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Growth of native tree species planted in montane reforestation projects in the Colombian and Ecuadorian Andes differs among site and species Matthew C. Bare 1 Mark S. Ashton 1 Received: 9 April 2015 / Accepted: 28 October 2015 Ó Springer Science+Business Media Dordrecht 2015 Abstract The tropical Andes in Ecuador and Colombia are a biodiversity hotspot that has endured centuries of forest clearance and degradation. Forest restoration has been identi- fied as a regional conservation priority; in recent decades, native species reforestation projects have proliferated, but little information exists on growth performance of com- monly planted tree species in relation to site and soil nutrient status. This study analyzed growth of seven common native species (Alnus acuminata, Baccharis bogotensis, Cedrela montana, Myrica pubesens, Quercus humboltii, Sambucus nigra, Smallanthus pyramidalis) on 12 montane forest sites across the northern region of the tropical Andes. Andean alder (A. acuminata) was the most commonly planted species, and grows at a mean annual diameter increment (MAI-d) of 1.81 cm y -1 and a mean annual height increment (MAI-h) of 0.95 m y -1 . S. pyramidalis, a short lived pioneer of the Asteraceae family, also exhibited fast growth rates of 1.64 cm MAI-d and 1.21 m MAI-h. Andean oak (Q. hum- boltii) was the second-most commonly planted species, growing with an MAI-d of 0.99 cm and MAI-h of 0.56 m. Soil magnesium and potassium were significant predictors of MAI-d and MAI-h for A. acuminata, while soil nitrogen, phosphorous, sodium, and calcium were negatively associated with growth (p \ .001). We speculate that A. acuminata did not grow as well on soils richer in calcium and phosphorus because they were less conducive to nitrogen symbiosis common to this species. Soil magnesium and calcium were signif- icant predictors (p \ .05) of diameter growth for Q. humboltii. For both species, we attribute growth responses to soil nutrients as a result of the variable nature of fertility in the complex and variable soils that make up the volcanic and surficial geological landscape of the northern Andes. Results indicate that native species can grow in a variety of soil conditions, and exhibit growth rates comparable to non-native species. However, our results suggest native species are site restricted for best growth and should be planted on particular soils. We make recommendations for reforestation for the species in this study. & Matthew C. Bare [email protected] 1 Yale School of Forestry and Environmental Studies, 360 Prospect Street, New Haven, CT 06511, USA 123 New Forests DOI 10.1007/s11056-015-9519-z

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Growth of native tree species planted in montanereforestation projects in the Colombian and EcuadorianAndes differs among site and species

Matthew C. Bare1 • Mark S. Ashton1

Received: 9 April 2015 / Accepted: 28 October 2015� Springer Science+Business Media Dordrecht 2015

Abstract The tropical Andes in Ecuador and Colombia are a biodiversity hotspot that has

endured centuries of forest clearance and degradation. Forest restoration has been identi-

fied as a regional conservation priority; in recent decades, native species reforestation

projects have proliferated, but little information exists on growth performance of com-

monly planted tree species in relation to site and soil nutrient status. This study analyzed

growth of seven common native species (Alnus acuminata, Baccharis bogotensis, Cedrela

montana,Myrica pubesens, Quercus humboltii, Sambucus nigra, Smallanthus pyramidalis)

on 12 montane forest sites across the northern region of the tropical Andes. Andean alder

(A. acuminata) was the most commonly planted species, and grows at a mean annual

diameter increment (MAI-d) of 1.81 cm y-1 and a mean annual height increment (MAI-h)

of 0.95 m y-1. S. pyramidalis, a short lived pioneer of the Asteraceae family, also

exhibited fast growth rates of 1.64 cm MAI-d and 1.21 m MAI-h. Andean oak (Q. hum-

boltii) was the second-most commonly planted species, growing with an MAI-d of 0.99 cm

and MAI-h of 0.56 m. Soil magnesium and potassium were significant predictors of MAI-d

and MAI-h for A. acuminata, while soil nitrogen, phosphorous, sodium, and calcium were

negatively associated with growth (p\ .001). We speculate that A. acuminata did not

grow as well on soils richer in calcium and phosphorus because they were less conducive

to nitrogen symbiosis common to this species. Soil magnesium and calcium were signif-

icant predictors (p\ .05) of diameter growth for Q. humboltii. For both species, we

attribute growth responses to soil nutrients as a result of the variable nature of fertility in

the complex and variable soils that make up the volcanic and surficial geological landscape

of the northern Andes. Results indicate that native species can grow in a variety of soil

conditions, and exhibit growth rates comparable to non-native species. However, our

results suggest native species are site restricted for best growth and should be planted on

particular soils. We make recommendations for reforestation for the species in this study.

& Matthew C. [email protected]

1 Yale School of Forestry and Environmental Studies, 360 Prospect Street, New Haven, CT 06511,USA

123

New ForestsDOI 10.1007/s11056-015-9519-z

Keywords Restoration � Tropical Andes � Growth rates � Alnus acuminata � Quercushumboltii � Nitrogen fixation � Smallanthus pyramidalis � Soil fertility

Introduction

Worldwide, the area of degraded forest and abandoned agricultural land is growing, and

both passive and active forms of restoration have the potential to conserve biodiversity,

stabilize eroded landscapes, and sequester carbon (Silver et al. 2000). Across the tropics,

large areas of abandoned and marginal agricultural land have potential for establishment of

second-growth forest (Chazdon 2008), and restoration through enrichment planting (Millet

et al. 2013) or native tree plantations (Wishnie et al. 2007; Lamb 2011; Rodrigues et al.

2011). Such restoration activities can facilitate forest recovery and augment forest tree

diversity (Parrotta et al. 1997; Holl et al. 2000; Ashton et al. 2001; Lamb et al. 2005).

The tropical Andes biodiversity hotspot, stretching from Venezuela to Chile, is an

important ecological region with great potential for forest restoration (Conservation

International 2014). Within the tropical Andes, the northern Andean montane forests of

Colombia and Ecuador (Dinerstein et al. 1995) hold high rates of species richness and

endemism (Gentry 1992), but have lost significant areas of natural forest (Etter et al. 2008).

However, many areas of the northern montane forest are experiencing forest regrowth:

between 2000 and 2010, Colombia gained approximately 23,773 square kilometers of forest

and Ecuador 5867 square kilometers, both largely in the montane regions (Aide et al. 2013).

Worldwide studies find that approximately an equal amount of forest area is undergoing

reforestation or natural regrowth as is being deforested (200,000–300,000 km2 y-1), and

that much of the regrowth area is in hilly and mountainous regions on marginal soils and

steep slopes such as in the tropical Andes (Asner et al. 2009).

Within the northern Andean montane forest, conservation of native forest fragments and

forest restoration are conservation priorities (Conservation Internacional Colombia 2014).

Fragments and native tree plantings in these forests are found to be an important source of

plant and bird biodiversity (Kattan et al. 1994; Murcia 1997; Gilroy et al. 2014). One

commonly planted montane tree is Andean alder (Alnus acuminata Kunth.), a fast growing

nitrogen-fixing tree, useful for soil enrichment in silvo-pastoral systems. A comparison of a

native A. acuminata plantation with natural forest regeneration in the Colombian Andes

found that A. acuminata plantings are taller than natural forest re-growth with a similar

basal area, although natural forest regrowth had higher total plant richness (Murcia 1997).

Studies in southern Ecuador have found that A. acuminata can achieve fast growth rates,

even greater than exotics such as Eucalyptus saligna and Pinus patula, especially in gaps

(Weber et al. 2008; Gunter et al. 2009).

Despite the importance of forest restoration in the northern Andes, few studies exist on

the growth rates of common native species in diverse sites. Most research examines the

growth of A. acuminata (Cornelius et al. 1996; Rıos et al. 2004; Medina et al. 2008; Weber

et al. 2008; Gunter et al. 2009); these studies test the growth of A. acuminiata of different

seed provenances, or different strains and application methods of the nitrogen-fixing

Frankia bacteria associated with Alnus. In southern Ecuador, a few studies have evaluated

the growth of other native species such as Heliocarpus americanus, Piptocoma discolor,

Cedrela montana, and Juglans neotropica in experimental plots; these studies find that

native early successional trees such as A. acuminiata, H. americanus, and P. discolor grow

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fast in planted sites (Weber et al. 2008; Gunter et al. 2009). These studies have also found

that seed selection, provenance, and quality are important determinants of planting success,

in addition to silvicultural treatments such as weed control (Stimm et al. 2008; Weber et al.

2008). In this site, Wilcke et al. (2008a) showed that tree growth is also affected by soil

fertility, altitude, and land use history; studies in other tropical montane ecosystems make

similar conclusions (Grubb 1977; Bautista-Cruz and del Castillo 2005). In the Neotropics

more generally, numerous studies have measured growth rates of commonly planted

lowland trees (Worbes 1999 in Venezuela; Hooper et al. 2002, Griscom et al. 2005, and

Wishnie et al. 2007 in Panama; and Haggar et al. 1997 and Piotto et al. 2003 in Costa

Rica). Elsewhere in the tropics, studies have shown that selected native species can achieve

growth rates comparable or superior to those of fast growing exotics (McNamara et al.

2006; Schneider et al. 2014).

Nevertheless, although a few studies provide information on growth of selected species

in experimental conditions, growth data from a wider range of field conditions and soil

nutrient concentrations is necessary for a better understanding of commonly planted spe-

cies in the northern Andes. In the tropics generally, old and lowland tropical soils are P

limited whereas young, highland tropical soils are more likely to be N limited (Vitousek

and Farrington 1997; Davidson et al. 2004). In the northern Andes, however, soil condi-

tions are highly variable, often a result of volcanic activity and landslides (Bussmann et al.

2008; Wilcke et al. 2008b). There is very little grey literature and no published data on

many tree species that have been more recently planted, such as Smallanthus pyramidalis

Triana., a fast growing Asteraceae tree commonly used for erosion control and live fences.

Another important tree of montane forest, both ecologically and for timber, is Andean oak

(Quercus humboltii Bonpl.). This tree is found in Panama, Venezuela, Colombia, and

Ecuador, and dominates montane forest across much of its range in Colombia (Leon et al.

2009), but few published data are available on its growth rates and soil affinities.

Restoration practice is growing in the tropical Andes, especially in Colombia and

Ecuador (Murcia et al. 2015). State ministries have directed large-scale reforestation

projects with exotic timbers since the middle twentieth century, and since the 1990s, non-

governmental organizations, international donors, and research institutions have become

engaged in numerous small projects focused on ecological restoration (CESA-Intercoop-eration Suiza 1992; Endo 1994; Meza et al. 2006; Andrade-Perez 2007; Farley 2007). Most

recently, private sector financing has become more available for restoration via payments

for watershed services, climate change mitigation, and mining offsets (Bare 2014).

However, while many agencies publish general guides, little specific data are available on

native tree plantings.

Colombia has recently prepared a national plan for restoration (Ospina Arango and

Vanegas Pinzon 2010), largely based on the Society for Ecological Restoration primer

(Society for Ecological Restoration 2004). This plan describes restoration of forest

ecosystems with goals of providing habitat connectivity, biodiversity, and ecosystem

functions like water provision, however, it offers little guidance on species selection and

background of established field projects in Colombia. In Ecuador, detailed information

exists about a study site in the southern Andes, but little information is available about

plantings elsewhere in the country.

The first objective of our study was to build on what little has been published and to

evaluate the growth performance of a range of native tree species planted in forest

restoration projects in the northern Andean montane forests. Our second objective is to

compare growth of the most commonly selected tree species in relation to soil nutrition on

reforestation sites.

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Methods

Study area

Sites were located in the montane forest of the northern region of the Tropical Andes,

which covers approximately 423,000 km2 (Dinerstein et al. 1995) (Fig. 1). The montane

forest is normally described as being from an elevation of around 1000 to 3200–3500 m,

where the forest transitions into high altitude grassland known as paramo (Hammen 1974;

Armenteras et al. 2003). In fact, some researchers describe the upper montane—paramo

boundary as human influenced (Sarmiento and Frolich 2002; Bakker et al. 2008). Lower

montane forests have an average annual temperature between 19 and 23 �C with an annual

precipitation ranging between 1500 and 1700mm. Upper montane forests have an average

annual temperature between 9 and 16 �C, with an annual precipitation between 700 mm in

dry inter-Andean valleys to 3000 mm on slopes of the wetter Pacific-side (Olson et al.

Fig. 1 Map depicting study sites in Colombia and Ecuador

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1995). Vegetation changes rapidly along the altitudinal gradient. Lower elevation forests

are dominated by palms (Arecaceae), and the angiospermous families Melastomataceae,

Lauraceae, Rubiaceae, Malvaceae, and Fabeaceae. Higher elevation forests transition to

Myricaceae, Fagaceae, Clusiaceae, Ericaceae, and Asteraceae, while palms and Melas-

tomataceae remain common (Armenteras et al. 2003; Homeier et al. 2008). Much of the

higher montane forest on wet slopes in Colombia is dominated by Andean oak (Q. hum-

boltii) (Leon et al. 2009). Higher elevation forests have lower total species richness but

normally higher rates of endemism, particularly among vascular epiphytes (Gentry 1992).

Most of the northern Andes as a whole are volcanic ash derived soils (Andisols). These

soils typically display high amounts of soil carbon, dense networks of micropores, high

water retention, and low bulk density (Tonneijck et al. 2010). Aluminum–humus com-

plexes are common in acidic soils (Zehetner et al. 2003). Other areas in the Andes shaped

by erosion and landslides or that were not derived from volcanic ash deposits are classified

as Entisols or Inceptisols (Cambisols) (Wilcke et al. 2008b). Throughout much of the

northern Andes, landslides are common and play a significant role in the soil heterogeneity

and shaping forest vegetation (Bussmann et al. 2008).

The northern Andean montane ecosystem is the most densely settled area of Ecuador

and Colombia, and agriculture has been the primary driver of land use change over the past

several centuries (Sarmiento and Frolich 2002; Etter et al. 2008). In Colombia, approxi-

mately 75 % of the population lives in the Andean region; in Ecuador it is approximately

50 % (Colombia Censo General 2005; Ecuador en Cifras Resultados 2015). Land use

activity in the higher areas is most often associated with potato cultivation, and coffee and

fruit trees in the lower lying areas, although cattle pasture is common throughout the region

and is replacing some agricultural crops (Etter et al. 2006; Guhl 2008). Coffee cultivation

is focused on areas of better access and soil fertility, whereas cattle pasture and estab-

lishment of natural second-growth is more likely to occur on less fertile soils and on steep,

remote mountain areas (Etter et al. 2006; Asner et al. 2009; Aide et al. 2013). Across the

region, forest fragments are spread throughout the agricultural landscape (Etter et al. 2006;

Murgueitio et al. 2011; Lerner et al. 2014). Mining is practiced throughout the region, but

is a minor driver of forest clearing compared to agriculture (Etter et al. 2008).

While most forest clearing in the Andean montane ecosystem occurred over the past

centuries, some clearing continues today. In Colombia nationwide, Hansen et al. (2013)

calculate a rate of forest loss of 3.0 % from 2000 to 2012 or an average annual loss of

0.25 % (in the forest cover[25 % threshold). The areas with highest amounts of forest loss

were the departments of Caqueta, Meta, and Antioquia; all located primarily in montane—

lowland forest transition zones of the Andes. In Ecuador, Hansen et al. (2013) calculate a

2.7 % forest loss from 2000 to 2012 or 0.23 % average annual rate of forest cover loss. The

areas with the highest amounts of forest loss were the lowland Amazon and coastal regions,

although other studies find high continued rates of forest loss in montane regions of

southern Ecuador (Tapia-Armijos et al. 2015).

Site selection

Our study sites were focused on projects with a native forest restoration goal. Timber

plantations using exotic trees were excluded. Forest restoration projects were identified

using expert interviews and internet search, followed up with interviews with key infor-

mants. Project managers from various sectors (academic, government, NGO) were con-

tacted for background information, project reports, and interviews. Seventy projects,

primarily in the montane region of the two countries, were identified and catalogued.

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Project data was triangulated when possible using written reports, interviews with project

managers, and third party interviews with other restoration practitioners in the region.

Of seventy projects catalogued as the most promising based on our initial survey and

interviews, sixteen were selected for field visits and data collection. These sites were

selected because they had an implementation record of [5 years (established prior to

2008), availability of information about date of planting and species planted, and a basic

record of site protection (not necessarily maintenance of the planted trees, but merely

protection of the site from fire or re-conversion to pasture or agriculture). Of the 16 sites

where data were collected, four were discarded after site survey because of site aban-

donment or unclear planting data; the remaining 12 were finally used for data analysis. The

goals of these restoration projects were for a mix of purposes including scientific research,

conservation and landscape connectivity, watershed protection, and agroforestry (live

fences, nutrient retention). Most sites were fenced to prevent cattle grazing, but not fer-

tilized and only minimally weeded (see Appendix 1 for complete site details and

objectives).

Sampling design

Because sites were derived from a variety of sources, planting design and species varied

greatly. In the study sites, trees varied between 5 and 15 years of age and were spaced

between 2 and 5 m. Study sites were grouped into large ([2 ha) and small (\2 ha). Small

sites were sampled via census (all trees were measured); in large sites, three line transects

crossing the entirety of the planting site (50–500 m) were selected randomly, and all trees

within 5 m of the center line were measured. In all sites, planted trees with height greater

than diameter at breast height (dbh) (1.3 m) were identified to species, measured for dbh,

and ocular estimates of tree canopy height made to the nearest half meter, using a survey

rod for calibration. Data was collected in 2013 (see Appendix 1 for details).

Soil samples were collected from 3 to 5 random locations at each restoration site;

approximately 100 g were collected from the A horizon, approximately 2–4 cm below the

mineral soil surface. Composite samples from each site were analyzed in the field for

texture and then air dried and shipped to the U.S. for chemical analysis. Air-dried samples

were analyzed for pH at the Yale School of Forestry and Environmental Studies soil

laboratory (Greeley Memorial Laboratory). Soil carbon, organic matter, cation exchange

capacity, and additional nutrients (N, P, K, Na, Mg, and Ca) were analyzed at the

University of Georgia Department of Crop and Soil Sciences Lab for Environmental

Analysis. Dissolved carbon was determined using a Shimadzu TOC-5050A Total Organic

Carbon Analyzer. Analysis was based on loss of ignition (David 1988). All other elements

were determined by spectrophotometric methods and ion chromatography using a DIO-

NEX DX500 modular system (University of Georgia University of Georgia Laboratory for

Environmental Analysis 2015).

Data analysis

Based on the data gathered, a total of seven species were identified for data anlysis: A.

acuminata Kunth. (Betulaceae, known locally as aliso, or Andean alder in English), B.

bogotensis Kunth. (Asteraceae, known locally as chilco), C. montana Moritz ex Turcz.

(Meliaceae, known locally as cedro de montana), Myrica pubesens Humb. & Bonpl. ex

Willd. (Myricaceae, known locally as laurel de cera), Q. humboltii Bonpl. (Fagaceae,

known locally as roble, or Andean oak in English), S. nigra L. (Adoxaceae, known in

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English as elderberry, native to Europe), and S. pyramidalis Triana. (Asteraceae, known

locally as arboloco). Mean annual increment for height and diameter were calculated by

taking measurements in 2013 and averaging growth over the age of the tree. Two-way

analysis of variance (ANOVA) was performed to test significance of species, site, and

interaction effects on mean annual increments of diameters and height (MAI-d, MAI-h) of

the seven common species in the study. Mean annual increments were compared among

sites and among species for statistical significance using a Tukey test. Multiple regression

analysis (backwards stepwise, Minitab 16) was used on soil nutrient variables for the MAI-

d and MAI-h of the two most commonly found trees, A. acuminata and Q. humboltii. Soil

texture, pH, organic matter, soil carbon, cation exchange capacity, aluminum, and site

elevation showed no significant effects and were removed from further analysis. Sampling

design and data analysis draw significantly on a similar study conducted by (Schneider

et al. 2014).

Results

A total of 802 trees were measured of 45 different species. Statistics were calculated on

the seven species most commonly found across the 12 sites. A. acuminata was by far the

most commonly planted species, being a popular restoration tree for its fast growth and

nitrogen-fixing ability. A. acuminata represented 44 % of all trees sampled across

reforestation sites, planted at seven sites. Q. humboltii was found at four sites and S.

pyramidalis, a fast-growing, short-lived Asteraceae tree common to disturbed areas, was

found at three sites. Mid-successional timber trees such as C. montana, Tabebuia rosea

(Bignoniaceae), J. neotropica (Juglandaceae), and Podocarpus spp. (Podocarpaceae)

were planted at several sites, but many individuals of these species had died due to

intense competition with pasture grass (see Appendix 2 for a partial list of species

planted).

Growth rates between species were significantly different, as were growth rates between

sites (Table 1). The interaction effect between site and species was significant, indicating

that species differed in their growth rates and changed ranking in relation to each other

across the different restoration sites and soils. Tukey studentized t test comparisons of

growth rates among species revealed A. acuminata had the greatest diameter growth,

averaging 1.81 cm y-1, along with S. pyramidalis at 1.63 cm y-1 (Fig. 2). Growth was

significantly greater in these two species compared to all other species measured except C.

Table 1 Two-way ANOVA of mean annual increment for diameter (cm) and height (m) by sites, speciesand interaction between sites and species

Source N df Mean SD F p R2 (adj)

MAI-d (cm)

Site 12 11 1.40 0.47 5.303 \.0001 .553

Species 7 6 1.21 0.41 4.094 .001

Site 9 species 17 2.944 .001

MAI-h (m)

Site 12 11 0.82 0.26 5.368 \.0001 .573

Species 7 6 0.71 0.32 8.504 \.0001

Site 9 species 17 7.357 \.0001

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montana. C. montana showed a wide range of growth rates perhaps because of a small

sample size or its inherent variability in growth and site establishment. B. bogotensis, S.

nigra, and Myrica pubenscens are all small spreading trees and exhibited moderate to slow

diameter growth but high rates of canopy spread.

Smallanthus pyramidalis showed the highest mean annual increment for height at

1.21 m y-1, which was significantly greater than all other species (Fig. 2). A. acuminata

averaged 0.95 m y-1, not statistically different from B. bogotensis and C. montana, but

statistically different from the 0.56 m y-1 average height growth of Q. humboltii.

Two high elevation pasture sites exhibited the greatest MAI of diameter and height,

largely because these sites are dominated by fast-growing A. acuminata (Fig. 3). Reasons

for slow growth rates in certain sites include species selection and land use history; the

slowest growing site was a previous mine site, and the second-slowest site was a 16-year

monodominant plantation of Q. humboltii.

Regression analysis of A. acuminata and Q. humboltii, the two species found at more

than three sites, showed that diameter and height growth varied significantly in relation

to soil fertility (Table 2). Diameter of A. acuminata was positively correlated with

magnesium and potassium, and negatively correlated with nitrogen, sodium, phospho-

rous, and calcium. Q. humboltii diameter growth was positively correlated with mag-

nesium and calcium, but height was positively correlated with only magnesium. Soil

nutrients explained between 34.18 and 44.60 % of the variation in growth rates for the

two species.

Fig. 2 Mean annual increment of seven commonly planted species recorded. Gray bars show diametergrowth (mean annual increment) and hatched bars show height growth (mean annual increment). Error barsdepict standard errors. Letters indicate Tukey grouping: species that do not share a letter are significantlydifferent, for example, mean diameter increment in A. acuminata is statistically significantly different fromB. bogotensis but not from S. pyramidalis. See Appendix 2 for average mean annual increment of otherspecies measured

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Discussion

Growth of native species

Compared with other studies of A. acuminata, average diameter growth across the present

sites in Ecuador and Colombia was about average (1.81 cm y-1) compared to that reported

for other studies elsewhere in the northern Andes and Costa Rica (e.g. 0.90–2.96 cm y-1;

Table 3). Many of these studies tested different provenances or experimental Frankia

bacteria inoculation treatments; most collected mean annual increment measurements

systematically over the first 6–24 months of plant growth as compared to this study that

evaluated much older plantings but inferred growth from time since planting. However, A.

Fig. 3 Mean annual increment of planted species at various restoration sites. Gray bars show diametergrowth (mean annual increment) and hatched bars show height growth (mean annual increment). Error barsdepict standard errors. See Appendix 1 for full site description

Table 2 Significant predictors of mean annual increment of diameter (MAI-d) and mean annual incrementof height (MAI-h) in two species found at more than three sites

Species Degreesoffreedom

Regression coefficient

N Na Mg P K Ca R2

adj

MAI-d

A. acuminata 6 -1.6** -.045** 0.003** -0.093** 0.002** -0.001** 44.6

Q. humboltii 3 ns ns 0.001* ns ns 0.0002* 34.18

MAI-h

A. acuminata 6 -0.624** ns 0.001** -0.039** 0.001** -0.0003** 37.93

Q. humboltii 3 ns ns 0.001** ns ns ns 44.14

Significance levels ** p\ .001; * p\ .05

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123

acuminata growth in our study was comparable to growth of other commonly planted

native and exotic plantation species in the Andean region (Table 3), see also (Gunter et al.

2009).

Quercus humboltii averaged faster diameter growth compared to the literature

(Table 3), but the only literature available was from secondary forest with strong com-

petition from other species, not a plantation where trees are purposefully spaced to provide

open growing space. S. pyramidalis showed similar rapid growth, but is short lived and less

valued for timber.

Table 3 Growth rates of A. acuminata and Q. humboltii in various restoration sites and trials in theTropical Andes and montane Neotropics, compared with exotics A. decurrens and P. patula. Measurementsfrom this study are in bold

Species Location Treatment Diametergrowth(cm)

Method Source

A. decurrens Colombia(Caldas)

No treatment 1.83 During 15 months Quiceno andMedina (2006)

A. decurrens Colombia(Antioquia)

None .051 During 1 year Medina et al.(2008)

A. acuminata Colombia(Caldas)

No treatment 3.28 Daily growth during afew monthsextrapolated to year

Rıos et al.(2004)

A. acuminata 1780 mCosta Rica

Plantation 2.96 Averaged over the lifeof 9 years

Roque et al.2009

A. acuminata TurrialbaCosta Rica

Plantation 2.00 Over 40 months Cornelius et al.(1996)

A. acuminata** NorthernAndes(various)

Various 1.81 Averaged over the lifeof several years

Present study

A. acuminata Colombia(Jardin,Antiq)

Rhizosphericorganisms

1.64 Average of 6treatments during16 weeks

Molina et al.(2008)

A. acuminata Colombia(Antioquia)

Rhizosphericorganisms

1.31 During 1 year Medina et al.(2008)

A. acuminata Ecuador(Loja)

Shade 1.13 During 24 months Aguirre andWeber (2007),unpublished

A. acuminata Colombia(Antioquia)

None 0.88 During 1 year Medina et al.(2008)

Quercushumboldtii**

Colombia (4sites)

Plantation 0.99 Averaged over the lifeof several years

Present study

Quercushumboldtii

Colombia 16 yearsecondaryforest

0.58 Averaged over the lifeof several years

Becerra (1989)

Quercushumboldtii

Colombia 2nd forest 0.21 Averaged over the lifeof several years

Leon et al.(2009)

P. patula Colombia 4.5 yearplantation

2.11 During 3.5 years Endo and Mesa(1992)

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Soil nutrients

Regressions showed A. acuminata diameter and height growth was positively correlated

with magnesium and potassium concentrations and negatively correlated with nitrogen,

sodium, phosphorous, and calcium. Interestingly, our study suggests that magnesium and

calcium are strong positive and negative predictors respectively of tree growth for the two

species tested. This may be related to the large difference in fertility of northern Andean

soils of volcanic (often fertile, high pH, high cation exchange capacity, high calcium) and

non-volcanic glacial origin (often low fertility, low pH, low cation exchange capacity, low

calcium). In particular, the nitrogen fixing species A. acuminata did not grow as well on

soils richer in calcium and phosphorus (we suggest these soils are Andisols), perhaps

because they were less conducive to nitrogen symbiosis. We speculate that species growth

could also be negatively affected by other interacting site factors that we did not measure

such as wind, animal browse, site treatment (use of herbicides, weeding) or soil moisture

availability. In this study, sites practicing silvo-pastoral management protected planted

trees with fencing, but animal browsing still could have occurred from smaller native

herbivores.

The finding that A. acuminata is negatively associated with soil nitrogen is interesting,

as it is a nitrogen-fixing tree. In sites with dense stands of A. acuminata, one would expect

higher growth to correspond with higher soil nitrogen, not necessarily because the tree

responds to nitrogen fertility but because the tree enriches the soil with N fixation and

litterfall. However, it is also possible that A. acuminata grows slower in high nitrogen sites

because its association with nitrogen-fixing bacteria is absent (the symbiotic relation is not

necessary) and because of greater competition with grass and other surrounding nitrogen-

demanding vegetation, particularly when sites are not maintained (Davidson et al. 2004).

A. acuminata is also ectomycorrhizal, suggesting that it can grow well in low-nutrient

environments (Becerra et al. 2005). Similarly, a study of Alnus nepalensis in India found

that seedlings with mycorrhizal fungi grew slower in conditions of higher soil fertility (Jha

et al. 1993).

Quercus humboltii diameter growth was positively correlated with increased amounts of

soil magnesium and calcium. Height growth was correlated with magnesium. Again, like

Alnus, Quercus is an ectomycorrhizal genus. Other studies have shown that the symbiotic

plant-fungal relationship makes Quercus more nutrient-use efficient, particularly for

phosphorous and magnesium (Lehto and Zwiazek 2011; Simard et al. 2003). Other studies

have found that ectomycorrhizal presence is a stronger predictor of tree growth than soil

fertility (Zangaro et al. 2007), suggesting that parameters other than soil fertility (e.g. soil

water availability) could explain the growth of these species. Lastly, studies in the Andes

found that soil texture was an important predictor of plantation tree growth, specifically,

that trees grew better in clay loam (Henri 2001); while eroded soil significantly reduces

growth (Carpenter et al. 2004). In this study, soil texture was not correlated with growth of

planted species.

Finally, it is important to note that the height and diameter growth measured in this

study represents only one form of plant response to soil fertility. Growth allocation above-

and below-ground can differ among species. Early-successional species in fertile envi-

ronments usually allocate growth to above-ground biomass, whereas mid and late-suc-

cessional species often allocate more growth below-ground, especially in nutrient poor and

drought-stressed soils (Poorter 2001; Zangaro et al. 2007). In this study, elevation was not

found to be a significant predictor of tree growth, possibly because elevation effects were

New Forests

123

modified by species selection or site history. Some low elevation sites were slow growing

because they contained mid-successional trees instead of fast growing pioneers (sites 4 and

6 in Appendix 1), while some high elevation sites were fast growing because they con-

tained fast growing A. acuminata (sites 8 and 9 in Appendix 1). Moreover, many low and

mid-elevation sites suffered a more intense land use history with greater erosion (sites 1, 2,

4, 10, and 12), whereas the high elevation sites experienced a lighter land use history of

low intensity pasture. Finally, an additional factor not evaluated in this study is the effect

of seed provenance and quality, as well as silvicultural treatments after planting, factors

which have been found to influence tree survival and growth (Stimm et al. 2008; Weber

et al. 2008).

Management applications

Not surprisingly, mid-successional species such as Q. humobltii and C. montana showed

slower diameter and height growth than pioneer species A. acuminata and S. pyramiadlis.

In this study, C. montana exhibited slow growth but with significant variability; other

studies that monitored plantings of the related Cedrela odorata in tropical lowland sites

of Central America report similar levels of variability (Wishnie et al. 2007). In this

study, other mid-successional species, Juglans neotropica, T. rosea, and Podocarpus

spp., were planted at five sites but all were \1 m in height and many were in poor

health, with few leaves and slow growth (personal observation). These slower-growing

species likely had trouble competing with the pasture grass present in almost all sites, a

factor that has been identified to inhibit tree recovery of J. neotropica and C. montana in

southern Ecuador (Gunter et al. 2009), as well as for other mid-successional species in

other tropical montane sites (Aide and Cavelier 1994; Sarmiento 1997; Holl et al. 2000)).

Additionally, a study in one of the same field sites used in this study (Estacion Cientıfica

San Francisco, southern Ecuador) finds that lack of mycorrhizal association may be a

limiting factor for reforestation, and that inoculation can assist seedling establishment

(Urgiles et al. 2009).

In this study, short-lived pioneer trees such as S. pyramidalis, Verbesina crasirramea,

and Ochroma pyramidalis, as well as longer-lived A. acuminata may be effective at

facilitating site conditions for mid-successional species. Some site managers practice this

facilitation intentionally by first planting pioneers and later enrichment planting the mid-

successional species. Other site managers practice facilitation unintentionally by planting

all species at once, and letting the more rapidly growing pioneer trees facilitate site

conditions for the mid-successional species. In southern Ecuador, shrubs and ferns were

found to facilitate the growth of certain mid-successional species (Gunter et al. 2009),

while in a meta-study of various restoration sites, facilitation has been found to assist

tree growth in mixed species plantings (Piotto 2008). Similarly, in this study, many sites

with dense infestations of the invasive leguminous shrub Ulex europaeus (gorse, or

retamo espinosa in Spanish, a species native to Europe but common throughout the

northern Andes) are treated with mechanical removal of gorse and broadcast seeding of

the bi-annual herbaceous plant Lupinus bogotensis to provide growing space and sunlight

for pioneer tree species and hopefully prevent re-colonization by the gorse. Use of nurse

plants such as Lupinus for restoration has been described widely in the literature

(Callaway and Walker 1997; Gomez-Aparicio et al. 2004; Blanco-Garcıa et al. 2011;

Reyes and Rıos 2011). Although it is practiced for site amelioration in areas of Ulex

New Forests

123

europeus colonization, some studies have found that nitrogen-fixing plants such as

Lupinus can actually facilitate weed invasion in habitats of native plants (Maron and

Connors 1996). Elsewhere, numerous researchers have recommended facilitation or site

amelioration using fast-growing species, either native or exotic (Brockerhoff et al. 2008;

Jacobs et al. 2015). In Costa Rica, Carpenter et al. (2004) recommend Pinus tecunumanii

to stabilize soil, provide habitat for seed dispersers, suppress weeds, and moderate

microclimate conditions, thus facilitating the establishment and growth of natives. In

Mexico, de la Luz Avendano-Yanez et al. (2015) find that P. patula plantations can

facilitate survival of native mid-successional trees (although inhibit growth). Parrotta

et al. (1997) and Holl et al. (2000) conclude that remnant pasture trees and fast-growing

pioneer trees are necessary to attract seed-dispersers and facilitate restoration. Similarly,

in sites with depleted soils or extreme microclimatic conditions (sun and wind), exotics

with wide ecological amplitudes may be necessary to ameliorate conditions for native

species with smaller niches (Calvo-Alvarado et al. 2007).

Other studies in the region have found nitrogen-fixing trees such as Inga spp. to be a

valuable means of site amelioration in degraded pasture in the Andes (Rhoades et al. 1998).

A. acuminata can be a valuable component of agroforestry systems, where it can serve as a

source of nitrogen fertilization for grass and as shade for cattle (Russo 1990). In southern

Ecuador, researchers have described the economic potential of agroforestry systems where

farmers rotate pasture and A. acuminata in order to reduce pressure on cutting of new

mature forest (Knoke et al. 2009). Similarly, groups in Colombia promote silvo-pastoral

systems with nitrogen-fixing A. acuminata and cattle fodder plants such as Leucaena

leucocephala, (Calle et al. 2009) as found in the sites of Pedro Palo and Rio Guacha in this

study.

Across the region, it should be noted that restoration sites observed in this study were

designed primarily for demonstration or research purposes and required significant

resource investments for planting and site maintenance. At the same time, much of the

region is undergoing a forest transition (Aide et al. 2013), where a significant amount of

land is returning from pasture and agricultural use back to forest. A recent study in

Colombia (Sanchez-Cuervo et al. 2012) found 28,000 km2 of area was reclaimed as sec-

ond-growth from 2001 to 2010, approximately twice as much land as areas that had lost

vegetative cover (deforestation). Most of the reforested areas have occurred from agri-

cultural abandonment, a finding consistent with analysis across Latin America (Aide and

Grau 2004; Rudel et al. 2009; Aide et al. 2013). Steep mountain pasture and coffee areas

are often the most marginal and are abandoned due to urbanization, low agricultural prices,

and/or rural violence (Etter et al. 2006, 2008). In a low-elevation montane forest region of

Ecuador, one study found increasing trends of spontaneous silvo-pastoral landscapes

(Lerner et al. 2014). In highly degraded sites with low nutrient levels such as the mines and

semi-urban areas observed in this study, active restoration may be needed. However, in the

mildly disturbed agricultural landscapes that comprise a significant area of the northern

Andean montane region, active restoration can be combined with agroforestry and silvo-

pastoral systems, using fast growing species such as A. acuminata. These species provide

rapid nutrient inputs to degraded soil, and frequently have greater timber value than other

early-succession trees (Knoke et al. 2009). In most cattle pasture areas, re-vegetation with

native species occurs naturally, although active management can promote the introduction

New Forests

123

of more valuable timber species (Calle et al. 2009; Murgueitio et al. 2011). In the frag-

mented agricultural landscapes that compose much of the tropical Andes, we suggest these

types of agroforestry-oriented restoration activities in order to minimize costs while

facilitating landscape connectivity.

Conclusions

This study provides valuable baseline information on commonly planted native tree

species in montane forests of the northern Andes. Restoration projects in Ecuador and

Colombia, including the ones observed in this study, are largely focused on these

montane forests, and have multiplied in the last two decades (Bare 2014; Murcia et al.

2015). Many of these projects involve silvo-pastoral landscapes (Murgueitio et al.

2011), payments for watershed services (Goldman-Benner et al. 2012; Saenz et al.

2014), and are driven by local or national governments (Bare 2014; Murcia et al.

2015). We show that native species, in particular Andean alder (A. acuminata), grows

fast in a range of restoration sites and soil conditions, but particularly those soils that

are relatively young and low in nitrogen. Our study contributes to a growing body of

literature that native species such as those studied can grow well on degraded sites in

the northern Andes (Murcia 1997; Gunter et al. 2009).

Acknowledgments The authors are grateful for financial support received from the Tropical ResourcesInstitute at the Yale School of Forestry and Environmental Studies and the Gordon and Betty MooreFoundation. Numerous colleagues have assisted with research planning, including Tina Schneider, FlorenciaMontagnini, Eva Garen, Alicia Calle, and Gillian Bloomfield of the Yale School of Forestry and Envi-ronmental Studies and the Environmental Leadership and Training Institute. In Colombia and Ecuador, theauthors are grateful for the assistance of Carolina Murcia of CIFOR, Jose Ignacio Barrera of the UniversidadJaveriana, Orlando Vargas of the Universidad Nacional, Nikolay Aguirre of the Universidad de Loja, dozensmore experts in the fields of conservation and forest restoration, and dozens more project managers,technicians, guides, ranchers, and farmers.

Appendix 1

See Table 4.

New Forests

123

Table

4Listofthetwelvereforestationsitesusedforthisstudyin

Colombia

andEcuador

Project

nam

eLocation

Lat

Lon

Elevation

Geography

Aspect

Soil

texture

Date

established

Size

1Cerros-

Eucalyptus

CerrosOccidentales,

Bogota

4.604232�N

,

74.058302�W

2700

Eastern

Cordillera,

Colombia

West

Loam

2009

Partof34.5

ha

Context:siteofa100-yearold

Eucalyptusreforestation,currentlyundergoingrestorationbythebotanicgarden

ofBogotawithpublicfunds.Objectives

areto

createdem

onstration

areasofnativemontaneforest.Restorationincludes

nativeplantings(m

ultiple

species,scattered),continual

maintenance

andweeding,andcontinual

enrichmentplantings

2Cerros-Gorse

CerrosOccidentales,

Bogota

4.603920�N

,

74.058428�W

2700

Eastern

Cordillera,

Colombia

West

Loam

2008

34.5

ha

Context:sameas

Cerros-Eucalyptussite,butthearea

was

invaded

bygorse(U

lexeuropaeus)duringthe1990sand2000s.Restorationactivityincludes

mechanicalremovalofUlex

europaeus,nativeplantings(m

ultiple

species,scattered),continual

maintenance

andweeding,andcontinual

enrichmentplantings

3Chisaca-

facilitation

Chisaca,

Bogota

4.375763�N

,

74.172475�W

3160

Eastern

Cordillera,

Colombia

Flat

Sandy

loam

2006–2008

10ha

Context:site

ofamunicipal

water

storagearea,invaded

byUlexeuropaeus.Restorationisundertaken

bythepublicwater

utility

ofBogota

incoordinationwiththeUniversidad

Nacional(Bogota),forthepurpose

ofscientificstudyandpublicdem

onstration.Restorationincludes

mechanicalremovaloftheinvasiveplant,nativeplantings(m

ultiplespecies,

scattered)andperiodic

weeding,butlittle

enrichmentplanting

4CORANT—

Ebejico

Ebejico,Antioquia

6.278767�N

,

75.760636�W

1700

Western

Cordillera,

Colombia

North

Loam

y

sand

2007

100haofpassiverestoration,100haof

enrichment,100haofprotection

Context:abandoned

pasture,managed

bythelocalpubliclandcorporation.Restorationincluded

planting(m

ultiple

species,scattered)butverylittle

maintenance

5Estacion

Cientıfica

San

Francisco

EstacionCientıfica

San

Francisco,Loja,

Ecuador

3.968652�S,

79.085204�W

2340

Eastern

Cordillera,

Ecuador

South

Silty loam

2003

4ha

New Forests

123

Table

4continued

Project

nam

eLocation

Lat

Lon

Elevation

Geography

Aspect

Soil

texture

Date

established

Size

Context:restorationispartofan

ongoingscientificexperim

entoperated

betweenalocaluniversity,anationalNGO,anddonors.Plantingsweredonein

rowswithmultiplespecies;

area

isfencedfrom

cowsbutnotweeded

6Pedro

Palolake

LagunaPedro

Palo,Tena,

Cundim

arca

4.685656�N

,

74.386229�W

2180

Central

Cordillera,

Colombia

Flat

Loam

1998

\5ha

Context:restorationobjectiveistheenlargem

entofan

oak

forestoriginally

foundborderingalake.

Project

iscoordinated

byalocalcitizen’s

associationandfunded

byvarious

publicagencies.Restorationincluded

initialplanting(onespecies,row

planting)butlittle

maintenance;area

isfencedto

protect

plantingsfrom

cows

7Pedro

Palo

corridors

LagunaPedro

Palo,Tena,

Cundim

arca

4.685193�N

,

74.377331�W

2020

Central

Cordillera,

Colombia

Flat

Loam

2008

2–5ha

Context:restorationobjectiveis

theestablishmentofsilvo-pastoralsystem

withlivefencesandecological

corridors;project

iscoordinated

byalocalcitizen’s

associationand

funded

byvariouspublicagencies.Restorationincluded

initialplanting(m

ultiple

species,scattered)andenrichmentplantingofmid-successional

speciesbelow

thepioneer

species.Areais

fencedfrom

cowsbutnotweeded

8Profafor

Nono,Pichincha,

Ecuador

0.095844�S,

78.608061�W

2820

Western

Cordillera,

Ecuador

East

Sandy

loam

2006

3ha

Context:project

was

conducted

byanational

NGO

withfundingto

conduct

voluntary

carbonoffsetsforinternational

donors.Areawas

plantedin

rows(m

ultiple

species)

onan

abandoned

pasture,in

landmanaged

byapublicagency.Areais

notmaintained

9ReservaEncenillo

Guasca,Cundim

arca

4.794627�N

,

73.914223�W

3200

Eastern

Cordillera,

Colombia

North

Loam

y

sand

2007

\2ha

Context:landisanature

reserve,owned

byanationalNGO.Therestorationprojectaimsto

restore

asm

allarea

ofthereservethatwas

previouslyin

cattlepasture.Areawas

planted

in2007(onespecies,row

plantings),withinfrequentweeding

New Forests

123

Table

4continued

Project

nam

eLocation

Lat

Lon

Elevation

Geography

Aspect

Soil

texture

Date

established

Size

10

Rio

Bogota

Suesca,Cundim

arca

5.404071�N

,

73.781451�W

2600

Eastern

Cordillera,

Colombia

Flat

Silty clay

loam

mostly

2005–2013

\2haalongriver

corridor

Context:landistheripariancorridor(publicright-of-way)ofasm

allwaterway.Restorationisperform

edbyalocalNGO.Restorationaimsto

preventerosionandrestore

ecosystem

functions.Areais

continually

weeded

andenrichmentplantedwithmultiple

species

11

Rıo

Guacha

Rio

Guachaarea,Boyaca

6.138158�N

,

73.090559�W

2000

Eastern

Cordillera,

Colombia

South

Silty clay

loam

2008

\2halivefences

Context:restorationobjectiveistheestablishmentofasilvo-pastoralsystem

withlivefence

andecologicalcorridorsthroughoutacattlepasture

landscape;restorationisundertaken

byanational

NGO

incoordinationwithlocallandowners(onprivateland).Plantingsaredonein

rows,maintenance

israre

butplantingsarefencedoff

from

cows

12

Zipamine

OIPeldar,Zipaquira,

Cundim

arca

5.067165�N

,

73.867447�W

2760

Eastern

Cordillera,

Colombia

Flat

Sandy

loam

2003

1ha

Context:restorationproject

istherehabilitationofan

abandoned

sandmine;

conducted

byan

environmentalconsultingfirm

foraminingcompany.Restorationinvolves

re-

establishmentofsoil(available

on-site),andplantingofmultiple

species(nativeandexotic),scattered

New Forests

123

Appendix 2

See Table 5.

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