| Literature DB >> 30128183 |
Matthew A Campbell1, D Ross Robertson1, Marta I Vargas1, Gerald R Allen2, W O McMillan1.
Abstract
We investigated a pantropical sub-family and genus of damselfishes, the sergeant-majors (Pomacentridae: Abudefdufinae: Abudefduf), to identify the tempo and mechanisms of speciation in the lineage. We examined sequence capture data from 500 loci and 20 species, with multiple individuals sampled from across the geographic ranges of widespread species. Utilizing a maximum likelihood framework, as well as a time-calibrated Bayesian phylogeny, the following key questions are addressed: What is the historical tempo of speciation? What are the relative contributions of vicariant, peripatric and parapatric speciation to sergeant-major diversity? How is speciation related to major variation in trophic ecology? The approximately 20 species of sergeant-majors fall into three main lineages. The ancestral condition appears to be benthivory, which is predominant in two lineages comprising six species. The remaining species of sergeant-majors, of which there are at least 15, fall within a clade composed entirely of planktivores. This clade is sister to a benthivore clade that included one species, Abudefduf notatus, in transition to planktivory. Most speciation of sergeant-majors, which appeared ∼24 million years ago, occurred in the last 10 million years. Present distributional patterns indicate vicariant speciation precipitated by the closure of land barriers between both sides of the Atlantic and the Pacific, and the emergence of land between the Indian and Pacific Oceans. Within this backdrop, frequent oscillations in sea level over the last 10 million years also appear to have generated conditions suitable for both peripatric and vicariant speciation, and most speciation within the genus appears linked to these changes in sea level. Diversification within the genus has been concentrated in planktivorous seargeant-majors rather than benthivores. The root cause is unclear, but does not appear to be related to differences in dispersal potential, which is greater in the planktivorous species, due to the ability of their post-larval juveniles to raft with floating debris. This elevated speciation rate in planktivores and their propensity to form local endemics may reflect relaxation of selective pressures (e.g., on crypticity) that limit speciation in benthivorous sergeant-majors. Finally, our data allow us to clarify relationships of geminate sergeant-major species, indicating that there are subdivisions within the Atlantic for both benthivore and planktivore geminate pairs that may have misled previous studies.Entities:
Keywords: Abudefdufinae; Feeding mode; Isthmus of Panama; Phylogenetics; Sergeant-majors; Vicariance
Year: 2018 PMID: 30128183 PMCID: PMC6097498 DOI: 10.7717/peerj.5357
Source DB: PubMed Journal: PeerJ ISSN: 2167-8359 Impact factor: 2.984
Figure 1Maximum likelihood phylogenetic tree of Abudefduf.
A maximum likelihood phylogenetic tree of Abudefduf generated from partitioned analysis of 361 ultraconserved element (UCE) loci. An optimal partitioning strategy was implemented (Lanfear et al., 2014; Lanfear et al., 2012). Each partition was modeled under the General Time Reversible (GTR) model of sequence evolution with gamma-distributed rate variation (Γ). Bootstrap support values are indicated with an asterisk (*) if equal to 100. The three lineages of Abudefduf are indicated (Clade A, B and C). Planktivorous lineages are highlighted and named in red with benthivorous lineages highlighted and named in blue. The tree is rooted by pomacentrid outgroups of the genera Chromis and Similiparma. The branch leading to an undescribed species, A. cf. vaigiensis, is colored gray. Appended to each leaf in the tree is the approximate geographic location of the sequenced individual using these abbreviations: EA, East Atlantic; WA, West Atlantic; EP, East Pacific; CP, Central Pacific; WP, West Pacific; EIO, East Indian Ocean; and WIO, West Indian Ocean. Individual identifiers are appended to sample names in Fig. S1. Photo credits: A. hoefleri S. Floeter, A. saxatilis DRR, A. troschelii GRA, A. conformis J. Randall, A. vaigiensis GRA, A. abdominalis GRA, A. sparoides GRA, A. sexfasciatus J. Greenfield (CC BY), A. natalensis J. Randall, A. whitleyi GRA, A. bengalensis G. Edgar (CC BY), A. lorenzi GRA, A. margariteus GRA, A. cf. vaigiensis J. Earle, A. notatus GRA, A. septemfasciatus GRA, A. sordidus GRA, A. taurus DRR, A. concolor GRA, A. declivifrons GRA.
Figure 2Time-calibrated phylogenetic tree of Abudefduf.
A time-calibrated phylogenetic tree of Abudefduf generated from 137 ultraconserved element (UCE) loci modeled under a single partition with the General Time Reversible (GTR) model with gamma-distributed rate variation (Γ). Fossil-calibrated nodes are indicated by black triangles and are described in Table S2. Posterior support at nodes is 1.00 unless otherwise indicated. Blue bars indicate 95% highest posterior density. The major trophic guilds are indicated by shading of red for planktivores and blue for benthivores. Regional endemics are indicated by a dagger (†). Invidual samples included in this analysis are indicated in Table S1. Vertical lines indicate 25 million year time divisions with 10 million years and 3 million years also indicated. Appended to each leaf in the tree is the approximate geographic location of the sequenced individual using these abbreviations: EA, East Atlantic; WA, West Atlantic; EP, East Pacific; CP, Central Pacific; WP, West Pacific; EIO, East Indian Ocean, and WIO, West Indian Ocean.
Figure 3Phylogenetic relationships of Abudefduf saxatilis and A. hoefleri samples sequenced in this study rooted by A. troschelii.
A maximum likelihood tree was generated by optimal partitioning (Lanfear et al., 2014; Lanfear et al., 2012) with each partition modeled with the General Time Reversible (GTR) model of sequence evolution and gamma-distributed rate variation (Γ). Values at nodes are bootstrap support values. Collection sites of samples are indicated after names and the general geographic area of collection indicated.