| Literature DB >> 22829879 |
Nicolas Hubert, Renny Kurnia Hadiaty, Emmanuel Paradis, Laurent Pouyaud.
Abstract
The rainbowfishes of the family Melanotaeniidae represent one of the largest radiations of freshwater fishes from the Indo-Australian archipelago. A total of 75 nominal species have been described, among which several have become very popular among tropical fish hobbyists because of their tendency to form large schools of colourful individuals. Facing habitat loss and competition or predation by introduced species, this group has become a priority in the conservation of ornamental fishes in Indonesia. In this context, several expeditions have been conducted between 2007 and 2010 in Indonesian Papua with the aim to initiate a large-scale survey of the genetic resources in this group. We assessed the diversity of the Papua rainbowfishes with DNA barcoding. We sequenced the mitochondrial COI gene for 350 specimens belonging to 53 nominal species throughout the Indo-Australian archipelago. Unexpected levels of cryptic diversity and endemism were detected since additional cryptic lineages were detected in several watersheds from the Vogelkop and the Lengguru massif. DNA barcoding supports the presence of nearly 30 evolutionary lineages among the 15 nominal species sampled in the Vogelkop and all these lineages are endemic to a single lake or watershed. This result highlights that the diversity of the family has been largely underestimated and urges for the identification of conservation priorities in Papua.Entities:
Mesh:
Year: 2012 PMID: 22829879 PMCID: PMC3400673 DOI: 10.1371/journal.pone.0040627
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Figure 1Map of the sampling localities.
Figure 2Major clades identified by COI barcodes and their geographic distribution.
A, Neighbour-joining tree of 360 COI barcodes with the four major clades identified. B, Map of the four clade range distributions.
Summary of K2P distances with respect to taxonomic levels.
| Comparisons | n | taxa | Number of comparisons | Min | Mean | Max | SD |
| Within Species | 322 | 41 | 2293 | 0 | 0.65 | 2.99 | 0.016 |
| Within Genus, among species | 349 | 4 | 43597 | 0 | 9.20 | 17.00 | 0.019 |
| Within Family, among genus | 350 | 2 | 13145 | 0 | 12.19 | 18.78 | 0.017 |
| Within Order, among families | 350 | 1 | 1725 | 16.566 | 19.64 | 22.22 | 0.020 |
Data are from 350 sequences from 69 species, five genera and two families (Table S1).
Figure 3Distribution of the K2P distances within different taxonomic categories for the 350 individuals and 69 species analysed.
Summary of the rainbowfish diversity analysed in this study and distribution of the genetic distance of each of the 66 species of Melanotaenidae (genera Melanotaenia, Chilatherina and Glossolepis) to the nearest-neighbour at COI (K2P model used for computing distances).
| Taxa | Number of species | <0.1 | 0.1–1.0 | 1.0–2.7 | >2.7 |
|
| 53 | 8 | 18 | 14 | 13 |
|
| 6 | 0 | 4 | 1 | 1 |
|
| 7 | 0 | 7 | 0 | 0 |
| Clade IA | 16 | 1 | 9 | 5 | 1 |
| Clade IB | 10 | 2 | 5 | 2 | 1 |
| Clade III | 22 | 5 | 2 | 7 | 8 |
| Clade IV | 18 | 5 | 9 | 1 | 3 |
The clades listed here correspond to the four major groups identified in the neighbour-joining tree (Fig. 2 and S1) and detailed in Table S1.
Figure 4Distribution of the K2P distances to the nearest-neighbour, mean and maximum intra-specific distances.
Summary of the phylogenetic variability within and among the four major clades, clades age estimates according to three hypotheses of molecular calibration and calibrations of absolute substitution rates per millions years of COI sequences based on geology.
| Geological event age (Myr) | Calibration (substitution rates per Myr) | ||||||||
| Mean | SE | H1 | H2 | H3 | Min | Max | Min | Max | |
| within I | 0.059 | 0.005 | 11.8 | 4.9 | 3.0 | – | – | – | – |
| within IA | 0.033 | 0.004 | 6.6 | 2.8 | 1.7 | – | – | – | – |
| within IB | 0.032 | 0.004 | 6.4 | 2.7 | 1.6 | 1.65 | 3.4 | 0.0194 | 0.0094 |
| within III | 0.042 | 0.004 | 8.4 | 3.5 | 2.1 | – | – | – | – |
| within IV | 0.051 | 0.006 | 10.2 | 4.3 | 2.6 | – | – | – | – |
| I vs II | 0.137 | 0.013 | 27.4 | 11.4 | 6.9 | 8 | 11 | 0.017 | 0.012 |
| I vs III | 0.128 | 0.012 | 25.6 | 10.7 | 6.4 | 8 | 11 | 0.016 | 0.012 |
| I vs IV | 0.130 | 0.011 | 26 | 10.8 | 6.5 | 8 | 11 | 0.016 | 0.012 |
| II vs III | 0.137 | 0.014 | 27.4 | 11.4 | 6.9 | 8 | 11 | 0.017 | 0.012 |
| II vs IV | 0.126 | 0.012 | 25.2 | 10.5 | 6.3 | 8 | 11 | 0.016 | 0.011 |
| III vs IV | 0.105 | 0.010 | 21 | 8.8 | 5.3 | 8 | 11 | 0.013 | 0.010 |
| IA vs IB | 0.077 | 0.009 | 15.4 | 6.4 | 3.9 | – | – | – | – |
assuming a ‘minimum’ substitution rate of 0.005 substitution per Myr [38], [40].
assuming a ‘fish’ substitution rate of 0.012 substitution per Myr [39].
assuming a ‘vertebrate’ substitution rate of 0.02 substitution per Myr [38].
calibration based on the mean K2P distance among species within clade IB and assuming that most speciation event in clade IB are related with the uplift of the Mok ridge [41], [42].
estimated geological age for the uplift of the Lengguru arch [41], [42].
substitution rate estimated based on the calibration with the geological age for the uplift of the Mok ridge.