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Plant Functional Traits and the Distribution of West African Rain Forest Trees alongthe Rainfall Gradient
Surya K. Maharjan1,2, Lourens Poorter1,2,5, Milena Holmgren2, Frans Bongers1, Jan J. Wieringa3, and William D. Hawthorne4
1 Forest Ecology and Forest Management Group, Wageningen University, PO Box 47, 6700 AA Wageningen, The Netherlands
2 Resource Ecology Group, Wageningen University, PO Box 47, 6700 AA Wageningen, The Netherlands
3 National Herbarium of The Netherlands—Wageningen University Branch, Biosystematics Group, Wageningen University,
General Foulkesweg 37, 6703 BL Wageningen, The Netherlands
4 Department of Plant Sciences, University of Oxford, South Parks Road, Oxford OX1 3RB, UK
ABSTRACT
Plant morphological and physiological traits affect the way plants tolerate environmental stresses and therefore play an important role in shaping species distributionpatterns in relation to environmental gradients. Despite our growing knowledge on the role of functional traits in structuring plant communities, few studies havetested their importance at large scales in the wet tropics. Here, we describe the distribution patterns of the most important West African rain forest timber species alongthe regional rainfall gradient and relate them to their functional traits. We found that the distribution patterns of 25 out of the 31 studied species (80%) weresignificantly related to mean annual rainfall. Shade tolerance and drought resistance were identified as the main strategy axes of variation. Wood density and leafdeciduousness emerged as the best predictor traits of species position along the rainfall gradient, explaining respectively 32 and 15 percent of the variation. Species traitstended to show stronger relationships with estimated optimum annual rainfall for each species than to the extreme rainfall conditions where they occur. The significantrole of rainfall in shaping timber species distribution and the strong relationships between species traits and rainfall indicate that changes in climate, especially decliningrainfall, could have strong effects on species composition and abundance in these tropical forests.
Key words: deciduousness; drought tolerance; plant strategy; rainfall; shade tolerance; species distribution; upper Guinea; wood density.
FUNCTIONAL RESPONSE TRAITS DETERMINE PLANT GROWTH, SURVIVAL
AND REPRODUCTIVE SUCCESS, and as a result, they are expected to play
an important role in shaping species distribution patterns along en-
vironmental gradients. The study of how functional response traits
affect the way plants tolerate environmental stresses and cope withdisturbances has played a central role in the development of eco-
logical theories (Grime 1974, 1977; Keddy 1992; Westoby 1998).
Most large-scale generalizations have compared the predominance
of morphological traits across vegetation types and evaluated their
potential adaptive role along environmental gradients (Ackerly
2004, Thuiller et al. 2004). In contrast, more detailed analysis
within vegetation types have concentrated on relationships between
functional traits at smaller-scale environmental gradients related to,for example, topography and exposition (Ackerly et al. 2002) and
irradiance and soil fertility (Veenendaal et al. 1996, Agyeman et al.1999). As reliable environmental response curves are lacking for
most tropical species, our knowledge of the importance of func-
tional traits for species partitioning of environmental gradients is
particularly poor for the tropics.
This study focused on the rainfall gradient, which is an im-
portant environmental factor determining plant species distribu-tion (Swaine 1996, Bongers et al. 1999, Engelbrecht et al. 2007),
composition (Hall & Swaine 1976, Bongers et al. 2004, Toledo
et al. 2011) and richness (ter Steege et al. 2006) in tropical forests.
Rainfall in West Africa has declined more rapidly than in any other
rain forest region during the past four decades (Malhi & Wright
2004), which could severely impact plant and animal diversity in
the region.
Plant species vary considerably in their morphological andphysiological traits giving rise to a continuum of plant strategies
(Reich et al. 2003). One fundamental axis of evolutionary special-
ization across ecosystems and biomes is that of high resource cap-
ture (rapid acquisition of resources) at one end of the spectrum and
high resource conservation (conservative use of resources) at the
other (Diaz et al. 2004). Consequently, along the rainfall gradient
rapid water acquisition and conservative water use could be impor-
tant strategies for the success of plant species. Conservative wateruse can be achieved through efficient use of limited water (i.e.,drought tolerance) or through drought avoidance (Markesteijn &
Poorter 2009). Drought-tolerant species are, in general, character-
ized by narrow and small leaves (Fonseca et al. 2000, Thuiller et al.2004), low specific leaf area (SLA) (Fonseca et al. 2000, Niinemets
2001) and high wood density (Searson et al. 2004, Poorter &
Markesteijn 2008). Drought-avoiding species are characterized by
deciduous leaves (Borchert 1994, Markesteijn & Poorter 2009) toavoid transpirational water loss in the dry season, and low wood
density (Borchert 1994) that allows for water storage in stems.
With increasing rainfall, forests also tend to become taller and
cast a deeper and more persistent shade. To regenerate successfully
in these wetter, more shaded environments species should be more
shade tolerant (Smith & Huston 1989), and have larger seeds toReceived 29 January 2010; revision accepted 23 September 2010.5Corresponding author; e-mail: lourens.poorter@wur.nl
BIOTROPICA 43(5): 552–561 2011 10.1111/j.1744-7429.2010.00747.x
552 r 2011 The Author(s)
Journal compilation r 2011 by The Association for Tropical Biology and Conservation
provide the seedling with sufficient seed reserves to survive in shade
(Grubb 1998, Leishman et al. 2000). Competition for light favors
larger maximum plant heights (Fonseca et al. 2000), and due to
little wind within closed canopy forests seed dispersal is more oftenby animals (Bullock 1995). Clearly, plants have to cope with mul-
tiple environmental conditions, and they can do so through differ-
ent traits. A question, therefore, is how these traits are associated,
and what plant strategies can be distinguished.
Here we studied the distribution patterns of 31 West African
rain forest timber species in relation to the rainfall gradient, and
related these patterns to 25 traits that have been identified in the
literature as important for plant growth, survival and reproduction.The use of timber species has several advantages: first, forest inven-
tories have been done at a sufficiently large scale and intensity to get
reliable distribution data; second, these species have been invento-
ried in several countries covering a large rainfall gradient; third, a
considerable amount of trait information is available in the litera-
ture; and fourth, it is important to know how these commercially
important species may respond to climate change. The selection of
timber species may, to some extent, also affect the results as timberspecies may not cover the full range of species traits found among
tropical trees (see ‘Methods’).
We addressed the following questions: (1) How do tree species
respond to the rainfall gradient in terms of abundance? (2) How are
functional traits associated and what plant strategies can be recog-
nized? (3) Which functional traits are the best predictors of species
distribution along the rainfall gradient?
METHODS
STUDY AREA.—This study focused on a steep rainfall gradient across
West African rain forests. Rainfall varies from ca 4000 mm/yr near
the coast in Liberia to ca 1000 mm/yr at the forest–savanna bound-
ary to the north and east (Poorter et al. 2004). Along the rainfall
gradient, vegetation changes from wet evergreen, to moist ever-green, moist semi-deciduous and dry semi-deciduous forests (Hall
& Swaine 1981, Bongers et al. 2004). At the driest end of the gra-
dient, there are some tiny fragments of dry evergreen forests in
Ghana, but these were not included in this study.
SPECIES SELECTION.—For this study, 31 timber species (see caption
of Fig. 2) were selected, for which forest inventory data were avail-able at the species level, and that were reliably identified in each
country. Several other important timber species were inventoried at
genus level only (e.g., Entandrophragma, Erythrophleum, Khaya and
Parinari spp.) but were not included in the analysis because trait
variations among congeners were relatively large. The use of timber
species may affect the results if such species do not cover the full
range of species traits found among tropical trees. Our selected
timber species do cover almost the full possible range in wood den-sity (0.25–1.09 g/cm3) but are, however, relatively large (the max-
imum observed height ranges from 30 to 60 m, while the forest
canopy is at 40 m) so understory species are under-represented.
SPECIES DISTRIBUTION DATA.—Species distribution was analyzed us-
ing forest inventory data from 176 forest inventory sites in Sierra
Leone (8), Liberia (26), Ivory Coast (37) and Ghana (105). Data
for Sierra Leone were collected by Small (1953), Savill and Fox(1967) and Davies (1987); for Liberia by German Forestry Mission
to Liberia (GFML 1967a, 1967b; Sachtler & Hamer 1967a,
1967b; Sachtler 1968) and Liberian Forest Service; for Ivory Coast
by SODEFOR (Clement & Guinaudeau 1973; SODEFOR 1978,
1979) and for Ghana by Wong (1989), Hawthorne and Abu Juam
(1995) and Hawthorne (1995, 1996). Inventoried area of each site
varied from 10 to 4500 ha. The abundance values for species were
expressed as number of trees 4 30 cm diameter at breast height perkm2 to have comparable abundance values for all sites. See Bongers
et al. (2004) for more details.
Using forward multiple regression, the abundance of a species
was regressed against environmental variables that are likely to in-
fluence large-scale species distribution patterns, such as annual rain-
fall, soil water holding capacity (WHC), cation (i.e., calcium,
magnesium and potassium) availability, altitude and their quadratic
terms. By including quadratic terms of the environmental variables,nonlinear responses of species to the environment could be mod-
eled (Jongman et al. 1987). Rainfall data were derived from a rain-
fall map based on data from 578 weather stations in West Africa,
using the inverse distance weighting interpolation method in Arc
View (Poorter et al. 2004). To increase the spatial resolution we
included as many weather stations as possible, with the drawback
that the length of the monitoring period and the years covered var-
ied between stations. WHC and cation availability data were calcu-lated based on the FAO soil map of Africa and a quantitative review
of chemical analyses of soil profiles (Batjes 1997). Soil depth and
soil texture were taken as parameters to determine WHC and it was
assumed that sandy soils have WHC of 75 mm/m, loamy soils of
100 mm/m and clayey soils of 125 mm/m. Altitude data were de-
rived from the Digital Chart of the World (ESRI 1984). To esti-
mate environmental conditions of a forest site, we used its center.
The regression analysis showed that in 25 out of 31 studied speciesrainfall is the most important environmental factor determining
species distribution and abundance. Of course, small-scale differ-
ences in soil conditions might explain smaller-scale distribution
patterns of trees, but here we focus on large-scale gradients.
The species-specific regression equations were used to show
how species respond to rainfall. Rainfall response curves were
drawn by varying rainfall only, while keeping the other environ-
mental variables in the regression equation constant, by using theaverage environmental conditions across the 176 forest inventory
sites in the equation (WHC: 70.3 mm/m; cation availability:
1.4 cmol/kg; altitude: 219 m). As the original forest inventory data
covered the rainfall range from 1200 to 3400 mm/yr, the species
response curves were made by interpolating abundance of each
timber species at 10 mm rainfall intervals between 1000 (forest–
savanna boundary) and 3400 mm/yr rainfall.
Species response curves represent the realized niche of eachspecies along an environmental gradient. The shape of the response
curve was described using minimum (Rmin), optimum (Ropt),
maximum (Rmax) and amplitude (Ramp) of annual rainfall (all in
Functional Traits Affect Species Distribution 553
mm/yr). Ramp is the difference between Rmax and Rmin and repre-
sents the range of annual rainfall where a species occurs. Ropt
represents annual rainfall level at which abundance of a species is
maximum (i.e., an estimation of ecological optimum). If theresponse curve would have completely fallen within the studied
rainfall gradient (as is the case for Petersianthus macrocarpus), then
the Ropt and rainfall amplitude could have been obtained from the
regression coefficients of the Gaussian curves. As several response
curves were cut-off at either the lower (e.g., Triplochiton scleroxylon)
or the higher (e.g., Tetraberlinia tubmaniana) end of the rainfall
gradient, rainfall parameters were derived in a different way: the
tenth and 90th percentiles for each species were taken as lower andupper limits of the niche (thus avoiding the more noisy extremes)
and their corresponding rainfall values are referred to as Rmin
and Rmax (Fig. 1). In cases where Ropt was located below Rmin (e.g.,T. scleroxylon; Fig. 1B), Ropt was assumed to have the same value as
Rmin; and in cases where Ropt was located above Rmax (e.g., T. tub-maniana), Ropt was assumed to have the same value as Rmax.
SPECIES TRAIT DATA.—To analyze the association of traits and how
to distinguish strategies amongst tree species, we selected 25 traits(Table 1) that are important for plant growth, survival and repro-
duction. Reproductive traits included the color and size of flowers
and fruits (as this determines the type of pollinators and dispersers),
FIGURE 1. Illustration of process of calculation of four rainfall parameters
(Rmin, Ropt, Rmax and Ramp) using the species response curves. Area under the
response curve is considered to be 100 percent. Dotted lines represent lower
(where lower 10% of species occurs), optimum (where abundance of species is
maximum) and upper (where upper 10% of species occurs) limits of realized
niche. Black dots along the horizontal axis corresponding to those dotted lines
represent the annual rainfall levels at those points, i.e., Rmin, Ropt and Rmax. Ramp
is simply the range between Rmin and Rmax. See methods section for more
detailed explanation.
TABLE 1. Twenty-five functional response traits selected for this study. Given are
trait names, trait attributes and their abbreviations used in categorical
principle component analysis (CATPCA). White, yellow, orange, pink,
yellowish-green, cream-color and silvery-gray were grouped as light color,
and red, blue, green, brown, purple and black were grouped as dark
color for flower and fruit color.
Species traits Trait attributes Abbreviations
Reproductive traits
Flower size 1: Small (length o 1 cm) Fl_Size
2: Medium (length 1–4 cm)
3: Large (length 4 4 cm)
Flower color 1: Light colored flower Fl_Light
2: Dark colored flower Fl_Dark
Fruit length (cm) Fr_Len
Fruit width (cm) Fr_Wid
Fruit color 1: Light colored fruit Fr_Light
2: Dark colored fruit Fr_Dark
Fruit type 1: Fleshy Fleshy
2: Dry Dry
Dispersal mode 1: Explosive D_Exp
2: Wind D_Win
3: Animals D_Ani
Seed traits
Number of seeds 1: One seed Nr_Seed
2: Few seeds (2–10)
3: Many seeds (4 10)
Seed length (cm) S_Len
Seed width (cm) S_Wid
Seedling type 1: Cryptocotylar epigeal reserve CER
2: Cryptocotylar hypogeal reserve CHR
3: Phanerocotylar epigeal
foliaceous
PEF
4: Phanerocotylar epigeal reserve PER
Leaf traits
Deciduousness 1: Deciduous Deci
2: Evergreen Ever
Leaf type 1: Simple Simp
2: Compound Comp
Leaf texture 1: Papery/herbaceous LT_Pap
2: Coriaceous LT_Cor
Leaf hairs 1: Without hairs No_hair
2: With hairs Hair
Leaf length (cm) L_Len
Leaf width (cm) L_Wid
Specific leaf area (cm2/g) SLA
Leaf N-concentration (mg/g) Nmass
Leaf P-concentration (mg/g) Pmass
Stem traits
Modulus of elasticity (kg/cm2) MOE
Wood density (g/cm3) WD
Size related traits
Maximum diameter (m) Dmax
Maximum height (m) Hmax
554 Maharjan, Poorter, Holmgren, Bongers, Wieringa, and Hawthorne
seed size, and number and dispersal syndrome. Leaf traits that
are important for the water and heat balance are leaf type (simple/
compound), size, texture, hairiness, SLA, nutrient concentrationsand deciduousness. SLA and nutrient concentration are important
for the carbon gain and growth potential of the plant. Modulus of
elasticity is related to stem stability, wood density is related to stem
construction costs, water storage and cavitation resistance, and
maximum height and diameter determine species competitive abil-
ity for light. The shade tolerance guild (shade-bearer, nonpioneer
light demander and pioneer; sensu Hawthorne 1995) is not a func-
tional trait but was included to reflect the overall strategy of a spe-cies as shade tolerance is important for species success in closed
tropical forests. Species trait data were assembled from published
sources (i.e., Siepel et al. 2004, Hawthorne & Jongkind 2006) and
herbarium specimens available at National Herbarium of The
Netherlands, Wageningen University Branch. Data on SLA (leaf
area divided by leaf mass), leaf nitrogen concentration (Nmass) and
leaf phosphorous concentration (Pmass) were measured using dried
leaf samples obtained from herbarium specimens.SLA is generally calculated as fresh leaf area divided by oven-
dried leaf mass. For this study, SLA was calculated as dried leaf area
divided by dried leaf mass (leaves were oven-dried initially and
stored at room temperature). In case of compound leaves, leaf area
was measured as the leaflet area. To evaluate the potential error in
SLA determination using herbarium leaves, we compared in a sep-
arate analysis of 32 West African species the leaf mass of freshly
oven-dried leaves with the leaf mass of oven-dried leaves stored atroom temperature. Freshly oven-dried leaves were, on average, 5
percent lighter than oven-dried leaves stored at room temperature.
To evaluate leaf area shrinkage during herbarium drying, fresh
leaves of 21 taxa were collected from the tropical greenhouse, and
leaf areas were measured before and after oven drying. Dry leaf areas
were, on average, 12 percent less than fresh leaf areas. The dried leaf
samples were analyzed for Nmass and Pmass. Owing to limited avail-
ability of duplicate specimens only 13 species could be analyzed.Leaf samples were weighed, crushed into powder, digested in tubes
using H2SO4–salicylic acid–H2O2 and selenium (Novozamsky
et al. 1983), and N- and P-content were then measured using
Skalar San-plus auto analyzer.
Species were classified into different seedling types (Garwood
1996), based on the exposure of the cotyledons (exposed: phanero-
cotylar [P]; hidden in the seed: cryptocotylar [C]), the position of
the cotyledons (aboveground: epigeal [E]; belowground: hypogeal[H]), and whether the cotyledons are photosynthetically active
(leaf-like and active: foliaceous [F]; thick and not active: reserve
[R]). Four seedling types were found in this study (for seedling type
abbreviations, see Table 1).
DATA ANALYSIS.—A categorical principle component analysis
(CATPCA) was used to evaluate trait associations and plant strat-
egies. CATPCA is a nonlinear equivalent of PCA (Linting 2007).
Twenty-three traits of 25 species with complete trait data were in-cluded in the analysis. As Nmass and Pmass data were not available for
all species, they were not included in the main analysis but were
later related to the species scores along the first two CATPCA axes.
To evaluate whether species traits predict species distribution
along the rainfall gradient a Pearsons correlation was used to relate
species traits to rainfall parameters. Where necessary, species traits
and rainfall parameters were log10-transformed before analysis to
improve normality and homoscedasticity. For categorical traits,differences in rainfall levels among categories were tested using a t-test or ANOVA. To identify the best predictors of species position
along the rainfall gradient a multiple categorical regression (CAT-
REG) analysis was used, which is a nonlinear equivalent of linear
multiple regression analysis (van der Kooij 2007). Rainfall param-
eters were used as the dependent variables and species traits
as the independent variables, as these traits should determine the
position of the species along the rainfall gradient. Continuoustraits were standardized by multiplying by ten and rounding them
to integers. Traits with limited number of observations (Nmass
and Pmass) were not included in the regression analysis. All
statistical analyses were done using PASW Statistics 17 (SPSS Inc.,
Chicago).
RESULTS
SPECIES RESPONSE TO THE RAINFALL GRADIENT.—Of the 31 timber
species included in this study, 25 species responded significantly to
the rainfall gradient. Of these 25 species, 14 species (56%) had sta-tistically normal response curves along the rainfall gradient with
clear minima, optima and maxima (e.g., P. macrocarpus, Pycnanthusangolensis; Fig. 2). The abundance of seven species (28%) decreased
along the rainfall gradient (e.g., Nesogordonia papaverifera,
T. scleroxylon; Fig. 2) and the abundance of four species (16%)
increased along the rainfall gradient (e.g., Anopyxis klaineana,
T. tubmaniana; Fig. 2).
TRAIT ASSOCIATIONS AND PLANT STRATEGIES.—CATPCA was used to
evaluate associations among species traits. First and second CAT-
PCA axes explained respectively 23 percent and 15 percent of trait
variation (Fig. 3A). Shade-bearers (e.g., Mammea africana,Turraeanthus africanus) and pioneers (e.g., Alstonia boonei, Ceibapentandra) differed in their position along the first CATPCA axis
(t-test, t = 4.97, Po 0.001), with pioneers having higher axis
scores. This indicates that the first axis corresponds to a gradient in
shade tolerance. Shade-bearers on the left side of the axis were char-
acterized by evergreen leaves, relatively small stature, large seeds and
seedlings with reserve type cotyledons (CHR, CER and PER seed-
lings, Table 1) while pioneer species on the right side of the axiswere characterized by deciduous leaves, large stature, small and nu-
merous seeds and seedlings with foliaceous photosynthetically ac-
tive cotyledons (PEF seedlings).
TABLE 1. Continued
Species traits Trait attributes Abbreviations
Guild 1: Shade-bearer SB
2: Nonpioneer light demander NPLD
3: Pioneer P
Functional Traits Affect Species Distribution 555
At the top of the second CATPCA axis were mainly low-rain-
fall species (e.g., Ricinodendron heudelotii, T. scleroxylon) occurring
in the areas with Ropt � 1500 mm/yr (Fig. 3B). At the bottom of
the second CATPCA axis were mainly high rainfall species (e.g., A.klaineana and T. tubmaniana) occurring in the areas with Ropt
Z3000 mm/yr (Fig. 3B). Indeed the species scores along the sec-
ond CATPCA axis were significantly and negatively correlated to
rainfall parameters (i.e., Rmin, Ropt and Rmax; Table 2) and this axis
thus corresponds to a gradient in drought resistance. Low-rainfall
species at the top of the axis were characterized by large leaf size
(large leaf width and length), high SLA and high leaf nutrient
FIGURE 3. Categorical principle component analysis (CATPCA) loading plots
(A) and species scores (B) of 25 timber species based on 23 traits. The first and
second axes explained 23 percent and 15 percent of the trait variation, respectively.
(A) Lines with dot originating from origin represent loadings for continuous and
ordinal traits while dots represent centroids for categorical traits. (A) Nmass and Pmass
(indicated by asterisk) were not included in the CATPCA, but were later related to
the CATPCA axes scores. (B) Open symbols represent species occurring in areas
with Ropt � 1500 mm/yr; closed symbols represent species occurring in areas with
Ropt Z3000 mm/yr and gray symbols represent species occurring in-between. Trait
abbreviations used in loading plots are given in Table 1. Species abbreviations used
in species scores plots refer to first three letters of the genus name and first three
letters of the species name. Species list is included in the caption of Fig. 2.
FIGURE 2. Species response curves of 31 timber species along the rainfall gra-
dient. (A) Species with maximum abundance Z100 per km2; (B) species with
maximum abundance Z20 per km2 and o 100 per km2; and (C) species with
maximum abundance o 20 per km2. Numbers refer to the 31 species selected
for the study, i.e., 1: Alstonia boonei; 2: Amphimas pterocarpoides; 3: Anopyxis
klaineana; 4: Anthonotha fragrans; 5: Antiaris toxicaria; 6: Canarium schwein-
furthii; 7: Ceiba pentandra; 8: Distemonanthus benthamianus; 9: Funtumia afric-
ana; 10: Gilbertiodendron preussii; 11: Guarea cedrata; 12: Guibourtia ehie; 13:
Heritiera utilis; 14: Klainedoxa gabonensis; 15: Lophira alata; 16: Lovoa trichilio-
ides; 17: Mammea africana; 18: Nauclea diderrichii; 19: Nesogordonia papaverif-
era; 20: Petersianthus macrocarpus; 21: Piptadeniastrum africanum; 22:
Pycnanthus angolensis; 23: Rhodognaphalon brevicuspe; 24: Ricinodendron heu-
delotii; 25: Terminalia ivorensis; 26: Terminalia superba; 27: Tetraberlinia tub-
maniana; 28: Tieghemella heckelii; 29: Triplochiton scleroxylon; 30: Turraeanthus
africanus; and 31: Zanthoxylum gilletii.
556 Maharjan, Poorter, Holmgren, Bongers, Wieringa, and Hawthorne
concentrations (high Nmass and Pmass), whereas high-rainfall species
at the bottom of the axis were characterized by high wood density,
high modulus of elasticity, seeds dispersed by active expulsion and
PER seedling types.
SPECIES TRAITS VS. THE RAINFALL GRADIENT.—Of the 15 continuous
species traits related to rainfall parameters, a similar number of
species traits (3–4) were significantly correlated to Rmin, Ropt and
Rmax whereas none was significantly correlated to Ramp (Table 2).
Most traits (Pmass, modulus of elasticity, wood density) showed a
stronger correlation to Ropt than to Rmin or to Rmax (Table 2). Thissuggests that Ropt is a better rainfall parameter to explain trait vari-
ations than Rmin or Rmax. Ropt was significantly correlated to Rmin
(Pearson’s r = 0.87, Po 0.01) and Rmax (Pearson’s r = 0.79, Po 0.01) indicating that Ropt is a good indicator of both Rmin and
Rmax. In addition, Ropt also reflects the average position of species
along the rainfall gradient. Thus, only Ropt was used for further an-
alyses. Only three out of 15 continuous species traits were signifi-
cantly correlated to Ropt (Table 2). Wood density and modulus ofelasticity increased significantly with increasing rainfall while Pmass
decreased significantly with increasing rainfall (Table 2).
Deciduous species occurred in significantly lower-rainfall areas
than evergreen species (t-test: t29 = 2.76, Po 0.05; Fig. 4A). Ropt
differed among dispersal modes (ANOVA: F2, 29 = 4.55, Po 0.05):
species dispersed by wind or animals tended to be more common in
low-rainfall areas than those dispersed by active expulsion of seeds
(Fig. 4B). Ropt also differed among seedling types (ANOVA:F3, 27 = 3.30, Po 0.05). Species with seedlings with foliaceous pho-
tosynthetically active cotyledons (PEF seedlings) occurred in lower
rainfall areas than those with seedlings with reserve type cotyledons
(CER, CHR and PER seedlings; Fig. 4C).
Ropt was regressed against species traits using a multiple CAT-
REG analysis to evaluate the relative importance of species traits
in explaining species distribution along the rainfall gradient. Wood
density and deciduousness emerged as the best traits explaining spe-cies distribution along the rainfall gradient. Ropt was positively asso-
ciated with wood density (CATREG: b = 0.43, partial R2 = 0.32,
Po 0.01; Fig. 5) and was negatively associated with deciduousness
(CATREG: b =� 0.41, partial R2 = 0.15, Po 0.01; Fig. 5).
DISCUSSION
SPECIES RESPONSE TO THE RAINFALL GRADIENT.—The majority of the
study species responded significantly to the rainfall gradient
TABLE 2. Pearson’s correlation between species scores along first two categorical
principle component analysis (CATPCA) axes and rainfall parameters,
and species traits and rainfall parameters. N indicates the number of
species included in the correlation analysis. Correlations in bold are sig-
nificant at Po 0.05 and those in bold and italic are significant at
Po 0.01. Diameter, fruit length, fruit width, seed length, seed width,
SLA, Pmass and Rmin were log10-transformed.
Rmin Ropt Rmax Ramp N
Strategy axis
CATPCA axis 1 � 0.24 � 0.35 � 0.30 � 0.10 25
CATPCA axis 2 � 0.40 � 0.49 � 0.57 � 0.16 25
Species traits
Flower size � 0.17 � 0.17 � 0.33 � 0.18 31
Fruit length 0.06 0.08 0.07 0.01 31
Fruit width 0.27 0.33 0.11 � 0.14 31
Leaf length � 0.01 0.02 � 0.12 � 0.03 31
Leaf N-content � 0.65 � 0.50 � 0.14 0.42 13
Leaf P-content � 0.72 � 0.78 � 0.59 0.04 13
Leaf width � 0.14 � 0.18 � 0.43 � 0.30 31
Maximum diameter � 0.03 � 0.03 0.04 0.08 31
Maximum height � 0.10 � 0.19 � 0.05 0.02 31
Modulus of elasticity 0.47 0.57 0.50 0.10 30
Number of seeds 0.02 0.05 0.05 0.03 31
Seed length 0.16 0.29 0.17 0.04 30
Seed width 0.13 0.29 0.26 0.14 30
Specific leaf area � 0.34 � 0.24 � 0.19 0.14 31
Wood density 0.47 0.57 0.44 0.05 29
FIGURE 4. Relationships between optimum annual rainfall (Ropt) and categorical species traits. Differences between the categories were tested using t-test and
ANOVA. Bar diagrams with same letters at the top are not significantly different while those with different letters at the top are significantly different (LSD post-hoc
test, Po 0.05). Error bars show mean� 1 SE. (A) Deci and Ever correspond to deciduous and evergreen species respectively. (B) Explosive, Wind and Animal
correspond to species dispersed by active expulsion of seeds, by wind and by animals, respectively. (C) CER, CHR, PEF and PER correspond to cryptocotylar epigeal
reserve, cryptocotylar hypogeal reserve, phanerocotylar epigeal foliaceous and phanerocotylar epigeal reserve seedling types, respectively.
Functional Traits Affect Species Distribution 557
indicating the important role of rainfall in shaping species distribu-
tion patterns in West Africa (cf. Swaine 1996, Bongers et al. 1999,
Holmgren & Poorter 2007). As expected, the abundance of many
species followed bell-shaped response curves along the rainfall gra-
dient with clear minima, optima and maxima (Fig. 2). Many spe-
cies had widespread distribution ranges represented by bell-shaped
response curves extending over the entire rainfall gradient (e.g., P.macrocarpus, P. angolensis; Fig. 2) and some had local distributionranges restricted to low-rainfall areas (e.g., N. papaverifera, T.scleroxylon; Fig. 2) or high-rainfall areas (e.g., A. klaineana, T. tub-maniana; Fig. 2) (cf. Holmgren & Poorter 2007).
During the past four decades, West Africa has experienced a
severe decline in rainfall (Malhi & Wright 2004) and even
a stronger decline in precipitation might be expected with a future
reduction in forest cover. As a result, species restricted to high-rainfall
areas (e.g., A. klaineana, T. tubmaniana) are likely to be more vulner-able, whereas species restricted to low-rainfall areas (e.g., N. papaverif-era, T. scleroxylon) are likely to become more abundant.
TRAIT ASSOCIATIONS RELATED TO SHADE TOLERANCE.—CATPCA in-
dicated that the first two strategy axes correspond to shade tolerance
and drought resistance, respectively. Shade tolerance emerged as the
primary strategy axis, possibly because all forest types have horizon-
tal (from the understory to gap centers) and vertical (from the un-
derstory to the canopy) gradients in light availability. The shadetolerance axis separated shade-tolerators (shade-bearers) from light-
demanding pioneers, with the nonpioneer light demanders being in
between (Fig. 3A). Shade-tolerators were characterized by evergreen
leaves, a relatively small stature, large seeds and hypogeal cotyle-
dons. These traits may enhance their performance under low-light
conditions. The presence of evergreen long-lived leaves ensures effi-
cient and conservative use of carbon resources in the shaded under-
story (Givnish 1988, Walters & Reich 1999, Poorter 2009). Therelatively small stature of these species is indicative of species’ ability
to tolerate asymmetric competition for light in moist forests. Large
seeds allows these species to produce larger seedlings with better
seedling survival in the shaded understory (Leishman et al. 2000,
Myers & Kitajima 2007). Experimental evidence shows that hypo-
geal cotyledons present among seedlings of shade-tolerators further
enhance seedling survival in the shaded understory (Baraloto &Forget 2007).
Light demanders were characterized by traits that enable these
species to take advantage of the higher amount of light available in
open areas. In high-light environments, water stress is more severe,
and most light-demanding species had a deciduous leaf habit by
which severe water stress during the dry season might be avoided.
Deciduous species are capable of more efficient light capture per
unit leaf mass (Antunez et al. 2001, Eamus & Prior 2001, Ruiz-Robleto & Villar 2005) because of their high SLA (Poorter &
Markesteijn 2008). This allows faster growth during the wet season,
which may partially compensate for a shorter growing season. The
relatively large stature of light-demanding species provides a com-
petitive advantage for light. The small seeds facilitate wind dis-
persal, which is common among species with emergent crowns that
colonize open areas (Bullock 1995, Holmgren & Poorter 2007).
The large number of seeds facilitates the colonization of new openareas (Dalling & Hubbell 2002). Small seeds have few reserves, and
the resulting seedlings tend to have foliaceous photosynthetically
active cotyledons to ensure optimum use of high irradiance, and
rapid heterotrophic growth (Kitajima 1992).
TRAIT ASSOCIATIONS RELATED TO DROUGHT RESISTANCE.—Drought
resistance (i.e., the capacity of a plant to withstand periods of dry-
ness; Larcher 1980) emerged as the secondary strategy axis. Thedrought resistance axis separated low-rainfall species from high-
rainfall species (Fig. 3B). Low-rainfall species were characterized by
large leaves, high SLA, high leaf nutrient concentration, low wood
density and modulus of elasticity, whereas high-rainfall species were
characterized by the opposite suite of traits (Fig. 3). A low wood
density enables low-rainfall species to store water in their stem to
enable flowering during the dry season and leaf flushing at the end
of dry season (Borchert 1994). During the wet season, this storedwater is not only used for daily transpiration (Meinzer et al. 2004)
but, more importantly, the high capacitance might buffer plants
against daily fluctuations in xylem tension and leaf water potential
(Meinzer et al. 2008). At even lower rainfall, it is expected that spe-
cies would have high wood density to resist drought-induced cav-
itation and avoid vessel implosion (Pratt et al. 2007, Markesteijn
et al. 2011). Low-rainfall species were also characterized by high leaf
nutrient concentrations (cf. Santiago et al. 2004), which implieshigher photosynthetic capacity because most of the leaf N and P are
allocated to photosynthetic enzymes. High leaf nutrient concentra-
tions reduce leaf internal CO2 concentrations and a strong CO2
gradient is created between leaf interior and the atmosphere allow-
ing fast diffusion of CO2 for a given stomatal aperture, thus
minimizing stomatal water loss (Wright et al. 2001). This enables
low-rainfall species to maintain a given photosynthetic capacity for
minimum use of water. Leaf deciduousness was not strongly asso-ciated with this multivariate drought resistance axis, although as an
individual trait it is one of the best predictors of species’ position
along the rainfall gradient (see below). Leaf area was higher for
FIGURE 5. Relationship between optimum annual rainfall and wood density
for 15 deciduous species (open symbols) and 14 evergreen species (closed sym-
bols). Regression line, coefficient of determination (R2) and significance level (P)
are shown.
558 Maharjan, Poorter, Holmgren, Bongers, Wieringa, and Hawthorne
low-rainfall species, whereas often the opposite is found (Fonseca etal. 2000).
Reproductive traits such as flower size and color did not load
high on the drought axis of the CATPCA. Reproductive traits donot affect drought resistance directly, but other studies found that
their relative occurrence does vary in forest communities along the
rainfall gradient, because of differences in the effectiveness or fre-
quency of pollinator- and dispersal-vectors. Dry forest species tend
to have ‘conspicuous’ flowers (that are large or bright) pollinated by
specialist pollinators such as large bees, hummingbirds or hawk-
moths (Gentry 1982), and tend to be wind-dispersed (thus taking
advantage of the seasonally open canopy). Wet forest species tend tobe animal dispersed (Bullock 1995).
TRAIT–RAINFALL RELATIONSHIPS AND BEST PREDICTOR TRAITS.—Of the
25 studied species traits, six traits showed significant relationships to
Ropt. Of these six traits, wood density and deciduousness emerged as
the best predictors of species distribution along the rainfall gradient
explaining 47 percent of the variation in Ropt. We expected that spe-cies traits would determine the minimum environmental conditions
that a species can tolerate. This apparently was not the case, because
species traits tended to show stronger relationships to Ropt than to
Rmin or any other rainfall parameter (Table 2). This suggests that traits
shape the realized niche, and especially the optimal conditions (i.e., in
this case Ropt) under which a species occurs.
Moist forests in high-rainfall areas cast deeper shade than dry
semi-deciduous forests in low-rainfall areas (Coomes & Grubb2000) due to high leaf area index and less seasonality of leaf cover
(Parker et al. 2005). Higher wood density provides greater struc-
tural stability and greater resistance against physical damage caused
by falling debris (van Gelder et al. 2006) and pathogens (Augs-
purger & Kelly 1984) in the shaded understory of moist forests.
Lower wood density, on the other hand, enhances growth in gaps
(Muller-Landau 2004, Poorter 2008) and enables species to store
water in their stem to enable flowering during the dry season andleaf flushing at the end of dry season (Borchert 1994). Wood den-
sity showed a significant positive relationship to rainfall (Table 2;
Fig. 5) and modulus of elasticity followed wood density because
they are closely related (Pearson’s r = 0.91, Po 0.001, N = 24; cf.van Gelder et al. 2006).
Deciduous species occurred in significantly lower rainfall areas
than evergreen species (Figs. 4A and 5). Shedding of leaves during
the dry season helps the plant to prevent water loss through leaftranspiration and enhances drought survival (Poorter & Mark-
esteijn 2008), which makes deciduous species more adapted to dry
forests (Givnish 2002). Evergreen leaves with long life-span, on the
other hand, ensure efficient and conservative use of carbon
resources in the shaded understory of moist forests (Poorter 2009).
Deciduousness is one of the strategies to survive in drier areas,
and another strategy, is to make evergreen, sclerophyllous leaves
(Ackerly 2004, Markesteijn & Poorter 2009). In dry forests, thisevergreen strategy is mostly confined to understory and subcanopy
species and rarely found for canopy species, which were the subject
of this study.
Dispersal mode, seedling type and Pmass showed significant re-
lationships with Ropt probably because they are important for spe-
cies success in high-light conditions of dry and open forests vs. the
low-light conditions of wet and closed forests. Wind dispersal isadvantageous in drier forests with a seasonally deciduous and open
canopy which is more exposed to wind (Bullock 1995). Foliaceous
photosynthetically cotyledons can contribute to carbon gain in
drier forests with a higher light availability, whereas reserve type
cotyledons can support seedlings in the shaded understory of wetter
forests where there is little carbon gain. Pmass might be higher in
low-rainfall areas for several reasons: First, dry forest species might
be more light demanding, and light-demanding species may benefitfrom P investment in leaves to realize a higher carbon gain. Second,
P investment in photosynthetic enzymes may draw down the inter-
nal CO2 concentration and enhance water use efficiency. Third, dry
forest soils are less leached and leaf nutrient concentrations may
therefore be higher.
In conclusion, the majority of the studied species responded
significantly to the rainfall gradient indicating the vital role of rain-
fall in shaping species distribution patterns. Based on the trait as-sociations, shade-tolerance and drought-avoidance were identified
as the key strategies for the success of timber species in West Africa.
Wood density and deciduousness emerged as the best predictors of
species distribution along the rainfall gradient. In addition to the
morphological traits evaluated here, physiological traits such as
the ability to tolerate low leaf water potentials and low leaf water
content are also good predictors of species drought tolerance and
distribution along rainfall gradients (Baltzer et al. 2008, Kursaret al. 2009).
ACKNOWLEDGMENTS
The authors express their sincere gratitude to the ECOSYN project
for providing access to the database; National Herbarium of The
Netherlands, Wageningen University Branch for providing access
to herbarium specimens; Carel Jongkind for making leaf samplesavailable for leaf analysis; Cajo ter Braak and Anita van der Kooij
for statistical advice, and Bryan Finegan, Louis Santiago, and an
anonymous reviewer for helpful comments. SKM was supported
by an Erasmus Mundus scholarship and LP by a grant from the
Wageningen graduate school Production Ecology and Resource
Conservation.
LITERATURE CITED
ACKERLY, D. 2004. Functional strategies of chaparral shrubs in relation to sea-sonal water deficit and disturbance. Ecol. Monogr. 74: 25–44.
ACKERLY, D. D., C. A. KNIGHT, S. B. WEISS, K. BARTON, AND K. P. STARMER.2002. Leaf size, specific leaf area and microhabitat distribution of chap-arral woody plants: Contrasting patterns in species level and communitylevel analyses. Oecologia 130: 449–457.
AGYEMAN, V. K., M. D. SWAINE, AND J. THOMPSON. 1999. Responses of tropicalforest tree seedlings to irradiance and the derivation of a light responseindex. J. Ecol. 87: 815–827.
ANTUNEZ, I., E. C. RETAMOSA, AND R. VILLAR. 2001. Relative growth rate inphylogenetically related deciduous and evergreen woody species. Oeco-logia 128: 172–180.
Functional Traits Affect Species Distribution 559
AUGSPURGER, C. K., AND C. K. KELLY. 1984. Pathogen mortality of tropical treeseedlings: Experimental studies of the effects of dispersal distance, seed-ling density, and light conditions. Oecologia 61: 211–217.
BALTZER, J. L., S. J. DAVIES, S. BUNYAVEJCHEWIN, AND N. S. M. NOOR. 2008. Therole of desiccation tolerance in determining tree species distributionsalong the Malay-Thai Peninsula. Funct. Ecol. 22: 221–231.
BARALOTO, C., AND P. M. FORGET. 2007. Seed size, seedling morphology, andresponse to deep shade and damage in neotropical rain forest trees. Am.J. Bot. 94: 901–911.
BATJES, N. H. 1997. A world dataset of derived soil properties byFAO–UNESCO soil unit for global modelling. Soil Use Manage. 13:9–16.
BONGERS, F., L. POORTER, AND W. D. HAWTHORNE. 2004. The forests of upperGuinea: Gradients in large species composition. In L. Poorter, F. Bong-ers, F. N. Kouame, and W. D. Hawthorne (Ed.). Biodiversity of WestAfrican forests: An ecological atlas of woody plant species, pp. 41–52.CABI Publishing, Wallingford, UK.
BONGERS, F., L. POORTER, R. S. A. R. VAN ROMPAEY, AND M. P. E. PARREN. 1999.Distribution of twelve moist forest canopy tree species in Liberia andCote d’Ivoire: Response curves to a climatic gradient. J. Veg. Sci. 10:371–382.
BORCHERT, R. 1994. Soil and stem water storage determine phenology and dis-tribution of tropical dry forest trees. Ecology 75: 1437–1449.
BULLOCK, S. H. 1995. Plant reproduction in neotropical dry forests. In S. H.Bullock, H. A. Mooney, and E. Medina (Ed.). Seasonally dry tropicalforests, pp. 277–303. Cambridge University Press, Cambridge, UK.
CLEMENT, J., AND M. GUINAUDEAU. 1973. Inventaire forestier du Perimetre In-dustriel XV. CTFT, Nogent-sur-Marne, France, 68pp.
COOMES, D. A., AND P. J. GRUBB. 2000. Impacts of root competition in forestsand woodlands: A theoretical framework and review of experiments.Ecol. Monogr. 70: 171–207.
DALLING, J. W., AND S. P. HUBBELL. 2002. Seed size, growth rate and gap mi-crosite conditions as determinants of recruitment success for pioneerspecies. J. Ecol. 90: 557–568.
DAVIES, A. G. 1987. The Gola forest reserves, Sierra Leone. Wildlife conserva-tion and forest management. IUCN, Gland, Switzerland, 130pp.
DIAZ, S., J. G. HODGSON, K. THOMPSON, M. CABIDO, J. H. C. CORNELISSEN,A. JALILI, G. MONTSERRAT-MARTI, J. P. GRIME, F. ZARRINKAMAR, Y. ASRI,S. R. BAND, S. BASCONCELO, P. CASTRO-DIEZ, G. FUNES, B. HAMZEHEE,M. KHOSHNEVI, N. PEREZ-HARGUINDEGUY, M. C. PEREZ-RONTOME,F. A. SHIRVANY, F. VENDRAMINI, S. YAZDANI, R. ABBAS-AZIMI, A. BOG-
AARD, S. BOUSTANI, M. CHARLES, M. DEHGHAN, L. DE TORRES-ESPUNY,V. FALCZUK, J. GUERRERO-CAMPO, A. HYND, G. JONES, E. KOWSARY,F. KAZEMI-SAEED, M. MAESTRO-MARTINEZ, A. ROMO-DIEZ, S. SHAW,B. SIAVASH, P. VILLAR-SALVADOR, AND M. R. ZAK. 2004. The plant traitsthat drive ecosystems: Evidence from three continents. J. Veg. Sci. 15:295–304.
EAMUS, D., AND L. PRIOR. 2001. Ecophysiology of trees of seasonally dry tropics:Comparisons among phenologies. Adv. Ecol. Res. 32: 113–197.
ENGELBRECHT, B. M. J., L. S. COMITA, R. CONDIT, T. A. KURSAR, M. T. TYREE,B. L. TURNER, AND S. P. HUBBELL. 2007. Drought sensitivity shapes spe-cies distribution patterns in tropical forests. Nature 447: 80–82.
ESRI. 1984. Digital chart of the world. US Geological Service, EROS DataCentre, Redlands, California.
FONSECA, C. R., J. M. OVERTON, B. COLLINS, AND M. WESTOBY. 2000. Shifts intrait-combinations along rainfall and phosphorus gradients. J. Ecol. 88:964–977.
GARWOOD, N. C. 1996. Functional morphology of tropical tree seedlings. In M.D. Swaine (Ed.). The ecology of tropical forest tree seedlings, pp.59–129. UNESCO, Paris, France.
GENTRY, A. H. 1982. Patterns of neotropical plant diversity. Evol. Biol. 15:1–84.
GFML. 1967a. Inventory of Grebo national forest. German Forestry Mission toLiberia, Technical report no. 5, Monrovia, Liberia, 54pp.
GFML. 1967b. Inventory of North-Gio, Gio and Gbi national forest. GermanForestry Mission to Liberia, Technical report no. 6, Monrovia, Liberia,45pp.
GIVNISH, T. J. 1988. Adaptation to sun and shade—a whole-plant perspective.Aust. J. Plant Physiol. 15: 63–92.
GIVNISH, T. J. 2002. Adaptive significance of evergreen vs. deciduous leaves:Solving the triple paradox. Silva Fenn. 36: 703–743.
GRIME, J. P. 1974. Vegetation classification by reference to strategies. Nature250: 26–31.
GRIME, J. P. 1977. Evidence for the existence of three primary strategies in plantsand its relevance to ecological and evolutionary theory. Am. Nat. 111:1169–1194.
GRUBB, P. J. 1998. A reassessment of the strategies of plants which cope withshortages of resources. Perspect. Plant Ecol. Evol. Syst. 1: 3–31.
HALL, J. B., AND M. D. SWAINE. 1976. Classification and ecology of closed-canopy forest in Ghana. J. Ecol. 64: 913–951.
HALL, J. B., AND M. D. SWAINE. 1981. Distribution and ecology of vascularplants in a tropical rain forest: Forest vegetation in Ghana. Junk, TheHague, The Netherlands.
HAWTHORNE, W. D. 1995. Ecological profiles of Ghanaian forest trees. ODAtropical forestry papers 29, Oxford Forestry Institute, 345pp.
HAWTHORNE, W. D. 1996. Holes and the sums of parts in Ghanaian forest:Regeneration, scale and sustainable use. Proc. R. Soc. Edinb. 104B:75–176.
HAWTHORNE, W. D., AND M. ABU JUAM. 1995. Forest protection in Ghana.IUCN, Gland, Switzerland, 203pp.
HAWTHORNE, W. D., AND C. C. H. JONGKIND. 2006. Woody plants of WesternAfrican forests: A guide to the forest trees, shrubs and lianes from Sen-egal to Ghana. Royal Botanic Gardens Kew, Kew, UK.
HOLMGREN, M., AND L. POORTER. 2007. Does a ruderal strategy dominate theendemic flora of the West African forests? J. Biogeogr. 34: 1100–1111.
JONGMAN, R. H., C. J. F. TER BRAAK, AND O. F. R. VAN TONGEREN. 1987. Dataanalysis in community and landscape ecology. Pudoc, Wageningen, TheNetherlands.
KEDDY, P. A. 1992. Assembly and response rules—2 goals for predictive com-munity ecology. J. Veg. Sci. 3: 157–164.
KITAJIMA, K. 1992. Relationship between photosynthesis and thickness of coty-ledons for tropical tree species. Funct. Ecol. 6: 582–589.
KURSAR, T. A., B. M. J. ENGELBRECHT, A. BURKE, M. T. TYREE, B. EL OMARI,AND J. P. GIRALDO. 2009. Tolerance to low leaf water status of tropicaltree seedlings is related to drought performance and distribution. Funct.Ecol. 23: 93–102.
LARCHER, W. 1980. Physiological plant ecology (2nd Edition). Springer, Berlin,Heidelberg.
LEISHMAN, M. R., I. J. WRIGHT, A. T. MOLES, AND M. WESTOBY. 2000. Theevolutionary ecology of seed size. In M. Fenner (Ed.). Seeds—the ecol-ogy of regeneration in plant communities (2nd Edition), pp. 31–57.CABI Publishing, Wallingford, UK.
LINTING, M. 2007. Nonparametric inference in nonlinear principal componentsanalysis: Exploration and beyond. Data theory group, department ofeducation, faculty of social and behavioural sciences. Leiden University,Leiden, The Netherlands.
MALHI, Y., AND J. WRIGHT. 2004. Spatial patterns and recent trends in the cli-mate of tropical rainforest regions. Philos. Trans. R. Soc. Lond. B:Biol.Sci. 359: 311–329.
MARKESTEIJN, L., AND L. POORTER. 2009. Seedling root morphology and biomassallocation of 62 tropical tree species in relation to drought- and shade-tolerance. J. Ecol. 97: 311–325.
MARKESTEIJN, L., L. POORTER, H. PAZ, L. SACK, AND F. BONGERS. 2011. Ecolog-ical differentiation in xylem cavitation resistance is associated with stemand leaf structural traits. Plant Cell Environ. 34: 137–148.
MEINZER, F. C., S. A. JAMES, AND G. GOLDSTEIN. 2004. Dynamics of transpira-tion, sap flow and use of stored water in tropical forest canopy trees. TreePhysiol. 24: 901–909.
560 Maharjan, Poorter, Holmgren, Bongers, Wieringa, and Hawthorne
MEINZER, F. C., D. R. WOODRUFF, J. C. DOMEC, G. GOLDSTEIN, P. I. CAMPA-
NELLO, M. G. GATTI, AND R. VILLALOBOS-VEGA. 2008. Coordination ofleaf and stem water transport properties in tropical forest trees.Oecologia 156: 31–41.
MULLER-LANDAU, H. C. 2004. Interspecific and inter-site variation in wood spe-cific gravity of tropical trees. Biotropica 36: 20–32.
MYERS, J. A., AND K. KITAJIMA. 2007. Carbohydrate storage enhances seedlingshade and stress tolerance in a neotropical forest. J. Ecol. 95: 383–395.
NIINEMETS, U. 2001. Global-scale climatic controls of leaf dry mass per area,density, and thickness in trees and shrubs. Ecology 82: 453–469.
NOVOZAMSKY, I., V. J. G. HOUBA, R. VANECK, AND W. VANVARK. 1983. A noveldigestion technique for multi-element plant analysis. Commun. Soil Sci.Plant Anal. 14: 239–248.
PARKER, G., C. TINOCO-OJANGUREN, A. MARTINEZ-YRIZAR, AND M. MAASS.2005. Seasonal balance and vertical pattern of photosynthetically activeradiation within canopies of a tropical dry deciduous forest ecosystem inMexico. J. Trop. Ecol. 21: 283–295.
POORTER, L. 2008. The relationships of wood-, gas- and water fractions of treestems to performance and life history variation in tropical trees. Ann.Bot. 102: 367–375.
POORTER, L. 2009. Leaf traits show different relationships with shade tolerancein moist versus dry tropical forests. New Phytol. 181: 890–900.
POORTER, L., F. BONGERS, AND R. H. M. J. LEMMENS. 2004. West African forests:Introduction. In L. Poorter, F. Bongers, F. N. Kouame, and W. D.Hawthorne (Ed.). Biodiversity of West African forests: An ecological at-las of woody plant species, pp. 5–14. CABI Publishing, Wallingford,UK.
POORTER, L., AND L. MARKESTEIJN. 2008. Seedling traits determine drought tol-erance of tropical tree species. Biotropica 40: 321–331.
PRATT, R. B., A. L. JACOBSEN, F. W. EWERS, AND S. D. DAVIS. 2007. Relation-ships among xylem transport, biomechanics and storage in stems androots of nine Rhamnaceae species of the California chaparral. NewPhytol. 174: 787–798.
REICH, P. B., I. J. WRIGHT, J. CAVENDER-BARES, J. M. CRAINE, J. OLEKSYN, M.WESTOBY, AND M. B. WALTERS. 2003. The evolution of plant functionalvariation: Traits, spectra, and strategies. Int. J. Plant Sci. 164:S143–S164.
RUIZ-ROBLETO, J., AND R. VILLAR. 2005. Relative growth rate and biomass allo-cation in ten woody species with different leaf longevity using phyloge-netic independent contrasts (PICs). Plant Biol. 7: 484–494.
SACHTLER, M. 1968. General report on national forest inventory in Liberia.German Forestry Mission to Liberia, Technical report no. 1, Monrovia,Liberia, 148pp.
SACHTLER, M., AND K. HAMER. 1967a. Inventory of Krahn-Bassa and Sapo na-tional forest. German Forestry Mission to Liberia, Technical report no.7, Monrovia, Liberia, 92pp.
SACHTLER, M., AND K. HAMER. 1967b. Reconnaissance of the national forests inNorthwest Liberia. Pilot inventory in the Lamco-concession on MountNimba. German Forestry Mission to Liberia, Technical report no. 9,Monrovia, Liberia, 38pp.
SANTIAGO, L. S., K. KITAJIMA, S. J. WRIGHT, AND S. S. MULKEY. 2004. Coordi-nated changes in photosynthesis, water relations and leaf nutritionaltraits of canopy trees along a precipitation gradient in lowland tropicalforest. Oecologia 139: 495–502.
SAVILL, P. S., AND J. E. D. FOX. 1967. Trees of Sierra Leone, Unpublished MS,O.F.I. library, Oxford
SEARSON, M. J., D. S. THOMAS, K. D. MONTAGU, AND J. P. CONROY. 2004.Wood density and anatomy of water-limited eucalypts. Tree Physiol. 24:1295–1302.
SIEPEL, A., L. POORTER, AND W. D. HAWTHORNE. 2004. Ecological profiles oflarge timber species. In L. Poorter, F. Bongers, F. N. Kouame, and W.D. Hawthorne (Ed.). Biodiversity of West African forests: An ecologicalatlas of woody plant species, pp. 391–445. CABI Publishing, Walling-ford, UK.
SMALL, D. 1953. Some ecological and vegetational studies in the Gola ForestReserve, S.E. Province, Sierra Leone. Unpublished MSc thesis, Queen’sUniversity, Belfast.
SMITH, T., AND M. HUSTON. 1989. A theory of the spatial and temporal dynam-ics of plant communities. Plant Ecol. 83: 49–69.
SODEFOR. 1978. Inventaire forestier national. Resultats de la region centre-sud. Abidjan, Cote d’Ivoire, SODEFOR.
SODEFOR. 1979. Inventaire forestier national. Resultats de la region nord-ouest. Abidjan, Cote d’Ivoire, SODEFOR.
SWAINE, M. D. 1996. Rainfall and soil fertility as factors limiting forest speciesdistributions in Ghana. J. Ecol. 84: 419–428.
TER STEEGE, H., N. C. A. PITMAN, O. L. PHILLIPS, J. CHAVE, D. SABATIER, A.DUQUE, J. F. MOLINO, M. F. PREVOST, R. SPICHIGER, H. CASTELLANOS, P.VON HILDEBRAND, AND R. VASQUEZ. 2006. Continental-scale patterns ofcanopy tree composition and function across Amazonia. Nature 443:444–447.
THUILLER, W., S. LAVOREL, G. MIDGLEY, S. LAVERGNE, AND T. REBELO. 2004.Relating plant traits and species distributions along bioclimatic gradientsfor 88 Leucadendron taxa. Ecology 85: 1688–1699.
TOLEDO, M., L. POORTER, M. PENA-CLAROS, A. ALARCON, J. BALCAZAR,J. CHUVINA, C. LEANO, J. C. LICONA, H. TER STEEGE, AND F. BONGERS.2011. Patterns and determinants of floristic variation across lowlandforests of Bolivia. Biotropica, (in press).
VAN DER KOOIJ, A. J. 2007. Prediction accuracy and stability of regression withoptimal scaling transformations. Child & Family Studies and Data The-ory (AGP-D), Department of Education and Child Studies, Faculty ofSocial and Behavioural Sciences, Leiden University, Leiden.
VAN GELDER, H. A., L. POORTER, AND F. J. STERCK. 2006. Wood mechanics,allometry, and life-history variation in a tropical rain forest tree com-munity. New Phytol. 171: 367–378.
VEENENDAAL, E. M., M. D. SWAINE, R. T. LECHA, M. F. WALSH, I. K. ABEBRESE,AND K. OWUSUAFRIYIE. 1996. Responses of West African forest treeseedlings to irradiance and soil fertility. Funct. Ecol. 10: 501–511.
WALTERS, M. B., AND P. B. REICH. 1999. Low-light carbon balance and shadetolerance in the seedlings of woody plants: Do winter deciduous andbroad-leaved evergreen species differ? New Phytol. 143: 143–154.
WESTOBY, M. 1998. A leaf-height-seed (LHS) plant ecology strategy scheme.Plant Soil 199: 213–227.
WONG, J. 1989. Ghana forest inventory proceedings, Accra, 29–30 March 1989,Ghana Forestry Department and UK Overseas Development Adminis-tration, London.
WRIGHT, I. J., P. B. REICH, AND M. WESTOBY. 2001. Strategy shifts in leaf phys-iology, structure and nutrient content between species of high- and low-rainfall and high- and low-nutrient habitats. Funct. Ecol. 15: 423–434.
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