Systematic and historical biogeography of the Bryconidae (Ostariophysi: Characiformes) suggesting a new rearrangement of its genera and an old origin of Mesoamerican ichthyofauna
© Abe et al.; licensee BioMed Central Ltd. 2014
Received: 8 April 2014
Accepted: 30 June 2014
Published: 8 July 2014
Recent molecular hypotheses suggest that some traditional suprageneric taxa of Characiformes require revision, as they may not constitute monophyletic groups. This is the case for the Bryconidae. Various studies have proposed that this family (considered a subfamily by some authors) may be composed of different genera. However, until now, no phylogenetic study of all putative genera has been conducted.
In the present study, we analyzed 27 species (46 specimens) of all currently recognized genera of the Bryconidae (ingroup) and 208 species representing all other families and most genera of the Characiformes (outgroup). Five genes were sequenced: 16SrRNA, Cytochrome b, recombination activating gene 1 and 2 and myosin heavy chain 6 cardiac muscle. The final matrix contained 4699 bp and was analyzed by maximum likelihood, maximum parsimony and Bayesian analyses. The results show that the Bryconidae, composed of Brycon, Chilobrycon, Henochilus and Salminus, is monophyletic and is the sister group of Gasteropelecidae + Triportheidae. However, the genus Brycon is polyphyletic. Fossil studies suggest that the family originated approximately 47 million years ago (Ma) and that one of the two main lineages persisted only in trans-Andean rivers, including Central American rivers, suggesting a much older origin of Mesoamerican ichthyofauna than previously accepted.
Bryconidae is composed by five main clades, including the genera Brycon, Chilobrycon, Henochilus and Salminus, but a taxonomic review of these groups is needed. Our results point to a possible ancient invasion of Central America, dating about 20.3 ± 5.0 Ma (late Oligocene - early Miocene), to explain the occurrence of Brycon in Central America.
The order Characiformes contains approximately 2000 species distributed among 23 families, with 19 exclusively Neotropical families and four exclusively African families [1–3]. The order comprises one of the largest freshwater fish radiations. Among characiform genera, Brycon is one of the most speciose, containing 42 species [4, 5]. Members of this genus occur from southern Mexico to Panama, across the trans-Andean South American river basins from northern Peru to the Maracaibo system in Venezuela, in all major river drainages in cis-Andean South America, and in most Atlantic and Caribbean coastal river basins . Brycon species are medium- to large-sized fishes, with a maximum standard length from 15 cm (Brycon pesu) to approximately 70 cm (Brycon orbygnianus and Brycon amazonicus). Brycon species are important food fishes throughout Central and South America , with catches estimated to approximately 5,100 tons for the year 2007 in Brazil .
Despite their wide distribution, species diversity, and commercial importance, the taxonomy of the Bryconidae remains unclear. Species in Panama and the trans-Andean rivers of northern South America were extensively studied by Eigenmann , Hildebrand  and Dahl . In contrast, the taxonomy of Brycon species in the cis-Andean river basins was revised by Lima  in an unpublished master's thesis. Lima  published a taxonomic synthesis of the Bryconinae, which, in addition to the genus Brycon, included two monotypic genera: Chilobrycon Géry & Rham, 1981 and Henochilus Garman, 1890.
The phylogenetic relationships within the Bryconidae have been the subject of several studies; however, a detailed hypothesis of the relationships among its species and with other Characiformes is absent. Regan  was the first author to propose a relationship between Brycon and Chalceus. In the same study, he further proposed that Salminus and Hystricodon (=Exodon) were related to Brycon. Eigenmann  proposed the classification of the subfamily Bryconinae, including the genera Brycon and Chalceus. Géry  proposed that the Bryconinae instead be classified as the subfamily Chalceinae; however, in 1972, Géry  followed the Bryconinae classification and divided the subfamily in three tribes: Bryconini, Triportheini and Salminini. The same classification scheme was used in Géry´s  seminal book on characiforms.
In a comparative osteological study of Brycon and Salminus, Roberts  suggested that the apparent similarities between them may reflect the primitive position of Brycon. Uj  proposed a new classification, the family Bryconidae, which included Brycon, Chalceus, Catabasis, Lignobrycon, Salminus, Triportheus, Chilobrycon and Bryconexodon. Mirande  recognized the subfamily Bryconinae, comprised of Brycon, Triportheus, Chilobrycon, Henochilus, and Lignobrycon. The latter three genera were not studied by Mirande ; however, whereas Chilobrycon and Henochilus are recognized as closely related to Brycon, Lignobrycon appears distinct, and the absence of representatives of this genus may be responsible for the unusual result reported by the author. Molecular data [1, 19–21] supports the close relationship between Brycon and Salminus proposed by Uj . In the broadest molecular phylogenetic study of the Characiformes published to date, Oliveira et al. analyzed specimens of Brycon, Henochilus and Salminus and recognized them as a monophyletic group, the family Bryconidae.
Given the importance of the Bryconidae among the Characiformes, as stated above, two mitochondrial and three nuclear genes of representatives of all genera of this family, along with representatives of all other Characiformes families [as defined by 1], were analyzed in the present study to formulate a hypothesis of the relationships among species and genera of the Bryconidae and between this family and the other Characiformes. In addition, a time-calibrated tree was constructed to investigate the temporal relationships between the origin of Bryconidae groups and the main geological events in South America.
Selection of taxa and delineation of the ingroup and outgroup
Species of Bryconidae analyzed in the present phylogenetic study
Position in Figure 1
Laguna de Castilleros, Venezuela
07º30'50.9''N 66º09'19.8'' W
Rio Tomo, Colombia
04°25'27.1'' N 69°17'12.5'' W
Rio Negro, Amazonas, Brazil
03°05'05.2''.S 59°47'23.7'' W
Brycon aff. atrocaudatus
Rio Santa, Peru
08°40’24.0'' S 78°09'16.3'' W
Río Llano Sucio, Panama
09°19’26.2'' N 79°46'08.2'' W
Laguna de Castilleros, Venezuela
07º30’50.9” N 66º09’19.8” W
Rio Machado, Rondônia, Brazil
10°43'36.0' S 61°55'12.9'' W
Rio Negro, Amazonas, Brazil
00°08'09.4" S 67°05'03.4" W
Brycon cf. falcatus
Rio Culuene, Mato Grosso, Brazil
13°49'00.0'' N 53°15'08.0'' W
Rio Mucuri, Minas Gerais, Brazil
17°41'42.4' S 40°46'11.3'' W
Rio Mucuri, Minas Gerais, Brazil
17°41'42.4' S 40°46'11.3'' W
Lagoa da Égua, Mato Grosso, Brazil
13°20'05.1'' S 50°42'16.2'' W
Rio Negro, Mato Grosso do Sul, Brazil
19°34'33.7' S 56°14'49.5'' W
Rio Cuiabá, Rio São Lourenço, Mato Grosso, Brazil
17°50’45.3'' S 57°24'11.7'' W
Rio Cuiabá, Mato Grosso, Brazil
15°54'50.0’ S 56°02'07.0' W
Lagoa Feia, Rio de Janeiro, Brazil
22°00'00.0'' S 41°20'00.0'' W
Rio Amazonas, Iquitos, Peru
03°48'11.5' S 73°13'12.4'' W
Rio Rancheria, Colombia
11°0' 23.57 N 74°14'48.80'' W
Rio Cauca, Antioquia, Colombia
07°57'28.5'' N 75°12'00.0'' W
Rio Paraná, São Paulo, Brazil
20°55'27.90'' S 51°37'32.62'' W
Rio Capivari, Minas Gerais, Brazil
21° 30' 16.0" S 44°34' 29" W
Rio Itagaçaba, São Paulo, Brazil
22°39'26.3'' S 44°45'49.8'' W
Rio dos Prazeres, São Paulo, Brazil
23°35'43.8'' S 45°34'08.0'' W
21°59'45.74'' S 47°25'36.57' W'
Rio São Francisco, Minas Gerais, Brazil
18°11'28.50" S 45°14'51.42" W
Rio das Garças, Mato Grosso, Brazil
15°54'18.1'' S 52°19'24.2'' W
Rio Jari, Amapá, Brazil
00°34’11” S 52°33’19'' W
Rio Guamá, Pará, Brazil
01°34'00.5'' S 47°09'51.4'' W
Río Llano Sucio, Panama
09°19’26.2'' N 79°46'08.2'' W
Rio Mucuri, Minas Gerais, Brazil
17°41'42.4' S 40°46'11.3'' W
Estação de Piscicultura da CEMIG, Minas Gerais, Brazil
15°31'19.0'' S 41°30'18.0'' W
Rio Tumbes, Peru
03°48'17.9'' S 80°29'52.5'' W
Rio Santo Antônio, Minas Gerais, Brazil
17°53 60.00'' S 40° 13'0.00'' W
Rio Cauca, Antioquia, Colombia
07°57'28.5'' N 75°12'00.0'' W
Rio Mogi-Guaçu, São Paulo, Brazil
21°55' 37.60'' S 47°22'4.40'' W
Rio São Francisco, Minas Gerais, Brazil
18°11'21.0' S 45°15'10.3'' W
Rio Paranapanema, São Paulo, Brazil
23°20' S 48°34' W
Rio Tapirapé, Pará, Brazil
05° 22' 22.30'' S 49°07'0.94'' W
Molecular data collection
Total DNA was extracted from ethanol-preserved muscle samples using the DNeasy Tissue Extraction Kit (Qiagen), following the manufacturer’s instructions. Partial sequences of the mitochondrial genes 16SrRNA and Cytochrome b (Cytb) and the nuclear genes recombination activating gene 1 (Rag1), recombination activating gene 2 (Rag2) and myosin, heavy chain 6, cardiac muscle, alpha (Myh6) were amplified by polymerase chain reaction (PCR) with the same primers utilized by Oliveira et al.. Amplifications were performed in a total volume of 25 μl consisting of 2.5 μl of 10X buffer (10 mM Tris-HCL + 15 mM MgCl2 buffer), 0.5 μl of MgCl2 (50 mM), 0.5 μl of each primer (5 μM); 0.4 μl of dNTPs (200 nM of each), 0.2 μl of Taq Platinum polymerase (Invitrogen; 5 U/μl), 1 μl of template DNA (10-50 ng) and 19.4 μl of ddH2O. The thermo-cycler profile used for the fragments 16SrRNA and Cyt b consisted of 35 cycles, 30 s at 95°C, 45-120 s at 50-55°C (according to primer and species), and 90 s at 72°C. Nested-PCR was used to amplify the nuclear genes Rag1, Rag2 and Myh6. Amplification conditions for these genes in both rounds of PCR consisted of 15 cycles, 30 s at 95°C, 45 s at 56°C (according to primer), and 30 s at 72°C followed by 15 cycles, 30 s at 95°C, 45 s at 54°C (according to primer), and 90 s at 72°C. PCR products were purified using ExoSap-IT® (USB Corporation), sequenced using the “Big DyeTM Terminator v 3.1 Cycle Sequencing Ready Reaction Kit” (Applied Biosystems), purified again by ethanol precipitation and loaded into an automatic sequencer 3130-Genetic Analyzer (Applied Biosystems) at Instituto de Biociências, Universidade Estadual Paulista, Botucatu, São Paulo, Brazil. Contigs were assembled and edited in BioEdit 184.108.40.206 . In cases of unclear nucleotide identity, IUPAC ambiguity codes were applied. All obtained sequences were deposited in GenBank (Table 1).
Alignment and phylogenetic analyses
Sequences of each gene were aligned using the Muscle algorithm under default parameters  and the alignments inspected by eye for any obvious misalignments that were subsequently corrected. A quality control step was included in our workflow as described in Oliveira et al.. Genetic distances among sequences were calculated in Mega 5.04 . To evaluate the occurrence of substitution saturation, we estimated the index of substitution saturation (Iss) in DAMBE 5.2.31  as described in Xia et al. and Xia and Lemey .
Comparison of log likelihoods, AIC and BIC values among different partitioning schemes (from 1 to 13 partitions)
Number of partitions*
Number of parameters
Maximum parsimony (MP) analyses were conducted with PAUP* 4.0b10 . Heuristic searches were performed with minimally 1000 random addition replicates and TBR branch swapping. All characters were unordered, all character transformations were equally weighted, and branches with a maximum length of zero were collapsed. Gaps were treated as missing data since experiments were they were treated as a fifth base did not result in better resolved trees. Clade robustness was assessed using 1000 bootstrap pseudoreplicates  with the same parameters as described above.
RAxML , running in the web servers RAxML-HPC2 on TG [33, 34], was used for all maximum likelihood analyses with a mixed partition model. Random starting trees were ran for each independent ML tree search, and all other parameters were set to default values. All ML analyses were conducted following the 13 partitions sch. as suggested by the AIC and BIC (Table 2). Topological robustness was investigated using 1000 non-parametric bootstrap replicates.
Phylogenetic analyses using a partitioned Bayesian inference were conducted in MrBayes 3.1.2 . A mixed model analysis was implemented, allowing individual models of nucleotide substitution to be estimated independently for each partition. Because MrBayes 3.1.2 only implements 1, 2, and 6 substitution rate models, it was often not possible to implement the preferred model as selected by the AIC. In these situations, the nearest overparameterized model was used to avoid the negative consequences of model violation or underparameterization [28, 36]. As a consequence, the model for all partitions was set as “lset nst = 6” and “rates = invgamma” (G + I), with the commands “unlink” and “prset ratepr = variable” used to unlink the model parameters across the data partitions and define a rate multiplier for each partition. Two independent Bayesian analyses were conducted. Four independent MCMC chains were run with 30,000,000 replicates each, with one tree sampled every 1000 steps. The distribution of the log likelihood scores was examined to determine stationarity for each search and decide if extra runs were required to achieve convergence using the program Tracer 1.4 . Initial trees estimated prior to convergence were discarded as part of the burn-in procedure, and the remaining trees were used to construct a 50% majority rule consensus tree in PAUP*.
The estimation of divergence times in the inferred phylogeny was carried out using BEAST (Bayesian evolutionary analysis sampling trees) 1.8.0  on a reduced dataset that included the family Bryconidae and representatives of the families Gasteropelecidae and Triportheidae. To calibrate our molecular tree we followed the guideline proposed by Parham et al. . Initially, two fossils were chosen: Lignobrycon ligniticus and Brycon avus. Lignobrycon ligniticus (Woodward, 1898) (type specimen: BMNH P9012) was described in the genus Tetragonopterus and moved to Lignobrycon by Eigenmann and Myers . Malabarba  in a phylogenetic study showed that L. ligniticus is the sister group of L. myersi (a species included in our phylogeny) and these two species are the sister group of Triportheus. Brycon avus (Woodward, 1898) (type specimen: BMNH P9224) was described in the genus Tetragonopterus and moved to Brycon by Travassos and Silva . Malabarba ( – unpublished thesis) showed that B. avus is placed within the genus Brycon but its relationships with the remaining species of this genus was not resolved which make very difficult its use in our phylogeny. Considering that B. avus does not meet all criteria proposed by Parham et al.  we discuss it putative relationship with the species we analyzed in the present study but we did not use it to calibrate our trees.
These two species were described based on complete specimens collected in the Tremembé Formation, Taubaté Basin, São Paulo, Brazil. Geological studies  have confirmed the age of this formation as Oligocene, as also suggested by studies in mammalian fossils  and pollens [46, 47]. According to the International Commission on Stratigraphy (http://www.stratigraphy.org) Oligocene extended from 33.9 to 23.03 million years ago (Ma). These dates were implemented in BEAST with a log-normal prior offset with a mean and standard deviation of 28.5 ± 5.5. We used a birth-death model for the speciation likelihood and a random starting tree. The analysis was run for 50 million generations and sampled every 10000th generation. Stationarity and sufficient mixing of parameters (ESS > 200) were checked using Tracer 1.5 . A consensus tree was built using TreeAnnotator v 1.6.2 .
Partial sequences of two mitochondrial (16SrRNA and Cytb) and three nuclear genes (Myh6, Rag1 and Rag2) were obtained for 254 specimens, 41 of which were sequenced in the present study (Additional file 1). The final matrix contained 4699 bp and was deposited in TreeBase (http://www.treebase.org) under number 15409 and in DRYAD (http://www.datadryad.org - http://datadryad.org/resource/doi:10.5061/dryad.kt24p).
Information content and characteristics of each gene partition
Number of sequences
bp after alignment
Number of variable sites
Number of informative characters under parsimony
% informative characters under parsimony
Overall mean genetic distance (p-distance)
0.122 ± 0.008
0.216 ± 0.007
0.083 ± 0.004
0.108 ± 0.004
0.110 ± 0.004
0.134 ± 0.002
Nucleotide substitution model
GTR + I + Γ
TN93 + I + Γ
T92 + I + Γ
K2P + I + Γ
K2P + I + Γ
GTR + I + Γ
α (shape) parameter of Γ distribution
Proportion of invariants (I) sites
Six different partitioning schemes, ranging from one to 13 partitions (Table 2), were tested to establish the optimal number of data partitions (following ) for the final analysis. The results showed that the 13 partition model was the best choice; however, ML analysis conducted with the other partitioning schemes produced the same final topology, with minor differences in branch length and support values (data not shown).
Phylogenetic relationships of the Bryconidae
Estimates of divergence times of Bryconidae clades
Phylogenetic relationships among the Bryconidae and other Characiformes taxa
Our study represents the first phylogenetic analysis in which all genera currently assigned to the Bryconidae [1, 4] were investigated. Our results indicate that Brycon, Chilobrycon and Henochilus belong to a monophyletic group, as suggested by Lima . Our study also corroborates the hypothesis that Salminus is closely related to Brycon[1, 17, 20, 21, 50, 51].
All of our analyses identified the Bryconidae as the sister group of the clade composed of the families Gasteropelecidae and Triportheidae This is an interesting result, as our previous study  suggested that the Bryconidae may be the sister group of the Gasteropelecidae. These different results appear to be due to the larger number of representatives of the Bryconidae in the present analysis, emphasizing the importance of using a large number of taxa in phylogenetic studies.
According to Weitzman , the presence of expanded coracoids in Triportheus and the so-called subfamily Gasteropelecinae is likely due to convergent evolution; i.e., they arose independently in these groups. This view was adopted by several other authors, such as Castro and Vari  and Mirande . Thus, our results are inconsistent with the current morphology-based topology that identifies the Triportheidae and the Gasteropelecidae as non-sister groups. However, based on morphological analyses, Gregory and Conrad  suggested that "Chalcinus (=Triportheus) is much the nearer to the structural ancestor of Gasteropelecus", a hypotheses similar to that found in the present study. In contrast, the putative relationship between Triportheus and the Bryconidae, is supported by several authors, including Malabarba  and Mirande . However, considering that the support in MP studies was lower than 50% further studies involving more samples and more genes will be necessary for a better discussion about the relationships of these families.
Phylogenetic position of Salminus
Salminus is an economically and ecologically important genus, composed of medium to large fishes. Members of the genus are found throughout most of South America, including one trans-Andean representative, S. affinis. The taxonomic history of Salminus is complex. In the first review of the genus, Eigenmann  recognized S. affinis (Magdalena River and Upper Amazonas), S. hilarii (Paraná, São Francisco, Amazon and Orinoco Rivers), S. maxillosus (La Plata basin), and S. brevidens (São Francisco River). Presently, four species are recognized: S. affinis (trans-Andean species from Magdalena, Rancheria and Sinú Rivers, Colombia), S. hilarii (São Francisco, Upper Paraná river basins, Araguaia, Tocantins, Upper Amazonas and Orinoco Rivers), S. brasiliensis (La Plata Basin, Jacuí River and Upper Madeira river basin), and Salminus franciscanus[56–59]. A morphological distinction among specimens of S. hilarii from São Francisco and Upper Paraná river basins and those from Araguaia, Tocantins, Upper Amazonas and Orinoco Rivers was observed by Lima  and thus in the present study the first group is here identified as S. hilarii and the second as Salminus sp.
Morphological studies do not suggest a close relationship between Salminus and Brycon[4, 16, 18, 57]. Géry , without a phylogenetic analyses, included the tribe Salminini in the subfamily Bryconinae. Our study corroborates previous molecular hypothesis that identify Salminus as closely related to Brycon[1, 20, 21, 51, 60]. Moreover, our results show that Salminus is a genus interspersed among Brycon species, as observed by Calcagnotto et al..
Our phylogeny is the first published hypothesis of the evolutionary history of this genus and shows that Salminus hilarii is the sister group of all remaining species and that Salminus sp. and S. affinis and S. brasiliensis and S. franciscanus are sister species. However, Lima  reported similar results in his unpublished thesis.
Phylogenetic relationships among Bryconidae species
According to our results, the family Bryconidae consists of five main clades. The first clade is composed of four trans-Andean species of Brycon and Chilobrycon. B. chagrensis is the sister group of all remained species in this clade. After this we have B. petrosus in the BEAST analysis and B. henni in the ML analysis as a sister group to a monophyletic lineage with two clades, one composed of B. aff. atrocaudatus and B. henni (B. petrosus) and the second consisting of C. deuterodon. In their description of the genus Chilobrycon, Géry and Rham  suggested that this genus belongs to the subfamily Bryconinae and can be differentiated from Brycon species primarily by the presence of spatulated and tricuspid teeth and the absence of an upper lip. Although several trans-Andean species of Brycon were not available for analysis in the present study, the species B. chagrensis was described by Kner (1863) as Chalcinopsis chagrensis that was considered a junior synonymous of B. chagrensis and thus the whole taxonomy of this group need to be revised.
The second clade is composed of all the species of Salminus, as discussed above. The third clade consists of four samples of Brycon pesu. Eigenmann  proposed that the genus Holobrycon include Brycon pesu Müller & Troschell, 1841, because adult specimens of this genus lack a fontanel, unlike that observed in all Brycon species. Thus, our data reinforce Eigenmann's proposition that Holobrycon represents a valid genus; however, these nomenclature changes require close evaluation in future studies.
The fourth clade is comprised of one trans-Andean species of Brycon (B. moorei) and several Brycon species from the Amazon, Orinoco, São Francisco, and Paraná-Paraguay Rivers. The inclusion of B. moorei in this clade and the presence of Brycon species in our first clade show that the cis- and trans-Andean Brycon spp. are not monophyletic. The relationship among cis-Andean species of this clade was not resolved in the present study. Notably, the species B. orthotaenia, B. orbignyianus and B. hilarii are morphologically very similar (FCT Lima, pers. comm.).
The fifth clade is composed of two lineages: the first contains B. melanopterus, B. falcatus, and B. cf. falcatus (Amazon and Orinoco) and the second comprises B. nattereri (upper Paraná), B. opalinus, B. insignis, B. vermelha, B. ferox, Brycon sp., and Henochilus from Brazilian coastal rivers. The sister relationship of B. melanopterus, B. falcatus, and B. cf. falcatus was expected, as the three species are very similar morphologically. The Brycon species from coastal rivers are also morphologically similar (FCT Lima, pers. comm.). The close relationships among those species inhabiting Brazilian coastal regions is interesting as the Eastern Brazilian coastal rivers were connected many times during the Neogene and Quaternary , and ancestor groups may have spread throughout this area.
Based on recently collected specimens, Castro et al. re-described Henochilus wheatlandii and analyzed its relationship with other characiforms using sequences of the genes 12S and 16S. Their results indicated a close relationship between Brycon and Henochilus, as did those of Hilsdorf et al.. Henochilus is morphologically very similar to Brycon and Chilobrycon, with fewer tooth series. This trait may be an autapomorphy of this species .
Origin and diversification of Bryconidae groups
The study of the distribution patterns of freshwater fishes in association with historical biogeography provides an excellent opportunity to test alternative models of evolution of hydrographic basins . Fossil characiforms were described from South America, Africa, Europe, and the Arabian Peninsula . Additionally, a putative characiform fossil was described from Canada . The main lineages of Neotropical freshwater fishes were present in South America by the Lower Cretaceous, and much of their diversification occurred before or during the Paleogene [67–69]. Molecular analyses of Citharinoidei  also corroborate the hypotheses of the origin of the order Characiformes as the Lower Cretaceous. Conversely, Eocene-Oligocene articulated specimens of characiforms from the Entre-Córregos Formation, southern Minas Gerais State, eastern Brazil, were described as Tremembichthys sp., cf. Brycon avus, and an undetermined Characidae . More recently, Weiss et al. described two characiforms from this same locality: Paleotetra entrecorregos and P. aiuruoca. From the Tremembé Formation (Oligocene), five characiform species were described, all based on articulated specimens: Lignobrycon ligniticus, Megacheirodon unicus, Brycon avus, Cyphocharax mosesi, and Plesiocurimata alvarengai. Two other species, Procharax minor and Lignobrycon altus, were described based on poorly preserved specimens from the Plio-Pleistocene sediments of Nova York shales (northern Brazil) .
Using the information available for Lignobrycon ligniticus, that met all suggested points signaled by Parham et al.  regarding the use of fossils to calibrate molecular trees, we estimate the origin of the Bryconidae at 46.7 ± 11.8 Ma (Figure 4), corresponding to the Eocene-Paleocene. According to López-Fernandes and Alberts , major marine regressions exposed large areas of interior floodplains during the Oligocene (as in earlier epochs), allowing dramatic and sometimes rapid expansion of freshwater habitats. The formation of the so-called "foreland basin"  may have permitted the rapid expansion of a primitive Bryconidae throughout the proto-Paraná and proto-Amazon system.
Within the Bryconidae, clade 1 originated 37.5 ± 9.7 Ma. This clade is composed of trans-Andean species, including Chilobrycon deuterodon and B. aff. atrocaudatus from Peru, B. henni from Colombia, and Brycon chagrensis and B. petrosus from Panama. The last closure of the Panama Isthmus is generally considered to have occurred between 3.1-2.8 Ma [75, 76]. However, some alternative hypotheses regarding faunal exchanges between Central and South America have been proposed. According to Haq et al., during the lower middle Miocene, sea levels were generally very high, but two sea-level drops of almost 100 m may have occurred between 17 and 15 Ma, which could have permitted the migration of fish from South to Central America. Recent geological studies [78, 79] suggest that the Panamanian land bridge may be much older (ca. 23-25 Ma). The GAARlandia hypothesis  proposes that a geological connection was present between the central part of Central America and South America 32 Ma, formed via a land bridge between the Greater Antilles and the Aves Islands Ridge. Finally, a Cretaceous Island Arc  has been proposed linking Central America, the Greater Antilles, and South America 80–70 Ma. Some have argued that this Cretaceous Island Arc may have persisted until 49 Ma .
Although some previous molecular studies suggest that some primary freshwater fishes from Central America originated after the formation of the Panama landbridge at the end of Tertiary [83, 84], an earlier colonization of Mesoamerica has been proposed for other freshwater fishes [85–90]. Additionally, molecular studies of terrestrial taxa support a late Oligocene/early Miocene land connection between Central and South America [91–96]. Thus, although our molecular clock may be limited by the absence of older Bryconidae fossils and, potentially, additional samples, the results obtained are in accordance with an ancient invasion of Central America, dating at least from the origin of the ancestor of B. chagrensis, 20.3 ± 5.0 Ma and could be related with the changes in sea level during the lower middle Miocene . However, the hypothesis of multiple invasions, as proposed by Reeves and Bermingham , is also in accordance with our data since the ancestor of B. petrosus originated at 10.1 ± 2.8 Ma (Figure 4).
Clade 2, comprised exclusively of Salminus, originated 29.6 ± 7.8 Ma (Figure 4). A recent Salminus fossil found in eastern Argentina was dated as from the early late Miocene (Tortonian - 7.1 to 11.2 Ma) , consistent with our hypotheses. The first cladogenesis in this group gave origin to the ancestor of S. hilarii and the ancestor of the remaining lineages. S. hilarii has a restricted distribution in the Upper Paraná and São Francisco Rivers . Our data suggest that the split between lineages of S. brasiliensis (in the Paraná, Paraguay and Uruguay River basins and adjacent areas) and S. franciscanus (São Francisco River basin) occurred at 5.9 ± 1.8 Ma (Figure 4). In his study of Hypostomus, Montoya-Burgos  identified a separation time of his samples from the Paraná and São Francisco Rivers (Clade D3) of between 5.7 and 6.4 Ma, a result similar to that of the present study and that of Beurlen (1970; cited by ), who suggested that a connection between these basins may have been present from the Tertiary until 1.8 Ma. The cladogenesis that gave origin to Salminus sp. (Amazon basin) and S. affinis (Magdalena River basin) occurred at 3.6 ± 1.5 Ma (Figure 4). According to Hoorn et al., the most intense periods of formation of the northern Andean mountains occurred from the late middle Miocene (~12 Ma) to early Pliocene (~4.5 Ma), a timeframe close to the putative separation time we identified between Salminus sp. and S. affinis.
Clade 3, consisting of Brycon pesu, originated 26.7 ± 6.4 Ma. Although this clade is represented by a single species in our study, recent analysis have shown that it is a species complex, composed by several underscribed species (FCT Lima, pers. comm.). This clade is widely distributed throughout the Amazon and Orinoco River basins, as well as in rivers from Guyana, Suriname and French Guiana , but our specimens are only from the Amazon basin. Our data suggest a rapid diversification within the last 6.7 ± 2.0 Ma. This period approximately coincides with the final formation of the Amazon and Orinoco drainages  and other coastal drainages in north South America. Additional analysis with samples from other drainages and the possible new species will be necessary to better understand the diversification of this group.
Clades 4 and 5 originated 22.3 ± 6.0 Ma. Clade 4 has two main lineages. Brycon moorei (Magdalena River basin) ancestor diverged from the other species at 18.2 ± 4.8 Ma. This old separation time coincides with the first peak of mountain building in the Northern Andes (late Oligocene to early Miocene, approximately 23 Ma), coinciding with the diversification of the first modern mountain plant and animal genera . Although in our general phylogeny (Figure 3) the remained species in the clade 4 were not statistically well separated in all analyses the Bayesian inference suggest that several lineages originated in different times. Thus, B. orthotaenia (São Francisco River basin) ancestor diverged from the other species of this group at 15.2 ± 4.0 Ma (Figure 4). Several authors have suggested that the fish fauna of the São Francisco basin are a hybrid combination of groups from adjacent basins [100, 101]. Thus, the present data suggest that those connections may have been present since the early Miocene. B. amazonicus (Amazon, Orinoco and Essequibo River basins) ancestor diverged from B. hilarii (Paraguay River basin) 12.6 ± 3.3 Ma (Figure 4). According to Lundberg et al., the headwater capture of the Upper Paraguay by the Amazonas occurred due to the shift south to the Michicola Arch, 11.8 - 10.0 Ma, a time period very close to that we found. The divergence of B. orbygnianus (La Plata River basin) ancestor from B. gouldingi ancestor (Tocantins River basin) 10.7 ± 3.1 Ma may also have occurred after the shift of the Michicola Arch.
In clade 5, Brycon falcatus (Amazon and Orinoco River basins and rivers in Guyana, Suriname and French Guiana), B. cf. falcatus (Culuene River, a tributary of Xingu River) and B. melanopterus (Amazon River basin) ancestors diverged approximately 18.4 ± 5.2 Ma from the remaining species of this clade that inhabit the Paraná-Paraguay, São Francisco and coastal rivers in eastern Brazil (Figure 4). This time coincides with the formation of Chapare Buttress, a structural divide that formed between the paleo-Amazonas-Orinoco and Paraguay basins 30 - 20 Ma .
The divergence of B. falcatus ancestor from the Orinoco River (sample number 15563) from B. falcatus ancestor from the Negro River (sample number 32395) occurred 4.4 ± 1.4 Ma (Figure 4). Studies in the Callichthyinae have shown that specimens of Hoplosternum litoralle and Megalechis picta from the Amazon and Orinoco diverged approximately 11.7 to 6 Ma, respectively . These data are in accordance with the separation of the Amazon and Orinoco with the formation of Vaupes Arch (late Miocene) and subsequent changes up until the Holocene, when the Andean mountains attained their present configuration .
The remaining species in clade 5 are restricted to the Upper Paraná and São Francisco Rivers (Brycon nattereri) and coastal rivers (B. opalinus, Henochilus wheatlandii, B. vermelha, B. insignis, B. ferox and Brycon sp.) and originated 15.1 ± 3.9 Ma (Figure 4). In this group, B. opalinus from the Paraiba do Sul River is the sister group of the remaining species. This species occurs in the area of the Tremembé formation (Oligocene), where the fossils Brycon avus and Lignobrycon ligniticus were found . Considering B. avus as an Oligocene species it is more possible that it is the sister group of clades 3 to 5 than close relative to the Brycon species that today inhabit the Brazilian coastal area. A future phylogenetic analyses including this species will be necessary to test this hypotheses.
The relationship between the Brycon species of the Amazon and south coastal rivers (clade 5) may be due to the dispersal of a now extinct form from the Paraguay River that dispersed from the south northward into Paraguay and the south coastal rivers as could be B. avus. The other species in this group diverged more recently (end of the Miocene and Pliocene), and events such as global climate oscillations and eustatic sea-level fluxes  may have produced ancient connections among these coastal rivers, allowing species dispersion and speciation.
In summary, our results align with several geological events in South America, but suggest an old colonization of Central America. However, further studies that include several as yet unsampled Brycon species are necessary to better understand the relationships among some lesser known species such as B. coquenani, B. polylepis and B. whitei, which could provide new insights into the relationships among Brycon species as well as the origin of some taxa.
Bryconidae is composed by five main clades, including the genera Brycon, Chilobrycon, Henochilus and Salminus, but a taxonomic review of these groups is needed. Our results points to a possible ancient invasion of Central America, dating about 20.3 ± 5.0 Ma (late Oligocene/early Miocene), to explain the occurrence of Brycon in Central America.
The authors thank all individuals who assisted us in the collection and identification of the specimens studied here, with special thanks to Dr. Mauro Nirchio, Universidad de Oriente; Hernan Ortega, Museo de Historia Natural, Universidad Nacional Mayor de San Marcos; and Dr. Oris Sanjur, Smithsonian Tropical Research Institute for donations of tissue samples and help with a collection expedition. Special thanks go to Dr. Flávio Lima for his friendly assistance in species identification and thoughtful review and comments on the manuscript. KTA, TCM, and GSA were supported by the Fundação de Amparo à Pesquisa do Estado de São Paulo – FAPESP (06/06749-0, 10/17999-2, 06/05744-4, respectively). CO is a CNPq (Conselho Nacional de Desenvolvimento Científico e Tecnológico do Brasil) researcher (CNPq grant number 309632/2007-2).
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