BIOTROPICA 38(2): 183–195 2006
10.1111/j.1744-7429.2006.00124.x
Distribution and Flowering Ecology of Bromeliads along Two Climatically Contrasting
Elevational Transects in the Bolivian Andes1
Thorsten Krömer2 , Michael Kessler
Institute of Plant Sciences, Department of Systematic Botany, University of Göttingen, Untere Karspüle 2, 37073 Göttingen, Germany
and
Sebastian K. Herzog3
Institut für Vogelforschung “Vogelwarte Helgoland,” An der Vogelwarte 21, 26386 Wilhelmshaven, Germany
ABSTRACT
We compared the diversity, taxonomic composition, and pollination syndromes of bromeliad assemblages and the diversity and abundance of hummingbirds along two
climatically contrasting elevational gradients in Bolivia. Elevational patterns of bromeliad species richness differed noticeably between transects. Along the continuously
wet Carrasco transect, species richness peaked at mid-elevations, whereas at Masicurı́ most species were found in the hot, semiarid lowlands. Bromeliad assemblages
were dominated by large epiphytic tank bromeliads at Carrasco and by small epiphytic, atmospheric tillandsias at Masicurı́. In contrast to the epiphytic taxa, terrestrial
bromeliads showed similar distributions across both transects. At Carrasco, hummingbird-pollination was the most common pollination mode, whereas at Masicurı́
most species were entomophilous. The proportion of ornithophilous species increased with elevation on both transects, whereas entomophily showed the opposite
pattern. At Carrasco, the percentage of ornithophilous bromeliad species was significantly correlated with hummingbird abundance but not with hummingbird
species richness. Bat-pollination was linked to humid, tropical conditions in accordance with the high species richness of bats in tropical lowlands. At Carrasco,
mixed hummingbird/bat-pollination was found especially at mid-elevations, i.e., on the transition between preferential bat-pollination in the lowlands and preferential
hummingbird-pollination in the highlands. In conclusion, both richness patterns and pollination syndromes of bromeliad assemblages varied in distinct and readily
interpretable ways in relation to environmental humidity and temperature, and bromeliad pollination syndromes appear to follow the elevational gradients exhibited
by their pollinators.
RESUMEN
Comparamos la diversidad, composición taxonómica y sı́ndromes de polinización de comunidades de bromeliáceas con la diversidad y abundancia de colibrı́es a lo
largo de dos gradientes altitudinales climáticamente diferentes en Bolivia. Los patrones de elevación de riqueza de especies de bromeliáceas difirieron notoriamente
entre los transectos. A lo largo del transecto permanentemente húmedo de Carrasco, la riqueza de las especies alcanzó su punto máximo a elevaciones intermedias,
mientras que en Masicurı́ la mayorı́a de las especies se encontraron en tierras bajas, calientes y semiáridas. Las comunidades de bromeliáceas estuvieron dominadas por
grandes bromeliáceas epifiticas tanque en Carrasco y por pequeñas tillandsias atmosféricas epifiticas en Masicurı́. En contraste a los taxones epifiticos, la distribución
de bromeliáceas terrestres fue bastante similar en ambos transectos. En Carrasco, la polinización por colibrı́es fue la manera de polinización más común, mientras
que en Masicurı́ la mayorı́a de las especies fueron entomófilas. La proporción de especies ornitófilas aumentó con la elevación en ambos transectos, mientras que la
entomófila mostró el patrón contrario. En Carrasco, el porcentaje de especies de bromeliáceas ornitófilas estuvo correlacionado significativamente con la abundancia
de colibrı́es pero no con la riqueza de especies de colibrı́es. La polinización por murciélagos se relacionó con condiciones húmedas y tropicales, coincidiendo con
la alta riqueza de especies de murciélagos en las tierras bajas tropicales. En Carrasco, polinización mixta de colibrı́es/murciélagos fue encontrada principalmente
a elevaciones intermedias, es decir, en la transición entre polinización preferencial por murciélagos en tierras bajas y polinización preferencial por colibrı́es en las
montañas. En conclusión, los patrones de riqueza y sı́ndromes de polinización de comunidades de bromeliáceas varı́an de maneras distintas y fácilmente interpretables
en relación a condiciones de humedad y temperatura. Los sı́ndromes de polinización de bromeliáceas parecen seguir los patrones exhibidos por sus polinizadores
preferenciales.
Key words: bats; Bolivia; Bromeliaceae; diversity; hummingbirds; pollination; tropical montane forest.
THE TROPICAL ANDES ARE AMONG THE BOTANICALLY MOST DIVERSE
regions worldwide (Barthlott et al. 1996). Due to the difficulties
of studying species-rich tropical plant communities, however, our
knowledge of the magnitude and distribution of this diversity is still
fragmentary (Gentry 1995). The most conspicuous changes of community composition and richness in tropical mountains perhaps are
1
Received 11 February 2005; revision accepted 26 April 2005.
Corresponding author. Current address: Estación de Biologı́a Tropical “Los
Tuxtlas,” Universidad Nacional Autónoma de México, Apartado Postal 94, San
Andrés Tuxtla, Veracruz 95701, México; e-mail: tkroemer@ibiologia.unam.mx
3 Current address: Asociación Armonı́a, BirdLife International, Casilla 3566,
Santa Cruz de la Sierra, Bolivia.
2
related to differences in elevation, but few studies have covered entire elevational gradients in enough detail to describe with precision
how tropical forest characteristics change with elevation (Lieberman
et al. 1996). The majority of elevational studies have focused on
species richness (e.g., Gentry 1995, Lieberman et al. 1996, Vázquez
& Givnish 1998, Krömer et al. 2005) and elevational zonation of
vegetation types (see Frahm & Gradstein 1991). Also, most studies have been based on woody plants (e.g., Gentry 1988, 1995;
Kitayama 1992; Lieberman et al. 1996), even though the majority of plant species in humid tropical forests belong to nontree life
forms (Gentry & Dodson 1987, Ibisch 1996, Balslev et al. 1998).
As a result, it is not yet known whether a general relationship exists
C 2005 The Author(s)
C 2005 by The Association for Tropical Biology and Conservation
Journal compilation
183
184
Krömer, Kessler, and Herzog
between species richness and elevation, or even whether a universal
explanation or model exists (Colwell & Hurtt 1994; Rahbek 1995,
1997).
The family Bromeliaceae is almost exclusively restricted to
the New World tropics. Nearly 50 percent of the estimated 3000
bromeliad species are epiphytic (Benzing 2000). These have leaftrichomes of varied forms which function as moisture- and nutrientabsorptive appendages (Benzing 1990, 2000). Studies on the elevational distribution and ecology of bromeliads are rare: Pittendrigh
(1948) examined the vertical distribution of epiphytic bromeliads in Trinidad, Gilmartin (1973) related the distribution of 17
species growing on both slopes of the Ecuadorian Andes to meteorological data, and Garcı́a-Franco and Peters (1987) and CastañoMeneses et al. (2003) analyzed the spatial distribution patterns
of selected species of Tillandsia along an elevational gradient in
Mexico. Bromeliads have a wide range of pollinators, including
bats, birds, and insects, and also include autogamous taxa (Gardner
1986, Till 1992, Benzing 2000, Kessler & Krömer 2000). Furthermore, bromeliads are one of the most important food sources for
hummingbirds in many Neotropical forest regions (Cruden 1972;
Araujo et al. 1994; Sazima et al. 1995a, 1996; Dziedzioch et al.
2003).
In the present study, we compared the diversity, taxonomic
composition, and pollination syndromes of bromeliad assemblages
as well as the diversity and abundance of hummingbirds along
two climatically contrasting elevational gradients in Bolivia. Our
primary aim was to study qualitatively the relationship of bromeliad
pollination syndromes and one pollinator group (hummingbirds) to
temperature and rainfall. By using two transects differing strikingly
in humidity, we hoped to be able to disentangle the relative effects
of elevation as such from that of humidity, which often also varies
with elevation (Kessler et al. 2001). We did not specifically study
bats and insects as pollinators due to the difficulties of sampling
them quantitatively.
METHODS
STUDY AREA AND THE ENVIRONMENT.—Carrasco National Park covers an area of 6226 km2 on the eastern slope in the department of
Cochabamba, Bolivia (Ergueta & Gómez 1997; Fig. 1). Ranging
from 300 to 4500 m, the park contains a complete set of elevational
vegetation belts, many of which are in almost pristine state, especially at 1000–3000 m. The topography is extremely steep, with a
horizontal distance of only 35–45 km from the highest peaks to the
level lowlands of the Chapare region. The present study was conducted from 450 m near the cave “Cuevas del Repechón” to 3950
m along the old, now unused gravel road from Cochabamba to Villa
Tunari (17◦ 03′ –09′ S, 65◦ 27′ –37′ W). Lowland forests were studied
at 300–400 m in Parque Ecoturı́stico Machı́a and on the grounds of
Hotel El Puente in the vicinity of the town of Villa Tunari (16◦ 58′ S,
65◦ 26′ W). These two sites, which are among the few forest areas
remaining in a region largely devoted to coca cultivation (Henkel
1995), are hereafter referred to as Villa Tunari.
Mean annual precipitation at Villa Tunari, the only reliable climatic station in the region, is 5676 mm (10 yr data, Ibisch 1996).
FIGURE 1. Map of Bolivia showing the location of the study sites.
Most precipitation falls between November and May, but even in
the “dry” season from June to October every month receives >100
mm, thus creating a perhumid climate (sensu Lauer et al. 1996).
There are no climatic stations at higher elevations, but since the
steep topography concentrates the convective precipitation on a narrow belt, precipitation is undoubtedly higher than in the lowlands.
Ibisch (1996) estimated >3500 mm mean annual precipitation at
2200 m elevation in the somewhat sheltered valley of Sehuencas,
but it is likely that slopes directly exposed to incoming clouds at
mid-elevations (1000–3000 m) in the NW of the park receive annual precipitation in excess of 8000 mm (J. Böhner, pers. comm.).
Additional humidity is contributed by dew and fog condensation
(Ibisch 1996). Mean annual temperature is 24.6◦ C at Villa Tunari
and 12–15◦ C at 2200 m at Sehuencas (Ibisch 1996), with an annual
variability of about 5◦ C. Nocturnal frosts occur down to 2000 m
(Ibisch 1996, T. Krömer & M. Kessler, pers. obs.), especially during
periodic influxes of southern polar winds during austral winter.
The natural vegetation of the entire study area consists of evergreen forest. Navarro (1997) proposed a preliminary delimitation of
seven vegetation belts in Carrasco National Park defined by characteristic tree species, but in-depth studies of the forest vegetation are
lacking. Tree community composition probably corresponds to that
generally observed along humid east-Andean slopes (Gentry 1988,
1995; Ibisch 1996; Navarro 1997). Because of the steep topography and high rainfall, landslides are common and a considerable
portion of the vegetation consists of varying stages of natural forest
succession (Ibisch 1996, Kessler 1999). Above about 3500 m forests
are dominated by Polylepis racemosa (Rosaceae; 3500–3800 m) and
P. pepei (3800–4200 m). These Polylepis forests have largely been
destroyed through centuries of human-induced burning and today
are restricted to relict patches, mostly in ravines or on boulder slopes
(Kessler 1995, Fjeldså & Kessler 1996).
The second transect was located in the Masicurı́ valley from the
confluence of the Masicurı́ and Grande rivers (19◦ 02′ S, 63◦ 42′ W;
500 m) to the highest accessible peaks at San Lorenzo (18◦ 41′ S,
63◦ 55′ W; 2500 m) on the west side of the valley along the road
Elevational Patterns of Bromeliads 185
from Vallegrande to Masicurı́ in western Departamento de Santa
Cruz, Bolivia (Fig. 1). Mean annual precipitation at the village
of Masicurı́ (800 m) is 1792 mm. Precipitation declines toward
lower elevations, with values between 1000 and 1200 mm reported
from various climatic stations along the Andean foothill base to
the east of the study area. At higher elevations, precipitation and
fog intensity increase noticeably (see Bianchi 1981, for data from
Argentina), especially at about 1000–1200 m elevation (T. Krömer
& M. Kessler, pers. obs.), but no quantitative measurements are
available. Mean annual temperature is about 25◦ C at 500 m and
declines by about 0.6◦ C per 100 m elevational increase (Eriksen
1986, Gerold 1987). Climate is seasonal, with about 75 percent
of the precipitation falling in the austral summer (November to
April), and a lower frost limit in the austral winter at 800 m (Eriksen
1986). Of particular importance is the regular influx of cold polar
fronts along the Andean base in austral winter, locally known as
surazos, which reduce temperatures considerably for several days
and represent the main source of precipitation in this season (Fjeldså
et al. 1999).
In accordance with climatic changes, three main elevational
vegetation zones were discernible at Masicurı́ which are typical
for this biogeographic region as a whole (Cabrera 1976, Ribera
et al. 1992, Navarro 1997, Schulenberg & Awbrey 1997). Up to
850–1000 m, forests were deciduous to semideciduous and composed primarily of Leguminosae such as Anadenanthera macrocarpa
(Benth.) Brenan, Enterolobium contortisiliquum (Well) Morong.,
and Parapiptadenia excelsa (Griseb.) Baker. Between 850–1000 m
and about 1800 m, forests were evergreen and contained Cedrela
lilloi C. DC (Meliaceae), Chrysophyllum gonocarpum (Mart. &
Eichl.) Engl. (Sapotaceae), Crinodendron tucumanum Lillo (Elaeocarpaceae), Ficus spp. (Moraceae), Miconia spp. (Melastomataceae),
as well as numerous naturalized orange trees (Citrus aurantium L.).
Above 1800 m, the evergreen forest was dominated by Podocarpus
parlatorei Pilger (Podocarpaceae) and numerous Myrtaceae such as
Blepharocalyx salicifolius (H.B.K.) O. Berg, Myrcianthes callicoma
McVaugh, M. pseudomato (Legrand) McVaugh, and Siphoneugenia
occidentalis Legrand.
Human activity varied according to climatic and topographic
conditions. The alluvial plain of the Masicurı́ valley was completely
deforested and used for intensive agriculture. Agricultural areas on
slopes were located primarily at 900–1200 m and at 1700–2000 m,
corresponding to the elevations with the most benign climate and
least steeply inclined slopes. Forests on hillsides and slopes throughout the entire transect experienced selective timber extraction (especially Cedrela, Podocarpus, Tabebuia spp., depending on vegetation
zone) and extensive cattle grazing. Many higher mountain areas had
been burnt to establish cattle pastures.
BOTANICAL SAMPLING.—Fieldwork was conducted in 1996 from
23 June to 11 September along the Carrasco transect, from 12
to 19 September at Villa Tunari, and from 9 to 15 July 1995
and 20 May to 14 June 1996 in the Masicurı́ area. Bromeliads
were studied on 283 plots of 400 m2 , mostly of square shape but
occasionally in other shapes to minimize habit heterogeneity. At
Carrasco, we studied 183 plots (24 at 300–500 m, 24 at 500–1000
m, 24 at 1000–1500 m, 23 at 1500–2000 m, 26 at 2000–2500
m, 25 at 2500–3000, 20 at 3000–3500 m, and 17 at 3500–4000
m), and 100 plots at Masicurı́ (27 at 450–1000 m, 21 at 1000–
1500 m, 26 at 1500–2000 m, 26 at 2000–2400 m). Plot size
corresponds to the minimum area required for representative surveys
of bromeliads in the vegetation types sampled and is small enough
to keep environmental factors more or less uniform throughout
the plots (Kessler & Bach 1999). Elevation was measured with
a handheld Eschenbach altimeter to the nearest 50 m, correcting
for weather-related inaccuracies by repeated measures and through
reference to 1:250.000 topographic maps. Presence/absence of all
species was registered in each plot, treating terrestrial and epiphytic
plants separately. All species encountered in the survey area (but
not in every single plot) were collected in triplicate and have been
deposited at the Herbario Nacional de Bolivia (LPB, including all
unicates), with the specialist H. Luther at Sarasota (SAR), and at
the Herbarium Göttingen (GOET).
POLLINATION MODES.—All recorded species (except for two Greigia
species where no information was available) were grouped into four
broad categories according to their main pollination mode as ornithophilous, chiropterophilous, entomophilous, mixed or unspecific (two or all of the first three categories). Classification was based
on information from published sources (Gardner 1986; Bernardello
et al. 1991; Till 1992; Stiles & Freeman 1993; Sazima et al. 1995a,
1996; Benzing 2000; Dziedzioch et al. 2003), personal field observations of flower visitors (assuming that regular flower visitors
with appropriate morphology to come into contact with anthers
and styles are pollinators), and on nectar contents analysis of 79
bromeliad species by High Performance Liquid Chromatography
(Krömer 2005), which allows inferences to pollinators (Baker &
Baker 1983, Bernardello et al. 1991, Schwerdtfeger 1996). Species
for which no such information was available were classified based on
deductions from morphology and flower coloration (Gardner 1986,
Baker & Baker 1990). A more detailed classification, especially of
the entomophilous taxa, was not possible since many bromeliad
species are little known with respect to their pollinators and because
even species with apparently clear-cut pollination syndromes often
have more than one pollinator (Sazima et al. 1994).
HUMMINGBIRD DATA.—Hummingbird communities were surveyed
by S. K. Herzog in exactly the same areas as the botanical sampling
with two exceptions on the Masicurı́ transect. At the lower end
of that transect, surveys were restricted to the confluence of the
Masicurı́ and Grande rivers (ca 500 m), with a survey gap extending
up to an elevation of 1100 m. The accessible habitat in the intervening area was too degraded by human activities for a meaningful,
comparable bird survey. At the upper end of the Masicurı́ transect
(>2000 m), bird observations were concentrated on forest habitats,
whereas bromeliads were sampled in all available habitats, including degraded shrubby areas. Fieldwork on the Carrasco transect
was conducted between 22 June and 19 September 1996 (Herzog
et al. 2005). The Masicurı́ transect was surveyed from 20 May to
13 June 1996, with a second visit to the confluence of the Masicurı́
186
Krömer, Kessler, and Herzog
and Grande rivers from 10 to 14 August 1999 (Herzog & Kessler
2002).
Surveys followed the field procedures outlined in Herzog
et al. (2002), which are only briefly summarized here. While walking slowly and quietly from dawn to midday and often again in
late afternoon along roads, trails, and through the habitat where
feasible, S. K. Herzog continuously recorded all visual and acoustical observations of all birds including hummingbirds (including
numbers of individuals per species) within 50 m of the observer.
The observer’s movement rate largely depended on the level of bird
activity. When spending longer periods in one spot and during occasional re-sampling of an area (the latter occurred to approximately
the same degree in all elevational belts and thus did not introduce a
systematic error), repeated counts of obviously territorial individuals
were avoided. Tape recordings were made extensively to supplement
observations and to identify unknown voices. Observation time exceeded 22 h in every belt.
DATA ANALYSIS.—Transects were divided into steps of 500 m, pooling all data within each step. Bromeliad richness was expressed as
the total number of species recorded in each elevational belt, while
the frequency of pollination modes was expressed as the percentage
of species with a specific mode within a given belt. Hummingbird species richness was expressed as the total number of species
recorded (i.e., raw species counts) in each elevational belt, and the
number of species observed divided by the number of hours of observation time in that belt. Hummingbird abundance in each belt
was expressed as the number of individuals (regardless of species
identity) observed divided by the number of hours of observation
time in that belt. Concordance of the richness and abundance patterns of hummingbird-pollinated bromeliads and hummingbirds
was calculated via correlation analyses.
RESULTS
SPECIES RICHNESS AND DISTRIBUTION OF BROMELIADS.—On the
Carrasco transect, a total of 49 bromeliad species in 10 genera was
found (Appendix 1). Nearly 50 percent of these species belonged
to the genera Guzmania and Tillandsia, which together included
23 species. Divided into life forms, there were 15 terrestrial species
in 4 genera (Fosterella, Greigia, Pitcairnia, Puya) and 34 species of
epiphytic tank bromeliads in 6 genera (Aechmea, Billbergia, Guzmania, Racinaea, Tillandsia, Werauhia). Highest species numbers
were found in the elevational belts 1000–1500 m (23 species) and
1500–2500 m (19 species in each) (Fig. 2). Among the terrestrial
genera, Pitcairnia had by far the widest elevational amplitude and
was found in the lower and middle parts of the transect up to 2500
m. Fosterella was found only at mid-elevations (1100–1550 m),
whereas Greigia and Puya were limited to the upper half of the transect. Epiphytic Guzmania, Tillandsia, and Racinaea covered a broad
elevational range, extending from the lowlands to at least 3000 m.
In contrast, Aechmea, Billbergia, and Werauhia were limited to the
lower parts of the transect.
On the Masicurı́ transect, we collected a total of 30 species
in 8 genera (Appendix 1). The genus Tillandsia with 12 species
FIGURE 2. Number of bromeliad species along the elevational transect in
Carrasco (white columns) and Masicurı́ (black columns).
was by far the most important, followed by Fosterella and Puya
with 5 species each. The 16 terrestrial bromeliads belonged to 5
genera (Bromelia, Dyckia, Fosterella, Pitcairnia, Puya), whereas the
14 epiphytic species included 12 atmospheric tillandsias and 2 tank
bromeliads (Aechmea, Vriesea). The highest number of species was
found at 500–1000 m with 17 species (Fig. 2). The terrestrial
genera Fosterella and Pitcairnia covered a wide elevational range
of 500–1750 and 750–1950 m, respectively. Bromelia and Dyckia
were limited to the lowlands, whereas Puya mostly occurred at high
elevations but was also found down to 600 m. Among the epiphytic
genera, Tillandsia covered the entire transect, whereas Aechmea and
Vriesea were found only at mid-elevations.
POLLINATION MODES.—On the Carrasco transect, 51 percent of all
recorded species were ornithophilous (Table 1), especially in the
epiphytic genera Tillandsia (8 species) and Guzmania (5) and the
terrestrial genera Pitcairnia (4) and Puya (4) (Appendix 1). Among
the five chiropterophilous species, three were Guzmania, whereas all
eight entomophilous species belonged to the genera Fosterella and
Racinaea. Species with unspecialized pollination modes belonged
mainly to the genera Aechmea and Tillandsia. The special case of
species with mixed pollination by both bats and birds was dominated
by Guzmania.
On the Masicurı́ transect, 40 percent of all species were
ornithophilous (Table 1), including all species of the terrestrial
genera Dyckia (1 species), Pitcairnia (4), and Puya (5) (Appendix 1). None of the species were chiropterophilous. The entomophilous species (47%) belonged to the genera Fosterella and
Tillandsia, and the unspecialized species belonged to Aechmea and
Bromelia.
Analyzing the frequency of pollination modes via the number of records within all plots revealed that on both transects ornithophilous species were less frequent than expected by their species
numbers, whereas chiropterophilous species and species with mixed
pollination by both bats and birds were more frequent in Carrasco
(Table 1).
Elevational Patterns of Bromeliads 187
TABLE 1. Species numbers and frequency (number of plot-records relative to total number of plot-records; % are given relative to total species numbers and numbers of
records, respectively) of different pollination modes (orn = ornithophilous, chi = chiropterophilous, ent = entomophilous, mi = mixed or unspecific, mi (chi/orn)
= mixed ornithophilous/chiropterophilous) among bromeliads along the elevational transects at Carrasco and Masicurı́.
Carrasco
Species number
%
Masicurı́
Records
%
Species number
%
Records
%
orn
24
51
216
40
12
40
63
35
chi
ent
mi
5
8
6
11
17
13
101
65
40
19
12
7
0
14
4
47
13
72
44
40
25
4
47
8
100
118
540
22
100
0
30
100
179
100
mi (chi/orn)
Total
Looking at the elevational distribution of pollination modes,
on the Carrasco transect the relative contribution of ornithophilous
species increased from 20 percent at 300 m to 100 percent above
3000 m, whereas the values for chiropterophilous species declined
from 54 percent at 300 m to <10 percent above 2000 m (Fig. 3).
Species with mixed bat/hummingbird-pollination showed a mixed
pattern and reached their highest value of 47 percent at 2000–2500
m. Entomophilous species reached their highest contributions (14–
17%) at 1000–3000 m, whereas unspecialized species declined from
25 percent in the lowlands to 0 percent at high elevations.
On the Masicurı́ transect, the relative contribution of ornithophilous species increased from 10 percent at 500 m to around
70 percent at 1500–2450 m (Fig. 3). Entomophilous species declined from 62 percent at 500 m to 8 percent at 1500–2000 m,
and increased again to 31 percent above 2000 m. The unspecialized species showed a decline from 28 percent in the lowlands to 0
percent at high elevations.
tion time, richness peaked at 3000–3500 m (0.36 species/h), with a
minor peak at 1500–2000 m (0.28 species/h; Fig. 4). Abundance of
hummingbirds, however, showed an overall increase with elevation
and peaked above 3000 m (4.3 individuals/h). On the Masicurı́
transect, a total of only 12 hummingbird species in 10 genera were
recorded, including 7 species and 4 genera not observed on the Carrasco transect (Appendix 2). Species richness (7), number of species
per hour (0.23), and abundance (1.3 individuals/h) all peaked at
1500–2000 m (Fig. 4).
At Carrasco, there was no significant correlation between
species richness of hummingbird-pollinated bromeliads and hummingbirds, but highly significant correlations to the number of
hummingbird species recorded per hour (r = 0.9, P < 0.01), and
the number of hummingbird individuals recorded per hour (r =
0.98, P < 0.01) (Fig. 5). At Masicurı́, there were no significant correlations between the richness and abundance values of bromeliads
and hummingbirds.
HUMMINGBIRD RICHNESS AND ABUNDANCE.—We recorded a total
of 28 hummingbird species in 22 genera along the Carrasco transect
(Appendix 2). Hummingbird richness reached a maximum of 10
species at 1000–2000 m, but when standardizing values for observa-
DISCUSSION
SPECIES RICHNESS AND DISTRIBUTION.—Elevational patterns of
species richness differed noticeably between the transects (Fig. 2).
FIGURE 3. Relative representation of different pollination modes among bromeliads along the elevational transect in Carrasco and Masicurı́.
188
Krömer, Kessler, and Herzog
FIGURE 4. Number of hummingbird species, number of hummingbird species recorded per hour, and number of hummingbird individuals recorded per hour
along the elevational transect at Carrasco (white columns) and Masicurı́ (black columns).
The perhumid Carrasco transect had its highest number of species
at 1000–2500 m. This is the elevational range of the main cloud
condensation level typically observed in the Bolivian Andes and is
characterized by maximum humidity and moderate temperatures.
Opposed to this, at Masicurı́ most species were found in the hot,
semiarid lowlands, whereas the temperate, semihumid zone of the
Tucumano-Boliviano forest at 1000–2000 m was relatively poor in
species. These patterns correspond to those of previous studies both
for Andean rain forests (Sugden & Robins 1979, Sugden 1981,
Cleef et al. 1984) and for dry forests (Ibisch 1996).
These contrasting patterns likely reflect the climatic conditions
of the transects. At Carrasco, with its perhumid climate, bromeliad
assemblages are dominated by large epiphytic tank bromeliads,
whereas in semihumid Masicurı́ they are characterized by small,
epiphytic, atmospheric (“gray”) tillandsias. Tank bromeliads capture rain and humidity with dense rosettes formed by the bases of
their leaves and cannot survive long periods of heat and dryness. In
contrast, atmospheric tillandsias capture water from dew condensa-
tion and rain by leaves covered with specialized scales (Smith 1989;
Benzing 1990, 2000). The paucity of tank bromeliads at higher
elevations at Masicurı́ probably reflects the regular occurrence of
frost in the area (Kessler 2002b).
In contrast to the epiphytic taxa, the distribution of terrestrial bromeliads was much more similar among transects. Although
only one species (Fosterella albicans) was common to both transects,
the main genera Fosterella, Pitcairnia, and Puya were the same and
showed comparable richness patterns. Whereas Fosterella and Pitcairnia were found only at low and mid-elevations, Puya was almost
limited to the upper parts of both transects, which are characterized by extreme climatic conditions with high solar radiation and
night temperatures below freezing. These three genera are by far
the most numerous and important terrestrial bromeliad genera in
Bolivia (Krömer et al. 1999, Krömer 2000) and can be found in
all biogeographic regions of the country. The remaining terrestrial
genera are less common and were found only at one of the two
transects: Greigia is a typical element in the understory of montane
FIGURE 5. Correlation between number of hummingbird species/number of hummingbird species recorded per hour/number of hummingbird individuals recorded
per hour, and the relative contribution of ornithophilous bromeliads in Carrasco and Masicurı́.
Elevational Patterns of Bromeliads 189
and cloud forests, whereas Bromelia and Dyckia are common in
dry lowland to mid-elevation areas where they colonize open and
disturbed areas (Krömer et al. 1999, Vásquez & Ibisch 2003, Will
et al. in press). In conclusion, the uptake of water and nutrients
through the root system clearly renders terrestrial bromeliads less
dependent on climatic conditions, in particular on humidity, than
their epiphytic relatives.
POLLINATION MODES.—On the Carrasco transect, hummingbirdpollination was the most common pollination mode. This corresponds to the overall situation in Bolivia, where 61 percent
of all species are ornithophilous, compared to 24 percent entomophilous, 7 percent chiropterophilous, 4 percent autogamous,
and 3 percent with mixed pollination modes (Kessler & Krömer
2000). Ornithophily was also common at Masicurı́, but even more
species were entomophilous. On both transects, the percentage of
ornithophilous species increased with elevation, although values
were generally higher in perhumid Carrasco compared to semiarid
Masicurı́. Bromeliad richness correlated very well with the abundance of hummingbirds along the Carrasco transect but not with
hummingbird species richness. At Masicurı́, the low number of
hummingbirds above 2000 m is striking, but may be partly due
to a sampling bias. Whereas bromeliads were sampled in all available habitats, including degraded shrublands where most species
were found, bird observations were concentrated on forest habitats,
where hummingbirds and bird-pollinated bromeliads were rare (S.
K. Herzog, pers. obs.). One caveat in this context is the seasonal
elevational migratory movements of hummingbirds (Stiles 1977,
1978) that may lead to temporary shifts in their elevational distribution of richness and abundance. We do not believe that this
would have severely affected our results because when we used the
full known elevational range of each hummingbird species (based
on Hennessey et al. 2003) to calculate the elevational pattern of
species richness (data not shown), the resulting pattern closely
corresponded to the richness pattern documented here. Nevertheless, it would certainly be interesting to study the seasonal variation of bromeliad flowering and hummingbird abundances and
richness.
Hummingbirds play a crucial role in the pollination of both
epiphytic and terrestrial plants in Andean forests (Stiles 1978,
Feinsinger 1983, Bawa 1990, Dziedzioch et al. 2003). Many epiphytic bird-pollinated bromeliads are adapted to their pollinators
by producing few flowers over relatively long time periods (Ackerman 1986; Benzing 1990, 2000), thereby assuring a constant food
supply for hummingbirds for which bromeliads are among the most
important food plants (Cruden 1972; Araujo et al. 1994; Sazima
et al. 1995a, 1996). In contrast, ornithophilous terrestrial bromeliads often tend to produce many flowers over short time periods, attracting an abundance of hummingbirds (Kraemer et al. 1993). We
are unaware of any published explanation for this striking contrast
in pollination strategies between epiphytic and terrestrial bromeliads, but we hypothesize that limitations in water availability may
force epiphytic bromeliads to limit nectar production and to offset
this disadvantage by providing a long-term reliable nectar source.
For example, the rosette plant Lobelia rhynchopetalum (Hochst. ex
A. Rich.) Hemsl. (Campanulaceae), which resembles large Puya
species in habit and ecology, uses 0.3–0.6 liter of water per day
vegetatively and up to 3.4 liter when flowering, mostly for the production of up to 2 liter of nectar (R. Zimmermann, pers. comm.).
The only comparable study on epiphytic bromeliads (Ordano &
Ornelas 2004) shows that nectar removal by pollinators induces
higher nectar production through a dilution of the sugar contents,
i.e., through higher water secretion, but the overall limited amount
of water (<20 ml) does not allow an inference on whether the pollination strategy is influenced by water availability. Ecophysiological
studies of the water budget of epiphytic and terrestrial bromeliads
during flowering and nonflowering periods may be used to test the
hypothesis presented here.
Entomophily was of limited importance along the Carrasco
transect and at middle elevations along the Masicurı́ transect, but
was the most important pollination mode at low elevations at Masicurı́, mainly due to the prevalence of species of Tillandsia and Fosterella. Contrasting hummingbird and insect pollination, we found
thus that hummingbird-pollination among the bromeliad assemblages increased with decreasing temperatures and with increasing
humidity, while entomophily showed the opposite pattern. This
general pattern was paralleled by the hummingbird assemblages, especially considering abundance. A probable reason for the predominance of hummingbirds as pollinators in cold and humid habitats
is that they are the best-adapted major biotic pollinator group under these conditions. As warm-blooded organisms, hummingbirds
can function even at low temperatures, and their ability to fall into
torpor at night is highly energy-efficient. Opposed to this, insects
depend on warm and dry conditions for optimal activity. In seasonal
climates, such as along the lower part of the Masicurı́ transect, the
seasonal shortage of nectar is deleterious to hummingbirds and is
favorable to insects, which, in the case of some Hymenoptera, can
store nectar or pollen and therefore represent the dominant pollinator group under these conditions (Proctor et al. 1996, Kessler &
Krömer 2000).
The importance of bat-pollination among bromeliads in tropical lowlands has been largely overlooked until very recently. Whereas
many species of the genera Vriesea and Werauhia are known to be
chiropteriphilous (Grant 1995, Sazima et al. 1995b), there are few
additional records of bat-pollinated bromeliads (Benzing 2000).
However, recent observations have shown that about 35 percent
(8 of 18) of the Bolivian species of the genus Guzmania are very
likely pollinated by small nectar-feeding bats (Phyllostomidae: Glossophaginae) (Krömer 2003a). Their floral syndrome includes small,
night-blooming flowers with brown or green bracts, greenish to
whitish petals, and mostly a specific smell such as garlic-like odor
in Guzmania sphaeroidea. Further chiropterophilous bromeliads are
found in the genera Billbergia (B. robert-readii), Pitcairnia (P. crassa),
and Puya (P. ferruginea; Krömer 2003a). All these, in contrast to
Guzmania, have large and nectar-rich flowers, which suggests that
they are pollinated by fairly large bat species. Both Bolivian species
of Werauhia are characterized by bell-shaped (campanulate) flowers
that fit like a “head-mask” on the elongated rostrum of the nectarfeeding bats. Werauhia gladioliflora, a relatively frequent species in
lower montane forest, primarily grows in the understory and the
190
Krömer, Kessler, and Herzog
trunk area, where its flowers are projected into the open air (Krömer
2003b). This exposure, similar to cauliflory, provides space for wing
movements of the bats during hovering. Generally speaking, batpollination is clearly linked to humid, tropical conditions (Kessler
& Krömer 2000) in accordance with the high species richness of
bats in tropical lowlands (Patterson et al. 1996).
Interestingly, at 1500–2500 m on the Carracso transect, we
found three Guzmania (G. danielii, G. killipiana, G. morreniana) and one Pitcairnia (P. cf. trianae) species that could not
be readily assigned to any of the main pollination syndromes,
but which contributed 23–49 percent of all bromeliad individuals. On the one hand, the inconspicuous, brownish flowering
stands of the Guzmania species and their nocturnal anthesis (T.
Krömer, pers. obs.) suggest bat-pollination. Further, they have
hexose-rich nectar (T. Krömer, pers. comm.), corresponding to
typical bat-pollinated species (Baker & Baker 1983). However,
the flowers are also open during the day and are scentless (at
least to human observers), which suggests that they are also pollinated by hummingbirds, as indeed observed in G. killipiana in
Ecuador (Dziedzioch et al. 2003). Similar intermediate pollination syndromes have been found for three species of the genus
Abutilon (Malvaceae) (Buzato et al. 1994) and for Siphocampylos
sulfureus E. Wimm. (Lobeliaceae) (Sazima et al. 1994). Strikingly,
on the Carrasco transect, mixed hummingbird/bat-pollination was
found especially at mid-elevations, i.e., in the transition zone between preferential bat-pollination in the lowlands and preferential
hummingbird-pollination in the highlands.
Species with mixed pollination visited by hummingbirds and
insects were found most frequently at low elevations along both
transects. Such unspecific pollination has repeatedly been recorded
among bromeliads and other tropical plants (Bernardello et al. 1991,
Seres & Ramı́rez 1995, Benzing 2000). A possible explanation for
the prevalence of this mode in the lowlands could be the absence of
harsh environmental conditions limiting the availability of specific
pollinators. Under harsh conditions with few available pollinators,
it may be advantageous for plants to adapt to specific pollinators in
order to ensure reliable pollination (Kessler & Krömer 2000).
In conclusion, we found that both the richness patterns and
pollination syndromes of bromeliad assemblages varied in distinct
and readily interpretable ways in relation to environmental humidity and temperature, as shown by the different patterns on the two
climatically contrasting study transects. In all cases, the prevalence
of certain pollination syndromes under specific climatic conditions
was determined by the physiological adaptations and tolerances of
the pollinator taxa, suggesting that in the studied plant–animal interactions the plants adapt mainly to the animals and not vice versa.
This interpretation is further supported by the fact that bromeliad
richness trailed hummingbird abundance at Carrasco, whereas hummingbird diversity was largely independent of bromeliad diversity. Naturally, the adaptive potential of bromeliads is limited by
their ecophysiological growth adaptations to ecoclimatic conditions
(Benzing 2000; Kessler 2002a,b). How the respective bromeliad
genera realize the adaptation to a certain pollinator is apparently influenced by life form, and potentially by other life history attributes
as well. Our study thus suggests that bromeliads strive toward an
optimization of their pollination success by pollinator shifts and
different nectar reward strategies within the limitations of their
evolutionary and ecophysiological bounds.
ACKNOWLEDGMENTS
For help and good companionship during fieldwork, we thank A.
Acebey, J. A. Balderrama, J. Gonzales, A. Green, B. Hibbits, I.
Jimenez, J.-C. Ledesma, and M. Sonnentag. We further thank H.
Luther and P. L. Ibisch for specimen identification and two anonymous reviewers for valuable comments. This study would have been
impossible without the logistic support by the Herbario Nacional
de Bolivia, La Paz, in particular by S. G. Beck, M. Cusicanqui, A.
de Lima, R. de Michel, and M. Moraes. For working and collecting
permits we thank the Dirección Nacional de Conservación de la
Biodiversidad (DNCB), La Paz. This study was supported by the
Deutsche Forschungsgemeinschaft, the A. F. W. Schimper-Stiftung,
the DIVA project under the Danish Environmental Programme,
the German Academic Exchange Service, Fauna and Flora International, and the Gesellschaft für Tropenornithologie.
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Elevational Patterns of Bromeliads 193
APPENDIX 1.
Bromeliad species observed on the Carrasco and Masicurı́ elevational transects in the Bolivian Andes. Pollination mode based on 1 published sources: a Sazima
et al. (1995a), b Benzing (2000), c Dziedzioch et al. (2003); 2 personal observation; 3 nectar content: a Bernardello et al. (1991), b Stiles and Freeman (1993),
c T. Krömer, pers. comm.; 4 deduction based on flower morphology.
Species
Corolla
length (mm)
Bract
color
Petal
color
Pollination
mode
Elevational range
Carrasco
Aechmea angustifolia Poepp. & Endl.
12–16
Red
Yellow
mi4
300–1050
Aechmea distichantha Lem.
Aechmea longifolia (Rudge) L. B. Sm. & M. A.
Spencer
18
25–30
Rose
Pink or rose
White, purple or blue
White
mi1a,2,3a
mi3c
400–450
Billbergia jandebrabanderi R. Vásquez & P. L.
Ibisch
Bromelia serra Griseb.
85–100
Pink
Green
orn3c
850–1600
15
Red
Blue-purple
mi3a
5.5
4–5
Green
Green
Red-orange
White
White
orn4
ent1b
ent1b
5
Green
Green
Green
White
White
White
ent1b
ent1b
ent1b
32
Green
Castaneous
White
Pale purple
ent1b
no data
1700–2200
Greigia cf. kessleri H. Luther
Guzmania besseae H. Luther
Guzmania calothyrsus Mez
20
ca 25
45
Brown
Castaneous
Green to brown
Rosey purple
White
White
no data
orn1c
chi2
2600–3500
2000–2200
300–900
Guzmania danielii L. B. Sm.
Guzmania gloriosa (André) André ex Mez
Guzmania killipiana L. B. Sm.
ca 25
50
38
Castaneous
Red
Castaneous
White
Yellow
White
mi (chi/orn)3c
orn1c
mi (chi/orn) 1c,3c
1600–2700
1700–3000
650–2600
Guzmania marantoidea (Rusby) H. Luther
Guzmania melinonis Regel
Guzmania morreniana (Linden Hortus) Mez
ca 25
28
22
Red
Red
Castaneous
Violet
Yellow
White
orn4
orn3c
mi (chi/orn)3c
1000–1300
300–1050
1300–2300
Guzmania retusa L. B. Sm.
Guzmania roetzlii (E. Morren) Mez
Guzmania sphaeroidea (André) André ex Mez
23
23
ca 25
Green
Pale green
Green or brown
White
White
Cream or green
chi2
mi2
chi3c
1300–1600
500–1050
450–1550
Guzmania squarrosa (Mez & Sodiro) L. B. Sm.
& Pittendrigh
Mezobromelia capituligera (Grisebach) J. R.
ca 50
Red to orange
Yellow
orn3c
Dyckia cf. leptostachya Baker
Fosterella albicans (Griseb.) L. B. Sm.
Fosterella chaparensis Ibisch, Vásquez & Gross
Fosterella cf. schidosperma (Baker) L. B. Sm.
Fosterella spec. 1 MK 5284
Fosterella spec. 2 MK 5373
Fosterella spec. 3 MK 5973
Greigia cochabambae H. Luther
1500–1950
500–800
1300
1550
500
1000
1250
1600
28
Red or orange
White or yellow
orn4
500–2200
53
Red
Red
orn4
650–1300
Pitcairnia brittoniana Mez
Pitcairnia divaricata Wittmack
40
50
Red
Yellow or orange
Red
orn3b
orn4
650–1750
Pitcairnia lanuginosa Ruiz & Pavón
Pitcairnia paniculata (Ruiz & Pavón) Ruiz &
Pavón
90
45
Green with purple lines
Red
orn4
orn4
300–900
300–1300
Greenish yellow
mi (chi/orn)3c
orn?4
orn?4
1900–2500
Castaneous
White
Greenish white
Yellow
orn4
chi1b,2
orn3c
2800–2950
2200–2550
3450–3800
Brown
Blue
Blue-green
Dark violet
orn4
orn3c
orn4
ca 45
Puya atra L. B. Sm.
Puya ferruginea (Ruiz & Pavón) L. B. Sm.
Puya herzogii Wittmack
60
140
50
Puya leptostachya L. B. Sm.
Puya nana Wittm.
Puya sanctae-crucis (Baker) L. B. Sm.
30
40
40
Green
500–550
1750
1100–1300
Grant
Pitcairnia amboroensis Ibisch, Vásquez, Gross
& Kessler
Pitcairnia cf. trianae André
Pitcairnia spec. 1 MK 5956
Pitcairnia spec. 2 MK 6010
Masicurı́
1750–1900
1900–1950
750–1200
1150
3650
2100–2400
1950–2150
194
Krömer, Kessler, and Herzog
APPENDIX 1.
Continued.
Species
Puya cf. secunda L. B. Sm.
Puya serranoensis Rauh
Corolla
length (mm)
40
60–70
Bract
color
Red
Rose
Petal
color
Dark violet
Blue-green
Racinaea seemannii (Baker) M. A. Spencer &
L. B. Sm.
Racinaea spiculosa (Grisebach) M. A. Spencer
& L. B. Sm.
Racinaea tetrantha (Ruiz & Pavón) M. A.
Spencer & L. B. Sm.
orn3c
orn3c
Elevational range
Carrasco
Masicurı́
2200
2100–2400
orn?4
orn?4
Puya spec.1 MK 5332
Puya spec.2 MK 6516
Racinaea kessleri H. Luther
Racinaea schumanniana (Wittmack) J. R.
Grant
Pollination
mode
750
2400
5–7
5
Brown
Green
Yellow
White to yellowish
ent4
ent4
2950
650–2550
12–15
Red
White
orn1c,3c
2000–3150
5–10
Greenish white
ent4
650–1400
14
Yellow
ent1c
2500–2950
Yellow
Violet
ent?4
orn4
orn4
1600–2550
1300–2500
2200
mi4
mi4 , auto1
orn1c,3a
1800–2550
Racinaea spec. MK 6976
Tillandsia asplundii L. B. Sm.
Tillandsia australis Mez
?
20
20–40
Tillandsia bryoides Griseb.
Tillandsia capillaris Ruiz & Pavón
Tillandsia complanata Bentham
5–9
5
20–25
Red or purple
Sulphur-yellow
White, yellow or brown
Rose, purple or blue
Tillandsia didisticha (E. Morren) Baker
Tillandsia fendleri Grisebach
15–20
25–45
Red
Yellow or red
White
Blue-violet
mi2,3a
orn4
650–1400
Tillandsia ionochroma André ex Mez
Tillandsia kessleri H. Luther
Tillandsia cf. kuntzeana Mez
20
35
20–25
Red
Yellow
Blue or violet
Violet
Violet
orn4
orn4
orn3c
2700–3400
2100–3000
1700–3050
Tillandsia krukoffiana L. B. Sm.
Tillandsia loliacea Martius ex Schultes f.
Tillandsia pohliana Mez
10
6–10
18–25
Blue
Pale violet to yellow
White
orn4
mi4
mi4
Tillandsia recurvata (L.) L.
Tillandsia cf. reichenbachii Baker
Tillandsia cf. rusbyi Baker
10–13
7
30
Green
Pale violet or white
Blue-violet
White
mi4 , auto1
mi4
mi4
Tillandsia spiralipetala Gouda
Tillandsia streptocarpa Baker
Tillandsia tenuifolia L.
12
18–25
20
Green
Yellow-brown
Blue or purple
White, rose or blue
mi4
mi4
orn3a
500–1250
500–1550
800–2300
Tillandsia tricholepis Baker
Tillandsia usneoides (L.) L.
Tillandsia violascens Mez
7
9–11
7
Green
Yellow greenish
Pale green
Violet
mi4
mi4
mi4
500–1000
1200–2450
1300–1550
Vriesea maxoniana (L.B. Sm.) L. B. Sm.
Werauhia gladioliflora (Wendland) J. R. Grant
45
40–70
Greenish yellow
Green
Yellow
Greenish white
orn4
chi1b
300–1500
Red
Green to pale rose
Red
Pink to red
500
1250–2450
500–1800
2200
1100
500–1000
750–800
500–1000
500–600
500–1050
1000–1900
Elevational Patterns of Bromeliads 195
APPENDIX 2. Elevational distribution of hummingbird species observed along the study transects. Taxonomy and species sequence follow Remsen et al. (2005).
Species
Carrasco
Phaethornis ruber (Linnaeus)
P. stuarti Hartert
300–500
500–1000
P. pretrei (Lesson & DelLattre)
P. malaris (Nordmann)
Campylopterus largipennis (Boddaert)
300–2000
300–1500
Colibri delphinae (Lesson)
C. thalassinus (Swainson)
Anthracothorax nigricollis (Vieillot)
1500–2000
1000–3000
300–500
Klais guimeti (Bourcier)
Lophornis delattrei (Lesson)
500–1500
1500–2000
Chlorostilbon mellisugus (Linnaeus)
C. aureoventris (d’Orbigny & Lafresnaye)
Thalurania furcata (J. F. Gmelin)
2000–2500
300–1000
Hylocharis chrysura (Shaw)
Chrysuronia oenone (Lesson)
Amazilia chionogaster (Tschudi)
300–1000
500–1950
A. fimbriata (J. F. Gmelin)
Adelomyia melanogenys (Fraser)
Heliodoxa leadbeateri (Bourcier)
300–500
1100–3000
1500–2000
Aglaeactis pamela (d’Orbigny)
Coeligena coeligena (Lesson)
C. torquata (Boissonneau)
3000–3500
1100–2000
2000–3500
C. violifer (Gould)
Pterophanes cyanopterus (Fraser)
Patagona gigas (Vieillot)
2500–3500
2500–3500
3000–3500
Heliangelus amethysticollis (d’Orbigny & Lafresnaye)
Eriocnemis glaucopoides (d’Orbigny & Lafresnaye)
2000–3500
Ocreatus underwoodii (Lesson)
Sappho sparganura (Shaw)
Metallura tyrianthina (Loddiges)
1100–2000
2000–3500
M. aeneocauda (Gould)
Algaiocercus kingi (Lesson)
Schistes geoffroyi (Bourcier)
2500–3500
1100–2500
300–2000
Heliomaster longirostris (Audebert & Vieillot)
Microstilbon burmeisteri (P. L. Sclater)
Masicurı́
1100–1950
1100–1500
1500–1950
1100–1950
500
500–2500
500
1100–1950
1500–1950
2000–2500
300–500
500