The Andean uplift is one of the major orographic events in the New World and has impacted considerably the diversification of numerous Neotropical lineages. Despite its importance for biogeography, the specific role of mountain ranges as a dispersal barrier between South and Central American lowland plant lineages is still poorly understood. The swan orchids (Cycnoches) comprise ca 34 epiphytic species distributed in lowland and pre-montane forests of Central and South America. Here, we study the historical biogeography of Cycnoches to better understand the impact of the Andean uplift on the diversification of Neotropical lowland plant lineages. Using novel molecular sequences (five nuclear and plastid regions) and twelve biogeographic models, we infer that the most recent common ancestor of Cycnoches originated in Amazonia ca 5 Mya. The first colonization of Central America occurred from a direct migration event from Amazonia, and multiple bidirectional trans-Andean migrations between Amazonia and Central America took place subsequently. Notably, these rare biological exchanges occurred well after major mountain building periods. The Andes have limited plant migration, yet it has seldom allowed episodic gene exchange of lowland epiphyte lineages such as orchids with great potential for effortless dispersal because of the very light, anemochorous seeds.
Neotropical landscape and biodiversity have long drawn the attention of naturalists1, 2. The tropical Andes are of particular interest as the world’s premier biodiversity hotspot, with both an extraordinary species richness and a remarkable level of endemism3,4,5. The combination of molecular phylogenies with species distributions and the fossil record has uncovered different biotic and abiotic factors that fostered diversification in the Neotropics6,7,8,9,10. Biogeographical studies applying modern phylogenetic methods on Neotropical plant clades (e.g. Begonia 11, Cyathostegia 12, Dioscorea 13, Heliotropium 14, Lupinus 15, 16, Arecaceae17, Orchidaceae18, Rubiaceae6) have generally demonstrated the importance of geological processes such as mountain building and establishing the Isthmus of Panama for the diversification of Neotropical plants19.
One of the most biologically important abiotic processes in the diverse geological history of the Americas is the rise of the Andes7, 14, 20. Andean mountain building was driven by plate tectonic re-adjustments that started during the Palaeogene and continued until the Pliocene7. The fossil record (e.g. palynological3, 21 and geological data: isotope measurements22, sediment loads, apatite fission-track data7) collectively indicate that the Andean uplift was a partially constant process punctuated by periods of intensified mountain building. Two of the most intense uplift periods occurred around 12 (mid-Miocene) and 4.5 million years ago (Mya; early Pliocene7). During these periods, the Northern Andes reached elevations as high as 4500 m in the Pliocene, whereas the Central Andes already peaked an altitude of 4500 m during the mid-Miocene7, 23.
Newly formed mountain ranges may had a strong impact on the adjacent Amazonian landscapes and the inhabiting organisms due to the transformation of its drainage systems24. The Andes also influenced local and regional climates by forming the only barrier to atmospheric circulation in the Neotropics25, 26. The rise of the Andes led to the formation of island-like habitats and of local microclimates and soil conditions that eventually fostered species diversification15, 27, 28. At the same time, the Andes provided physical and/or ecological barriers to species dispersal and migration. For instance, the efficiency of the Northern Andes as migration barrier is shown for Andean centred woody species of Crematosperma, Klarobelia, Malmea, and Mosannona (Annonaceae29). Propagules are dispersed by animals in these lineages30, and none of their constituent species occur in both east and west of the Andes mountain range29.
Recent phylogenetic studies provide solid evidence for the important role of Andean uplift in diversification of highland-dwelling plant groups (e.g. Lupinus 15; Bartsia 31; centropogonid Campanulaceae9). However, the impact of such orogenic processes for the lowland flora is still poorly understood4, 6, 32. Thus, the question remains whether Andean uplift has indeed been an abiotic barrier to migration for epiphytic lineages such as lowland orchids and bromeliads, both being important components of Neotropical forests.
Epiphytic diversity is dramatically greater in the Neotropics than in any other tropical region around the world33, 34, being twice as high than, for instance, in Australasia35,36,37,38. Several traits shared by Neotropical epiphytic taxa, and related to their reproductive biology, may explain such overwhelming differences in diversity. One of the most prominent shared traits is the lightness and the very small size of the propagules, occasionally with highly elaborated surfaces (e.g. bromeliads, ferns, orchids, Pinguicula 35). The potential of dust-like seeds for rare longer distance dispersals by wind might be greater compared with other plants with propagules locally dispersed by animals (e.g. Araceae39). Indeed, detailed studies on epiphyte orchid seed dispersal and gene flow provide evidence for the rarely long distance exchange of orchid propagules between geographical areas40,41,42. Nonetheless, the frequency and tempo of lowland epiphyte migrations across geological barriers such as the Andes remains largely unknown. Well-sampled phylogenies for epiphyte clades have been lacking to address this issue.
Several wind-dispersed plant lineages (e.g. Begonia 11; bromeliads43) span across the Neotropical region, many of which are restricted to lowland elevations. One example is the orchid tribe Cymbidieae comprising ca 3900 species that are mostly distributed in the Neotropics (but with few representatives in the Old World Tropics44). To Neotropical Cymbidieae belong the swan orchids (Cycnoches) that are known for the striking sexual dimorphisms45 and pollination syndrome46. Molecular phylogenetics and morphological studies conducted to date confirm the inclusion of Cycnoches within Catasetinae47,48,49 and its sister group relationship to Mormodes 45, 50, 51.
Cycnoches encompasses 34 species of epiphytes52 that are distributed from Southern Mexico to Central Brazil and Bolivia. Its species are best represented in the Amazonian forests of Brazil, Ecuador, and Peru, but also in the Llanos and Caribbean regions of Colombia and Venezuela52, 53. They commonly inhabit lowland tropical wet forests, ranging from 0 to 800 m. Cycnoches species are pollinated by male euglossine bees, which collect volatile compounds produced by flowers but also from other sources (e.g. rotten wood, faeces46). They have rather a restricted geographical range, and most of them are distributed in single biogeographical areas. Nevertheless, one species (C. chlorochilon) is distributed on both sides of the Northern Andes52.
Because of the striking sexual system they have evolved45, swan orchids have long attracted the attention of several prominent naturalists including Charles Darwin54. Despite this long interest, previous phylogenetic studies have only been included up to three species of Cycnoches probably because of their scarceness both in the wild and in herbarium collections47, 48, 50, 51, 55. The lack of a solid and well-sampled phylogeny of Cycnoches, has precluded addressing specific questions concerning the role of Andean uplift in their biogeographical history, a question urged by their distribution on the two sides of the Andes. The narrow geographical distribution of almost all extant Cycnoches species and their restricted habitat preference given (i.e. lowland wet forests), we expect the swan orchids diversification to be strongly influenced by the Andean uplift. In particular, we hypothesize that Andean uplift restricted genetic exchange in Cycnoches, as already reported for other plant lineages6, 13, 29. To test this hypothesis, we generated a strongly supported 5-loci phylogeny, sampling 23 out of 34 accepted Cycnoches species and comprising its known diversity and distribution, and performed models of biogeographical analyses.
Phylogeny of Cycnoches
Our phylogeny comprised 23 out of 34 accepted species of Cycnoches. Table S5 provides detailed alignment descriptions. The concatenated nuclear alignment was 2395 bp in length and included 310 parsimony informative sites, and the concatenated plastid alignment was 2419 bp and comprised 171 parsimony informative positions. Independently derived nuclear and plastid phylogenies revealed topologies with conflicting and highly supported phylogenetic placements. PACo analysis revealed 22 potential outlier OTUs (see below; Figs S1 and S2) belonging to eleven species of Cycnoches (19 outliers), one species of Dressleria, and two of Mormodes. After inspection of the potentially conflicting OTUs placement in nuclear and plastid phylogenies (Fig. S2), 20 outliers were confirmed as conflicting terminals (Tab. S6) and were excluded from the concatenated nuclear-plastid DNA matrix. Thus, only two terminals (i.e. Dressleria severiniana and one representative of C. lehmannii) were misclassified by PACo as conflicting (Figs S1 and S2; see Appendix S1 for a detailed explanation on outlier handling).
Within Cycnoches, the nuclear phylogeny recovered three maximally supported clades (A, B, C; Fig. 1). Clade A included all sequenced accessions of Cycnoches hagii and was recovered as sister group of the remaining species of Cycnoches comprising clades B and C. By contrast, the plastid phylogeny showed two main maximally supported clades (namely I and II), each including a set of intermingled species from clades A, B, and C. The best ML tree inferred from the non-conflicting, concatenated nuclear and plastid dataset, showing the internal phylogenetic relationships of Cycnoches, is presented in Figure 2. Almost all internal nodes of the backbone phylogeny were highly, if not maximally supported by Maximum Likelihood Bootstrap Support (MLBS) and Posterior Probability (PP) values. Cycnoches segregated into three main lineages (clades A, B and C). Clade A (i.e. all specimens of C. haagii) was sister group of the remaining species of Cycnoches clustering in clades B and C.
Molecular dating of Cycnoches
Comparison of marginal likelihood estimates (MLE) of tree priors and clock models revealed that an uncorrelated molecular clock combined to a birth-death tree prior with incomplete sampling best fitted our data (MLE of –14244.47; Tab. 1). Nevertheless, Bayes factors (BF) clearly rejected the strict clock models (BF = 72, 45, and 40 for all tree priors), but did not provide strong evidence to support an incomplete sampling birth-death model vs a standard birth-death model (BF = 1.08; Tab. 1). Analysis of the log file produced by dating analyses under the relaxed clock and tree models are also shown in Table 1. Overall, they yielded CV values between 0.35 and 0.42 (indicating there was among branch rate heterogeneity, which argued for the use of a relaxed molecular clock). Therefore, results obtained from a dated phylogeny with relaxed molecular clock and birth-death standard speciation model (Tab. 1) are presented only (Figs 3 and S4).
A chronogram showing absolute ages estimated under a relaxed clock is presented in Figure 3 (see also Fig. S4 for the 95% confidence intervals) and shows that Cycnoches and Mormodes shared a common ancestor during the beginning of the late Miocene (9.1 Mya ± 3). Diversification of Cycnoches took place around 5 Mya ± 2 at end of the late Miocene. The split between Cycnoches clades B and C occurred during late Pliocene (3 Mya ± 2), whereas both clades were estimated to be of Pleistocene ages (1.2 and 1.6 Mya ± 1, respectively).
Ancestral area estimations
Table 2 provides ML statistics for the biogeographical models as inferred in BioGeoBEARS. The best fitting model was the BAYAREA star, including the founder-event speciation. This model revealed Amazonia as the most likely ancestral area of Cycnoches (Figs 3 and S5). The MRCA of clades B and C was reconstructed to have inhabited in the Amazonian region. The MRCA of clade C occurred in Central America, whereas the MRCA of clade B inhabited in Amazonia region.
We inferred three independent trans-Andean migration events between Amazonia and Central America. The first migration from Amazonia to Central America took place towards the late Pliocene (±1 Mya), after the divergence of MRCAs of clades B and C. A second migration from Central America to Amazonia took place around mid-Pleistocene (±1 Mya) by the MRCA of C. maculatum, C. manoelae, C. peruvianum, C. quatuorcristis, and C. suarezii. The last biotical exchange from Amazonia to Central America was dated to late Pleistocene (±0.5 Mya) with the MRCA of C. chlorochilon, C. ventricosum, and C. warszewiczii.
Influence of Andean orogeny on the biogeography of a Neotropical epiphyte group
Our study provides a solid phylogenetic framework for the evolution of Cycnoches in time and space. Central America has been considered the most likely region of Cycnoches origin, probably because of its locally elevated species richness as compared to other areas in the Neotropics56. However, our analyses reject this evolutionary scenario, which instead support a South American origin of Cycnoches in the late Miocene (ca 5 Mya ±2; Figs 3 and S5). The estimated ancestral area of Cycnoches MRCA largely reflects the current distribution of early diverging lineages such as C. haagii, a species today distributed in Amazonia and the Guiana Shield.
The early diversification of Cycnoches has taken place well after the most intense mountain building events of the Northern and Central Andes ca 12 and 10 Mya, respectively7, 57,58,59, and our results indicate a less limiting role of the Andes as a biogeographic barrier for the diversification of Cycnoches. Two migrations from Amazonia to Central America and one reverse colonisation event imply rare, ancient dispersals across the Andes during last 5 million years (Fig. 3). During the early Pliocene (i.e. the period when Cycnoches has started to diversify), the Northern Andes of Colombia and Venezuela have already reached elevations up to at least 3000 m7. Moreover, three migrations from Amazonia to Central America and back, respectively, took place ~2 Mya, when the Northern and Central Andes already peaked at a mean elevation of 4000 m (see mean Andean elevation displayed in the inset of Fig. 3). Such dispersals might have been assisted by vegetation expansions and contractions due to dramatic temperature changes after the mid-Miocene climatic optimum6, 27 that are known to have affected the distribution ranges of lineages in Central and South America60. These changes in vegetation ranges might have shortened the distances between populations distributed in either side of the Andes.
Similar trans-Andean migrations are reported for bromeliads43, ferns32, and more recently in Cymbidieae orchids18. In Bromeliaceae (subfamily Bromelioideae), direct migrations from the Brazilian Shield towards Central America have taken place around 7 Mya43, a period where Northern Andes reached a paleoelevation of ~2000 m7. Furthermore, biotical exchanges between South and Central America have also been reported in the fern complex Jamesonia-Eriosorus 32. Here, migrants from the Brazilian coast colonized and further established in Central Andes, and from there subsequently migrated towards Central America during the late Pleistocene61. In Cymbidieae orchids, direct migrations from Amazonia to Central America in Catasetinae and Zygopetalinae were inferred to have taken place early during the evolutionary history of such lineages during middle Miocene (~15 Mya18). During this time period, Colombian and Venezuelan Andes peaked a mean elevation of ca 1100 m7.
The Andes does not appear to be a limiting barrier of genetic exchange for Neotropical epiphyte lineages such as Cycnoches compared with zoochorous groups (e.g. Annonaceae29, Rubiaceae6). The rapid colonisation of Central America and Amazonia may be related to the biology of the group having anemochorous seed dispersal and an epiphytic habit. Most orchid seeds are characterized by their minute size and reduced weight, as well as by their elaborated seed coats42, 62. These traits allow them to easily remain airborne for extended periods of time and might promote rare long distance dispersals over geographical barriers62. Our results of ancestral area estimations provide support for these seldom migrations across the Andes. Moreover, Cycnoches species might have good dispersal potential as well because of their seeds, which are between 100–300 µm long, 50–60 µm wide, and about 3–4 µg weight42, 63.
Phylogenetic conflict between nuclear and plastid phylogenies in Cycnoches
Our study brings important insights for the species relationships within Cycnoches. Previous phylogenetic studies about Catasetinae have included not more than three species of Cycnoches 47, 48, 50, 51, 55, hence keeping internal relationships (and corresponding conflicts, see below) of the lineages unresolved. Serious phylogenetic incongruence between nuclear and plastid tree topologies of Catasetinae has been firstly identified by Pérez-Escobar and colleagues64, but the plausibility of the trees were not discussed before.
All major clades in our nuclear phylogeny are consistent with morphological concepts of Cycnoches (Fig. 1a). Cycnoches haagii (Clade A) differs from other Cycnoches species by the fleshy oblong, curved pair set of calli located towards the base of the labellum. Clade B includes species with conspicuously large male flowers and an entire to 4-lobed labellum blade. Clade C comprises species with proportionately small male flowers and labella with 8–10 marginal projections53. The consistency between molecules and morphology is challenged by an apparent correlation between the plastid molecular tree and the distributions of particular lineages (Fig. 1b): Clade I comprises species occurring mostly in Amazonia, Caribbean-Llanos, and Guiana shield regions (except C. chlorochilon and C. warszewiczii present in Costa Rica and Panama). Clade II, in turn, includes species exclusively distributed in Central America and Chocó regions.
Topological incongruence between phylogenies derived from different genomes is a widespread phenomenon in phylogenetic inferences65,66,67,68,69. Examples from several angiosperm lineages (e.g. Araceae39, Asteraceae70, Saxifragaceae71) have long revealed conflicting patterns, in which the nuclear phylogeny is in accordance with morphology, whereas the plastid relationships correlate to geographical distributions. The nuclear-morphological and plastid-geographical phylogenetic relationship patterns recovered in Cycnoches follow this phenomenon, which might be associated to the genetic exchange promoted by seeds vs pollen. More importantly, the differential levels of gene flow facilitated by seed and pollen dispersal, and the transmission modes of plastids, may explain the incongruences observed between nuclear and plastid datasets67. Here, the lower genetic exchange promoted by seed dispersal72, 73 support the conserved geographical structure in the (maternally inherited74, 75) plastid phylogeny, while the congruence of morphological traits with the (biparentally inherited) nuclear tree might be related with the higher levels of genetic exchange facilitated by pollen67, 76.
Another process with explanatory power for the nuclear-plastid conflict observed in the clade is hybridization. Euglossine-bee-pollinated orchids such as Cycnoches produce a blend of volatile compounds, which attracts male Euglossine bees, and pollination takes place while bees collect such compounds produced by specialized tissues in the flower77. Species-specific production of floral blends and therefore attraction of a unique set of pollinator(s) has been accounted as an isolative reproductive barrier in Euglossine bee pollinated orchids46, 78. Nevertheless, intra-specific variation of fragrances produced by the flower has been reported in several orchid lineages such as Stanhopea 79 and even Cycnoches 80. Fragrance variation may result on attraction of a set of pollinators that are shared by species co-occurring in the same biogeographical region (e.g. C. dianae, C. guttulatum, and C. pachydactylon 80) with similar composition of the fragrance profile, providing an opportunity to hybridization to occur. Little is known about pollinators of Cycnoches, but our own observations of pollinator sharing between species and presence of polymorphic species may argue for the possibility of past hybridization processes.
Based on a solid, comprehensively sampled phylogeny we provide macroevolutionary evidence for a South American origin of Cycnoches. Our biogeographical analysis indicates colonization of Central America via a direct migration from the Amazonian basin. More importantly, the analyses support three recent trans-Andean, bidirectional migration processes between Central America and Amazonia, which is indicative for plausibility of rare long distance dispersals in lowland epiphytic orchids, and suggest a less limiting role of the Andean barrier on swan orchids migration. Consequently, our study enlightens the semi-permeability of Andean mountain building on the range evolution and diversification of lowland Neotropical epiphytic lineages. Our study paves the way for detailed studies on the effect of Andean orogeny in population gene flow of epiphytic orchids occurring at both sides of the range.
Material and Methods
Taxon sampling, DNA sequencing, and phylogenetic analyses
Species names, geographical origins, voucher specimens, and GenBank accession numbers of sequences included in phylogenetic analyses are provided in Table S1. Our study builds-up upon previous DNA data matrices43, 51, 63. Genomic DNA was extracted from herbarium and fresh leaf material with the NucleoSpin plant kit (Macherey-Nagel; Düren, Germany). We amplified and sequenced nuclear ribosomal external and internal transcribed spacers (ETS and ITS, respectively), and a fragment of the Xdh gene. We also sequenced a ~1500 bp fragment of the plastid gene ycf1, as well as the trnS–trnG intergenic spacer. Amplification and sequencing settings, as well as sequencing primers used for ITS, ETS, Xdh, trnS–trnG, and ycf1, are the same as previously reported64, 81 (Tab. S2). In this study, 84 sequences were newly generated (Tab. S1).
Loci were aligned separately using MAFFT 7.182. For nuclear ribosomal RNA loci and plastid trnS–trnG spacer, secondary structure of molecules was taken into account (i.e. the -qINSi option). Congruence between nuclear and plastid datasets was assessed as previously done by Pérez-Escobar and colleagues64, and using PACo83. The procedure is available as a pipeline (http://www.uv.es/cophylpaco/) and was also employed to identify operational terminal units (OTUs) from the plastid dataset that are in conflict with the nuclear dataset (potential outliers detected by PACo are shown in Figs S1 and S2). A detailed explanation on PACo and a rationale on outlier handling is provided as Extended Materials and Methods of Appendix S1.
Phylogenetic analyses of separate and concatenated loci were carried out under maximum likelihood (ML) and Bayesian inference (BI). The best-fitting evolutionary models for ML and Bayesian analyses (for each data partition) were selected using jModelTest v.2.1.684, relying on a Likelihood Ratio Test (LRT) and the Akaike information criterion (AIC) (Tab. S3). Phylogenetic inference relied on the ML approach implemented in RAXML-HPC v.8.2.485 and BI as implemented in MRBAYES v.3.2.286 and were carried out on the CIPRES Science Gateway computing facility87. Bayesian inferences were performed with two independent runs, each with four Markov chains Monte Carlo (MCMC) running for 30 million generations each, and sampled every 1000th generation (all other prior settings by default). Log files derived from MRBAYES were examined, and the convergence of MCMC was assessed using TRACER (available at: http://tree.bio.ed.ac.uk/software/tracer/). Node support values were assessed for both the ML tree using MLBS and the consensus Bayesian tree using PP.
Molecular clock dating
A few orchid macrofossils are available for Orchidaceae88, 89, but these are assigned to lineages very distantly related to our groups of interest. Using distant outgroups to calibrate our Cycnoches phylogeny would have created extensive sampling heterogeneities, which can result in spurious results90. Thus, we had to rely on secondary calibrations. In order to obtain the best secondary calibration points possible, we first generated an Orchidaceae-wide fossil-calibrated phylogeny, sampling 316 orchid species as representatively as possible along the tree. Loci, number of sequences, and settings for absolute age estimation of the Orchidaceae-wide fossil calibrate phylogeny are provided in the Extended Materials and Methods of Appendix S1. The ages obtained were very similar to recent orchid dating studies91, 92, and the dated phylogeny is shown in Figure S3.
We selected two secondary calibrations for dating of Cycnoches: (i) the crown group of Catasetinae was set to 19.8 Mya with a standard deviation of 4 to reflect the 95% CI, and (ii) and the root of the Cycnoches tree (i.e. MRCA of Cyrtopodium + Catasetinae) was set to 27.1 Mya with a standard deviation of 6. To explore the clock-likeness of the data, we used both strict clock and uncorrelated lognormal clock models, and compared different tree priors (pure-birth, standard birth-death, and incomplete sampling birth-death). For strict molecular clock calibration, we placed a single constraint only at the tree root (27.1 Mya with a standard deviation of 6) using a normal distribution. The best-fitting tree speciation model was selected using Bayes factors calculated from marginal likelihoods computed for every model using the stepping-stone sampling93 (Tab. 1). For each clock model, we ran two MCMC analyses with 20 million generations each, sampled every 1000th generation. For the relaxed molecular clock analyses, we estimated the coefficient of variation (CV) to inform us on the rate heterogeneity among branches (CV approaching zero indicates that a strict clock model cannot be rejected). Parameter convergence was confirmed using TRACER (http://tree.bio.ed.ac.uk/software/tracer/). All dating analyses were performed at the CIPRES Science Gateway computing facility87.
Ancestral area estimations
Species ranges of Cycnoches were coded from the collection site and/or type locality of the material sequenced, which reflect the distribution ranges for every taxon included in our phylogeny (except for C. chlorochilon and C. pentadactylon, which also occur in Central America and Southeastern South America, respectively; see below). Representative taxa from Catasetum, Cyrtopodium, Galeandra, and Mormodes (~36% of the total species sampling - 17 species) that cover the distribution range of Cycnoches, were chosen as outgroup for biogeographical analyses. Coding matrix for ingroup and outgroup taxa is provided in Appendix S1. Distribution data of Cycnoches and outgroup taxa were obtained from own field observations, literature94, 95 and from herbarium specimens (Herbaria AMES, COL, F, M, MO, SEL, US); this information was employed to code outgroup distribution ranges.
Biogeographical areas were derived from distribution maps of the orchids under investigation as well as species distributions observed in other plant lineages (e.g. Rubiaceae6; Bromeliaceae43). We coded for eight biogeographical areas using the R-package ‘SpeciesGeocodeR’96: (1) Central America comprising southern Mexico through Panama; (2) Caribbean-Llanos comprising the coastal northernmost areas and plains of Colombia and Venezuela97; (3) Guiana Shield encompasses areas above 800 m in Colombia, Venezuela, Brazil, Guyana, Suriname, and French Guiana; (4) Amazonia encompassing lowlands and pre-montane forest below 800 m in Colombia, Ecuador, Peru, Brazil, Venezuela, Guyana, Suriname, and French Guiana6; (5) Chocó comprising lowlands below 500 m of the western Andes in Colombia and Ecuador; (6) Northern Andes including elevated areas above 800 m from Southernmost Peru to Northern Colombia and Northeast Venezuela; (7) Central Andes comprising areas above 800 m in Northern Peru to Northern Chile and Northeast Argentina; (8) South-eastern South America encompassing part of the Brazilian shield, the Atlantic forest, South-eastern Bolivia, Paraguay, Uruguay, and Northern Argentina.
To infer ancestral areas in Cycnoches, we used the R-package ‘BioGeoBEARS’ (Biogeography with Bayesian and Likelihood Evolutionary Analysis in R script98). Using BioGeoBEARS, we tested the fit of six biogeographic models with and without founder-event speciation (or jump speciation), altogether testing the role and contribution of evolutionary processes that were taken into account to explain today’s observed distributions (i.e. range expansions, local extinctions, founder-event speciation, vicariance, and speciation despite sympatry) in a joint statistical framework. It is therefore capable of model testing and of determining, which process fits better the geographical and phylogenetic data for any particular clade.
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We are grateful to Martina Silber (Munich, Germany) for valuable assistance in the lab; to Susanne S. Renner, and two anonymous reviewers for discussion; to Mario Blanco (San José, Costa Rica), Diego Bogarín (San José, Costa Rica), Norman Cash and family (Managua, Nicaragua) for the great help provided during field trip, to Boris Schlumpberger (Hannover, Germany), Andres Maduro (Panama City, Panama), Ivan G. Alvarez (David, Panama), Lankester Botanical Garden (Cartago, Costa Rica), Gustavo Romero (Herbarium HUH, Cambridge, U.S.A) and University of Costa Rica for providing plant material. We also thank the Smithsonian Tropical Research Institute (Panama City) and Costa Rican Ministry of Environment (MINAET) for providing research permits (No. SE/AP-20-13 and 026-2013-SINAC, respectively). This work was supported by the Colombian Administrative Department of Science and Technology (COLCIENCIAS; granted to OAPE). We thank the Deutsche Forschungsgemeinschaft (grants GE828/12-1, GO1459/8-1) for financial support.
The authors declare that they have no competing interests.
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Pérez-Escobar, O.A., Gottschling, M., Chomicki, G. et al. Andean Mountain Building Did not Preclude Dispersal of Lowland Epiphytic Orchids in the Neotropics. Sci Rep 7, 4919 (2017). https://doi.org/10.1038/s41598-017-04261-z
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