyptus globulus at the additive (ra), subrace (rs) and phenotypic (rp) levels.

S/G Extractives Cellulose Pulp yield Diameter Density
Klason lignin ra −0.31** 0.62*** −0.90*** −0.92*** −0.38* −0.23*
rs −0.56* 0.90*** −0.98*** −0.95*** −0.32 0.45
rp −0.41*** 0.69*** −0.86*** −0.82*** 0.10*** −0.02
S/G ra −0.59*** 0.45*** 0.47*** 0.33* −0.28**
rs −0.78*** 0.73** 0.79*** 0.02 −0.72**
rp −0.49*** 0.55*** 0.57*** −0.03 −0.30***
Extractives ra −0.68*** −0.61*** −0.29 0.03
rs −0.93*** −0.95*** −0.07 0.58*
rp −0.74*** −0.66*** 0.20*** 0.25***
Cellulose ra 0.91*** 0.45*** 0.18
rs 0.99*** 0.30 −0.51
rp 0.90*** 0.04 −0.07**
Pulp yield ra 0.53*** 0.17
rs 0.33 −0.58*
rp 0.07** −0.07***
Diameter ra 0.06
rs 0.05
rp 0.03

The significance of the correlation from zero is indicated (*P < 0.05, **P < 0.01, ***P < 0.001).

Subrace level genetic variation

In addition to the significant additive genetic variation within subraces, there were highly significant differences between the subraces of E. globulus for all wood chemical traits as well as density, diameter, and pulp yield (Table 1). The level of differentiation between subraces for diameter was significant but low, consistent with its low heritability. The coefficient of subrace variation (CVs) ranged from 2.05 for pulp yield to an atypical high of 13.7 for extractives. When viewed relative to the additive genetic variation within populations (as measured by either QST or CVs/CVa), the level of genetic variation between subraces for all wood chemical traits was markedly higher than that observed for diameter, and even density (Table 1). QST was significantly (P < 0.001) greater than the race level divergence in neutral molecular markers measured by FST for all the wood chemical traits (Table 1).

At the subrace level, the patterns of variation in the four wood chemical traits (Klason lignin, S/G, extractives and cellulose) were not independent, with all rs estimates significant (P < 0.05) and most above |0.7| in magnitude (Table 2). The subrace differences in Klason lignin were negatively correlated with S/G (rs = −0.56 ± 0.11) and cellulose (rs = −0.98 ± 0.03) and positively correlated with extractives (rs = 0.90 ± 0.06). Of the wood chemical traits, S/G appeared to be the most genetically independent at the subrace and additive genetic level (Table 2). The subrace variation in S/G was negatively correlated with extractives (rs = −0.78 ± 0.11) and positively correlated with cellulose (rs = 0.73 ± 0.13).

The subraces showed broad-scale geographic structure in the wood chemical traits (Figure 1); as for cellulose (Stackpole et al. 2010b). The main differentiation was between the mainland and Tasmanian subraces. The linear regression of subrace means on subrace latitude of origin was significant for S/G (R2 = 76%, P < 0.001), density (R2 = 49%, P < 0.01), cellulose (R2 = 30%, P < 0.05) and extractives (R2 = 28%, P < 0.05) (Table 1), consistent with latitudinal clines in these traits to varying degrees. The strongest latitudinal cline was with S/G, which tended to increase southward (Figure 1). The highest S/G values (2.10–2.07) occurred in southeastern Tasmania and the inland northeastern Tasmania, southern Tasmania, and Tasman Peninsula subraces and, excluding the last due to small number of families sampled, their subrace means were significantly (P < 0.05) higher than all other subraces (see supporting information). The lowest subrace means (range, 1.82–1.96) were from the mainland Victorian subraces from the Otways, Strzelecki Ranges, and Gippsland. Most subraces with intermediate S/G (1.99–2.02; Figure 1) were from the Bass Strait islands (King Island, Furneaux and South Furneaux). Notable deviations from this latitudinal cline were significant differences in S/G between geographically proximal subraces in Victoria (Strzelecki Foothills 1.93 vs. Strzelecki Ranges, 1.85; Gippsland Coastal Plain, 1.82) and Tasmania (inland northeastern Tasmania 2.08 vs. northeastern Tasmania 1.96).

While extractives had a higher coefficient of variation between subraces (CVs) than S/G, only a small fraction of this variation could be explained by the latitudinal cline. Extractives content was highest in the Victorian and northeastern Tasmanian subraces (range, 4.9–5.6; except for Gippsland Foothills; seesupporting information) and lowest in subraces from the south of Tasmania (3.7–4.3; Figure 1c). King Island was also notable for its low extractives (3.9). Of particular note is the significantly high extractives content in the two coastal northeastern Tasmanian races (St. Helens, 5.6; inland northeastern Tasmania, 5.5) compared with all other eastern Tasmanian subraces (3.7–4.4) as well as the subraces immediately northward on the Furneaux Islands (Southern Furneaux, 4.2; Flinders Island, 4.4; see supporting information).

Klason lignin showed no significant latitudinal trend over the full geographic range (Table 1; Figure 1), even though there was a weak subrace correlation with S/G (Table 2). As with extractives, Klason lignin increased northward along the continuous distribution of E. globulus on the eastern Tasmanian seaboard (Figure 1). While the magnitude of the differences was not large, the Klason lignin of the three northern Tasmanian subraces (St. Helens, 21.3, northeastern Tasmania, 20.8; inland northeastern Tasmania, 20.8) was significantly greater than that of the south-eastern Tasmania (20.2) and southern Tasmania (19.6) subraces (see supporting information).

Discussion

A key finding of our study is the significant genetic variation in wood chemical composition which occurs between the subraces of E. globulus. These subraces clearly differ in Klason lignin content. The pattern of variation observed was similar to that reported by Poke et al. (2006) from a different field site in Tasmania (Pearson correlation among the nine localities in common; r = 0.7, P < 0.05), indicating relatively stable genetic differences between localities across sites. There are few forest tree studies of genetic variation in lignin content and these focus on conifers (Schutt 1958 cited in Zobel and Jett 1995; Sewell et al. 2002; Wainhouse et al. 1998). In Picea sitchensis, bark lignin content displayed a latitudinal trend, thought to be associated with resistance to pests and pathogens (Wainhouse et al. 1998). Broad-scale provenance variation in lignin content has also been demonstrated in a large-scale study of the native American grass Panicum virgatum (Casler 2005; Casler et al. 2004). No significant latitudinal trend was detected for lignin content in the present study, but one was detected for S/G.

There is some evidence that this clinal decrease in S/G with decreasing latitude within E. globulus may be part of a much broader continent-wide trend that transgresses multiple eucalypt species. First, while the wood specimens for each species were derived from different sites, Rencoret et al. (2008) reported that the S/G of E. globulus (at 2.6) was higher than that of species naturally distributed to its north, viz: E. maidenii (2.0), E. nitens (2.1), and particularly E. grandis (1.9). Second, del Rio et al. (2005) reported that the S/G of E. globulus (4.9) was higher than that of the closely related but more northerly distributed E. pseudoglobulus (3.7). Third, these trends are also evident across less-related species sampled from native forest from Tasmania to Papua New Guinea (Kawamura and Bland 1967). Despite these studies using different S/G analytical procedures that can give different results, E. globulus always had higher S/G than the species distributed to its north in a given study. There is continuous molecular and morphological variation from Tasmanian E. globulus to the closely related, northerly E. bicostata and E. pseudoglobulus, and the low S/G in the mainland subraces of E. globulus is potentially reflective of their intermediate status (Jones 2009). As with S/G, there is also the possibility that extractives content between eucalypt species increase northward across the climatic gradient between 40° S and 25° S. In E. globulus, for example, in a common environment trial it was shown that the extractives content of the wood from the closely related and more northerly distributed E. bicostata (5.7 ± 1.2) and E. maidenii (6.7 ± 1.0) was higher than that of E. globulus (3.7 ± 1.1) (Miranda and Pereira 2001), which again could reflect an extension of the intraspecific cline observed in extractives.

There are two lines of evidence to indicate that the broad-scale pattern of genetic differentiation in the various wood components of E. globulus is a result of divergent natural selection across the geographic range of the species. First, the quantitative differentiation as measured by QST is significantly greater than that of the neutral marker FST for all wood chemical components, which suggests that subrace divergence has been driven by natural (diversifying) selection (Latta 1998). Second, the broad-scale trends discussed above for S/G and extractives, and the significant associations between latitude of subrace origin and S/G, shows that the genetic differentiation parallels a broad-scale climatic/environmental gradient (Aitken 2004). The observed genetic variation in wood chemical composition may be due to an evolutionary response to abiotic or biotic stresses acting singly or simultaneously (Roelofs et al. 2008). For instance, variation in lignin content is likely to be of adaptive importance (Gonzalez-Martinez et al. 2006), as it has primary roles in stem strength (Coleman et al. 2008), maintenance of water conduction (Gindl 2001; Plomion et al. 2001; Voelker 2009; Walker 2006), and possibly defense (Blanchette 1991; Campbell and Sederoff 1996; Del Río et al. 2002; Coleman et al. 2008; Salmore and Hunter 2001; Schwarze et al. 2000; Syafii et al. 1988; Wainhouse and Ashburner 1996), each of which are probably affected by spatially varying selection pressures. There is also evidence that variation in S/G may similarly be of adaptive significance (Anterola and Lewis 2002; Coleman et al. 2008; Walker 2006). For example, guaiacyl is preferentially deposited in the walls of vessels (Watanabe et al. 2004; Wu et al. 1992), an arrangement that may exploit its higher hydrophobicity compared with syringyl, and is thought to confer higher hydrostatic impermeability to the vessel wall (Walker 2006). Genetically modified Populus genotypes with a higher proportion of guaiacyl have demonstrated increased resistance to breaking of the water column in the vessels (embolism) following water stress (Anterola and Lewis 2002; Coleman et al. 2008).

As with lignin, wood extractives are also thought to play a role in the tree defense against pathogens (Boddy 2001; Gierlinger et al. 2004; Taylor et al. 2002). To test for a geographic relationship between decay and wood chemical composition, published mean wood decay of E. globulus at the subrace level, available from Hamilton et al. (2007), and the locality means available from Poke et al. (2006) were regressed against lignin, extractives, and S/G in the present trial. The regressions were generally not significant; however, there was a single significant negative association (R2 = 65%; P < 0.05) between extractives levels from the present study and the locality level wood decay of Poke et al. (2006). This is a reasonable correlation for traits across two different trials conducted some years apart. However, as wood decay risk is likely to be higher in wetter climates, it will be challenging to unravel the roles of biotic and abiotic factors in shaping the natural patterns of genetic variation in wood chemical composition (Armbruster and Schwaegerle 1996). In addition, identifying which traits are under selection is complicated by the fact that the chemical traits are genetically correlated with each other, as well as with wood density and growth (see also Poke et al. 2006).

The pulpwood breeding objective for E. globulus aims to minimize the cost of pulp production per hectare by improving growth rate, density, and pulp yield (Greaves et al. 1997). While not currently considered breeding objectives, low total lignin and high S/G (Del Rio et al. 2005; Guerra et al. 2008; Macleod 2007; Pinto et al. 2002) are linked to more efficient chemical pulping, and these traits could be used as selection traits (Clarke 2009). Our study shows that there is significant additive genetic variation in these breeding objective and wood chemical traits, indicating their potential for genetic improvement through both between and within subrace selection. Within subraces, our additive genetic correlations indicate that selecting for increased growth will result in weak correlated genetic responses in wood chemistry, both increasing cellulose and S/G and decreasing lignin content. The positive additive genetic correlation observed between diameter and cellulose (ra = 0.45) was consistent with that of Apiolaza et al. (2005) (ra = 0.61 ns) and the average correlation of ra = 0.56 for five sites of E. nitens (Hamilton and Potts 2008), but was substantially different from the negative correlations (ra -0.16 to -0.43) previously reported by Raymond et al. (2001) in E. globulus. A previous small-scale study in E. globulus did not detect a significant additive genetic correlation between growth and lignin (Poke et al. 2006). However, the significant negative genetic correlation in our study (ra = −0.38) is informative given that two quantitative trait loci (QTL) for lignin have been shown to colocate with QTL for growth in hybrid eucalypts (Kirst et al. 2004). A higher rate of lignin production was associated with slower growth, possibly due to competition between the traits for carbon-based products.

Our results suggest that the only correlated response expected from selection for increased wood density within E. globulus subraces is a tendency for lignin and S/G to decrease. A negative phenotypic correlation between S/G and wood density was found in E. globulus by da Seca and Domingues (2006), a result that occurred at the phenotypic, additive genetic, and subrace levels in the present study. No additive genetic relationship was observed between density and extractives, similar to previous studies that also did not find a genetic (Miranda and Pereira 2002; Poke et al. 2006) or phenotypic (Ona et al. 1998) correlation. The present study also indicated that selection for increased pulp yield would result in increased cellulose content and S/G but reduced lignin and extractives content and higher S/G. The high subrace and additive genetic correlations between pulp yield and cellulose content demonstrate that they are effectively the same trait (Stackpole et al. 2010b). This is consistent with QTL studies in E. globulus, where all QTL that were identified for pulp yield colocated with cellulose QTL, although not all cellulose QTL colocated with QTL for pulp yield (Freeman et al. 2009; Thamarus et al. 2004). A significant negative genetic correlation of pulp yield and cellulose with Klason lignin has been reported previously in E. globulus (Poke et al. 2006). A negative phenotypic correlation has also been reported between Klason lignin and cellulose content (Ona et al. 1998). Such a negative relationship is expected due to the physical complementarity of cellulose and lignin in wood structure (Plomion et al. 2001).

In conclusion, our large-scale study has shown significant genetic variation in wood chemical composition at two-geographic scales within the native gene pool of E. globulus. There is evidence that this variation may be an adaptive response to either biotic or abiotic factors, although unraveling the nature of this selection will be challenging due to the strong correlation among traits and potential for correlation among the environmental selection agents across the geographic range of the species. Regardless of the cause of the patterns of genetic variation, the genetic correlations observed are generally favorable for a pulp wood breeding objective. This applies both among the chemical traits themselves as well as their correlation with the main breeding objective traits of growth, wood density and pulp yield. However, a future challenge will be to determine whether breeding objectives for adaptation to specific environments (e.g., drier or high disease risk areas) will be compatible with industrial objectives for the improvement of wood properties.

Supplementary Material

Supporting Information

Acknowledgments

We thank Gunns Limited for making the trial available for study. Kelsey Joyce, Linda Ballard, and Mark Reynolds assisted in field and laboratory work. We thank Chris Harwood for comments on the manuscript, Geoff Downes for advice with NIR modelling and Greg Dutkowski advice on data analysis, including formulating the likelihood ratio tests for QST. We also thank the Australian Research Council and industry partners on Linkage grant (LP0453704), the Southern Tree Breeding Association, and the Cooperative Research Centre for Forestry for their support.

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